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Ni B, Yu X, Duan X, Zou Y. Wetland soil organic carbon balance is reversed by old carbon and iron oxide additions. Front Microbiol 2024; 14:1327265. [PMID: 38260908 PMCID: PMC10800826 DOI: 10.3389/fmicb.2023.1327265] [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: 10/24/2023] [Accepted: 12/18/2023] [Indexed: 01/24/2024] Open
Abstract
Iron (Fe) oxides can stabilize organic carbon (OC) through adsorption and co-precipitation, while microbial Fe reduction can disrupt Fe-bound OC (Fe-OC) and further increase OC mineralization. The net effects of OC preservation and mineralization mediated by Fe oxides are still unclear, especially for old carbon (formed from plant litters over millions of years) and crystalline Fe oxides. Accelerating the recovery of wetland carbon sinks is critical for mitigating climate change and achieving carbon neutrality. Quantifying the net effect of Fe-mediated OC mineralization and preservation is vital for understanding the role of crystalline Fe oxides in carbon cycling and promoting the recovery of soil carbon sinks. Here, we explored the OC balances mediated by hematite (Hem) and lignite addition (Lig) to freshwater wetland (FW, rich in C and Fe) and saline-alkaline wetland (SW, poor in C and Fe) soil slurries, incubated under anaerobic conditions. Results showed that Lig caused net OC accumulation (FW: 5.9 ± 3.6 mg g-1; SW: 8.3 ± 3.2 mg g-1), while Hem caused dramatic OC loss, particularly in the FW soils. Hem inhibited microbial Fe(III) reduction by decreasing the relative abundance of Fe respiration reducers, while substantially enhancing OC mineralization through the shift in the microbial community structure of FW soils. Lig resulted in carbon emission, but its contribution to preservation by the formation of Fe-OC was far higher than that which caused OC loss. We concluded that crystalline Fe oxide addition solely favored the increase of OC mineralization by adjusting the microbial community structure, while old carbon enriched with an aromatic and alkyl promoted Fe-OC formation and further increased OC persistence. Our findings could be employed for wetland restoration, particularly for the recovery of soil carbon sinks.
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Affiliation(s)
- Bingbo Ni
- State Key Laboratory of Black Soils Conservation and Utilization and Heilongjiang Xingkai Lake Wetland Ecosystem National Observation and Research Station and Key Laboratory of Wetland Ecology and Environment and Jilin Provincial Joint Key Laboratory of Changbai Mountain Wetland and Ecology, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, China
- University of Chinese Academy of Sciences, Beijing, China
| | - Xiaofei Yu
- State Environmental Protection Key Laboratory for Wetland Conservation and Vegetation Restoration and Jilin Provincial Key Laboratory of Ecological Restoration and Ecosystem Management and Key Laboratory of Vegetation Ecology of Ministry of Education, School of Environment, Northeast Normal University, Changchun, China
| | - Xun Duan
- State Key Laboratory of Black Soils Conservation and Utilization and Heilongjiang Xingkai Lake Wetland Ecosystem National Observation and Research Station and Key Laboratory of Wetland Ecology and Environment and Jilin Provincial Joint Key Laboratory of Changbai Mountain Wetland and Ecology, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, China
- University of Chinese Academy of Sciences, Beijing, China
| | - Yuanchun Zou
- State Key Laboratory of Black Soils Conservation and Utilization and Heilongjiang Xingkai Lake Wetland Ecosystem National Observation and Research Station and Key Laboratory of Wetland Ecology and Environment and Jilin Provincial Joint Key Laboratory of Changbai Mountain Wetland and Ecology, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, China
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2
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Videvall E, Burraco P, Orizaola G. Impact of ionizing radiation on the environmental microbiomes of Chornobyl wetlands. ENVIRONMENTAL POLLUTION (BARKING, ESSEX : 1987) 2023; 330:121774. [PMID: 37178954 DOI: 10.1016/j.envpol.2023.121774] [Citation(s) in RCA: 7] [Impact Index Per Article: 7.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/17/2023] [Revised: 04/21/2023] [Accepted: 05/02/2023] [Indexed: 05/15/2023]
Abstract
Radioactive contamination has the potential to cause damage to DNA and other biomolecules. Anthropogenic sources of radioactive contamination include accidents in nuclear power plants, such as the one in Chornobyl in 1986 which caused long-term radioactive pollution. Studies on animals within radioactive zones have provided us with a greater understanding of how wildlife can persevere despite chronic radiation exposure. However, we still know very little about the effects of radiation on the microbial communities in the environment. We examined the impact of ionizing radiation and other environmental factors on the diversity and composition of environmental microbiomes in the wetlands of Chornobyl. We combined detailed field sampling along a gradient of radiation together with 16 S rRNA high-throughput metabarcoding. While radiation did not affect the alpha diversity of the microbiomes in sediment, soil, or water, it had a significant effect on the beta diversity in all environment types, indicating that the microbial composition was affected by ionizing radiation. Specifically, we detected several microbial taxa that were more abundant in areas with high radiation levels within the Chornobyl Exclusion Zone, including bacteria and archaea known to be radioresistant. Our results reveal the existence of rich and diverse microbiomes in Chornobyl wetlands, with multiple taxonomic groups that are able to thrive despite the radioactive contamination. These results, together with additional field and laboratory-based approaches examining how microbes cope with ionizing radiation will help to forecast the functionality and re-naturalization dynamics of radiocontaminated environments.
