1
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Piecha M, Kreyling J, Couwenberg J, Pester M, Guenther A, Henningsen L, Weil M, Jurasinski G, Blume-Werry G, Urich T, Wang H. Plant roots but not hydrology control microbiome composition and methane flux in temperate fen mesocosms. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 940:173480. [PMID: 38796012 DOI: 10.1016/j.scitotenv.2024.173480] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/20/2024] [Revised: 05/21/2024] [Accepted: 05/22/2024] [Indexed: 05/28/2024]
Abstract
The rewetting of formerly drained peatlands can help to counteract climate change through the reduction of CO2 emissions. However, this can lead to resuming CH4 emissions due to changes in the microbiome, favoring CH4-producing archaea. How plants, hydrology and microbiomes interact as ultimate determinants of CH4 dynamics is still poorly understood. Using a mesocosm approach, we studied peat microbiomes, below-ground root biomass and CH4 fluxes with three different water level regimes (stable high, stable low and fluctuating) and four different plant communities (bare peat, Carex rostrata, Juncus inflexus and their mixture) over the course of one growing season. A significant difference in microbiome composition was found between mesocosms with and without plants, while the difference between plant species identity or water regimes was rather weak. A significant difference was also found between the upper and lower peat, with the difference increasing as plants grew. By the end of the growing season, the methanogen relative abundance was higher in the sub-soil layer, as well as in the bare peat and C. rostrata pots, as compared to J. inflexus or mixture pots. This was inversely linked to the larger root area of J. inflexus. The root area also negatively correlated with CH4 fluxes which positively correlated with the relative abundance of methanogens. Despite the absence or low abundance of methanotrophs in many samples, the integration of methanotroph abundance improved the quality of the correlation with CH4 fluxes, and methanogens and methanotrophs together determined CH4 fluxes in a structural equation model. However, water regime showed no significant impact on plant roots and methanogens, and consequently, on CH4 fluxes. This study showed that plant roots determined the microbiome composition and, in particular, the relative abundance of methanogens and methanotrophs, which, in interaction, drove the CH4 fluxes.
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Affiliation(s)
- Marc Piecha
- Department of Bacterial Physiology, Institute of Microbiology, 17489 Greifswald, Germany
| | - Juergen Kreyling
- Experimental Plant Ecology, Institute of Botany and Landscape Ecology, 17489 Greifswald, Germany
| | - John Couwenberg
- Experimental Plant Ecology, Institute of Botany and Landscape Ecology, 17489 Greifswald, Germany
| | - Michael Pester
- Department of Microorganisms, Leibniz Institute, German Collection of Microorganisms and Cell Cultures GmbH, 38124 Braunschweig, Germany; Institute of Microbiology, Technical University of Braunschweig, 38106 Braunschweig, Germany
| | - Anke Guenther
- Landscape Ecology, Faculty of Agricultural and Environmental Sciences, University of Rostock, 18059 Rostock, Germany
| | - Levke Henningsen
- Experimental Plant Ecology, Institute of Botany and Landscape Ecology, 17489 Greifswald, Germany
| | - Micha Weil
- Department of Bacterial Physiology, Institute of Microbiology, 17489 Greifswald, Germany
| | - Gerald Jurasinski
- Landscape Ecology, Faculty of Agricultural and Environmental Sciences, University of Rostock, 18059 Rostock, Germany; Peatland Science, University of Greifswald, 17489 Greifswald, Germany
| | - Gesche Blume-Werry
- Experimental Plant Ecology, Institute of Botany and Landscape Ecology, 17489 Greifswald, Germany; Department of Ecology and Environmental Sciences, Umeå University, 901 87 Umeå, Sweden
| | - Tim Urich
- Department of Bacterial Physiology, Institute of Microbiology, 17489 Greifswald, Germany
| | - Haitao Wang
- Department of Bacterial Physiology, Institute of Microbiology, 17489 Greifswald, Germany.
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2
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Pan Z, Yang S, Lou H, Gong J, Zhou B, Wang H, Li H, Li J, Dai Y, Yi Y, Gao C, Huang X. Small reservoirs can enhance the terrestrial carbon sink of controlled basins in karst areas worldwide. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 951:175517. [PMID: 39147046 DOI: 10.1016/j.scitotenv.2024.175517] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/21/2024] [Revised: 08/12/2024] [Accepted: 08/12/2024] [Indexed: 08/17/2024]
Abstract
The concentration of Greenhouse Gas (GHG) in the atmosphere has sharply increased since the Industrial Revolution, leading to climate warming and severe environmental problems. It has become a consensus that GHG emissions of large reservoirs essentially constitute inland aquatic GHG emissions. However, questions remain regarding whether small karst reservoir (SKR) is only a substantial source of GHG emissions like large reservoirs, and how much GHG emission it can offset by affecting the terrestrial carbon sink (TCS) of its controlled basin. We selected two basins in the karst area of southwestern China, with built and planned SKRs, and quantitatively analysed the impact of the SKR on basin-scale water and carbon cycles during 2000-2020 using multi-source remote sensing data and the Google Earth Engine. Results showed that the associated increase in the TCS in the SKR-controlled basin can completely offset the GHG emissions and TCS losses caused by submerged land, resulting in a 21.48 % faster increase rate of TCS and a 12.20 % greater increase in TCS caused by human activities than in non-karst reservoir basin. Meanwhile, by intercepting both surface and groundwater runoff, the SKR-controlled basin showed a 329.55 % faster increase rate of available surface water resources than the non-karst reservoir basin, alleviating the problem of engineering water shortages and enhancing the drought resistance capacity. Moreover, in the three major karst areas worldwide, and especially in southwestern China, faster vegetation restoration and TCS increase exist in most SKR-controlled basins, and this increase is enhanced with increasing proximity to the water surface. This study revealed that SKR is more than a substantial source of GHG emissions; it can also effectively enhance the TCS and available surface water resources in controlled basin, which is of great significance for achieving carbon neutrality goals while maintaining the sustainability of water and carbon cycle in karst areas.
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Affiliation(s)
- Zihao Pan
- College of Water Sciences, Beijing Normal University, Beijing 100875, China
| | - Shengtian Yang
- College of Water Sciences, Beijing Normal University, Beijing 100875, China
| | - Hezhen Lou
- College of Water Sciences, Beijing Normal University, Beijing 100875, China.
| | - Jiyi Gong
- College of Water Sciences, Beijing Normal University, Beijing 100875, China; College of Life Sciences, Guizhou Normal University, Guiyang 550025, China
| | - Baichi Zhou
- College of Water Sciences, Beijing Normal University, Beijing 100875, China
| | - Huaixing Wang
- College of Water Sciences, Beijing Normal University, Beijing 100875, China
| | - Hao Li
- College of Water Sciences, Beijing Normal University, Beijing 100875, China
| | - Jiekang Li
- College of Water Sciences, Beijing Normal University, Beijing 100875, China
| | - Yunmeng Dai
- College of Water Sciences, Beijing Normal University, Beijing 100875, China
| | - Yin Yi
- College of Life Sciences, Guizhou Normal University, Guiyang 550025, China
| | - Chengcheng Gao
- Guiyang Water Resources and Hydropower Survey, Design and Research Institute, Guiyang 550081, China
| | - Xueyong Huang
- Guiyang Water Resources and Hydropower Survey, Design and Research Institute, Guiyang 550081, China
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3
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Nijman TPA, van Giersbergen Q, Heuts TS, Nouta R, Boonman CCF, Velthuis M, Kruijt B, Aben RCH, Fritz C. Drainage effects on carbon budgets of degraded peatlands in the north of the Netherlands. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 935:172882. [PMID: 38697540 DOI: 10.1016/j.scitotenv.2024.172882] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/15/2023] [Revised: 04/03/2024] [Accepted: 04/27/2024] [Indexed: 05/05/2024]
Abstract
Peatlands store vast amounts of carbon (C). However, land-use-driven drainage causes peat oxidation, resulting in CO2 emission. There is a growing need for ground-truthing CO2 emission and its potential drivers to better quantify long-term emission trends in peatlands. This will help improve National Inventory Reporting and ultimately aid the design and verification of mitigation measures. To investigate regional drivers of CO2 emission, we estimated C budgets using custom-made automated chamber systems measuring CO2 concentrations corrected for carbon export and import. Chamber systems were rotated among thirteen degraded peatland pastures in Friesland (the Netherlands). These peatlands varied in water table depth (WTD), drainage-irrigation management (fixed regulated ditch water level (DWL), subsurface irrigation, furrow irrigation, or dynamic regulated DWL), and soil moisture. We investigated (1) whether drainage-irrigation management and related hydrological drivers could explain variation in C budgets, (2) how nighttime ecosystem respiration (Reconight) related to hydrological drivers, and (3) how C budgets compared with estimates from Tier 1 and Tier 2 models regularly used in National Inventory Reporting. Deep-drained peatlands largely overlapped with C budgets from shallow-drained peatlands. The variation in C budgets could not be explained with drainage-irrigation measures or annual WTD, likely because of high variation between sites. Reconightincreased from 85 to 250 kg CO2 ha-1 day-1 as the WTD dropped from 0 to 50 cm across all sites. A deeper WTD had no apparent effect on Reconight, which could be explained by the unimodal relationship we found between Reconight and soil moisture. Finally, C budgets estimated by Tier 1 emission factors and Tier 2 national models mismatched the between-site and between-year variation found in chamber-based estimated NECBs. To conclude, our study showed that shallow WTDs greatly determine C budgets and that regional C budgets, which can be accurately measure with periodic automated chamber measurements, are instrumental for model validation.
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Affiliation(s)
- Thomas P A Nijman
- Department of Ecology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ, Nijmegen, the Netherlands
| | - Quint van Giersbergen
- Department of Ecology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ, Nijmegen, the Netherlands.
| | - Tom S Heuts
- Department of Ecology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ, Nijmegen, the Netherlands
| | - Reinder Nouta
- Department of Ecology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ, Nijmegen, the Netherlands; Wetterskip Fryslân, Fryslânplein 3, 8914 BZ, Leeuwarden, the Netherlands
| | - Coline C F Boonman
- Center for Biodiversity Dynamics in a Changing World (BIOCHANGE), Department of Biology, Aarhus University, Ny Munkegade 116, 8000 Aarhus, Denmark
| | - Mandy Velthuis
- Department of Ecology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ, Nijmegen, the Netherlands
| | - Bart Kruijt
- Water Systems and Global Change Group, Wageningen University, Droevendaalsesteeg 3, 6708 PB, Wageningen, the Netherlands
| | - Ralf C H Aben
- Department of Ecology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ, Nijmegen, the Netherlands
| | - Christian Fritz
- Department of Ecology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ, Nijmegen, the Netherlands; Integrated Research on Energy, Environment and Society (IREES), University of Groningen, Nijenborgh 6, 9747 AG Groningen, Netherlands
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4
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Beamish D, White JC. On the detailed mapping of peat (raised bogs) using airborne radiometric data. JOURNAL OF ENVIRONMENTAL RADIOACTIVITY 2024; 277:107462. [PMID: 38805777 DOI: 10.1016/j.jenvrad.2024.107462] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/21/2024] [Revised: 05/22/2024] [Accepted: 05/24/2024] [Indexed: 05/30/2024]
Abstract
This study concerns the applied use of the natural radioactivity in soils. The relevance of airborne radiometric (gamma ray) survey data to peat mapping is now well established and such data have been used in a stand-alone sense and as covariates in machine learning algorithms. Here we present a method to use these data to accurately map the boundaries of peat (raised bogs). This has the potential to assist with the estimation of carbon stocks using a property-based assessment of soil. The significance of such regionally-uniform survey data lies in the subsurface information carried by the measurement which contrasts with the surficial nature of many other covariates. Soils attenuate radiometric flux by virtue of their bulk density (and associated carbon content) and water saturation level. The high attenuation levels in low density, wet peat materials give rise to a distinctive soil response. Here an entirely physics-based assessment of flux attenuation is carried out both theoretically and empirically. Radiometric data from the ongoing Tellus airborne survey of Ireland are used. The study area is characterised by an extensive assemblage of discrete raised peat bogs in a framework of largely mineral soils. Peat is detected by a property contrast with adjacent soils and so we consider all soils within the study area. The relatively low lateral resolution of the airborne data is demonstrated by modelling and we examine the behaviour of a combined spatial derivative of the data. The procedure allows the identification of the edges of the 128 peat polygons considered and indicates other additional potential areas of subsurface peat. The data appear to resolve the differences that exist across three available soil/peat databases that are used for the validation of the results obtained.
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Affiliation(s)
- David Beamish
- British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK.
| | - James C White
- British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK.
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5
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Tolunay D, Kowalchuk GA, Erkens G, Hefting MM. Aerobic and anaerobic decomposition rates in drained peatlands: Impact of botanical composition. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 930:172639. [PMID: 38670365 DOI: 10.1016/j.scitotenv.2024.172639] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/01/2024] [Revised: 04/12/2024] [Accepted: 04/18/2024] [Indexed: 04/28/2024]
Abstract
Drained peatlands in temperate climates are under threat from climate change and human activities. The resulting decomposition of organic matter plays a major role in regulating the associated land subsidence rates, yet the determinants of aerobic and anaerobic peat decomposition rates are not fully understood. In this study, we sought to gain insight into the drivers of decomposition rates in botanically diverse peatlands (sedge, reed, wood, and moss dominant) under oxic and anoxic conditions. Peat samples were collected from the anoxic zone and incubated for 24 h (short) and 15 weeks (long) under either oxic or anoxic conditions. CO2 emissions, hydrolytic and oxidative exoenzyme potential activities, phenolic compound concentrations, and several edaphic factors were measured at the end of each incubation period. We found that 15 weeks of oxygen exposure of anoxic peat samples accelerated the average CO2 emissions by 3.9-fold. Reed and sedge peat respired more than wood and moss peat under anoxic conditions. Interestingly, CO2 emissions from anoxic peat layers under permanently anoxic conditions were substantial and given the thickness of peat deposits in the field, such activities may play an important role in long-term land subsidence rates and total CO2 emissions from drained peatlands. The results from the long-term incubations showed that decomposition rates appear to be also controlled by factors other than oxygen intrusion such as substrate availability. In summary, the botanical composition of the peat matrix, incubation conditions and time of incubation are all important factors that need to be considered when predicting peat decomposition and subsequent land subsidence rates.
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Affiliation(s)
- Duygu Tolunay
- Ecology and Biodiversity, Institute of Environmental Biology, Utrecht University, Padualaan 8, 3584 CH Utrecht, the Netherlands.
| | - George A Kowalchuk
- Ecology and Biodiversity, Institute of Environmental Biology, Utrecht University, Padualaan 8, 3584 CH Utrecht, the Netherlands
| | - Gilles Erkens
- Ecology and Biodiversity, Institute of Environmental Biology, Utrecht University, Padualaan 8, 3584 CH Utrecht, the Netherlands; Department of Physical Geography, Utrecht University, P.O. Box 80115, 3508 TC Utrecht, the Netherlands; Deltares Research Institute, P.O. Box 85467, 3508 AL Utrecht, the Netherlands
| | - Mariet M Hefting
- Ecology and Biodiversity, Institute of Environmental Biology, Utrecht University, Padualaan 8, 3584 CH Utrecht, the Netherlands; Amsterdam Institute for Life and Environment (A-LIFE) Systems ecology Section, Vrije Universiteit Amsterdam, the Netherlands
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6
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Campeau A, He H, Riml J, Humphreys E, Dalva M, Roulet N. Wind as a Driver of Peat CO 2 Dynamics in a Northern Bog. Ecosystems 2024; 27:621-635. [PMID: 39091378 PMCID: PMC11289004 DOI: 10.1007/s10021-024-00904-1] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/14/2023] [Accepted: 02/15/2024] [Indexed: 08/04/2024]
Abstract
Excess CO2 accumulated in soils is typically transported to the atmosphere through molecular diffusion along a concentration gradient. Because of the slow and constant nature of this process, a steady state between peat CO2 production and emissions is often established. However, in peatland ecosystems, high peat porosity could foster additional non-diffusive transport processes, whose dynamics may become important to peat CO2 storage, transport and emission. Based on a continuous record of in situ peat pore CO2 concentration within the unsaturated zone of a raised bog in southern Canada, we show that changes in wind speed create large diel fluctuations in peat pore CO2 store. Peat CO2 builds up overnight and is regularly flushed out the following morning. Persistently high wind speed during the day maintains the peat CO2 with concentrations close to that of the ambient air. At night, wind speed decreases and CO2 production overtakes the transport rate leading to the accumulation of CO2 in the peat. Our results indicate that the effective diffusion coefficient fluctuates based on wind speed and generally exceeds the estimated molecular diffusion coefficient. The balance between peat CO2 accumulation and transport is most dynamic within the range of 0-2 m s-1 wind speeds, which occurs over 75% of the growing season and dominates night-time measurements. Wind therefore drives considerable temporal dynamics in peat CO2 transport and storage, particularly over sub-daily timescales, such that peat CO2 emissions can only be directly related to biological production over longer timescales. Supplementary Information The online version contains supplementary material available at 10.1007/s10021-024-00904-1.
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Affiliation(s)
- A. Campeau
- Department of Forest Ecology and Management, Swedish University of Agricultural Sciences, Umeå, Sweden
- Department of Geography, McGill University, Montreal, Canada
- Present Address: Department of Geography, University of Montréal, Montreal, Quebec Canada
| | - H. He
- Department of Geography, McGill University, Montreal, Canada
| | - J. Riml
- Department of Sustainable Development, Environmental Science and Engineering, KTH Royal Institute of Technology, Stockholm, Sweden
| | - E. Humphreys
- Department of Geography and Environmental Studies, Carleton University, Ottawa, Canada
| | - M. Dalva
- Department of Geography, McGill University, Montreal, Canada
| | - N. Roulet
- Department of Geography, McGill University, Montreal, Canada
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7
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Awala SI, Gwak JH, Kim Y, Jung MY, Dunfield PF, Wagner M, Rhee SK. Nitrous oxide respiration in acidophilic methanotrophs. Nat Commun 2024; 15:4226. [PMID: 38762502 PMCID: PMC11102522 DOI: 10.1038/s41467-024-48161-z] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/03/2024] [Accepted: 04/22/2024] [Indexed: 05/20/2024] Open
Abstract
Aerobic methanotrophic bacteria are considered strict aerobes but are often highly abundant in hypoxic and even anoxic environments. Despite possessing denitrification genes, it remains to be verified whether denitrification contributes to their growth. Here, we show that acidophilic methanotrophs can respire nitrous oxide (N2O) and grow anaerobically on diverse non-methane substrates, including methanol, C-C substrates, and hydrogen. We study two strains that possess N2O reductase genes: Methylocella tundrae T4 and Methylacidiphilum caldifontis IT6. We show that N2O respiration supports growth of Methylacidiphilum caldifontis at an extremely acidic pH of 2.0, exceeding the known physiological pH limits for microbial N2O consumption. Methylocella tundrae simultaneously consumes N2O and CH4 in suboxic conditions, indicating robustness of its N2O reductase activity in the presence of O2. Furthermore, in O2-limiting conditions, the amount of CH4 oxidized per O2 reduced increases when N2O is added, indicating that Methylocella tundrae can direct more O2 towards methane monooxygenase. Thus, our results demonstrate that some methanotrophs can respire N2O independently or simultaneously with O2, which may facilitate their growth and survival in dynamic environments. Such metabolic capability enables these bacteria to simultaneously reduce the release of the key greenhouse gases CO2, CH4, and N2O.
