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Tomazelli D, Klauberg-Filho O, Mendes LW, Goss-Souza D. The impact of land-use changes and management intensification on bacterial communities in the last decade: a review. Appl Environ Microbiol 2024; 90:e0030924. [PMID: 38874336 PMCID: PMC11267915 DOI: 10.1128/aem.00309-24] [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] [Indexed: 06/15/2024] Open
Abstract
In the last decade, advances in soil bacterial ecology have contributed to increasing agricultural production. Brazil is the world leading agriculture producer and leading soil biodiversity reservoir. Meanwhile, there is still a significant gap in the knowledge regarding the soil microscopic life and its interactions with agricultural practices, and the replacement of natural vegetation by agroecosystems is yet to be unfolded. Through high throughput DNA sequencing, scientists are now exploring the complexity of soil bacterial communities and their relationship with soil and environmental characteristics. This study aimed to investigate the progress of bacterial ecology studies in Brazil over the last 10 years, seeking to understand the effect of the conversion of natural vegetation in agricultural systems on the diversity and structure of the soil microbial communities. We conducted a systematic search for scientific publication databases. Our systematic search has matched 62 scientific articles from three different databases. Most of the studies were placed in southeastern and northern Brazil, with no records of studies about microbial ecology in 17 out of 27 Brazilian states. Out of the 26 studies that examined the effects of replacing natural vegetation with agroecosystems, most authors concluded that changes in soil pH and vegetation cover replacement were the primary drivers of shifts in microbial communities. Understanding the ecology of the bacteria inhabiting Brazilian soils in agroecosystems is paramount for developing more efficient soil management strategies and cleaner agricultural technologies.
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Affiliation(s)
- Daniela Tomazelli
- Department of Soils and Natural Resources, Santa Catarina State University, Lages, Santa Catarina, Brazil
| | - Osmar Klauberg-Filho
- Department of Soils and Natural Resources, Santa Catarina State University, Lages, Santa Catarina, Brazil
| | - Lucas William Mendes
- Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, São Paulo, Brazil
| | - Dennis Goss-Souza
- College of Agronomy, Federal Institute of Paraná, Palmas, Paraná, Brazil
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2
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Lim J, Wehmeyer H, Heffner T, Aeppli M, Gu W, Kim PJ, Horn MA, Ho A. Resilience of aerobic methanotrophs in soils; spotlight on the methane sink under agriculture. FEMS Microbiol Ecol 2024; 100:fiae008. [PMID: 38327184 PMCID: PMC10872700 DOI: 10.1093/femsec/fiae008] [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: 09/05/2023] [Revised: 01/19/2024] [Accepted: 02/06/2024] [Indexed: 02/09/2024] Open
Abstract
Aerobic methanotrophs are a specialized microbial group, catalyzing the oxidation of methane. Disturbance-induced loss of methanotroph diversity/abundance, thus results in the loss of this biological methane sink. Here, we synthesized and conceptualized the resilience of the methanotrophs to sporadic, recurring, and compounded disturbances in soils. The methanotrophs showed remarkable resilience to sporadic disturbances, recovering in activity and population size. However, activity was severely compromised when disturbance persisted or reoccurred at increasing frequency, and was significantly impaired following change in land use. Next, we consolidated the impact of agricultural practices after land conversion on the soil methane sink. The effects of key interventions (tillage, organic matter input, and cover cropping) where much knowledge has been gathered were considered. Pairwise comparisons of these interventions to nontreated agricultural soils indicate that the agriculture-induced impact on the methane sink depends on the cropping system, which can be associated to the physiology of the methanotrophs. The impact of agriculture is more evident in upland soils, where the methanotrophs play a more prominent role than the methanogens in modulating overall methane flux. Although resilient to sporadic disturbances, the methanotrophs are vulnerable to compounded disturbances induced by anthropogenic activities, significantly affecting the methane sink function.