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Affiliation(s)
- Elin Videvall
- Department of Ecology, Evolution and Organismal Biology, Brown University, Providence, RI, 02912, USA; Institute at Brown for Environment and Society, Brown University, Providence, RI, 02912, USA; Center for Conservation Genomics, Smithsonian Conservation Biology Institute, 20013, Washington, DC, USA; Animal Ecology, Department of Ecology and Genetics, Evolutionary Biology Centre, Uppsala University, 75236, Uppsala, Sweden
| | - Pablo Burraco
- Animal Ecology, Department of Ecology and Genetics, Evolutionary Biology Centre, Uppsala University, 75236, Uppsala, Sweden; Doñana Biological Station, Spanish Research Council (EBD-CSIC), 41092, Sevilla, Spain
| | - Germán Orizaola
- IMIB-Biodiversity Research Institute (Univ. Oviedo-CSIC-Princip. Asturias), 33600, Mieres, Asturias, Spain; Zoology Unit, Department of Biology of Organisms and Systems, University of Oviedo, 33071, Oviedo, Asturias, Spain.
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3
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Zhou N, Kupper RJ, Catalano JG, Thompson A, Chan CS. Biological Oxidation of Fe(II)-Bearing Smectite by Microaerophilic Iron Oxidizer Sideroxydans lithotrophicus Using Dual Mto and Cyc2 Iron Oxidation Pathways. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2022; 56:17443-17453. [PMID: 36417801 PMCID: PMC9731265 DOI: 10.1021/acs.est.2c05142] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/18/2022] [Revised: 10/03/2022] [Accepted: 10/24/2022] [Indexed: 06/16/2023]
Abstract
Fe(II) clays are common across many environments, making them a potentially significant microbial substrate, yet clays are not well established as an electron donor. Therefore, we explored whether Fe(II)-smectite supports the growth of Sideroxydans lithotrophicus ES-1, a microaerophilic Fe(II)-oxidizing bacterium (FeOB), using synthesized trioctahedral Fe(II)-smectite and 2% oxygen. S. lithotrophicus grew substantially and can oxidize Fe(II)-smectite to a higher extent than abiotic oxidation, based on X-ray near-edge spectroscopy (XANES). Sequential extraction showed that edge-Fe(II) is oxidized before interior-Fe(II) in both biotic and abiotic experiments. The resulting Fe(III) remains in smectite, as secondary minerals were not detected in biotic and abiotic oxidation products by XANES and Mössbauer spectroscopy. To determine the genes involved, we compared S. lithotrophicus grown on smectite versus Fe(II)-citrate using reverse-transcription quantitative PCR and found that cyc2 genes were highly expressed on both substrates, while mtoA was upregulated on smectite. Proteomics confirmed that Mto proteins were only expressed on smectite, indicating that ES-1 uses the Mto pathway to access solid Fe(II). We integrate our results into a biochemical and mineralogical model of microbial smectite oxidation. This work increases the known substrates for FeOB growth and expands the mechanisms of Fe(II)-smectite alteration in the environment.
