First pan-Arctic assessment of dissolved organic carbon in lakes of the permafrost region

Lakes in permafrost regions are dynamic landscape components and play an important role for climate change feedbacks. Lake processes such as mineralization and flocculation of dissolved organic carbon (DOC), one of the main carbon fractions in lakes, contribute to the greenhouse effect and are part...

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Published in:Biogeosciences
Main Authors: Stolpmann L., Coch C., Morgenstern A., Boike J., Fritz M., Herzschuh U., Stoof-Leichsenring K., Dvornikov Y., Heim B., Lenz J., Larsen A., Anthony K.W., Jones B., Frey K., Grosse G.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH
Subjects:
Ice
Online Access:https://repository.rudn.ru/records/article/record/74530/
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spelling ftrudnuniv:oai:repository.rudn.ru:r/74530 2023-05-15T14:51:18+02:00 First pan-Arctic assessment of dissolved organic carbon in lakes of the permafrost region Stolpmann L. Coch C. Morgenstern A. Boike J. Fritz M. Herzschuh U. Stoof-Leichsenring K. Dvornikov Y. Heim B. Lenz J. Larsen A. Anthony K.W. Jones B. Frey K. Grosse G. https://repository.rudn.ru/records/article/record/74530/ EN eng Copernicus GmbH https://doi.org/10.5194/bg-18-3917-2021 https://repository.rudn.ru/records/article/record/74530/ Biogeosciences Article ftrudnuniv https://doi.org/10.5194/bg-18-3917-2021 2022-01-03T09:48:39Z Lakes in permafrost regions are dynamic landscape components and play an important role for climate change feedbacks. Lake processes such as mineralization and flocculation of dissolved organic carbon (DOC), one of the main carbon fractions in lakes, contribute to the greenhouse effect and are part of the global carbon cycle. These processes are in the focus of climate research, but studies so far are limited to specific study regions. In our synthesis, we analyzed 2167 water samples from 1833 lakes across the Arctic in permafrost regions of Alaska, Canada, Greenland, and Siberia to provide first pan-Arctic insights for linkages between DOC concentrations and the environment. Using published data and unpublished datasets from the author team, we report regional DOC differences linked to latitude, permafrost zones, ecoregions, geology, near-surface soil organic carbon contents, and ground ice classification of each lake region. The lake DOC concentrations in our dataset range from 0 to 1130 mg L-1 (10.8 mg L-1 median DOC concentration). Regarding the permafrost regions of our synthesis, we found median lake DOC concentrations of 12.4 mg L-1 (Siberia), 12.3 mg L-1 (Alaska), 10.3 mg L-1 (Greenland), and 4.5 mg L-1 (Canada). Our synthesis shows a significant relationship between lake DOC concentration and lake ecoregion. We found higher lake DOC concentrations at boreal permafrost sites compared to tundra sites. We found significantly higher DOC concentrations in lakes in regions with ice-rich syngenetic permafrost deposits (yedoma) compared to non-yedoma lakes and a weak but significant relationship between soil organic carbon content and lake DOC concentration as well as between ground ice content and lake DOC. Our pan-Arctic dataset shows that the DOC concentration of a lake depends on its environmental properties, especially on permafrost extent and ecoregion, as well as vegetation, which is the most important driver of lake DOC in this study. This new dataset will be fundamental to quantify a pan-Arctic lake DOC pool for estimations of the impact of lake DOC on the global carbon cycle and climate change. Article in Journal/Newspaper Arctic Climate change Greenland Ice permafrost Tundra Alaska Siberia Peoples' Friendship University of Russia (RUDN): Open repository Arctic Arctic Lake ENVELOPE(-130.826,-130.826,57.231,57.231) Canada Greenland Biogeosciences 18 12 3917 3936
institution Open Polar
collection Peoples' Friendship University of Russia (RUDN): Open repository
op_collection_id ftrudnuniv
language English
