1
|
Mafra D, Borges NA, Baptista BG, Martins LF, Borland G, Shiels PG, Stenvinkel P. What Can the Gut Microbiota of Animals Teach Us about the Relationship between Nutrition and Burden of Lifestyle Diseases? Nutrients 2024; 16:1789. [PMID: 38892721 PMCID: PMC11174762 DOI: 10.3390/nu16111789] [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: 05/16/2024] [Revised: 05/31/2024] [Accepted: 06/03/2024] [Indexed: 06/21/2024] Open
Abstract
The gut microbiota performs several crucial roles in a holobiont with its host, including immune regulation, nutrient absorption, synthesis, and defense against external pathogens, significantly influencing host physiology. Disruption of the gut microbiota has been linked to various chronic conditions, including cardiovascular, kidney, liver, respiratory, and intestinal diseases. Studying how animals adapt their gut microbiota across their life course at different life stages and under the dynamics of extreme environmental conditions can provide valuable insights from the natural world into how the microbiota modulates host biology, with a view to translating these into treatments or preventative measures for human diseases. By modulating the gut microbiota, opportunities to address many complications associated with chronic diseases appear. Such a biomimetic approach holds promise for exploring new strategies in healthcare and disease management.
Collapse
Affiliation(s)
- Denise Mafra
- Graduate Program in Medical Sciences and Graduate Program in Nutrition Sciences, Federal Fluminense University (UFF), Niterói 24020-141, Brazil;
- Graduate Program in Biological Sciences—Physiology, Federal University of Rio de Janeiro (UFRJ), Rio de Janeiro 21941-909, Brazil
| | - Natália A. Borges
- Graduate Program in Food, Nutrition, and Health, Institute of Nutrition, State University of Rio de Janeiro (UERJ), Rio de Janeiro 21941-909, Brazil;
| | - Beatriz G. Baptista
- Graduate Program in Medical Sciences and Graduate Program in Nutrition Sciences, Federal Fluminense University (UFF), Niterói 24020-141, Brazil;
| | - Layla F. Martins
- Department of Biochemistry, Institute of Chemistry, University of São Paulo (USP), São Paulo 05508-220, Brazil;
| | - Gillian Borland
- School of Molecular Biosciences, University of Glasgow, Glasgow G12 8QQ, UK; (G.B.); (P.G.S.)
| | - Paul G. Shiels
- School of Molecular Biosciences, University of Glasgow, Glasgow G12 8QQ, UK; (G.B.); (P.G.S.)
| | - Peter Stenvinkel
- Division of Renal Medicine, Department of Clinical Science, Technology and Intervention, Karolinska Institutet, 17165 Stockholm, Sweden;
| |
Collapse
|
2
|
Ren Z, Ye S, Li H, Huang X, Chen L, Cao S, Chen T. Biological Interactions and Environmental Influences Shift Microeukaryotes in Permafrost Active Layer Soil Across the Qinghai-Tibet Plateau. MICROBIAL ECOLOGY 2023; 86:2756-2769. [PMID: 37542537 DOI: 10.1007/s00248-023-02280-0] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/26/2023] [Accepted: 07/27/2023] [Indexed: 08/07/2023]
Abstract
Permafrost active layer soils are harsh environments with thaw/freeze cycles and sub-zero temperatures, harboring diverse microorganisms. However, the distribution patterns, assembly mechanism, and driving forces of soil microeukaryotes in permafrost remain largely unknown. In this study, we investigated microeukaryotes in permafrost active layer across the Qinghai-Tibet Plateau (QTP) using 18S rRNA gene sequencing. The results showed that the microbial eukaryotic communities were dominated by Nematozoa, Ciliophora, Ascomycota, Cercozoa, Arthropoda, and Basidiomycota in terms of relative abundance and operational taxonomic unit (OTU) richness. Nematozoa had the highest relative abundance, while Ciliophora had the highest OTU richness. These phyla had strong interactions between each other. Their alpha diversity and community structure were differently influenced by the factors associated to location, climate, and soil properties, particularly the soil properties. Significant but weak distance-decay relationships with different slopes were established for the communities of these dominant phyla, except for Basidiomycota. According to the null model, community assemblies of Nematozoa and Cercozoa were dominated by heterogeneous selection, Ciliophora and Ascomycota were dominated by dispersal limitation, while Arthropoda and Basidiomycota were highly dominated by non-dominant processes. The assembly mechanisms can be jointly explained by biotic interactions, organism treats, and environmental influences. Modules in the co-occurrence network of the microeukaryotes were composed by members from different taxonomic groups. These modules also had interactions and responded to different environmental factors, within which, soil properties had strong influences on these modules. The results suggested the importance of biological interactions and soil properties in structuring microbial eukaryotic communities in permafrost active layer soil across the QTP.
Collapse
Affiliation(s)
- Ze Ren
- State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, 73 Beijing East Road, Nanjing, 210008, China.
- Advanced Institute of Natural Sciences, Beijing Normal University, Zhuhai, 519087, China.
| | - Shudan Ye
- Faculty of Arts and Sciences, Beijing Normal University, Zhuhai, 519087, China
| | - Hongxuan Li
- Faculty of Arts and Sciences, Beijing Normal University, Zhuhai, 519087, China
| | - Xilei Huang
- Faculty of Arts and Sciences, Beijing Normal University, Zhuhai, 519087, China
| | - Luyao Chen
- Faculty of Arts and Sciences, Beijing Normal University, Zhuhai, 519087, China
| | - Shengkui Cao
- School of Geographical Science, Qinghai Normal University, Xining, 810008, China
| | - Tao Chen
- Center for Grassland Microbiome, State Key Laboratory of Grassland Agro-ecosystems, Lanzhou University, 768 Jiayuguan W Road, Lanzhou, 730020, China.
| |
Collapse
|
3
|
Simister RL, Iulianella Phillips BP, Wickham AP, Cayer EM, Hart CJR, Winterburn PA, Crowe SA. DNA sequencing, microbial indicators, and the discovery of buried kimberlites. COMMUNICATIONS EARTH & ENVIRONMENT 2023; 4:387. [PMID: 38665197 PMCID: PMC11041713 DOI: 10.1038/s43247-023-01020-z] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 02/19/2023] [Accepted: 09/19/2023] [Indexed: 04/28/2024]
Abstract
Population growth and technological advancements are placing growing demand on mineral resources. New and innovative exploration technologies that improve detection of deeply buried mineralization and host rocks are required to meet these demands. Here we used diamondiferous kimberlite ore bodies as a test case and show that DNA amplicon sequencing of soil microbial communities resolves anomalies in microbial community composition and structure that reflect the surface expression of kimberlites buried under 10 s of meters of overburden. Indicator species derived from laboratory amendment experiments were employed in an exploration survey in which the species distributions effectively delineated the surface expression of buried kimberlites. Additional indicator species derived directly from field observations improved the blind discovery of kimberlites buried beneath similar overburden types. Application of DNA sequence-based analyses of soil microbial communities to mineral deposit exploration provides a powerful illustration of how genomics technologies can be leveraged in the discovery of critical new resources.