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Affiliation(s)
- Jiyeon Lim
- Institute for Microbiology, Leibniz Universität Hannover, Herrenhäuser Str. 2, 30419 Hannover, Germany
| | - Helena Wehmeyer
- Nestlè Research, Route du Jorat 57, CH 1000 Lausanne 26, Switzerland
| | - Tanja Heffner
- Institute for Microbiology, Leibniz Universität Hannover, Herrenhäuser Str. 2, 30419 Hannover, Germany
| | - Meret Aeppli
- Environmental Engineering Institute IIE-ENAC, Laboratory SOIL, Ecole Polytechnique Fédérale de Lausanne (EPFL), Valais Wallis, CH 1950 Sion, Switzerland
| | - Wenyu Gu
- Environmental Engineering Institute IIE-ENAC, Laboratory MICROBE, Ecole Polytechnique Fédérale de Lausanne (EPFL), CH 1015 Lausanne, Switzerland
| | - Pil Joo Kim
- Division of Applied Life Science, Gyeongsang National University, Jinju 660-701, Republic of Korea
| | - Marcus A Horn
- Institute for Microbiology, Leibniz Universität Hannover, Herrenhäuser Str. 2, 30419 Hannover, Germany
| | - Adrian Ho
- Nestlè Research, Route du Jorat 57, CH 1000 Lausanne 26, Switzerland
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3
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Aryee G, Luecke SM, Dahlen CR, Swanson KC, Amat S. Holistic View and Novel Perspective on Ruminal and Extra-Gastrointestinal Methanogens in Cattle. Microorganisms 2023; 11:2746. [PMID: 38004757 PMCID: PMC10673468 DOI: 10.3390/microorganisms11112746] [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: 10/23/2023] [Revised: 11/08/2023] [Accepted: 11/09/2023] [Indexed: 11/26/2023] Open
Abstract
Despite the extensive research conducted on ruminal methanogens and anti-methanogenic intervention strategies over the last 50 years, most of the currently researched enteric methane (CH4) abatement approaches have shown limited efficacy. This is largely because of the complex nature of animal production and the ruminal environment, host genetic variability of CH4 production, and an incomplete understanding of the role of the ruminal microbiome in enteric CH4 emissions. Recent sequencing-based studies suggest the presence of methanogenic archaea in extra-gastrointestinal tract tissues, including respiratory and reproductive tracts of cattle. While these sequencing data require further verification via culture-dependent methods, the consistent identification of methanogens with relatively greater frequency in the airway and urogenital tract of cattle, as well as increasing appreciation of the microbiome-gut-organ axis together highlight the potential interactions between ruminal and extra-gastrointestinal methanogenic communities. Thus, a traditional singular focus on ruminal methanogens may not be sufficient, and a holistic approach which takes into consideration of the transfer of methanogens between ruminal, extra-gastrointestinal, and environmental microbial communities is of necessity to develop more efficient and long-term ruminal CH4 mitigation strategies. In the present review, we provide a holistic survey of the methanogenic archaea present in different anatomical sites of cattle and discuss potential seeding sources of the ruminal methanogens.
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Affiliation(s)
- Godson Aryee
- Department of Microbiological Sciences, North Dakota State University, Fargo, ND 58108, USA; (G.A.); (S.M.L.)
| | - Sarah M. Luecke
- Department of Microbiological Sciences, North Dakota State University, Fargo, ND 58108, USA; (G.A.); (S.M.L.)
| | - Carl R. Dahlen
- Department of Animal Sciences, and Center for Nutrition and Pregnancy, North Dakota State University, Fargo, ND 58102, USA; (C.R.D.); (K.C.S.)
| | - Kendall C. Swanson
- Department of Animal Sciences, and Center for Nutrition and Pregnancy, North Dakota State University, Fargo, ND 58102, USA; (C.R.D.); (K.C.S.)
| | - Samat Amat
- Department of Microbiological Sciences, North Dakota State University, Fargo, ND 58108, USA; (G.A.); (S.M.L.)
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4
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Bieluczyk W, Asselta FO, Navroski D, Gontijo JB, Venturini AM, Mendes LW, Simon CP, Camargo PBD, Tadini AM, Martin-Neto L, Bendassolli JA, Rodrigues RR, van der Putten WH, Tsai SM. Linking above and belowground carbon sequestration, soil organic matter properties, and soil health in Brazilian Atlantic Forest restoration. JOURNAL OF ENVIRONMENTAL MANAGEMENT 2023; 344:118573. [PMID: 37459811 DOI: 10.1016/j.jenvman.2023.118573] [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: 03/21/2023] [Revised: 06/27/2023] [Accepted: 07/02/2023] [Indexed: 09/17/2023]
Abstract
Forest restoration mitigates climate change by removing CO2 and storing C in terrestrial ecosystems. However, incomplete information on C storage in restored tropical forests often fails to capture the ecosystem's holistic C dynamics. This study provides an integrated assessment of C storage in above to belowground subsystems, its consequences for greenhouse gas (GHG) fluxes, and the quantity, quality, and origin of soil organic matter (SOM) in restored Atlantic forests in Brazil. Relations between SOM properties and soil health indicators were also explored. We examined two restorations using tree planting ('active restoration'): an 8-year-old forest with green manure and native trees planted in two rounds, and a 15-year-old forest with native-planted trees in one round without green manure. Restorations were compared to reformed pasture and primary forest sites. We measured C storage in soil layers (0-10, 10-20, and 20-30 cm), litter, and plants. GHG emissions were assessed using CH4 and CO2 fluxes. SOM quantity was evaluated using C and N, quality using humification index (HLIFS), and origin using δ13C and δ15N. Nine soil health indicators were interrelated with SOM attributes. The primary forest presented the highest C stocks (107.7 Mg C ha-1), followed by 15- and 8-year-old restorations and pasture with 69.8, 55.5, and 41.8 Mg C ha-1, respectively. Soil C stocks from restorations and pasture were 20% lower than primary forest. However, 8- and 15-year-old restorations stored 12.3 and 28.3 Mg ha-1 more aboveground C than pasture. The younger forest had δ13C and δ15N values of 2.1 and 1.7‰, respectively, lower than the 15-year-old forest, indicating more C derived from C3 plants and biological N fixation. Both restorations and pasture had at least 34% higher HLIFS in deeper soil layers (10-30 cm) than primary forest, indicating a lack of labile SOM. Native and 15-year-old forests exhibited higher soil methane influx (141.1 and 61.9 μg m-2 h-1). Forests outperformed pasture in most soil health indicators, with 69% of their variance explained by SOM properties. However, SOM quantity and quality regeneration in both restorations approached the pristine forest state only in the top 10 cm layer, while deeper soil retained agricultural degradation legacies. In conclusion, active restoration of the Atlantic Forest is a superior approach compared to pasture reform for GHG mitigation. Nonetheless, the development of restoration techniques to facilitate labile C input into deeper soil layers (>10 cm) is needed to further improve soil multifunctionality and long-term C storage.
