PLEISTOCENE-HOLOCENE PALAEOENVIRONMENTAL RECORDS FROM PERMAFROST SEQUENCES AT THE KARA SEA COAST (NW SIBERIA, RUSSIA)

The Kara Sea coasts were studied using comprehensive stratigraphic and geocryological methods. The paper presents the new analytical studies of ground ice and Quaternary deposits of Western Taymyr and presents the results of spore and pollen, foraminifera, grain-size, mineralogical, geochemical, oxy...

Full description

Bibliographic Details
Published in:GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY
Main Authors: Irina Streletskaya, Evgeny Gusev, Alexander Vasiliev, Gleb Oblogov, Anatoly Molodkov
Format: Article in Journal/Newspaper
Language:English
Published: Russian Geographical Society 2013
Subjects:
Ice
Online Access:https://ges.rgo.ru/jour/article/view/140
https://doi.org/10.24057/2071-9388-2013-6-3-60-76
id ftjges:oai:oai.gesj.elpub.ru:article/140
record_format openpolar
institution Open Polar
collection Geography, Environment, Sustainability (E-Journal)
op_collection_id ftjges
language English
topic arctic coasts;permafrost;tabular massive ground ice;stable isotopes;syngenetic polygonal ice wedges;palaeoclimate
spellingShingle arctic coasts;permafrost;tabular massive ground ice;stable isotopes;syngenetic polygonal ice wedges;palaeoclimate
Irina Streletskaya
Evgeny Gusev
Alexander Vasiliev
Gleb Oblogov
Anatoly Molodkov
PLEISTOCENE-HOLOCENE PALAEOENVIRONMENTAL RECORDS FROM PERMAFROST SEQUENCES AT THE KARA SEA COAST (NW SIBERIA, RUSSIA)
topic_facet arctic coasts;permafrost;tabular massive ground ice;stable isotopes;syngenetic polygonal ice wedges;palaeoclimate
description The Kara Sea coasts were studied using comprehensive stratigraphic and geocryological methods. The paper presents the new analytical studies of ground ice and Quaternary deposits of Western Taymyr and presents the results of spore and pollen, foraminifera, grain-size, mineralogical, geochemical, oxygen isotopic, and other analyses. Several stratigraphic-geocryological transects from Yenisey and Gydan Bays enable us to refine the stratigraphy and palaeogeographical reconstruction of the environments and freezing of Late Pleistocene-Holocene sediments. Marine sedimentation conditions during the late Kargino time (MIS3) changed to continental conditions in MIS2 and MIS1. Marine sediments were frozen syn- and epigenetically with cryotexture and ground ice formation. Ice wedges formation corresponds to the end of the Pleistocene (MIS2) and during cooler periods of the Holocene.
format Article in Journal/Newspaper
author Irina Streletskaya
Evgeny Gusev
Alexander Vasiliev
Gleb Oblogov
Anatoly Molodkov
author_facet Irina Streletskaya
Evgeny Gusev
Alexander Vasiliev
Gleb Oblogov
Anatoly Molodkov
author_sort Irina Streletskaya
title PLEISTOCENE-HOLOCENE PALAEOENVIRONMENTAL RECORDS FROM PERMAFROST SEQUENCES AT THE KARA SEA COAST (NW SIBERIA, RUSSIA)
title_short PLEISTOCENE-HOLOCENE PALAEOENVIRONMENTAL RECORDS FROM PERMAFROST SEQUENCES AT THE KARA SEA COAST (NW SIBERIA, RUSSIA)
title_full PLEISTOCENE-HOLOCENE PALAEOENVIRONMENTAL RECORDS FROM PERMAFROST SEQUENCES AT THE KARA SEA COAST (NW SIBERIA, RUSSIA)
