Articles | Volume 14, issue 18
https://doi.org/10.5194/bg-14-4229-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-14-4229-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Biogeochemical cycling at the aquatic–terrestrial interface is linked to parafluvial hyporheic zone inundation history
Pacific Northwest National Laboratory, Richland, WA 99352, USA
Emily B. Graham
Pacific Northwest National Laboratory, Richland, WA 99352, USA
Alex R. Crump
Pacific Northwest National Laboratory, Richland, WA 99352, USA
David W. Kennedy
Pacific Northwest National Laboratory, Richland, WA 99352, USA
Elvira B. Romero
Pacific Northwest National Laboratory, Richland, WA 99352, USA
Carolyn G. Anderson
Pacific Northwest National Laboratory, Richland, WA 99352, USA
Karl L. Dana
Pacific Northwest National Laboratory, Richland, WA 99352, USA
Charles T. Resch
Pacific Northwest National Laboratory, Richland, WA 99352, USA
Jim K. Fredrickson
Pacific Northwest National Laboratory, Richland, WA 99352, USA
James C. Stegen
Pacific Northwest National Laboratory, Richland, WA 99352, USA
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- Historical Contingency in Microbial Resilience to Hydrologic Perturbations H. Song et al. 10.3389/frwa.2021.590378
- Subsurface biogeochemistry is a missing link between ecology and hydrology in dam-impacted river corridors E. Graham et al. 10.1016/j.scitotenv.2018.11.414
- At the Nexus of History, Ecology, and Hydrobiogeochemistry: Improved Predictions across Scales through Integration J. Stegen 10.1128/mSystems.00167-17
- A unified conceptual framework for prediction and control of microbiomes J. Stegen et al. 10.1016/j.mib.2018.06.002
- Responses of microbial activity in hyporheic pore water to biogeochemical changes in a drying headwater stream A. Harjung et al. 10.1111/fwb.13258
- Dry-Wet Cycles Affect Nitrous Oxide Emissions Across Aquatic-Terrestrial Interfaces: A Mesocosms Study R. Pinto et al. 10.3389/fsoil.2022.849210
- Denitrification and associated nitrous oxide and carbon dioxide emissions from the Amazonian wetlands J. Guilhen et al. 10.5194/bg-17-4297-2020
- Antecedent conditions determine the biogeochemical response of coastal soils to seawater exposure A. Sengupta et al. 10.1016/j.soilbio.2020.108104
- Influences of organic carbon speciation on hyporheic corridor biogeochemistry and microbial ecology J. Stegen et al. 10.1038/s41467-018-02922-9
- Catchment‐Scale Shifts in the Magnitude and Partitioning of Carbon Export in Response to Changing Hydrologic Connectivity in a Northern Hardwood Forest O. Senar et al. 10.1029/2018JG004468
- River-floodplain restoration and hydrological effects on GHG emissions: Biogeochemical dynamics in the parafluvial zone R. Machado dos Santos Pinto et al. 10.1016/j.scitotenv.2020.136980
- Abundant bacteria shaped by deterministic processes have a high abundance of potential antibiotic resistance genes in a plateau river sediment Y. Zhao et al. 10.3389/fmicb.2022.977037
- Grazers superimpose humidity effect on stream biofilm resistance and resilience to dry-rewet stress A. Oprei et al. 10.1016/j.scitotenv.2018.12.316
- Groundwater Regulates Interannual Variations in Evapotranspiration in a Riparian Semiarid Ecosystem J. Missik et al. 10.1029/2020JD033078
- Coupling surface flow with high-performance subsurface reactive flow and transport code PFLOTRAN R. Wu et al. 10.1016/j.envsoft.2021.104959
- Disturbance triggers non-linear microbe–environment feedbacks A. Sengupta et al. 10.5194/bg-18-4773-2021
- Microbial Community Structure and Metabolic Potential of the Hyporheic Zone of a Large Mid-Stream Channel Bar J. Sackett et al. 10.1080/01490451.2019.1621964
- Integrating field observations and process-based modeling to predict watershed water quality under environmental perturbations X. Chen et al. 10.1016/j.jhydrol.2020.125762
- Spatial gradients in the characteristics of soil-carbon fractions are associated with abiotic features but not microbial communities A. Sengupta et al. 10.5194/bg-16-3911-2019
- Long-term functional recovery and associated microbial community structure after sediment drying and bedform migration A. Oprei et al. 10.3389/fevo.2023.1112519
- Long-term nitrogen addition affects the phylogenetic turnover of soil microbial community responding to moisture pulse C. Liu et al. 10.1038/s41598-017-17736-w
21 citations as recorded by crossref.
