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Symochko L, Demyanyuk O, Crisan V, Dinca L. Microbial transformation of soil organic matter under varying agricultural management systems in Ukraine. Front Microbiol 2024; 14:1287701. [PMID: 38274742 PMCID: PMC10808755 DOI: 10.3389/fmicb.2023.1287701] [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: 09/02/2023] [Accepted: 12/19/2023] [Indexed: 01/27/2024] Open
Abstract
Introduction This paper presents comparative studies on the content and structure of organic matter (OM) and the activity of microbiological cellulose destruction in three types of Ukrainian soils intensively used in agricultural production. Methods The highest content of humus in the arable layer (4.9%), OM (410 t ha-1), and total carbon (30.9 mg C g-1 soil) was determined in chernic phaeozems, which is 2.2-2.5 times higher than in albic retisols. The soil of natural ecosystems is characterised by a high content of microbial carbon (Cmic) in the carbon fraction of organic soil compounds. Results and discussion In arable soils, the content and reserves of humus and soil organic matter (SOM) have decreased by an average of 1.5-2 times. The most considerable loss of humus reserves in the soil profile was identified in albic retisols (1.96-1.44 times) and the smallest in chernic phaeozems (1.27-1.81 times). During the long-term systematic application of mineral fertilisers, the Corg content decreased by 8-21% in chernic phaeozems, 12-33% in greyzemic phaeozems, and 6-38% in albic retisols. A significant difference of 2.1-8.0 times was determined regarding the number of aerobic cellulolytic microorganisms and 1.3-3.3 times in the potential cellulolytic activity of the studied soils. The high number of cellulose-destroying microorganisms is characteristic of chernic phaeozems with a high content of OM in the soil; the advantage over other types of studied soils was 1.4 times and 7.8 times for greyzemic phaeozems and albic retisols, respectively. Among the studied soil types, high values of CO2 emissions were identified in chernic phaeozems. Intensive agricultural practices in Ukrainian soils have significantly altered the content and composition of organic matter, leading to reduced humus and soil organic matter reserves. The study also underscores the importance of considering the abundance of cellulose-destroying microorganisms and their potential activity in assessing soil health and sustainability.
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Affiliation(s)
- Lyudmyla Symochko
- Faculty of Biology, Uzhhorod National University, Uzhhorod, Ukraine
- Department of Life Sciences, Faculty of Science and Technology, University of Coimbra, Coimbra, Portugal
- Institute of Agroecology and Environmental Management, Kyiv, Ukraine
| | - Olena Demyanyuk
- Institute of Agroecology and Environmental Management, Kyiv, Ukraine
| | - Vlad Crisan
- Romanian National Institute of Research and Development in Forestry “Marin Dracea” Brasov branch, Braşov, Romania
| | - Lucian Dinca
- Romanian National Institute of Research and Development in Forestry “Marin Dracea” Brasov branch, Braşov, Romania
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2
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Ringeval B, Demay J, Goll DS, He X, Wang YP, Hou E, Matej S, Erb KH, Wang R, Augusto L, Lun F, Nesme T, Borrelli P, Helfenstein J, McDowell RW, Pletnyakov P, Pellerin S. A global dataset on phosphorus in agricultural soils. Sci Data 2024; 11:17. [PMID: 38167392 PMCID: PMC10762041 DOI: 10.1038/s41597-023-02751-6] [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: 02/13/2023] [Accepted: 11/14/2023] [Indexed: 01/05/2024] Open
Abstract
Numerous drivers such as farming practices, erosion, land-use change, and soil biogeochemical background, determine the global spatial distribution of phosphorus (P) in agricultural soils. Here, we revised an approach published earlier (called here GPASOIL-v0), in which several global datasets describing these drivers were combined with a process model for soil P dynamics to reconstruct the past and current distribution of P in cropland and grassland soils. The objective of the present update, called GPASOIL-v1, is to incorporate recent advances in process understanding about soil inorganic P dynamics, in datasets to describe the different drivers, and in regional soil P measurements for benchmarking. We trace the impact of the update on the reconstructed soil P. After the update we estimate a global averaged inorganic labile P of 187 kgP ha-1 for cropland and 91 kgP ha-1 for grassland in 2018 for the top 0-0.3 m soil layer, but these values are sensitive to the mineralization rates chosen for the organic P pools. Uncertainty in the driver estimates lead to coefficients of variation of 0.22 and 0.54 for cropland and grassland, respectively. This work makes the methods for simulating the agricultural soil P maps more transparent and reproducible than previous estimates, and increases the confidence in the new estimates, while the evaluation against regional dataset still suggests rooms for further improvement.
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Affiliation(s)
- Bruno Ringeval
- ISPA, Bordeaux Sciences Agro, INRAE, 33140, Villenave d'Ornon, France.
| | - Josephine Demay
- ISPA, Bordeaux Sciences Agro, INRAE, 33140, Villenave d'Ornon, France
| | - Daniel S Goll
- Université Paris Saclay, CEA-CNRS-UVSQ, LSCE/IPSL, Gif-sur-Yvette, France
| | - Xianjin He
- Université Paris Saclay, CEA-CNRS-UVSQ, LSCE/IPSL, Gif-sur-Yvette, France
| | | | - Enqing Hou
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
| | - Sarah Matej
- Institute of Social Ecology, University of Natural Resources and Life Sciences, Vienna, Austria
| | - Karl-Heinz Erb
- Institute of Social Ecology, University of Natural Resources and Life Sciences, Vienna, Austria
| | - Rong Wang
- Department of Environmental Science and Engineering, Fudan University, Shanghai, 200438, China
| | - Laurent Augusto
- ISPA, Bordeaux Sciences Agro, INRAE, 33140, Villenave d'Ornon, France
| | - Fei Lun
- College of Land Science and Technology, China Agricultural University, Beijing, 100193, China
| | - Thomas Nesme
- ISPA, Bordeaux Sciences Agro, INRAE, 33140, Villenave d'Ornon, France
| | - Pasquale Borrelli
- Department of Science, Roma Tre University, 00146, Rome, Italy
- Department of Biological Environment, Kangwon National University, Chuncheon, 24341, Republic of Korea
| | - Julian Helfenstein
- Soil Geography and Landscape Group, University of Wageningen, Wageningen, 6700AA, The Netherlands
| | - Richard W McDowell
- AgResearch, Lincoln Science Centre, Private Bag 4749, Christchurch, 8140, New Zealand
- Faculty of Agriculture and Life Sciences, Lincoln University, Lincoln, PO Box 84, 7647, Christchurch, New Zealand
| | - Peter Pletnyakov
- Faculty of Agriculture and Life Sciences, Lincoln University, Lincoln, PO Box 84, 7647, Christchurch, New Zealand
| | - Sylvain Pellerin
- ISPA, Bordeaux Sciences Agro, INRAE, 33140, Villenave d'Ornon, France
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3
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Goll DS, Bauters M, Zhang H, Ciais P, Balkanski Y, Wang R, Verbeeck H. Atmospheric phosphorus deposition amplifies carbon sinks in simulations of a tropical forest in Central Africa. THE NEW PHYTOLOGIST 2023; 237:2054-2068. [PMID: 36226674 DOI: 10.1111/nph.18535] [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: 01/03/2022] [Accepted: 09/18/2022] [Indexed: 06/16/2023]
Abstract
Spatial redistribution of nutrients by atmospheric transport and deposition could theoretically act as a continental-scale mechanism which counteracts declines in soil fertility caused by nutrient lock-up in accumulating biomass in tropical forests in Central Africa. However, to what extent it affects carbon sinks in forests remains elusive. Here we use a terrestrial biosphere model to quantify the impact of changes in atmospheric nitrogen and phosphorus deposition on plant nutrition and biomass carbon sink at a typical lowland forest site in Central Africa. We find that the increase in nutrient deposition since the 1980s could have contributed to the carbon sink over the past four decades up to an extent which is similar to that from the combined effects of increasing atmospheric carbon dioxide and climate change. Furthermore, we find that the modelled carbon sink responds to changes in phosphorus deposition, but less so to nitrogen deposition. The pronounced response of ecosystem productivity to changes in nutrient deposition illustrates a potential mechanism that could control carbon sinks in Central Africa. Monitoring the quantity and quality of nutrient deposition is needed in this region, given the changes in nutrient deposition due to human land use.