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Affiliation(s)
- Nanqing Zhou
- School
of Marine Science and Policy, University
of Delaware, Newark, Delaware 19716, United
States
| | - Robert J. Kupper
- Department
of Earth and Planetary Sciences, Washington
University in St. Louis, Saint
Louis, Missouri 63130, United States
| | - Jeffrey G. Catalano
- Department
of Earth and Planetary Sciences, Washington
University in St. Louis, Saint
Louis, Missouri 63130, United States
| | - Aaron Thompson
- Department
of Crop and Soil Sciences, University of
Georgia, Athens, Georgia 30602, United States
| | - Clara S. Chan
- School
of Marine Science and Policy, University
of Delaware, Newark, Delaware 19716, United
States
- Department
of Earth Sciences, University of Delaware, Newark, Delaware 19716, United States
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4
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Chakraborty A, Suchy M, Hubert CRJ, Ryan MC. Vertical stratification of microbial communities and isotope geochemistry tie groundwater denitrification to sampling location within a nitrate-contaminated aquifer. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 820:153092. [PMID: 35038526 DOI: 10.1016/j.scitotenv.2022.153092] [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: 08/06/2021] [Revised: 12/29/2021] [Accepted: 01/09/2022] [Indexed: 06/14/2023]
Abstract
Nitrate pollution is a major threat to groundwater quality in agricultural areas. Natural attenuation of nitrate in contaminated aquifers is mediated by denitrifying microbial populations in anoxic environments. Vertical distribution of denitrifying microbial communities in aquifers is greatly influenced by groundwater redox conditions, local hydrogeological parameters, and seasonal variability in groundwater flow and recharge. In this study, we investigated groundwater geochemistry and the composition of bacterial and archaeal communities with increasing depth in a shallow nitrate-contaminated aquifer in British Columbia, Canada. High-resolution passive diffusion sampling was conducted to collect groundwater at 10-cm intervals from 4 to 20 m below ground surface (mbgs) in the aquifer. Geochemical analyses of major ions indicated a general shift in the groundwater chemistry below 16 mbgs including decreasing chloride concentrations that suggest two-end member mixing of shallow and deep groundwater with different chemistries. A redoxcline was further observed within a 2 m transition zone at 18-20 mbgs characterized by sharp declines in nitrate concentrations and increases in sulfate and total inorganic carbon. Excursions in δ15N-NO3- and δ18O-NO3- in the same depth interval are consistent with denitrification, and a concomitant decrease in δ34S-SO42- suggested that denitrification was coupled to sulfide or sulfur oxidation. Microbial communities within this depth interval were significantly dissimilar to those above and below, featuring putative lithotrophic denitrifying bacteria belonging to the genera Sulfurifustis, Sulfuritalea and Sulfuricella. These lineages were detected in greatest abundance at 19 mbgs while the abundances of putative heterotrophic sulfate-reducing bacteria belonging to the genus Desulfosporosinus were greatest at 20 mbgs. In addition to help distinguish denitrification from mixing-induced changes in groundwater chemistry, the above observed vertical stratification of the microbial key players connects nitrate removal to the locations of the aquifer sampled.
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Affiliation(s)
- Anirban Chakraborty
- Department of Biological Sciences, University of Calgary, Calgary, Alberta, Canada.
| | - Martin Suchy
- Environment and Climate Change Canada, Vancouver, British Columbia, Canada
| | - Casey R J Hubert
- Department of Biological Sciences, University of Calgary, Calgary, Alberta, Canada
| | - M Cathryn Ryan
- Department of Geoscience, University of Calgary, Calgary, Alberta, Canada
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5
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Napieralski SA, Fang Y, Marcon V, Forsythe B, Brantley SL, Xu H, Roden EE. Microbial chemolithotrophic oxidation of pyrite in a subsurface shale weathering environment: Geologic considerations and potential mechanisms. GEOBIOLOGY 2022; 20:271-291. [PMID: 34633148 DOI: 10.1111/gbi.12474] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/18/2021] [Revised: 09/02/2021] [Accepted: 09/27/2021] [Indexed: 06/13/2023]
Abstract
Oxidative weathering of pyrite plays an important role in the biogeochemical cycling of Fe and S in terrestrial environments. While the mechanism and occurrence of biologically accelerated pyrite oxidation under acidic conditions are well established, much less is known about microbially mediated pyrite oxidation at circumneutral pH. Recent work (Percak-Dennett et al., 2017, Geobiology, 15, 690) has demonstrated the ability of aerobic chemolithotrophic microorganisms to accelerate pyrite oxidation at circumneutral pH and proposed two mechanistic models by which this phenomenon might occur. Here, we assess the potential relevance of aerobic microbially catalyzed circumneutral pH pyrite oxidation in relation to subsurface shale weathering at Susquehanna Shale Hills Critical Zone Observatory (SSHCZO) in Pennsylvania, USA. Specimen pyrite mixed with native shale was incubated in groundwater for 3 months at the inferred depth of in situ pyrite oxidation. The colonized materials were used as an inoculum for pyrite-oxidizing enrichment cultures. Microbial activity accelerated the release of sulfate across all conditions. 16S rRNA gene sequencing and metagenomic analysis revealed the dominance of a putative chemolithoautotrophic sulfur-oxidizing bacterium from the genus Thiobacillus in the enrichment cultures. Previously proposed models for aerobic microbial pyrite oxidation were assessed in terms of physical constraints, enrichment culture geochemistry, and metagenomic analysis. Although we conclude that subsurface pyrite oxidation at SSCHZO is largely abiotic, this work nonetheless yields new insight into the potential pathways by which aerobic microorganisms may accelerate pyrite oxidation at circumneutral pH. We propose a new "direct sulfur oxidation" pathway, whereby sulfhydryl-bearing outer membrane proteins mediate oxidation of pyrite surfaces through a persulfide intermediate, analogous to previously proposed mechanisms for direct microbial oxidation of elemental sulfur. The action of this and other direct microbial pyrite oxidation pathways have major implications for controls on pyrite weathering rates in circumneutral pH sedimentary environments where pore throat sizes permit widespread access of microorganisms to pyrite surfaces.