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Affiliation(s)
- Wanderlei Bieluczyk
- University of São Paulo, Center for Nuclear Energy in Agriculture, Cell and Molecular Biology Laboratory, 303 Centenário Avenue, Piracicaba, SP, 13416-000, Brazil; University of São Paulo, Center for Nuclear Energy in Agriculture, Isotopic Ecology Laboratory, 303 Centenário Avenue, Piracicaba, SP, 13416-000, Brazil.
| | - Fernanda Ometto Asselta
- University of São Paulo, Center for Nuclear Energy in Agriculture, Cell and Molecular Biology Laboratory, 303 Centenário Avenue, Piracicaba, SP, 13416-000, Brazil.
| | - Deisi Navroski
- University of São Paulo, Center for Nuclear Energy in Agriculture, Cell and Molecular Biology Laboratory, 303 Centenário Avenue, Piracicaba, SP, 13416-000, Brazil.
| | - Júlia Brandão Gontijo
- University of São Paulo, Center for Nuclear Energy in Agriculture, Cell and Molecular Biology Laboratory, 303 Centenário Avenue, Piracicaba, SP, 13416-000, Brazil.
| | - Andressa Monteiro Venturini
- Princeton Institute for International and Regional Studies, Princeton University, Princeton, NJ, USA; Department of Biology, Stanford University, Stanford, CA, USA.
| | - Lucas William Mendes
- University of São Paulo, Center for Nuclear Energy in Agriculture, Cell and Molecular Biology Laboratory, 303 Centenário Avenue, Piracicaba, SP, 13416-000, Brazil.
| | - Carla Penha Simon
- University of São Paulo, Center for Nuclear Energy in Agriculture, Isotopic Ecology Laboratory, 303 Centenário Avenue, Piracicaba, SP, 13416-000, Brazil.
| | - Plínio Barbosa de Camargo
- University of São Paulo, Center for Nuclear Energy in Agriculture, Isotopic Ecology Laboratory, 303 Centenário Avenue, Piracicaba, SP, 13416-000, Brazil.
| | - Amanda Maria Tadini
- Brazilian Agricultural Research Corporation, Embrapa Instrumentation, 1452 XV de Novembro Street, São Carlos, SP, 13560-970, Brazil.
| | - Ladislau Martin-Neto
- Brazilian Agricultural Research Corporation, Embrapa Instrumentation, 1452 XV de Novembro Street, São Carlos, SP, 13560-970, Brazil.
| | - José Albertino Bendassolli
- University of São Paulo, Center for Nuclear Energy in Agriculture, Stable Isotope Laboratory, 303 Centenário Avenue, Piracicaba, SP, 13416-000, Brazil.
| | - Ricardo Ribeiro Rodrigues
- University of São Paulo, "Luiz de Queiroz" College of Agriculture, Laboratory of Ecology and Forest Restoration, 11 Pádua Dias Avenue, Piracicaba, SP, 13418-900, Brazil.
| | - Wim H van der Putten
- Netherlands Institute of Ecology, NIOO-KNAW, Department of Terrestrial Ecology, 6708, PB, Wageningen, Netherlands; Laboratory of Nematology, Wageningen University, P.O. Box 8123, 6700, ES, Wageningen, the Netherlands.
| | - Siu Mui Tsai
- University of São Paulo, Center for Nuclear Energy in Agriculture, Cell and Molecular Biology Laboratory, 303 Centenário Avenue, Piracicaba, SP, 13416-000, Brazil.