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Affiliation(s)
- Samuel Imisi Awala
- Department of Biological Sciences and Biotechnology, Chungbuk National University, 1 Chungdae-ro, Seowon-Gu, Cheongju, 28644, Republic of Korea
- Center for Ecology and Environmental Toxicology, Chungbuk National University, 1 Chungdae-Ro, Seowon-Gu, Cheongju, 28644, South Korea
| | - Joo-Han Gwak
- Department of Biological Sciences and Biotechnology, Chungbuk National University, 1 Chungdae-ro, Seowon-Gu, Cheongju, 28644, Republic of Korea
| | - Yongman Kim
- Department of Biological Sciences and Biotechnology, Chungbuk National University, 1 Chungdae-ro, Seowon-Gu, Cheongju, 28644, Republic of Korea
| | - Man-Young Jung
- Interdisciplinary Graduate Programme in Advance Convergence Technology and Science, Jeju National University, Jeju, Republic of Korea
- Department of Science Education, Jeju National University, Jeju, Republic of Korea
- Jeju Microbiome Center, Jeju National University, Jeju, Republic of Korea
| | - Peter F Dunfield
- Department of Biological Sciences, University of Calgary, 2500 University Dr. NW, Calgary, AB, T2N 1N4, Canada
| | - Michael Wagner
- Division of Microbial Ecology, Department of Microbiology and Ecosystem Science, Centre for Microbiology and Environmental Systems Science, University of Vienna, Althanstrasse 14, A-1090, Vienna, Austria
- Department of Chemistry and Bioscience, Center for Microbial Communities, Aalborg University, Fredrik Bajers Vej 7H, 9220, Aalborg, Denmark
| | - Sung-Keun Rhee
- Department of Biological Sciences and Biotechnology, Chungbuk National University, 1 Chungdae-ro, Seowon-Gu, Cheongju, 28644, Republic of Korea.
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8
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Riquelme del Río B, Sepulveda-Jauregui A, Salas-Rabaza JA, Mackenzie R, Thalasso F. Fine-Scale Spatial Variability of Greenhouse Gas Emissions From a Subantarctic Peatland Bog. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2024; 58:7393-7402. [PMID: 38622815 PMCID: PMC11064220 DOI: 10.1021/acs.est.3c10746] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/20/2023] [Revised: 04/02/2024] [Accepted: 04/04/2024] [Indexed: 04/17/2024]
Abstract
Peatlands are recognized as crucial greenhouse gas sources and sinks and have been extensively studied. Their emissions exhibit high spatial heterogeneity when measured on site using flux chambers. However, the mechanism by which this spatial variability behaves on a very fine scale remains unclear. This study investigates the fine-scale spatial variability of greenhouse gas emissions from a subantarctic Sphagnum peatland bog. Using a recently developed skirt chamber, methane emissions and ecosystem respiration (as carbon dioxide) were measured at a submeter scale resolution, at five specific 3 × 3 m plots, which were examined across the site throughout a single campaign during the Austral summer season. The results indicated that methane fluxes were significantly less homogeneously distributed compared with ecosystem respiration. Furthermore, we established that the spatial variation scale, i.e., the minimum spatial domain over which notable changes in methane emissions and ecosystem respiration occur, was <0.56 m2. Factors such as ground height relative to the water table and vegetation coverage were analyzed. It was observed that Tetroncium magellanicum exhibited a notable correlation with higher methane fluxes, likely because of the aerenchymatous nature of this species, facilitating gas transport. This study advances understanding of gas exchange patterns in peatlands but also emphasizes the need for further efforts for characterizing spatial dynamics at a very fine scale for precise greenhouse gas budget assessment.
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Affiliation(s)
- Brenda Riquelme del Río
- Cape
Horn International Center, Universidad de
Magallanes, Teniente Muñoz 166, Puerto Williams 6350000,Chile
- Millennium
Institute Biodiversity of Antarctic and Subantarctic Ecosystems (BASE), Las Palmeras, 3425, Santiago 7800003, Chile
| | - Armando Sepulveda-Jauregui
- Environmental
Biogeochemistry Laboratory, Centro de Investigación Gaia Antártica
(CIGA), Universidad de Magallanes, Av. Bulnes 01855, Punta Arenas 6210427, Chile
- Ecosystem
Processes, Plankton and Microbial Ecology, IGB Leibniz-Institute of Freshwater Ecology and Inland Fisheries, Zur alten Fischerhütte 2, Stechlin 16775, Germany
| | - Julio A. Salas-Rabaza
- Cape
Horn International Center, Universidad de
Magallanes, Teniente Muñoz 166, Puerto Williams 6350000,Chile
| | - Roy Mackenzie
- Cape
Horn International Center, Universidad de
Magallanes, Teniente Muñoz 166, Puerto Williams 6350000,Chile
- Millennium
Institute Biodiversity of Antarctic and Subantarctic Ecosystems (BASE), Las Palmeras, 3425, Santiago 7800003, Chile
| | - Frederic Thalasso
- Cape
Horn International Center, Universidad de
Magallanes, Teniente Muñoz 166, Puerto Williams 6350000,Chile
- Departamento
de Biotecnología y Bioingeniería, Centro de Investigación y de Estudios Avanzados del Instituto
Politécnico Nacional (Cinvestav), Av. IPN 2508, Mexico City 07360, Mexico
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9
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He T, Ding W, Cheng X, Cai Y, Zhang Y, Xia H, Wang X, Zhang J, Zhang K, Zhang Q. Meta-analysis shows the impacts of ecological restoration on greenhouse gas emissions. Nat Commun 2024; 15:2668. [PMID: 38531906 DOI: 10.1038/s41467-024-46991-5] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/09/2023] [Accepted: 03/15/2024] [Indexed: 03/28/2024] Open
Abstract
International initiatives set ambitious targets for ecological restoration, which is considered a promising greenhouse gas mitigation strategy. Here, we conduct a meta-analysis to quantify the impacts of ecological restoration on greenhouse gas emissions using a dataset compiled from 253 articles. Our findings reveal that forest and grassland restoration increase CH4 uptake by 90.0% and 30.8%, respectively, mainly due to changes in soil properties. Conversely, wetland restoration increases CH4 emissions by 544.4%, primarily attributable to elevated water table depth. Forest and grassland restoration have no significant effect on N2O emissions, while wetland restoration reduces N2O emissions by 68.6%. Wetland restoration enhances net CO2 uptake, and the transition from net CO2 sources to net sinks takes approximately 4 years following restoration. The net ecosystem CO2 exchange of the restored forests decreases with restoration age, and the transition from net CO2 sources to net sinks takes about 3-5 years for afforestation and reforestation sites, and 6-13 years for clear-cutting and post-fire sites. Overall, forest, grassland and wetland restoration decrease the global warming potentials by 327.7%, 157.7% and 62.0% compared with their paired control ecosystems, respectively. Our findings suggest that afforestation, reforestation, rewetting drained wetlands, and restoring degraded grasslands through grazing exclusion, reducing grazing intensity, or converting croplands to grasslands can effectively mitigate greenhouse gas emissions.
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Affiliation(s)
- Tiehu He
- Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan, 430074, P.R. China
- Danjiangkou Wetland Ecosystem Field Scientific Observation and Research Station, the Chinese Academy of Sciences & Hubei Province, Wuhan, 430074, P.R. China
- Key Laboratory of Lake and Watershed Science for Water Security, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, China
- Hubei Key Laboratory of Wetland Evolution & Ecological Restoration, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan, 430074, China
| | - Weixin Ding
- State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, 210008, China
| | - Xiaoli Cheng
- School of Ecology and Environmental Science, Yunnan University, Kunming, 650091, P. R. China
| | - Yanjiang Cai
- State Key Laboratory of Subtropical Silviculture, Zhejiang A&F University, Hangzhou, 311300, China
| | - Yulong Zhang
- Eastern Forest Environmental Threat Assessment Center, Southern Research Station, USDA Forest Service, Research Triangle Park, NC, 27709, USA
| | - Huijuan Xia
- Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan, 430074, P.R. China
- Danjiangkou Wetland Ecosystem Field Scientific Observation and Research Station, the Chinese Academy of Sciences & Hubei Province, Wuhan, 430074, P.R. China
| | - Xia Wang
- Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan, 430074, P.R. China
- Danjiangkou Wetland Ecosystem Field Scientific Observation and Research Station, the Chinese Academy of Sciences & Hubei Province, Wuhan, 430074, P.R. China
| | - Jiehao Zhang
- Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan, 430074, P.R. China
- Danjiangkou Wetland Ecosystem Field Scientific Observation and Research Station, the Chinese Academy of Sciences & Hubei Province, Wuhan, 430074, P.R. China
| | - Kerong Zhang
- Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan, 430074, P.R. China.
- Danjiangkou Wetland Ecosystem Field Scientific Observation and Research Station, the Chinese Academy of Sciences & Hubei Province, Wuhan, 430074, P.R. China.
- Key Laboratory of Lake and Watershed Science for Water Security, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, China.
- Hubei Key Laboratory of Wetland Evolution & Ecological Restoration, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan, 430074, China.
| | - Quanfa Zhang
- Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan, 430074, P.R. China
- Danjiangkou Wetland Ecosystem Field Scientific Observation and Research Station, the Chinese Academy of Sciences & Hubei Province, Wuhan, 430074, P.R. China
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10
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Gios E, Verbruggen E, Audet J, Burns R, Butterbach-Bahl K, Espenberg M, Fritz C, Glatzel S, Jurasinski G, Larmola T, Mander Ü, Nielsen C, Rodriguez AF, Scheer C, Zak D, Silvennoinen HM. Unraveling microbial processes involved in carbon and nitrogen cycling and greenhouse gas emissions in rewetted peatlands by molecular biology. BIOGEOCHEMISTRY 2024; 167:609-629. [PMID: 38707517 PMCID: PMC11068585 DOI: 10.1007/s10533-024-01122-6] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 05/31/2023] [Accepted: 01/22/2024] [Indexed: 05/07/2024]
Abstract
Restoration of drained peatlands through rewetting has recently emerged as a prevailing strategy to mitigate excessive greenhouse gas emissions and re-establish the vital carbon sequestration capacity of peatlands. Rewetting can help to restore vegetation communities and biodiversity, while still allowing for extensive agricultural management such as paludiculture. Belowground processes governing carbon fluxes and greenhouse gas dynamics are mediated by a complex network of microbial communities and processes. Our understanding of this complexity and its multi-factorial controls in rewetted peatlands is limited. Here, we summarize the research regarding the role of soil microbial communities and functions in driving carbon and nutrient cycling in rewetted peatlands including the use of molecular biology techniques in understanding biogeochemical processes linked to greenhouse gas fluxes. We emphasize that rapidly advancing molecular biology approaches, such as high-throughput sequencing, are powerful tools helping to elucidate the dynamics of key biogeochemical processes when combined with isotope tracing and greenhouse gas measuring techniques. Insights gained from the gathered studies can help inform efficient monitoring practices for rewetted peatlands and the development of climate-smart restoration and management strategies. Supplementary Information The online version contains supplementary material available at 10.1007/s10533-024-01122-6.
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Affiliation(s)
- Emilie Gios
- NINA, Norwegian Institute for Nature Research, PO Box 5685, Torgarden, NO-7485 Trondheim, Norway
| | - Erik Verbruggen
- Plants and Ecosystems Research Group, Department of Biology, University of Antwerp, Universiteitsplein 1, Wilrijk, 2610 Antwerp, Belgium
| | - Joachim Audet
- Department of Ecoscience, Aarhus University, C.F. Møllers Allé, 8000 Aarhus, Denmark
| | - Rachel Burns
- Department of Geosciences and Natural Resource Management, University of Copenhagen, 1350 Copenhagen, Denmark
| | - Klaus Butterbach-Bahl
- Institute of Meteorology and Climate Research, Atmospheric Environmental Research, Karlsruhe Institute of Technology, 82467 Garmisch-Partenkirchen, Germany
- Department of Agroecology, Pioneer Center for Research in Sustainable Agricultural Futures (Land-CRAFT), Aarhus University, 8000 Aarhus, Denmark
| | - Mikk Espenberg
- Department of Geography, Institute of Ecology and Earth Sciences, University of Tartu, 46 St., Vanemuise, 51003 Tartu, Estonia
| | - Christian Fritz
- Aquatic Ecology and Environmental Biology, Radboud Institute for Biological and Environmental Sciences (RIBES), Radboud University, Heyendaalseweg 135, 6525 AJ Nijmegen, The Netherlands
| | - Stephan Glatzel
- Department of Geography and Regional Research, University of Vienna, Althanstraße 14, 1090 Vienna, Austria
| | - Gerald Jurasinski
- Faculty of Agriculture and Environment, Landscape Ecology and Site Evaluation, University of Rostock, Justus-von-Liebig-Weg 6, 18059 Rostock, Germany
- Department of Maritime Systems, Faculty of Interdisciplinary Research, University of Rostock, Albert- Einstein-Straße 3, 18059 Rostock, Germany
| | - Tuula Larmola
- Natural Resources Institute Finland (Luke), 00790 Helsinki, Finland
| | - Ülo Mander
- Department of Geography, Institute of Ecology and Earth Sciences, University of Tartu, 46 St., Vanemuise, 51003 Tartu, Estonia
| | - Claudia Nielsen
- Department of Agroecology, Faculty of Technical Sciences, Aarhus University, Blichers Alle 20, 8830 Tjele, Denmark
- CBIO, Centre for Circular Bioeconomy, Aarhus University, 8830 Tjele, Denmark
| | - Andres F. Rodriguez
- Department of Agroecology, Faculty of Technical Sciences, Aarhus University, Blichers Alle 20, 8830 Tjele, Denmark
| | - Clemens Scheer
- Institute of Meteorology and Climate Research, Atmospheric Environmental Research, Karlsruhe Institute of Technology, 82467 Garmisch-Partenkirchen, Germany
| | - Dominik Zak
- Department of Ecoscience, Aarhus University, C.F. Møllers Allé, 8000 Aarhus, Denmark
- Department of Ecohydrology and Biogeochemistry, Leibniz-Institute of Freshwater Ecology and Inland Fisheries, Müggelseedamm 301, 12587 Berlin, Germany
| | - Hanna M. Silvennoinen
- NINA, Norwegian Institute for Nature Research, PO Box 5685, Torgarden, NO-7485 Trondheim, Norway
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11
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Cui R, Chen A, Hu W, Fu B, Liu G, Zhang D. Appropriate stoichiometric ratios of dissolved organic carbon and nitrate can trigger a transition in nitrate removal in groundwater around plateau lakes, Southwest China. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 916:170313. [PMID: 38278230 DOI: 10.1016/j.scitotenv.2024.170313] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/01/2023] [Revised: 12/25/2023] [Accepted: 01/18/2024] [Indexed: 01/28/2024]
Abstract
Increasing dissolved organic carbon (DOC) in groundwater as a carbon source for microorganisms that stimulate nitrate attenuation is considered a sustainable strategy to mitigate nitrate pollution in groundwater. However, little is known on the stoichiometric ratio of DOC and nitrate required in groundwater nitrate reduction processes, which has become an obstacle for evaluating the current status of DOC limitations on nitrate reduction. Here, the NO3--N and DOC concentrations in groundwater around 8 plateau lakes were investigated, and a microcosm experiment was performed to elucidate the effects of different DOC:NO3--N levels in groundwater on NO3--N reduction, and the current status of DOC limitations on groundwater NO3--N reduction around 8 lakes was further evaluated. The results indicated that nearly 41 % of the groundwater NO3--N concentrations exceeded the WHO threshold for drinking water (11.3 mg L-1) and 79 % of the groundwater DOC concentrations exceeded 5 mg L-1. The differences in groundwater NO3--N and DOC concentrations among the 8 lakes were controlled by the intensity of agricultural and human activities and hydrogeological background. The stoichiometric ratio of DOC:NO3--N regulated the NO3--N reduction process, and groundwater NO3--N accumulation rate appeared to become limited and sharply decreased when the DOC concentration was approximately 10 mg L-1 or when the DOC:NO3--N ratio was close to 1:1, and the DOC:NO3--N ratio threshold for limiting the NO3--N reduction process was approximately 2.25. Based on this threshold, >33 %-86 % of the groundwater samples around the 8 plateau lakes were strongly limited in the reduction of groundwater NO3--N due to a lack of sufficient DOC provides energy for heterotrophic microorganisms. Additionally, we highlight that the sustainable strategy of increasing DOC to stimulate groundwater NO3- attenuation should be combined with short-term strategies to jointly coordinate and control groundwater NO3- pollution.
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Affiliation(s)
- Rongyang Cui
- Agricultural Environment and Resources Institute, Yunnan Academy of Agricultural Sciences, Kunming 650201, China; Key Laboratory of Mountain Surface Processes and Ecological Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610299, China; University of Chinese Academy of Sciences, Beijing 100049, China
| | - Anqiang Chen
- Agricultural Environment and Resources Institute, Yunnan Academy of Agricultural Sciences, Kunming 650201, China.
| | - Wanli Hu
- Agricultural Environment and Resources Institute, Yunnan Academy of Agricultural Sciences, Kunming 650201, China
| | - Bin Fu
- Agricultural Environment and Resources Institute, Yunnan Academy of Agricultural Sciences, Kunming 650201, China
| | - Gangcai Liu
- Key Laboratory of Mountain Surface Processes and Ecological Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610299, China
| | - Dan Zhang
- College of Resources and Environment, Yunnan Agricultural University, Kunming 650201, China.
