Concentration and stable carbon and hydrogen isotopes of lipid biomarkers in a thermokarst lake in Arctic Alaska ...

Arctic lakes and wetlands contribute a substantial amount of methane to the contemporary atmosphere, yet profound knowledge gaps remain regarding the intensity and climatic control of past methane emissions from this source. In this study, we reconstruct methane turnover and environmental conditions...

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Main Authors: Elvert, Marcus, Pohlman, John W, Becker, Kevin W, Gaglioti, Benjamin V, Hinrichs, Kai-Uwe, Wooller, Matthew J
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2017
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.873658
https://doi.pangaea.de/10.1594/PANGAEA.873658
id ftdatacite:10.1594/pangaea.873658
record_format openpolar
spelling ftdatacite:10.1594/pangaea.873658 2024-09-15T18:39:05+00:00 Concentration and stable carbon and hydrogen isotopes of lipid biomarkers in a thermokarst lake in Arctic Alaska ... Elvert, Marcus Pohlman, John W Becker, Kevin W Gaglioti, Benjamin V Hinrichs, Kai-Uwe Wooller, Matthew J 2017 application/zip https://dx.doi.org/10.1594/pangaea.873658 https://doi.pangaea.de/10.1594/PANGAEA.873658 en eng PANGAEA https://dx.doi.org/10.1177/0959683616645942 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Center for Marine Environmental Sciences MARUM article Collection Supplementary Publication Series of Datasets 2017 ftdatacite https://doi.org/10.1594/pangaea.87365810.1177/0959683616645942 2024-08-01T11:01:20Z Arctic lakes and wetlands contribute a substantial amount of methane to the contemporary atmosphere, yet profound knowledge gaps remain regarding the intensity and climatic control of past methane emissions from this source. In this study, we reconstruct methane turnover and environmental conditions, including estimates of mean annual and summer temperature, from a thermokarst lake (Lake Qalluuraq) on the Arctic Coastal Plain of northern Alaska for the Holocene by using source-specific lipid biomarkers preserved in a radiocarbon-dated sediment core. Our results document a more prominent role for methane in the carbon cycle when the lake basin was an emergent fen habitat between ~12,300 and ~10,000 cal yr BP, a time period closely coinciding with the Holocene Thermal Maximum (HTM) in North Alaska. Enhanced methane turnover was stimulated by relatively warm temperatures, increased moisture, nutrient supply, and primary productivity. After ~10,000 cal yr BP, a thermokarst lake with abundant submerged mosses ... : Supplement to: Elvert, Marcus; Pohlman, John W; Becker, Kevin W; Gaglioti, Benjamin V; Hinrichs, Kai-Uwe; Wooller, Matthew J (2016): Methane turnover and environmental change from Holocene lipid biomarker records in a thermokarst lake in Arctic Alaska. The Holocene, 26(11), 1766-1777 ... Article in Journal/Newspaper Thermokarst Alaska DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Center for Marine Environmental Sciences MARUM
spellingShingle Center for Marine Environmental Sciences MARUM
Elvert, Marcus
Pohlman, John W
Becker, Kevin W
Gaglioti, Benjamin V
Hinrichs, Kai-Uwe
Wooller, Matthew J
Concentration and stable carbon and hydrogen isotopes of lipid biomarkers in a thermokarst lake in Arctic Alaska ...
topic_facet Center for Marine Environmental Sciences MARUM
description Arctic lakes and wetlands contribute a substantial amount of methane to the contemporary atmosphere, yet profound knowledge gaps remain regarding the intensity and climatic control of past methane emissions from this source. In this study, we reconstruct methane turnover and environmental conditions, including estimates of mean annual and summer temperature, from a thermokarst lake (Lake Qalluuraq) on the Arctic Coastal Plain of northern Alaska for the Holocene by using source-specific lipid biomarkers preserved in a radiocarbon-dated sediment core. Our results document a more prominent role for methane in the carbon cycle when the lake basin was an emergent fen habitat between ~12,300 and ~10,000 cal yr BP, a time period closely coinciding with the Holocene Thermal Maximum (HTM) in North Alaska. Enhanced methane turnover was stimulated by relatively warm temperatures, increased moisture, nutrient supply, and primary productivity. After ~10,000 cal yr BP, a thermokarst lake with abundant submerged mosses ... : Supplement to: Elvert, Marcus; Pohlman, John W; Becker, Kevin W; Gaglioti, Benjamin V; Hinrichs, Kai-Uwe; Wooller, Matthew J (2016): Methane turnover and environmental change from Holocene lipid biomarker records in a thermokarst lake in Arctic Alaska. The Holocene, 26(11), 1766-1777 ...
format Article in Journal/Newspaper
author Elvert, Marcus
Pohlman, John W
Becker, Kevin W
Gaglioti, Benjamin V
Hinrichs, Kai-Uwe
Wooller, Matthew J
author_facet Elvert, Marcus
Pohlman, John W
Becker, Kevin W
Gaglioti, Benjamin V
Hinrichs, Kai-Uwe
Wooller, Matthew J
author_sort Elvert, Marcus
title Concentration and stable carbon and hydrogen isotopes of lipid biomarkers in a thermokarst lake in Arctic Alaska ...
title_short Concentration and stable carbon and hydrogen isotopes of lipid biomarkers in a thermokarst lake in Arctic Alaska ...
title_full Concentration and stable carbon and hydrogen isotopes of lipid biomarkers in a thermokarst lake in Arctic Alaska ...
title_fullStr Concentration and stable carbon and hydrogen isotopes of lipid biomarkers in a thermokarst lake in Arctic Alaska ...
title_full_unstemmed Concentration and stable carbon and hydrogen isotopes of lipid biomarkers in a thermokarst lake in Arctic Alaska ...
title_sort concentration and stable carbon and hydrogen isotopes of lipid biomarkers in a thermokarst lake in arctic alaska ...
publisher PANGAEA
publishDate 2017
url https://dx.doi.org/10.1594/pangaea.873658
https://doi.pangaea.de/10.1594/PANGAEA.873658
genre Thermokarst
Alaska
genre_facet Thermokarst
Alaska
op_relation https://dx.doi.org/10.1177/0959683616645942
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.87365810.1177/0959683616645942
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