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Affiliation(s)
| | - Yihang Fang
- Department of Geoscience, University of Wisconsin-Madison, Madison, Wisconsin, USA
| | - Virginia Marcon
- Earth and Environmental Systems Institute, University Park, Pennsylvania, USA
- The Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania, USA
| | - Brandon Forsythe
- Earth and Environmental Systems Institute, University Park, Pennsylvania, USA
| | - Susan L Brantley
- Earth and Environmental Systems Institute, University Park, Pennsylvania, USA
- The Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania, USA
| | - Huifang Xu
- Department of Geoscience, University of Wisconsin-Madison, Madison, Wisconsin, USA
| | - Eric E Roden
- Department of Geoscience, University of Wisconsin-Madison, Madison, Wisconsin, USA
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6
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Mujica-Alarcon JF, Thornton SF, Rolfe SA. Long-term dynamic changes in attached and planktonic microbial communities in a contaminated aquifer. ENVIRONMENTAL POLLUTION (BARKING, ESSEX : 1987) 2021; 277:116765. [PMID: 33647805 DOI: 10.1016/j.envpol.2021.116765] [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: 10/09/2020] [Revised: 02/12/2021] [Accepted: 02/13/2021] [Indexed: 06/12/2023]
Abstract
Biodegradation is responsible for most contaminant removal in plumes of organic compounds and is fastest at the plume fringe where microbial cell numbers and activity are highest. As the plume migrates from the source, groundwater containing the contaminants and planktonic microbial community encounters uncontaminated substrata on which an attached community subsequently develops. While attached microbial communities are important for biodegradation, the time needed for their establishment, their relationship with the planktonic community and the processes controlling their development are not well understood. We compare the dynamics of development of attached microbial communities on sterile substrata in the field and laboratory microcosms, sampled simultaneously at intervals over two years. We show that attached microbial cell numbers increased rapidly and stabilised after similar periods of incubation (∼100 days) in both field and microcosm experiments. These timescales were similar even though variation in the contaminant source evident in the field was absent in microcosm studies, implying that this period was an emergent property of the attached microbial community. 16S rRNA gene sequencing showed that attached and planktonic communities differed markedly, with many attached organisms strongly preferring attachment. Successional processes were evident, both in community diversity indices and from community network analysis. Community development was governed by both deterministic and stochastic processes and was related to the predilection of community members for different lifestyles and the geochemical environment.
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Affiliation(s)
- Juan F Mujica-Alarcon
- Groundwater Protection and Restoration Group, Department of Civil and Structural Engineering, University of Sheffield, Sheffield, United Kingdom; Department of Animal and Plant Sciences, University of Sheffield, Sheffield, United Kingdom
| | - Steven F Thornton
- Groundwater Protection and Restoration Group, Department of Civil and Structural Engineering, University of Sheffield, Sheffield, United Kingdom
| | - Stephen A Rolfe
- Department of Animal and Plant Sciences, University of Sheffield, Sheffield, United Kingdom.
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7
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Danczak RE, Johnston MD, Kenah C, Slattery M, Wilkins MJ. Capability for arsenic mobilization in groundwater is distributed across broad phylogenetic lineages. PLoS One 2019; 14:e0221694. [PMID: 31490939 PMCID: PMC6730927 DOI: 10.1371/journal.pone.0221694] [Citation(s) in RCA: 11] [Impact Index Per Article: 2.2] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/04/2018] [Accepted: 08/13/2019] [Indexed: 01/24/2023] Open
Abstract
Despite the importance of microbial activity in mobilizing arsenic in groundwater aquifers, the phylogenetic distribution of contributing microbial metabolisms is understudied. Groundwater samples from Ohio aquifers were analyzed using metagenomic sequencing to identify functional potential that could drive arsenic cycling, and revealed mechanisms for direct (i.e., Ars system) and indirect (i.e., iron reduction) arsenic mobilization in all samples, despite differing geochemical conditions. Analyses of 194 metagenome-assembled genomes (MAGs) revealed widespread functionality related to arsenic mobilization throughout the bacterial tree of life. While arsB and arsC genes (components of an arsenic resistance system) were found in diverse lineages with no apparent phylogenetic bias, putative aioA genes (aerobic arsenite oxidase) were predominantly identified in Methylocystaceae MAGs. Both previously described and undescribed respiratory arsenate reduction potential via arrA was detected in Betaproteobacteria, Deltaproteobacteria, and Nitrospirae MAGs, whereas sulfate reduction potential was primarily limited to members of the Deltaproteobacteria and Nitrospirae. Lastly, iron reduction potential was detected in the Ignavibacteria, Deltaproteobacteria, and Nitrospirae. These results expand the phylogenetic distribution of taxa that may play roles in arsenic mobilization in subsurface systems. Specifically, the Nitrospirae are a much more functionally diverse group than previously assumed and may play key biogeochemical roles in arsenic-contaminated ecosystems.
