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Bagra K, Kneis D, Padfield D, Szekeres E, Teban-Man A, Coman C, Singh G, Berendonk TU, Klümper U. Contrary effects of increasing temperatures on the spread of antimicrobial resistance in river biofilms. mSphere 2024; 9:e0057323. [PMID: 38323843 PMCID: PMC10900892 DOI: 10.1128/msphere.00573-23] [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: 10/10/2023] [Accepted: 01/10/2024] [Indexed: 02/08/2024] Open
Abstract
River microbial communities regularly act as the first barrier of defense against the spread of antimicrobial resistance genes (ARGs) that enter environmental microbiomes through wastewater. However, how the invasion dynamics of wastewater-borne ARGs into river biofilm communities will shift due to climate change with increasing average and peak temperatures remains unknown. Here, we aimed to elucidate the effects of increasing temperatures on the naturally occurring river biofilm resistome, as well as the invasion success of foreign ARGs entering through wastewater. Natural biofilms were grown in a low-anthropogenic impact river and transferred to artificial laboratory recirculation flume systems operated at three different temperatures (20°C, 25°C, and 30°C). After 1 week of temperature acclimatization, significant increases in the abundance of the naturally occurring ARGs in biofilms were detected at higher temperatures. After this acclimatization period, biofilms were exposed to a single pulse of wastewater, and the invasion dynamics of wastewater-borne ARGs were analyzed over 2 weeks. After 1 day, wastewater-borne ARGs were able to invade the biofilms successfully with no observable effect of temperature on their relative abundance. However, thereafter, ARGs were lost at a far increased rate at 30°C, with ARG levels dropping to the initial natural levels after 14 days. Contrary to the lower temperatures, ARGs were either lost at slower rates or even able to establish themselves in biofilms with stable relative abundances above natural levels. Hence, higher temperatures come with contrary effects on river biofilm resistomes: naturally occurring ARGs increase in abundance, while foreign, invading ARGs are lost at elevated speeds.IMPORTANCEInfections with bacteria that gained resistance to antibiotics are taking millions of lives annually, with the death toll predicted to increase. River microbial communities act as a first defense barrier against the spread of antimicrobial resistance genes (ARGs) that enter the environment through wastewater after enrichment in human and animal microbiomes. The global increase in temperature due to climate change might disrupt this barrier effect by altering microbial community structure and functions. We consequently explored how increasing temperatures alter ARG spread in river microbial communities. At higher temperatures, naturally occurring ARGs increased in relative abundance. However, this coincided with a decreased success rate of invading foreign ARGs from wastewater to establish themselves in the communities. Therefore, to predict the effects of climate change on ARG spread in river microbiomes, it is imperative to consider if the river ecosystem and its resistome are dominated by naturally occurring or invading foreign ARGs.
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Affiliation(s)
- Kenyum Bagra
- Institute for Hydrobiology, Technische Universität Dresden, Dresden, Germany
- Indian Institute of Technology, Roorkee, Uttarakhand, India
| | - David Kneis
- Institute for Hydrobiology, Technische Universität Dresden, Dresden, Germany
| | - Daniel Padfield
- Environment and Sustainability Institute, University of Exeter, Exeter, United Kingdom
| | - Edina Szekeres
- Institute of Biological Research Cluj, NIRDBS, Cluj-Napoca, Romania
| | - Adela Teban-Man
- Institute of Biological Research Cluj, NIRDBS, Cluj-Napoca, Romania
| | - Cristian Coman
- Institute of Biological Research Cluj, NIRDBS, Cluj-Napoca, Romania
| | - Gargi Singh
- Indian Institute of Technology, Roorkee, Uttarakhand, India
| | - Thomas U. Berendonk
- Institute for Hydrobiology, Technische Universität Dresden, Dresden, Germany
| | - Uli Klümper
- Institute for Hydrobiology, Technische Universität Dresden, Dresden, Germany
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2
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Bhattarai B, Sigurdsson BD, Sigurdsson P, Leblans N, Janssens I, Meynzer W, Devarajan AK, Truu J, Truu M, Ostonen I. Soil warming duration and magnitude affect the dynamics of fine roots and rhizomes and associated C and N pools in subarctic grasslands. ANNALS OF BOTANY 2023; 132:269-279. [PMID: 37471454 PMCID: PMC10583211 DOI: 10.1093/aob/mcad102] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/12/2023] [Accepted: 07/18/2023] [Indexed: 07/22/2023]
Abstract