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12
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Peacock M, Lawson C, Gowing D, Gauci V. Water table depth and plant species determine the direction and magnitude of methane fluxes in floodplain meadow soils. Ecol Evol 2024; 14:e11147. [PMID: 38469053 PMCID: PMC10925825 DOI: 10.1002/ece3.11147] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/08/2023] [Revised: 01/22/2024] [Accepted: 02/29/2024] [Indexed: 03/13/2024] Open
Abstract
Methane (CH4) is a powerful greenhouse gas with ongoing efforts aiming to quantify and map emissions from natural and managed ecosystems. Wetlands play a significant role in the global CH4 budget, but uncertainties in their total emissions remain large, due to a combined lack of CH4 data and fuzzy boundaries between mapped ecosystem categories. European floodplain meadows are anthropogenic ecosystems that originated due to traditional management for hay cropping. These ecosystems are seasonally inundated by river water, and straddle the boundary between grassland and wetland ecosystems; however, an understanding of their CH4 function is lacking. Here, we established a replicated outdoor floodplain-meadow mesocosm experiment to test how water table depth (45, 30, 15 cm below the soil surface) and plant composition affect CH4 fluxes over an annual cycle. Water table was a major controller on CH4, with significantly higher fluxes (overall mean 9.3 mg m-2 d-1) from the high (15 cm) water table treatment. Fluxes from high water table mesocosms with bare soil were low (mean 0.4 mg m-2 d-1), demonstrating that vegetation drove high emissions. Larger emissions came from high water table mesocosms with aerenchymatous plant species (e.g. Alopecurus pratensis, mean 12.8 mg m-2 d-1), suggesting a role for plant-mediated transport. However, at low (45 cm) water tables A. pratensis mesocosms were net CH4 sinks, suggesting that there is plasticity in CH4 exchange if aerenchyma are present. Plant cutting to simulate a hay harvest had no effect on CH4, further supporting a role for plant-mediated transport. Upscaling our CH4 fluxes to a UK floodplain meadow using hydrological modelling showed that the meadow was a net CH4 source because oxic periods of uptake were outweighed by flooding-induced anoxic emissions. Our results show that floodplain meadows can be either small sources or sinks of CH4 over an annual cycle. Their CH4 exchange appears to respond to soil temperature, moisture status and community composition, all of which are likely to be modified by climate change, leading to uncertainty around the future net contribution of floodplain meadows to the CH4 cycle.
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Affiliation(s)
- Mike Peacock
- Department of Geography and Planning, School of Environmental SciencesUniversity of LiverpoolLiverpoolUK
- Department of Aquatic Sciences and AssessmentSwedish University of Agricultural SciencesUppsalaSweden
| | - Clare Lawson
- School of Environment, Earth and Ecosystem SciencesOpen UniversityMilton KeynesUK
| | - David Gowing
- School of Environment, Earth and Ecosystem SciencesOpen UniversityMilton KeynesUK
| | - Vincent Gauci
- Birmingham Institute of Forest ResearchUniversity of BirminghamBirminghamUK
- School of Geography Earth and Environmental ScienceUniversity of BirminghamBirminghamUK
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13
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Zhang J, Chen H, Wang M, Liu X, Peng C, Wang L, Yu D, Zhu Q. An optimized water table depth detected for mitigating global warming potential of greenhouse gas emissions in wetland of Qinghai-Tibetan Plateau. iScience 2024; 27:108856. [PMID: 38303693 PMCID: PMC10830858 DOI: 10.1016/j.isci.2024.108856] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/18/2023] [Revised: 11/18/2023] [Accepted: 01/06/2024] [Indexed: 02/03/2024] Open
Abstract
Climate change and human activities have intensified variations of water table depth (WTD) in wetlands around the world, which may strongly affect greenhouse gas emissions. Here, we analyzed how emissions of CO2, CH4, and N2O from the Zoige wetland on the Qinghai-Tibetan Plateau (QTP) vary with the WTD. Our data indicate that the wetland shows net positive global warming potential (11.72 tCO2-e ha-1 yr-1), and its emissions of greenhouse gases are driven primarily by WTD. Our analysis suggests that an optimal WTD exists, which at our study site was approximately 18 cm, for mitigating increases in global warming potential from the wetland. Our study provides insights into how climate change and human acitivies affect greenhouse gas emissions from alpine wetlands, and they suggest that water table management may be effective at mitigating future increases in emissions.
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Affiliation(s)
- Jiang Zhang
- College of Geography and Remote Sensing, Hohai University, Nanjing 210098, China
- Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
| | - Huai Chen
- Chengdu Institute of Biology, Chinese Academy of Sciences, Chengdu 610041, China
| | - Meng Wang
- Key Laboratory of Geographical Processes and Ecological Security in Changbai Mountains, Ministry of Education, School of Geographical Sciences, Northeast Normal University, Changchun 130024, China
| | - Xinwei Liu
- Chengdu Institute of Biology, Chinese Academy of Sciences, Chengdu 610041, China
| | - Changhui Peng
- Institute of Environment Sciences, Department of Biology Sciences, University of Quebec at Montreal, Case Postale 8888, Succursale Centre-Ville, Montreal Quebec H3C 3P8, Canada
- School of Geography Science, Hunan Normal University, Changsha 410081, China
| | - Le Wang
- College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China
| | - Dongxue Yu
- College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China
| | - Qiuan Zhu
- College of Geography and Remote Sensing, Hohai University, Nanjing 210098, China
- National Earth System Science Data Center, National Science & Technology Infrastructure of China, Beijing 100101, China
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14
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Jensen AB, Eller F, Sorrell BK. Comparative flooding tolerance of Typha latifolia and Phalaris arundinacea in wetland restoration: Insights from photosynthetic CO 2 response curves, photobiology and biomass allocation. Heliyon 2024; 10:e23657. [PMID: 38187246 PMCID: PMC10767378 DOI: 10.1016/j.heliyon.2023.e23657] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/31/2023] [Revised: 12/01/2023] [Accepted: 12/08/2023] [Indexed: 01/09/2024] Open
Abstract
Tall helophytes such as Typha latifolia and Phalaris arundinacea often rapidly colonise after rewetting of former agricultural soil and are therefore often the first plants to contribute to the soil carbon pool. In this study we carried out a mesocosm experiment where these two species grew at three different water levels relative to the soil surface (-15 cm, 0 cm, +15 cm). After eight weeks' growth, measurements of photosynthetic CO2-response curves, stomatal conductance and chlorophyll fluorescence of photosystem II were carried out to detect flooding stress. After 10 weeks' growth, the plants were harvested and biomass production, biomass allocation and specific leaf area were determined. T. latifolia had a higher and more stable photosynthetic performance across all water level treatments, which resulted in an overall higher aboveground and belowground production than P. arundinacea. In contrast, Vcmax and Jmax decreased by 41 % and 42 %, respectively from drained to flooded conditions with signs of flooding stress as impairment of the photosynthetic apparatus. Moreover, increasing water level resulted in maintenance of aboveground organs for P. arundinacea but a decrease in allocation to belowground organs. P. arundinacea did not invest in a higher specific leaf area to counter the decreased photosynthesis under flooding. From -15 cm to 0 cm water levels, P. arundinacea showed a 68 % reduction in belowground biomass, which has negative implication for carbon retention immediately after rewetting. In contrast, recolonization of T. latifolia is likely to be a suitable contributor to the soil carbon pool due to its stable physiology and high above- and belowground biomass production at all water depths, and also likely under natural water level fluctuations. We showed that even though both species are generally considered wetland plants, they are likely to support considerably different photosynthetic carbon assimilation and soil carbon sequestration rates.
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Affiliation(s)
- Asger Buur Jensen
- Department of Biology, Aarhus University, Ole Worms Alle 1, DK-8000, Aarhus C, Denmark
| | - Franziska Eller
- Department of Biology, Aarhus University, Ole Worms Alle 1, DK-8000, Aarhus C, Denmark
| | - Brian K. Sorrell
- Department of Biology, Aarhus University, Ole Worms Alle 1, DK-8000, Aarhus C, Denmark
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15
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Mackin F, Flynn R, Fernandez-Valverde F. Application of a GIS-Based Hydrological Model to Predict Surface Wetness of Blanket Bogs. WETLANDS (WILMINGTON, N.C.) 2024; 44:10. [PMID: 38188226 PMCID: PMC10764537 DOI: 10.1007/s13157-023-01765-5] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 11/23/2022] [Accepted: 12/16/2023] [Indexed: 01/09/2024]
Abstract
Understanding hydrological processes operating on relatively intact blanket bogs provides a scientific basis for establishing achievable restoration targets for damaged sites. A GIS-based hydrological model, developed to assess restoration potential of Irish raised bogs, was adapted and applied to four relatively intact blanket bogs in Ireland. The Modified Flow Accumulation Capacity (MFAC) model utilised high-resolution topographic data to predict surface wetness, based on climatic conditions, contributing catchment and local surface slope. Modifications to MFAC parameters aimed to account for differences in hydrological processes between raised bogs and blanket bogs. Application of a climatic correction factor accounted for variations in effective rainfall between the four study sites, while monitoring of water table levels indicated a log-linear relationship between MFAC values and summer water table levels and range of water table fluctuations. Deviations from the observed relationship between MFAC and water table levels were associated with hydrological pressures, such as artificial drainage or the occurrence of subsurface macropores (peat pipes), which further lowered summer water tables. Despite being effective as a predictor of relative surface wetness, the relationship between MFAC and ecological variables such as Sphagnum spp. cover proved poor, pointing to the impact of past activities and damage caused by anthropogenic pressures. Findings demonstrated MFAC as an effective tool in predicting surface wetness within blanket bog-covered landscapes, thus proving useful to peatland practitioners in planning and prioritising areas for restoration. Supplementary Information The online version contains supplementary material available at 10.1007/s13157-023-01765-5.
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Affiliation(s)
- Francis Mackin
- School of Natural and Built Environment, The Queen’s University of Belfast, David Keir Building, Stranmillis Road, Belfast, BT9 5AG UK
| | - Raymond Flynn
- School of Natural and Built Environment, The Queen’s University of Belfast, David Keir Building, Stranmillis Road, Belfast, BT9 5AG UK
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16
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Wei H, Zhang K, Chai N, Wang Y, Li Y, Yang J, Harrison MT, Liu K, Wan P, Zhang W, Sun G, Li Z, Zhang F. Exploring low-carbon mulching strategies for maize and wheat on-farm: Spatial responses, factors and mitigation potential. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 906:167441. [PMID: 37774862 DOI: 10.1016/j.scitotenv.2023.167441] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/17/2023] [Revised: 09/26/2023] [Accepted: 09/26/2023] [Indexed: 10/01/2023]
Abstract
Mulching strategies - including plastic film mulching (FM) and straw mulching (SM) - can enhance crop yields while affecting multiple greenhouse gas (GHG) fluxes. However, most of currently published site-based studies only focus on a certain gas, resulting in an inability to spatially integrated understanding of changes in agricultural global warming potential (GWP) and greenhouse gas intensity (GHGI) caused by mulching across China. Thus, we developed an optimal model considering crop type, meteorology, soil and management variables by four machine learning methods, namely support vector machine, multilayer perceptron, random forest, and gradient boosting machine (GBM). Then we mapped the relative changes in yield and GHG fluxes caused by mulching strategies. The GBM model had the best simulation capability for yield and GHGs in China. Our result showed that FM increased yield in maize (25 %) and wheat (19 %), while SM respectively increased by 14 % and 11 %. Among the relative changes due to mulching strategies, yield and N2O emissions were mainly influenced by soil fertility and soil properties, CH4 uptakes and CO2 emissions were more affected by environmental factors. GWP in maize and wheat average increased by 40 % under FM, while SM decreased GWP by 14 % and 2 %, respectively. Besides, FM average increased GHGI in maize and wheat by 17 % and 9 %, and SM decreased GHGI by 22 % and 12 %, respectively. Spatially, FM reduced maize GWP on 19 % of cropland, while SM reduced maize and wheat GWP on 71 % and 64 % of cropland, respectively. Soil pH was significantly correlated with ΔGHGI in maize and wheat. Our analysis not only estimated for the first time the spatial effects of mulching strategies across China, but also systematically analyzes the agricultural carbon emission mitigation potential of mulching strategies, which promote the development of low-carbon agriculture based on locally appropriate mulching strategies.
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Affiliation(s)
- Huihui Wei
- State Key Laboratory of Herbage Improvement and Grassland Agro-ecosystems, School of Ecology, Lanzhou University, Lanzhou, Gansu 730000, China
| | - Kaiping Zhang
- State Key Laboratory of Herbage Improvement and Grassland Agro-ecosystems, School of Ecology, Lanzhou University, Lanzhou, Gansu 730000, China
| | - Ning Chai
- State Key Laboratory of Herbage Improvement and Grassland Agro-ecosystems, School of Ecology, Lanzhou University, Lanzhou, Gansu 730000, China
| | - Yue Wang
- State Key Laboratory of Herbage Improvement and Grassland Agro-ecosystems, School of Ecology, Lanzhou University, Lanzhou, Gansu 730000, China
| | - Yuling Li
- State Key Laboratory of Herbage Improvement and Grassland Agro-ecosystems, School of Ecology, Lanzhou University, Lanzhou, Gansu 730000, China
| | - Jianjun Yang
- State Key Laboratory of Herbage Improvement and Grassland Agro-ecosystems, School of Ecology, Lanzhou University, Lanzhou, Gansu 730000, China
| | - Matthew Tom Harrison
- Tasmanian Institute of Agriculture, University of Tasmania, Newnham Drive, Launceston, Tasmania 7428, Australia
| | - Ke Liu
- Tasmanian Institute of Agriculture, University of Tasmania, Newnham Drive, Launceston, Tasmania 7428, Australia
| | - Pingxing Wan
- State Key Laboratory of Herbage Improvement and Grassland Agro-ecosystems, School of Ecology, Lanzhou University, Lanzhou, Gansu 730000, China
| | - Wenjuan Zhang
- Institute of Qinghai Provincial Natural Resources Survey and Monitoring, Xining, Qinghai 810000, China
| | - Guojun Sun
- State Key Laboratory of Herbage Improvement and Grassland Agro-ecosystems, School of Ecology, Lanzhou University, Lanzhou, Gansu 730000, China
| | - Zhansheng Li
- Asia Hub, Sanya Institute of Nanjing Agricultural University, Nanjing Agricultural University, Sanya, Hainan 572000, China
| | - Feng Zhang
- State Key Laboratory of Herbage Improvement and Grassland Agro-ecosystems, School of Ecology, Lanzhou University, Lanzhou, Gansu 730000, China.
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17
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Candry P, Godfrey BJ, Winkler MKH. Microbe-cellulose hydrogels as a model system for particulate carbon degradation in soil aggregates. ISME COMMUNICATIONS 2024; 4:ycae068. [PMID: 38800124 PMCID: PMC11126157 DOI: 10.1093/ismeco/ycae068] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 01/11/2024] [Revised: 04/12/2024] [Accepted: 05/03/2024] [Indexed: 05/29/2024]
Abstract
Particulate carbon (C) degradation in soils is a critical process in the global C cycle governing greenhouse gas fluxes and C storage. Millimeter-scale soil aggregates impose strong controls on particulate C degradation by inducing chemical gradients of e.g. oxygen, as well as limiting microbial mobility in pore structures. To date, experimental models of soil aggregates have incorporated porosity and chemical gradients but not particulate C. Here, we demonstrate a proof-of-concept encapsulating microbial cells and particulate C substrates in hydrogel matrices as a novel experimental model for soil aggregates. Ruminiclostridium cellulolyticum was co-encapsulated with cellulose in millimeter-scale polyethyleneglycol-dimethacrylate (PEGDMA) hydrogel beads. Microbial activity was delayed in hydrogel-encapsulated conditions, with cellulose degradation and fermentation activity being observed after 13 days of incubation. Unexpectedly, hydrogel encapsulation shifted product formation of R. cellulolyticum from an ethanol-lactate-acetate mixture to an acetate-dominated product profile. Fluorescence microscopy enabled simultaneous visualization of the PEGDMA matrix, cellulose particles, and individual cells in the matrix, demonstrating growth on cellulose particles during incubation. Together, these microbe-cellulose-PEGDMA hydrogels present a novel, reproducible experimental soil surrogate to connect single cells to process outcomes at the scale of soil aggregates and ecosystems.
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Affiliation(s)
- Pieter Candry
- Civil and Environmental Engineering, University of Washington, 201 More Hall, Seattle, WA 98195-2700, United States
- Laboratory of Systems and Synthetic Biology, Wageningen University & Research, 6708 WE, Wageningen, The Netherlands
- Laboratory of Systems and Synthetic Biology, Wageningen University & Research, 6708 WE, Wageningen, The Netherlands. E-mail:
| | - Bruce J Godfrey
- Civil and Environmental Engineering, University of Washington, 201 More Hall, Seattle, WA 98195-2700, United States
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18
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Cobb AR, Dommain R, Yeap K, Hannan C, Dadap NC, Bookhagen B, Glaser PH, Harvey CF. A unified explanation for the morphology of raised peatlands. Nature 2024; 625:79-84. [PMID: 38093013 DOI: 10.1038/s41586-023-06807-w] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/09/2022] [Accepted: 10/31/2023] [Indexed: 01/05/2024]
Abstract
Raised peatlands, or bogs, are gently mounded landforms that are composed entirely of organic matter1-4 and store the most carbon per area of any terrestrial ecosystem5. The shapes of bogs are critically important because their domed morphology4,6,7 accounts for much of the carbon that bogs store and determines how they will respond to interventions8,9 to stop greenhouse gas emissions and fires after anthropogenic drainage10-13. However, a general theory to infer the morphology of bogs is still lacking4,6,7. Here we show that an equation based on the processes universal to bogs explains their morphology across biomes, from Alaska, through the tropics, to New Zealand. In contrast to earlier models of bog morphology that attempted to describe only long-term equilibrium shapes4,6,7 and were, therefore, inapplicable to most bogs14-16, our approach makes no such assumption and makes it possible to infer full shapes of bogs from a sample of elevations, such as a single elevation transect. Our findings provide a foundation for quantitative inference about the morphology, hydrology and carbon storage of bogs through Earth's history, as well as a basis for planning natural climate solutions by rewetting damaged bogs around the world.