Collapse
Affiliation(s)
- Rachel L. Simister
- Department of Microbiology & Immunology, University of British Columbia, Vancouver, BC V6T 1Z3 Canada
- Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T 1Z4 Canada
| | - Bianca P. Iulianella Phillips
- Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T 1Z4 Canada
- MDRU-Mineral Deposit Research Unit, Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T 1Z4 Canada
| | - Andrew P. Wickham
- Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T 1Z4 Canada
- MDRU-Mineral Deposit Research Unit, Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T 1Z4 Canada
| | - Erika M. Cayer
- Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T 1Z4 Canada
- MDRU-Mineral Deposit Research Unit, Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T 1Z4 Canada
| | - Craig J. R. Hart
- Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T 1Z4 Canada
- MDRU-Mineral Deposit Research Unit, Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T 1Z4 Canada
| | - Peter A. Winterburn
- Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T 1Z4 Canada
- MDRU-Mineral Deposit Research Unit, Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T 1Z4 Canada
| | - Sean A. Crowe
- Department of Microbiology & Immunology, University of British Columbia, Vancouver, BC V6T 1Z3 Canada
- Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, BC V6T 1Z4 Canada
| |
Collapse
|
4
|
Tang X, Zhang M, Fang Z, Yang Q, Zhang W, Zhou J, Zhao B, Fan T, Wang C, Zhang C, Xia Y, Zheng Y. Changing microbiome community structure and functional potential during permafrost thawing on the Tibetan Plateau. FEMS Microbiol Ecol 2023; 99:fiad117. [PMID: 37766397 DOI: 10.1093/femsec/fiad117] [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: 11/21/2022] [Revised: 09/13/2023] [Accepted: 09/27/2023] [Indexed: 09/29/2023] Open
Abstract
Large amounts of carbon sequestered in permafrost on the Tibetan Plateau (TP) are becoming vulnerable to microbial decomposition in a warming world. However, knowledge about how the responsible microbial community responds to warming-induced permafrost thaw on the TP is still limited. This study aimed to conduct a comprehensive comparison of the microbial communities and their functional potential in the active layer of thawing permafrost on the TP. We found that the microbial communities were diverse and varied across soil profiles. The microbial diversity declined and the relative abundance of Chloroflexi, Bacteroidetes, Euryarchaeota, and Bathyarchaeota significantly increased with permafrost thawing. Moreover, warming reduced the similarity and stability of active layer microbial communities. The high-throughput qPCR results showed that the abundance of functional genes involved in liable carbon degradation and methanogenesis increased with permafrost thawing. Notably, the significantly increased mcrA gene abundance and the higher methanogens to methanotrophs ratio implied enhanced methanogenic activities during permafrost thawing. Overall, the composition and functional potentials of the active layer microbial community in the Tibetan permafrost region are susceptible to warming. These changes in the responsible microbial community may accelerate carbon degradation, particularly in the methane releases from alpine permafrost ecosystems on the TP.
Collapse
Affiliation(s)
- Xiaotong Tang
- State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an, Shaanxi 710069, China
| | - Miao Zhang
- School of Environmental Science and Engineering, College of Engineering, Southern University of Science and Technology, Shenzhen, Guangdong 518055, China
| | - Zhengkun Fang
- State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an, Shaanxi 710069, China
| | - Qing Yang
- School of Environmental Science and Engineering, College of Engineering, Southern University of Science and Technology, Shenzhen, Guangdong 518055, China
| | - Wan Zhang
- Shenzhen Key Laboratory of Marine Archaea Geo-Omics, Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, Guangdong 518055, China
| | - Jiaxing Zhou
- State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an, Shaanxi 710069, China
| | - Bixi Zhao
- School of Environmental Science and Engineering, College of Engineering, Southern University of Science and Technology, Shenzhen, Guangdong 518055, China
| | - Tongyu Fan
- State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an, Shaanxi 710069, China
| | - Congzhen Wang
- State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an, Shaanxi 710069, China
| | - Chuanlun Zhang
- Shenzhen Key Laboratory of Marine Archaea Geo-Omics, Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, Guangdong 518055, China
| | - Yu Xia
- School of Environmental Science and Engineering, College of Engineering, Southern University of Science and Technology, Shenzhen, Guangdong 518055, China
| | - Yanhong Zheng
- State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an, Shaanxi 710069, China
| |
Collapse
|
5
|
Han S, Lucas-Borja ME, Chen W, Huang Q. Soil glomalin-related protein affects aggregate N 2O fluxes by modulating denitrifier communities in a fertilized soil. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 880:163147. [PMID: 37023815 DOI: 10.1016/j.scitotenv.2023.163147] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/18/2023] [Revised: 03/19/2023] [Accepted: 03/25/2023] [Indexed: 05/27/2023]
Abstract
Agricultural ecosystems contribute significantly to atmospheric emissions of soil nitrous oxide (N2O), which exacerbate environmental pollution and contribute to global warming. Glomalin-related soil protein (GRSP) stabilizes soil aggregates and enhances soil carbon and nitrogen storage in agricultural ecosystems. However, the underlying mechanisms and relative importance of GRSP on N2O fluxes within soil aggregate fraction remain largely unclear. We examined the GRSP content, denitrifying bacterial community composition, and potential N2O fluxes across three aggregate-size fractions (2000-250 μm, 250-53 μm, and <53 μm) under a long-term fertilization agricultural ecosystem, subjected to mineral fertilizer or manure and their combination. Our findings indicated that various fertilization treatments have no discernible impact on the size distribution of soil aggregates, paving the way to further research into the impact of soil aggregates on GRSP content, the denitrifying bacterial community composition, and potential N2O fluxes. GRSP content increased with the increase in soil aggregate size. Potential N2O fluxes (including gross N2O production and N2O reduction and net N2O production) among aggregates were highest in microaggregates (250-53 μm), followed by macroaggregates (2000-250 μm) and lowest in silt + clay (<53 μm) fractions. Potential N2O fluxes had a positive response to soil aggregate GRSP fractions. The non-metric multidimensional scaling analysis revealed that soil aggregate size could drive the denitrifying functional microbial community composition, and deterministic processes play more critical roles than stochasticity processes in driving denitrifying functional composition under soil aggregate fractions. Procrustes analysis revealed a significant correlation between denitrifying microbial community, soil aggregate GRSP fractions, and potential N2O fluxes. Our study suggests that soil aggregate GRSP fractions influence potential nitrous oxide fluxes by affecting denitrifying microbial functional composition within soil aggregate.
