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 G2201-i ca...

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Published in:Limnology and Oceanography: Methods
Main Authors: Uhlig, Christiane, Loose, Brice
Format: Article in Journal/Newspaper
Language:unknown
Published: 2017
Subjects:
Online Access:https://epic.awi.de/id/eprint/45456/
https://epic.awi.de/id/eprint/45456/1/Uhlig_et_al-2017-Limnology_and_Oceanography__Methods.pdf
https://hdl.handle.net/10013/epic.51638
https://hdl.handle.net/10013/epic.51638.d001
id ftawi:oai:epic.awi.de:45456
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spelling ftawi:oai:epic.awi.de:45456 2023-05-15T14:26:41+02:00 Using stable isotopes and gas concentrations for independent constraints on microbial methane oxidation at Arctic Ocean temperatures Uhlig, Christiane Loose, Brice 2017-07-31 application/pdf https://epic.awi.de/id/eprint/45456/ https://epic.awi.de/id/eprint/45456/1/Uhlig_et_al-2017-Limnology_and_Oceanography__Methods.pdf https://hdl.handle.net/10013/epic.51638 https://hdl.handle.net/10013/epic.51638.d001 unknown https://epic.awi.de/id/eprint/45456/1/Uhlig_et_al-2017-Limnology_and_Oceanography__Methods.pdf https://hdl.handle.net/10013/epic.51638.d001 Uhlig, C. orcid:0000-0001-7278-6522 and Loose, B. (2017) Using stable isotopes and gas concentrations for independent constraints on microbial methane oxidation at Arctic Ocean temperatures , Limnology & Oceanography: Methods . doi:10.1002/lom3.10199 <https://doi.org/10.1002/lom3.10199> , hdl:10013/epic.51638 EPIC3Limnology & Oceanography: Methods Article isiRev 2017 ftawi 2021-12-24T15:43:17Z 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 G2201-i cavity ring-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 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*d) at in situ methane concentration and a maximal oxidation potential of 271 ± 41 nmol / (L*d). 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. Article in Journal/Newspaper Arctic Arctic Arctic Ocean Alaska Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Arctic Arctic Ocean Limnology and Oceanography: Methods 15 8 737 751
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
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 G2201-i cavity ring-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 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*d) at in situ methane concentration and a maximal oxidation potential of 271 ± 41 nmol / (L*d). 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 Article in Journal/Newspaper
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
publishDate 2017
url https://epic.awi.de/id/eprint/45456/
https://epic.awi.de/id/eprint/45456/1/Uhlig_et_al-2017-Limnology_and_Oceanography__Methods.pdf
https://hdl.handle.net/10013/epic.51638
https://hdl.handle.net/10013/epic.51638.d001
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic
Arctic Ocean
Alaska
genre_facet Arctic
Arctic
Arctic Ocean
Alaska
op_source EPIC3Limnology & Oceanography: Methods
op_relation https://epic.awi.de/id/eprint/45456/1/Uhlig_et_al-2017-Limnology_and_Oceanography__Methods.pdf
https://hdl.handle.net/10013/epic.51638.d001
Uhlig, C. orcid:0000-0001-7278-6522 and Loose, B. (2017) Using stable isotopes and gas concentrations for independent constraints on microbial methane oxidation at Arctic Ocean temperatures , Limnology & Oceanography: Methods . doi:10.1002/lom3.10199 <https://doi.org/10.1002/lom3.10199> , hdl:10013/epic.51638
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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