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Affiliation(s)
- Daniel S Goll
- Laboratoire des Sciences du Climat et de l'Environnement, Commissariat à l'Énergie Atomique et aux Énergies Alternatives, CNRS, Université de Versailles Saint-Quentin, Université Paris Saclay, Gif-sur-Yvette, 91190, France
| | - Marijn Bauters
- Isotope Bioscience Laboratory-ISOFYS, Ghent University, Ghent, 9000, Belgium
- Department of Environment, Computational and Applied Vegetation Ecology - CAVElab, Ghent University, Ghent, 9000, Belgium
| | - Haicheng Zhang
- Department Geoscience, Environment & Society, Université Libre de Bruxelles, Bruxelles, 1050, Belgium
| | - Philippe Ciais
- Laboratoire des Sciences du Climat et de l'Environnement, Commissariat à l'Énergie Atomique et aux Énergies Alternatives, CNRS, Université de Versailles Saint-Quentin, Université Paris Saclay, Gif-sur-Yvette, 91190, France
| | - Yves Balkanski
- Laboratoire des Sciences du Climat et de l'Environnement, Commissariat à l'Énergie Atomique et aux Énergies Alternatives, CNRS, Université de Versailles Saint-Quentin, Université Paris Saclay, Gif-sur-Yvette, 91190, France
| | - Rong Wang
- Department of Environmental Science and Engineering, Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention, Fudan University, Shanghai, 200438, China
- Integrated Research on Disaster Risk International Center of Excellence on Risk Interconnectivity and Governance on Weather/Climate Extremes Impact and Public Health, Fudan University, Shanghai, 200438, China
- Department of Atmospheric and Oceanic Sciences, Institute of Atmospheric Sciences, Fudan University, Shanghai, 200438, China
- Center for Urban Eco-Planning & Design, Fudan University, Shanghai, 200438, China
- Big Data Institute for Carbon Emission and Environmental Pollution, Fudan University, Shanghai, 200438, China
- Shanghai Institute of Pollution Control and Ecological Security, Shanghai, 200092, China
| | - Hans Verbeeck
- Department of Environment, Computational and Applied Vegetation Ecology - CAVElab, Ghent University, Ghent, 9000, Belgium
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4
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Cunha HFV, Andersen KM, Lugli LF, Santana FD, Aleixo IF, Moraes AM, Garcia S, Di Ponzio R, Mendoza EO, Brum B, Rosa JS, Cordeiro AL, Portela BTT, Ribeiro G, Coelho SD, de Souza ST, Silva LS, Antonieto F, Pires M, Salomão AC, Miron AC, de Assis RL, Domingues TF, Aragão LEOC, Meir P, Camargo JL, Manzi AO, Nagy L, Mercado LM, Hartley IP, Quesada CA. Direct evidence for phosphorus limitation on Amazon forest productivity. Nature 2022; 608:558-562. [PMID: 35948632 DOI: 10.1038/s41586-022-05085-2] [Citation(s) in RCA: 30] [Impact Index Per Article: 15.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/29/2021] [Accepted: 07/07/2022] [Indexed: 11/09/2022]
Abstract
The productivity of rainforests growing on highly weathered tropical soils is expected to be limited by phosphorus availability1. Yet, controlled fertilization experiments have been unable to demonstrate a dominant role for phosphorus in controlling tropical forest net primary productivity. Recent syntheses have demonstrated that responses to nitrogen addition are as large as to phosphorus2, and adaptations to low phosphorus availability appear to enable net primary productivity to be maintained across major soil phosphorus gradients3. Thus, the extent to which phosphorus availability limits tropical forest productivity is highly uncertain. The majority of the Amazonia, however, is characterized by soils that are more depleted in phosphorus than those in which most tropical fertilization experiments have taken place2. Thus, we established a phosphorus, nitrogen and base cation addition experiment in an old growth Amazon rainforest, with a low soil phosphorus content that is representative of approximately 60% of the Amazon basin. Here we show that net primary productivity increased exclusively with phosphorus addition. After 2 years, strong responses were observed in fine root (+29%) and canopy productivity (+19%), but not stem growth. The direct evidence of phosphorus limitation of net primary productivity suggests that phosphorus availability may restrict Amazon forest responses to CO2 fertilization4, with major implications for future carbon sequestration and forest resilience to climate change.
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Affiliation(s)
| | - Kelly M Andersen
- Asian School of the Environment, Nanyang Technological University, Singapore, Singapore.,Geography, College of Life and Environmental Sciences, University of Exeter, Exeter, UK
| | - Laynara Figueiredo Lugli
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil.,TUM School of Life Sciences, Technical University of Munich, Freising, Germany
| | - Flavia Delgado Santana
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil
| | - Izabela Fonseca Aleixo
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil
| | - Anna Martins Moraes
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil
| | - Sabrina Garcia
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil
| | - Raffaello Di Ponzio
- Biological Dynamics of Forest Fragment Project, National Institute for Amazonian Research, Manaus, Brazil
| | - Erick Oblitas Mendoza
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil
| | - Bárbara Brum
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil
| | - Jéssica Schmeisk Rosa
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil
| | | | | | - Gyovanni Ribeiro
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil
| | - Sara Deambrozi Coelho
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil
| | | | - Lara Siebert Silva
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil
| | - Felipe Antonieto
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil
| | - Maria Pires
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil
| | - Ana Cláudia Salomão
- Biological Dynamics of Forest Fragment Project, National Institute for Amazonian Research, Manaus, Brazil
| | - Ana Caroline Miron
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil.,Department of Biology, University of Hamburg, Hamburg, Germany
| | - Rafael L de Assis
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil.,Natural History Museum, University of Oslo, Oslo, Norway
| | - Tomas F Domingues
- Faculdade de Filosofia, Ciência e Letras de Ribeirão Preto, Universidade de São Paulo, São Paulo, Brazil
| | - Luiz E O C Aragão
- Geography, College of Life and Environmental Sciences, University of Exeter, Exeter, UK.,National Institute for Space Research, São Jose dos Campos, São Paulo, Brazil
| | - Patrick Meir
- School of Geosciences, University of Edinburgh, Edinburgh, UK.,Research School of Biology, Australian National University, Canberra, Australian Capital Territory, Australia
| | - José Luis Camargo
- Biological Dynamics of Forest Fragment Project, National Institute for Amazonian Research, Manaus, Brazil
| | - Antonio Ocimar Manzi
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil.,National Institute for Space Research, São Jose dos Campos, São Paulo, Brazil
| | | | - Lina M Mercado
- Geography, College of Life and Environmental Sciences, University of Exeter, Exeter, UK.,UK Centre for Ecology and Hydrology, Wallingford, UK
| | - Iain P Hartley
- Geography, College of Life and Environmental Sciences, University of Exeter, Exeter, UK
| | - Carlos Alberto Quesada
- Coordination of Environmental Dynamics, National Institute for Amazonian Research, Manaus, Brazil
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5
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Braghiere RK, Fisher JB, Allen K, Brzostek E, Shi M, Yang X, Ricciuto DM, Fisher RA, Zhu Q, Phillips RP. Modeling Global Carbon Costs of Plant Nitrogen and Phosphorus Acquisition. JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS 2022; 14:e2022MS003204. [PMID: 36245670 PMCID: PMC9539603 DOI: 10.1029/2022ms003204] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 05/18/2022] [Revised: 08/02/2022] [Accepted: 08/06/2022] [Indexed: 06/16/2023]
Abstract
Most Earth system models (ESMs) do not explicitly represent the carbon (C) costs of plant nutrient acquisition, which leads to uncertainty in predictions of the current and future constraints to the land C sink. We integrate a plant productivity-optimizing nitrogen (N) and phosphorus (P) acquisition model (fixation & uptake of nutrients, FUN) into the energy exascale Earth system (E3SM) land model (ELM). Global plant N and P uptake are dynamically simulated by ELM-FUN based on the C costs of nutrient acquisition from mycorrhizae, direct root uptake, retranslocation from senescing leaves, and biological N fixation. We benchmarked ELM-FUN with three classes of products: ILAMB, a remotely sensed nutrient limitation product, and CMIP6 models; we found significant improvements in C cycle variables, although the lack of more observed nutrient data prevents a comprehensive level of benchmarking. Overall, we found N and P co-limitation for 80% of land area, with the remaining 20% being either predominantly N or P limited. Globally, the new model predicts that plants invested 4.1 Pg C yr-1 to acquire 841.8 Tg N yr-1 and 48.1 Tg P yr-1 (1994-2005), leading to significant downregulation of global net primary production (NPP). Global NPP is reduced by 20% with C costs of N and 50% with C costs of NP. Modeled and observed nutrient limitation agreement increases when N and P are considered together (r 2 from 0.73 to 0.83).