Collapse
Affiliation(s)
- Shun Han
- State Key Laboratory of Agricultural Microbiology, Huazhong Agricultural University, Wuhan, China
| | - Manuel Esteban Lucas-Borja
- Escuela Técnica Superior Ingenieros Agrónomos y Montes, Universidad de Castilla-La Mancha, Campus Universitario, E-02071 Albacete, Spain
| | - Wenli Chen
- State Key Laboratory of Agricultural Microbiology, Huazhong Agricultural University, Wuhan, China.
| | - Qiaoyun Huang
- State Key Laboratory of Agricultural Microbiology, Huazhong Agricultural University, Wuhan, China; Key Laboratory of Arable Land Conservation (Middle and Lower Reaches of Yangtze River), Ministry of Agriculture, College of Resources and Environment, Huazhong Agricultural University, Wuhan, China
| |
Collapse
|
6
|
Coluccia M, Besaury L. Acidobacteria members harbour an abundant and diverse carbohydrate-active enzymes (cazyme) and secreted proteasome repertoire, key factors for potential efficient biomass degradation. Mol Genet Genomics 2023:10.1007/s00438-023-02045-x. [PMID: 37335345 DOI: 10.1007/s00438-023-02045-x] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/05/2022] [Accepted: 06/05/2023] [Indexed: 06/21/2023]
Abstract
The Acidobacteria phylum is a very abundant group (20-30% of microbial communities in soil ecosystems); however, little is known about these microorganisms and their ability to degrade the biomass and lignocellulose due to the difficulty of culturing them. We, therefore, bioinformatically studied the content of lignocellulolytic enzymes (total and predicted secreted enzymes) and secreted peptidases in an in silico library containing 41 Acidobacteria genomes. The results showed a high abundance and diversity of total and secreted Carbohydrate-Active enzymes (cazyme) families among the Acidobacteria compared to known previous degraders. Indeed, the relative abundance of cazymes in some genomes represented more than 6% of the gene coding proteins with at least 300 cazymes. The same observation was made with the predicted secreted peptidases with several families of secreted peptidases, which represented at least 1.5% of the gene coding proteins in several genomes. These results allowed us to highlight the lignocellulolytic potential of the Acidobacteria phylum in the degradation of lignocellulosic biomass, which could explain its high abundance in the environment.
Collapse
Affiliation(s)
- Marion Coluccia
- Université de Reims Champagne Ardenne, INRAE, FARE, UMR A 614, Chaire AFERE, 51097, Reims, France
| | - Ludovic Besaury
- Université de Reims Champagne Ardenne, INRAE, FARE, UMR A 614, Chaire AFERE, 51097, Reims, France.
| |
Collapse
|
7
|
Xiang D, Wang G, Tian J, Li W. Global patterns and edaphic-climatic controls of soil carbon decomposition kinetics predicted from incubation experiments. Nat Commun 2023; 14:2171. [PMID: 37061518 PMCID: PMC10105724 DOI: 10.1038/s41467-023-37900-3] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/06/2022] [Accepted: 04/03/2023] [Indexed: 04/17/2023] Open
Abstract
Knowledge about global patterns of the decomposition kinetics of distinct soil organic matter (SOM) pools is crucial to robust estimates of land-atmosphere carbon fluxes under climate change. However, the current Earth system models often adopt globally-consistent reference SOM decomposition rates (kref), ignoring effects from edaphic-climate heterogeneity. Here, we compile a comprehensive set of edaphic-climatic and SOM decomposition data from published incubation experiments and employ machine-learning techniques to develop models capable of predicting the expected sizes and kref of multiple SOM pools (fast, slow, and passive). We show that soil texture dominates the turnover of the fast pools, whereas pH predominantly regulates passive SOM decomposition. This suggests that pH-sensitive bacterial decomposers might have larger effects on stable SOM decomposition than previously believed. Using these predictive models, we provide a 1-km resolution global-scale dataset of the sizes and kref of these SOM pools, which may improve global biogeochemical model parameterization and predictions.
Collapse
Affiliation(s)
- Daifeng Xiang
- State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan, 430072, China
- Institute for Water-Carbon Cycles and Carbon Neutrality, School of Water Resources and Hydropower Engineering, Wuhan University, Wuhan, 430072, China
| | - Gangsheng Wang
- State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan, 430072, China.
- Institute for Water-Carbon Cycles and Carbon Neutrality, School of Water Resources and Hydropower Engineering, Wuhan University, Wuhan, 430072, China.
| | - Jing Tian
- State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan, 430072, China
- Institute for Water-Carbon Cycles and Carbon Neutrality, School of Water Resources and Hydropower Engineering, Wuhan University, Wuhan, 430072, China
| | - Wanyu Li
- State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan, 430072, China
- Institute for Water-Carbon Cycles and Carbon Neutrality, School of Water Resources and Hydropower Engineering, Wuhan University, Wuhan, 430072, China
| |
Collapse
|
8
|
Mishra A, Singh L, Singh D. Unboxing the black box-one step forward to understand the soil microbiome: A systematic review. MICROBIAL ECOLOGY 2023; 85:669-683. [PMID: 35112151 PMCID: PMC9957845 DOI: 10.1007/s00248-022-01962-5] [Citation(s) in RCA: 9] [Impact Index Per Article: 9.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 11/03/2021] [Accepted: 01/10/2022] [Indexed: 06/14/2023]
Abstract
Soil is one of the most important assets of the planet Earth, responsible for maintaining the biodiversity and managing the ecosystem services for both managed and natural ecosystems. It encompasses large proportion of microscopic biodiversity, including prokaryotes and the microscopic eukaryotes. Soil microbiome is critical in managing the soil functions, but their activities have diminutive recognition in few systems like desert land and forest ecosystems. Soil microbiome is highly dependent on abiotic and biotic factors like pH, carbon content, soil structure, texture, and vegetation, but it can notably vary with ecosystems and the respective inhabitants. Thus, unboxing this black box is essential to comprehend the basic components adding to the soil systems and supported ecosystem services. Recent advancements in the field of molecular microbial ecology have delivered commanding tools to examine this genetic trove of soil biodiversity. Objective of this review is to provide a critical evaluation of the work on the soil microbiome, especially since the advent of the NGS techniques. The review also focuses on advances in our understanding of soil communities, their interactions, and functional capabilities along with understanding their role in maneuvering the biogeochemical cycle while underlining and tapping the unprecedented metagenomics data to infer the ecological attributes of yet undiscovered soil microbiome. This review focuses key research directions that could shape the future of basic and applied research into the soil microbiome. This review has led us to understand that it is difficult to generalize that soil microbiome plays a substantiated role in shaping the soil networks and it is indeed a vital resource for sustaining the ecosystem functioning. Exploring soil microbiome will help in unlocking their roles in various soil network. It could be resourceful in exploring and forecasting its impacts on soil systems and for dealing with alleviating problems like rapid climate change.