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Shi W, Tang S, Zhang S. Microbiome of High-Rank Coal Reservoirs in the High-Production Areas of the Southern Qinshui Basin. Microorganisms 2023; 11:microorganisms11020497. [PMID: 36838462 PMCID: PMC9963281 DOI: 10.3390/microorganisms11020497] [Citation(s) in RCA: 2] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/29/2022] [Revised: 02/09/2023] [Accepted: 02/15/2023] [Indexed: 02/19/2023] Open
Abstract
To study the distribution features of microorganisms in distinct hydrological areas of the southern Qinshui Basin, C-N-S microorganisms were studied using 16S RNA sequencing, metagenome sequencing and geochemical technologies, showing the high sensitivity of microorganisms to the hydrodynamic dynamics of coal. The hydrodynamic intensity of the #3 coal gradually decreased from the runoff areas to the stagnant areas. The stagnant zones have higher reservoir pressure, methane content, δ13CDIC and TDS and lower SO42-, Fe3+ and NO3- concentrations than the runoff areas. C-N-S-cycling microorganisms, including those engaged in methanogenesis, nitrate respiration, fermentation, nitrate reduction, dark oxidation of sulfur compounds, sulfate respiration, iron respiration, chlorate reduction, aromatic compound degradation, denitrification, ammonification and nitrogen fixation, were more abundant in the stagnant areas. The relative abundance of C-N-S functional genes, including genes related to C metabolism (e.g., mcr, mer, mtr, fwd and mtd), N metabolism (e.g., nifDKH, nirK, narGHI, nosZ, amoB, norC and napAB) and sulfur metabolism (e.g., dsrAB and PAPSS), increased in the stagnant zones, indicating that there was active microbiological C-N-S cycling in the stagnant areas. The degradation and fermentation of terrestrial plant organic carbon and coal seam organic matter could provide substrates for methanogens, while nitrogen fixation and nitrification can provide nitrogen for methanogens, which are all favorable factors for stronger methanogenesis in stagnant areas. The coal in the study area is currently in the secondary biogenic gas generation stage because of the rising of the strata, which recharges atmospheric precipitation. The random forest model shows that the abundance of C-N-S microorganisms and genes could be used to distinguish different hydrological zones in coal reservoirs. Since stagnant zones are usually high-gas-bearing zones and high-production areas of CBM exploration, these microbiological indicators can be used as effective parameters to identify high-production-potential zones. In addition, nitrate respiration and sulfate respiration microorganisms consumed NO3- and SO42-, causing a decrease in the content of these two ions in the stagnant areas.
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Affiliation(s)
- Wei Shi
- MOE Key Lab of Marine Reservoir Evolution and Hydrocarbon Enrichment Mechanism, Beijing 100083, China
- MOLR Key Lab of Shale Gas Resources Survey and Strategic Evaluation, Beijing 100083, China
- School of Energy Resources, China University of Geosciences (Beijing), Beijing 100083, China
| | - Shuheng Tang
- MOE Key Lab of Marine Reservoir Evolution and Hydrocarbon Enrichment Mechanism, Beijing 100083, China
- MOLR Key Lab of Shale Gas Resources Survey and Strategic Evaluation, Beijing 100083, China
- School of Energy Resources, China University of Geosciences (Beijing), Beijing 100083, China
- Correspondence:
| | - Songhang Zhang
- MOE Key Lab of Marine Reservoir Evolution and Hydrocarbon Enrichment Mechanism, Beijing 100083, China
- MOLR Key Lab of Shale Gas Resources Survey and Strategic Evaluation, Beijing 100083, China
- School of Energy Resources, China University of Geosciences (Beijing), Beijing 100083, China
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Leal ODA, Jiménez-Morillo NT, González-Pérez JA, Knicker H, de Souza Costa F, Jiménez-Morillo PN, de Carvalho Júnior JA, dos Santos JC, Pinheiro Dick D. Soil Organic Matter Molecular Composition Shifts Driven by Forest Regrowth or Pasture after Slash-and-Burn of Amazon Forest. INTERNATIONAL JOURNAL OF ENVIRONMENTAL RESEARCH AND PUBLIC HEALTH 2023; 20:3485. [PMID: 36834184 PMCID: PMC9962374 DOI: 10.3390/ijerph20043485] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 01/06/2023] [Revised: 02/11/2023] [Accepted: 02/15/2023] [Indexed: 06/18/2023]
Abstract
Slash-and-burn of Amazon Forest (AF) for pasture establishment has increased the occurrence of AF wildfires. Recent studies emphasize soil organic matter (SOM) molecular composition as a principal driver of post-fire forest regrowth and restoration of AF anti-wildfire ambience. Nevertheless, SOM chemical shifts caused by AF fires and post-fire vegetation are rarely investigated at a molecular level. We employed pyrolysis-gas chromatography-mass spectrometry to reveal molecular changes in SOM (0-10, 40-50 cm depth) of a slash-burn-and-20-month-regrowth AF (BAF) and a 23-year Brachiaria pasture post-AF fire (BRA) site compared to native AF (NAF). In BAF (0-10 cm), increased abundance of unspecific aromatic compounds (UACs), polycyclic aromatic hydrocarbons (PAHs) and lipids (Lip) coupled with a depletion of polysaccharides (Pol) revealed strong lingering effects of fire on SOM. This occurs despite fresh litter deposition on soil, suggesting SOM minimal recovery and toxicity to microorganisms. Accumulation of recalcitrant compounds and slow decomposition of fresh forest material may explain the higher carbon content in BAF (0-5 cm). In BRA, SOM was dominated by Brachiaria contributions. At 40-50 cm, alkyl and hydroaromatic compounds accumulated in BRA, whereas UACs accumulated in BAF. UACs and PAH compounds were abundant in NAF, possibly air-transported from BAF.
