Mobilization of terrestrial organic matter from thawing Arctic permafrost regions: Insights from lignin-derived phenols and their compound-specific radiocarbon ages
Global climate change is expected to have a huge impact on Arctic warming, leading to an increased remobilization of permafrost organic carbon. More than twice as much carbon as in the atmosphere is contained in permafrost soils, and may upon destabilization expose large amounts of organic matter to...
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Language: | English |
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Universität Bremen
2023
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ftsubbremen:oai:media.suub.uni-bremen.de:Publications/elib/7462 2023-12-24T10:13:20+01:00 Mobilization of terrestrial organic matter from thawing Arctic permafrost regions: Insights from lignin-derived phenols and their compound-specific radiocarbon ages Cao, Mengli Tesi, Tommaso Mollenhauer, Gesine 2023-11-10 application/pdf https://media.suub.uni-bremen.de/handle/elib/7462 https://doi.org/10.26092/elib/2686 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib74629 eng eng Universität Bremen Fachbereich 05: Geowissenschaften (FB 05) https://media.suub.uni-bremen.de/handle/elib/7462 https://doi.org/10.26092/elib/2686 doi:10.26092/elib/2686 urn:nbn:de:gbv:46-elib74629 info:eu-repo/semantics/openAccess CC BY 4.0 (Attribution) Alle Rechte vorbehalten Permafrost Organic carbon Arctic Climate warming Lignin 550 550 Earth sciences and geology ddc:550 Dissertation doctoralThesis 2023 ftsubbremen https://doi.org/10.26092/elib/2686 2023-11-26T23:09:42Z Global climate change is expected to have a huge impact on Arctic warming, leading to an increased remobilization of permafrost organic carbon. More than twice as much carbon as in the atmosphere is contained in permafrost soils, and may upon destabilization expose large amounts of organic matter to microbial degradation and release climate-forcing greenhouse gases. As an important link in the land-ocean continuum, rivers are important pathways for permafrost OC remobilization. Arctic ocean sediments are thus receptors of terrestrial OC remobilization for a large part of the circum-Arctic drainage basin and offer an archive to study past terrestrial OC remobilization as during the last deglaciation. This thesis studies terrestrial OC in sub-Arctic ocean sediments to study OC remobilization from permafrost regions across temporal and spatial scales. A detailed study of two sediment cores from the Bering Sea and Okhotsk Sea, allowed the reconstruction of vegetation development, permafrost OC mobilization, and transport pathways of permafrost OC remobilization during the last deglaciation. Vegetation development and permafrost OC remobilization have been investigated by analyses of the mass accumulation rate of terrestrial biomarkers (lignin phenols and lipids). To study the influence of climatic conditions on the stability of inland permafrost soils, the sea surface temperature of the Bering Sea was investigated (TEXL86). For the study of terrestrial OC remobilization from different carbon pools, compound-specific radiocarbon analysis (CSRA) was applied to terrestrial compounds (lignin-derived phenols). A modified method for the purification of lignin-derived phenols was used for CSRA. Downcore records of lignin flux from the Yukon and Amur basins covering the early deglaciation to the Holocene are discussed in the first study. It was found that vegetation change and permafrost remobilization occurred earlier in the Yukon than in the Amur basin. The retreat of sea ice coupled with increased sea surface ... Doctoral or Postdoctoral Thesis Arctic Arctic Ocean Bering Sea Climate change Ice okhotsk sea permafrost Sea ice Yukon Media SuUB Bremen (Staats- und Universitätsbibliothek Bremen) Arctic Arctic Ocean Yukon Bering Sea Okhotsk |
institution |
Open Polar |
collection |
Media SuUB Bremen (Staats- und Universitätsbibliothek Bremen) |
op_collection_id |
ftsubbremen |
language |
English |
topic |
Permafrost Organic carbon Arctic Climate warming Lignin 550 550 Earth sciences and geology ddc:550 |
spellingShingle |
Permafrost Organic carbon Arctic Climate warming Lignin 550 550 Earth sciences and geology ddc:550 Cao, Mengli Mobilization of terrestrial organic matter from thawing Arctic permafrost regions: Insights from lignin-derived phenols and their compound-specific radiocarbon ages |
