Ice Complex formation in arctic East Siberia during the MIS3 Interstadial

A continuous 15 m long sequence of Ice Complex permafrost (Yedoma) exposed in a thermo-cirque at the southern coast of Bol'shoy Lyakhovsky Island (New Siberian Archipelago, Dmitry Laptev Strait) was studied to reconstruct past landscape and environmental dynamics. The sequence accumulated durin...

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Main Authors: Wetterich, Sebastian, Tumskoy, Vladimir, Rudaya, Natalia, Andreev, Andrei A., Opel, Thomas, Meyer, Hanno, Schirrmeister, Lutz, Huels, Matthias
Format: Article in Journal/Newspaper
Language:English
Published: PERGAMON-ELSEVIER SCIENCE LTD 2014
Subjects:
Ice
Online Access:https://kups.ub.uni-koeln.de/44846/
id ftubkoeln:oai:USBKOELN.ub.uni-koeln.de:44846
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spelling ftubkoeln:oai:USBKOELN.ub.uni-koeln.de:44846 2023-05-15T14:26:59+02:00 Ice Complex formation in arctic East Siberia during the MIS3 Interstadial Wetterich, Sebastian Tumskoy, Vladimir Rudaya, Natalia Andreev, Andrei A. Opel, Thomas Meyer, Hanno Schirrmeister, Lutz Huels, Matthias 2014 https://kups.ub.uni-koeln.de/44846/ eng eng PERGAMON-ELSEVIER SCIENCE LTD Wetterich, Sebastian, Tumskoy, Vladimir, Rudaya, Natalia orcid:0000-0003-1536-6470 , Andreev, Andrei A., Opel, Thomas orcid:0000-0003-1315-8256 , Meyer, Hanno orcid:0000-0003-4129-4706 , Schirrmeister, Lutz orcid:0000-0001-9455-0596 and Huels, Matthias (2014). Ice Complex formation in arctic East Siberia during the MIS3 Interstadial. Quat. Sci. Rev., 84. S. 39 - 56. OXFORD: PERGAMON-ELSEVIER SCIENCE LTD. ISSN 0277-3791 ddc:no doc-type:article publishedVersion 2014 ftubkoeln 2022-11-09T07:28:53Z A continuous 15 m long sequence of Ice Complex permafrost (Yedoma) exposed in a thermo-cirque at the southern coast of Bol'shoy Lyakhovsky Island (New Siberian Archipelago, Dmitry Laptev Strait) was studied to reconstruct past landscape and environmental dynamics. The sequence accumulated during the Marine Isotope Stage 3 (MIS3) Interstadial between >49 and 29 ka BP in an ice-wedge polygon. The frozen deposits were cryolithologically described and sampled on a vertical bluff between two ice wedges. According to sedimentological and geochronological data, the section is subdivided into three units which correlate with environmental conditions of the early, middle, and late MIS3 period. Palynological data support this stratification. The stable isotope signature of texture ice in the polygon structure reflects fractionation due to local freeze thaw processes, while the signature of an approximately 5 m wide and more than 17 m high ice wedge fits very well into the regional stable-water isotope record. Regional climate dynamics during the MIS3 Interstadial and local landscape conditions of the polygonal patterned ground controlled the Ice Complex formation. The sequence presented here completes previously published MIS3 permafrost records in Northeast Siberia. Late Quaternary stadial-interstadial climate variability in arctic West Beringia is preserved at millennial resolution in the Ice Complex. A MIS3 climate optimum was revealed between 48 and 38 ka BP from the Ice Complex on Bol'shoy Lyakhovsky Island. (C) 2013 Elsevier Ltd. All rights reserved. Article in Journal/Newspaper Arctic Arctic Ice laptev permafrost wedge* Beringia Siberia Cologne University: KUPS Arctic Island C ENVELOPE(-115.753,-115.753,60.834,60.834)
institution Open Polar
collection Cologne University: KUPS
op_collection_id ftubkoeln
language English
topic ddc:no
spellingShingle ddc:no
Wetterich, Sebastian
Tumskoy, Vladimir
Rudaya, Natalia
Andreev, Andrei A.