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Affiliation(s)
- Otávio dos Anjos Leal
- Institute of Bio- and Geosciences—Agrosphere (IBG-3), Forschungszentrum Jülich GmbH, Wilhelm-Johnen-Straße, 52428 Jülich, Germany
| | - Nicasio T. Jiménez-Morillo
- Mediterranean Institute for Agriculture, Environment and Development-MED, Universidade de Évora, Ap 94, 7002-554 Évora, Portugal
- Instituto de Recursos Naturales y Agrobiología de Sevilla (IRNAS-CSIC), Av. Reina Mercedes 10, 41012 Seville, Spain
| | - José A. González-Pérez
- Instituto de Recursos Naturales y Agrobiología de Sevilla (IRNAS-CSIC), Av. Reina Mercedes 10, 41012 Seville, Spain
| | - Heike Knicker
- Instituto de Recursos Naturales y Agrobiología de Sevilla (IRNAS-CSIC), Av. Reina Mercedes 10, 41012 Seville, Spain
| | | | - Pedro N. Jiménez-Morillo
- Departamento de Sistemas Físicos, Químicos y Biológicos, Universidad Pablo de Olavide, Ctra. Utrera, 1, 41013 Seville, Spain
| | - João Andrade de Carvalho Júnior
- Departamento de Energia, Universidade Estadual Paulista, Av. Ariberto Pereira da Cunha, 333, Portal das Colinas, Guaratinguetá 12516-410, Brazil
| | - José Carlos dos Santos
- Laboratório Associado de Combustão e Propulsão, Instituto Nacional de Pesquisas Espaciais (INPE), Rodovia Presidente Dutra, km 40, Cachoeira Paulista 12630-00, Brazil
| | - Deborah Pinheiro Dick
- Departamento de Química, Universidade Federal do Rio Grande do Sul, Av. Bento Gonçalves, 9500, Porto Alegre 91501-970, Brazil
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Fonseca de Souza L, Alvarez DO, Domeignoz-Horta LA, Gomes FV, de Souza Almeida C, Merloti LF, Mendes LW, Andreote FD, Bohannan BJM, Mazza Rodrigues JL, Nüsslein K, Tsai SM. Maintaining grass coverage increases methane uptake in Amazonian pastures, with a reduction of methanogenic archaea in the rhizosphere. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 838:156225. [PMID: 35623507 DOI: 10.1016/j.scitotenv.2022.156225] [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: 03/08/2022] [Revised: 05/20/2022] [Accepted: 05/21/2022] [Indexed: 06/15/2023]
Abstract
Cattle ranching is the largest driver of deforestation in the Brazilian Amazon. The rainforest-to-pasture conversion affects the methane cycle in upland soils, changing it from sink to source of atmospheric methane. However, it remains unknown if management practices could reduce the impact of land-use on methane cycling. In this work, we evaluated how pasture management can regulate the soil methane cycle either by maintaining continuous grass coverage on pasture soils, or by liming the soil to amend acidity. Methane fluxes from forest and pasture soils were evaluated in moisture-controlled greenhouse experiments with and without grass cover (Urochloa brizantha cv. Marandu) or liming. We also assessed changes in the soil microbial community structure of both bare (bulk) and rhizospheric pasture soils through high throughput sequencing of the 16S rRNA gene, and quantified the methane cycling microbiota by their respective marker genes related to methane generation (mcrA) or oxidation (pmoA). The experiments used soils from eastern and western Amazonia, and concurrent field studies allowed us to confirm greenhouse data. The presence of a grass cover not only increased methane uptake by up to 35% in pasture soils, but also reduced the abundance of the methane-producing community. In the grass rhizosphere this reduction was up to 10-fold. Methane-producing archaea belonged to the genera Methanosarcina sp., Methanocella sp., Methanobacterium sp., and Rice Cluster I. Further, we showed that soil liming to increasing pH compromised the capacity of forest and pasture soils to be a sink for methane, and instead converted formerly methane-consuming forest soils to become methane sources in only 40-80 days. Liming reduced the relative abundance of Beijerinckiacea family in forest soils, which account for many known methanotrophs. Our results demonstrate that pasture management that maintains grass coverage can mitigate soil methane emissions, compared to bare (bulk) pasture soil.