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Affiliation(s)
- R. K. Braghiere
- Jet Propulsion LaboratoryCalifornia Institute of TechnologyPasadenaCAUSA
- Joint Institute for Regional Earth System Science and EngineeringUniversity of California Los AngelesLos AngelesCAUSA
- Division of Geological and Planetary SciencesCalifornia Institute of TechnologyPasadenaCAUSA
| | - J. B. Fisher
- Schmid College of Science and TechnologyChapman UniversityOrangeCAUSA
| | - K. Allen
- Manaaki Whenua—Landcare ResearchLincolnNew Zealand
| | - E. Brzostek
- Department of BiologyWest Virginia UniversityMorgantownWVUSA
| | - M. Shi
- Pacific Northwest National LaboratoryRichlandWAUSA
| | - X. Yang
- Environmental Sciences Division and Climate Change Science InstituteOak Ridge National LaboratoryOak RidgeTNUSA
| | - D. M. Ricciuto
- Environmental Sciences Division and Climate Change Science InstituteOak Ridge National LaboratoryOak RidgeTNUSA
| | - R. A. Fisher
- Center for International Climate ResearchOsloNorway
- Laboratoire Évolution & Diversité BiologiqueCNRS:UMRUniversité Paul SabatierToulouseFrance
| | - Q. Zhu
- Climate and Ecosystem Sciences DivisionClimate Sciences DepartmentLawrence Berkeley National LaboratoryBerkeleyCAUSA
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6
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Lie Z, Zhou G, Huang W, Kadowaki K, Tissue DT, Yan J, Peñuelas J, Sardans J, Li Y, Liu S, Chu G, Meng Z, He X, Liu J. Warming drives sustained plant phosphorus demand in a humid tropical forest. GLOBAL CHANGE BIOLOGY 2022; 28:4085-4096. [PMID: 35412664 DOI: 10.1111/gcb.16194] [Citation(s) in RCA: 8] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/13/2021] [Revised: 04/06/2022] [Accepted: 04/06/2022] [Indexed: 06/14/2023]
Abstract
Phosphorus (P) is often one of the most limiting nutrients in highly weathered soils of humid tropical forests and may regulate the responses of carbon (C) feedback to climate warming. However, the response of P to warming at the ecosystem level in tropical forests is not well understood because previous studies have not comprehensively assessed changes in multiple P processes associated with warming. Here, we detected changes in the ecosystem P cycle in response to a 7-year continuous warming experiment by translocating model plant-soil ecosystems across a 600-m elevation gradient, equivalent to a temperature change of 2.1°C. We found that warming increased plant P content (55.4%) and decreased foliar N:P. Increased plant P content was supplied by multiple processes, including enhanced plant P resorption (9.7%), soil P mineralization (15.5% decrease in moderately available organic P), and dissolution (6.8% decrease in iron-bound inorganic P), without changing litter P mineralization and leachate P. These findings suggest that warming sustained plant P demand by increasing the biological and geochemical controls of the plant-soil P-cycle, which has important implications for C fixation in P-deficient and highly productive tropical forests in future warmer climates.
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Affiliation(s)
- Zhiyang Lie
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- University of Chinese Academy of Sciences, Beijing, China
- Field Science Education and Research Center, Kyoto University, Kyoto, Japan
| | - Guoyi Zhou
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
| | - Wenjuan Huang
- Department of Ecology, Evolution, and Organismal Biology, Iowa State University, Ames, Iowa, USA
| | - Kohmei Kadowaki
- Field Science Education and Research Center, Kyoto University, Kyoto, Japan
- The Hakubi Center for Advanced Research, Graduate School of Agriculture, Kyoto University, Kyoto, Japan
| | - David T Tissue
- Hawkesbury Institute for the Environment, Western Sydney University, Hawkesbury Campus, Richmond, New South Wales, Australia
- Global Centre for Land-Based Innovation, Western Sydney University, Hawkesbury Campus, Richmond, New South Wales, Australia
| | - Junhua Yan
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
| | - Josep Peñuelas
- CSIC, Global Ecology Unit CREAF-CEAB-UAB, Bellaterra, Catalonia, Spain
- CREAF, Cerdanyola del Valles, Catalonia, Spain
| | - Jordi Sardans
- CSIC, Global Ecology Unit CREAF-CEAB-UAB, Bellaterra, Catalonia, Spain
- CREAF, Cerdanyola del Valles, Catalonia, Spain
| | - Yuelin Li
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
| | - Shizhong Liu
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
| | - Guowei Chu
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
| | - Ze Meng
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
| | - Xinhua He
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
| | - Juxiu Liu
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
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7
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Hu Y, Chen J, Hui D, Wang YP, Li J, Chen J, Chen G, Zhu Y, Zhang L, Zhang D, Deng Q. Mycorrhizal fungi alleviate acidification-induced phosphorus limitation: Evidence from a decade-long field experiment of simulated acid deposition in a tropical forest in south China. GLOBAL CHANGE BIOLOGY 2022; 28:3605-3619. [PMID: 35175681 DOI: 10.1111/gcb.16135] [Citation(s) in RCA: 12] [Impact Index Per Article: 6.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/03/2022] [Revised: 02/15/2022] [Accepted: 02/15/2022] [Indexed: 06/14/2023]
Abstract
South China has been experiencing very high rate of acid deposition and severe soil acidification in recent decades, which has been proposed to exacerbate the regional ecosystem phosphorus (P) limitation. We conducted a 10-year field experiment of simulated acid deposition to examine how acidification impacts seasonal changes of different soil P fractions in a tropical forest with highly acidic soils in south China. As expected, acid addition significantly increased occluded P pool but reduced the other more labile P pools in the dry season. In the wet season, however, acid addition did not change microbial P, soluble P and labile organic P pools. Acid addition significantly increased exchangeable Al3+ and Fe3+ and the activation of Fe oxides in both seasons. Different from the decline of microbial abundance in the dry season, acid addition increased ectomycorrhizal fungi and its ratio to arbuscular mycorrhiza fungi in the wet season, which significantly stimulated phosphomonoesterase activities and likely promoted the dissolution of occluded P. Our results suggest that, even in already highly acidic soils, the acidification-induced P limitation could be alleviated by stimulating ectomycorrhizal fungi and phosphomonoesterase activities. The differential responses and microbial controls of seasonal soil P transformation revealed here should be implemented into ecosystem biogeochemical model for predicting plant productivity under future acid deposition scenarios.
