Spatial heterogeneity of sedimentary organic carbon accumulation and degradation along the Arctic continental margins
The warming climate has led to the translocation of a large amount of terrestrial organic carbon (TerrOC) from permafrost into the Arctic Ocean through river transport and coastal erosion. The fate of sedimentary organic carbon (SOC) varies dramatically and thus affects climate-carbon feedback. We a...
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ftdans:oai:easy.dans.knaw.nl:easy-dataset:337830 2024-04-21T07:55:56+00:00 Spatial heterogeneity of sedimentary organic carbon accumulation and degradation along the Arctic continental margins sun, Y (via Mendeley Data) 2024-03-26T13:21:29.936Z http://nbn-resolving.org/urn:nbn:nl:ui:13-3e-lsom https://easy.dans.knaw.nl/ui/datasets/id/easy-dataset:337830 unknown 1 29gycgdhc2 http://nbn-resolving.org/urn:nbn:nl:ui:13-3e-lsom doi:10.17632/29gycgdhc2.1 https://easy.dans.knaw.nl/ui/datasets/id/easy-dataset:337830 OPEN_ACCESS: The data are archived in Easy, they are accessible elsewhere through the DOI https://dans.knaw.nl/en/about/organisation-and-policy/legal-information/DANSLicence.pdf yifang sun Interdisciplinary sciences 2024 ftdans https://doi.org/10.17632/29gycgdhc2.1 2024-03-27T15:21:25Z The warming climate has led to the translocation of a large amount of terrestrial organic carbon (TerrOC) from permafrost into the Arctic Ocean through river transport and coastal erosion. The fate of sedimentary organic carbon (SOC) varies dramatically and thus affects climate-carbon feedback. We analyzed the spatial heterogeneity of SOC sources and degradation along the East Siberian Arctic Shelf (ESAS) with bulk parameters (total organic carbon, δ13C) and a biomarker (lignin) for comparison of the spatial heterogeneity of TerrOC degradation between the broad ESAS and the narrow Amerasian continental shelf. The results show that the relative importance of river runoff, coastal erosion, and primary productivity causes alongshore variations in organic carbon (OC) sources within the ESAS, highlighting the effects of land-based inputs and ocean currents. Meanwhile, the variations of OC sources show gradually diminishing terrestrial signals in the seaward direction. The simultaneous offshore decrease in OC loadings and increase in lignin degradation indicate that the degradation of TerrOC within a water depth of 100 m is a key mechanism driving the cross-shelf loss of OC in the ESAS. Compared to the broad ESAS, the inconspicuous variations in Λ8/SSA and 3,5-Bd/V across the narrow Amerasian margin suggest that the width of the continental shelf is vital in determining the fate of TerrOC, despite greater levels of recalcitrant petrogenic OC in the Beaufort Sea. In general, the insights have profound implications for evaluating the coastal remobilization and preservation of SOC and its climate-carbon feedback across diverse pan-Arctic continental shelves. THIS DATASET IS ARCHIVED AT DANS/EASY, BUT NOT ACCESSIBLE HERE. TO VIEW A LIST OF FILES AND ACCESS THE FILES IN THIS DATASET CLICK ON THE DOI-LINK ABOVE Other/Unknown Material Arctic Ocean Beaufort Sea permafrost Data Archiving and Networked Services (DANS): EASY (KNAW - Koninklijke Nederlandse Akademie van Wetenschappen) |
institution |
Open Polar |
collection |
Data Archiving and Networked Services (DANS): EASY (KNAW - Koninklijke Nederlandse Akademie van Wetenschappen) |
op_collection_id |
ftdans |
language |
unknown |
topic |
Interdisciplinary sciences |
spellingShingle |
Interdisciplinary sciences sun, Y (via Mendeley Data) Spatial heterogeneity of sedimentary organic carbon accumulation and degradation along the Arctic continental margins |
topic_facet |
Interdisciplinary sciences |
description |
The warming climate has led to the translocation of a large amount of terrestrial organic carbon (TerrOC) from permafrost into the Arctic Ocean through river transport and coastal erosion. The fate of sedimentary organic carbon (SOC) varies dramatically and thus affects climate-carbon feedback. We analyzed the spatial heterogeneity of SOC sources and degradation along the East Siberian Arctic Shelf (ESAS) with bulk parameters (total organic carbon, δ13C) and a biomarker (lignin) for comparison of the spatial heterogeneity of TerrOC degradation between the broad ESAS and the narrow Amerasian continental shelf. The results show that the relative importance of river runoff, coastal erosion, and primary productivity causes alongshore variations in organic carbon (OC) sources within the ESAS, highlighting the effects of land-based inputs and ocean currents. Meanwhile, the variations of OC sources show gradually diminishing terrestrial signals in the seaward direction. The simultaneous offshore decrease in OC loadings and increase in lignin degradation indicate that the degradation of TerrOC within a water depth of 100 m is a key mechanism driving the cross-shelf loss of OC in the ESAS. Compared to the broad ESAS, the inconspicuous variations in Λ8/SSA and 3,5-Bd/V across the narrow Amerasian margin suggest that the width of the continental shelf is vital in determining the fate of TerrOC, despite greater levels of recalcitrant petrogenic OC in the Beaufort Sea. In general, the insights have profound implications for evaluating the coastal remobilization and preservation of SOC and its climate-carbon feedback across diverse pan-Arctic continental shelves. THIS DATASET IS ARCHIVED AT DANS/EASY, BUT NOT ACCESSIBLE HERE. TO VIEW A LIST OF FILES AND ACCESS THE FILES IN THIS DATASET CLICK ON THE DOI-LINK ABOVE |
author |
sun, Y (via Mendeley Data) |
author_facet |
sun, Y (via Mendeley Data) |
author_sort |
sun, Y (via Mendeley Data) |
title |
Spatial heterogeneity of sedimentary organic carbon accumulation and degradation along the Arctic continental margins |
title_short |
Spatial heterogeneity of sedimentary organic carbon accumulation and degradation along the Arctic continental margins |
title_full |
Spatial heterogeneity of sedimentary organic carbon accumulation and degradation along the Arctic continental margins |
title_fullStr |
Spatial heterogeneity of sedimentary organic carbon accumulation and degradation along the Arctic continental margins |
title_full_unstemmed |
Spatial heterogeneity of sedimentary organic carbon accumulation and degradation along the Arctic continental margins |
title_sort |
spatial heterogeneity of sedimentary organic carbon accumulation and degradation along the arctic continental margins |
publishDate |
2024 |
url |
http://nbn-resolving.org/urn:nbn:nl:ui:13-3e-lsom https://easy.dans.knaw.nl/ui/datasets/id/easy-dataset:337830 |
genre |
Arctic Ocean Beaufort Sea permafrost |
genre_facet |
Arctic Ocean Beaufort Sea permafrost |
op_relation |
1 29gycgdhc2 http://nbn-resolving.org/urn:nbn:nl:ui:13-3e-lsom doi:10.17632/29gycgdhc2.1 https://easy.dans.knaw.nl/ui/datasets/id/easy-dataset:337830 |
op_rights |
OPEN_ACCESS: The data are archived in Easy, they are accessible elsewhere through the DOI https://dans.knaw.nl/en/about/organisation-and-policy/legal-information/DANSLicence.pdf yifang sun |
op_doi |
https://doi.org/10.17632/29gycgdhc2.1 |
_version_ |
1796938161173037056 |