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Affiliation(s)
- Alexander R Cobb
- Singapore-MIT Alliance for Research and Technology (SMART), Singapore, Singapore.
| | - René Dommain
- Earth Observatory of Singapore, Nanyang Technological University, Singapore, Singapore
- Asian School of the Environment, Nanyang Technological University, Singapore, Singapore
- National Museum of Natural History, Smithsonian Institution, Washington, DC, USA
| | - Kimberly Yeap
- School of Civil and Environmental Engineering, Nanyang Technological University, Singapore, Singapore
| | - Cao Hannan
- School of Computer Science and Engineering, Nanyang Technological University, Singapore, Singapore
| | - Nathan C Dadap
- Department of Earth System Science, Stanford University, Stanford, CA, USA
| | - Bodo Bookhagen
- Institute of Geosciences, University of Potsdam, Potsdam, Germany
| | - Paul H Glaser
- Department of Earth & Environmental Sciences, University of Minnesota, Minneapolis, MN, USA
| | - Charles F Harvey
- Singapore-MIT Alliance for Research and Technology (SMART), Singapore, Singapore
- Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, MA, USA
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19
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Jebari A, Pereyra-Goday F, Kumar A, Collins AL, Rivero MJ, McAuliffe GA. Feasibility of mitigation measures for agricultural greenhouse gas emissions in the UK. A systematic review. AGRONOMY FOR SUSTAINABLE DEVELOPMENT 2023; 44:2. [PMID: 38161803 PMCID: PMC10754757 DOI: 10.1007/s13593-023-00938-0] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Accepted: 11/24/2023] [Indexed: 01/03/2024]
Abstract
The UK Government has set an ambitious target of achieving a national "net-zero" greenhouse gas economy by 2050. Agriculture is arguably placed at the heart of achieving net zero, as it plays a unique role as both a producer of GHG emissions and a sector that has the capacity via land use to capture carbon (C) when managed appropriately, thus reducing the concentration of carbon dioxide (CO2) in the atmosphere. Agriculture's importance, particularly in a UK-specific perspective, which is also applicable to many other temperate climate nations globally, is that the majority of land use nationwide is allocated to farming. Here, we present a systematic review based on peer-reviewed literature and relevant "grey" reports to address the question "how can the agricultural sector in the UK reduce, or offset, its direct agricultural emissions at the farm level?" We considered the implications of mitigation measures in terms of food security and import reliance, energy, environmental degradation, and value for money. We identified 52 relevant studies covering major foods produced and consumed in the UK. Our findings indicate that many mitigation measures can indeed contribute to net zero through GHG emissions reduction, offsetting, and bioenergy production, pending their uptake by farmers. While the environmental impacts of mitigation measures were covered well within the reviewed literature, corresponding implications regarding energy, food security, and farmer attitudes towards adoption received scant attention. We also provide an open-access, informative, and comprehensive dataset for agri-environment stakeholders and policymakers to identify the most promising mitigation measures. This research is of critical value to researchers, land managers, and policymakers as an interim guideline resource while more quantitative evidence becomes available through the ongoing lab-, field-, and farm-scale trials which will improve the reliability of agricultural sustainability modelling in the future. Supplementary Information The online version contains supplementary material available at 10.1007/s13593-023-00938-0.
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Affiliation(s)
- Asma Jebari
- Net Zero and Resilient Farming, Rothamsted Research, North Wyke, Okehampton, EX20 2SB Devon UK
| | - Fabiana Pereyra-Goday
- Instituto Nacional de Investigacion Agropecuaria (INIA), Ruta 8 km 281, Treinta y Tres, postcode 33000 Montevideo, Uruguay
| | - Atul Kumar
- Net Zero and Resilient Farming, Rothamsted Research, North Wyke, Okehampton, EX20 2SB Devon UK
| | - Adrian L. Collins
- Net Zero and Resilient Farming, Rothamsted Research, North Wyke, Okehampton, EX20 2SB Devon UK
| | - M. Jordana Rivero
- Net Zero and Resilient Farming, Rothamsted Research, North Wyke, Okehampton, EX20 2SB Devon UK
| | - Graham A. McAuliffe
- Net Zero and Resilient Farming, Rothamsted Research, North Wyke, Okehampton, EX20 2SB Devon UK
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20
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Mander Ü, Espenberg M, Melling L, Kull A. Peatland restoration pathways to mitigate greenhouse gas emissions and retain peat carbon. BIOGEOCHEMISTRY 2023; 167:523-543. [PMID: 38707516 PMCID: PMC11068583 DOI: 10.1007/s10533-023-01103-1] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 06/21/2023] [Accepted: 11/04/2023] [Indexed: 05/07/2024]
Abstract
Peatlands play a crucial role in the global carbon (C) cycle, making their restoration a key strategy for mitigating greenhouse gas (GHG) emissions and retaining C. This study analyses the most common restoration pathways employed in boreal and temperate peatlands, potentially applicable in tropical peat swamp forests. Our analysis focuses on the GHG emissions and C retention potential of the restoration measures. To assess the C stock change in restored (rewetted) peatlands and afforested peatlands with continuous drainage, we adopt a conceptual approach that considers short-term C capture (GHG exchange between the atmosphere and the peatland ecosystem) and long-term C sequestration in peat. The primary criterion of our conceptual model is the capacity of restoration measures to capture C and reduce GHG emissions. Our findings indicate that carbon dioxide (CO2) is the most influential part of long-term climate impact of restored peatlands, whereas moderate methane (CH4) emissions and low N2O fluxes are relatively unimportant. However, lateral losses of dissolved and particulate C in water can account up to a half of the total C stock change. Among the restored peatland types, Sphagnum paludiculture showed the highest CO2 capture, followed by shallow lakes and reed/grass paludiculture. Shallow lakeshore vegetation in restored peatlands can reduce CO2 emissions and sequester C but still emit CH4, particularly during the first 20 years after restoration. Our conceptual modelling approach reveals that over a 300-year period, under stable climate conditions, drained bog forests can lose up to 50% of initial C content. In managed (regularly harvested) and continuously drained peatland forests, C accumulation in biomass and litter input does not compensate C losses from peat. In contrast, rewetted unmanaged peatland forests are turning into a persistent C sink. The modelling results emphasized the importance of long-term C balance analysis which considers soil C accumulation, moving beyond the short-term C cycling between vegetation and the atmosphere. Supplementary Information The online version contains supplementary material available at 10.1007/s10533-023-01103-1.
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Affiliation(s)
- Ülo Mander
- Institute of Ecology and Earth Sciences, University of Tartu, Tartu, Estonia
| | - Mikk Espenberg
- Institute of Ecology and Earth Sciences, University of Tartu, Tartu, Estonia
| | - Lulie Melling
- Sarawak Tropical Peat Research Institute, Kuching, Sarawak Malaysia
| | - Ain Kull
- Institute of Ecology and Earth Sciences, University of Tartu, Tartu, Estonia
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21
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Mason VG, Burden A, Epstein G, Jupe LL, Wood KA, Skov MW. Blue carbon benefits from global saltmarsh restoration. GLOBAL CHANGE BIOLOGY 2023; 29:6517-6545. [PMID: 37746862 DOI: 10.1111/gcb.16943] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/02/2023] [Revised: 08/30/2023] [Accepted: 08/31/2023] [Indexed: 09/26/2023]
Abstract
Coastal saltmarshes are found globally, yet are 25%-50% reduced compared with their historical cover. Restoration is incentivised by the promise that marshes are efficient storers of 'blue' carbon, although the claim lacks substantiation across global contexts. We synthesised data from 431 studies to quantify the benefits of saltmarsh restoration to carbon accumulation and greenhouse gas uptake. The results showed global marshes store approximately 1.41-2.44 Pg carbon. Restored marshes had very low greenhouse gas (GHG) fluxes and rapid carbon accumulation, resulting in a mean net accumulation rate of 64.70 t CO2 e ha-1 year-1 . Using this estimate and potential restoration rates, we find saltmarsh regeneration could result in 12.93-207.03 Mt CO2 e accumulation per year, offsetting the equivalent of up to 0.51% global energy-related CO2 emissions-a substantial amount, considering marshes represent <1% of Earth's surface. Carbon accumulation rates and GHG fluxes varied contextually with temperature, rainfall and dominant vegetation, with the eastern coasts of the USA and Australia particular hotspots for carbon storage. While the study reveals paucity of data for some variables and continents, suggesting need for further research, the potential for saltmarsh restoration to offset carbon emissions is clear. The ability to facilitate natural carbon accumulation by saltmarshes now rests principally on the action of the management-policy community and on financial opportunities for supporting restoration.
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Affiliation(s)
- Victoria G Mason
- School of Ocean Sciences, Bangor University, Anglesey, UK
- Department of Estuarine and Delta Systems, Royal Netherlands Institute for Sea Research (NIOZ) and Utrecht University, Yerseke, The Netherlands
- Department of Physical Geography, Faculty of Geosciences, Utrecht University, Utrecht, The Netherlands
| | - Annette Burden
- UK Centre for Ecology & Hydrology, Environment Centre Wales, Bangor, UK
| | - Graham Epstein
- Centre for Ecology and Conservation, University of Exeter, Cornwall, UK
- Department of Biology, University of Victoria, Victoria, British Columbia, Canada
| | - Lucy L Jupe
- Wildfowl & Wetlands Trust, Slimbridge Wetland Centre, Slimbridge, UK
| | - Kevin A Wood
- Wildfowl & Wetlands Trust, Slimbridge Wetland Centre, Slimbridge, UK
| | - Martin W Skov
- School of Ocean Sciences, Bangor University, Anglesey, UK
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22
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Zhang W, Tao X, Hu Z, Kang E, Yan Z, Zhang X, Wang J. The driving effects of nitrogen deposition on nitrous oxide and associated gene abundances at two water table levels in an alpine peatland. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 898:165525. [PMID: 37451456 DOI: 10.1016/j.scitotenv.2023.165525] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/21/2022] [Revised: 07/04/2023] [Accepted: 07/11/2023] [Indexed: 07/18/2023]
Abstract
Alpine peatlands are recognized as a weak or negligible source of nitrous oxide (N2O). Anthropogenic activities and climate change resulted in the altered water table (WT) levels and increased nitrogen (N) deposition, which could potentially transition this habitat into a N2O emission hotspot. However, the underlying mechanism related with the effects is still uncertain. Hence, we conducted a mesocosm experiment to address the response of growing-season N2O emissions and the gene abundances of nitrification (bacterial amoA) and denitrification (narG, nirS, norB and nosZ) to the increased N deposition (20 kg N ha-1 yr-1) at two WT levels (WT-30, 30 cm below soil surface; WT10, 10 cm above soil surface) in the Zoige alpine peatland, Qinghai-Tibetan Plateau. The results showed that the WT did not affect N2O emissions, and this was attributed with the limitation of soil NO3-. The higher WT level increased denitrification (narG and nirS gene abundance) resulting in the depletion of soil NO3-, but the consequent NO3- deficiency further limited denitrification, while the WT did not affect nitrification (bacterial amoA gene abundance). Meanwhile, the N deposition increased N2O emissions, regardless of WT levels. This was associated with the N-deposition induced increase in denitrification-related gene abundances of narG, nirS, norB and nosZ at WT-30 and narG at WT10. Additionally, the N2O emission factor assigned to N deposition was 1.3 % at WT-30 and 0.9 % at WT10, respectively. Our study provided comprehensive understanding of the mechanisms referring N2O emissions in response to the interactions between climate change and human disturbance from this high-altitude peatland.
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Affiliation(s)
- Wantong Zhang
- Institute of Wetland Research, Chinese Academy of Forestry, Beijing Key Laboratory of Wetland Services and Restoration, Beijing 100091, China; Insititute of Urban Agriculture, Chinese Academy of Agricultural Sciences, Chengdu 610218, China; Sino-Danish Centre for Education and Research, University of Chinese Academy of Sciences, Beijing 100049, China
| | - Xiuping Tao
- Insititute of Urban Agriculture, Chinese Academy of Agricultural Sciences, Chengdu 610218, China
| | - Zhengyi Hu
- Sino-Danish Centre for Education and Research, University of Chinese Academy of Sciences, Beijing 100049, China
| | - Enze Kang
- Institute of Wetland Research, Chinese Academy of Forestry, Beijing Key Laboratory of Wetland Services and Restoration, Beijing 100091, China
| | - Zhongqing Yan
- Institute of Wetland Research, Chinese Academy of Forestry, Beijing Key Laboratory of Wetland Services and Restoration, Beijing 100091, China; Sichuan Zoige Wetland Ecosystem Research Station, Tibetan Autonomous Prefecture of Aba 624500, China
| | - Xiaodong Zhang
- Institute of Wetland Research, Chinese Academy of Forestry, Beijing Key Laboratory of Wetland Services and Restoration, Beijing 100091, China; Sichuan Zoige Wetland Ecosystem Research Station, Tibetan Autonomous Prefecture of Aba 624500, China
| | - Jinzhi Wang
- Institute of Wetland Research, Chinese Academy of Forestry, Beijing Key Laboratory of Wetland Services and Restoration, Beijing 100091, China; Sichuan Zoige Wetland Ecosystem Research Station, Tibetan Autonomous Prefecture of Aba 624500, China.
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23
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Nielsen CK, Elsgaard L, Jørgensen U, Lærke PE. Soil greenhouse gas emissions from drained and rewetted agricultural bare peat mesocosms are linked to geochemistry. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 896:165083. [PMID: 37391135 DOI: 10.1016/j.scitotenv.2023.165083] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/23/2022] [Revised: 06/19/2023] [Accepted: 06/21/2023] [Indexed: 07/02/2023]
Abstract
In view of climate considerations regarding the management of peatlands, there is a need to assess whether rewetting can mitigate greenhouse gas (GHG) emissions, and notably how site-specific soil-geochemistry will influence differences in emission magnitudes. However, there are inconsistent results regarding the correlation of soil properties with heterotrophic respiration (Rh) of carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) from bare peat. In this study, we determined 1) soil-, and site-specific geochemical components as drivers for emissions from Rh on five Danish fens and bogs, and 2) emission magnitudes under drained and rewetted conditions. For this, a mesocosm experiment was performed under equal exposure to climatic conditions and water table depths controlled to either -40 cm, or -5 cm. For the drained soils, we found that annual cumulative emissions, accounting for all three gases, were dominated by CO2, contributing with, on average, 99 % to a varying global warming potential (GWP) of 12.2-16.9 t CO2eq ha-1 yr-1. Rewetting lowered annual cumulative emissions from Rh by 3.2-5.1 t CO2eq ha-1 yr-1 for fens and bogs, respectively, despite a high variability of site-specific CH4 emissions, contributing with 0.3-3.4 t CO2 ha-1 yr-1 to the GWP. Overall, analyses using generalized additive models (GAM) showed that emission magnitudes were well explained by geochemical variables. Under drained conditions, significant soil-specific predictor variables for CO2 flux magnitudes were pH, phosphorus (P), and the soil substrate's relative water holding capacity (WHC). When rewetted, CO2 and CH4 emissions from Rh were affected by pH, WHC, as well as contents of P, total carbon and nitrogen. In conclusion, our results found the highest GHG reduction on fen peatlands, further highlighting that peat nutrient status and acidity, and the potential availability of alternative electron acceptors, might be used as proxies for prioritising peatland areas for GHG mitigation efforts by rewetting.
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Affiliation(s)
- C K Nielsen
- Department of Agroecology, Faculty of Technology, Aarhus University, Blichers Alle 20, 8830 Tjele, Denmark; CBIO, Centre for Circular Bioeconomy, Aarhus University, Denmark.
| | - L Elsgaard
- Department of Agroecology, Faculty of Technology, Aarhus University, Blichers Alle 20, 8830 Tjele, Denmark
| | - U Jørgensen
- Department of Agroecology, Faculty of Technology, Aarhus University, Blichers Alle 20, 8830 Tjele, Denmark; CBIO, Centre for Circular Bioeconomy, Aarhus University, Denmark
| | - P E Lærke
- Department of Agroecology, Faculty of Technology, Aarhus University, Blichers Alle 20, 8830 Tjele, Denmark; CBIO, Centre for Circular Bioeconomy, Aarhus University, Denmark
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24
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Tuohy P, O' Sullivan L, Bracken CJ, Fenton O. Drainage status of grassland peat soils in Ireland: Extent, efficacy and implications for GHG emissions and rewetting efforts. JOURNAL OF ENVIRONMENTAL MANAGEMENT 2023; 344:118391. [PMID: 37354592 DOI: 10.1016/j.jenvman.2023.118391] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/28/2023] [Revised: 06/01/2023] [Accepted: 06/11/2023] [Indexed: 06/26/2023]
Abstract
Peatlands have been artificially drained and degraded over 100s of years and have released huge amounts of carbon dioxide (CO2) as a result. In organic grassland soils, raising the water table to prevent such emissions is being proposed to meet national greenhouse gas emission targets for the land use sector. At present, all of these soils (335,000 ha) are assumed to be drained (as no information has been available on their drainage status) within national emission inventory reporting and are therefore responsible for significant emissions (8-9 million tonnes CO2-equivalent annually). The objective of the present study was to collate studies relating to the drainage status of peat soils in Ireland to present alternative scenarios with regard to actual drainage status of organic soils and their estimated emissions. From a drainage design perspective, evidence suggests that relatively small proportions of the grassland peat area was drained effectively using optimal in-field drain spacings required to control the water table at 0.4-0.5 m. Open drains excavated on such soils have limited capacity to laterally control the water table depth beyond short distances. Furthermore, the lack of long-term routine maintenance post installation ensures the redundancy of many drainage systems over time. New drainage installations are therefore likely replacing existing infrastructure and not necessarily increasing the drained area at any given time. This evidence supports literature from the 1980s which state that relatively low proportions of the grassland peat area has been subjected to effective drainage. Scenario testing results showed that likely emissions from the most probable scenario (with total area drained equating to 90,000-120,000 ha) are 3.6-4.7 million tonnes CO2-equivalent, approximately 40-53% of current national emission inventory estimates. The incorporation of such a refinement into the national inventory could offer a significant reduction in estimated GHG emissions from the grassland land use sector in national emission inventory reporting.
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Affiliation(s)
- P Tuohy
- Animal and Grassland Research and Innovation Centre, Teagasc, Moorepark, Fermoy, Co. Cork, P61 P302, Ireland.
| | - L O' Sullivan
- Environmental Research Centre, Teagasc, Johnstown Castle, Wexford, Co. Wexford, Y35 Y521, Ireland.
| | - C J Bracken
- Environmental Research Centre, Teagasc, Johnstown Castle, Wexford, Co. Wexford, Y35 Y521, Ireland.
| | - O Fenton
- Environmental Research Centre, Teagasc, Johnstown Castle, Wexford, Co. Wexford, Y35 Y521, Ireland.
