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Ice Complex permafrost of MIS5 age in the Dmitry Laptev Strait coastal region (East Siberian Arctic)

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dc.contributor.author Wetterich S.
dc.contributor.author Tumskoy V.
dc.contributor.author Rudaya N.
dc.contributor.author Kuznetsov V.
dc.contributor.author Maksimov F.
dc.contributor.author Opel T.
dc.contributor.author Meyer H.
dc.contributor.author Andreev A.
dc.contributor.author Schirrmeister L.
dc.date.accessioned 2018-09-19T20:28:27Z
dc.date.available 2018-09-19T20:28:27Z
dc.date.issued 2016
dc.identifier.issn 0277-3791
dc.identifier.uri https://dspace.kpfu.ru/xmlui/handle/net/142936
dc.description.abstract © 2015 Elsevier LtdIce Complex deposits (locally known as the Buchchagy Ice Complex) are exposed at both coasts of the East Siberian Dmitry Laptev Strait and preserved below the Yedoma Ice Complex that formed during MIS3 and MIS2 (Marine Isotope Stage) and lateglacial-Holocene thermokarst deposits (MIS1). Radioisotope disequilibria (230Th/U) of peaty horizons date the Buchchagy Ice Complex deposition to 126 + 16/−13 kyr and 117 + 19/−14 kyr until 98 ± 5 kyr and 89 ± 5 kyr. The deposit is characterised by poorly-sorted medium-to-coarse silts with cryogenic structures of horizontal ice bands, lens-like, and lens-like reticulated segregation ice. Two peaty horizons within the Buchchagy Ice Complex and syngenetic ice wedges (2–4 m wide, up to 10 m high) are striking. The isotopic composition (δ18O, δD) of Buchchagy ice-wedge ice indicates winter conditions colder than during the MIS3 interstadial and warmer than during MIS2 stadial, and similar atmospheric winter moisture sources as during the MIS2 stadial. Buchchagy Ice Complex pollen spectra reveal tundra-steppe vegetation and harsher summer conditions than during the MIS3 interstadial and rather similar vegetation as during the MIS2 stadial. Short-term climatic variability during MIS5 is reflected in the record. Even though the regional chronostratigraphic relationship of the Buchchagy Ice Complex to the Last Interglacial remains unclear because numerical dating is widely lacking, the present study indicates permafrost (Ice Complex) formation during MIS5 sensu lato, and its preservation afterwards. Palaeoenvironmental insights into past climate and the periglacial landscape dynamics of arctic lowlands in eastern Siberia are deduced from the record.
dc.relation.ispartofseries Quaternary Science Reviews
dc.subject 230 Th/U dating
dc.subject Beringia
dc.subject Bol'shoy Lyakhovsky Island
dc.subject Cryostratigraphy
dc.subject Marine Isotope Stage 5
dc.subject Oyogos Yar
dc.subject Palaeoenvironments
dc.subject Permafrost
dc.title Ice Complex permafrost of MIS5 age in the Dmitry Laptev Strait coastal region (East Siberian Arctic)
dc.type Article
dc.relation.ispartofseries-volume 147
dc.collection Публикации сотрудников КФУ
dc.relation.startpage 298
dc.source.id SCOPUS02773791-2016-147-SID84989836110


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    Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.

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