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Affiliation(s)
- Robert E. Danczak
- Department of Microbiology, Ohio State University, Columbus, OH, United States of America
| | - Michael D. Johnston
- School of Earth Sciences, Ohio State University, Columbus, OH, United States of America
| | - Chris Kenah
- Ohio Environmental Protection Agency, Columbus, OH, United States of America
| | - Michael Slattery
- Ohio Environmental Protection Agency, Columbus, OH, United States of America
| | - Michael J. Wilkins
- Department of Soil and Crop Sciences, Colorado State University, Fort Collins, CO, United States of America
- * E-mail:
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8
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Smith HJ, Zelaya AJ, De León KB, Chakraborty R, Elias DA, Hazen TC, Arkin AP, Cunningham AB, Fields MW. Impact of hydrologic boundaries on microbial planktonic and biofilm communities in shallow terrestrial subsurface environments. FEMS Microbiol Ecol 2018; 94:5107865. [PMID: 30265315 PMCID: PMC6192502 DOI: 10.1093/femsec/fiy191] [Citation(s) in RCA: 31] [Impact Index Per Article: 5.2] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/30/2018] [Accepted: 09/26/2018] [Indexed: 12/12/2022] Open
Abstract
Subsurface environments contain a large proportion of planetary microbial biomass and harbor diverse communities responsible for mediating biogeochemical cycles important to groundwater used by human society for consumption, irrigation, agriculture and industry. Within the saturated zone, capillary fringe and vadose zones, microorganisms can reside in two distinct phases (planktonic or biofilm), and significant differences in community composition, structure and activity between free-living and attached communities are commonly accepted. However, largely due to sampling constraints and the challenges of working with solid substrata, the contribution of each phase to subsurface processes is largely unresolved. Here, we synthesize current information on the diversity and activity of shallow freshwater subsurface habitats, discuss the challenges associated with sampling planktonic and biofilm communities across spatial, temporal and geological gradients, and discuss how biofilms may be constrained within shallow terrestrial subsurface aquifers. We suggest that merging traditional activity measurements and sequencing/-omics technologies with hydrological parameters important to sediment biofilm assembly and stability will help delineate key system parameters. Ultimately, integration will enhance our understanding of shallow subsurface ecophysiology in terms of bulk-flow through porous media and distinguish the respective activities of sessile microbial communities from more transient planktonic communities to ecosystem service and maintenance.
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Affiliation(s)
- H J Smith
- Center for Biofilm Engineering, Montana State University, Bozeman, MT
- ENIGMA (www.enigma.lbl.gov) Environmental Genomics and Systems Biology Division, Biosciences Area, Lawrence Berkeley National Laboratory, 1 Cyclotron Road, MS:977, Berkeley, CA 94720
| | - A J Zelaya
- Center for Biofilm Engineering, Montana State University, Bozeman, MT
- Department of Microbiology & Immunology, Montana State University, Bozeman, MT
- ENIGMA (www.enigma.lbl.gov) Environmental Genomics and Systems Biology Division, Biosciences Area, Lawrence Berkeley National Laboratory, 1 Cyclotron Road, MS:977, Berkeley, CA 94720
| | - K B De León
- Department of Biochemistry, University of Missouri, Columbia, MO
- ENIGMA (www.enigma.lbl.gov) Environmental Genomics and Systems Biology Division, Biosciences Area, Lawrence Berkeley National Laboratory, 1 Cyclotron Road, MS:977, Berkeley, CA 94720
| | - R Chakraborty
- Climate and Ecosystems Science Division, Lawrence Berkeley National Laboratory, Berkeley, CA
- ENIGMA (www.enigma.lbl.gov) Environmental Genomics and Systems Biology Division, Biosciences Area, Lawrence Berkeley National Laboratory, 1 Cyclotron Road, MS:977, Berkeley, CA 94720
| | - D A Elias
- Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN
- ENIGMA (www.enigma.lbl.gov) Environmental Genomics and Systems Biology Division, Biosciences Area, Lawrence Berkeley National Laboratory, 1 Cyclotron Road, MS:977, Berkeley, CA 94720
| | - T C Hazen
- Department of Civil and Environmental Engineering, University of Tennessee, Knoxville, TN
- ENIGMA (www.enigma.lbl.gov) Environmental Genomics and Systems Biology Division, Biosciences Area, Lawrence Berkeley National Laboratory, 1 Cyclotron Road, MS:977, Berkeley, CA 94720
| | - A P Arkin
- Department of Bioengineering, Lawrence Berkeley National Laboratory, Berkeley, CA
- ENIGMA (www.enigma.lbl.gov) Environmental Genomics and Systems Biology Division, Biosciences Area, Lawrence Berkeley National Laboratory, 1 Cyclotron Road, MS:977, Berkeley, CA 94720
| | - A B Cunningham
- Center for Biofilm Engineering, Montana State University, Bozeman, MT
- Department of Civil Engineering, Montana State University, Montana State University, Bozeman, MT
| | - M W Fields
- Center for Biofilm Engineering, Montana State University, Bozeman, MT