title_fullStr PLEISTOCENE-HOLOCENE PALAEOENVIRONMENTAL RECORDS FROM PERMAFROST SEQUENCES AT THE KARA SEA COAST (NW SIBERIA, RUSSIA)
title_full_unstemmed PLEISTOCENE-HOLOCENE PALAEOENVIRONMENTAL RECORDS FROM PERMAFROST SEQUENCES AT THE KARA SEA COAST (NW SIBERIA, RUSSIA)
title_sort pleistocene-holocene palaeoenvironmental records from permafrost sequences at the kara sea coast (nw siberia, russia)
publisher Russian Geographical Society
publishDate 2013
url https://ges.rgo.ru/jour/article/view/140
https://doi.org/10.24057/2071-9388-2013-6-3-60-76
long_lat ENVELOPE(89.987,89.987,68.219,68.219)
ENVELOPE(82.680,82.680,71.828,71.828)
geographic Arctic
Kara Sea
Taymyr
Yenisey
geographic_facet Arctic
Kara Sea
Taymyr
Yenisey
genre Arctic
Arctic
Foraminifera*
Ice
Kara Sea
permafrost
Polar Geography
Polar Research
Taymyr
wedge*
Siberia
genre_facet Arctic
Arctic
Foraminifera*
Ice
Kara Sea
permafrost
Polar Geography
Polar Research
Taymyr
wedge*
Siberia
op_source GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY; Vol 6, No 3 (2013); 60-76
2542-1565
2071-9388
op_relation https://ges.rgo.ru/jour/article/view/140/140
Atlas of paleogeographic maps (2004) In: M.N. Alekseev (Ed.), Shelf Regions of Eurasia for
the Mesozoic and Cenozoic. Moscow, Nauchnyy Mir, 2, pp. 13–12 (in Russian).
Bolshiyanov, D.Yu. (2006) Passivnoe oledenenie Arktiki i Antarktidy (Passive glaciation of
the Arctic and Antarctic). AARI, St. Petersburg, 295 p. (in Russian)
Craig, H. (1961) Isotopic variations in meteoric waters. Science 133, pp. 1702–1703.
Danilov, I.D. (1969) Merzlotno-facial’noe stroenie vodorazdel’nyh plejstocenovyh otlozhenij
nizhnego techenija reki Eniseja (Cryofacial structure of the Pleistocene sediments of
dividing ridges in the lower course of the Yenisey River). Problemy kriolitologii (Problems
of cryolithology), 1, Moscow University Press, pp. 93–105 (in Russian).
Danilov, I.D. (1978) Pleistotsen morskikh subarkticheskikh ravnin (The Pleistocene of marine
subarctic plains). Moscow University Press, 198 p. (in Russian).
Dansgaard, W. (1964) Stable isotopes in precipitation. Tellus 16, pp. 436–468.
Gusev, E.A., Arslanov, H.A., Maksimov, F.E., Molodkov, A.N., Kuznetsov, V.Yu., Smirnov, S.B.,
Chernov, S.B., Zherebtsov, I.E., Levchenko, S.B. (2011) New geochronological data on the
Neopleistocene-Holocene sediments from the lower Yenisey area // Problemy Arktiki i
Antarktiki, 2(88), pp. 36–44 (in Russian).
Gusev, Е.А., Molodkov, A.N. (2012) Structure of sediments of the final stage of the Kazantsevo
Transgression (MIS5) in the North of Western Siberia // Proccedings, Earth Sciences,
Vol. 443. Part 2. pp. 458–461.
Kaplyanskaya, F.A, Tarnogradsky, V.D. (1986) Remnants of the Pleistocene ice sheets in
the permafrost zone as an object for paleoglaciological research. Polar Geography and
Geology 10, pp. 257–265.
Matyukhin, A.G., Streletskaya, I.D. (2012) The Salinity of Cryogenic Quaternary Deposits in
the Yenisei North. In: V.P. Melnikov (Ed.), Proceeding of the Tenth International Conference
on Permafrost, The Northern Publisher, Salekhard, Russia, 2, pp. 259–262.