BACKGROUND AND AIMS The response of subarctic grassland's below-ground to soil warming is key to understanding this ecosystem's adaptation to future climate. Functionally different below-ground plant organs can respond differently to changes in soil temperature (Ts). We aimed to understand the below-ground adaptation mechanisms by analysing the dynamics and chemistry of fine roots and rhizomes in relation to plant community composition and soil chemistry, along with the duration and magnitude of soil warming. METHODS We investigated the effects of the duration [medium-term warming (MTW; 11 years) and long-term warming (LTW; > 60 years)] and magnitude (0-8.4 °C) of soil warming on below-ground plant biomass (BPB), fine root biomass (FRB) and rhizome biomass (RHB) in geothermally warmed subarctic grasslands. We evaluated the changes in BPB, FRB and RHB and the corresponding carbon (C) and nitrogen (N) pools in the context of ambient, Ts < +2 °C and Ts > +2 °C scenarios. KEY RESULTS BPB decreased exponentially in response to an increase in Ts under MTW, whereas FRB declined under both MTW and LTW. The proportion of rhizomes increased and the C-N ratio in rhizomes decreased under LTW. The C and N pools in BPB in highly warmed plots under MTW were 50 % less than in the ambient plots, whereas under LTW, C and N pools in warmed plots were similar to those in non-warmed plots. Approximately 78 % of the variation in FRB, RHB, and C and N concentration and pools in fine roots and rhizomes was explained by the duration and magnitude of soil warming, soil chemistry, plant community functional composition, and above-ground biomass. Plant's below-ground biomass, chemistry and pools were related to a shift in the grassland's plant community composition - the abundance of ferns increased and BPB decreased towards higher Ts under MTW, while the recovery of below-ground C and N pools under LTW was related to a higher plant diversity. CONCLUSION Our results indicate that plant community-level adaptation of below ground to soil warming occurs over long periods. We provide insight into the potential adaptation phases of subarctic grasslands.
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Affiliation(s)
- Biplabi Bhattarai
- Institute of Ecology and Earth Sciences, University of Tartu, Estonia
| | - Bjarni D Sigurdsson
- Faculty of Environmental and Forest Sciences, The Agricultural University of Iceland, Iceland
| | - Páll Sigurdsson
- Faculty of Environmental and Forest Sciences, The Agricultural University of Iceland, Iceland
| | - Niki Leblans
- Climate Impact Research Centre, Umeå University, Sweden
| | - Ivan Janssens
- Department of Biology, University of Antwerp, Belgium
| | | | | | - Jaak Truu
- Institute of Molecular and Cell Biology, University of Tartu, Estonia
| | - Marika Truu
- Institute of Molecular and Cell Biology, University of Tartu, Estonia
| | - Ivika Ostonen
- Institute of Ecology and Earth Sciences, University of Tartu, Estonia
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3
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Robinson SI, O’Gorman EJ, Frey B, Hagner M, Mikola J. Soil organic matter, rather than temperature, determines the structure and functioning of subarctic decomposer communities. GLOBAL CHANGE BIOLOGY 2022; 28:3929-3943. [PMID: 35263490 PMCID: PMC9310844 DOI: 10.1111/gcb.16158] [Citation(s) in RCA: 4] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 08/13/2021] [Accepted: 02/05/2022] [Indexed: 06/14/2023]
Abstract
The impacts of climate change on ecosystem structure and functioning are likely to be strongest at high latitudes due to the adaptation of biota to relatively low temperatures and nutrient levels. Soil warming is widely predicted to alter microbial, invertebrate, and plant communities, with cascading effects on ecosystem functioning, but this has largely been demonstrated over short-term (<10 year) warming studies. Using a natural soil temperature gradient spanning 10-35°C, we examine responses of soil organisms, decomposition, nitrogen cycling, and plant biomass production to long-term warming. We find that decomposer organisms are surprisingly resistant to chronic warming, with no responses of bacteria, fungi, or their grazers to temperature (fungivorous nematodes being an exception). Soil organic matter content instead drives spatial variation in microorganism abundances and mineral N availability. The few temperature effects that appear are more focused: root biomass and abundance of root-feeding nematodes decrease, and nitrification increases with increasing soil temperature. Our results suggest that transient responses of decomposers and soil functioning to warming may stabilize over time following acclimation and/or adaptation, highlighting the need for long-term, ecosystem-scale studies that incorporate evolutionary responses to soil warming.