Collapse
Affiliation(s)
- Apurva Mishra
- Academy of Scientific and Innovative Research [AcSIR], Ghaziabad, 201002, India
- Environmental Biotechnology and Genomics Division, , CSIR-National Environmental Engineering Research Institute, Nehru Marg, Nagpur, 440020, Maharashtra, India
| | - Lal Singh
- Environmental Biotechnology and Genomics Division, , CSIR-National Environmental Engineering Research Institute, Nehru Marg, Nagpur, 440020, Maharashtra, India
| | - Dharmesh Singh
- Institute for Medical Microbiology, Immunology and Hygiene, Technical University of Munich, Trogerstrasse 30, 81675, Munich, Bavaria, Germany.
| |
Collapse
|
9
|
Yang Y, Cheng S, Fang H, Guo Y, Li Y, Zhou Y, Shi F, Vancampenhout K. Linkages between the molecular composition of dissolved organic matter and soil microbial community in a boreal forest during freeze-thaw cycles. Front Microbiol 2023; 13:1012512. [PMID: 36699583 PMCID: PMC9868181 DOI: 10.3389/fmicb.2022.1012512] [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: 08/05/2022] [Accepted: 12/19/2022] [Indexed: 01/11/2023] Open
Abstract
Soil dissolved organic matter (DOM) plays a vital role in biogeochemical processes. Global warming leads to increased freeze-thaw cycles (FTCs) in boreal forest soils, which can change DOM production and consumption. However, the interactions between the chemical composition of DOM molecules and the microbial communities that drive C decomposition in the context of freeze-thaw are poorly understood. Here, a FTCs incubation experiment was conducted. Combined with pyrolysis gas chromatography-mass spectrometry and high-throughput sequencing techniques, the relationships between DOM chemodiversity and microbial community structure were assessed. Results indicated that both low-frequency (2FTCs) and high-frequency freeze-thaw cycles (6FTCs) significantly increased soil dissolved organic carbon (DOC) contents in the surface (0-10 cm) and subsurface (50-60 cm) soil layers. In the topsoil, FTCs significantly reduced the relative abundance of aromatic compounds, but increased the relative proportions of alkanes, phenols, fatty acid methyl esters (Me) and polysaccharides in the DOM. In the subsuface soil layer, only the relative abundance of Me in the 6FTCs treatment increased significantly. The response of bacterial communities to FTCs was more sensitive than that of fungi, among which only the relative abundance of Gammaproteobacteria increased by FTCs. Moreover, the relative abundance of these taxa was positively correlated with the increment of DOC. Co-occurrence networks confirmed DOM-bacterial interactions, implying that specific microorganisms degrade specific substrates. At class level, Gammaproteobacteria were significantly positively correlated with labile C (polysaccharides and alkanes), whereas other bacterial classes such as Actinobacteria, Alphaproteobacteria, and Thermoleophilia were significantly positively correlated with aromatic compounds in the topsoil. Collectively, FTCs tended to activate DOM and enhance its biodegradability of DOM, potentially hampering DOC accumulation and C sequestration. These findings highlight the potential of DOM molecular mechanisms to regulate the functional states of soil bacterial communities under increased FTCs.
Collapse
Affiliation(s)
- Yan Yang
- Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China,College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China
| | - Shulan Cheng
- College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China,Shulan Cheng,
| | - Huajun Fang
- Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China,College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China,Northwest Plateau Institute of Biology, Chinese Academy of Sciences, Xining, China,The Zhongke-Ji’an Institute for Eco-Environmental Sciences, Ji’an, China,*Correspondence: Huajun Fang,
| | - Yifan Guo
- Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China
| | - Yuna Li
- College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China
| | - Yi Zhou
- College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China
| | - Fangying Shi
- Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China
| | - Karen Vancampenhout
- Division of Forest, Nature and Landscape, Department of Earth and Environmental Sciences, Faculty of Sciences, KU Leuven, Leuven, Belgium
| |
Collapse
|
10
|
Ren Z, Cao S, Chen T, Zhang C, Yu J. Bacterial functional redundancy and carbon metabolism potentials in soil, sediment, and water of thermokarst landscapes across the Qinghai-Tibet Plateau: Implications for the fate of permafrost carbon. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 852:158340. [PMID: 36041614 DOI: 10.1016/j.scitotenv.2022.158340] [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: 07/10/2022] [Revised: 08/23/2022] [Accepted: 08/23/2022] [Indexed: 06/15/2023]
Abstract
Permafrost thaw create widespread thermokarst landscapes. As a result, distinct habitats are provided to harbor different bacterial communities in degraded permafrost soil (PBCs), thermokarst lake sediment (SBCs), and lake water (WBCs), driving carbon metabolism differentially. In this study, we investigated functional diversity and redundancy, and carbon metabolism potentials of PBCs, SBCs, and WBCs in thermokarst landscapes across the Qinghai-Tibet Plateau. The results showed that PBCs and SBCs had higher taxonomic and functional alpha diversity than WBCs, while WBCs had lower functional redundancy. WBCs had the highest beta diversity followed by SBCs and PBCs, suggesting strong determination of taxonomic variations on functional differences. Community assembly processes also had significant influences on beta diversity, especially for SBCs. Metabolism pathways of carbohydrate metabolism, methane metabolism, and carbon fixation were enriched differentially in PBCs, SBCs, and WBCs, suggesting different C fate in distinct habitats. Carbohydrate metabolism data suggested that PBCs might have stronger potentials to mineralize a greater diversity of organic carbon substrate than SBCs and WBCs, promoting degradation of organic carbon stocks in degraded permafrost soils. Methane metabolism data showed that SBCs had a stronger methanogenesis potential followed by PBCs and WBCs, while PBCs had a stronger methane oxidation potential. High abundance of genes involving in formaldehyde assimilation might suggested that a large proportion of produced methane might be assimilated by methanotrophs in the thermokarst landscapes. Both aerobic and anaerobic carbon fixation pathways were enriched in PBCs. The results added our understanding of functional properties and biogeochemical carbon cycles in thermokarst landscapes, improving our abilities in accurate modeling of carbon dynamics and the ultimate fate of permafrost carbon in a warming world.
Collapse
Affiliation(s)
- Ze Ren
- Research and Development Center for Watershed Environmental Eco-Engineering, Advanced Institute of Natural Sciences, Beijing Normal University, Zhuhai 519087, China; School of Environment, Beijing Normal University, Beijing 100875, China.
| | - Shengkui Cao
- School of Geographical Science, Qinghai Normal University, Xining 810008, China.
| | - Tao Chen
- Center for Grassland Microbiome, State Key Laboratory of Grassland Agro-ecosystems, Lanzhou University, Lanzhou 730020, China
| | - Cheng Zhang
- Research and Development Center for Watershed Environmental Eco-Engineering, Advanced Institute of Natural Sciences, Beijing Normal University, Zhuhai 519087, China; School of Engineering Technology, Beijing Normal University, Zhuhai 519087, China
| | - Jinlei Yu
- Key Laboratory of Geographic Information Science, Ministry of Education, East China Normal University, Shanghai 200241, China
| |
Collapse
|
11
|
Zeng XM, Feng J, Chen J, Delgado-Baquerizo M, Zhang Q, Zhou XQ, Yuan Y, Feng S, Zhang K, Liu YR, Huang Q. Microbial assemblies associated with temperature sensitivity of soil respiration along an altitudinal gradient. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 820:153257. [PMID: 35065115 DOI: 10.1016/j.scitotenv.2022.153257] [Citation(s) in RCA: 4] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/04/2021] [Revised: 01/14/2022] [Accepted: 01/15/2022] [Indexed: 06/14/2023]
Abstract
Identifying the drivers of the response of soil microbial respiration to warming is integral to accurately forecasting the carbon-climate feedbacks in terrestrial ecosystems. Microorganisms are the fundamental drivers of soil microbial respiration and its response to warming; however, the specific microbial communities and properties involved in the process remain largely undetermined. Here, we identified the associations between microbial community and temperature sensitivity (Q10) of soil microbial respiration in alpine forests along an altitudinal gradient (from 2974 to 3558 m) from the climate-sensitive Tibetan Plateau. Our results showed that changes in microbial community composition accounted for more variations of Q10 values than a wide range of other factors, including soil pH, moisture, substrate quantity and quality, microbial biomass, diversity and enzyme activities. Specifically, co-occurring microbial assemblies (i.e., ecological clusters or modules) targeting labile carbon consumption were negatively correlated with Q10 of soil microbial respiration, whereas microbial assemblies associated with recalcitrant carbon decomposition were positively correlated with Q10 of soil microbial respiration. Furthermore, there were progressive shifts of microbial assemblies from labile to recalcitrant carbon consumption along the altitudinal gradient, supporting relatively high Q10 values in high-altitude regions. Our results provide new insights into the link between changes in major microbial assemblies with different trophic strategies and Q10 of soil microbial respiration along an altitudinal gradient, highlighting that warming could have stronger effects on microbially-mediated soil organic matter decomposition in high-altitude regions than previously thought.
