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...

Full description

Bibliographic Details
Published in:Biogeosciences
Main Authors: L. Stolpmann, C. Coch, A. Morgenstern, J. Boike, M. Fritz, U. Herzschuh, K. Stoof-Leichsenring, Y. Dvornikov, B. Heim, J. Lenz, A. Larsen, K. Walter Anthony, B. Jones, K. Frey, G. Grosse
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2021
Subjects:
Ice
Online Access:https://doi.org/10.5194/bg-18-3917-2021
https://doaj.org/article/2872d38cb9414d7eb9c4b0dcdc34fb9d
id ftdoajarticles:oai:doaj.org/article:2872d38cb9414d7eb9c4b0dcdc34fb9d
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:2872d38cb9414d7eb9c4b0dcdc34fb9d 2023-05-15T14:51:15+02:00 First pan-Arctic assessment of dissolved organic carbon in lakes of the permafrost region L. Stolpmann C. Coch A. Morgenstern J. Boike M. Fritz U. Herzschuh K. Stoof-Leichsenring Y. Dvornikov B. Heim J. Lenz A. Larsen K. Walter Anthony B. Jones K. Frey G. Grosse 2021-06-01T00:00:00Z https://doi.org/10.5194/bg-18-3917-2021 https://doaj.org/article/2872d38cb9414d7eb9c4b0dcdc34fb9d EN eng Copernicus Publications https://bg.copernicus.org/articles/18/3917/2021/bg-18-3917-2021.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-18-3917-2021 1726-4170 1726-4189 https://doaj.org/article/2872d38cb9414d7eb9c4b0dcdc34fb9d Biogeosciences, Vol 18, Pp 3917-3936 (2021) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.5194/bg-18-3917-2021 2022-12-31T05:29:24Z 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 ... Article in Journal/Newspaper Arctic Climate change Greenland Ice permafrost Tundra Alaska Siberia Directory of Open Access Journals: DOAJ Articles Arctic Canada Greenland Biogeosciences 18 12 3917 3936
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
spellingShingle Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
L. Stolpmann
C. Coch
A. Morgenstern
J. Boike
M. Fritz
U. Herzschuh
K. Stoof-Leichsenring
Y. Dvornikov
B. Heim
J. Lenz
A. Larsen
K. Walter Anthony
B. Jones
K. Frey
G. Grosse
First pan-Arctic assessment of dissolved organic carbon in lakes of the permafrost region
topic_facet Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
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 ...
format Article in Journal/Newspaper
author L. Stolpmann
C. Coch
A. Morgenstern
J. Boike
M. Fritz
U. Herzschuh
K. Stoof-Leichsenring
Y. Dvornikov
B. Heim
J. Lenz
A. Larsen
K. Walter Anthony
B. Jones
K. Frey
G. Grosse
author_facet L. Stolpmann
C. Coch
A. Morgenstern
J. Boike
M. Fritz
U. Herzschuh
K. Stoof-Leichsenring
Y. Dvornikov
B. Heim
J. Lenz
A. Larsen
K. Walter Anthony
B. Jones
K. Frey
G. Grosse
author_sort L. Stolpmann
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 Publications
publishDate 2021
url https://doi.org/10.5194/bg-18-3917-2021
https://doaj.org/article/2872d38cb9414d7eb9c4b0dcdc34fb9d
geographic Arctic
Canada
Greenland
geographic_facet Arctic
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, Vol 18, Pp 3917-3936 (2021)
op_relation https://bg.copernicus.org/articles/18/3917/2021/bg-18-3917-2021.pdf
https://doaj.org/toc/1726-4170
https://doaj.org/toc/1726-4189
doi:10.5194/bg-18-3917-2021
1726-4170
1726-4189
https://doaj.org/article/2872d38cb9414d7eb9c4b0dcdc34fb9d
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
_version_ 1766322304160104448