Review article: Terrestrial dissolved organic carbon in northern permafrost
As the permafrost region warms and permafrost soils thaw, vast stores of soil organic carbon (C) become vulnerable to enhanced microbial decomposition and lateral transport into aquatic ecosystems as dissolved organic carbon (DOC). The mobilization of permafrost soil C can drastically alter the net...
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2024
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ftdoajarticles:oai:doaj.org/article:fbb91441113f492aaba3680e7ef5ee64 2024-09-15T18:29:17+00:00 Review article: Terrestrial dissolved organic carbon in northern permafrost L. Heffernan D. N. Kothawala L. J. Tranvik 2024-03-01T00:00:00Z https://doi.org/10.5194/tc-18-1443-2024 https://doaj.org/article/fbb91441113f492aaba3680e7ef5ee64 EN eng Copernicus Publications https://tc.copernicus.org/articles/18/1443/2024/tc-18-1443-2024.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-18-1443-2024 1994-0416 1994-0424 https://doaj.org/article/fbb91441113f492aaba3680e7ef5ee64 The Cryosphere, Vol 18, Pp 1443-1465 (2024) Environmental sciences GE1-350 Geology QE1-996.5 article 2024 ftdoajarticles https://doi.org/10.5194/tc-18-1443-2024 2024-08-05T17:49:44Z As the permafrost region warms and permafrost soils thaw, vast stores of soil organic carbon (C) become vulnerable to enhanced microbial decomposition and lateral transport into aquatic ecosystems as dissolved organic carbon (DOC). The mobilization of permafrost soil C can drastically alter the net northern permafrost C budget. DOC entering aquatic ecosystems becomes biologically available for degradation as well as other types of aquatic processing. However, it currently remains unclear which landscape characteristics are most relevant to consider in terms of predicting DOC concentrations entering aquatic systems from permafrost regions. Here, we conducted a systematic review of 111 studies relating to, or including, concentrations of DOC in terrestrial permafrost ecosystems in the northern circumpolar region published between 2000 and 2022. We present a new permafrost DOC dataset consisting of 2845 DOC concentrations, collected from the top 3 m in permafrost soils across the northern circumpolar region. Concentrations of DOC ranged from 0.1 to 500 mg L −1 (median = 41 mg L −1 ) across all permafrost zones, ecoregions, soil types, and thermal horizons. Across the permafrost zones, the highest median DOC concentrations were in the sporadic permafrost zone (101 mg L −1 ), while lower concentrations were found in the discontinuous (60 mg L −1 ) and continuous (59 mg L −1 ) permafrost zones. However, median DOC concentrations varied in these zones across ecosystem type, with the highest median DOC concentrations in each ecosystem type of 66 and 63 mg L −1 found in coastal tundra and permafrost bog ecosystems, respectively. Coastal tundra (130 mg L −1 ), permafrost bogs (78 mg L −1 ), and permafrost wetlands (57 mg L −1 ) had the highest median DOC concentrations in the permafrost lens, representing a potentially long-term store of DOC. Other than in Yedoma ecosystems, DOC concentrations were found to increase following permafrost thaw and were highly constrained by total dissolved nitrogen concentrations. This ... Article in Journal/Newspaper permafrost The Cryosphere Tundra Directory of Open Access Journals: DOAJ Articles The Cryosphere 18 3 1443 1465 |
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Directory of Open Access Journals: DOAJ Articles |
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English |
topic |
Environmental sciences GE1-350 Geology QE1-996.5 |
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Environmental sciences GE1-350 Geology QE1-996.5 L. Heffernan D. N. Kothawala L. J. Tranvik Review article: Terrestrial dissolved organic carbon in northern permafrost |
topic_facet |
Environmental sciences GE1-350 Geology QE1-996.5 |
description |
As the permafrost region warms and permafrost soils thaw, vast stores of soil organic carbon (C) become vulnerable to enhanced microbial decomposition and lateral transport into aquatic ecosystems as dissolved organic carbon (DOC). The mobilization of permafrost soil C can drastically alter the net northern permafrost C budget. DOC entering aquatic ecosystems becomes biologically available for degradation as well as other types of aquatic processing. However, it currently remains unclear which landscape characteristics are most relevant to consider in terms of predicting DOC concentrations entering aquatic systems from permafrost regions. Here, we conducted a systematic review of 111 studies relating to, or including, concentrations of DOC in terrestrial permafrost ecosystems in the northern circumpolar region published between 2000 and 2022. We present a new permafrost DOC dataset consisting of 2845 DOC concentrations, collected from the top 3 m in permafrost soils across the northern circumpolar region. Concentrations of DOC ranged from 0.1 to 500 mg L −1 (median = 41 mg L −1 ) across all permafrost zones, ecoregions, soil types, and thermal horizons. Across the permafrost zones, the highest median DOC concentrations were in the sporadic permafrost zone (101 mg L −1 ), while lower concentrations were found in the discontinuous (60 mg L −1 ) and continuous (59 mg L −1 ) permafrost zones. However, median DOC concentrations varied in these zones across ecosystem type, with the highest median DOC concentrations in each ecosystem type of 66 and 63 mg L −1 found in coastal tundra and permafrost bog ecosystems, respectively. Coastal tundra (130 mg L −1 ), permafrost bogs (78 mg L −1 ), and permafrost wetlands (57 mg L −1 ) had the highest median DOC concentrations in the permafrost lens, representing a potentially long-term store of DOC. Other than in Yedoma ecosystems, DOC concentrations were found to increase following permafrost thaw and were highly constrained by total dissolved nitrogen concentrations. This ... |
format |
Article in Journal/Newspaper |
author |
L. Heffernan D. N. Kothawala L. J. Tranvik |
author_facet |
L. Heffernan D. N. Kothawala L. J. Tranvik |
author_sort |
L. Heffernan |
title |
Review article: Terrestrial dissolved organic carbon in northern permafrost |
title_short |
Review article: Terrestrial dissolved organic carbon in northern permafrost |
title_full |
Review article: Terrestrial dissolved organic carbon in northern permafrost |
title_fullStr |
Review article: Terrestrial dissolved organic carbon in northern permafrost |
title_full_unstemmed |
Review article: Terrestrial dissolved organic carbon in northern permafrost |
title_sort |
review article: terrestrial dissolved organic carbon in northern permafrost |
publisher |
Copernicus Publications |
publishDate |
2024 |
url |
https://doi.org/10.5194/tc-18-1443-2024 https://doaj.org/article/fbb91441113f492aaba3680e7ef5ee64 |
genre |
permafrost The Cryosphere Tundra |
genre_facet |
permafrost The Cryosphere Tundra |
op_source |
The Cryosphere, Vol 18, Pp 1443-1465 (2024) |
op_relation |
https://tc.copernicus.org/articles/18/1443/2024/tc-18-1443-2024.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-18-1443-2024 1994-0416 1994-0424 https://doaj.org/article/fbb91441113f492aaba3680e7ef5ee64 |
op_doi |
https://doi.org/10.5194/tc-18-1443-2024 |
container_title |
The Cryosphere |
container_volume |
18 |
container_issue |
3 |
container_start_page |
1443 |
op_container_end_page |
1465 |
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1810470693025873920 |