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Affiliation(s)
- Yuanliu Hu
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China
- Center for Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou, China
- University of Chinese Academy of Sciences, Beijing, China
- Department of Agroecology, Aarhus University, Tjele, Denmark
| | - Ji Chen
- Department of Agroecology, Aarhus University, Tjele, Denmark
- Aarhus University Centre for Circular Bioeconomy, Aarhus University, Tjele, Denmark
- iCLIMATE Interdisciplinary Centre for Climate Change, Aarhus University, Roskilde, Denmark
| | - Dafeng Hui
- Department of Biological Sciences, Tennessee State University, Nashville, Tennessee, USA
| | - Ying-Ping Wang
- CSIRO Oceans and Atmosphere, Aspendale, Victoria, Australia
| | - Jianling Li
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China
- Center for Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou, China
| | - Jingwen Chen
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China
- Center for Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou, China
- University of Chinese Academy of Sciences, Beijing, China
| | - Guoyin Chen
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China
- Center for Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou, China
- University of Chinese Academy of Sciences, Beijing, China
| | - Yiren Zhu
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China
- Center for Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou, China
- University of Chinese Academy of Sciences, Beijing, China
| | - Leiyi Zhang
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China
- Center for Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou, China
| | - Deqiang Zhang
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China
- Center for Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou, China
| | - Qi Deng
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China
- Center for Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou, China
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8
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Contribution of Incorporating the Phosphorus Cycle into TRIPLEX-CNP to Improve the Quantification of Land Carbon Cycle. LAND 2022. [DOI: 10.3390/land11060778] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 12/10/2022]
Abstract
Phosphorus (P) is a key and a limiting nutrient in ecosystems and plays an important role in many physiological and biochemical processes, affecting both terrestrial ecosystem productivity and soil carbon storage. However, only a few global land surface models have incorporated P cycle and used to investigate the interactions of C-N-P and its limitation on terrestrial ecosystems. The overall objective of this study was to integrate the P cycle and its interaction with carbon (C) and nitrogen (N) into new processes model of TRIPLEX-CNP. In this study, key processes of the P cycle, including P pool sizes and fluxes in plant, litter, and soil were integrated into a new model framework, TRIPLEX-CNP. We also added dynamic P:C ratios for different ecosystems. Based on sensitivity analysis results, we identified the phosphorus resorption coefficient of leaf (rpleaf) as the most influential parameter to gross primary productivity (GPP) and biomass, and determined optimal coefficients for different plant functional types (PFTs). TRIPLEX-CNP was calibrated with 49 sites and validated against 116 sites across eight biomes globally. The results suggested that TRIPLEX-CNP performed well on simulating the global GPP and soil organic carbon (SOC) with respective R2 values of 0.85 and 0.78 (both p < 0.01) between simulated and observed values. The R2 of simulation and observation of total biomass are 0.67 (p < 0.01) by TRIPLEX-CNP. The overall model performance had been improved in global GPP, total biomass and SOC after adding the P cycle comparing with the earlier version. Our work represents the promising step toward new coupled ecosystem process models for improving the quantifications of land carbon cycle and reducing uncertainty.
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9
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Wang Y, Huang Y, Augusto L, Goll DS, Helfenstein J, Hou E. Toward a Global Model for Soil Inorganic Phosphorus Dynamics: Dependence of Exchange Kinetics and Soil Bioavailability on Soil Physicochemical Properties. GLOBAL BIOGEOCHEMICAL CYCLES 2022; 36:e2021GB007061. [PMID: 35865755 PMCID: PMC9286372 DOI: 10.1029/2021gb007061] [Citation(s) in RCA: 5] [Impact Index Per Article: 2.5] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 05/03/2021] [Revised: 02/28/2022] [Accepted: 03/02/2022] [Indexed: 06/15/2023]
Abstract
The representation of phosphorus (P) cycling in global land models remains quite simplistic, particularly on soil inorganic phosphorus. For example, sorption and desorption remain unresolved and their dependence on soil physical and chemical properties is ignored. Empirical parameter values are usually based on expert knowledge or data from few sites with debatable global representativeness in most global land models. To overcome these issues, we compiled from data of inorganic soil P fractions and calculated the fraction of added P remaining in soil solution over time of 147 soil samples to optimize three parameters in a model of soil inorganic P dynamics. The calibrated model performed well (r 2 > 0.7 for 122 soil samples). Model parameters vary by several orders of magnitude, and correlate with soil P fractions of different inorganic pools, soil organic carbon and oxalate extractable metal oxide concentrations among the soil samples. The modeled bioavailability of soil P depends on, not only, the desorption rates of labile and sorbed pool, inorganic phosphorus fractions, the slope of P sorbed against solution P concentration, but also on the ability of biological uptake to deplete solution P concentration and the time scale. The model together with the empirical relationships of model parameters on soil properties can be used to quantify bioavailability of soil inorganic P on various timescale especially when coupled within global land models.
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Affiliation(s)
| | | | - Laurent Augusto
- INRAEBordeaux Sciences AgroUMR 1391 ISPAVillenave d'OrnonFrance
| | - Daniel S. Goll
- Université Paris SaclayCEA‐CNRS‐UVSQLSCE/IPSLGif sur YvetteFrance
| | | | - Enqing Hou
- Key Laboratory of Vegetation Restoration and Management of Degraded EcosystemsSouth China Botanical GardenChinese Academy of SciencesGuangzhouChina
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10
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Souza LFT, Billings SA. Temperature and pH mediate stoichiometric constraints of organically derived soil nutrients. GLOBAL CHANGE BIOLOGY 2022; 28:1630-1642. [PMID: 34767675 PMCID: PMC9298831 DOI: 10.1111/gcb.15985] [Citation(s) in RCA: 7] [Impact Index Per Article: 3.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 06/21/2021] [Accepted: 10/27/2021] [Indexed: 06/13/2023]
Abstract
It remains unclear how warming will affect resource flows during soil organic matter (SOM) decomposition, in part due to uncertainty in how exoenzymes produced by microbes and roots will function. Rising temperatures can enhance the activity of most exoenzymes, but soil pH can impose limitations on their catalytic efficiency. The effects of temperature and pH on enzyme activity are often examined in environmental samples, but purified enzyme kinetics reveal fundamental attributes of enzymes' intrinsic temperature responses and how relative release of decay-liberated resources (their flow ratios) can change with environmental conditions. In this paper, we illuminate the principle that fundamental, biochemical limitations on SOM release of C, N, and P during decay, and differential exoenzymes' responses to the environment, can exert biosphere-scale significance on the stoichiometry of bioavailable soil resources. To that end, we combined previously published intrinsic temperature sensitivities of two hydrolytic enzymes that release C and N during decay with a novel data set characterizing the kinetics of a P-releasing enzyme (acid phosphatase) across an ecologically relevant pH gradient. We use these data to estimate potential change in the flow ratios derived from these three enzymes' activities (C:N, C:P, and N:P) at the global scale by the end of the century, based on temperature projections and soil pH distribution. Our results highlight how the temperature sensitivity of these hydrolytic enzymes and the influence of pH on that sensitivity can govern the relative availability of bioavailable resources derived from these enzymes. The work illuminates the utility of weaving well-defined kinetic constraints of microbes' exoenzymes into models that incorporate changing SOM inputs and composition, nutrient availability, and microbial functioning into their efforts to project terrestrial ecosystem functioning in a changing climate.