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25
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Parker TC, Clemmensen KE. Understanding the role of fungi in peatland degradation after drainage. THE NEW PHYTOLOGIST 2023; 240:10-12. [PMID: 37551053 DOI: 10.1111/nph.19196] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 08/09/2023]
Abstract
This article is a Commentary on Defrenne et al. (2023), 240: 412–425.
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Affiliation(s)
- Thomas C Parker
- Ecological Sciences, The James Hutton Institute, Craigiebuckler, Aberdeen, AB15 8QH, UK
| | - Karina E Clemmensen
- Department of Forest Mycology and Plant Pathology, Swedish University of Agricultural Sciences, Uppsala, SE-75007, Sweden
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26
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Li K, Wang Z, Xiang Q, Zhao X, Ji L, Xin Y, Sun J, Liu C, Shen X, Xu X, Chen Q. Coupling of soil methane emissions at different depths under typical coastal wetland vegetation types. CHEMOSPHERE 2023; 338:139505. [PMID: 37454988 DOI: 10.1016/j.chemosphere.2023.139505] [Citation(s) in RCA: 2] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/30/2023] [Revised: 07/02/2023] [Accepted: 07/12/2023] [Indexed: 07/18/2023]
Abstract
As an important source of atmospheric methane, methane emissions from coastal wetlands are affected by many factors. However, the methane emission process and interrelated coupling mechanisms in coastal wetland soils of a variety of environments remain unclear owing to complex interactions between intensified anthropogenic activities and climate change in recent years. In this study, we investigated methane cycling processes and the response mechanisms of environmental and microbial factors in soils at different depths under four typical coastal wetland vegetation types of the Yellow River Delta, China, using laboratory culture and molecular biology techniques. Our results show that methane generation pathways differed among the different soil layers, and that the methane emission process has a special response to soil N compounds (NO3-, NH4+). We found that nitrogen can indirectly affect methane emission by impacting key physicochemical properties (pH, oxidation reduction potential, etc.) and some functional communities (mcrA, ANME-2d, sulfate-reducing bacteria (SRB), narG, nosZII). Methane production processes in shallow soils compete closely with sulfate reduction processes, while methane emissions facilitated in deeper soils due to denitrification processes. We believe that our results provide a reference for future research and wetland management practices that seek to mitigate the global greenhouse effect and climate change.
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Affiliation(s)
- Kun Li
- College of Geography and Environment, Shandong Normal University, Jinan, 250014, PR China
| | - Zihao Wang
- College of Geography and Environment, Shandong Normal University, Jinan, 250014, PR China; College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao, 266100, PR China
| | - Qingyue Xiang
- College of Geography and Environment, Shandong Normal University, Jinan, 250014, PR China
| | - Xinkun Zhao
- College of Geography and Environment, Shandong Normal University, Jinan, 250014, PR China
| | - Linhui Ji
- College of Geography and Environment, Shandong Normal University, Jinan, 250014, PR China
| | - Yu Xin
- College of Geography and Environment, Shandong Normal University, Jinan, 250014, PR China
| | - Jingyu Sun
- College of Geography and Environment, Shandong Normal University, Jinan, 250014, PR China
| | - Chenmiao Liu
- College of Geography and Environment, Shandong Normal University, Jinan, 250014, PR China
| | - Xiaoyan Shen
- College of Geography and Environment, Shandong Normal University, Jinan, 250014, PR China
| | - Xiaoya Xu
- College of Geography and Environment, Shandong Normal University, Jinan, 250014, PR China.
| | - Qingfeng Chen
- College of Geography and Environment, Shandong Normal University, Jinan, 250014, PR China.
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27
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Tian W, Wang H, Xiang X, Loni PC, Qiu X, Wang R, Huang X, Tuovinen OH. Water table level controls methanogenic and methanotrophic communities and methane emissions in a Sphagnum-dominated peatland. Microbiol Spectr 2023; 11:e0199223. [PMID: 37747896 PMCID: PMC10580971 DOI: 10.1128/spectrum.01992-23] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/15/2023] [Accepted: 07/27/2023] [Indexed: 09/27/2023] Open
Abstract
Peatlands are important sources of the greenhouse gas methane emissions equipoised by methanogens and methanotrophs. However, knowledge about how microbial functional groups associated with methane production and oxidation respond to water table fluctuations has been limited to date. Here, methane-related microbial communities and the potentials of methane production and oxidation were determined along sectioned peat layers in a subalpine peatland across four Sphagnum-dominated sites with different water table levels. Methane fluxes were also monitored at these sites. The results showed that mcrA gene copies for methanogens were the highest in the 10- to 15-cm peat layer, which was also characterized by the maximum potential methane production (24.53 ± 1.83 nmol/g/h). Copy numbers of the pmoA gene for type Ia and Ib methanotrophs were enriched in the 0-5 cm peat layer with the highest potential methane oxidation (43.09 ± 3.44 nmol/g/h). For the type II methanotrophs, the pmoA gene copies were higher in the 10- to 15-cm peat layer. Hydrogenotrophic methanogens and type II methanotrophs dominated the methane functional groups. Deterministic process contributed more to methanogenic and methanotrophic community assemblages in comparison with stochastic process. The level of water table significantly shaped methanogenic and methanotrophic community structures and regulated methane fluxes. Compared with vascular plants, Sphagnum mosses significantly reduced the methane emissions in peatlands. Collectively, these findings enhance a comprehensive understanding of the effect of the water table level on methane functional groups, with consequential implications for reducing methane emissions within peatland ecosystems.IMPORTANCEThe water table level is recognized as a critical factor in regulating methane emissions, which are largely dependent on the balance of methanogens and methanotrophs. Previous studies on peat methane emissions have been mostly focused on spatial-temporal variations and the relationship with meteorological conditions. However, the role of the water table level in methane emissions remains unknown. In this work, four representative microhabitats along a water table gradient in a Sphagnum-dominated peatland were sampled to gain an insight into methane functional communities and methane emissions as affected by the water table level. The changes in methane-related microbial community structure and assembly were used to characterize the response to the water table level. This study improves the understanding of the changes in methane-related microbial communities and methane emissions with water table levels in peatlands.
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Affiliation(s)
- Wen Tian
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China
- College of Resource and Environment, Anhui Science and Technology of University, Chuzhou, China
- Hubei Key Laboratory of Critical Zone Evolution, China University of Geosciences, Wuhan, China
| | - Hongmei Wang
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China
| | - Xing Xiang
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China
- College of Life Science, Shangrao Normal University, Shangrao, China
| | - Prakash C. Loni
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China
| | - Xuan Qiu
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China
| | - Ruicheng Wang
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China
| | - Xianyu Huang
- Hubei Key Laboratory of Critical Zone Evolution, China University of Geosciences, Wuhan, China
| | - Olli H. Tuovinen
- Department of Microbiology, Ohio State University, Columbus, Ohio, USA
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28
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Temmink RJM, Robroek BJM, van Dijk G, Koks AHW, Käärmelahti SA, Barthelmes A, Wassen MJ, Ziegler R, Steele MN, Giesen W, Joosten H, Fritz C, Lamers LPM, Smolders AJP. Wetscapes: Restoring and maintaining peatland landscapes for sustainable futures. AMBIO 2023; 52:1519-1528. [PMID: 37222914 PMCID: PMC10406990 DOI: 10.1007/s13280-023-01875-8] [Citation(s) in RCA: 2] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/01/2023] [Revised: 04/21/2023] [Accepted: 04/24/2023] [Indexed: 05/25/2023]
Abstract
Peatlands are among the world's most carbon-dense ecosystems and hotspots of carbon storage. Although peatland drainage causes strong carbon emissions, land subsidence, fires and biodiversity loss, drainage-based agriculture and forestry on peatland is still expanding on a global scale. To maintain and restore their vital carbon sequestration and storage function and to reach the goals of the Paris Agreement, rewetting and restoration of all drained and degraded peatlands is urgently required. However, socio-economic conditions and hydrological constraints hitherto prevent rewetting and restoration on large scale, which calls for rethinking landscape use. We here argue that creating integrated wetscapes (wet peatland landscapes), including nature preserve cores, buffer zones and paludiculture areas (for wet productive land use), will enable sustainable and complementary land-use functions on the landscape level. As such, transforming landscapes into wetscapes presents an inevitable, novel, ecologically and socio-economically sound alternative for drainage-based peatland use.
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Affiliation(s)
- Ralph J. M. Temmink
- Environmental Sciences, Copernicus Institute of Sustainable Development, Utrecht University, Princetonlaan 8a, 3584 CB Utrecht, The Netherlands
- Aquatic Ecology and Environmental Biology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ Nijmegen, The Netherlands
| | - Bjorn J. M. Robroek
- Aquatic Ecology and Environmental Biology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ Nijmegen, The Netherlands
- School of Biological Science, University of Southampton, Southampton, SO17 1BJ UK
| | - Gijs van Dijk
- Aquatic Ecology and Environmental Biology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ Nijmegen, The Netherlands
- B-WARE Research Centre, Toernooiveld 1, 6525 ED Nijmegen, The Netherlands
| | - Adam H. W. Koks
- Aquatic Ecology and Environmental Biology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ Nijmegen, The Netherlands
- B-WARE Research Centre, Toernooiveld 1, 6525 ED Nijmegen, The Netherlands
| | - Sannimari A. Käärmelahti
- Aquatic Ecology and Environmental Biology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ Nijmegen, The Netherlands
| | - Alexandra Barthelmes
- Institute of Botany and Landscape Ecology, University of Greifswald, Partner in the Greifswald Mire Centre, Soldmannstr. 15, 17487 Greifswald, Germany
| | - Martin J. Wassen
- Environmental Sciences, Copernicus Institute of Sustainable Development, Utrecht University, Princetonlaan 8a, 3584 CB Utrecht, The Netherlands
| | - Rafael Ziegler
- Department of Management, HEC Montréal, Édifice Côte-Sainte-Catherine 3000, Chemin de La Côte-Sainte-Catherine, Montreal, Canada
| | - Magdalena N. Steele
- School of Biological Science, University of Southampton, Southampton, SO17 1BJ UK
| | - Wim Giesen
- Associate with Naturalis Biodiversity Center, Darwinweg 2, 2333 CR Leiden, The Netherlands
| | - Hans Joosten
- Institute of Botany and Landscape Ecology, University of Greifswald, Partner in the Greifswald Mire Centre, Soldmannstr. 15, 17487 Greifswald, Germany
| | - Christian Fritz
- Aquatic Ecology and Environmental Biology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ Nijmegen, The Netherlands
| | - Leon P. M. Lamers
- Aquatic Ecology and Environmental Biology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ Nijmegen, The Netherlands
- B-WARE Research Centre, Toernooiveld 1, 6525 ED Nijmegen, The Netherlands
| | - Alfons J. P. Smolders
- Aquatic Ecology and Environmental Biology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ Nijmegen, The Netherlands
- B-WARE Research Centre, Toernooiveld 1, 6525 ED Nijmegen, The Netherlands
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Jovani‐Sancho AJ, O'Reilly P, Anshari G, Chong XY, Crout N, Evans CD, Evers S, Gan JY, Gibbins CN, Gusmayanti E, Jamaludin J, Jaya A, Page S, Yosep Y, Upton C, Wilson P, Sjögersten S. CH 4 and N 2 O emissions from smallholder agricultural systems on tropical peatlands in Southeast Asia. GLOBAL CHANGE BIOLOGY 2023; 29:4279-4297. [PMID: 37100767 PMCID: PMC10946781 DOI: 10.1111/gcb.16747] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/01/2022] [Revised: 04/11/2023] [Accepted: 04/13/2023] [Indexed: 05/17/2023]
Abstract
There are limited data for greenhouse gas (GHG) emissions from smallholder agricultural systems in tropical peatlands, with data for non-CO2 emissions from human-influenced tropical peatlands particularly scarce. The aim of this study was to quantify soil CH4 and N2 O fluxes from smallholder agricultural systems on tropical peatlands in Southeast Asia and assess their environmental controls. The study was carried out in four regions in Malaysia and Indonesia. CH4 and N2 O fluxes and environmental parameters were measured in cropland, oil palm plantation, tree plantation and forest. Annual CH4 emissions (in kg CH4 ha-1 year-1 ) were: 70.7 ± 29.5, 2.1 ± 1.2, 2.1 ± 0.6 and 6.2 ± 1.9 at the forest, tree plantation, oil palm and cropland land-use classes, respectively. Annual N2 O emissions (in kg N2 O ha-1 year-1 ) were: 6.5 ± 2.8, 3.2 ± 1.2, 21.9 ± 11.4 and 33.6 ± 7.3 in the same order as above, respectively. Annual CH4 emissions were strongly determined by water table depth (WTD) and increased exponentially when annual WTD was above -25 cm. In contrast, annual N2 O emissions were strongly correlated with mean total dissolved nitrogen (TDN) in soil water, following a sigmoidal relationship, up to an apparent threshold of 10 mg N L-1 beyond which TDN seemingly ceased to be limiting for N2 O production. The new emissions data for CH4 and N2 O presented here should help to develop more robust country level 'emission factors' for the quantification of national GHG inventory reporting. The impact of TDN on N2 O emissions suggests that soil nutrient status strongly impacts emissions, and therefore, policies which reduce N-fertilisation inputs might contribute to emissions mitigation from agricultural peat landscapes. However, the most important policy intervention for reducing emissions is one that reduces the conversion of peat swamp forest to agriculture on peatlands in the first place.
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Affiliation(s)
| | - Patrick O'Reilly
- School of Geography, Geology & the EnvironmentUniversity of LeicesterLeicesterUK
- School of Biological and Environmental SciencesLiverpool John Mores UniversityLiverpoolUK
| | - Gusti Anshari
- Magister of Environmental ScienceUniversitas TanjungpuraPontianakIndonesia
- Soil Science DepartmentUniversitas TanjungpuraPontianakIndonesia
| | - Xin Yi Chong
- School of Environmental and Geographical SciencesUniversity of Nottingham MalaysiaSemenyihMalaysia
| | - Neil Crout
- School of BiosciencesUniversity of NottinghamLoughboroughUK
| | | | - Stephanie Evers
- School of Biological and Environmental SciencesLiverpool John Mores UniversityLiverpoolUK
- School of Environmental and Geographical SciencesUniversity of Nottingham MalaysiaSemenyihMalaysia
| | - Jing Ye Gan
- School of Environmental and Geographical SciencesUniversity of Nottingham MalaysiaSemenyihMalaysia
| | - Christopher N. Gibbins
- School of Environmental and Geographical SciencesUniversity of Nottingham MalaysiaSemenyihMalaysia
| | - Evi Gusmayanti
- Magister of Environmental ScienceUniversitas TanjungpuraPontianakIndonesia
- Agrotechnology DepartmentUniversitas TanjungpuraPontianakIndonesia
| | | | - Adi Jaya
- Faculty of AgricultureUniversity of Palangka RayaPalangka RayaIndonesia
| | - Susan Page
- School of Geography, Geology & the EnvironmentUniversity of LeicesterLeicesterUK
| | - Yosep Yosep
- Faculty of AgricultureUniversity of Palangka RayaPalangka RayaIndonesia
| | - Caroline Upton
- School of Geography, Geology & the EnvironmentUniversity of LeicesterLeicesterUK
| | - Paul Wilson
- School of BiosciencesUniversity of NottinghamLoughboroughUK
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30
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Wang Y, Xue K. Cold-adaptative methanogens and methanotrophs drive ecosystem feedback. Sci Bull (Beijing) 2023; 68:1359-1360. [PMID: 37321870 DOI: 10.1016/j.scib.2023.05.032] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 06/17/2023]
Affiliation(s)
- Yanfen Wang
- College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China; Beijing Yanshan Earth Critical Zone National Research Station, University of Chinese Academy of Sciences, Beijing 101408, China; State Key Laboratory of Tibetan Plateau Earth System Science (LATPES), Beijing 100101, China.
| | - Kai Xue
- College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China; Beijing Yanshan Earth Critical Zone National Research Station, University of Chinese Academy of Sciences, Beijing 101408, China
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31
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Antonijević D, Hoffmann M, Prochnow A, Krabbe K, Weituschat M, Couwenberg J, Ehlert S, Zak D, Augustin J. The unexpected long period of elevated CH 4 emissions from an inundated fen meadow ended only with the occurrence of cattail (Typha latifolia). GLOBAL CHANGE BIOLOGY 2023; 29:3678-3691. [PMID: 37029755 DOI: 10.1111/gcb.16713] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/06/2022] [Accepted: 03/17/2023] [Indexed: 06/06/2023]
Abstract
Drainage and agricultural use transform natural peatlands from a net carbon (C) sink to a net C source. Rewetting of peatlands, despite of high methane (CH4 ) emissions, holds the potential to mitigate climate change by greatly reducing CO2 emissions. However, the time span for this transition is unknown because most studies are limited to a few years. Especially, nonpermanent open water areas often created after rewetting, are highly productive. Here, we present 14 consecutive years of CH4 flux measurements following rewetting of a formerly long-term drained peatland in the Peene valley. Measurements were made at two rewetted sites (non-inundated vs. inundated) using manual chambers. During the study period, significant differences in measured CH4 emissions occurred. In general, these differences overlapped with stages of ecosystem transition from a cultivated grassland to a polytrophic lake dominated by emergent helophytes, but could also be additionally explained by other variables. This transition started with a rapid vegetation shift from dying cultivated grasses to open water floating and submerged hydrophytes and significantly increased CH4 emissions. Since 2008, helophytes have gradually spread from the shoreline into the open water area, especially in drier years. This process was periodically delayed by exceptional inundation and eventually resulted in the inundated site being covered by emergent helophytes. While the period between 2009 and 2015 showed exceptionally high CH4 emissions, these decreased significantly after cattail and other emergent helophytes became dominant at the inundated site. Therefore, CH4 emissions declined only after 10 years of transition following rewetting, potentially reaching a new steady state. Overall, this study highlights the importance of an integrative approach to understand the shallow lakes CH4 biogeochemistry, encompassing the entire area with its mosaic of different vegetation forms. This should be ideally done through a study design including proper measurement site allocation as well as long-term measurements.