Collapse
Affiliation(s)
- Xiao-Min Zeng
- State Key Laboratory of Agricultural Microbiology, Huazhong Agricultural University, Wuhan 430070, China; College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, China; State Environmental Protection Key Laboratory of Soil Health and Green Remediation, Wuhan 430070, China
| | - Jiao Feng
- College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, China
| | - Ji Chen
- Department of Agroecology, Aarhus University, Tjele 8830, Denmark
| | | | - Qianggong Zhang
- Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
| | - Xin-Quan Zhou
- College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, China
| | - Yusen Yuan
- College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, China
| | - Songhui Feng
- College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, China
| | - Kexin Zhang
- College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, China
| | - Yu-Rong Liu
- State Key Laboratory of Agricultural Microbiology, Huazhong Agricultural University, Wuhan 430070, China; College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, China; State Environmental Protection Key Laboratory of Soil Health and Green Remediation, Wuhan 430070, China.
| | - Qiaoyun Huang
- State Key Laboratory of Agricultural Microbiology, Huazhong Agricultural University, Wuhan 430070, China; College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, China
| |
Collapse
|
12
|
Long-Term Compost Amendment Spurs Cellulose Decomposition by Driving Shifts in Fungal Community Composition and Promoting Fungal Diversity and Phylogenetic Relatedness. mBio 2022; 13:e0032322. [PMID: 35491853 PMCID: PMC9239258 DOI: 10.1128/mbio.00323-22] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/25/2022] Open
Abstract
Cellulose is the most abundant polysaccharide in plant biomass and an important precursor of soil organic matter formation. Fungi play a key role in carbon cycling dynamics because they tend to decompose recalcitrant materials. Here, we applied [12C]cellulose and [13C]cellulose to distinguish the effects of application of compost, nitrogen-phosphorus-potassium (NPK) fertilizer, and no fertilizer (control) for 27 years upon cellulose decomposition via RNA-based stable isotope probing (RNA-SIP). The loss ratio of added cellulose C in compost soil was 67.6 to 106.7% higher than in NPK and control soils during their 20-day incubation. Dothideomycetes (mainly members of the genus Cryptococcus) dominated cellulose utilization in compost soil, whereas the copiotrophic Sordariomycetes were more abundant in NPK and unfertilized soils. Compared with NPK and control soils, compost application increased the diversity of 13C-assimilating fungi. The 13C-labeled fungal communities in compost soil were more phylogenetically clustered and exhibited greater species relatedness than those in NPK and control soils, perhaps because of stringent filtering of narrow-spectrum organic resources and biological invasion originating from added compost. These changes led to an augmented decomposition capacity of fungal species for cellulose-rich substrates and reduced cellulose C sequestration efficiency. The RNA-SIP technique is more sensitive to responses of fungi to altered soil resource availability than DNA-SIP. Overall, long-term compost application modified fungal community composition and promoted fungal diversity and phylogenetic relatedness, accelerating the decomposition of substrate cellulose in soil. This work also highlights the RNA-SIP technique’s value for comprehensively assessing the contributions of active fungi to the substrate decomposition process.
Collapse
|
13
|
Beugnon R, Du J, Cesarz S, Jurburg SD, Pang Z, Singavarapu B, Wubet T, Xue K, Wang Y, Eisenhauer N. Tree diversity and soil chemical properties drive the linkages between soil microbial community and ecosystem functioning. ISME COMMUNICATIONS 2021; 1:41. [PMID: 37938251 PMCID: PMC9723754 DOI: 10.1038/s43705-021-00040-0] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/03/2021] [Revised: 07/27/2021] [Accepted: 08/05/2021] [Indexed: 05/26/2023]
Abstract
Microbial respiration is critical for soil carbon balance and ecosystem functioning. Previous studies suggest that plant diversity influences soil microbial communities and their respiration. Yet, the linkages between tree diversity, microbial biomass, microbial diversity, and microbial functioning have rarely been explored. In this study, we measured two microbial functions (microbial physiological potential, and microbial respiration), together with microbial biomass, microbial taxonomic and functional profiles, and soil chemical properties in a tree diversity experiment in South China, to disentangle how tree diversity affects microbial respiration through the modifications of the microbial community. Our analyses show a significant positive effect of tree diversity on microbial biomass (+25% from monocultures to 24-species plots), bacterial diversity (+12%), and physiological potential (+12%). In addition, microbial biomass and physiological potential, but not microbial diversity, were identified as the key drivers of microbial respiration. Although soil chemical properties strongly modulated soil microbial community, tree diversity increased soil microbial respiration by increasing microbial biomass rather than changing microbial taxonomic or functional diversity. Overall, our findings suggest a prevalence of microbial biomass over diversity in controlling soil carbon dynamics.
Collapse
Affiliation(s)
- Rémy Beugnon
- German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Puschstrasse 4, Leipzig, Germany.
- Institute of Biology, Leipzig University, Puschstrasse 4, Leipzig, Germany.
| | - Jianqing Du
- Yanshan Earth Critical Zone and Surface Fluxes Research Station, College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China
| | - Simone Cesarz
- German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Puschstrasse 4, Leipzig, Germany
- Institute of Biology, Leipzig University, Puschstrasse 4, Leipzig, Germany
| | - Stephanie D Jurburg
- German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Puschstrasse 4, Leipzig, Germany
- Institute of Biology, Leipzig University, Puschstrasse 4, Leipzig, Germany
| | - Zhe Pang
- Yanshan Earth Critical Zone and Surface Fluxes Research Station, College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China
| | - Bala Singavarapu
- German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Puschstrasse 4, Leipzig, Germany
- UFZ-Helmholtz Centre for Environmental Research, Department of Community Ecology, Theodor-Lieser-Str. 4, Halle (Saale), Germany
- Institute of Biology/Geobotany and Botanical Garden, Martin Luther University Halle-Wittenberg, Am Kirchtor, Halle, Germany
| | - Tesfaye Wubet
- German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Puschstrasse 4, Leipzig, Germany
- UFZ-Helmholtz Centre for Environmental Research, Department of Community Ecology, Theodor-Lieser-Str. 4, Halle (Saale), Germany
| | - Kai Xue
- Yanshan Earth Critical Zone and Surface Fluxes Research Station, College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China.
- CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, China.
| | - Yanfen Wang
- Yanshan Earth Critical Zone and Surface Fluxes Research Station, College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China
- CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, China
| | - Nico Eisenhauer
- German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Puschstrasse 4, Leipzig, Germany
- Institute of Biology, Leipzig University, Puschstrasse 4, Leipzig, Germany
| |
Collapse
|
14
|
Sun T, Wang Y, Lucas-Borja ME, Jing X, Feng W. Divergent vertical distributions of microbial biomass with soil depth among groups and land uses. JOURNAL OF ENVIRONMENTAL MANAGEMENT 2021; 292:112755. [PMID: 33992868 DOI: 10.1016/j.jenvman.2021.112755] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/15/2020] [Revised: 04/30/2021] [Accepted: 05/02/2021] [Indexed: 06/12/2023]
Abstract
Soil microbial biomass is key to improving the prediction of soil organic carbon (SOC) dynamics by modeling. However, the driving mechanism of microbial biomass of different groups with soil depth is poorly understood across sites. Here, we compiled the biomass of different microbial groups (i.e., fungi, bacteria, gram-positive bacteria G+, and gram-negative bacteria G-) from the surface to a soil depth of 1 m from 71 soil profiles across three continents. We found that the biomass of microbial groups all decreased with soil depth but at different magnitudes, while the relative abundance of microbial groups, except G-, was relatively stable along soil profiles. Soil fungal biomass had a shallower vertical distribution than bacteria, especially G+, with 89% fungi and 76% G+ in the top 10 cm soils. In addition, a greater proportion of microbial biomass (71-89%) compared to SOC (64%) was in the top 10 cm soils, suggesting that microbes and SOC exhibited different vertical distributions. The vertical distributions of microbial biomass of different groups were significantly correlated with SOC and clay content but not with climate, and these distributions were different among land uses, highlighting the great influences of edaphic factors on vertical distributions of microbial biomass. The relationship between microbial biomass and soil depth provides a feasible way to estimate microbial biomass at different soil depths, which can serve as a benchmark to improve the prediction of SOC dynamics of entire soil profile at large scales.
Collapse
Affiliation(s)
- Tingting Sun
- State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, Xinjiang, 830011, China; University of Chinese Academy of Sciences, Beijing, 100049, China; National Fukang Station of Desert Ecosystem Ecology, Field Sciences Observation and Research Station, Chinese Academy of Sciences, Fukang, Xinjiang, 831505, China
| | - Yugang Wang
- State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, Xinjiang, 830011, China; University of Chinese Academy of Sciences, Beijing, 100049, China; National Fukang Station of Desert Ecosystem Ecology, Field Sciences Observation and Research Station, Chinese Academy of Sciences, Fukang, Xinjiang, 831505, China
| | - Manuel Esteban Lucas-Borja
- University of Castilla-La Mancha (UCLM), Technical School of Agricultural and Mountain Engineering (ETSIAM), Albacete, 02071, Spain
| | - Xin Jing
- Department of Earth and Environmental Sciences, KU Leuven, Celestijnenlaan 200E, 3001, Leuven, Belgium
| | - Wenting Feng
- Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing, 100081, China.
| |
Collapse
|
15
|
Reduced microbial stability in the active layer is associated with carbon loss under alpine permafrost degradation. Proc Natl Acad Sci U S A 2021; 118:2025321118. [PMID: 34131077 DOI: 10.1073/pnas.2025321118] [Citation(s) in RCA: 106] [Impact Index Per Article: 35.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 02/01/2023] Open
Abstract
Permafrost degradation may induce soil carbon (C) loss, critical for global C cycling, and be mediated by microbes. Despite larger C stored within the active layer of permafrost regions, which are more affected by warming, and the critical roles of Qinghai-Tibet Plateau in C cycling, most previous studies focused on the permafrost layer and in high-latitude areas. We demonstrate in situ that permafrost degradation alters the diversity and potentially decreases the stability of active layer microbial communities. These changes are associated with soil C loss and potentially a positive C feedback. This study provides insights into microbial-mediated mechanisms responsible for C loss within the active layer in degraded permafrost, aiding in the modeling of C emission under future scenarios.
Collapse
|
16
|
Nam S, Alday JG, Kim M, Kim H, Kim Y, Park T, Lim HS, Lee BY, Lee YK, Jung JY. The relationships of present vegetation, bacteria, and soil properties with soil organic matter characteristics in moist acidic tundra in Alaska. THE SCIENCE OF THE TOTAL ENVIRONMENT 2021; 772:145386. [PMID: 33770858 DOI: 10.1016/j.scitotenv.2021.145386] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/06/2020] [Revised: 01/19/2021] [Accepted: 01/19/2021] [Indexed: 06/12/2023]
Abstract
Soil organic matter (SOM) is related to vegetation, soil bacteria, and soil properties; however, not many studies link all these parameters simultaneously, particularly in tundra ecosystems vulnerable to climate change. Our aim was to describe the relationships between vegetation, bacteria, soil properties, and SOM composition in moist acidic tundra by integrating physical, chemical, and molecular methods. A total of 70 soil samples were collected at two different depths from 36 spots systematically arranged over an area of about 300 m × 50 m. Pyrolysis-gas chromatography/mass spectrometry and pyrosequencing of the 16S rRNA gene were used to identify the molecular compositions of the SOM and bacterial community, respectively. Vegetation and soil physicochemical properties were also measured. The sampling sites were grouped into three, based on their SOM compositions: Sphagnum moss-derived SOM, lipid-rich materials, and aromatic-rich materials. Our results show that SOM composition is spatially structured and linked to microtopography; however, the vegetation, soil properties, and bacterial community composition did not show overall spatial structuring. Simultaneously, soil properties and bacterial community composition were the main factors explaining SOM compositional variation, while vegetation had a residual effect. Verrucomicrobia and Acidobacteria were related to polysaccharides, and Chloroflexi was linked to aromatic compounds. These relationships were consistent across different hierarchical levels. Our results suggest that SOM composition at a local scale is closely linked with soil factors and the bacterial community. Comprehensive observation of ecosystem components is recommended to understand the in-situ function of bacteria and the fate of SOM in the moist acidic tundra.