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Affiliation(s)
- Ligia F. T. Souza
- Department of Ecology and Evolutionary BiologyKansas Biological Survey & Center for Ecological ResearchUniversity of KansasLawrenceKansasUSA
| | - Sharon A. Billings
- Department of Ecology and Evolutionary BiologyKansas Biological Survey & Center for Ecological ResearchUniversity of KansasLawrenceKansasUSA
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11
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Vallicrosa H, Sardans J, Maspons J, Zuccarini P, Fernández-Martínez M, Bauters M, Goll DS, Ciais P, Obersteiner M, Janssens IA, Peñuelas J. Global maps and factors driving forest foliar elemental composition: the importance of evolutionary history. THE NEW PHYTOLOGIST 2022; 233:169-181. [PMID: 34614196 DOI: 10.1111/nph.17771] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/16/2021] [Accepted: 09/19/2021] [Indexed: 06/13/2023]
Abstract
Consistent information on the current elemental composition of vegetation at global scale and the variables that determine it is lacking. To fill this gap, we gathered a total of 30 912 georeferenced records on woody plants foliar concentrations of nitrogen (N), phosphorus (P) and potassium (K) from published databases, and produced global maps of foliar N, P and K concentrations for woody plants using neural networks at a resolution of 1 km2 . We used data for climate, atmospheric deposition, soil and morphoclimatic groups to train the neural networks. Foliar N, P and K do not follow clear global latitudinal patterns but are consistent with the hypothesis of soil substrate age. We additionally built generalized linear mixed models to investigate the evolutionary history effect together with the effects of environmental effects. In this comparison, evolutionary history effects explained most of the variability in all cases (mostly > 60%). These results emphasize the determinant role of evolutionary history in foliar elemental composition, which should be incorporated in upcoming dynamic global vegetation models.
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Affiliation(s)
- Helena Vallicrosa
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Bellaterra, Catalonia, 08913, Spain
- CREAF, Cerdanyola del Vallès, Catalonia, 08913, Spain
| | - Jordi Sardans
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Bellaterra, Catalonia, 08913, Spain
- CREAF, Cerdanyola del Vallès, Catalonia, 08913, Spain
| | - Joan Maspons
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Bellaterra, Catalonia, 08913, Spain
- CREAF, Cerdanyola del Vallès, Catalonia, 08913, Spain
| | - Paolo Zuccarini
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Bellaterra, Catalonia, 08913, Spain
- CREAF, Cerdanyola del Vallès, Catalonia, 08913, Spain
| | - Marcos Fernández-Martínez
- Research Group PLECO (Plants and Ecosystems), Department of Biology, University of Antwerp, Wilrijk, B-2610, Belgium
| | - Marijn Bauters
- Research Group PLECO (Plants and Ecosystems), Department of Biology, University of Antwerp, Wilrijk, B-2610, Belgium
| | | | | | - Michael Obersteiner
- Ecosystems Services and Management, International Institute for Applied Systems Analysis (IIASA), Schlossplatz 1, Laxenburg, A-2361, Austria
| | - Ivan A Janssens
- Research Group PLECO (Plants and Ecosystems), Department of Biology, University of Antwerp, Wilrijk, B-2610, Belgium
| | - Josep Peñuelas
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Bellaterra, Catalonia, 08913, Spain
- CREAF, Cerdanyola del Vallès, Catalonia, 08913, Spain
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12
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Margalef O, Sardans J, Maspons J, Molowny-Horas R, Fernández-Martínez M, Janssens IA, Richter A, Ciais P, Obersteiner M, Peñuelas J. The effect of global change on soil phosphatase activity. GLOBAL CHANGE BIOLOGY 2021; 27:5989-6003. [PMID: 34383341 DOI: 10.1111/gcb.15832] [Citation(s) in RCA: 20] [Impact Index Per Article: 6.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/09/2021] [Accepted: 07/20/2021] [Indexed: 06/13/2023]
Abstract
Soil phosphatase enzymes are produced by plant roots and microorganisms and play a key role in the cycling of phosphorus (P), an often-limiting element in terrestrial ecosystems. The production of these enzymes in soil is the most important biological strategy for acquiring phosphate ions from organic molecules. Previous works showed how soil potential phosphatase activity is mainly driven by climatic conditions and soil nitrogen (N) and carbon. Nonetheless, future trends of the activity of these enzymes under global change remain little known. We investigated the influence of some of the main drivers of change on soil phosphatase activity using a meta-analysis of results from 97 published studies. Our database included a compilation of N and P fertilization experiments, manipulation experiments with increased atmospheric CO2 concentration, warming, and drought, and studies comparing invaded and non-invaded ecosystems. Our results indicate that N fertilization leads to higher phosphatase activity, whereas P fertilization has the opposite effect. The rise of atmospheric CO2 levels or the arrival of invasive species also exhibits positive response ratios on the activity of soil phosphatases. However, the occurrence of recurrent drought episodes decreases the activity of soil phosphatases. Our analysis did not reveal statistically significant effects of warming on soil phosphatase activity. In general, soil enzymatic changes in the reviewed experiments depended on the initial nutrient and water status of the ecosystems. The observed patterns evidence that future soil phosphatase activity will not only depend on present-day soil conditions but also on potential compensations or amplifications among the different drivers of global change. The responses of soil phosphatases to the global change drivers reported in this study and the consideration of cost-benefit approaches based on the connection of the P and N cycle will be useful for a better estimation of phosphatase production in carbon (C)-N-P models.
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Affiliation(s)
- Olga Margalef
- RISKNAT Research Group, Department of Earth and Ocean Dynamics, University of Barcelona, Barcelona, Spain
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Barcelona, Spain
- CREAF, Barcelona, Spain
| | - Jordi Sardans
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Barcelona, Spain
- CREAF, Barcelona, Spain
| | - Joan Maspons
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Barcelona, Spain
- CREAF, Barcelona, Spain
| | | | - Marcos Fernández-Martínez
- Research Group Plants and Ecosystems (PLECO), Department of Biology, University of Antwerp, Wilrijk, Belgium
| | - Ivan A Janssens
- Research Group Plants and Ecosystems (PLECO), Department of Biology, University of Antwerp, Wilrijk, Belgium
| | - Andreas Richter
- Centre for Microbiology and Environmental Systems Science, University of Vienna, Vienna, Austria
| | - Philippe Ciais
- Laboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ-Université Paris-Saclay, Gif-sur-Yvette, France
| | | | - Josep Peñuelas
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Barcelona, Spain
- CREAF, Barcelona, Spain
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13
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Abstract
While widespread imitation of the productivity of the land biosphere by nutrients, like nitrogen and phosphorus, was demonstrated many decades ago, representation of nutrient cycles in global land models has been relatively recent. Over the last three years, significant progress has been made in understanding some of the key processes and their representation in global land models. They include the significance of plant–microbial interaction in affecting nutrient cycles, inorganic soil phosphorus transformation, and nitrogen release from rocks. As a result, our understanding of the linkages among geology, biology, and climate controlling nutrient cycles is improving. However, progress in modelling nutrient cycles at a global scale is still confronted with large uncertainties in representing key processes owing to lack of data at the relevant scales for evaluating coupled carbon and nutrient cycles. Here we recommend two approaches to advance modelling of land nutrient cycles: the application of machine learning techniques to bridge the gap between global modelling and scattered site-level information and the use of optimality principles to identify key mechanisms driving spatial and temporal patterns of nutrients.