Meyer, H., Schönicke, L., Wand, U., Hubberten, H.-W., Friedrichsen, H. (2000) Isotope studies
of hydrogen and oxygen in ground ice – experiences with the equilibration technique.
Isotopes in Environmental and Health Studies 36, pp. 133–149.
Nazarov, D.V. (2011) Quaternary deposits of the central part of the West Siberian Arctic.
Ph.D thesis. Geol. Mineral. Sciences. St. Petersburg State University. 26 p.
Oblogov, G.E., Streletskaya, I.D., Vasiliev, A.A., Gusev, E.A., Arslanov, H.A. (2012) Quaternary
deposits and geocryological conditions of Gydan Bay Coast of the Kara Sea. In: V.P. Melnikov
(Ed.), Proceeding of the Tenth International Conference on Permafrost, 2012, The
Northern Publisher, Salekhard, Russia, 2, pp. 293–296.
Romanenko, F.A., Mikhalev, D.V., Nikolaev, V.I. (2001) Podzemnye l’dy na ostrovah u beregov
Tajmyra (Ground ice on the islands next to the Taymyr coastline). MGI (Materials of
Glaciological Studies. Chronicles, Discussion) 91, pp. 129–137 (in Russian).
Solomatin, V.I. (1982) Pogrebennye relikty lednikovogo l’da na severe Zapadnoj Sibiri
(Buried relicts of glacial ice in the north of West Siberia). MGI (Materials of Glaciological
Studies. Chronicles, Discussion) 29, pp. 233–240 (in Russian).
Stein, R., Niessen, F., Dittmers, K., Levitan, M., Schoster, F., Simstich, J., Steinke, T., Stepanets,
O. (2002) Siberian river run-off and late Quaternary glaciation in the southern Kara Sea,
Arctic ocean: preliminary results. Polar Research 21(2), 315-322. doi:10.1111/j.1751–
2002.tb00086.x
Streletskaya, I.D., Vasilev, A.A. (2009) Izotopnyj sostav poligonal’no-zhil’nyh l’dov zapadnogo
Tajmyra (Isotopic composition of polygonal wedge ice of Western Taymyr). Kriosfera
Zemli (Earth Cryosphere), 13 (3), pp. 59–69 (in Russian).
Streletskaya, I.D., Vasiliev, A.A. (2012) The Ice Complex of Western Taymyr. In: V.P. Melnikov
(Ed.), Proceeding of the Tenth International Conference on Permafrost, The Northern Publisher,
op_rights Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal the right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.Authors can enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgment of its initial publication in this journal.Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access).The information and opinions presented in the Journal reflect the views of the authors and not of the Journal or its Editorial Board or the Publisher. The GES Journal has used its best endeavors to ensure that the information is correct and current at the time of publication but takes no responsibility for any error, omission, or defect therein.