Collapse
Affiliation(s)
- Sungjin Nam
- Korea Polar Research Institute, Incheon 21990, Republic of Korea
| | - Josu G Alday
- Joint Research Unit CTFC - AGROTECNIO, Av. Alcalde Rovira Roure 191, E25198 Lleida, Spain; Department of Crop and Forest Sciences, University of Lleida, Av. Alcalde Rovira Roure 191, E25198 Lleida, Spain
| | - Mincheol Kim
- Korea Polar Research Institute, Incheon 21990, Republic of Korea
| | - Hyemin Kim
- Korea Polar Research Institute, Incheon 21990, Republic of Korea
| | - Yongkang Kim
- Department of Statistics, Seoul National University, Seoul 08826, Republic of Korea
| | - Taesung Park
- Department of Statistics, Seoul National University, Seoul 08826, Republic of Korea
| | - Hyoun Soo Lim
- Department of Geological Sciences, Pusan National University, Busan 46241, Republic of Korea
| | - Bang Yong Lee
- Korea Polar Research Institute, Incheon 21990, Republic of Korea
| | - Yoo Kyung Lee
- Korea Polar Research Institute, Incheon 21990, Republic of Korea.
| | - Ji Young Jung
- Korea Polar Research Institute, Incheon 21990, Republic of Korea.
| |
Collapse
|
17
|
Ji X, Abakumov E, Chigray S, Saparova S, Polyakov V, Wang W, Wu D, Li C, Huang Y, Xie X. Response of carbon and microbial properties to risk elements pollution in arctic soils. JOURNAL OF HAZARDOUS MATERIALS 2021; 408:124430. [PMID: 33176958 DOI: 10.1016/j.jhazmat.2020.124430] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/05/2020] [Revised: 10/27/2020] [Accepted: 10/28/2020] [Indexed: 06/11/2023]
Abstract
A 180-day incubation study was conducted to evaluate the effects of risk elements (REs) on organic carbon use and microbial activities in organic soils in the Arctic during the summer snowmelt period. Soils were artificially spiked with Cd, Pb, Cr, Ni, Cu, As, and a combination of these REs according to the levels measured in Arctic soils from REs-polluted industrial sites. During the incubation period, microbial activities and microbial biomass carbon (MBC) formation were inhibited, and microbial quotient (qCO2) values were relatively high in the spiked soils indicating that more energy was used by microbes for maintenance under REs stress. Meanwhile, microbial metabolism was significantly restrained. Microbial Specific phospholipid fatty acids (PLFAs) were reduced in RE spiked soils relative to the control, especially in the As- and multi-RE-spiked soils. The abundance of both fungi and bacteria was reduced in response to RE amendments by 14-24% and 1-55%, respectively. PLFA biomarkers indicated a shift in soil microbial community structure and activities influenced by REs, consequently having a negative effect on soil organic carbon degradation. This study addresses the knowledge gap regarding the alternation of biochemical reactions in Arctic soils under anthropogenic REs with relevant contamination levels.
Collapse
Affiliation(s)
- Xiaowen Ji
- Key Laboratory of Poyang Lake Environment and Resource Utilization, Ministry of Education, School of Resources Environmental & Chemical Engineering, Nanchang University, Nanchang 330031, PR China; Department of Applied Ecology, Saint Petersburg State University, Saint Petersburg 199178, Russian Federation; School of Environment and Sustainability, University of Saskatchewan, Saskatoon SK, S7N 5B3, Canada
| | - Evgeny Abakumov
- Department of Applied Ecology, Saint Petersburg State University, Saint Petersburg 199178, Russian Federation
| | - Svetlana Chigray
- Department of Applied Ecology, Saint Petersburg State University, Saint Petersburg 199178, Russian Federation
| | - Sheker Saparova
- Department of Applied Ecology, Saint Petersburg State University, Saint Petersburg 199178, Russian Federation
| | - Vyacheslav Polyakov
- Department of Applied Ecology, Saint Petersburg State University, Saint Petersburg 199178, Russian Federation; Arctic and Antarctic Research Institute, Saint Petersburg, 199397, Russian Federation; Department of Soil Science and Agrochemistry, Saint-Petersburg State Agrarian University, Pushkin, Saint Petersburg 19660, Russian Federation
| | - Wenjuan Wang
- Department of Applied Ecology, Saint Petersburg State University, Saint Petersburg 199178, Russian Federation
| | - Daishe Wu
- Key Laboratory of Poyang Lake Environment and Resource Utilization, Ministry of Education, School of Resources Environmental & Chemical Engineering, Nanchang University, Nanchang 330031, PR China
| | - Chunlan Li
- Institute for Global Innovation and Development, East China Normal University, Shanghai 200062, PR China; School of Urban and Regional Sciences, East China Normal University, Shanghai 200241, PR China
| | - Yu Huang
- Center for Eco-Environment Research, Nanjing Hydraulic Research Institute, Nanjing 210098, PR China
| | - Xianchuan Xie
- Key Laboratory of Poyang Lake Environment and Resource Utilization, Ministry of Education, School of Resources Environmental & Chemical Engineering, Nanchang University, Nanchang 330031, PR China; State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, Nanjing 210093, PR China.
| |
Collapse
|
18
|
Tao X, Feng J, Yang Y, Wang G, Tian R, Fan F, Ning D, Bates CT, Hale L, Yuan MM, Wu L, Gao Q, Lei J, Schuur EAG, Yu J, Bracho R, Luo Y, Konstantinidis KT, Johnston ER, Cole JR, Penton CR, Tiedje JM, Zhou J. Winter warming in Alaska accelerates lignin decomposition contributed by Proteobacteria. MICROBIOME 2020; 8:84. [PMID: 32503635 PMCID: PMC7275452 DOI: 10.1186/s40168-020-00838-5] [Citation(s) in RCA: 27] [Impact Index Per Article: 6.8] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/22/2019] [Accepted: 04/15/2020] [Indexed: 06/01/2023]
Abstract
BACKGROUND In a warmer world, microbial decomposition of previously frozen organic carbon (C) is one of the most likely positive climate feedbacks of permafrost regions to the atmosphere. However, mechanistic understanding of microbial mediation on chemically recalcitrant C instability is limited; thus, it is crucial to identify and evaluate active decomposers of chemically recalcitrant C, which is essential for predicting C-cycle feedbacks and their relative strength of influence on climate change. Using stable isotope probing of the active layer of Arctic tundra soils after depleting soil labile C through a 975-day laboratory incubation, the identity of microbial decomposers of lignin and, their responses to warming were revealed. RESULTS The β-Proteobacteria genus Burkholderia accounted for 95.1% of total abundance of potential lignin decomposers. Consistently, Burkholderia isolated from our tundra soils could grow with lignin as the sole C source. A 2.2 °C increase of warming considerably increased total abundance and functional capacities of all potential lignin decomposers. In addition to Burkholderia, α-Proteobacteria capable of lignin decomposition (e.g. Bradyrhizobium and Methylobacterium genera) were stimulated by warming by 82-fold. Those community changes collectively doubled the priming effect, i.e., decomposition of existing C after fresh C input to soil. Consequently, warming aggravates soil C instability, as verified by microbially enabled climate-C modeling. CONCLUSIONS Our findings are alarming, which demonstrate that accelerated C decomposition under warming conditions will make tundra soils a larger biospheric C source than anticipated. Video Abstract.