- Fungi and cercozoa regulate methane-associated prokaryotes in wetland methane emissions L. Wang et al. 10.3389/fmicb.2022.1076610
- Historical Contingency in Microbial Resilience to Hydrologic Perturbations H. Song et al. 10.3389/frwa.2021.590378
- Subsurface biogeochemistry is a missing link between ecology and hydrology in dam-impacted river corridors E. Graham et al. 10.1016/j.scitotenv.2018.11.414
- At the Nexus of History, Ecology, and Hydrobiogeochemistry: Improved Predictions across Scales through Integration J. Stegen 10.1128/mSystems.00167-17
- A unified conceptual framework for prediction and control of microbiomes J. Stegen et al. 10.1016/j.mib.2018.06.002
- Responses of microbial activity in hyporheic pore water to biogeochemical changes in a drying headwater stream A. Harjung et al. 10.1111/fwb.13258
- Dry-Wet Cycles Affect Nitrous Oxide Emissions Across Aquatic-Terrestrial Interfaces: A Mesocosms Study R. Pinto et al. 10.3389/fsoil.2022.849210
- Denitrification and associated nitrous oxide and carbon dioxide emissions from the Amazonian wetlands J. Guilhen et al. 10.5194/bg-17-4297-2020
- Antecedent conditions determine the biogeochemical response of coastal soils to seawater exposure A. Sengupta et al. 10.1016/j.soilbio.2020.108104
- Influences of organic carbon speciation on hyporheic corridor biogeochemistry and microbial ecology J. Stegen et al. 10.1038/s41467-018-02922-9
- Catchment‐Scale Shifts in the Magnitude and Partitioning of Carbon Export in Response to Changing Hydrologic Connectivity in a Northern Hardwood Forest O. Senar et al. 10.1029/2018JG004468
- River-floodplain restoration and hydrological effects on GHG emissions: Biogeochemical dynamics in the parafluvial zone R. Machado dos Santos Pinto et al. 10.1016/j.scitotenv.2020.136980
- Abundant bacteria shaped by deterministic processes have a high abundance of potential antibiotic resistance genes in a plateau river sediment Y. Zhao et al. 10.3389/fmicb.2022.977037
- Grazers superimpose humidity effect on stream biofilm resistance and resilience to dry-rewet stress A. Oprei et al. 10.1016/j.scitotenv.2018.12.316
- Groundwater Regulates Interannual Variations in Evapotranspiration in a Riparian Semiarid Ecosystem J. Missik et al. 10.1029/2020JD033078
- Coupling surface flow with high-performance subsurface reactive flow and transport code PFLOTRAN R. Wu et al. 10.1016/j.envsoft.2021.104959
- Disturbance triggers non-linear microbe–environment feedbacks A. Sengupta et al. 10.5194/bg-18-4773-2021
- Microbial Community Structure and Metabolic Potential of the Hyporheic Zone of a Large Mid-Stream Channel Bar J. Sackett et al. 10.1080/01490451.2019.1621964
- Integrating field observations and process-based modeling to predict watershed water quality under environmental perturbations X. Chen et al. 10.1016/j.jhydrol.2020.125762
- Spatial gradients in the characteristics of soil-carbon fractions are associated with abiotic features but not microbial communities A. Sengupta et al. 10.5194/bg-16-3911-2019
- Long-term functional recovery and associated microbial community structure after sediment drying and bedform migration A. Oprei et al. 10.3389/fevo.2023.1112519
Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
The history of river inundation influences shoreline sediment biogeochemical cycling and microbial dynamics. Sediment exhibited a binary respiration response to rewetting, in which respiration from less recently saturated sediment was suppressed relative to more recently saturated sediment, likely due to inhibition of fungal metabolic activity. River shorelines should likely be integrated as a distinct environment into hydrobiogeochemical models to predict watershed biogeochemical function.
The history of river inundation influences shoreline sediment biogeochemical cycling and...
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