Opel, Thomas
Meyer, Hanno
Schirrmeister, Lutz
Huels, Matthias
Ice Complex formation in arctic East Siberia during the MIS3 Interstadial
topic_facet ddc:no
description A continuous 15 m long sequence of Ice Complex permafrost (Yedoma) exposed in a thermo-cirque at the southern coast of Bol'shoy Lyakhovsky Island (New Siberian Archipelago, Dmitry Laptev Strait) was studied to reconstruct past landscape and environmental dynamics. The sequence accumulated during the Marine Isotope Stage 3 (MIS3) Interstadial between >49 and 29 ka BP in an ice-wedge polygon. The frozen deposits were cryolithologically described and sampled on a vertical bluff between two ice wedges. According to sedimentological and geochronological data, the section is subdivided into three units which correlate with environmental conditions of the early, middle, and late MIS3 period. Palynological data support this stratification. The stable isotope signature of texture ice in the polygon structure reflects fractionation due to local freeze thaw processes, while the signature of an approximately 5 m wide and more than 17 m high ice wedge fits very well into the regional stable-water isotope record. Regional climate dynamics during the MIS3 Interstadial and local landscape conditions of the polygonal patterned ground controlled the Ice Complex formation. The sequence presented here completes previously published MIS3 permafrost records in Northeast Siberia. Late Quaternary stadial-interstadial climate variability in arctic West Beringia is preserved at millennial resolution in the Ice Complex. A MIS3 climate optimum was revealed between 48 and 38 ka BP from the Ice Complex on Bol'shoy Lyakhovsky Island. (C) 2013 Elsevier Ltd. All rights reserved.
format Article in Journal/Newspaper
author Wetterich, Sebastian
Tumskoy, Vladimir
Rudaya, Natalia
Andreev, Andrei A.
Opel, Thomas
Meyer, Hanno
Schirrmeister, Lutz
Huels, Matthias
author_facet Wetterich, Sebastian
Tumskoy, Vladimir
Rudaya, Natalia
Andreev, Andrei A.
Opel, Thomas
Meyer, Hanno
Schirrmeister, Lutz
Huels, Matthias
author_sort Wetterich, Sebastian
title Ice Complex formation in arctic East Siberia during the MIS3 Interstadial
title_short Ice Complex formation in arctic East Siberia during the MIS3 Interstadial
title_full Ice Complex formation in arctic East Siberia during the MIS3 Interstadial
title_fullStr Ice Complex formation in arctic East Siberia during the MIS3 Interstadial
title_full_unstemmed Ice Complex formation in arctic East Siberia during the MIS3 Interstadial
title_sort ice complex formation in arctic east siberia during the mis3 interstadial
publisher PERGAMON-ELSEVIER SCIENCE LTD
publishDate 2014
url https://kups.ub.uni-koeln.de/44846/
long_lat ENVELOPE(-115.753,-115.753,60.834,60.834)
geographic Arctic
Island C
geographic_facet Arctic
Island C
genre Arctic
Arctic
Ice
laptev
permafrost
wedge*
Beringia
Siberia
genre_facet Arctic
Arctic
Ice
laptev
permafrost
wedge*
Beringia
Siberia
op_relation Wetterich, Sebastian, Tumskoy, Vladimir, Rudaya, Natalia orcid:0000-0003-1536-6470 , Andreev, Andrei A., Opel, Thomas orcid:0000-0003-1315-8256 , Meyer, Hanno orcid:0000-0003-4129-4706 , Schirrmeister, Lutz orcid:0000-0001-9455-0596 and Huels, Matthias (2014). Ice Complex formation in arctic East Siberia during the MIS3 Interstadial. Quat. Sci. Rev., 84. S. 39 - 56. OXFORD: PERGAMON-ELSEVIER SCIENCE LTD. ISSN 0277-3791
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