Collapse
Affiliation(s)
- Xuanyu Tao
- Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA
- Institute for Environmental Genomics, University of Oklahoma, Norman, OK, 73019, USA
- School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, OK, 73019, USA
| | - Jiajie Feng
- Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA
- Institute for Environmental Genomics, University of Oklahoma, Norman, OK, 73019, USA
- School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, OK, 73019, USA
| | - Yunfeng Yang
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, 100084, China.
| | - Gangsheng Wang
- Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA
- Institute for Environmental Genomics, University of Oklahoma, Norman, OK, 73019, USA
- School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, OK, 73019, USA
| | - Renmao Tian
- Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA
- Institute for Environmental Genomics, University of Oklahoma, Norman, OK, 73019, USA
- School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, OK, 73019, USA
| | - Fenliang Fan
- Key Laboratory of Plant Nutrition and Fertilizer, Ministry of Agriculture, Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing, 100081, China
| | - Daliang Ning
- Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA
- Institute for Environmental Genomics, University of Oklahoma, Norman, OK, 73019, USA
- School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, OK, 73019, USA
| | - Colin T Bates
- Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA
- Institute for Environmental Genomics, University of Oklahoma, Norman, OK, 73019, USA
- School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, OK, 73019, USA
| | - Lauren Hale
- Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA
- Institute for Environmental Genomics, University of Oklahoma, Norman, OK, 73019, USA
- School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, OK, 73019, USA
| | - Mengting M Yuan
- Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA
- Institute for Environmental Genomics, University of Oklahoma, Norman, OK, 73019, USA
- School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, OK, 73019, USA
| | - Linwei Wu
- Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA
- Institute for Environmental Genomics, University of Oklahoma, Norman, OK, 73019, USA
- School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, OK, 73019, USA
| | - Qun Gao
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, 100084, China
| | - Jiesi Lei
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, 100084, China
| | - Edward A G Schuur
- Center for Ecosystem Science and Society, Northern Arizona University, Flagstaff, AZ, 86011, USA
| | - Julian Yu
- College of Integrative Sciences and Arts, Arizona State University, Mesa, AZ, 85212, USA
- Center for Fundamental and Applied Microbiomics, The Biodesign Institute, Arizona State University, Tempe, AZ, 85281, USA
| | - Rosvel Bracho
- School of Forest Resources and Conservation, Department of Biology, University of Florida, Gainesville, FL, 32611, USA
| | - Yiqi Luo
- Center for Ecosystem Science and Society, Northern Arizona University, Flagstaff, AZ, 86011, USA
| | - Konstantinos T Konstantinidis
- School of Civil and Environmental Engineering, School of Biology, and Center for Bioinformatics and Computational Genomics, Georgia Institute of Technology, Atlanta, GA, 30332, USA
| | - Eric R Johnston
- School of Civil and Environmental Engineering, School of Biology, and Center for Bioinformatics and Computational Genomics, Georgia Institute of Technology, Atlanta, GA, 30332, USA
| | - James R Cole
- Center for Microbial Ecology, Michigan State University, East Lansing, MI, 48824, USA
| | - C Ryan Penton
- College of Integrative Sciences and Arts, Arizona State University, Mesa, AZ, 85212, USA
- Center for Fundamental and Applied Microbiomics, The Biodesign Institute, Arizona State University, Tempe, AZ, 85281, USA
| | - James M Tiedje
- Center for Microbial Ecology, Michigan State University, East Lansing, MI, 48824, USA
| | - Jizhong Zhou
- Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
- Institute for Environmental Genomics, University of Oklahoma, Norman, OK, 73019, USA.
- School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, OK, 73019, USA.
- State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, 100084, China.
- Earth and Environmental Sciences, Lawrence Berkeley National Laboratory, Berkeley, CA, 94720, USA.
| |
Collapse
|
19
|
Metagenomics-Guided Discovery of Potential Bacterial Metallothionein Genes from the Soil Microbiome That Confer Cu and/or Cd Resistance. Appl Environ Microbiol 2020; 86:AEM.02907-19. [PMID: 32111593 DOI: 10.1128/aem.02907-19] [Citation(s) in RCA: 12] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/16/2019] [Accepted: 02/15/2020] [Indexed: 12/18/2022] Open
Abstract
Metallothionein (MT) genes are valuable genetic materials for developing metal bioremediation tools. Currently, a limited number of prokaryotic MTs have been experimentally identified, which necessitates the expansion of bacterial MT diversity. In this study, we conducted a metagenomics-guided analysis for the discovery of potential bacterial MT genes from the soil microbiome. More specifically, we combined resistance gene enrichment through diversity loss, metagenomic mining with a dedicated MT database, evolutionary trace analysis, DNA chemical synthesis, and functional genomic validation to identify novel MTs. Results showed that Cu stress induced a compositional change in the soil microbiome, with an enrichment of metal-resistant bacteria in soils with higher Cu concentrations. Shotgun metagenomic sequencing was performed to obtain the gene pool of environmental DNA (eDNA), which was subjected to a local BLAST search against an MT database for detecting putative MT genes. Evolutional trace analysis led to the identification of 27 potential MTs with conserved cysteine/histidine motifs different from those of known prokaryotic MTs. Following chemical synthesis of these 27 potential MT genes and heterologous expression in Escherichia coli, six of them were found to improve the hosts' growth substantially and enhanced the hosts' sorption of Cu, Cd, and Zn, among which MT5 led to a 13.7-fold increase in Cd accumulation. Furthermore, four of them restored Cu and/or Cd resistance in two metal-sensitive E. coli strains.IMPORTANCE The metagenomics-guided procedure developed here bypasses the difficulties encountered in classic PCR-based approaches and led to the discovery of novel MT genes, which may be useful in developing bioremediation tools. The procedure used here expands our knowledge on the diversity of bacterial MTs in the environment and may also be applicable to identify other functional genes from eDNA.
Collapse
|
20
|
Luo Y, Schuur EAG. Model parameterization to represent processes at unresolved scales and changing properties of evolving systems. GLOBAL CHANGE BIOLOGY 2020; 26:1109-1117. [PMID: 31782216 DOI: 10.1111/gcb.14939] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/12/2019] [Revised: 11/21/2019] [Accepted: 11/22/2019] [Indexed: 06/10/2023]
Abstract
Modeling has become an indispensable tool for scientific research. However, models generate great uncertainty when they are used to predict or forecast ecosystem responses to global change. This uncertainty is partly due to parameterization, which is an essential procedure for model specification via defining parameter values for a model. The classic doctrine of parameterization is that a parameter is constant. However, it is commonly known from modeling practice that a model that is well calibrated for its parameters at one site may not simulate well at another site unless its parameters are tuned again. This common practice implies that parameter values have to vary with sites. Indeed, parameter values that are estimated using a statistically rigorous approach, that is, data assimilation, vary with time, space, and treatments in global change experiments. This paper illustrates that varying parameters is to account for both processes at unresolved scales and changing properties of evolving systems. A model, no matter how complex it is, could not represent all the processes of one system at resolved scales. Interactions of processes at unresolved scales with those at resolved scales should be reflected in model parameters. Meanwhile, it is pervasively observed that properties of ecosystems change over time, space, and environmental conditions. Parameters, which represent properties of a system under study, should change as well. Tuning has been practiced for many decades to change parameter values. Yet this activity, unfortunately, did not contribute to our knowledge on model parameterization at all. Data assimilation makes it possible to rigorously estimate parameter values and, consequently, offers an approach to understand which, how, how much, and why parameters vary. To fully understand those issues, extensive research is required. Nonetheless, it is clear that changes in parameter values lead to different model predictions even if the model structure is the same.
Collapse
Affiliation(s)
- Yiqi Luo
- Department of Biological Sciences, Center for Ecosystem Sciences and Society, Northern Arizona University, Flagstaff, AZ, USA
| | - Edward A G Schuur
- Department of Biological Sciences, Center for Ecosystem Sciences and Society, Northern Arizona University, Flagstaff, AZ, USA
| |
Collapse
|