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Affiliation(s)
- Sinikka I. Robinson
- Ecosystems and Environment Research ProgrammeUniversity of HelsinkiHelsinkiFinland
| | | | - Beat Frey
- Swiss Federal Research Institute WSLBirmensdorfSwitzerland
| | - Marleena Hagner
- Ecosystems and Environment Research ProgrammeUniversity of HelsinkiHelsinkiFinland
- Natural Resources Institute Finland (Luke)JokioinenFinland
| | - Juha Mikola
- Ecosystems and Environment Research ProgrammeUniversity of HelsinkiHelsinkiFinland
- Natural Resources Institute Finland (Luke)HelsinkiFinland
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4
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Silva I, Alves M, Malheiro C, Silva ARR, Loureiro S, Henriques I, González-Alcaraz MN. Short-Term Responses of Soil Microbial Communities to Changes in Air Temperature, Soil Moisture and UV Radiation. Genes (Basel) 2022; 13:genes13050850. [PMID: 35627235 PMCID: PMC9142034 DOI: 10.3390/genes13050850] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/23/2022] [Revised: 05/04/2022] [Accepted: 05/07/2022] [Indexed: 01/31/2023] Open
Abstract
We analyzed the effects on a soil microbial community of short-term alterations in air temperature, soil moisture and ultraviolet radiation and assessed the role of invertebrates (species Enchytraeus crypticus) in modulating the community’s response to these factors. The reference soil, Lufa 2.2, was incubated for 48 h, with and without invertebrates, under the following conditions: standard (20 °C + 50% water holding capacity (WHC)); increased air temperature (15–25 °C or 20–30 °C + 50% WHC); flood (20 °C + 75% WHC); drought (20 °C + 25% WHC); and ultraviolet radiation (UV) (20 °C + 50% WHC + UV). BIOLOG EcoPlates and 16S rDNA sequencing (Illumina) were used to assess the microbial community’s physiological profile and the bacterial community’s structure, respectively. The bacterial abundance (estimated by 16S rDNA qPCR) did not change. Most of the conditions led to an increase in microbial activity and a decrease in diversity. The structure of the bacterial community was particularly affected by higher air temperatures (20–30 °C, without E. crypticus) and floods (with E. crypticus). Effects were observed at the class, genera and OTU levels. The presence of invertebrates mostly resulted in the attenuation of the observed effects, highlighting the importance of considering microbiome–invertebrate interactions. Considering future climate changes, the effects described here raise concern. This study provides fundamental knowledge to develop effective strategies to mitigate these negative outcomes. However, long-term studies integrating biotic and abiotic factors are needed.