Авторы, публикующие в данном журнале, соглашаются со следующим:Авторы сохраняют за собой авторские права на работу и предоставляют журналу право первой публикации работы на условиях лицензии Creative Commons Attribution License, которая позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Авторы сохраняют право заключать отдельные контрактные договорённости, касающиеся не-эксклюзивного распространения версии работы в опубликованном здесь виде (например, размещение ее в институтском хранилище, публикацию в книге), со ссылкой на ее оригинальную публикацию в этом журнале.Авторы имеют право размещать их работу
op_rightsnorm CC-BY
op_doi https://doi.org/10.24057/2071-9388-2013-6-3-60-76
https://doi.org/10.1111/j.1751
https://doi.org/10.1002/ppp.707
https://doi.org/10.1016/j.quascirev
container_title GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY
container_volume 6
container_issue 3
container_start_page 60
op_container_end_page 76
_version_ 1766302350136311808
spelling ftjges:oai:oai.gesj.elpub.ru:article/140 2023-05-15T14:28:11+02:00 PLEISTOCENE-HOLOCENE PALAEOENVIRONMENTAL RECORDS FROM PERMAFROST SEQUENCES AT THE KARA SEA COAST (NW SIBERIA, RUSSIA) Irina Streletskaya Evgeny Gusev Alexander Vasiliev Gleb Oblogov Anatoly Molodkov 2013-09-01 application/pdf https://ges.rgo.ru/jour/article/view/140 https://doi.org/10.24057/2071-9388-2013-6-3-60-76 eng eng Russian Geographical Society https://ges.rgo.ru/jour/article/view/140/140 Atlas of paleogeographic maps (2004) In: M.N. Alekseev (Ed.), Shelf Regions of Eurasia for the Mesozoic and Cenozoic. Moscow, Nauchnyy Mir, 2, pp. 13–12 (in Russian). Bolshiyanov, D.Yu. (2006) Passivnoe oledenenie Arktiki i Antarktidy (Passive glaciation of the Arctic and Antarctic). AARI, St. Petersburg, 295 p. (in Russian) Craig, H. (1961) Isotopic variations in meteoric waters. Science 133, pp. 1702–1703. Danilov, I.D. (1969) Merzlotno-facial’noe stroenie vodorazdel’nyh plejstocenovyh otlozhenij nizhnego techenija reki Eniseja (Cryofacial structure of the Pleistocene sediments of dividing ridges in the lower course of the Yenisey River). Problemy kriolitologii (Problems of cryolithology), 1, Moscow University Press, pp. 93–105 (in Russian). Danilov, I.D. (1978) Pleistotsen morskikh subarkticheskikh ravnin (The Pleistocene of marine subarctic plains). Moscow University Press, 198 p. (in Russian). Dansgaard, W. (1964) Stable isotopes in precipitation. Tellus 16, pp. 436–468. Gusev, E.A., Arslanov, H.A., Maksimov, F.E., Molodkov, A.N., Kuznetsov, V.Yu., Smirnov, S.B., Chernov, S.B., Zherebtsov, I.E., Levchenko, S.B. (2011) New geochronological data on the Neopleistocene-Holocene sediments from the lower Yenisey area // Problemy Arktiki i Antarktiki, 2(88), pp. 36–44 (in Russian). Gusev, Е.А., Molodkov, A.N. (2012) Structure of sediments of the final stage of the Kazantsevo Transgression (MIS5) in the North of Western Siberia // Proccedings, Earth Sciences, Vol. 443. Part 2. pp. 458–461. Kaplyanskaya, F.A, Tarnogradsky, V.D. (1986) Remnants of the Pleistocene ice sheets in the permafrost zone as an object for paleoglaciological research. Polar Geography and Geology 10, pp. 257–265. Matyukhin, A.G., Streletskaya, I.D. (2012) The Salinity of Cryogenic Quaternary Deposits in the Yenisei North. In: V.P. Melnikov (Ed.), Proceeding of the Tenth International Conference on Permafrost, The Northern Publisher, Salekhard, Russia, 2, pp. 259–262. Meyer, H., Schönicke, L., Wand, U., Hubberten, H.-W., Friedrichsen, H. (2000) Isotope studies of hydrogen and oxygen in ground ice – experiences with the equilibration technique. Isotopes in Environmental and Health Studies 36, pp. 133–149. Nazarov, D.V. (2011) Quaternary deposits of the central part of the West Siberian Arctic. Ph.D thesis. Geol. Mineral. Sciences. St. Petersburg State University. 