Articles | Volume 21, issue 9
Hydrol. Earth Syst. Sci., 21, 4283–4300, 2017
https://doi.org/10.5194/hess-21-4283-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 21, 4283–4300, 2017
https://doi.org/10.5194/hess-21-4283-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
31 Aug 2017
Research article
| 31 Aug 2017
Carbon isotopes of dissolved inorganic carbon reflect utilization of different carbon sources by microbial communities in two limestone aquifer assemblages
Martin E. Nowak et al.
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Cited
24 citations as recorded by crossref.
- Thiosulfate- and hydrogen-driven autotrophic denitrification by a microbial consortium enriched from groundwater of an oligotrophic limestone aquifer S. Kumar et al. 10.1093/femsec/fiy141
- Nitrogen Loss from Pristine Carbonate-Rock Aquifers of the Hainich Critical Zone Exploratory (Germany) Is Primarily Driven by Chemolithoautotrophic Anammox Processes S. Kumar et al. 10.3389/fmicb.2017.01951
- Contrasting biogeochemical processes revealed by stable isotopes of H2O, N, C and S in shallow aquifers underlying agricultural lowlands N. Colombani et al. 10.1016/j.scitotenv.2019.07.238
- In situ production of core and intact bacterial and archaeal tetraether lipids in groundwater S. Ding et al. 10.1016/j.orggeochem.2018.10.005
- Carbon and iron isotope approach elucidates the enrichment of geogenic phosphorus in alluvial-lacustrine sedimentary aquifers Y. Tao et al. 10.1016/j.jhydrol.2022.127517
- Divergent microbial communities in groundwater and overlying soils exhibit functional redundancy for plant-polysaccharide degradation M. Taubert et al. 10.1371/journal.pone.0212937
- Predominance of Cand. Patescibacteria in Groundwater Is Caused by Their Preferential Mobilization From Soils and Flourishing Under Oligotrophic Conditions M. Herrmann et al. 10.3389/fmicb.2019.01407
- Fiber-Enhanced Raman Gas Spectroscopy for the Study of Microbial Methanogenesis A. Knebl et al. 10.1021/acs.analchem.0c02507
- Tracking down carbon inputs underground from an arid zone Australian calcrete M. Saccò et al. 10.1371/journal.pone.0237730
- Evaluation of geochemical processes and nitrate pollution sources at the Ljubljansko polje aquifer (Slovenia): A stable isotope perspective N. Ogrinc et al. 10.1016/j.scitotenv.2018.07.245
- The microbial dimension of submarine groundwater discharge: current challenges and future directions C. Ruiz-González et al. 10.1093/femsre/fuab010
- Linkage Between Dissolved Organic Matter Transformation, Bacterial Carbon Production, and Diversity in a Shallow Oligotrophic Aquifer: Results From Flow-Through Sediment Microcosm Experiments R. Hofmann et al. 10.3389/fmicb.2020.543567
- Does rapid glacial recession affect feeding habits of alpine stream insects? M. Sertić Perić et al. 10.1111/fwb.13621
- 14 C‐Free Carbon Is a Major Contributor to Cellular Biomass in Geochemically Distinct Groundwater of Shallow Sedimentary Bedrock Aquifers V. Schwab et al. 10.1029/2017WR022067
- Molecular Signals of Heterogeneous Terrestrial Environments Identified in Dissolved Organic Matter: A Comparative Analysis of Orbitrap and Ion Cyclotron Resonance Mass Spectrometers C. Simon et al. 10.3389/feart.2018.00138
- Isolation of Individual Saturated Fatty Acid Methyl Esters Derived From Groundwater Phospholipids by Preparative High‐Pressure Liquid Chromatography for Compound‐Specific Radiocarbon Analyses V. Schwab et al. 10.1029/2018WR024076
- Fueling Diversity in the Subsurface: Composition and Age of Dissolved Organic Matter in the Critical Zone S. Benk et al. 10.3389/feart.2019.00296
- Use of δ18O, δ 13C and NO3−to identify hydrogeochemical processes related to contamination in an aquifer located in central Mexico J. Morales-Arredondo et al. 10.1007/s11631-021-00519-6
- Spring Water of an Alpine Karst Aquifer Is Dominated by a Taxonomically Stable but Discharge-Responsive Bacterial Community D. Savio et al. 10.3389/fmicb.2019.00028
- Organic Carbon transport model of abandoned river channels - A motif for floodplain geomorphology influencing biogeochemical swaying of arsenic D. Ghosh et al. 10.1016/j.scitotenv.2020.144400
- Occurrence and Origin of Methane Entrapped in Sediments and Rocks of a Calcareous, Alpine Glacial Catchment B. Zhu et al. 10.1029/2018JG004651
- Filtration and exposure to benzalkonium chloride or sodium chloride to preserve water samples for dissolved inorganic carbon analysis H. Takahashi et al. 10.2343/geochemj.2.0570
- Enrichment of Geogenic Ammonium in Quaternary Alluvial–Lacustrine Aquifer Systems: Evidence from Carbon Isotopes and DOM Characteristics Y. Du et al. 10.1021/acs.est.0c00131
- Constraining source attribution of methane in an alluvial aquifer with multiple recharge pathways C. Iverach et al. 10.1016/j.scitotenv.2019.134927
24 citations as recorded by crossref.