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Affiliation(s)
- Isabel Silva
- CEF (Center for Functional Ecology), Department of Life Sciences, Faculty of Sciences and Technology, University of Coimbra, 3000-456 Coimbra, Portugal;
- CESAM (Centre for Marine and Environmental Studies), Department of Biology, University of Aveiro, 3810-193 Aveiro, Portugal; (C.M.); (A.R.R.S.); (S.L.)
| | - Marta Alves
- CBQF—Center for Biotechnology and Fine Chemistry, School of Biotechnology, Portuguese Catholic University, 4169-005 Porto, Portugal;
| | - Catarina Malheiro
- CESAM (Centre for Marine and Environmental Studies), Department of Biology, University of Aveiro, 3810-193 Aveiro, Portugal; (C.M.); (A.R.R.S.); (S.L.)
| | - Ana Rita R. Silva
- CESAM (Centre for Marine and Environmental Studies), Department of Biology, University of Aveiro, 3810-193 Aveiro, Portugal; (C.M.); (A.R.R.S.); (S.L.)
| | - Susana Loureiro
- CESAM (Centre for Marine and Environmental Studies), Department of Biology, University of Aveiro, 3810-193 Aveiro, Portugal; (C.M.); (A.R.R.S.); (S.L.)
| | - Isabel Henriques
- CEF (Center for Functional Ecology), Department of Life Sciences, Faculty of Sciences and Technology, University of Coimbra, 3000-456 Coimbra, Portugal;
- Correspondence: (I.H.); (M.N.G.-A.)
| | - M. Nazaret González-Alcaraz
- Department of Agricultural Engineering of the E.T.S.I.A. & Soil Ecology and Biotechnology Unit of the Institute of Plant Biotechnology, Technical University of Cartagena, 30203 Cartagena, Spain
- Correspondence: (I.H.); (M.N.G.-A.)
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5
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Söllinger A, Séneca J, Borg Dahl M, Motleleng LL, Prommer J, Verbruggen E, Sigurdsson BD, Janssens I, Peñuelas J, Urich T, Richter A, Tveit AT. Down-regulation of the bacterial protein biosynthesis machinery in response to weeks, years, and decades of soil warming. SCIENCE ADVANCES 2022; 8:eabm3230. [PMID: 35333567 PMCID: PMC8956259 DOI: 10.1126/sciadv.abm3230] [Citation(s) in RCA: 12] [Impact Index Per Article: 6.0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/10/2021] [Accepted: 02/03/2022] [Indexed: 05/26/2023]
Abstract
How soil microorganisms respond to global warming is key to infer future soil-climate feedbacks, yet poorly understood. Here, we applied metatranscriptomics to investigate microbial physiological responses to medium-term (8 years) and long-term (>50 years) subarctic grassland soil warming of +6°C. Besides indications for a community-wide up-regulation of centralmetabolic pathways and cell replication, we observed a down-regulation of the bacterial protein biosynthesis machinery in the warmed soils, coinciding with a lower microbial biomass, RNA, and soil substrate content. We conclude that permanently accelerated reaction rates at higher temperatures and reduced substrate concentrations result in cellular reduction of ribosomes, the macromolecular complexes carrying out protein biosynthesis. Later efforts to test this, including a short-term warming experiment (6 weeks, +6°C), further supported our conclusion. Down-regulating the protein biosynthesis machinery liberates energy and matter, allowing soil bacteria to maintain high metabolic activities and cell division rates even after decades of warming.