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Affiliation(s)
- Leandro Fonseca de Souza
- Center for Nuclear Energy in Agriculture, University of Sao Paulo, Piracicaba, SP, Brazil; Department of Microbiology, University of Massachusetts, Amherst, MA, USA.
| | - Dasiel Obregon Alvarez
- Center for Nuclear Energy in Agriculture, University of Sao Paulo, Piracicaba, SP, Brazil; Applied Soil Ecology Lab, School of Environmental Sciences, University of Guelph, Guelph, ON, Canada
| | - Luiz A Domeignoz-Horta
- Department of Microbiology, University of Massachusetts, Amherst, MA, USA; Department of Evolutionary Biology and Environmental Studies, University of Zurich, Zurich, Switzerland
| | - Fabio Vitorino Gomes
- Center for Nuclear Energy in Agriculture, University of Sao Paulo, Piracicaba, SP, Brazil
| | | | - Luis Fernando Merloti
- Center for Nuclear Energy in Agriculture, University of Sao Paulo, Piracicaba, SP, Brazil
| | - Lucas William Mendes
- Center for Nuclear Energy in Agriculture, University of Sao Paulo, Piracicaba, SP, Brazil
| | | | | | | | - Klaus Nüsslein
- Department of Microbiology, University of Massachusetts, Amherst, MA, USA
| | - Siu Mui Tsai
- Center for Nuclear Energy in Agriculture, University of Sao Paulo, Piracicaba, SP, Brazil
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8
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Venturini AM, Dias NMS, Gontijo JB, Yoshiura CA, Paula FS, Meyer KM, Nakamura FM, da França AG, Borges CD, Barlow J, Berenguer E, Nüsslein K, Rodrigues JLM, Bohannan BJM, Tsai SM. Increased soil moisture intensifies the impacts of forest-to-pasture conversion on methane emissions and methane-cycling communities in the Eastern Amazon. ENVIRONMENTAL RESEARCH 2022; 212:113139. [PMID: 35337832 DOI: 10.1016/j.envres.2022.113139] [Citation(s) in RCA: 9] [Impact Index Per Article: 4.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/06/2021] [Revised: 02/24/2022] [Accepted: 03/15/2022] [Indexed: 06/14/2023]
Abstract
Climatic changes are altering precipitation patterns in the Amazon and may influence soil methane (CH4) fluxes due to the differential responses of methanogenic and methanotrophic microorganisms. However, it remains unclear if these climate feedbacks can amplify land-use-related impacts on the CH4 cycle. To better predict the responses of soil CH4-cycling microorganisms and emissions under altered moisture levels in the Eastern Brazilian Amazon, we performed a 30-day microcosm experiment manipulating the moisture content (original moisture; 60%, 80%, and 100% of field capacity - FC) of forest and pasture soils. Gas samples were collected periodically for gas chromatography analysis, and methanogenic archaeal and methanotrophic bacterial communities were assessed using quantitative PCR and metagenomics. Positive and negative daily CH4 fluxes were observed for forest and pasture, indicating that these soils can act as both CH4 sources and sinks. Cumulative emissions and the abundance of methanogenesis-related genes and taxonomic groups were affected by land use, moisture, and their interaction. Pasture soils at 100% FC had the highest abundance of methanogens and CH4 emissions, 22 times higher than forest soils under the same treatment. Higher ratios of methanogens to methanotrophs were found in pasture than in forest soils, even at field capacity conditions. Land use and moisture were significant factors influencing the composition of methanogenic and methanotrophic communities. The diversity and evenness of methanogens did not change throughout the experiment. In contrast, methanotrophs exhibited the highest diversity and evenness in pasture soils at 100% FC. Taken together, our results suggest that increased moisture exacerbates soil CH4 emissions and microbial responses driven by land-use change in the Amazon. This is the first report on the microbial CH4 cycle in Amazonian upland soils that combined one-month gas measurements with advanced molecular methods.