- Department of Microbiology & Immunology, Montana State University, Bozeman, MT
- ENIGMA (www.enigma.lbl.gov) Environmental Genomics and Systems Biology Division, Biosciences Area, Lawrence Berkeley National Laboratory, 1 Cyclotron Road, MS:977, Berkeley, CA 94720
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9
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Whitman T, Neurath R, Perera A, Chu-Jacoby I, Ning D, Zhou J, Nico P, Pett-Ridge J, Firestone M. Microbial community assembly differs across minerals in a rhizosphere microcosm. Environ Microbiol 2018; 20:4444-4460. [PMID: 30047192 DOI: 10.1111/1462-2920.14366] [Citation(s) in RCA: 39] [Impact Index Per Article: 6.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/22/2018] [Revised: 07/20/2018] [Accepted: 07/20/2018] [Indexed: 11/30/2022]
Abstract
Mineral-associated microbes drive many critical soil processes, including mineral weathering, soil aggregation and cycling of mineral-sorbed organic matter. To investigate the interactions between soil minerals and microbes in the rhizosphere, we incubated three types of minerals (ferrihydrite, kaolinite and quartz) and a native soil mineral fraction near roots of a common Californian annual grass, Avena barbata, growing in its resident soil. We followed microbial colonization of these minerals for up to 2.5 months - the plant's lifespan. Bacteria and fungi that colonized mineral surfaces during this experiment differed across mineral types and differed from those in the background soil, implying that microbial colonization was the result of processes in addition to passive movement with water to mineral surfaces. Null model analysis revealed that dispersal limitation was a dominant factor structuring mineral-associated microbial communities for all mineral types. Once bacteria arrived at a mineral surface, capacity for rapid growth appeared important, as ribosomal copy number was significantly correlated with relative enrichment on minerals. Glomeromycota (a phylum associated with arbuscular mycorrhizal fungi) appeared to preferentially associate with ferrihydrite surfaces. The mechanisms enabling the colonization of soil minerals may be foundational in shaping the overall soil microbiome composition and development of persistent organic matter in soils.
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Affiliation(s)
- Thea Whitman
- Department of Environmental Science, Policy, and Management, University of California, Berkeley, Berkeley, CA, USA.,Department of Soil Science, University of Wisconsin-Madison, Madison, WI, USA
| | - Rachel Neurath
- Department of Environmental Science, Policy, and Management, University of California, Berkeley, Berkeley, CA, USA.,Lawrence Livermore National Laboratory, Physical and Life Science Directorate, Livermore, CA, USA
| | - Adele Perera
- Department of Environmental Science, Policy, and Management, University of California, Berkeley, Berkeley, CA, USA
| | - Ilexis Chu-Jacoby
- Department of Environmental Science, Policy, and Management, University of California, Berkeley, Berkeley, CA, USA
| | - Daliang Ning
- Consolidated Core Laboratory, University of Oklahoma, Norman, OK, USA.,Institute for Environmental Genomics, University of Oklahoma, Norman, OK, USA.,Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, USA
| | - Jizhong Zhou
- Institute for Environmental Genomics, University of Oklahoma, Norman, OK, USA.,Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, USA.,School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, OK, USA.,Lawrence Berkeley National Laboratory, Earth and Environmental Sciences, Berkeley, CA, USA.,State Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, China
| | - Peter Nico
- Lawrence Berkeley National Laboratory, Earth and Environmental Sciences, Berkeley, CA, USA
| | - Jennifer Pett-Ridge
- Lawrence Livermore National Laboratory, Physical and Life Science Directorate, Livermore, CA, USA
| | - Mary Firestone
- Department of Environmental Science, Policy, and Management, University of California, Berkeley, Berkeley, CA, USA.,Lawrence Berkeley National Laboratory, Earth and Environmental Sciences, Berkeley, CA, USA
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10
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Aquilina L, Roques C, Boisson A, Vergnaud-Ayraud V, Labasque T, Pauwels H, Pételet-Giraud E, Pettenati M, Dufresne A, Bethencourt L, Bour O. Autotrophic denitrification supported by biotite dissolution in crystalline aquifers (1): New insights from short-term batch experiments. THE SCIENCE OF THE TOTAL ENVIRONMENT 2018; 619-620:842-853. [PMID: 29734630 DOI: 10.1016/j.scitotenv.2017.11.079] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/15/2017] [Revised: 11/07/2017] [Accepted: 11/07/2017] [Indexed: 06/08/2023]
Abstract
