Organic Carbon in Ice Complex deposits - characteristics and origin of the Yedoma Suite in East Siberian Arctic lowlands
Ongoing climate change and global warming may change the Ice Complex formation of the Yedoma Suite from a long-term carbon sink to a major carbon source due to thawing of organic-rich sediments and the subsequent release of greenhouse gases.The origin of Late-Pleistocene ice-rich, fine-grained perma...
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ftawi:oai:epic.awi.de:20977 2024-09-15T17:51:34+00:00 Organic Carbon in Ice Complex deposits - characteristics and origin of the Yedoma Suite in East Siberian Arctic lowlands Schirrmeister, Lutz Wetterich, Sebastian Grosse, Guido Siegert, Christine Overduin, Pier Paul Hubberten, Hans-Wolfgang 2009 application/pdf https://epic.awi.de/id/eprint/20977/ https://epic.awi.de/id/eprint/20977/1/Sch2009bf.pdf https://hdl.handle.net/10013/epic.33276 https://hdl.handle.net/10013/epic.33276.d001 unknown https://epic.awi.de/id/eprint/20977/1/Sch2009bf.pdf https://hdl.handle.net/10013/epic.33276.d001 Schirrmeister, L. orcid:0000-0001-9455-0596 , Wetterich, S. orcid:0000-0001-9234-1192 , Grosse, G. orcid:0000-0001-5895-2141 , Siegert, C. , Overduin, P. P. orcid:0000-0001-9849-4712 and Hubberten, H. W. (2009) Organic Carbon in Ice Complex deposits - characteristics and origin of the Yedoma Suite in East Siberian Arctic lowlands , 8th International Carbon Dioxide Conference, 2009, September 13-19 Jena, Germany. . hdl:10013/epic.33276 EPIC38th International Carbon Dioxide Conference, 2009, September 13-19 Jena, Germany. Conference notRev 2009 ftawi 2024-06-24T04:01:33Z Ongoing climate change and global warming may change the Ice Complex formation of the Yedoma Suite from a long-term carbon sink to a major carbon source due to thawing of organic-rich sediments and the subsequent release of greenhouse gases.The origin of Late-Pleistocene ice-rich, fine-grained permafrost sequences (Ice Complex deposits) in arctic and subarctic Siberia has been disputed for over a century. Corresponding permafrost sequences are frequently exposed along sea coasts and river banks in so-called Yedoma hills, which are considered to be the erosional remnants of Late Pleistocene accumulation plains. We have summarized cryolithological, sedimentological, geochronological, and stratigraphical results from 14 study sites along the Laptev and East Siberian Sea coasts in order to compare and correlate the local datasets. The Ice Complex was predominantly formed under subaerial conditions in polygonal tundra landscapes. Ice Complex deposits at all sites are sequences of buried cryosols. Separate cryosol horizons are characterized by brownish organic-rich patches, peat nests, and numerous individual plant remains ranging from well-preserved grass roots to twigs and leaves. Cryoturbation patterns of 0.5 to 1 m thickness are very common. The average total organic carbon content (TOC) is relative high for individual sites (1.2 to 4.8 wt%), but strongly varies for individual horizons within a sequence (0.5 to 27 wt%). Such variation in TOC is caused by alternation of mineral- and organic-rich horizons and the presence of irregular patches where organic remains concentrated during deposition. The TOC variations are similar to modern typical Aquiturbels in polygon walls (0.5-3.5 wt%) and typical Historthels in polygon centers (1 to >20 wt%), and therefore its occurrence represents a massive permafrost carbon reservoir. According to several paleo-botanical analyses, herbs (e.g. Artemisia, Carophyllaceae, Asteraceae), grasses (e.g. Poacea, Cyperacea), and partly some dwarf shrubs (e.g. Salix, Alnus, Betula) ... Conference Object Arctic Climate change East Siberian Sea Global warming Ice laptev permafrost Subarctic Tundra Siberia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
institution |
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 |