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Affiliation(s)
- Andressa M Venturini
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, 13416-000, Brazil; Princeton Institute for International and Regional Studies, Princeton University, Princeton, NJ, 08544, USA.
| | - Naissa M S Dias
- Environmental Biogeochemistry Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, 13416-000, Brazil
| | - Júlia B Gontijo
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, 13416-000, Brazil
| | - Caio A Yoshiura
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, 13416-000, Brazil
| | - Fabiana S Paula
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, 13416-000, Brazil; Department of Biological Oceanography, Oceanographic Institute, University of São Paulo, São Paulo, SP, 05508-120, Brazil
| | - Kyle M Meyer
- Institute of Ecology and Evolution, University of Oregon, Eugene, OR, 97403, USA; Department of Integrative Biology, University of California - Berkeley, Berkeley, CA, 94720, USA
| | - Fernanda M Nakamura
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, 13416-000, Brazil
| | - Aline G da França
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, 13416-000, Brazil
| | - Clovis D Borges
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, 13416-000, Brazil
| | - Jos Barlow
- Lancaster Environment Centre, Lancaster University, Lancaster, LA1 4YQ, UK
| | - Erika Berenguer
- Lancaster Environment Centre, Lancaster University, Lancaster, LA1 4YQ, UK; Environmental Change Institute, University of Oxford, Oxford, OX1 3QY, UK
| | - Klaus Nüsslein
- Department of Microbiology, University of Massachusetts, Amherst, MA, 01003, USA
| | - Jorge L M Rodrigues
- Department of Land, Air, and Water Resources, University of California - Davis, Davis, CA, 95616, USA
| | - Brendan J M Bohannan
- Institute of Ecology and Evolution, University of Oregon, Eugene, OR, 97403, USA
| | - Siu M Tsai
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, 13416-000, Brazil
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9
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Venturini AM, Gontijo JB, Mandro JA, Paula FS, Yoshiura CA, da França AG, Tsai SM. Genome-resolved metagenomics reveals novel archaeal and bacterial genomes from Amazonian forest and pasture soils. Microb Genom 2022; 8. [PMID: 35894927 PMCID: PMC9455692 DOI: 10.1099/mgen.0.000853] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/28/2022] Open
Abstract
Amazonian soil microbial communities are known to be affected by the forest-to-pasture conversion, but the identity and metabolic potential of most of their organisms remain poorly characterized. To contribute to the understanding of these communities, here we describe metagenome-assembled genomes (MAGs) recovered from 12 forest and pasture soil metagenomes of the Brazilian Eastern Amazon. We obtained 11 forest and 30 pasture MAGs (≥50% of completeness and ≤10 % of contamination), distributed among two archaeal and 11 bacterial phyla. The taxonomic classification results suggest that most MAGs may represent potential novel microbial taxa. MAGs selected for further evaluation included members of Acidobacteriota, Actinobacteriota, Desulfobacterota_B, Desulfobacterota_F, Dormibacterota, Eremiobacterota, Halobacteriota, Proteobacteria, and Thermoproteota, thus revealing their roles in carbohydrate degradation and mercury detoxification as well as in the sulphur, nitrogen, and methane cycles. A methane-producing Archaea of the genus Methanosarcina was almost exclusively recovered from pasture soils, which can be linked to a sink-to-source shift after the forest-to-pasture conversion. The novel MAGs constitute an important resource to help us unravel the yet-unknown microbial diversity in Amazonian soils and its functional potential and, consequently, the responses of these microorganisms to land-use change.
