Using stable isotopes and gas concentrations for independent constraints on microbial methane oxidation at Arctic Ocean temperatures

Microbial oxidation of methane in oxic water bodies is an important control on the amount of dissolved methane which is released from the ocean to the atmosphere. We explored the use of stable isotope methane spikes to quantify methane oxidation rates in Arctic seawater samples. A Picarro G2201â€i c...

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Published in:Limnology and Oceanography: Methods
Main Authors: Uhlig, Christiane, Loose, Brice
Format: Text
Language:unknown
Published: DigitalCommons@URI 2017
Subjects:
Online Access:https://digitalcommons.uri.edu/gsofacpubs/633
https://doi.org/10.1002/lom3.10199
https://digitalcommons.uri.edu/context/gsofacpubs/article/1592/viewcontent/Loose_UsingStable_2017.pdf
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spelling ftunivrhodeislan:oai:digitalcommons.uri.edu:gsofacpubs-1592 2024-09-15T17:54:07+00:00 Using stable isotopes and gas concentrations for independent constraints on microbial methane oxidation at Arctic Ocean temperatures Uhlig, Christiane Loose, Brice 2017-01-01T08:00:00Z application/pdf https://digitalcommons.uri.edu/gsofacpubs/633 https://doi.org/10.1002/lom3.10199 https://digitalcommons.uri.edu/context/gsofacpubs/article/1592/viewcontent/Loose_UsingStable_2017.pdf unknown DigitalCommons@URI https://digitalcommons.uri.edu/gsofacpubs/633 doi:10.1002/lom3.10199 https://digitalcommons.uri.edu/context/gsofacpubs/article/1592/viewcontent/Loose_UsingStable_2017.pdf http://creativecommons.org/licenses/by/4.0/ Graduate School of Oceanography Faculty Publications text 2017 ftunivrhodeislan https://doi.org/10.1002/lom3.10199 2024-08-21T00:09:33Z Microbial oxidation of methane in oxic water bodies is an important control on the amount of dissolved methane which is released from the ocean to the atmosphere. We explored the use of stable isotope methane spikes to quantify methane oxidation rates in Arctic seawater samples. A Picarro G2201â€i cavity ringâ€down spectrometer was used to determine methane concentration and isotope ratios from headspace samples in foil incubators. The methane mass balance and the change in stable isotope ratios served as independent constraints on methane oxidation. For a fractionation factor of 1.025 oxidation rate constants determined with both methods agreed within 20% for small changes in isotope ratio (e.g., 10‰). For large changes in isotope ratio (e.g., 90‰), which was outside the calibration range, methods diverged. Rate constants down to 0.01 d−1 could be resolved with high statistical support. Stable isotope infrared spectroscopy to determine methane oxidation in foil incubators (ISMOFI) was successfully tested on under ice seawater from Utqiagvik, Alaska, by repeated sampling from each incubation vessel. Depending on the amount of isotope spike added, we determined oxidation rates of 0.15 ± 0.02 nmol L−1 d−1 at in situ methane concentration and a maximal oxidation potential of 271 ± 41 nmol L−1 d−1. The ISMOFI method permits variable incubation durations from days to months in a single incubator. The method is transportable and applicable in a variety of field or seagoing laboratory environments, and it avoids the use of hazardous substances such as radioisotopes and toxic chemicals. Text Arctic Ocean Alaska University of Rhode Island: DigitalCommons@URI Limnology and Oceanography: Methods 15 8 737 751
institution Open Polar
collection University of Rhode Island: DigitalCommons@URI
op_collection_id ftunivrhodeislan
language unknown
description Microbial oxidation of methane in oxic water bodies is an important control on the amount of dissolved methane which is released from the ocean to the atmosphere. We explored the use of stable isotope methane spikes to quantify methane oxidation rates in Arctic seawater samples. A Picarro G2201â€i cavity ringâ€down spectrometer was used to determine methane concentration and isotope ratios from headspace samples in foil incubators. The methane mass balance and the change in stable isotope ratios served as independent constraints on methane oxidation. For a fractionation factor of 1.025 oxidation rate constants determined with both methods agreed within 20% for small changes in isotope ratio (e.g., 10‰). For large changes in isotope ratio (e.g., 90‰), which was outside the calibration range, methods diverged. Rate constants down to 0.01 d−1 could be resolved with high statistical support. Stable isotope infrared spectroscopy to determine methane oxidation in foil incubators (ISMOFI) was successfully tested on under ice seawater from Utqiagvik, Alaska, by repeated sampling from each incubation vessel. Depending on the amount of isotope spike added, we determined oxidation rates of 0.15 ± 0.02 nmol L−1 d−1 at in situ methane concentration and a maximal oxidation potential of 271 ± 41 nmol L−1 d−1. The ISMOFI method permits variable incubation durations from days to months in a single incubator. The method is transportable and applicable in a variety of field or seagoing laboratory environments, and it avoids the use of hazardous substances such as radioisotopes and toxic chemicals.
format Text
author Uhlig, Christiane
Loose, Brice
spellingShingle Uhlig, Christiane
Loose, Brice
Using stable isotopes and gas concentrations for independent constraints on microbial methane oxidation at Arctic Ocean temperatures
author_facet Uhlig, Christiane
Loose, Brice
author_sort Uhlig, Christiane
title Using stable isotopes and gas concentrations for independent constraints on microbial methane oxidation at Arctic Ocean temperatures
title_short Using stable isotopes and gas concentrations for independent constraints on microbial methane oxidation at Arctic Ocean temperatures
title_full Using stable isotopes and gas concentrations for independent constraints on microbial methane oxidation at Arctic Ocean temperatures
title_fullStr Using stable isotopes and gas concentrations for independent constraints on microbial methane oxidation at Arctic Ocean temperatures
title_full_unstemmed Using stable isotopes and gas concentrations for independent constraints on microbial methane oxidation at Arctic Ocean temperatures
title_sort using stable isotopes and gas concentrations for independent constraints on microbial methane oxidation at arctic ocean temperatures
publisher DigitalCommons@URI
publishDate 2017
url https://digitalcommons.uri.edu/gsofacpubs/633
https://doi.org/10.1002/lom3.10199
https://digitalcommons.uri.edu/context/gsofacpubs/article/1592/viewcontent/Loose_UsingStable_2017.pdf
genre Arctic Ocean
Alaska
genre_facet Arctic Ocean
Alaska
op_source Graduate School of Oceanography Faculty Publications
op_relation https://digitalcommons.uri.edu/gsofacpubs/633
doi:10.1002/lom3.10199
https://digitalcommons.uri.edu/context/gsofacpubs/article/1592/viewcontent/Loose_UsingStable_2017.pdf
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1002/lom3.10199
container_title Limnology and Oceanography: Methods
container_volume 15
container_issue 8
container_start_page 737
op_container_end_page 751
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