We investigate denitrification mechanisms through batch experiments using crushed rock and groundwater from a granitic aquifer subject to long term pumping (Ploemeur, France). Except for sterilized experiments, extensive denitrification reaction induces NO3 decreases ranging from 0.3 to 0.6mmol/L. Carbon concentrations, either organic or inorganic, remain relatively stable and do not document potential heterotrophic denitrification. Batch experiments show a clear effect of mineral dissolution which is documented through cation (K, Na, Ca) and Fluoride production. These productions are tightly related to denitrification progress during the experiment. Conversely, limited amounts of SO4, systematically lower than autotrophic denitrification coupled to sulfur oxidation stoichiometry, are produced during the experiments which indicates that sulfur oxidation is not likely even when pyrite is added to the experiments. Analysis of cation ratios, both in isolated minerals of the granite and within water of the batch, allow the mineral dissolution during the experiments to be quantified. Using cation ratios, we show that batch experiments are characterized mainly by biotite dissolution. As biotite contains 21 to 30% of Fe and 0.3 to 1.7% of F, it constitutes a potential source for these two elements. Denitrification could be attributed to the oxidation of Fe(II) contained in biotite. We computed the amount of K and F produced through biotite dissolution when entirely attributing denitrification to biotite dissolution. Computed amounts show that this process may account for the observed K and F produced. We interpret these results as the development of microbial activity which induces mineral dissolution in order to uptake Fe(II) which is used for denitrification. Although pyrite is probably available, SO4 and cation measurements favor a large biotite dissolution reaction which could account for all the observed Fe production. Chemical composition of groundwater produced from the Ploemeur site indicates similar denitrification processes although original composition shows mainly plagioclase dissolution.
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Affiliation(s)
- Luc Aquilina
- Université Rennes 1 - CNRS, OSUR - Géosciences Rennes, Av. du Général Leclerc, 35 042 Rennes, France.
| | - Clément Roques
- ETH Zürich, Department of Earth Sciences, Sonneggstrasse 5, 8092 Zürich, Switzerland.
| | - Alexandre Boisson
- BRGM DAT Bretagne, Rennes Atalante Beaulieu 2 rue de Jouanet, 35700 Rennes, France
| | - Virginie Vergnaud-Ayraud
- Université Rennes 1 - CNRS, OSUR - Géosciences Rennes, Av. du Général Leclerc, 35 042 Rennes, France
| | - Thierry Labasque
- Université Rennes 1 - CNRS, OSUR - Géosciences Rennes, Av. du Général Leclerc, 35 042 Rennes, France
| | - Hélène Pauwels
- BRGM D3E, 3 av. Guillemin, BP 36009, 45060 Orléans Cedex 2, France
| | | | - Marie Pettenati
- BRGM D3E, 3 av. Guillemin, BP 36009, 45060 Orléans Cedex 2, France
| | - Alexis Dufresne
- Université Rennes 1 - CNRS, OSUR - Ecobio, Av. du Général Leclerc, 35 042 Rennes, France
| | - Lorine Bethencourt
- Université Rennes 1 - CNRS, OSUR - Ecobio, Av. du Général Leclerc, 35 042 Rennes, France
| | - Olivier Bour
- Université Rennes 1 - CNRS, OSUR - Géosciences Rennes, Av. du Général Leclerc, 35 042 Rennes, France
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Bray MS, Wu J, Reed BC, Kretz CB, Belli KM, Simister RL, Henny C, Stewart FJ, DiChristina TJ, Brandes JA, Fowle DA, Crowe SA, Glass JB. Shifting microbial communities sustain multiyear iron reduction and methanogenesis in ferruginous sediment incubations. GEOBIOLOGY 2017; 15:678-689. [PMID: 28419718 PMCID: PMC7780294 DOI: 10.1111/gbi.12239] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/13/2017] [Accepted: 03/17/2017] [Indexed: 05/16/2023]
Abstract
Reactive Fe(III) minerals can influence methane (CH4 ) emissions by inhibiting microbial methanogenesis or by stimulating anaerobic CH4 oxidation. The balance between Fe(III) reduction, methanogenesis, and CH4 oxidation in ferruginous Archean and Paleoproterozoic oceans would have controlled CH4 fluxes to the atmosphere, thereby regulating the capacity for CH4 to warm the early Earth under the Faint Young Sun. We studied CH4 and Fe cycling in anoxic incubations of ferruginous sediment from the ancient ocean analogue Lake Matano, Indonesia, over three successive transfers (500 days in total). Iron reduction, methanogenesis, CH4 oxidation, and microbial taxonomy were monitored in treatments amended with ferrihydrite or goethite. After three dilutions, Fe(III) reduction persisted only in bottles with ferrihydrite. Enhanced CH4 production was observed in the presence of goethite, highlighting the potential for reactive Fe(III) oxides to inhibit methanogenesis. Supplementing the media with hydrogen, nickel and selenium did not stimulate methanogenesis. There was limited evidence for Fe(III)-dependent CH4 oxidation, although some incubations displayed CH4 -stimulated Fe(III) reduction. 16S rRNA profiles continuously changed over the course of enrichment, with ultimate dominance of unclassified members of the order Desulfuromonadales in all treatments. Microbial diversity decreased markedly over the course of incubation, with subtle differences between ferrihydrite and goethite amendments. These results suggest that Fe(III) oxide mineralogy and availability of electron donors could have led to spatial separation of Fe(III)-reducing and methanogenic microbial communities in ferruginous marine sediments, potentially explaining the persistence of CH4 as a greenhouse gas throughout the first half of Earth history.