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Affiliation(s)
- Andressa M Venturini
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, Brazil.,Princeton Institute for International and Regional Studies, Princeton University, Princeton, NJ, USA
| | - Júlia B Gontijo
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, Brazil
| | - Jéssica A Mandro
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, Brazil
| | - Fabiana S Paula
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, Brazil.,Department of Biological Oceanography, Oceanographic Institute, University of São Paulo, São Paulo, SP, Brazil
| | - Caio A Yoshiura
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, Brazil
| | - Aline G da França
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, Brazil
| | - Siu M Tsai
- Cell and Molecular Biology Laboratory, Center for Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, SP, Brazil
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10
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Shi W, Tang S, Huang W, Zhang S, Li Z. Distribution Characteristics of C-N-S Microorganism Genes in Different Hydraulic Zones of High-Rank Coal Reservoirs in Southern Qinshui Basin. ACS OMEGA 2021; 6:21395-21409. [PMID: 34471743 PMCID: PMC8387991 DOI: 10.1021/acsomega.1c02169] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/26/2021] [Accepted: 08/02/2021] [Indexed: 06/03/2023]
Abstract
Microbial decomposition of carbon and biogenic methane in coal is one of the most important issues in CBM exploration. Using metagenomic technologies, the microbial C-N-S functional genes in different hydraulic zones of high-rank coal reservoirs were systematically studied, demonstrating the high sensitivity of this ecosystem to hydrodynamic conditions. The results show that the hydrodynamic strength of coal reservoir #3 in the Shizhuangnan block gradually weakened from east to west, forming a transitional feature from a runoff area to a stagnant area. Compared with runoff areas, stagnant areas have higher reservoir pressure, gas content, and ion concentrations. The relative abundance of genes associated with C, N, and S cycling increased from the runoff area to the stagnant area, including cellulose-degrading genes (e.g., cellulose 1,4-beta-cellobiosidase), methane metabolism genes (e.g., mcr, fwd, mtd, mer, and mtr), N-cycling genes (e.g., nifDKH, amoB, narGHI, napAB, nirK, norC, and nosZ), and S-cycling genes (e.g., dsrAB, sir, cysN, sat, aprAB, and PAPSS). This indicates that the stagnant zone had a more active microbial C-N-S cycle. The machine learning model shows that these significantly different genes could be used as effective indices to distinguish runoff and stagnant areas. Carbon and hydrogen isotopes indicate that methane in the study area was thermally generated. Methanogens compete with anaerobic heterotrophic bacteria to metabolize limited substrates, resulting in a low abundance of methanogens. In addition, the existence of methane-oxidizing bacteria suggests that biogenic methane was consumed by methanotrophic bacteria, which is the main reason why biogenic methane in the study area was not effectively preserved. In addition, weakened hydrodynamic conditions increased genes involved in nutrient cycling, including organic matter decomposition, methanogenesis, denitrification, and sulfate reduction, which contributed to the increase in CO2 and consumption of sulfate and nitrate from runoff areas to stagnant areas.
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Affiliation(s)
- Wei Shi
- MOE
Key Lab of Marine Reservoir Evolution and Hydrocarbon Enrichment Mechanism, China University of Geosciences, Beijing 100083, China
- MOLR
Key Lab of Shale Gas Resources Survey and Strategic Evaluation, China University of Geosciences, Beijing 100083, China
- School
of Energy Resources, China University of
Geosciences (Beijing), Beijing 100083, China
| | - Shuheng Tang
- MOE
Key Lab of Marine Reservoir Evolution and Hydrocarbon Enrichment Mechanism, China University of Geosciences, Beijing 100083, China
- MOLR
Key Lab of Shale Gas Resources Survey and Strategic Evaluation, China University of Geosciences, Beijing 100083, China
- School
of Energy Resources, China University of
Geosciences (Beijing), Beijing 100083, China
| | - Wenhui Huang
- MOE
Key Lab of Marine Reservoir Evolution and Hydrocarbon Enrichment Mechanism, China University of Geosciences, Beijing 100083, China
- MOLR
Key Lab of Shale Gas Resources Survey and Strategic Evaluation, China University of Geosciences, Beijing 100083, China
- School
of Energy Resources, China University of
Geosciences (Beijing), Beijing 100083, China
| | - Songhang Zhang
- MOE
Key Lab of Marine Reservoir Evolution and Hydrocarbon Enrichment Mechanism, China University of Geosciences, Beijing 100083, China
- MOLR
Key Lab of Shale Gas Resources Survey and Strategic Evaluation, China University of Geosciences, Beijing 100083, China
- School
of Energy Resources, China University of
Geosciences (Beijing), Beijing 100083, China
| | - Zhongcheng Li
- China
United Coalbed Methane Corporation Ltd., Beijing 100011, China
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11
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Microbial Communities in Methane Cycle: Modern Molecular Methods Gain Insights into Their Global Ecology. ENVIRONMENTS 2021. [DOI: 10.3390/environments8020016] [Citation(s) in RCA: 11] [Impact Index Per Article: 3.7] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/16/2022]
Abstract
The role of methane as a greenhouse gas in the concept of global climate changes is well known. Methanogens and methanotrophs are two microbial groups which contribute to the biogeochemical methane cycle in soil, so that the total emission of CH4 is the balance between its production and oxidation by microbial communities. Traditional identification techniques, such as selective enrichment and pure-culture isolation, have been used for a long time to study diversity of methanogens and methanotrophs. However, these techniques are characterized by significant limitations, since only a relatively small fraction of the microbial community could be cultured. Modern molecular methods for quantitative analysis of the microbial community such as real-time PCR (Polymerase chain reaction), DNA fingerprints and methods based on high-throughput sequencing together with different “omics” techniques overcome the limitations imposed by culture-dependent approaches and provide new insights into the diversity and ecology of microbial communities in the methane cycle. Here, we review available knowledge concerning the abundances, composition, and activity of methanogenic and methanotrophic communities in a wide range of natural and anthropogenic environments. We suggest that incorporation of microbial data could fill the existing microbiological gaps in methane flux modeling, and significantly increase the predictive power of models for different environments.
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