Thermokarst Processes and Depositional Events in a Tundra Lake, Northeastern Siberia
The relationships between thermokarst activity, limnogeological processes and climate change in the Siberian Arctic are not well understood. The objective of this paper is to identify the factors controlling the patterns of deposition, using grain-size distributions, organic contents, elemental comp...
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Online Access: | https://epic.awi.de/id/eprint/32031/ https://hdl.handle.net/10013/epic.41360 |
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ftawi:oai:epic.awi.de:32031 2024-09-15T18:02:25+00:00 Thermokarst Processes and Depositional Events in a Tundra Lake, Northeastern Siberia Biskaborn, Boris Herzschuh, Ulrike Bolshiyanov, D. Y. Schwamborn, Georg Diekmann, Bernhard 2013 https://epic.awi.de/id/eprint/32031/ https://hdl.handle.net/10013/epic.41360 unknown Wiley Online Library Biskaborn, B. orcid:0000-0003-2378-0348 , Herzschuh, U. orcid:0000-0003-0999-1261 , Bolshiyanov, D. Y. , Schwamborn, G. and Diekmann, B. orcid:0000-0001-5129-3649 (2013) Thermokarst Processes and Depositional Events in a Tundra Lake, Northeastern Siberia , Permafrost and Periglacial Processes . doi:10.1002/ppp.1769 <https://doi.org/10.1002/ppp.1769> , hdl:10013/epic.41360 EPIC3Permafrost and Periglacial Processes, Wiley Online Library Article isiRev 2013 ftawi https://doi.org/10.1002/ppp.1769 2024-06-24T04:06:16Z The relationships between thermokarst activity, limnogeological processes and climate change in the Siberian Arctic are not well understood. The objective of this paper is to identify the factors controlling the patterns of deposition, using grain-size distributions, organic contents, elemental compositions and mineralogical compositions of a 137-cm-long sediment core with a maximum age of ~10.9 cal. kyr BP from Lake El’gene-Kyuele, in the tundra of north-eastern Siberia. Eight fine sand layers are attributed to depositional events associated with thaw slump activity acting upon orthogonally oriented patterns of the ice-wedge networks in the ice-rich permafrost on the NW margin of the lake catchment. Sr/Rb ratios, which correspond to the total feldspar and illite content, serve as high-resolution grain-size proxies. The Br content relates to the total organic carbon (TOC) content, and the Fe/Mn ratio reflects the degree of oxidisation. Our results indicate a relationship between repeated phases of fine sand input and retrogressive thaw slumping dependent on hydroclimate variability and orthogonally oriented ice-wedge networks within the catchment. Article in Journal/Newspaper Climate change Ice permafrost Permafrost and Periglacial Processes Thermokarst Tundra wedge* Siberia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Permafrost and Periglacial Processes 24 3 160 174 |
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Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
The relationships between thermokarst activity, limnogeological processes and climate change in the Siberian Arctic are not well understood. The objective of this paper is to identify the factors controlling the patterns of deposition, using grain-size distributions, organic contents, elemental compositions and mineralogical compositions of a 137-cm-long sediment core with a maximum age of ~10.9 cal. kyr BP from Lake El’gene-Kyuele, in the tundra of north-eastern Siberia. Eight fine sand layers are attributed to depositional events associated with thaw slump activity acting upon orthogonally oriented patterns of the ice-wedge networks in the ice-rich permafrost on the NW margin of the lake catchment. Sr/Rb ratios, which correspond to the total feldspar and illite content, serve as high-resolution grain-size proxies. The Br content relates to the total organic carbon (TOC) content, and the Fe/Mn ratio reflects the degree of oxidisation. Our results indicate a relationship between repeated phases of fine sand input and retrogressive thaw slumping dependent on hydroclimate variability and orthogonally oriented ice-wedge networks within the catchment. |
format |
Article in Journal/Newspaper |
author |
Biskaborn, Boris Herzschuh, Ulrike Bolshiyanov, D. Y. Schwamborn, Georg Diekmann, Bernhard |
spellingShingle |
Biskaborn, Boris Herzschuh, Ulrike Bolshiyanov, D. Y. Schwamborn, Georg Diekmann, Bernhard Thermokarst Processes and Depositional Events in a Tundra Lake, Northeastern Siberia |
author_facet |
Biskaborn, Boris Herzschuh, Ulrike Bolshiyanov, D. Y. Schwamborn, Georg Diekmann, Bernhard |
author_sort |
Biskaborn, Boris |
title |
Thermokarst Processes and Depositional Events in a Tundra Lake, Northeastern Siberia |
title_short |
Thermokarst Processes and Depositional Events in a Tundra Lake, Northeastern Siberia |
title_full |
Thermokarst Processes and Depositional Events in a Tundra Lake, Northeastern Siberia |
title_fullStr |
Thermokarst Processes and Depositional Events in a Tundra Lake, Northeastern Siberia |
title_full_unstemmed |
Thermokarst Processes and Depositional Events in a Tundra Lake, Northeastern Siberia |
title_sort |
thermokarst processes and depositional events in a tundra lake, northeastern siberia |
publisher |
Wiley Online Library |
publishDate |
2013 |
url |
https://epic.awi.de/id/eprint/32031/ https://hdl.handle.net/10013/epic.41360 |
genre |
Climate change Ice permafrost Permafrost and Periglacial Processes Thermokarst Tundra wedge* Siberia |
genre_facet |
Climate change Ice permafrost Permafrost and Periglacial Processes Thermokarst Tundra wedge* Siberia |
op_source |
EPIC3Permafrost and Periglacial Processes, Wiley Online Library |
op_relation |
Biskaborn, B. orcid:0000-0003-2378-0348 , Herzschuh, U. orcid:0000-0003-0999-1261 , Bolshiyanov, D. Y. , Schwamborn, G. and Diekmann, B. orcid:0000-0001-5129-3649 (2013) Thermokarst Processes and Depositional Events in a Tundra Lake, Northeastern Siberia , Permafrost and Periglacial Processes . doi:10.1002/ppp.1769 <https://doi.org/10.1002/ppp.1769> , hdl:10013/epic.41360 |
op_doi |
https://doi.org/10.1002/ppp.1769 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
24 |
container_issue |
3 |
container_start_page |
160 |
op_container_end_page |
174 |
_version_ |
1810439876496064512 |