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Affiliation(s)
- M. S. Bray
- School of Biology, Georgia Institute of Technology, Atlanta, GA, USA
| | - J. Wu
- School of Biology, Georgia Institute of Technology, Atlanta, GA, USA
| | - B. C. Reed
- School of Biology, Georgia Institute of Technology, Atlanta, GA, USA
| | - C. B. Kretz
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA
| | - K. M. Belli
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA
| | - R. L. Simister
- Departments of Microbiology & Immunology and Earth, Ocean, & Atmospheric Sciences, University of British Columbia, Vancouver, BC, Canada
| | - C. Henny
- Research Center for Limnology, Indonesian Institute of Sciences, Cibinong, Indonesia
| | - F. J. Stewart
- School of Biology, Georgia Institute of Technology, Atlanta, GA, USA
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA
| | - T. J. DiChristina
- School of Biology, Georgia Institute of Technology, Atlanta, GA, USA
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA
| | - J. A. Brandes
- Skidaway Institute of Oceanography, Savannah, GA, USA
| | - D. A. Fowle
- Department of Geology, University of Kansas, Lawrence, KS, USA
| | - S. A. Crowe
- Departments of Microbiology & Immunology and Earth, Ocean, & Atmospheric Sciences, University of British Columbia, Vancouver, BC, Canada
| | - J. B. Glass
- School of Biology, Georgia Institute of Technology, Atlanta, GA, USA
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA
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Colonization Habitat Controls Biomass, Composition, and Metabolic Activity of Attached Microbial Communities in the Columbia River Hyporheic Corridor. Appl Environ Microbiol 2017; 83:AEM.00260-17. [PMID: 28600318 DOI: 10.1128/aem.00260-17] [Citation(s) in RCA: 10] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/30/2017] [Accepted: 06/02/2017] [Indexed: 01/25/2023] Open
Abstract
Hydrologic exchange plays a critical role in biogeochemical cycling within the hyporheic zone (the interface between river water and groundwater) of riverine ecosystems. Such exchange may set limits on the rates of microbial metabolism and impose deterministic selection on microbial communities that adapt to dynamically changing dissolved organic carbon (DOC) sources. This study examined the response of attached microbial communities (in situ colonized sand packs) from groundwater, hyporheic, and riverbed habitats within the Columbia River hyporheic corridor to "cross-feeding" with either groundwater, river water, or DOC-free artificial fluids. Our working hypothesis was that deterministic selection during in situ colonization would dictate the response to cross-feeding, with communities displaying maximal biomass and respiration when supplied with their native fluid source. In contrast to expectations, the major observation was that the riverbed colonized sand had much higher biomass and respiratory activity, as well as a distinct community structure, compared with those of the hyporheic and groundwater colonized sands. 16S rRNA gene amplicon sequencing revealed a much higher proportion of certain heterotrophic taxa as well as significant numbers of eukaryotic algal chloroplasts in the riverbed colonized sand. Significant quantities of DOC were released from riverbed sediment and colonized sand, and separate experiments showed that the released DOC stimulated respiration in the groundwater and piezometer colonized sand. These results suggest that the accumulation and degradation of labile particulate organic carbon (POC) within the riverbed are likely to release DOC, which may enter the hyporheic corridor during hydrologic exchange, thereby stimulating microbial activity and imposing deterministic selective pressure on the microbial community composition.IMPORTANCE The influence of river water-groundwater mixing on hyporheic zone microbial community structure and function is an important but poorly understood component of riverine biogeochemistry. This study employed an experimental approach to gain insight into how such mixing might be expected to influence the biomass, respiration, and composition of hyporheic zone microbial communities. Colonized sands from three different habitats (groundwater, river water, and hyporheic) were "cross-fed" with either groundwater, river water, or DOC-free artificial fluids. We expected that the colonization history would dictate the response to cross-feeding, with communities displaying maximal biomass and respiration when supplied with their native fluid source. By contrast, the major observation was that the riverbed communities had much higher biomass and respiration, as well as a distinct community structure compared with those of the hyporheic and groundwater colonized sands. These results highlight the importance of riverbed microbial metabolism in organic carbon processing in hyporheic corridors.
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