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Affiliation(s)
- Andrea Söllinger
- Department of Arctic and Marine Biology, UiT The Arctic University of Norway, Tromsø, Norway
| | - Joana Séneca
- Centre for Microbiology and Environmental Systems Science, University of Vienna, Vienna, Austria
| | - Mathilde Borg Dahl
- Institute of Microbiology, University of Greifswald, Greifswald, Germany
| | - Liabo L. Motleleng
- Department of Arctic and Marine Biology, UiT The Arctic University of Norway, Tromsø, Norway
| | - Judith Prommer
- Centre for Microbiology and Environmental Systems Science, University of Vienna, Vienna, Austria
| | | | | | | | - Josep Peñuelas
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Barcelona, Spain
- CREAF, Barcelona, Spain
| | - Tim Urich
- Institute of Microbiology, University of Greifswald, Greifswald, Germany
| | - Andreas Richter
- Centre for Microbiology and Environmental Systems Science, University of Vienna, Vienna, Austria
| | - Alexander T. Tveit
- Department of Arctic and Marine Biology, UiT The Arctic University of Norway, Tromsø, Norway
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6
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Moinet GYK, Dhami MK, Hunt JE, Podolyan A, Liáng LL, Schipper LA, Whitehead D, Nuñez J, Nascente A, Millard P. Soil microbial sensitivity to temperature remains unchanged despite community compositional shifts along geothermal gradients. GLOBAL CHANGE BIOLOGY 2021; 27:6217-6231. [PMID: 34585498 PMCID: PMC9293425 DOI: 10.1111/gcb.15878] [Citation(s) in RCA: 10] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/10/2021] [Accepted: 08/24/2021] [Indexed: 05/29/2023]
Abstract
Climate warming may be exacerbated if rising temperatures stimulate losses of soil carbon to the atmosphere. The direction and magnitude of this carbon-climate feedback are uncertain, largely due to lack of knowledge of the thermal adaptation of the physiology and composition of soil microbial communities. Here, we applied the macromolecular rate theory (MMRT) to describe the temperature response of the microbial decomposition of soil organic matter (SOM) in a natural long-term warming experiment in a geothermally active area in New Zealand. Our objective was to test whether microbial communities adapt to long-term warming with a shift in their composition and their temperature response that are consistent with evolutionary theory of trade-offs between enzyme structure and function. We characterized the microbial community composition (using metabarcoding) and the temperature response of microbial decomposition of SOM (using MMRT) of soils sampled along transects of increasing distance from a geothermally active zone comprising two biomes (a shrubland and a grassland) and sampled at two depths (0-50 and 50-100 mm), such that ambient soil temperature and soil carbon concentration varied widely and independently. We found that the different environments were hosting microbial communities with distinct compositions, with thermophile and thermotolerant genera increasing in relative abundance with increasing ambient temperature. However, the ambient temperature had no detectable influence on the MMRT parameters or the relative temperature sensitivity of decomposition (Q10 ). MMRT parameters were, however, strongly correlated with soil carbon concentration and carbon:nitrogen ratio. Our findings suggest that, while long-term warming selects for warm-adapted taxa, substrate quality and quantity exert a stronger influence than temperature in selecting for distinct thermal traits. The results have major implications for our understanding of the role of soil microbial processes in the long-term effects of climate warming on soil carbon dynamics and will help increase confidence in carbon-climate feedback projections.
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Affiliation(s)
- Gabriel Y. K. Moinet
- Soil Biology GroupWageningen University and ResearchWageningenThe Netherlands
- Manaaki Whenua – Landcare ResearchLincolnNew Zealand
| | | | - John E. Hunt
- Manaaki Whenua – Landcare ResearchLincolnNew Zealand
| | | | - Liyĭn L. Liáng
- Manaaki Whenua – Landcare ResearchPalmerston NorthNew Zealand
| | | | | | | | | | - Peter Millard
- Manaaki Whenua – Landcare ResearchLincolnNew Zealand
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7
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Yang S, Liebner S, Svenning MM, Tøsdal Tveit A. Decoupling of microbial community dynamics and functions in Arctic peat soil exposed to short term warming. Mol Ecol 2021; 30:5094-5104. [PMID: 34387003 DOI: 10.1111/mec.16118] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/13/2021] [Revised: 07/26/2021] [Accepted: 07/30/2021] [Indexed: 11/27/2022]
Abstract
Temperature is an important factor governing microbe-mediated carbon feedback from permafrost soils. The link between taxonomic and functional microbial responses to temperature change remains elusive due to the lack of studies assessing both aspects of microbial ecology. Our previous study reported microbial metabolic and trophic shifts in response to short-term temperature increases in Arctic peat soil, and linked these shifts to higher CH4 and CO2 production rates (Tveit et al., 2015). Here, we studied the taxonomic composition and functional potential of samples from the same experiment. We see that along a high-resolution temperature gradient (1 - 30 °C), microbial communities change discretely, but not continuously or stochastically, in response to rising temperatures. The taxonomic variability may thus in part reflect the varied temperature responses of individual taxa and the competition between these taxa for resources. These taxonomic responses contrast the stable functional potential (metagenomics-based) across all temperatures or the previously observed metabolic or trophic shifts at key temperatures. Furthermore, with rising temperatures we observed a progressive decrease in species diversity (Shannon Index) and increased dispersion of greenhouse gas (GHG) production rates. We conclude that the taxonomic variation is decoupled from both the functional potential of the community and the previously observed temperature-dependent changes in microbial function. However, the reduced diversity at higher temperatures might help explain the higher variability in GHG production at higher temperatures.