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Affiliation(s)
- Ying-Ping Wang
- CSIRO Oceans and Atmosphere, PMB 1, Aspendale Victoria 3195, Australia
| | - Daniel S Goll
- Université Paris Saclay, CEA-CNRS-UVSQ, LSCE/IPSL, Gif sur Yvette, France
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14
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Hou E, Wen D, Jiang L, Luo X, Kuang Y, Lu X, Chen C, Allen KT, He X, Huang X, Luo Y. Latitudinal patterns of terrestrial phosphorus limitation over the globe. Ecol Lett 2021; 24:1420-1431. [DOI: 10.1111/ele.13761] [Citation(s) in RCA: 30] [Impact Index Per Article: 10.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/19/2020] [Revised: 03/22/2021] [Accepted: 03/25/2021] [Indexed: 01/25/2023]
Affiliation(s)
- Enqing Hou
- Center for Ecosystem Science and Society Northern Arizona University Flagstaff AZ USA
| | - Dazhi Wen
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems South China Botanical Garden, Chinese Academy of Sciences Guangzhou China
- Center of Plant Ecology, Core Botanical Gardens Chinese Academy of Sciences Guangzhou China
| | - Lifen Jiang
- Center for Ecosystem Science and Society Northern Arizona University Flagstaff AZ USA
| | - Xianzhen Luo
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems South China Botanical Garden, Chinese Academy of Sciences Guangzhou China
- Center of Plant Ecology, Core Botanical Gardens Chinese Academy of Sciences Guangzhou China
| | - Yuanwen Kuang
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems South China Botanical Garden, Chinese Academy of Sciences Guangzhou China
- Center of Plant Ecology, Core Botanical Gardens Chinese Academy of Sciences Guangzhou China
| | - Xiankai Lu
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems South China Botanical Garden, Chinese Academy of Sciences Guangzhou China
- Center of Plant Ecology, Core Botanical Gardens Chinese Academy of Sciences Guangzhou China
| | - Chengrong Chen
- Australian Rivers Institute, School of Environment and Science Griffith University Nathan Qld. Australia
| | - Keanan T. Allen
- Center for Ecosystem Science and Society Northern Arizona University Flagstaff AZ USA
| | - Xianjin He
- Key Laboratory of the Three Gorges Reservoir Region's Eco‐Environment, Ministry of Education Chongqing University Chongqing China
| | - Xingzhao Huang
- School of Forestry & Landscape of Architecture Anhui Agricultural University Hefei China
| | - Yiqi Luo
- Center for Ecosystem Science and Society Northern Arizona University Flagstaff AZ USA
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15
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Chen J, van Groenigen KJ, Hungate BA, Terrer C, van Groenigen JW, Maestre FT, Ying SC, Luo Y, Jørgensen U, Sinsabaugh RL, Olesen JE, Elsgaard L. Long-term nitrogen loading alleviates phosphorus limitation in terrestrial ecosystems. GLOBAL CHANGE BIOLOGY 2020; 26:5077-5086. [PMID: 32529708 DOI: 10.1111/gcb.15218] [Citation(s) in RCA: 49] [Impact Index Per Article: 12.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/28/2020] [Accepted: 05/21/2020] [Indexed: 05/02/2023]
Abstract
Increased human-derived nitrogen (N) deposition to terrestrial ecosystems has resulted in widespread phosphorus (P) limitation of net primary productivity. However, it remains unclear if and how N-induced P limitation varies over time. Soil extracellular phosphatases catalyze the hydrolysis of P from soil organic matter, an important adaptive mechanism for ecosystems to cope with N-induced P limitation. Here we show, using a meta-analysis of 140 studies and 668 observations worldwide, that N stimulation of soil phosphatase activity diminishes over time. Whereas short-term N loading (≤5 years) significantly increased soil phosphatase activity by 28%, long-term N loading had no significant effect. Nitrogen loading did not affect soil available P and total P content in either short- or long-term studies. Together, these results suggest that N-induced P limitation in ecosystems is alleviated in the long-term through the initial stimulation of soil phosphatase activity, thereby securing P supply to support plant growth. Our results suggest that increases in terrestrial carbon uptake due to ongoing anthropogenic N loading may be greater than previously thought.
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Affiliation(s)
- Ji Chen
- Department of Agroecology, Aarhus University, Tjele, Denmark
- Aarhus University Center for Circular Bioeconomy, Aarhus University, Tjele, Denmark
- iCLIMATE Interdisciplinary Centre for Climate Change, Aarhus University, Roskilde, Denmark
| | - Kees J van Groenigen
- Department of Geography, College of Life and Environmental Sciences, University of Exeter, Exeter, UK
| | - Bruce A Hungate
- Center for Ecosystem Science and Society and Department of Biological Sciences, Northern Arizona University, Flagstaff, AZ, USA
| | - César Terrer
- Physical and Life Sciences Directorate, Lawrence Livermore National Laboratory (LLNL), Livermore, CA, USA
| | | | - Fernando T Maestre
- Instituto Multidisciplinar para el Estudio del Medio "Ramon Margalef", Universidad de Alicante, Alicante, Spain
- Departamento de Ecología, Universidad de Alicante, Alicante, Spain
| | - Samantha C Ying
- Department of Environmental Sciences, University of California, Riverside, CA, USA
| | - Yiqi Luo
- Center for Ecosystem Science and Society and Department of Biological Sciences, Northern Arizona University, Flagstaff, AZ, USA
| | - Uffe Jørgensen
- Department of Agroecology, Aarhus University, Tjele, Denmark
- Aarhus University Center for Circular Bioeconomy, Aarhus University, Tjele, Denmark
| | | | - Jørgen E Olesen
- Department of Agroecology, Aarhus University, Tjele, Denmark
- iCLIMATE Interdisciplinary Centre for Climate Change, Aarhus University, Roskilde, Denmark
| | - Lars Elsgaard
- Department of Agroecology, Aarhus University, Tjele, Denmark
- iCLIMATE Interdisciplinary Centre for Climate Change, Aarhus University, Roskilde, Denmark
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16
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Penuelas J, Janssens IA, Ciais P, Obersteiner M, Sardans J. Anthropogenic global shifts in biospheric N and P concentrations and ratios and their impacts on biodiversity, ecosystem productivity, food security, and human health. GLOBAL CHANGE BIOLOGY 2020; 26:1962-1985. [PMID: 31912629 DOI: 10.1111/gcb.14981] [Citation(s) in RCA: 68] [Impact Index Per Article: 17.0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/09/2019] [Revised: 12/23/2019] [Accepted: 12/24/2019] [Indexed: 06/10/2023]
Abstract
The availability of carbon (C) from high levels of atmospheric carbon dioxide (CO2 ) and anthropogenic release of nitrogen (N) is increasing, but these increases are not paralleled by increases in levels of phosphorus (P). The current unstoppable changes in the stoichiometries of C and N relative to P have no historical precedent. We describe changes in P and N fluxes over the last five decades that have led to asymmetrical increases in P and N inputs to the biosphere. We identified widespread and rapid changes in N:P ratios in air, soil, water, and organisms and important consequences to the structure, function, and biodiversity of ecosystems. A mass-balance approach found that the combined limited availability of P and N was likely to reduce C storage by natural ecosystems during the remainder of the 21st Century, and projected crop yields of the Millennium Ecosystem Assessment indicated an increase in nutrient deficiency in developing regions if access to P fertilizer is limited. Imbalances of the N:P ratio would likely negatively affect human health, food security, and global economic and geopolitical stability, with feedbacks and synergistic effects on drivers of global environmental change, such as increasing levels of CO2 , climatic warming, and increasing pollution. We summarize potential solutions for avoiding the negative impacts of global imbalances of N:P ratios on the environment, biodiversity, climate change, food security, and human health.
