Isotopic data of atmospheric methane from EDML and Vostok ice cores over a full glacial cycle ...

The response of natural CH4 sources to climate changes will be an important factor to consider as concentrations of this potent greenhouse gas continue to increase. Polar ice cores provide the means to assess this sensitivity in the past and have shown a close connection between CH4 levels and north...

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Main Authors: Möller, Lars, Sowers, Todd A, Bock, Michael, Spahni, Renato, Behrens, Melanie, Schmitt, Jochen, Miller, Heinz, Fischer, Hubertus
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2013
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.812116
https://doi.pangaea.de/10.1594/PANGAEA.812116
id ftdatacite:10.1594/pangaea.812116
record_format openpolar
spelling ftdatacite:10.1594/pangaea.812116 2024-09-15T17:47:21+00:00 Isotopic data of atmospheric methane from EDML and Vostok ice cores over a full glacial cycle ... Möller, Lars Sowers, Todd A Bock, Michael Spahni, Renato Behrens, Melanie Schmitt, Jochen Miller, Heinz Fischer, Hubertus 2013 application/zip https://dx.doi.org/10.1594/pangaea.812116 https://doi.pangaea.de/10.1594/PANGAEA.812116 en eng PANGAEA https://dx.doi.org/10.1038/ngeo1922 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 European Project for Ice Coring in Antarctica EPICA article Collection Supplementary Publication Series of Datasets 2013 ftdatacite https://doi.org/10.1594/pangaea.81211610.1038/ngeo1922 2024-08-01T10:51:52Z The response of natural CH4 sources to climate changes will be an important factor to consider as concentrations of this potent greenhouse gas continue to increase. Polar ice cores provide the means to assess this sensitivity in the past and have shown a close connection between CH4 levels and northern hemisphere temperature variability over the last glacial cycle. However, the contribution of the various CH4 sources and sinks to these changes is still a matter of debate. Contemporaneous stable CH4 isotope records in ice cores provide additional boundary conditions for assessing changes in the CH4 sources and sinks. Here we present new ice core CH4 isotope data covering the last 160,000 years, showing a clear decoupling between CH4 loading and carbon isotopic variations over most of the record. We suggest that d13CH4 variations were not dominated by a change in the source mix but rather by climate- and CO2-related ecosystem control on the isotopic composition of the methane precursor material, especially in ... : Supplement to: Möller, Lars; Sowers, Todd A; Bock, Michael; Spahni, Renato; Behrens, Melanie; Schmitt, Jochen; Miller, Heinz; Fischer, Hubertus (2013): Independent variations of CH4 emissions and isotopic composition over the past 160,000 years. Nature Geoscience, 6, 885-890 ... Article in Journal/Newspaper Antarc* Antarctica EPICA ice core DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic European Project for Ice Coring in Antarctica EPICA
spellingShingle European Project for Ice Coring in Antarctica EPICA
Möller, Lars
Sowers, Todd A
Bock, Michael
Spahni, Renato
Behrens, Melanie
Schmitt, Jochen
Miller, Heinz
Fischer, Hubertus
Isotopic data of atmospheric methane from EDML and Vostok ice cores over a full glacial cycle ...
topic_facet European Project for Ice Coring in Antarctica EPICA
description The response of natural CH4 sources to climate changes will be an important factor to consider as concentrations of this potent greenhouse gas continue to increase. Polar ice cores provide the means to assess this sensitivity in the past and have shown a close connection between CH4 levels and northern hemisphere temperature variability over the last glacial cycle. However, the contribution of the various CH4 sources and sinks to these changes is still a matter of debate. Contemporaneous stable CH4 isotope records in ice cores provide additional boundary conditions for assessing changes in the CH4 sources and sinks. Here we present new ice core CH4 isotope data covering the last 160,000 years, showing a clear decoupling between CH4 loading and carbon isotopic variations over most of the record. We suggest that d13CH4 variations were not dominated by a change in the source mix but rather by climate- and CO2-related ecosystem control on the isotopic composition of the methane precursor material, especially in ... : Supplement to: Möller, Lars; Sowers, Todd A; Bock, Michael; Spahni, Renato; Behrens, Melanie; Schmitt, Jochen; Miller, Heinz; Fischer, Hubertus (2013): Independent variations of CH4 emissions and isotopic composition over the past 160,000 years. Nature Geoscience, 6, 885-890 ...
format Article in Journal/Newspaper
author Möller, Lars
Sowers, Todd A
Bock, Michael
Spahni, Renato
Behrens, Melanie
Schmitt, Jochen
Miller, Heinz
Fischer, Hubertus
author_facet Möller, Lars
Sowers, Todd A
Bock, Michael
Spahni, Renato
Behrens, Melanie
Schmitt, Jochen
Miller, Heinz
Fischer, Hubertus
author_sort Möller, Lars
title Isotopic data of atmospheric methane from EDML and Vostok ice cores over a full glacial cycle ...
title_short Isotopic data of atmospheric methane from EDML and Vostok ice cores over a full glacial cycle ...
title_full Isotopic data of atmospheric methane from EDML and Vostok ice cores over a full glacial cycle ...
title_fullStr Isotopic data of atmospheric methane from EDML and Vostok ice cores over a full glacial cycle ...
title_full_unstemmed Isotopic data of atmospheric methane from EDML and Vostok ice cores over a full glacial cycle ...
title_sort isotopic data of atmospheric methane from edml and vostok ice cores over a full glacial cycle ...
publisher PANGAEA
publishDate 2013
url https://dx.doi.org/10.1594/pangaea.812116
https://doi.pangaea.de/10.1594/PANGAEA.812116
genre Antarc*
Antarctica
EPICA
ice core
genre_facet Antarc*
Antarctica
EPICA
ice core
op_relation https://dx.doi.org/10.1038/ngeo1922
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.81211610.1038/ngeo1922
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