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Affiliation(s)
- Sizhong Yang
- GFZ German Research Center for Geosciences, Section Geomicrobiology, Telegrafenberg, 14473, Potsdam, Germany.,Cyrosphere Research Station on the Qinghai-Tibet Plateau, State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environmental and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China
| | - Susanne Liebner
- GFZ German Research Center for Geosciences, Section Geomicrobiology, Telegrafenberg, 14473, Potsdam, Germany.,Institute of Biochemistry and Biology, University of Potsdam, 14476, Potsdam, Germany
| | - Mette Marianne Svenning
- Department of Arctic and Marine Biology, UiT The Arctic University of Norway, 9037, Tromsø, Norway
| | - Alexander Tøsdal Tveit
- Department of Arctic and Marine Biology, UiT The Arctic University of Norway, 9037, Tromsø, Norway
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8
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Fang C, Ke W, Campioli M, Pei J, Yuan Z, Song X, Ye J, Li F, Janssens IA. Unaltered soil microbial community composition, but decreased metabolic activity in a semiarid grassland after two years of passive experimental warming. Ecol Evol 2020; 10:12327-12340. [PMID: 33209291 PMCID: PMC7664004 DOI: 10.1002/ece3.6862] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/14/2019] [Revised: 09/04/2020] [Accepted: 09/07/2020] [Indexed: 11/25/2022] Open
Abstract
Soil microbial communities regulate soil carbon feedbacks to climate warming through microbial respiration (i.e., metabolic rate). A thorough understanding of the responses of composition, biomass, and metabolic rate of soil microbial community to warming is crucial to predict soil carbon stocks in a future warmer climate. Therefore, we conducted a field manipulative experiment in a semiarid grassland on the Loess Plateau of China to evaluate the responses of the soil microbial community to increased temperature from April 2015 to December 2017. Soil temperature was 2.0°C higher relative to the ambient when open-top chambers (OTCs) were used. Warming did not affect microbial biomass or the composition of microbial functional groups. However, warming significantly decreased microbial respiration, directly resulting from soil pH decrease driven by the comediation of aboveground biomass increase, inorganic nitrogen increase, and moisture decrease. These findings highlight that the soil microbial community structure of semiarid grasslands resisted the short-term warming by 2°C, although its metabolic rate declined.