26 p. Oblogov, G.E., Streletskaya, I.D., Vasiliev, A.A., Gusev, E.A., Arslanov, H.A. (2012) Quaternary deposits and geocryological conditions of Gydan Bay Coast of the Kara Sea. In: V.P. Melnikov (Ed.), Proceeding of the Tenth International Conference on Permafrost, 2012, The Northern Publisher, Salekhard, Russia, 2, pp. 293–296. Romanenko, F.A., Mikhalev, D.V., Nikolaev, V.I. (2001) Podzemnye l’dy na ostrovah u beregov Tajmyra (Ground ice on the islands next to the Taymyr coastline). MGI (Materials of Glaciological Studies. Chronicles, Discussion) 91, pp. 129–137 (in Russian). Solomatin, V.I. (1982) Pogrebennye relikty lednikovogo l’da na severe Zapadnoj Sibiri (Buried relicts of glacial ice in the north of West Siberia). MGI (Materials of Glaciological Studies. Chronicles, Discussion) 29, pp. 233–240 (in Russian). Stein, R., Niessen, F., Dittmers, K., Levitan, M., Schoster, F., Simstich, J., Steinke, T., Stepanets, O. (2002) Siberian river run-off and late Quaternary glaciation in the southern Kara Sea, Arctic ocean: preliminary results. Polar Research 21(2), 315-322. doi:10.1111/j.1751– 2002.tb00086.x Streletskaya, I.D., Vasilev, A.A. (2009) Izotopnyj sostav poligonal’no-zhil’nyh l’dov zapadnogo Tajmyra (Isotopic composition of polygonal wedge ice of Western Taymyr). Kriosfera Zemli (Earth Cryosphere), 13 (3), pp. 59–69 (in Russian). Streletskaya, I.D., Vasiliev, A.A. (2012) The Ice Complex of Western Taymyr. In: V.P. Melnikov (Ed.), Proceeding of the Tenth International Conference on Permafrost, The Northern Publisher, Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal the right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.Authors can enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgment of its initial publication in this journal.Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access).The information and opinions presented in the Journal reflect the views of the authors and not of the Journal or its Editorial Board or the Publisher. The GES Journal has used its best endeavors to ensure that the information is correct and current at the time of publication but takes no responsibility for any error, omission, or defect therein. Авторы, публикующие в данном журнале, соглашаются со следующим:Авторы сохраняют за собой авторские права на работу и предоставляют журналу право первой публикации работы на условиях лицензии Creative Commons Attribution License, которая позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Авторы сохраняют право заключать отдельные контрактные договорённости, касающиеся не-эксклюзивного распространения версии работы в опубликованном здесь виде (например, размещение ее в институтском хранилище, публикацию в книге), со ссылкой на ее оригинальную публикацию в этом журнале.Авторы имеют право размещать их работу CC-BY GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY; Vol 6, No 3 (2013); 60-76 2542-1565 2071-9388 arctic coasts;permafrost;tabular massive ground ice;stable isotopes;syngenetic polygonal ice wedges;palaeoclimate info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2013 ftjges https://doi.org/10.24057/2071-9388-2013-6-3-60-76 https://doi.org/10.1111/j.1751 https://doi.org/10.1002/ppp.707 https://doi.org/10.1016/j.quascirev 2021-05-21T07:34:48Z The Kara Sea coasts were studied using comprehensive stratigraphic and geocryological methods. The paper presents the new analytical studies of ground ice and Quaternary deposits of Western Taymyr and presents the results of spore and pollen, foraminifera, grain-size, mineralogical, geochemical, oxygen isotopic, and other analyses. Several stratigraphic-geocryological transects from Yenisey and Gydan Bays enable us to refine the stratigraphy and palaeogeographical reconstruction of the environments and freezing of Late Pleistocene-Holocene sediments. Marine sedimentation conditions during the late Kargino time (MIS3) changed to continental conditions in MIS2 and MIS1. Marine sediments were frozen syn- and epigenetically with cryotexture and ground ice formation. Ice wedges formation corresponds to the end of the Pleistocene (MIS2) and during cooler periods of the Holocene. Article in Journal/Newspaper Arctic Arctic Foraminifera* Ice Kara Sea permafrost Polar Geography Polar Research Taymyr wedge* Siberia Geography, Environment, Sustainability (E-Journal) Arctic Kara Sea Taymyr ENVELOPE(89.987,89.987,68.219,68.219) Yenisey ENVELOPE(82.680,82.680,71.828,71.828) GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 6 3 60 76