topic_facet |
Permafrost Organic carbon Arctic Climate warming Lignin 550 550 Earth sciences and geology ddc:550 |
description |
Global climate change is expected to have a huge impact on Arctic warming, leading to an increased remobilization of permafrost organic carbon. More than twice as much carbon as in the atmosphere is contained in permafrost soils, and may upon destabilization expose large amounts of organic matter to microbial degradation and release climate-forcing greenhouse gases. As an important link in the land-ocean continuum, rivers are important pathways for permafrost OC remobilization. Arctic ocean sediments are thus receptors of terrestrial OC remobilization for a large part of the circum-Arctic drainage basin and offer an archive to study past terrestrial OC remobilization as during the last deglaciation. This thesis studies terrestrial OC in sub-Arctic ocean sediments to study OC remobilization from permafrost regions across temporal and spatial scales. A detailed study of two sediment cores from the Bering Sea and Okhotsk Sea, allowed the reconstruction of vegetation development, permafrost OC mobilization, and transport pathways of permafrost OC remobilization during the last deglaciation. Vegetation development and permafrost OC remobilization have been investigated by analyses of the mass accumulation rate of terrestrial biomarkers (lignin phenols and lipids). To study the influence of climatic conditions on the stability of inland permafrost soils, the sea surface temperature of the Bering Sea was investigated (TEXL86). For the study of terrestrial OC remobilization from different carbon pools, compound-specific radiocarbon analysis (CSRA) was applied to terrestrial compounds (lignin-derived phenols). A modified method for the purification of lignin-derived phenols was used for CSRA. Downcore records of lignin flux from the Yukon and Amur basins covering the early deglaciation to the Holocene are discussed in the first study. It was found that vegetation change and permafrost remobilization occurred earlier in the Yukon than in the Amur basin. The retreat of sea ice coupled with increased sea surface ... |
author2 |
Tesi, Tommaso Mollenhauer, Gesine |
format |
Doctoral or Postdoctoral Thesis |
author |
Cao, Mengli |
author_facet |
Cao, Mengli |
author_sort |
Cao, Mengli |
title |
Mobilization of terrestrial organic matter from thawing Arctic permafrost regions: Insights from lignin-derived phenols and their compound-specific radiocarbon ages |
title_short |
Mobilization of terrestrial organic matter from thawing Arctic permafrost regions: Insights from lignin-derived phenols and their compound-specific radiocarbon ages |
title_full |
Mobilization of terrestrial organic matter from thawing Arctic permafrost regions: Insights from lignin-derived phenols and their compound-specific radiocarbon ages |
title_fullStr |
Mobilization of terrestrial organic matter from thawing Arctic permafrost regions: Insights from lignin-derived phenols and their compound-specific radiocarbon ages |
title_full_unstemmed |
Mobilization of terrestrial organic matter from thawing Arctic permafrost regions: Insights from lignin-derived phenols and their compound-specific radiocarbon ages |
title_sort |
mobilization of terrestrial organic matter from thawing arctic permafrost regions: insights from lignin-derived phenols and their compound-specific radiocarbon ages |
publisher |
Universität Bremen |
publishDate |
2023 |
url |
https://media.suub.uni-bremen.de/handle/elib/7462 https://doi.org/10.26092/elib/2686 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib74629 |
geographic |
Arctic Arctic Ocean Yukon Bering Sea Okhotsk |
geographic_facet |
Arctic Arctic Ocean Yukon Bering Sea Okhotsk |
genre |
Arctic Arctic Ocean Bering Sea Climate change Ice okhotsk sea permafrost Sea ice Yukon |
genre_facet |
Arctic Arctic Ocean Bering Sea Climate change Ice okhotsk sea permafrost Sea ice Yukon |
op_relation |
https://media.suub.uni-bremen.de/handle/elib/7462 https://doi.org/10.26092/elib/2686 doi:10.26092/elib/2686 urn:nbn:de:gbv:46-elib74629 |
op_rights |
info:eu-repo/semantics/openAccess CC BY 4.0 (Attribution) Alle Rechte vorbehalten |
op_doi |
https://doi.org/10.26092/elib/2686 |
_version_ |
1786181612929548288 |