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Affiliation(s)
- Danica Antonijević
- Research Area 1: Landscape Functioning, Leibniz Centre for Agricultural Landscape Research (ZALF) e.V., Müncheberg, Germany
| | - Mathias Hoffmann
- Research Area 1: Landscape Functioning, Leibniz Centre for Agricultural Landscape Research (ZALF) e.V., Müncheberg, Germany
| | - Annette Prochnow
- Leibniz-Institute for Agricultural Engineering Potsdam-Bornim, Potsdam, Germany
- Albrecht Daniel Thaer Institute for Agricultural and Horticultural Sciences, Humboldt Universität zu Berlin, Berlin, Germany
| | - Karoline Krabbe
- Institute of Botany and Landscape Ecology, Greifswald University, Partner in the Greifswald Mire Centre, Greifswald, Germany
| | - Mirjam Weituschat
- Institute of Botany and Landscape Ecology, Greifswald University, Partner in the Greifswald Mire Centre, Greifswald, Germany
| | - John Couwenberg
- Institute of Botany and Landscape Ecology, Greifswald University, Partner in the Greifswald Mire Centre, Greifswald, Germany
| | - Sigrid Ehlert
- Research Area 2: Land Use and Governance, Leibniz Centre for Agricultural Landscape Research (ZALF) e.V., Müncheberg, Germany
| | - Dominik Zak
- Department of Ecoscience, Aarhus University, Silkeborg, Denmark
- Department of Ecohydrology and Biogeochemistry, Leibniz-Institute of Freshwater Ecology and Inland Fisheries, Berlin, Germany
| | - Jürgen Augustin
- Research Area 1: Landscape Functioning, Leibniz Centre for Agricultural Landscape Research (ZALF) e.V., Müncheberg, Germany
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Chen X, Xue D, Wang Y, Qiu Q, Wu L, Wang M, Liu J, Chen H. Variations in the archaeal community and associated methanogenesis in peat profiles of three typical peatland types in China. ENVIRONMENTAL MICROBIOME 2023; 18:48. [PMID: 37280702 DOI: 10.1186/s40793-023-00503-y] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/08/2023] [Accepted: 05/15/2023] [Indexed: 06/08/2023]
Abstract
BACKGROUND Peatlands contain about 500 Pg of carbon worldwide and play a dual role as both a carbon sink and an important methane (CH4) source, thereby potentially influencing climate change. However, systematic studies on peat properties, microorganisms, methanogenesis, and their interrelations in peatlands remain limited, especially in China. Therefore, the present study aims to investigate the physicochemical properties, archaeal community, and predominant methanogenesis pathways in three typical peatlands in China, namely Hani (H), Taishanmiao (T), and Ruokeba (R) peatlands, and quantitively determine their CH4 production potentials. RESULTS These peatlands exhibited high water content (WC) and total carbon content (TC), as well as low pH values. In addition, R exhibited a lower dissolved organic carbon concentration (DOC), as well as higher total iron content (TFe) and pH values compared to those observed in T. There were also clear differences in the archaeal community between the three peatlands, especially in the deep peat layers. The average relative abundance of the total methanogens ranged from 10 to 12%, of which Methanosarcinales and Methanomicrobiales were the most abundant in peat samples (8%). In contrast, Methanobacteriales were mainly distributed in the upper peat layer (0-40 cm). Besides methanogens, Marine Benthic Group D/Deep-Sea Hydrothermal Vent Euryarchaeotic Group 1 (MBG-D/DHVEG-1), Nitrosotaleales, and several other orders of Bathyarchaeota also exhibited high relative abundances, especially in T. This finding might be due to the unique geological conditions, suggesting high archaeal diversity in peatlands. In addition, the highest and lowest CH4 production potentials were 2.38 and 0.22 μg g-1 d-1 in H and R, respectively. The distributions of the dominant methanogens were consistent with the respective methanogenesis pathways in the three peatlands. The pH, DOC, and WC were strongly correlated with CH4 production potentials. However, no relationship was found between CH4 production potential and methanogens, suggesting that CH4 production in peatlands may not be controlled by the relative abundance of methanogens. CONCLUSIONS The results of the present study provide further insights into CH4 production in peatlands in China, highlighting the importance of the archaeal community and peat physicochemical properties for studies on methanogenesis in distinct types of peatlands.
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Affiliation(s)
- Xuhui Chen
- CAS Key Laboratory of Mountain Ecological Restoration and Bioresource Utilization and Ecological Restoration Biodiversity Conservation Key Laboratory of Sichuan Province, Chengdu Institute of Biology, Chinese Academy of Sciences, No. 9, Section 4, South Renmin Road, Chengdu, 610041, China
- Zoige Peatland and Global Change Research Station, Chinese Academy of Sciences, Hongyuan, 624400, China
- University of Chinese Academy of Sciences, Beijing, 100049, China
| | - Dan Xue
- CAS Key Laboratory of Mountain Ecological Restoration and Bioresource Utilization and Ecological Restoration Biodiversity Conservation Key Laboratory of Sichuan Province, Chengdu Institute of Biology, Chinese Academy of Sciences, No. 9, Section 4, South Renmin Road, Chengdu, 610041, China.
- Zoige Peatland and Global Change Research Station, Chinese Academy of Sciences, Hongyuan, 624400, China.
| | - Yue Wang
- CAS Key Laboratory of Mountain Ecological Restoration and Bioresource Utilization and Ecological Restoration Biodiversity Conservation Key Laboratory of Sichuan Province, Chengdu Institute of Biology, Chinese Academy of Sciences, No. 9, Section 4, South Renmin Road, Chengdu, 610041, China
- University of Chinese Academy of Sciences, Beijing, 100049, China
| | - Qing Qiu
- CAS Key Laboratory of Mountain Ecological Restoration and Bioresource Utilization and Ecological Restoration Biodiversity Conservation Key Laboratory of Sichuan Province, Chengdu Institute of Biology, Chinese Academy of Sciences, No. 9, Section 4, South Renmin Road, Chengdu, 610041, China
- Zoige Peatland and Global Change Research Station, Chinese Academy of Sciences, Hongyuan, 624400, China
- University of Chinese Academy of Sciences, Beijing, 100049, China
| | - Lin Wu
- School of Forestry and Horticulture, Hubei Minzu University, Enshi, 445000, Hubei, China
| | - Meng Wang
- State Environmental Protection Key Laboratory of Wetland Ecology and Vegetation Restoration, Institute for Peat and Mire Research, Northeast Normal University, Changchun, 130024, China
| | - Jiawen Liu
- SQE Department, COFCO Coca-Cola Beverages (Sichuan) Company Limited, Chengdu, 610500, China
| | - Huai Chen
- CAS Key Laboratory of Mountain Ecological Restoration and Bioresource Utilization and Ecological Restoration Biodiversity Conservation Key Laboratory of Sichuan Province, Chengdu Institute of Biology, Chinese Academy of Sciences, No. 9, Section 4, South Renmin Road, Chengdu, 610041, China.
- Zoige Peatland and Global Change Research Station, Chinese Academy of Sciences, Hongyuan, 624400, China.
- CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences (CAS), Beijing, 100101, China.
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Thers H, Knudsen MT, Lærke PE. Comparison of GHG emissions from annual crops in rotation on drained temperate agricultural peatland with production of reed canary grass in paludiculture using an LCA approach. Heliyon 2023; 9:e17320. [PMID: 37441396 PMCID: PMC10333457 DOI: 10.1016/j.heliyon.2023.e17320] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/03/2023] [Revised: 05/15/2023] [Accepted: 06/13/2023] [Indexed: 07/15/2023] Open
Abstract
Drained peat soils contribute significantly to global human-caused CO2 emissions and reducing peat degradation via rewetting is high on the political agenda. Ceasing agricultural activities on rewetted soils might lead to land owner resistance and high societal expenses to compensate farmers. Continued biomass production adapted for wet conditions on peat soils potentially minimizes these costs and helps supplying the growing demand for e.g. materials, fuels and feed. Here we used a life cycle assessment approach (cradle to farm gate) to investigate the greenhouse gas (GHG) emissions related to three cases by applying IPCC (Intergovernmental Panel on Climate Change) emission factors and specific site conditions at a bog and a fen site that represent widely distributed temperate peat soils. Besides soil emissions, upstream emissions from input, operational emissions and emission related to rewetting construction work were included. The analyzed systems were deeply drained cash cropping on agricultural bog (potatoes (Solanum tuberosum L.), spring barley (Hordeum vulgare L.) and oat (Avena sativa L.), permanent Reed canary grass (RCG) (Phalaris arundinacea L.) production on non-drained bog and permanent RCG production on shallow-drained fen. The annual mean water table depths (WTD) were -70, -38 (estimated) and -13 cm, respectively. Results showed estimated GHG emissions of 40.5, 26.1 and 20.6 Mg CO2eq ha-1, respectively, corresponding to a 35% GHG reduction for the non-drained bog case as compared to the drained bog case, despite that the obtained WTD due to ceased drainage did not adhere to the IPCC rewetting threshold of -30 cm. Emissions related to crop management represented 7, 14 and 19% of total emissions. In the RCG cultivation on fen case, the WTD were controlled primarily by the water table of the nearby stream and total GHG emissions were even lower as compared to the RCG production on the non-drained bog reflecting the difference in WTD. Rewetting projects need to include careful knowledge of the specific peat area to foresee the actual reduction potential.
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Liu W, Fritz C, van Belle J, Nonhebel S. Production in peatlands: Comparing ecosystem services of different land use options following conventional farming. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 875:162534. [PMID: 36878291 DOI: 10.1016/j.scitotenv.2023.162534] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/26/2022] [Revised: 02/24/2023] [Accepted: 02/25/2023] [Indexed: 06/18/2023]
Abstract
Majority of Dutch peatlands are drained and used intensively as grasslands for dairy farming. This delivers high productivity but causes severe damage to ecosystem services supply. Peatland rewetting is the best way to reverse the damage, but high water levels do not fit with intensive dairy production. Paludiculture, defined as crop production under wet conditions, provides viable land use alternatives. However, performance of paludiculture is rarely compared to drainage-based agriculture. Here, we compared the performances of six land use options on peatland following a gradient of low, medium, and high water levels, including conventional and organic drainage-based dairy farming, low-input grasslands for grazing and mowing, and high-input paludiculture with reed and Sphagnum cultivation. For each land use option, we conducted environmental system analysis on model farm system defined by a literature based inventory analysis. The analysis used five ecosystem services as indicators of environmental impacts with a functional unit of 1-ha peat soil. Ecosystem services included biomass provisioning, climate, water, and nutrient regulation, and maintenance of habitat. Results showed that drainage-based dairy farming systems support high provisioning services but low regulation and maintenance services. Organic farming provides higher climate and nutrient regulation services than its conventional counterpart, but limited overall improvement due to the persistent drainage. Low-intensity grassland and paludiculture systems have high regulation and maintenance services value, but do not supply biomass provisioning comparable to the drainage-based systems. Without capitalizing the co-benefits of regulation and maintenance services, and accounting for the societal costs from ecosystem disservices including greenhouse gas emission and nitrogen pollution, it is not likely that the farmers will be incentivized to change the current farming system towards the wetter alternatives. Sustainable use of peatlands urges fundamental changes in land and water management along with the financial and policy support required.
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Affiliation(s)
- Weier Liu
- Integrated Research on Energy, Environment and Society (IREES), University of Groningen, the Netherlands.
| | - Christian Fritz
- Integrated Research on Energy, Environment and Society (IREES), University of Groningen, the Netherlands; Institute for Water and Wetland Research, Radboud University Nijmegen, the Netherlands
| | - Jasper van Belle
- Van Hall Larenstein University of Applied Sciences, the Netherlands
| | - Sanderine Nonhebel
- Integrated Research on Energy, Environment and Society (IREES), University of Groningen, the Netherlands
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Deshmukh CS, Susanto AP, Nardi N, Nurholis N, Kurnianto S, Suardiwerianto Y, Hendrizal M, Rhinaldy A, Mahfiz RE, Desai AR, Page SE, Cobb AR, Hirano T, Guérin F, Serça D, Prairie YT, Agus F, Astiani D, Sabiham S, Evans CD. Net greenhouse gas balance of fibre wood plantation on peat in Indonesia. Nature 2023; 616:740-746. [PMID: 37020018 PMCID: PMC10132972 DOI: 10.1038/s41586-023-05860-9] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/30/2022] [Accepted: 02/16/2023] [Indexed: 04/07/2023]
Abstract
Tropical peatlands cycle and store large amounts of carbon in their soil and biomass1-5. Climate and land-use change alters greenhouse gas (GHG) fluxes of tropical peatlands, but the magnitude of these changes remains highly uncertain6-19. Here we measure net ecosystem exchanges of carbon dioxide, methane and soil nitrous oxide fluxes between October 2016 and May 2022 from Acacia crassicarpa plantation, degraded forest and intact forest within the same peat landscape, representing land-cover-change trajectories in Sumatra, Indonesia. This allows us to present a full plantation rotation GHG flux balance in a fibre wood plantation on peatland. We find that the Acacia plantation has lower GHG emissions than the degraded site with a similar average groundwater level (GWL), despite more intensive land use. The GHG emissions from the Acacia plantation over a full plantation rotation (35.2 ± 4.7 tCO2-eq ha-1 year-1, average ± standard deviation) were around two times higher than those from the intact forest (20.3 ± 3.7 tCO2-eq ha-1 year-1), but only half of the current Intergovernmental Panel on Climate Change (IPCC) Tier 1 emission factor (EF)20 for this land use. Our results can help to reduce the uncertainty in GHG emissions estimates, provide an estimate of the impact of land-use change on tropical peat and develop science-based peatland management practices as nature-based climate solutions.
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Affiliation(s)
- Chandra S Deshmukh
- Asia Pacific Resources International Ltd., Pelalawan Regency, Indonesia.
| | - Ari P Susanto
- Asia Pacific Resources International Ltd., Pelalawan Regency, Indonesia
| | - Nardi Nardi
- Asia Pacific Resources International Ltd., Pelalawan Regency, Indonesia
| | - Nurholis Nurholis
- Asia Pacific Resources International Ltd., Pelalawan Regency, Indonesia
| | - Sofyan Kurnianto
- Asia Pacific Resources International Ltd., Pelalawan Regency, Indonesia
| | | | - M Hendrizal
- Asia Pacific Resources International Ltd., Pelalawan Regency, Indonesia
| | - Ade Rhinaldy
- Asia Pacific Resources International Ltd., Pelalawan Regency, Indonesia
| | - Reyzaldi E Mahfiz
- Asia Pacific Resources International Ltd., Pelalawan Regency, Indonesia
| | - Ankur R Desai
- Department of Atmospheric and Oceanic Sciences, University of Wisconsin-Madison, Madison, WI, USA
| | - Susan E Page
- School of Geography, Geology and the Environment, University of Leicester, Leicester, UK
| | - Alexander R Cobb
- Singapore-MIT Alliance for Research and Technology, Singapore, Singapore
| | - Takashi Hirano
- Research Faculty of Agriculture, Hokkaido University, Sapporo, Japan
| | - Frédéric Guérin
- Géosciences Environnement Toulouse, CNRS, IRD, Université Paul-Sabatier, Toulouse, France
| | - Dominique Serça
- LAERO, Université de Toulouse, CNRS, IRD, UT3, Toulouse, France
| | - Yves T Prairie
- UNESCO Chair in Global Environmental Change, Université du Québec à Montréal, Montréal, Québec, Canada
| | - Fahmuddin Agus
- National Research and Innovation Agency (BRIN), Cibinong, Indonesia
| | - Dwi Astiani
- Faculty of Forestry, Tanjungpura University, Pontianak, Indonesia
| | - Supiandi Sabiham
- Department of Soil Science and Land Resources, IPB University, Bogor, Indonesia
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36
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Li J, Jiang M, Pei J, Fang C, Li B, Nie M. Convergence of carbon sink magnitude and water table depth in global wetlands. Ecol Lett 2023; 26:797-804. [PMID: 36924007 DOI: 10.1111/ele.14199] [Citation(s) in RCA: 4] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/17/2022] [Revised: 02/21/2023] [Accepted: 02/21/2023] [Indexed: 03/18/2023]
Abstract
Wetlands are strategic areas for carbon uptake, but accurate assessments of their sequestration ability are limited by the uncertainty and variability in their carbon balances. Based on 2385 observations of annual net ecosystem production from global wetlands, we show that the mean net carbon sinks of inland wetlands, peatlands and coastal wetlands are 0.57, 0.29 and 1.88 tons of carbon per hectare per year, respectively, with a mean value of 0.57 tons of carbon per hectare per year weighted by the distribution area of different wetland types. Carbon sinks are mainly in Asia and North America. Within and across wetland types, we find that water table depth (WTD) exerts greater control than climate- and ecosystem-related variables, and an increase in WTD results in a stronger carbon sink. Our results highlight an urgent need to sustain wetland hydrology under global change; otherwise, wetlands are at high risk of becoming carbon sources to the atmosphere.
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Affiliation(s)
- Jinquan Li
- Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai, China
| | - Mingkai Jiang
- College of Life Sciences, Zhejiang University, Hangzhou, China
| | - Junmin Pei
- Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai, China
| | - Changming Fang
- Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai, China
| | - Bo Li
- Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai, China.,Yunnan Key Laboratory of Plant Reproductive Adaptation and Evolutionary Ecology and Centre for Invasion Biology, Institute of Biodiversity, School of Ecology and Environmental Science, Yunnan University, Kunming, China
| | - Ming Nie
- Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai, China
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Li G, Sun L, Wang J, Dou X, Ji S, Hu T, Gao C. Effects of pyrogenic carbon addition after fire on soil carbon mineralization in the Great Khingan Mountains peatlands (Northeast China). THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 864:161102. [PMID: 36566854 DOI: 10.1016/j.scitotenv.2022.161102] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/04/2022] [Revised: 12/16/2022] [Accepted: 12/17/2022] [Indexed: 06/17/2023]
Abstract
Wildfires play a critical role in regulating soil carbon (C) budgets in peatland ecosystems, and their frequency and intensity are increasing owing to climate change and human activities. Wildfires not only emit CO2 during the combustion process but also produce pyrogenic carbon (PyC), which accumulates in the soil C pool and influences soil C decomposition. However, the role of PyC after a fire in peatland soil C mineralization has rarely been examined. This study investigated the effects of PyC addition on peatland soil C mineralization and its potential driving mechanisms using an anaerobic/aerobic incubation experiment with peat soils collected from typical peatlands in the Great Khingan Mountains, Northeast China. The effect of PyC was more pronounced under aerobic conditions than under anaerobic conditions. The mean C- mineralization rates of soil were significantly increased by 45.2 ± 15.5 % and 87.6 ± 14.3 % with 10 % PyC250°C addition after the initial stage (D7) of aerobic and anaerobic incubation, but PyC600°C addition caused a to decrease. Compared with PyC600°C, PyC250°C addition significantly increased the available N content and altered the soil microbial activities, which may be the primary reason for the increase in C mineralization rates. Furthermore, adding a high concentration of PyC (10 %) reduced the concentration of phenolics but increased phenol oxidase activity, which promoted C mineralization rates. Thus, PyC250°C addition to peat soils mainly influences the microbial biomass C content through the accumulation of available N and phenolics, which ultimately positively affects C mineralization rates.