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Affiliation(s)
- Chao Fang
- Institute of EcologySchool of Applied MeteorologyNanjing University of Information Science and TechnologyNanjingChina
- State Key Laboratory of Grassland Agro‐ecosystemsInstitute of Arid AgroecologySchool of Life SciencesLanzhou UniversityLanzhouChina
- PLECO (Plants and Ecosystems)Department of BiologyUniversity of AntwerpWilrijkBelgium
| | - Wenbin Ke
- State Key Laboratory of Grassland Agro‐ecosystemsInstitute of Arid AgroecologySchool of Life SciencesLanzhou UniversityLanzhouChina
| | - Matteo Campioli
- PLECO (Plants and Ecosystems)Department of BiologyUniversity of AntwerpWilrijkBelgium
| | - Jiuying Pei
- State Key Laboratory of Grassland Agro‐ecosystemsInstitute of Arid AgroecologySchool of Life SciencesLanzhou UniversityLanzhouChina
| | - Ziqiang Yuan
- State Key Laboratory of Frozen Soil EngineeringNorthwest Institute of Eco‐Environment and ResourcesChinese Academy of ScienceLanzhouChina
| | - Xin Song
- State Key Laboratory of Grassland Agro‐ecosystemsInstitute of Arid AgroecologySchool of Life SciencesLanzhou UniversityLanzhouChina
| | - Jian‐Sheng Ye
- State Key Laboratory of Grassland Agro‐ecosystemsInstitute of Arid AgroecologySchool of Life SciencesLanzhou UniversityLanzhouChina
| | - Fengmin Li
- State Key Laboratory of Grassland Agro‐ecosystemsInstitute of Arid AgroecologySchool of Life SciencesLanzhou UniversityLanzhouChina
| | - Ivan A. Janssens
- PLECO (Plants and Ecosystems)Department of BiologyUniversity of AntwerpWilrijkBelgium
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9
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Newsham KK, Tripathi BM, Dong K, Yamamoto N, Adams JM, Hopkins DW. Bacterial Community Composition and Diversity Respond to Nutrient Amendment but Not Warming in a Maritime Antarctic Soil. MICROBIAL ECOLOGY 2019; 78:974-984. [PMID: 30989354 DOI: 10.1007/s00248-019-01373-z] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/16/2018] [Accepted: 03/22/2019] [Indexed: 06/09/2023]
Abstract
A resumption of climate warming in maritime Antarctica, arising from continued greenhouse gas emissions to the atmosphere, is predicted to lead to further expansions of plant populations across the region, with consequent increases in nutrient inputs to soils. Here, we test the main and interactive effects of warming, applied with open top chambers (OTCs), and nutrient amendment with tryptic soy broth (TSB), an artificial growth substrate, on bacterial community composition and diversity using Illumina sequencing of 16S rRNA genes in soil from a field experiment in the southern maritime Antarctic. Substantial effects of TSB application on bacterial communities were identified after 49 months, including reduced diversity, altered phylogenetic community assembly processes, increased Proteobacteria-to-Acidobacteria ratios and significant divergence in community composition, notably increases in the relative abundances of the gram-positive genera Arthrobacter, Paeniglutamicibacter and Planococcus. Contrary to previous observations from other maritime Antarctic field warming experiments, we recorded no effects of warming with OTCs, or interactive effects of OTCs and TSB application, on bacterial community composition or diversity. Based on these findings, we conclude that further warming of the maritime Antarctic is unlikely to influence soil bacterial community composition or diversity directly, but that increased nutrient inputs arising from enhanced plant growth across the region may affect the composition of soil bacterial communities, with possible effects on ecosystem productivity.
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Affiliation(s)
- Kevin K Newsham
- NERC British Antarctic Survey, Madingley Road, Cambridge, CB3 0ET, UK.
| | - Binu M Tripathi
- Korea Polar Research Institute, Incheon, 21990, Republic of Korea
| | - Ke Dong
- Department of Life Science, College of Natural Sciences, Kyonggi University, Suwon, Gyeonggi-do, 16227, Republic of Korea
| | - Naomichi Yamamoto
- Department of Environmental Health Sciences, Seoul National University, 1 Gwanak-ro, Gwanak-gu, Seoul, 08826, Republic of Korea
| | - Jonathan M Adams
- Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China
| | - David W Hopkins
- Scotland's Rural College, Peter Wilson Building, West Mains Road, Edinburgh, EH9 3JG, UK
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10
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Walker TWN, Kaiser C, Strasser F, Herbold CW, Leblans NIW, Woebken D, Janssens IA, Sigurdsson BD, Richter A. Microbial temperature sensitivity and biomass change explain soil carbon loss with warming. NATURE CLIMATE CHANGE 2018; 8:885-889. [PMID: 30288176 PMCID: PMC6166784 DOI: 10.1038/s41558-018-0259-x] [Citation(s) in RCA: 108] [Impact Index Per Article: 18.0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/20/2017] [Accepted: 07/19/2018] [Indexed: 05/25/2023]
Abstract
Soil microorganisms control carbon losses from soils to the atmosphere1-3, yet their responses to climate warming are often short-lived and unpredictable4-7. Two mechanisms, microbial acclimation and substrate depletion, have been proposed to explain temporary warming effects on soil microbial activity8-10. However, empirical support for either mechanism is unconvincing. Here we used geothermal temperature gradients (> 50 years of field warming)11 and a short-term experiment to show that microbial activity (gross rates of growth, turnover, respiration and carbon uptake) is intrinsically temperature sensitive and does not acclimate to warming (+ 6 ºC) over weeks or decades. Permanently accelerated microbial activity caused carbon loss from soil. However, soil carbon loss was temporary because substrate depletion reduced microbial biomass and constrained the influence of microbes over the ecosystem. A microbial biogeochemical model12-14 showed that these observations are reproducible through a modest, but permanent, acceleration in microbial physiology. These findings reveal a mechanism by which intrinsic microbial temperature sensitivity and substrate depletion together dictate warming effects on soil carbon loss via their control over microbial biomass. We thus provide a framework for interpreting the links between temperature, microbial activity and soil carbon loss on timescales relevant to Earth's climate system.
