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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Main Author: sun, Y (via Mendeley Data)
Language:unknown
Published: 2024
Subjects:
Online Access:http://nbn-resolving.org/urn:nbn:nl:ui:13-3e-lsom
https://easy.dans.knaw.nl/ui/datasets/id/easy-dataset:337830
id ftdans:oai:easy.dans.knaw.nl:easy-dataset:337830
record_format openpolar
spelling 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
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