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Affiliation(s)
- Josep Penuelas
- CSIC, Global Ecology Unit, CREAF-CSIC-UAB, Bellaterra, Spain
- CREAF, Cerdanyola del Valles, Spain
- Global Change Research Institute, Czech Academy of Sciences, Brno, Czech Republic
| | - Ivan A Janssens
- Research Group Plants and Ecosystems (PLECO), Department of Biology, University of Antwerp, Wilrijk, Belgium
| | - Philippe Ciais
- Laboratoire des Sciences du Climat et de l'Environnement, IPSL CEA CNRS UVSQ UPSACLAY, Gif-sur-Yvette, France
| | - Michael Obersteiner
- Ecosystems Services and Management, International Institute for Applied Systems Analysis (IIASA), Laxenburg, Austria
| | - Jordi Sardans
- CSIC, Global Ecology Unit, CREAF-CSIC-UAB, Bellaterra, Spain
- CREAF, Cerdanyola del Valles, Spain
- Global Change Research Institute, Czech Academy of Sciences, Brno, Czech Republic
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17
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Sun Y, Goll DS, Ciais P, Peng S, Margalef O, Asensio D, Sardans J, Peñuelas J. Spatial Pattern and Environmental Drivers of Acid Phosphatase Activity in Europe. Front Big Data 2020; 2:51. [PMID: 33693374 PMCID: PMC7931918 DOI: 10.3389/fdata.2019.00051] [Citation(s) in RCA: 6] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/31/2019] [Accepted: 12/26/2019] [Indexed: 11/13/2022] Open
Abstract
Acid phosphatase produced by plants and microbes plays a fundamental role in the recycling of soil phosphorus (P). A quantification of the spatial variation in potential acid phosphatase activity (AP) on large spatial scales and its drivers can help to reduce the uncertainty in our understanding of bio-availability of soil P. We applied two machine-learning methods (Random forests and back-propagation artificial networks) to simulate the spatial patterns of AP across Europe by scaling up 126 site observations of potential AP activity from field samples measured in the laboratory, using 12 environmental drivers as predictors. The back-propagation artificial network (BPN) method explained 58% of AP variability, more than the regression tree model (49%). In addition, BPN was able to identify the gradients in AP along three transects in Europe. Partial correlation analysis revealed that soil nutrients (total nitrogen, total P, and labile organic P) and climatic controls (annual precipitation, mean annual temperature, and temperature amplitude) were the dominant factors influencing AP variations in space. Higher AP occurred in regions with higher mean annual temperature, precipitation and higher soil total nitrogen. Soil TP and Po were non-monotonically correlated with modeled AP for Europe, indicating diffident strategies of P utilization by biomes in arid and humid area. This study helps to separate the influences of each factor on AP production and to reduce the uncertainty in estimating soil P availability. The BPN model trained with European data, however, could not produce a robust global map of AP due to the lack of representative measurements of AP for tropical regions. Filling this data gap will help us to understand the physiological basis of P-use strategies in natural soils.
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Affiliation(s)
- Yan Sun
- Laboratoire des Sciences du Climat et de 1'Environnement, CEA-CNRS-UVSQ, Gif sur Yvette, France
| | - Daniel S. Goll
- Laboratoire des Sciences du Climat et de 1'Environnement, CEA-CNRS-UVSQ, Gif sur Yvette, France
- Institute of Geography, University of Augsburg, Augsburg, Germany
| | - Philippe Ciais
- Laboratoire des Sciences du Climat et de 1'Environnement, CEA-CNRS-UVSQ, Gif sur Yvette, France
| | - Shushi Peng
- Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China
| | - Olga Margalef
- CSIC, Global Ecology Unit, Centre de Recerca Ecològica i Aplicacions Forestals, Consejo Superior de Investigaciones Científicas, UAB, Bellaterra, Spain
- Centre de Recerca Ecològica i Aplicacions Forestals, Cerdanyola del Vallès, Spain
| | - Dolores Asensio
- CSIC, Global Ecology Unit, Centre de Recerca Ecològica i Aplicacions Forestals, Consejo Superior de Investigaciones Científicas, UAB, Bellaterra, Spain
- Centre de Recerca Ecològica i Aplicacions Forestals, Cerdanyola del Vallès, Spain
| | - Jordi Sardans
- CSIC, Global Ecology Unit, Centre de Recerca Ecològica i Aplicacions Forestals, Consejo Superior de Investigaciones Científicas, UAB, Bellaterra, Spain
- Centre de Recerca Ecològica i Aplicacions Forestals, Cerdanyola del Vallès, Spain
| | - Josep Peñuelas
- CSIC, Global Ecology Unit, Centre de Recerca Ecològica i Aplicacions Forestals, Consejo Superior de Investigaciones Científicas, UAB, Bellaterra, Spain
- Centre de Recerca Ecològica i Aplicacions Forestals, Cerdanyola del Vallès, Spain
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18
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Jiang M, Caldararu S, Zaehle S, Ellsworth DS, Medlyn BE. Towards a more physiological representation of vegetation phosphorus processes in land surface models. THE NEW PHYTOLOGIST 2019; 222:1223-1229. [PMID: 30659603 DOI: 10.1111/nph.15688] [Citation(s) in RCA: 28] [Impact Index Per Article: 5.6] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/04/2018] [Accepted: 01/07/2019] [Indexed: 05/26/2023]
Abstract
Contents Summary 1223 I. Introduction 1223 II. Photosynthesis and respiration 1224 III. Biomass growth 1224 IV. Carbon allocation 1225 V. Plant internal P redistribution 1226 VI. Plant P uptake 1227 VII. Conclusion 1227 Acknowledgements 1228 References 1228 SUMMARY: Our ability to understand the effect of nutrient limitation on ecosystem productivity is key to the prediction of future terrestrial carbon storage. Significant progress has been made to include phosphorus (P) cycle processes in land surface models (LSMs), but these efforts are focused on the soil component of the P cycle. Incorporating the soil component is important to estimate plant-available P, but does not necessarily address the vegetation response to P limitation or plant-soil interactions. A more detailed representation of plant P processes is needed to link nutrient availability and ecosystem productivity. We review physiological and biochemical evidence for vegetation responses to P availability, and recommend ways to move towards a more physiological representation of vegetation P processes in LSMs.
