Ice Complex formation in arctic East Siberia during the MIS3 Interstadial

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...

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Published in:Quaternary Science Reviews
Main Authors: Wetterich, Sebastian, Tumskoy, Vladimir, Rudaya, Natalia A., Andreev, Andreev, Opel, Thomas, Meyer, Hanno, Schirrmeister, Lutz, Hüls, Matthias
Format: Article in Journal/Newspaper
Language:unknown
Published: PERGAMON-ELSEVIER SCIENCE LTD 2014
Subjects:
Ice
Online Access:https://epic.awi.de/id/eprint/34541/
https://epic.awi.de/id/eprint/34541/1/Wetterich_2014.pdf
https://hdl.handle.net/10013/epic.42763
https://hdl.handle.net/10013/epic.42763.d001
id ftawi:oai:epic.awi.de:34541
record_format openpolar
spelling ftawi:oai:epic.awi.de:34541 2023-05-15T14:27:52+02:00 Ice Complex formation in arctic East Siberia during the MIS3 Interstadial Wetterich, Sebastian Tumskoy, Vladimir Rudaya, Natalia A. Andreev, Andreev Opel, Thomas Meyer, Hanno Schirrmeister, Lutz Hüls, Matthias 2014 application/pdf https://epic.awi.de/id/eprint/34541/ https://epic.awi.de/id/eprint/34541/1/Wetterich_2014.pdf https://hdl.handle.net/10013/epic.42763 https://hdl.handle.net/10013/epic.42763.d001 unknown PERGAMON-ELSEVIER SCIENCE LTD https://epic.awi.de/id/eprint/34541/1/Wetterich_2014.pdf https://hdl.handle.net/10013/epic.42763.d001 Wetterich, S. orcid:0000-0001-9234-1192 , Tumskoy, V. , Rudaya, N. A. , Andreev, A. , Opel, T. orcid:0000-0003-1315-8256 , Meyer, H. orcid:0000-0003-4129-4706 , Schirrmeister, L. orcid:0000-0001-9455-0596 and Hüls, M. (2014) Ice Complex formation in arctic East Siberia during the MIS3 Interstadial , Quaternary Science Reviews, 84 , pp. 39-55 . doi:10.1016/j.quascirev.2013.11.009 <https://doi.org/10.1016/j.quascirev.2013.11.009> , hdl:10013/epic.42763 EPIC3Quaternary Science Reviews, PERGAMON-ELSEVIER SCIENCE LTD, 84, pp. 39-55, ISSN: 0277-3791 Article isiRev 2014 ftawi https://doi.org/10.1016/j.quascirev.2013.11.009 2022-04-03T23:09:55Z 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 freezeethaw 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 stadialinterstadial 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. Article in Journal/Newspaper Arctic Arctic Ice laptev permafrost wedge* Beringia Siberia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Arctic Quaternary Science Reviews 84 39 55
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description 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 freezeethaw 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 stadialinterstadial 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.
format Article in Journal/Newspaper
author Wetterich, Sebastian
Tumskoy, Vladimir
Rudaya, Natalia A.
Andreev, Andreev
Opel, Thomas
Meyer, Hanno
Schirrmeister, Lutz
Hüls, Matthias
spellingShingle Wetterich, Sebastian
Tumskoy, Vladimir
Rudaya, Natalia A.
Andreev, Andreev
Opel, Thomas
Meyer, Hanno
Schirrmeister, Lutz
Hüls, Matthias
Ice Complex formation in arctic East Siberia during the MIS3 Interstadial
author_facet Wetterich, Sebastian
Tumskoy, Vladimir
Rudaya, Natalia A.
Andreev, Andreev
Opel, Thomas
Meyer, Hanno
Schirrmeister, Lutz
Hüls, 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://epic.awi.de/id/eprint/34541/
https://epic.awi.de/id/eprint/34541/1/Wetterich_2014.pdf
https://hdl.handle.net/10013/epic.42763
https://hdl.handle.net/10013/epic.42763.d001
geographic Arctic
geographic_facet Arctic
genre Arctic
Arctic
Ice
laptev
permafrost
wedge*
Beringia
Siberia
genre_facet Arctic
Arctic
Ice
laptev
permafrost
wedge*
Beringia
Siberia
op_source EPIC3Quaternary Science Reviews, PERGAMON-ELSEVIER SCIENCE LTD, 84, pp. 39-55, ISSN: 0277-3791
op_relation https://epic.awi.de/id/eprint/34541/1/Wetterich_2014.pdf
https://hdl.handle.net/10013/epic.42763.d001
Wetterich, S. orcid:0000-0001-9234-1192 , Tumskoy, V. , Rudaya, N. A. , Andreev, A. , Opel, T. orcid:0000-0003-1315-8256 , Meyer, H. orcid:0000-0003-4129-4706 , Schirrmeister, L. orcid:0000-0001-9455-0596 and Hüls, M. (2014) Ice Complex formation in arctic East Siberia during the MIS3 Interstadial , Quaternary Science Reviews, 84 , pp. 39-55 . doi:10.1016/j.quascirev.2013.11.009 <https://doi.org/10.1016/j.quascirev.2013.11.009> , hdl:10013/epic.42763
op_doi https://doi.org/10.1016/j.quascirev.2013.11.009
container_title Quaternary Science Reviews
container_volume 84
container_start_page 39
op_container_end_page 55
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