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Affiliation(s)
- Guangxin Li
- Key Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, College of Forestry, Northeast Forestry University, Hexing Road 26, Harbin 150040, China; Key Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Shengbei Street 4888, 130102 Changchun, China
| | - Long Sun
- Key Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, College of Forestry, Northeast Forestry University, Hexing Road 26, Harbin 150040, China
| | - Jianyu Wang
- Key Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, College of Forestry, Northeast Forestry University, Hexing Road 26, Harbin 150040, China
| | - Xu Dou
- Key Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, College of Forestry, Northeast Forestry University, Hexing Road 26, Harbin 150040, China
| | - Shengzhen Ji
- Key Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Shengbei Street 4888, 130102 Changchun, China
| | - Tongxin Hu
- Key Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, College of Forestry, Northeast Forestry University, Hexing Road 26, Harbin 150040, China.
| | - Chuanyu Gao
- Key Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Shengbei Street 4888, 130102 Changchun, China.
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38
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Hambäck PA, Dawson L, Geranmayeh P, Jarsjö J, Kačergytė I, Peacock M, Collentine D, Destouni G, Futter M, Hugelius G, Hedman S, Jonsson S, Klatt BK, Lindström A, Nilsson JE, Pärt T, Schneider LD, Strand JA, Urrutia-Cordero P, Åhlén D, Åhlén I, Blicharska M. Tradeoffs and synergies in wetland multifunctionality: A scaling issue. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 862:160746. [PMID: 36513236 DOI: 10.1016/j.scitotenv.2022.160746] [Citation(s) in RCA: 4] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/08/2022] [Revised: 08/31/2022] [Accepted: 12/03/2022] [Indexed: 06/17/2023]
Abstract
Wetland area in agricultural landscapes has been heavily reduced to gain land for crop production, but in recent years there is increased societal recognition of the negative consequences from wetland loss on nutrient retention, biodiversity and a range of other benefits to humans. The current trend is therefore to re-establish wetlands, often with an aim to achieve the simultaneous delivery of multiple ecosystem services, i.e., multifunctionality. Here we review the literature on key objectives used to motivate wetland re-establishment in temperate agricultural landscapes (provision of flow regulation, nutrient retention, climate mitigation, biodiversity conservation and cultural ecosystem services), and their relationships to environmental properties, in order to identify potential for tradeoffs and synergies concerning the development of multifunctional wetlands. Through this process, we find that there is a need for a change in scale from a focus on single wetlands to wetlandscapes (multiple neighboring wetlands including their catchments and surrounding landscape features) if multiple societal and environmental goals are to be achieved. Finally, we discuss the key factors to be considered when planning for re-establishment of wetlands that can support achievement of a wide range of objectives at the landscape scale.
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Affiliation(s)
- P A Hambäck
- Dept of Ecology, Environment and Plant Sciences, Stockholm University, Stockholm, Sweden.
| | - L Dawson
- School of Forest Management, Swedish University of Agricultural Sciences, Skinnskatteberg, Sweden
| | - P Geranmayeh
- Dept of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences, Uppsala, Sweden
| | - J Jarsjö
- Dept of Physical Geography, Stockholm University, Stockholm, Sweden
| | - I Kačergytė
- Dept of Ecology, Swedish University of Agricultural Sciences, Uppsala, Sweden
| | - M Peacock
- Dept of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences, Uppsala, Sweden; Dept of Geography and Planning, School of Environmental Sciences, University of Liverpool, UK
| | - D Collentine
- Dept of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences, Uppsala, Sweden
| | - G Destouni
- Dept of Physical Geography, Stockholm University, Stockholm, Sweden
| | - M Futter
- Dept of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences, Uppsala, Sweden
| | - G Hugelius
- Dept of Physical Geography, Stockholm University, Stockholm, Sweden
| | - S Hedman
- The Rural Economy and Agricultural Society, Eldsberga, Sweden
| | - S Jonsson
- Dept of Environmental Science, Stockholm University, Stockholm, Sweden
| | - B K Klatt
- The Rural Economy and Agricultural Society, Eldsberga, Sweden; Dept of Biology, Lund University, Lund, Sweden
| | - A Lindström
- National Veterinary Institute, Uppsala, Sweden
| | - J E Nilsson
- Dept of Environmental and Biosciences, Halmstad University, Halmstad, Sweden; Dept of Ecology and Genetics, Uppsala University, Uppsala, Sweden
| | - T Pärt
- Dept of Ecology, Swedish University of Agricultural Sciences, Uppsala, Sweden
| | - L D Schneider
- The Rural Economy and Agricultural Society, Eldsberga, Sweden
| | - J A Strand
- The Rural Economy and Agricultural Society, Eldsberga, Sweden
| | | | - D Åhlén
- Dept of Ecology, Environment and Plant Sciences, Stockholm University, Stockholm, Sweden
| | - I Åhlén
- Dept of Physical Geography, Stockholm University, Stockholm, Sweden
| | - M Blicharska
- Natural Resources and Sustainable Development, Dept of Earth Sciences, Uppsala University, Uppsala, Sweden
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39
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Li J, Pei J, Fang C, Li B, Nie M. Opposing seasonal temperature dependencies of CO 2 and CH 4 emissions from wetlands. GLOBAL CHANGE BIOLOGY 2023; 29:1133-1143. [PMID: 36385719 DOI: 10.1111/gcb.16528] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/02/2022] [Revised: 11/14/2022] [Accepted: 11/15/2022] [Indexed: 06/16/2023]
Abstract
Wetlands are critically important to global climate change because of their role in modulating the release of atmospheric greenhouse gases (GHGs) carbon dioxide (CO2 ) and methane (CH4 ). Temperature plays a crucial role in wetland GHG emissions, while the general pattern for seasonal temperature dependencies of wetland CO2 and CH4 emissions is poorly understood. Here we show opposite seasonal temperature dependencies of CO2 and CH4 emissions by using 36,663 daily observations of simultaneous measurements of ecosystem-scale CO2 and CH4 emissions in 42 widely distributed wetlands from the FLUXNET-CH4 database. Specifically, the temperature dependence of CO2 emissions decreased with increasing monthly mean temperature, but the opposite was true for that of CH4 emissions. Neglecting seasonal temperature dependencies may overestimate wetland CO2 and CH4 emissions compared to the use of a year-based static and consistent temperature dependence parameter when only considering temperature effects. Our findings highlight the importance of incorporating the remarkable seasonality in temperature dependence into process-based biogeochemical models to predict feedbacks of wetland GHG emissions to climate warming.
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Affiliation(s)
- Jinquan Li
- Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai, China
| | - Junmin Pei
- Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai, China
| | - Changming Fang
- Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai, China
| | - Bo Li
- Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai, China
- Yunnan Key Laboratory of Plant Reproductive Adaptation and Evolutionary Ecology and Centre for Invasion Biology, Institute of Biodiversity, School of Ecology and Environmental Science, Yunnan University, Kunming, China
| | - Ming Nie
- Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai, China
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40
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Swails EE, Ardón M, Krauss KW, Peralta AL, Emanuel RE, Helton AM, Morse JL, Gutenberg L, Cormier N, Shoch D, Settlemyer S, Soderholm E, Boutin BP, Peoples C, Ward S. Response of soil respiration to changes in soil temperature and water table level in drained and restored peatlands of the southeastern United States. CARBON BALANCE AND MANAGEMENT 2022; 17:18. [PMID: 36401735 PMCID: PMC9675111 DOI: 10.1186/s13021-022-00219-5] [Citation(s) in RCA: 2] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 07/12/2022] [Accepted: 11/11/2022] [Indexed: 06/16/2023]
Abstract
BACKGROUND Extensive drainage of peatlands in the southeastern United States coastal plain for the purposes of agriculture and timber harvesting has led to large releases of soil carbon as carbon dioxide (CO2) due to enhanced peat decomposition. Growth in mechanisms that provide financial incentives for reducing emissions from land use and land-use change could increase funding for hydrological restoration that reduces peat CO2 emissions from these ecosystems. Measuring soil respiration and physical drivers across a range of site characteristics and land use histories is valuable for understanding how CO2 emissions from peat decomposition may respond to raising water table levels. We combined measurements of total soil respiration, depth to water table from soil surface, and soil temperature from drained and restored peatlands at three locations in eastern North Carolina and one location in southeastern Virginia to investigate relationships among total soil respiration and physical drivers, and to develop models relating total soil respiration to parameters that can be easily measured and monitored in the field. RESULTS Total soil respiration increased with deeper water tables and warmer soil temperatures in both drained and hydrologically restored peatlands. Variation in soil respiration was more strongly linked to soil temperature at drained (R2 = 0.57, p < 0.0001) than restored sites (R2 = 0.28, p < 0.0001). CONCLUSIONS The results suggest that drainage amplifies the impact of warming temperatures on peat decomposition. Proxy measurements for estimation of CO2 emissions from peat decomposition represent a considerable cost reduction compared to direct soil flux measurements for land managers contemplating the potential climate impact of restoring drained peatland sites. Research can help to increase understanding of factors influencing variation in soil respiration in addition to physical variables such as depth to water table and soil temperature.
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Affiliation(s)
- E E Swails
- TerraCarbon LLC, Peoria, IL, USA.
- Center for International Forestry Research, Bogor, Indonesia.
| | - M Ardón
- North Carolina State University, Raleigh, NC, USA
| | - K W Krauss
- U.S. Geological Survey, Wetland and Aquatic Research Center, Lafayette, LA, USA
| | - A L Peralta
- East Carolina University, Greenville, NC, USA
| | | | - A M Helton
- University of Connecticut, Storrs, CT, USA
| | - J L Morse
- Portland State University, Portland, OR, USA
| | | | - N Cormier
- U.S. Geological Survey, Wetland and Aquatic Research Center, Lafayette, LA, USA
- School of Natural Sciences, Macquarie University, Sydney, NSW, Australia
| | - D Shoch
- TerraCarbon LLC, Peoria, IL, USA
| | | | - E Soderholm
- The Nature Conservancy, North Carolina Chapter, Durham, NC, USA
| | - B P Boutin
- The Nature Conservancy, North Carolina Chapter, Durham, NC, USA
| | - C Peoples
- The Nature Conservancy, North Carolina Chapter, Durham, NC, USA
| | - S Ward
- United States Fish and Wildlife Service, Raleigh Ecological Services Field Office, Raleigh, NC, USA
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41
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Kwon MJ, Ballantyne A, Ciais P, Qiu C, Salmon E, Raoult N, Guenet B, Göckede M, Euskirchen ES, Nykänen H, Schuur EAG, Turetsky MR, Dieleman CM, Kane ES, Zona D. Lowering water table reduces carbon sink strength and carbon stocks in northern peatlands. GLOBAL CHANGE BIOLOGY 2022; 28:6752-6770. [PMID: 36039832 PMCID: PMC9805217 DOI: 10.1111/gcb.16394] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 04/11/2022] [Accepted: 07/04/2022] [Indexed: 06/15/2023]
Abstract
Peatlands at high latitudes have accumulated >400 Pg carbon (C) because saturated soil and cold temperatures suppress C decomposition. This substantial amount of C in Arctic and Boreal peatlands is potentially subject to increased decomposition if the water table (WT) decreases due to climate change, including permafrost thaw-related drying. Here, we optimize a version of the Organizing Carbon and Hydrology In Dynamic Ecosystems model (ORCHIDEE-PCH4) using site-specific observations to investigate changes in CO2 and CH4 fluxes as well as C stock responses to an experimentally manipulated decrease of WT at six northern peatlands. The unmanipulated control peatlands, with the WT <20 cm on average (seasonal max up to 45 cm) below the surface, currently act as C sinks in most years (58 ± 34 g C m-2 year-1 ; including 6 ± 7 g C-CH4 m-2 year-1 emission). We found, however, that lowering the WT by 10 cm reduced the CO2 sink by 13 ± 15 g C m-2 year-1 and decreased CH4 emission by 4 ± 4 g CH4 m-2 year-1 , thus accumulating less C over 100 years (0.2 ± 0.2 kg C m-2 ). Yet, the reduced emission of CH4 , which has a larger greenhouse warming potential, resulted in a net decrease in greenhouse gas balance by 310 ± 360 g CO2-eq m-2 year-1 . Peatlands with the initial WT close to the soil surface were more vulnerable to C loss: Non-permafrost peatlands lost >2 kg C m-2 over 100 years when WT is lowered by 50 cm, while permafrost peatlands temporally switched from C sinks to sources. These results highlight that reductions in C storage capacity in response to drying of northern peatlands are offset in part by reduced CH4 emissions, thus slightly reducing the positive carbon climate feedbacks of peatlands under a warmer and drier future climate scenario.
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Affiliation(s)
- Min Jung Kwon
- Laboratoire des Sciences du Climat et de l'EnvironnementCEA‐CNRS‐UVSQGif‐sur‐YvetteFrance
- Institute of Soil ScienceUniversity of HamburgHamburgGermany
| | - Ashley Ballantyne
- Laboratoire des Sciences du Climat et de l'EnvironnementCEA‐CNRS‐UVSQGif‐sur‐YvetteFrance
- Department of Ecosystem and Conservation ScienceUniversity of MontanaMissoulaMontanaUSA
| | - Philippe Ciais
- Laboratoire des Sciences du Climat et de l'EnvironnementCEA‐CNRS‐UVSQGif‐sur‐YvetteFrance
| | - Chunjing Qiu
- Laboratoire des Sciences du Climat et de l'EnvironnementCEA‐CNRS‐UVSQGif‐sur‐YvetteFrance
- INRAE, AgroParisTech, Université Paris‐SaclayGif‐sur‐YvetteFrance
| | - Elodie Salmon
- Laboratoire des Sciences du Climat et de l'EnvironnementCEA‐CNRS‐UVSQGif‐sur‐YvetteFrance
| | - Nina Raoult
- Laboratoire des Sciences du Climat et de l'EnvironnementCEA‐CNRS‐UVSQGif‐sur‐YvetteFrance
| | - Bertrand Guenet
- Laboratoire des Sciences du Climat et de l'EnvironnementCEA‐CNRS‐UVSQGif‐sur‐YvetteFrance
- Laboratoire de Géologie, Ecole Normale SupérieureCNRS, PSL Research UniversityParisFrance
| | - Mathias Göckede
- Systems DepartmentMax Planck Institute for BiogeochemistryJenaGermany
| | | | - Hannu Nykänen
- Department of Environmental and Biological SciencesUniversity of Eastern FinlandKuopioFinland
| | - Edward A. G. Schuur
- College of the Environment, Forestry, and Natural SciencesNorthern Arizona UniversityFlagstaffArizonaUSA
| | - Merritt R. Turetsky
- Institute of Arctic and Alpine ResearchUniversity of ColoradoBoulderColoradoUSA
| | | | - Evan S. Kane
- College of Forest Resources and Environmental ScienceMichigan Technological UniversityHoughtonMichiganUSA
- USDA Forest Service Northern Research StationHoughtonMichiganUSA
| | - Donatella Zona
- Department of Animal and Plant ScienceUniversity of SheffieldSheffieldUK
- Department of BiologySan Diego State UniversitySan DiegoCaliforniaUSA
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42
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Li T, Canadell JG, Yang XQ, Zhai P, Chao Q, Lu Y, Huang D, Sun W, Qin Z. Methane Emissions from Wetlands in China and Their Climate Feedbacks in the 21st Century. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2022; 56:12024-12035. [PMID: 35943239 DOI: 10.1021/acs.est.2c01575] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/15/2023]
Abstract
Wetlands are large sinks of carbon dioxide (CO2) and sources of methane (CH4). Both fluxes can be altered by wetland management (e.g., restoration), leading to changes in the climate system. Here, we use multiple models to assess CH4 emissions and CO2 sequestration from the wetlands in China and the impacts on climate under three climate scenarios and four wetland management scenarios with various levels of wetland restoration in the 21st century. We find that wetland restoration leads to increased CH4 emissions with a national total of 0.32-11.31 Tg yr-1. These emissions induce an additional radiative forcing of 0.0005-0.0075 W m-2 yr-1 and global annual mean air temperature rise of 0.0003-0.0053 °C yr-1, across all future climate and management scenarios. However, wetland restoration also resulted in net CO2 sequestration, leading to a combined net greenhouse gas sink in all climate management scenarios, except in the highest restoration level combined with the hottest climate scenario. The highest climate cooling was achieved under medium restoration, with the climate scenario consistent with the Paris agreement target of below 2 °C, with a cumulative global warming potential of -3.2 Pg CO2-eq (2020-2100). Wetland restoration in the Qinghai-Tibet Plateau offers the greatest cooling effect.