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Affiliation(s)
- Mingkai Jiang
- Hawkesbury Institute for the Environment, Western Sydney University, Locked Bag 1797, Penrith, NSW, 2751, Australia
| | - Silvia Caldararu
- Max Planck Institute for Biogeochemistry, PO Box 60 01 64, 07701, Jena, Germany
| | - Sönke Zaehle
- Max Planck Institute for Biogeochemistry, PO Box 60 01 64, 07701, Jena, Germany
| | - David S Ellsworth
- Hawkesbury Institute for the Environment, Western Sydney University, Locked Bag 1797, Penrith, NSW, 2751, Australia
| | - Belinda E Medlyn
- Hawkesbury Institute for the Environment, Western Sydney University, Locked Bag 1797, Penrith, NSW, 2751, Australia
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Hou E, Tan X, Heenan M, Wen D. A global dataset of plant available and unavailable phosphorus in natural soils derived by Hedley method. Sci Data 2018; 5:180166. [PMID: 30129932 PMCID: PMC6103263 DOI: 10.1038/sdata.2018.166] [Citation(s) in RCA: 19] [Impact Index Per Article: 3.2] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/06/2018] [Accepted: 06/29/2018] [Indexed: 11/09/2022] Open
Abstract
Soil phosphorus (P) fractions are critical for understanding soil P dynamics and availability. This paper provides a global dataset of soil P fractions separated by the Hedley method. The dataset also includes key environmental factors associated with soil P dynamics and availability, including climate factors, vegetation, soil and parent material types, soil age, and soil physiochemical properties such as particle size, bulk density, pH in water, organic carbon, total nitrogen, and extractable iron and aluminium concentrations. This dataset includes measures of Hedley P fractions of 802 soil samples and was gathered through a literature survey of 99 published studies. Plant availability of each soil P fraction was noted. We anticipate that the global dataset will provide valuable information for studying soil P dynamics and availability, and it will be fused into earth system models to better predict how terrestrial ecosystems will respond to global environmental changes.
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Affiliation(s)
- Enqing Hou
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China
| | - Xiang Tan
- Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, The Chinese Academy of Sciences, Wuhan 430074, China
| | - Marijke Heenan
- Department of Science, Information Technology and Innovation, Queensland Government, Dutton Park, Brisbane, Queens Land 4102, Australia
| | - Dazhi Wen
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China.,Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China
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20
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Hou E, Chen C, Luo Y, Zhou G, Kuang Y, Zhang Y, Heenan M, Lu X, Wen D. Effects of climate on soil phosphorus cycle and availability in natural terrestrial ecosystems. GLOBAL CHANGE BIOLOGY 2018; 24:3344-3356. [PMID: 29450947 DOI: 10.1111/gcb.14093] [Citation(s) in RCA: 71] [Impact Index Per Article: 11.8] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/08/2017] [Accepted: 02/07/2018] [Indexed: 06/08/2023]
Abstract
Climate is predicted to change over the 21st century. However, little is known about how climate change can affect soil phosphorus (P) cycle and availability in global terrestrial ecosystems, where P is a key limiting nutrient. With a global database of Hedley P fractions and key-associated physiochemical properties of 760 (seminatural) natural soils compiled from 96 published studies, this study evaluated how climate pattern affected soil P cycle and availability in global terrestrial ecosystems. Overall, soil available P, indexed by Hedley labile inorganic P fraction, significantly decreased with increasing mean annual temperature (MAT) and precipitation (MAP). Hypothesis-oriented path model analysis suggests that MAT negatively affected soil available P mainly by decreasing soil organic P and primary mineral P and increasing soil sand content. MAP negatively affected soil available P both directly and indirectly through decreasing soil primary mineral P; however, these negative effects were offset by the positive effects of MAP on soil organic P and fine soil particles, resulting in a relatively minor total MAP effect on soil available P. As aridity degree was mainly determined by MAP, aridity also had a relatively minor total effect on soil available P. These global patterns generally hold true irrespective of soil depth (≤10 cm or >10 cm) or site aridity index (≤1.0 or >1.0), and were also true for the low-sand (≤50%) soils. In contrast, available P of the high-sand (>50%) soils was positively affected by MAT and aridity and negatively affected by MAP. Our results suggest that temperature and precipitation have contrasting effects on soil P availability and can interact with soil particle size to control soil P availability.
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Affiliation(s)
- Enqing Hou
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Center for Ecosystem Science and Society, Northern Arizona University, Flagstaff, AZ, USA
- Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
| | - Chengrong Chen
- Griffith School of Environment, Griffith University, Nathan, QLD, Australia
| | - Yiqi Luo
- Center for Ecosystem Science and Society, Northern Arizona University, Flagstaff, AZ, USA
| | - Guoyi Zhou
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
| | - Yuanwen Kuang
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
| | - Yuguang Zhang
- Institute of Forestry Ecology, Environment and Protection, The Key Laboratory of Forest Ecology and Environment of State Forestry Administration, Chinese Academy of Forestry, Beijing, China
| | - Marijke Heenan
- Department of Science, Information Technology and Innovation, Queensland Government, Brisbane, QLD, Australia
| | - Xiankai Lu
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
| | - Dazhi Wen
- Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
- Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China
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Yuan Z, Jiang S, Sheng H, Liu X, Hua H, Liu X, Zhang Y. Human Perturbation of the Global Phosphorus Cycle: Changes and Consequences. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2018; 52:2438-2450. [PMID: 29402084 DOI: 10.1021/acs.est.7b03910] [Citation(s) in RCA: 83] [Impact Index Per Article: 13.8] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/10/2023]
Abstract
The phosphorus (P) cycle is an important Earth system process. While natural P mobilization is slow, humans have been altering P cycle by intensifying P releases from lithosphere to ecosystems. Here, we examined magnitudes of which humans have altered the P cycles by integrating the estimates from recent literatures, and furthermore illustrated the consequences. Based on our synthesis, human alterations have tripled the global P mobilization in land-water continuum and increased P accumulation in soil with 6.9 ± 3.3 Tg-P yr-1. Around 30% of atmospheric P transfer is caused by human activities, which plays a significant role than previously thought. Pathways involving with human alterations include phosphate extraction, fertilizers application, wastes generation, and P losses from cropland. This study highlights the importance of sustainable P supply as a control on future food security because of regional P scarcity, food demand increase and continuously P intensive food production. Besides, accelerated P loads are responsible for enhanced eutrophication worldwide, resulting in water quality impairment and aquatic biodiversity losses. Moreover, the P enrichment can definitely stimulate the cycling of carbon and nitrogen, implying the great need for incorporating P in models predicting the response of carbon and nitrogen cycles to global changes.
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Affiliation(s)
- Zengwei Yuan
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment , Nanjing University , Nanjing 210023 , China
| | - Songyan Jiang
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment , Nanjing University , Nanjing 210023 , China
| | - Hu Sheng
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment , Nanjing University , Nanjing 210023 , China
| | - Xin Liu
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment , Nanjing University , Nanjing 210023 , China
| | - Hui Hua
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment , Nanjing University , Nanjing 210023 , China
| | - Xuewei Liu
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment , Nanjing University , Nanjing 210023 , China
| | - You Zhang
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment , Nanjing University , Nanjing 210023 , China
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22
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Zhou Y, Boutton TW, Wu XB. Woody plant encroachment amplifies spatial heterogeneity of soil phosphorus to considerable depth. Ecology 2017; 99:136-147. [DOI: 10.1002/ecy.2051] [Citation(s) in RCA: 28] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Submit a Manuscript] [Subscribe] [Scholar Register] [Received: 03/11/2017] [Revised: 09/09/2017] [Accepted: 10/05/2017] [Indexed: 11/08/2022]
Affiliation(s)
- Yong Zhou
- Department of Ecosystem Science and Management Texas A&M University College StationTexas 77843 USA
| | - Thomas W. Boutton
- Department of Ecosystem Science and Management Texas A&M University College StationTexas 77843 USA
| | - X. Ben Wu
- Department of Ecosystem Science and Management Texas A&M University College StationTexas 77843 USA
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