- Thiosulfate- and hydrogen-driven autotrophic denitrification by a microbial consortium enriched from groundwater of an oligotrophic limestone aquifer S. Kumar et al. 10.1093/femsec/fiy141
- Nitrogen Loss from Pristine Carbonate-Rock Aquifers of the Hainich Critical Zone Exploratory (Germany) Is Primarily Driven by Chemolithoautotrophic Anammox Processes S. Kumar et al. 10.3389/fmicb.2017.01951
- Contrasting biogeochemical processes revealed by stable isotopes of H2O, N, C and S in shallow aquifers underlying agricultural lowlands N. Colombani et al. 10.1016/j.scitotenv.2019.07.238
- In situ production of core and intact bacterial and archaeal tetraether lipids in groundwater S. Ding et al. 10.1016/j.orggeochem.2018.10.005
- Carbon and iron isotope approach elucidates the enrichment of geogenic phosphorus in alluvial-lacustrine sedimentary aquifers Y. Tao et al. 10.1016/j.jhydrol.2022.127517
- Divergent microbial communities in groundwater and overlying soils exhibit functional redundancy for plant-polysaccharide degradation M. Taubert et al. 10.1371/journal.pone.0212937
- Predominance of Cand. Patescibacteria in Groundwater Is Caused by Their Preferential Mobilization From Soils and Flourishing Under Oligotrophic Conditions M. Herrmann et al. 10.3389/fmicb.2019.01407
- Fiber-Enhanced Raman Gas Spectroscopy for the Study of Microbial Methanogenesis A. Knebl et al. 10.1021/acs.analchem.0c02507
- Tracking down carbon inputs underground from an arid zone Australian calcrete M. Saccò et al. 10.1371/journal.pone.0237730
- Evaluation of geochemical processes and nitrate pollution sources at the Ljubljansko polje aquifer (Slovenia): A stable isotope perspective N. Ogrinc et al. 10.1016/j.scitotenv.2018.07.245
- The microbial dimension of submarine groundwater discharge: current challenges and future directions C. Ruiz-González et al. 10.1093/femsre/fuab010
- Linkage Between Dissolved Organic Matter Transformation, Bacterial Carbon Production, and Diversity in a Shallow Oligotrophic Aquifer: Results From Flow-Through Sediment Microcosm Experiments R. Hofmann et al. 10.3389/fmicb.2020.543567
- Does rapid glacial recession affect feeding habits of alpine stream insects? M. Sertić Perić et al. 10.1111/fwb.13621
- 14 C‐Free Carbon Is a Major Contributor to Cellular Biomass in Geochemically Distinct Groundwater of Shallow Sedimentary Bedrock Aquifers V. Schwab et al. 10.1029/2017WR022067
- Molecular Signals of Heterogeneous Terrestrial Environments Identified in Dissolved Organic Matter: A Comparative Analysis of Orbitrap and Ion Cyclotron Resonance Mass Spectrometers C. Simon et al. 10.3389/feart.2018.00138
- Isolation of Individual Saturated Fatty Acid Methyl Esters Derived From Groundwater Phospholipids by Preparative High‐Pressure Liquid Chromatography for Compound‐Specific Radiocarbon Analyses V. Schwab et al. 10.1029/2018WR024076
- Fueling Diversity in the Subsurface: Composition and Age of Dissolved Organic Matter in the Critical Zone S. Benk et al. 10.3389/feart.2019.00296
- Use of δ18O, δ 13C and NO3−to identify hydrogeochemical processes related to contamination in an aquifer located in central Mexico J. Morales-Arredondo et al. 10.1007/s11631-021-00519-6
- Spring Water of an Alpine Karst Aquifer Is Dominated by a Taxonomically Stable but Discharge-Responsive Bacterial Community D. Savio et al. 10.3389/fmicb.2019.00028
- Organic Carbon transport model of abandoned river channels - A motif for floodplain geomorphology influencing biogeochemical swaying of arsenic D. Ghosh et al. 10.1016/j.scitotenv.2020.144400
- Occurrence and Origin of Methane Entrapped in Sediments and Rocks of a Calcareous, Alpine Glacial Catchment B. Zhu et al. 10.1029/2018JG004651
- Filtration and exposure to benzalkonium chloride or sodium chloride to preserve water samples for dissolved inorganic carbon analysis H. Takahashi et al. 10.2343/geochemj.2.0570
- Enrichment of Geogenic Ammonium in Quaternary Alluvial–Lacustrine Aquifer Systems: Evidence from Carbon Isotopes and DOM Characteristics Y. Du et al. 10.1021/acs.est.0c00131
- Constraining source attribution of methane in an alluvial aquifer with multiple recharge pathways C. Iverach et al. 10.1016/j.scitotenv.2019.134927
Latest update: 03 Jul 2022
Short summary
In the present study we combined measurements of dissolved inorganic carbon (DIC) isotopes with a set of different geochemical and microbiological methods in order to get a comprehensive view of biogeochemical cycling and groundwater flow in two limestone aquifer assemblages. This allowed us to understand interactions and feedbacks between microbial communities, their carbon sources, and water chemistry.
In the present study we combined measurements of dissolved inorganic carbon (DIC) isotopes with...