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Affiliation(s)
- Tingting Li
- LAPC, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
- Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519000, China
| | - Josep G Canadell
- Global Carbon Project, CSIRO Oceans and Atmosphere, Canberra, ACT 2601, Australia
| | - Xiu-Qun Yang
- Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519000, China
- School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
| | - Panmao Zhai
- Chinese Academy of Meteorological Sciences, Beijing 100081, China
| | - Qingchen Chao
- Beijing Climate Center, China Meteorological Administration, Beijing 100081, China
| | - Yanyu Lu
- Anhui Institute of Meteorological Sciences, Key Laboratory of Atmospheric Sciences and Remote Sensing of Anhui Province, Hefei 230031, China
| | - Danqing Huang
- School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
| | - Wenjuan Sun
- Institute of Botany, Chinese Academy of Sciences, Beijing 100049, China
| | - Zhangcai Qin
- Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519000, China
- School of Atmospheric Sciences, Sun Yat-sen University, Guangzhou 510245, China
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43
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Dong F, Li Y, Qin C, Zhang X, Chen Y, Zhao X, Wang C. Information infrastructure and greenhouse gas emission performance in urban China: A difference-in-differences analysis. JOURNAL OF ENVIRONMENTAL MANAGEMENT 2022; 316:115252. [PMID: 35594820 DOI: 10.1016/j.jenvman.2022.115252] [Citation(s) in RCA: 4] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/09/2022] [Revised: 04/17/2022] [Accepted: 05/05/2022] [Indexed: 06/15/2023]
Abstract
Owing to its network spillover effect, information infrastructure performs outstandingly in promoting economic growth and technological innovation, and has received widespread attention. However, the ecological performance of information infrastructure, especially its impact on greenhouse gas (GHG) emission performance, has been less studied. To investigate this issue, using panel data for 281 prefecture-level cities in China from 2003 to 2018, we treat the Broadband China policy as a quasi-natural experiment in information infrastructure, and conduct a difference-in-differences (DID) analysis. The results show that: (1) Information infrastructure significantly improves urban GHG emission performance. This conclusion holds even after controlling for pilot selection endogeneity, sampling bias, and other policy interference. (2) Technological innovation, industrial structure upgrading, factor allocation enhancement, and tertiary agglomeration are effective channels for information infrastructure to improve GHG emission performance. (3) The treatment effect varies with city size, digital economy level, and economic status. Specifically, information infrastructure exhibits significant emission reduction performance in cities with large size, advanced digital economy, and leading economic status, while the emission reduction effect drops in other cities. This study provides insights into the transition to a carbon-neutral manner for infrastructure in China and other developing countries.
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Affiliation(s)
- Feng Dong
- School of Economics and Management, China University of Mining and Technology, Xuzhou, 221116, PR China.
| | - Yangfan Li
- School of Economics and Management, China University of Mining and Technology, Xuzhou, 221116, PR China
| | - Chang Qin
- School of Economics and Management, China University of Mining and Technology, Xuzhou, 221116, PR China
| | - Xiaoyun Zhang
- School of Economics and Management, China University of Mining and Technology, Xuzhou, 221116, PR China
| | - Yuhuan Chen
- School of Economics and Management, China University of Mining and Technology, Xuzhou, 221116, PR China
| | - Xu Zhao
- School of Economics and Management, China University of Mining and Technology, Xuzhou, 221116, PR China
| | - Chao Wang
- School of Public Policy and Management (School of Emergency Management), China University of Mining and Technology, Xuzhou, Jiangsu, 221116, PR China.
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44
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Freeman BWJ, Evans CD, Musarika S, Morrison R, Newman TR, Page SE, Wiggs GFS, Bell NGA, Styles D, Wen Y, Chadwick DR, Jones DL. Responsible agriculture must adapt to the wetland character of mid-latitude peatlands. GLOBAL CHANGE BIOLOGY 2022; 28:3795-3811. [PMID: 35243734 PMCID: PMC9314663 DOI: 10.1111/gcb.16152] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 12/21/2021] [Accepted: 01/31/2022] [Indexed: 06/14/2023]
Abstract
Drained, lowland agricultural peatlands are greenhouse gas (GHG) emission hotspots and a large but vulnerable store of irrecoverable carbon. They exhibit soil loss rates of ~2.0 cm yr-1 and are estimated to account for 32% of global cropland emissions while producing only 1.1% of crop kilocalories. Carbon dioxide emissions account for >80% of their terrestrial GHG emissions and are largely controlled by water table depth. Reducing drainage depths is, therefore, essential for responsible peatland management. Peatland restoration can substantially reduce emissions. However, this may conflict with societal needs to maintain productive use, to protect food security and livelihoods. Wetland agriculture strategies will, therefore, be required to adapt agriculture to the wetland character of peatlands, and balance GHG mitigation against productivity, where halting emissions is not immediately possible. Paludiculture may substantially reduce GHG emissions but will not always be viable in the current economic landscape. Reduced drainage intensity systems may deliver partial reductions in the rate of emissions, with smaller modifications to existing systems. These compromise systems may face fewer hurdles to adoption and minimize environmental harm until societal conditions favour strategies that can halt emissions. Wetland agriculture will face agronomic, socio-economic and water management challenges, and careful implementation will be required. Diversity of values and priorities among stakeholders creates the potential for conflict. Successful implementation will require participatory research approaches and co-creation of workable solutions. Policymakers, private sector funders and researchers have key roles to play but adoption risks would fall predominantly on land managers. Development of a robust wetland agriculture paradigm is essential to deliver resilient production systems and wider environmental benefits. The challenge of responsible use presents an opportunity to rethink peatland management and create thriving, innovative and green wetland landscapes for everyone's future benefit, while making a vital contribution to global climate change mitigation.
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Affiliation(s)
| | | | | | - Ross Morrison
- UK Centre for Ecology and HydrologyWallingfordOxfordshireUK
| | - Thomas R. Newman
- School of Geography, Geology and the EnvironmentUniversity of LeicesterLeicesterLeicestershireUK
| | - Susan E. Page
- School of Geography, Geology and the EnvironmentUniversity of LeicesterLeicesterLeicestershireUK
| | - Giles F. S. Wiggs
- School of Geography and the EnvironmentUniversity of OxfordOxfordOxfordshireUK
| | | | - David Styles
- Ryan InstituteNational University of Ireland GalwayGalwayIreland
| | - Yuan Wen
- School of Natural SciencesBangor UniversityBangorGwyneddUK
- College of Agronomy and BiotechnologyChina Agricultural UniversityBeijingChina
| | | | - Davey L. Jones
- School of Natural SciencesBangor UniversityBangorGwyneddUK
- SoilsWestCentre for Sustainable Farming SystemsFood Futures InstituteMurdoch UniversityMurdochWestern AustraliaAustralia
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45
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Temmink RJM, Lamers LPM, Angelini C, Bouma TJ, Fritz C, van de Koppel J, Lexmond R, Rietkerk M, Silliman BR, Joosten H, van der Heide T. Recovering wetland biogeomorphic feedbacks to restore the world's biotic carbon hotspots. Science 2022; 376:eabn1479. [PMID: 35511964 DOI: 10.1126/science.abn1479] [Citation(s) in RCA: 37] [Impact Index Per Article: 18.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/02/2022]
Abstract
Biogeomorphic wetlands cover 1% of Earth's surface but store 20% of ecosystem organic carbon. This disproportional share is fueled by high carbon sequestration rates and effective storage in peatlands, mangroves, salt marshes, and seagrass meadows, which greatly exceed those of oceanic and forest ecosystems. Here, we review how feedbacks between geomorphology and landscape-building vegetation underlie these qualities and how feedback disruption can switch wetlands from carbon sinks into sources. Currently, human activities are driving rapid declines in the area of major carbon-storing wetlands (1% annually). Our findings highlight the urgency to stop through conservation ongoing losses and to reestablish landscape-forming feedbacks through restoration innovations that recover the role of biogeomorphic wetlands as the world's biotic carbon hotspots.
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Affiliation(s)
- Ralph J M Temmink
- Environmental Sciences, Copernicus Institute of Sustainable Development, Utrecht University, Princetonlaan 8a, 3584 CB, Utrecht, Netherlands.,Department of Coastal Systems, Royal Netherlands Institute for Sea Research, 1790 AB Den Burg, Netherlands.,Aquatic Ecology and Environmental Biology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ Nijmegen, Netherlands
| | - Leon P M Lamers
- Aquatic Ecology and Environmental Biology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ Nijmegen, Netherlands.,B-WARE Research Centre, Toernooiveld 1, 6525 ED Nijmegen, Netherlands
| | - Christine Angelini
- Department of Environmental Engineering Sciences, Engineering School for Sustainable Infrastructure and Environment, University of Florida, Post Office Box 116580, Gainesville, FL 32611, USA
| | - Tjeerd J Bouma
- Department of Estuarine and Delta Systems, Royal Netherlands Institute for Sea Research, 4401 NT Yerseke, Netherlands.,Conservation Ecology Group, Groningen Institute for Evolutionary Life Sciences, University of Groningen, 9700 CC Groningen, Netherlands.,Building with Nature group, HZ University of Applied Sciences, Postbus 364, 4380 AJ Vlissingen, Netherlands.,Faculty of Geosciences, Department of Physical Geography, Utrecht University, 3508 TC Utrecht, Netherlands
| | - Christian Fritz
- Aquatic Ecology and Environmental Biology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ Nijmegen, Netherlands.,Integrated Research on Energy, Environment and Society (IREES), University of Groningen, Nijenborgh 6, Groningen, 9747 AG, Netherlands
| | - Johan van de Koppel
- Department of Estuarine and Delta Systems, Royal Netherlands Institute for Sea Research, 4401 NT Yerseke, Netherlands.,Conservation Ecology Group, Groningen Institute for Evolutionary Life Sciences, University of Groningen, 9700 CC Groningen, Netherlands
| | - Robin Lexmond
- Experimental Plant Ecology, Radboud Institute for Biological and Environmental Sciences, Radboud University, Heyendaalseweg 135, 6525 AJ Nijmegen, Netherlands
| | - Max Rietkerk
- Environmental Sciences, Copernicus Institute of Sustainable Development, Utrecht University, Princetonlaan 8a, 3584 CB, Utrecht, Netherlands
| | - Brian R Silliman
- Division of Marine Science and Conservation, Nicholas School of the Environment, Duke University, 135 Duke Marine Lab Road, Beaufort, NC, USA
| | - Hans Joosten
- Institute of Botany and Landscape Ecology, Greifswald University, Partner in the Greifswald Mire Centre, Soldmannstrasse 15, 17487 Greifswald, Germany
| | - Tjisse van der Heide
- Department of Coastal Systems, Royal Netherlands Institute for Sea Research, 1790 AB Den Burg, Netherlands.,Conservation Ecology Group, Groningen Institute for Evolutionary Life Sciences, University of Groningen, 9700 CC Groningen, Netherlands
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46
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Rewetting Tropical Peatlands Reduced Net Greenhouse Gas Emissions in Riau Province, Indonesia. FORESTS 2022. [DOI: 10.3390/f13040505] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/16/2022]
Abstract
Draining deforested tropical peat swamp forests (PSFs) converts greenhouse gas (GHG) sinks to sources and increases the likelihood of fire hazards. Rewetting deforested and drained PSFs before revegetation is expected to reverse this outcome. This study aims to quantify the GHG emissions of deforested PSFs that have been (a) reforested, (b) converted into oil palm, or (c) replanted with rubber. Before rewetting, heterotrophic soil respiration in reforested, oil palm, and rubber plantation areas were 48.91 ± 4.75 Mg CO2 ha−1 yr−1, 54.98 ± 1.53 Mg CO2 ha−1 yr−1, and 67.67 ± 2.13 Mg CO2 ha−1 yr−1, respectively. After rewetting, this decreased substantially by 21%, 36%, and 39%. Conversely, rewetting drained landscapes that used to be methane (CH4) sinks converted them into CH4 sources; almost twice as much methane was emitted after rewetting. Nitrous oxide (N2O) emissions tended to decrease; in nitrogen-rich rubber plantations, N2O emissions halved; in nitrogen-poor reforested areas, emissions reduced by up to a quarter after rewetting. Overall, rewetting reduced the net emissions up to 15.41 Mg CO2-eq ha−1 yr−1 (25%) in reforested, 18.36 Mg CO2-eq ha−1 yr−1 (18%) in oil palm, and 28.87 Mg CO2-eq ha−1 yr−1 (17%) in rubber plantation areas.
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47
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Apers S, De Lannoy GJM, Baird AJ, Cobb AR, Dargie GC, del Aguila Pasquel J, Gruber A, Hastie A, Hidayat H, Hirano T, Hoyt AM, Jovani‐Sancho AJ, Katimon A, Kurnain A, Koster RD, Lampela M, Mahanama SPP, Melling L, Page SE, Reichle RH, Taufik M, Vanderborght J, Bechtold M. Tropical Peatland Hydrology Simulated With a Global Land Surface Model. JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS 2022; 14:e2021MS002784. [PMID: 35860446 PMCID: PMC9285420 DOI: 10.1029/2021ms002784] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/18/2021] [Revised: 01/15/2022] [Accepted: 02/02/2022] [Indexed: 05/22/2023]
Abstract
Tropical peatlands are among the most carbon-dense ecosystems on Earth, and their water storage dynamics strongly control these carbon stocks. The hydrological functioning of tropical peatlands differs from that of northern peatlands, which has not yet been accounted for in global land surface models (LSMs). Here, we integrated tropical peat-specific hydrology modules into a global LSM for the first time, by utilizing the peatland-specific model structure adaptation (PEATCLSM) of the NASA Catchment Land Surface Model (CLSM). We developed literature-based parameter sets for natural (PEATCLSMTrop,Nat) and drained (PEATCLSMTrop,Drain) tropical peatlands. Simulations with PEATCLSMTrop,Nat were compared against those with the default CLSM version and the northern version of PEATCLSM (PEATCLSMNorth,Nat) with tropical vegetation input. All simulations were forced with global meteorological reanalysis input data for the major tropical peatland regions in Central and South America, the Congo Basin, and Southeast Asia. The evaluation against a unique and extensive data set of in situ water level and eddy covariance-derived evapotranspiration showed an overall improvement in bias and correlation compared to the default CLSM version. Over Southeast Asia, an additional simulation with PEATCLSMTrop,Drain was run to address the large fraction of drained tropical peatlands in this region. PEATCLSMTrop,Drain outperformed CLSM, PEATCLSMNorth,Nat, and PEATCLSMTrop,Nat over drained sites. Despite the overall improvements of PEATCLSMTrop,Nat over CLSM, there are strong differences in performance between the three study regions. We attribute these performance differences to regional differences in accuracy of meteorological forcing data, and differences in peatland hydrologic response that are not yet captured by our model.
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Affiliation(s)
- S. Apers
- Department of Earth and Environmental SciencesKU LeuvenHeverleeBelgium
| | | | - A. J. Baird
- School of GeographyUniversity of LeedsLeedsUK
| | - A. R. Cobb
- Center for Environmental Sensing and ModelingSingapore‐MIT Alliance for Research and TechnologySingaporeSingapore
| | | | - J. del Aguila Pasquel
- Instituto de Investigaciones de la Amazonia Peruana (IIAP)IquitosPeru
- Universidad Nacional de la Amazonia Peruana (UNAP)IquitosPeru
| | - A. Gruber
- Department of Earth and Environmental SciencesKU LeuvenHeverleeBelgium
| | - A. Hastie
- School of GeoSciencesUniversity of EdinburghEdinburghUK
| | - H. Hidayat
- Research Center for LimnologyNational Research and Innovation AgencyCibinongIndonesia
| | - T. Hirano
- Research Faculty of AgricultureHokkaido UniversitySapporoJapan
| | - A. M. Hoyt
- Department of Earth System ScienceStanford UniversityStanfordCAUSA
| | - A. J. Jovani‐Sancho
- UK Centre for Ecology and HydrologyBangorUK
- School of BiosciencesUniversity of NottinghamLoughboroughUK
| | - A. Katimon
- Faculty of Chemical Engineering TechnologyUniversiti Malaysia PerlisKangarMalaysia
| | - A. Kurnain
- Department of Soil ScienceLambung Mangkurat UniversityBanjarmasinIndonesia
| | - R. D. Koster
- Global Modeling and Assimilation OfficeNASA Goddard Space Flight CenterGreenbeltMDUSA
| | - M. Lampela
- Department of Forest SciencesUniversity of HelsinkiHelsinkiFinland
| | - S. P. P. Mahanama
- Global Modeling and Assimilation OfficeNASA Goddard Space Flight CenterGreenbeltMDUSA
- Science Systems and Applications Inc.LanhamMDUSA
| | - L. Melling
- Sarawak Tropical Peat Research InstituteKuchingMalaysia
| | - S. E. Page
- School of Geography, Geology and the EnvironmentUniversity of LeicesterLeicesterUK
| | - R. H. Reichle
- Global Modeling and Assimilation OfficeNASA Goddard Space Flight CenterGreenbeltMDUSA
| | - M. Taufik
- Department of Geophysics and MeteorologyIPB UniversityBogorIndonesia
| | - J. Vanderborght
- Department of Earth and Environmental SciencesKU LeuvenHeverleeBelgium
- Agrosphere InstituteIBG‐3Forschungszentrum JülichJülichGermany
| | - M. Bechtold
- Department of Earth and Environmental SciencesKU LeuvenHeverleeBelgium
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48
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Purola T, Lehtonen H. Farm-Level Effects of Emissions Tax and Adjustable Drainage on Peatlands. ENVIRONMENTAL MANAGEMENT 2022; 69:154-168. [PMID: 34648068 PMCID: PMC8758597 DOI: 10.1007/s00267-021-01543-1] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 06/17/2021] [Accepted: 09/20/2021] [Indexed: 06/13/2023]
Abstract
Drained agricultural peatlands emit significantly higher amounts of greenhouse gas (GHG) emissions per hectare than mineral soils. GHG abatement costs for representative cereals (CF) and dairy (DF) farms in southwestern Finland were estimated by integrating an emission-based tax together with an option to invest in a subsidized adjustable drainage system on peat soils in a farm-level dynamic optimization model. With an average 10% share of peat soils from overall farm area, emissions tax rates over 15 (CF) and 19 (DF) €/tCO2e triggered adjustable drainage investments with a significant reduction in GHG emissions per ha, when assuming no crop-yield effect from the adjustable drainage. Abatement costs for emissions tax rates €12-50/tCO2e/ha were €16-44/tCO2e (CF) and €26-51/tCO2e (DF) for whole farm-soil emissions, depending on the share of peatlands on the farm, on the yield effects of adjustable drainage, and on crop prices. High emissions tax rates imply higher abatement costs since farms have a limited capability to adjust their production and land use. Thus, emissions reductions from peatlands can be achieved at reasonable costs when investing in adjustable drainage on peatlands. The income losses due to emissions tax, however, are high, but they can be compensated for farmers by lumpsum payments independent of their production decisions. Since existing agricultural policies such as the EU CAP system may have limited effectiveness on GHG emissions, the emissions tax and adjustable drainage on peatlands could promote GHG abatement significantly on farms and areas with abundant peatlands.
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Affiliation(s)
- Tuomo Purola
- Luke Natural Resources Institute Finland - Economics and society, Latokartanonkaari 9, FI-00790, Helsinki, Finland.
| | - Heikki Lehtonen
- Luke Natural Resources Institute Finland - Economics and society, Latokartanonkaari 9, FI-00790, Helsinki, Finland
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