description Lakes in permafrost regions are dynamic landscape components and play an important role for climate change feedbacks. Lake processes such as mineralization and flocculation of dissolved organic carbon (DOC), one of the main carbon fractions in lakes, contribute to the greenhouse effect and are part of the global carbon cycle. These processes are in the focus of climate research, but studies so far are limited to specific study regions. In our synthesis, we analyzed 2167 water samples from 1833 lakes across the Arctic in permafrost regions of Alaska, Canada, Greenland, and Siberia to provide first pan-Arctic insights for linkages between DOC concentrations and the environment. Using published data and unpublished datasets from the author team, we report regional DOC differences linked to latitude, permafrost zones, ecoregions, geology, near-surface soil organic carbon contents, and ground ice classification of each lake region. The lake DOC concentrations in our dataset range from 0 to 1130 mg L-1 (10.8 mg L-1 median DOC concentration). Regarding the permafrost regions of our synthesis, we found median lake DOC concentrations of 12.4 mg L-1 (Siberia), 12.3 mg L-1 (Alaska), 10.3 mg L-1 (Greenland), and 4.5 mg L-1 (Canada). Our synthesis shows a significant relationship between lake DOC concentration and lake ecoregion. We found higher lake DOC concentrations at boreal permafrost sites compared to tundra sites. We found significantly higher DOC concentrations in lakes in regions with ice-rich syngenetic permafrost deposits (yedoma) compared to non-yedoma lakes and a weak but significant relationship between soil organic carbon content and lake DOC concentration as well as between ground ice content and lake DOC. Our pan-Arctic dataset shows that the DOC concentration of a lake depends on its environmental properties, especially on permafrost extent and ecoregion, as well as vegetation, which is the most important driver of lake DOC in this study. This new dataset will be fundamental to quantify a pan-Arctic lake DOC pool for estimations of the impact of lake DOC on the global carbon cycle and climate change.
format Article in Journal/Newspaper
author Stolpmann L.
Coch C.
Morgenstern A.
Boike J.
Fritz M.
Herzschuh U.
Stoof-Leichsenring K.
Dvornikov Y.
Heim B.
Lenz J.
Larsen A.
Anthony K.W.
Jones B.
Frey K.
Grosse G.
spellingShingle Stolpmann L.
Coch C.
Morgenstern A.
Boike J.
Fritz M.
Herzschuh U.
Stoof-Leichsenring K.
Dvornikov Y.
Heim B.
Lenz J.
Larsen A.
Anthony K.W.
Jones B.
Frey K.
Grosse G.
First pan-Arctic assessment of dissolved organic carbon in lakes of the permafrost region
author_facet Stolpmann L.
Coch C.
Morgenstern A.
Boike J.
Fritz M.
Herzschuh U.
Stoof-Leichsenring K.
Dvornikov Y.
Heim B.
Lenz J.
Larsen A.
Anthony K.W.
Jones B.
Frey K.
Grosse G.
author_sort Stolpmann L.
title First pan-Arctic assessment of dissolved organic carbon in lakes of the permafrost region
title_short First pan-Arctic assessment of dissolved organic carbon in lakes of the permafrost region
title_full First pan-Arctic assessment of dissolved organic carbon in lakes of the permafrost region
title_fullStr First pan-Arctic assessment of dissolved organic carbon in lakes of the permafrost region
title_full_unstemmed First pan-Arctic assessment of dissolved organic carbon in lakes of the permafrost region
title_sort first pan-arctic assessment of dissolved organic carbon in lakes of the permafrost region
publisher Copernicus GmbH
url https://repository.rudn.ru/records/article/record/74530/
long_lat ENVELOPE(-130.826,-130.826,57.231,57.231)
geographic Arctic
Arctic Lake
Canada
Greenland
geographic_facet Arctic
Arctic Lake
Canada
Greenland
genre Arctic
Climate change
Greenland
Ice
permafrost
Tundra
Alaska
Siberia
genre_facet Arctic
Climate change
Greenland
Ice
permafrost
Tundra
Alaska
Siberia
op_source Biogeosciences
op_relation https://doi.org/10.5194/bg-18-3917-2021
https://repository.rudn.ru/records/article/record/74530/
op_doi https://doi.org/10.5194/bg-18-3917-2021
container_title Biogeosciences
container_volume 18
container_issue 12
container_start_page 3917
op_container_end_page 3936
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