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Affiliation(s)
- Tom W. N. Walker
- Department of Microbiology & Ecosystem Science, Division of Terrestrial Ecosystem Research, University of Vienna, 1090 Vienna, Austria
- Department of Ecology & Evolution, Université de Lausanne, CH-1015, Switzerland
| | - Christina Kaiser
- Department of Microbiology & Ecosystem Science, Division of Terrestrial Ecosystem Research, University of Vienna, 1090 Vienna, Austria
- Institute of Applied Systems Analysis, 2361 Laxenburg, Austria
| | - Florian Strasser
- Department of Microbiology & Ecosystem Science, Division of Microbial Ecology, University of Vienna, 1090 Vienna, Austria
| | - Craig W. Herbold
- Department of Microbiology & Ecosystem Science, Division of Microbial Ecology, University of Vienna, 1090 Vienna, Austria
| | - Niki I. W. Leblans
- Department of Biology, University of Antwerp, 2610 Wilrijk, Antwerp, Belgium
- Agricultural University of Iceland, Hvanneyri, 311 Borgarnes, Iceland
| | - Dagmar Woebken
- Department of Microbiology & Ecosystem Science, Division of Microbial Ecology, University of Vienna, 1090 Vienna, Austria
| | - Ivan A. Janssens
- Department of Biology, University of Antwerp, 2610 Wilrijk, Antwerp, Belgium
| | | | - Andreas Richter
- Department of Microbiology & Ecosystem Science, Division of Terrestrial Ecosystem Research, University of Vienna, 1090 Vienna, Austria
- Institute of Applied Systems Analysis, 2361 Laxenburg, Austria
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11
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Holmstrup M, Ehlers BK, Slotsbo S, Ilieva‐Makulec K, Sigurdsson BD, Leblans NIW, Ellers J, Berg MP. Functional diversity of Collembola is reduced in soils subjected to short‐term, but not long‐term, geothermal warming. Funct Ecol 2018. [DOI: 10.1111/1365-2435.13058] [Citation(s) in RCA: 12] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/20/2023]
Affiliation(s)
- Martin Holmstrup
- Department of BioscienceAarhus University Silkeborg Denmark
- Aarhus Institute of Advanced StudiesAarhus University Aarhus C Denmark
| | | | - Stine Slotsbo
- Department of BioscienceAarhus University Silkeborg Denmark
| | | | | | - Niki I. W. Leblans
- Agricultural University of Iceland Borgarnes Iceland
- University of AntwerpDepartment of Biology Wilrijk Belgium
| | - Jacintha Ellers
- Department of Ecological ScienceAnimal Ecology GroupVrije Universiteit Amsterdam The Netherlands
| | - Matty P. Berg
- Department of Ecological ScienceAnimal Ecology GroupVrije Universiteit Amsterdam The Netherlands
- Groningen Institute of Evolutionary Life ScienceCommunity and Conservation Ecology GroupUniversity of Groningen Groningen The Netherlands
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