Ongoing climate change and global warming may change the Ice Complex formation of the Yedoma Suite from a long-term carbon sink to a major carbon source due to thawing of organic-rich sediments and the subsequent release of greenhouse gases.The origin of Late-Pleistocene ice-rich, fine-grained permafrost sequences (Ice Complex deposits) in arctic and subarctic Siberia has been disputed for over a century. Corresponding permafrost sequences are frequently exposed along sea coasts and river banks in so-called Yedoma hills, which are considered to be the erosional remnants of Late Pleistocene accumulation plains. We have summarized cryolithological, sedimentological, geochronological, and stratigraphical results from 14 study sites along the Laptev and East Siberian Sea coasts in order to compare and correlate the local datasets. The Ice Complex was predominantly formed under subaerial conditions in polygonal tundra landscapes. Ice Complex deposits at all sites are sequences of buried cryosols. Separate cryosol horizons are characterized by brownish organic-rich patches, peat nests, and numerous individual plant remains ranging from well-preserved grass roots to twigs and leaves. Cryoturbation patterns of 0.5 to 1 m thickness are very common. The average total organic carbon content (TOC) is relative high for individual sites (1.2 to 4.8 wt%), but strongly varies for individual horizons within a sequence (0.5 to 27 wt%). Such variation in TOC is caused by alternation of mineral- and organic-rich horizons and the presence of irregular patches where organic remains concentrated during deposition. The TOC variations are similar to modern typical Aquiturbels in polygon walls (0.5-3.5 wt%) and typical Historthels in polygon centers (1 to >20 wt%), and therefore its occurrence represents a massive permafrost carbon reservoir. According to several paleo-botanical analyses, herbs (e.g. Artemisia, Carophyllaceae, Asteraceae), grasses (e.g. Poacea, Cyperacea), and partly some dwarf shrubs (e.g. Salix, Alnus, Betula) ... |
format |
Conference Object |
author |
Schirrmeister, Lutz Wetterich, Sebastian Grosse, Guido Siegert, Christine Overduin, Pier Paul Hubberten, Hans-Wolfgang |
spellingShingle |
Schirrmeister, Lutz Wetterich, Sebastian Grosse, Guido Siegert, Christine Overduin, Pier Paul Hubberten, Hans-Wolfgang Organic Carbon in Ice Complex deposits - characteristics and origin of the Yedoma Suite in East Siberian Arctic lowlands |
author_facet |
Schirrmeister, Lutz Wetterich, Sebastian Grosse, Guido Siegert, Christine Overduin, Pier Paul Hubberten, Hans-Wolfgang |
author_sort |
Schirrmeister, Lutz |
title |
Organic Carbon in Ice Complex deposits - characteristics and origin of the Yedoma Suite in East Siberian Arctic lowlands |
title_short |
Organic Carbon in Ice Complex deposits - characteristics and origin of the Yedoma Suite in East Siberian Arctic lowlands |
title_full |
Organic Carbon in Ice Complex deposits - characteristics and origin of the Yedoma Suite in East Siberian Arctic lowlands |
title_fullStr |
Organic Carbon in Ice Complex deposits - characteristics and origin of the Yedoma Suite in East Siberian Arctic lowlands |
title_full_unstemmed |
Organic Carbon in Ice Complex deposits - characteristics and origin of the Yedoma Suite in East Siberian Arctic lowlands |
title_sort |
organic carbon in ice complex deposits - characteristics and origin of the yedoma suite in east siberian arctic lowlands |
publishDate |
2009 |
url |
https://epic.awi.de/id/eprint/20977/ https://epic.awi.de/id/eprint/20977/1/Sch2009bf.pdf https://hdl.handle.net/10013/epic.33276 https://hdl.handle.net/10013/epic.33276.d001 |
genre |
Arctic Climate change East Siberian Sea Global warming Ice laptev permafrost Subarctic Tundra Siberia |
genre_facet |
Arctic Climate change East Siberian Sea Global warming Ice laptev permafrost Subarctic Tundra Siberia |
op_source |
EPIC38th International Carbon Dioxide Conference, 2009, September 13-19 Jena, Germany. |
op_relation |
https://epic.awi.de/id/eprint/20977/1/Sch2009bf.pdf https://hdl.handle.net/10013/epic.33276.d001 Schirrmeister, L. orcid:0000-0001-9455-0596 , Wetterich, S. orcid:0000-0001-9234-1192 , Grosse, G. orcid:0000-0001-5895-2141 , Siegert, C. , Overduin, P. P. orcid:0000-0001-9849-4712 and Hubberten, H. W. (2009) Organic Carbon in Ice Complex deposits - characteristics and origin of the Yedoma Suite in East Siberian Arctic lowlands , 8th International Carbon Dioxide Conference, 2009, September 13-19 Jena, Germany. . hdl:10013/epic.33276 |
_version_ |
1810293510205603840 |