Sea level fluctuations and their signature in the composition and structure of polygonal wedge ice in the Yenisei River lower reaches
Late Pleistocene and Holocene polygonal-wedge ice is studied in the lower course of the Yenisei River. Ice distribution, features of the formation, chemical and microbiological composition were determined. It was established that ice wedges were formed on the slopes of the depression, in coastal-mar...
| Published in: | Ice and Snow |
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| Main Authors: | , , , , , , , , , , , , , |
| Format: | Article in Journal/Newspaper |
| Language: | Russian |
| Published: |
IGRAS
2015
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| Subjects: | |
| Online Access: | https://ice-snow.igras.ru/jour/article/view/43 https://doi.org/10.15356/2076-6734-2014-2-82-90 |
| _version_ | 1828683031712366592 |
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| author | O. Opokina L. E. Slagoda A. I. Tomberg B. M. Suslova Yu. A. Firsova D. T. Khodzher V. N. Zhuchenko A. О. Опокина Л. Е. Слагода А. И. Томберг В. М. Суслова Ю. А. Фирсова Д. Т. Ходжер В. Н. Жученко А. |
| author_facet | O. Opokina L. E. Slagoda A. I. Tomberg B. M. Suslova Yu. A. Firsova D. T. Khodzher V. N. Zhuchenko A. О. Опокина Л. Е. Слагода А. И. Томберг В. М. Суслова Ю. А. Фирсова Д. Т. Ходжер В. Н. Жученко А. |
| author_sort | O. Opokina L. |
| collection | Ice and Snow |
| container_issue | 2 |
| container_start_page | 82 |
| container_title | Ice and Snow |
| container_volume | 126 |
| description | Late Pleistocene and Holocene polygonal-wedge ice is studied in the lower course of the Yenisei River. Ice distribution, features of the formation, chemical and microbiological composition were determined. It was established that ice wedges were formed on the slopes of the depression, in coastal-marine lagoons and in thermokarst during Holocene. The evidence of thermoabrasion and thermokarst in sediments as well as the marine signal in composition of polygonal-wedge ice allowed clarifying the southern limit of the Holocene transgression. В низовьях р. Енисей изучены сартанские и голоценовые полигонально-жильные льды и вмещающие отложения. Проведён анализ их химического и микробиологического состава. Установлено, что голоценовые полигонально-жильные льды формировались в разных условиях: на склонах депрессий; в мелководных прибрежно-морских лагунах; на первой морской террасе; в термокарстовых понижениях. Показано, что осадконакопление и рост полигонально-жильных льдов в низовьях р. Енисей коррелирует с уровнем моря в голоцене. |
| format | Article in Journal/Newspaper |
| genre | Arctic Kara Sea Thermokarst термокарст* |
| genre_facet | Arctic Kara Sea Thermokarst термокарст* |
| geographic | Kara Sea Yenisei River |
| geographic_facet | Kara Sea Yenisei River |
| id | ftjias:oai:oai.ice.elpub.ru:article/43 |
| institution | Open Polar |
| language | Russian |
| long_lat | ENVELOPE(84.738,84.738,69.718,69.718) |
| op_collection_id | ftjias |
| op_doi | https://doi.org/10.15356/2076-6734-2014-2-82-9010.15356/2076-6734-2014-2 |
| op_relation | Antipina Z.N., Are F.E., Voichenko V.V., Molochushkin E.N. Cryolithozone of the Asian Arctic shelf. Pozdnechetvertichnaya istoriya i sedimentogenez okrainnykh i bnutrennikh morey. Late Pleistocene history and sedimentogenesis of the adjacent and enclosed seas). Moscow: Nauka, 1979; 183–189. [In Russian]. Astakhov V.I. On chronostratigraphic subdivisions of the Upper Pleistocene of Siberia Geologiya i geofizika. Geology and Geophysics. 2006, 47 (11): 1207–1220. [In Russian]. Vasil’chuk A.K. Reflection of Heinrich’ events on the pollen diagrams of massive wedge ice dated by radiocarbon and included the edoma deposits in the lower course of Kolyma River. Kriosfera Zemli. Earth Cryosphere. 2003, 7 (4): 3–138. [In Russian]. Vasil’chuk A.K. Povtorno-zhil’nye l’dy: geterotsiklichnost’, geterokhronnostt’, geterogennost’. Massive wedge ice. Moscow: Moscow State University, 2006: 404 p. [In Russian]. Vtyurin B.I. Podzemnye l’dy SSSR. Ground ice in the USSR. Moscow: Nauka, 1975: 215 p. [In Russian]. Grosswald M.G. Evraziyskie gidrosfernye katastrofy i oledenenie Arktiki. Eurasian hydrosphere catastrophes and glaciation in Arctic. Moscow: Scientific World, 1999: 120 p. [In Russian]. Gusev E.A., Arslanov H.A., Maksimov F.E., Molod’kov A.N., Kuznetsov V.Yu., Smirnov S.B., Chernov S.B., Zherebtsov I.E., Levchenko S.B. New geochronological data on neoPleistocene-Holocene deposits in the lower course of Yenissei River. Problemy Arktiki i Antarktiki. Problems of Arctic and Antarctic. 2011, 2: 36–44. [In Russian]. Gusev E.A., Molod’kov A.N. Structure of deposits in the final stage of Kazantsev transgression (MIS 5) at the North of West Siberia. Doklady Akademii Nauk. Proc. of the Academy of Sciences. 2012, 443 (6): 707–710. [In Russian]. Danilov I.D. Evolution of Arctic shelf in Late Cainozoik and cryogenic-glaciogenic processes within its limits. Kriosfera Zemli. Earth Cryosphere. 1997, 1 (2): 36–41. [In Russian]. Ivanov A.V. Kriogennaya metamorfizhatsiya khimicheskogo sostava prirodnykh l’dov, zamerzayushchikh i talykh vod. Cryogenic metamorphism of the chemical composition of nature ice, freezing and melting water. Khabarovsk: Dalnauka, 1998: 164 p. [In Russian]. Kalyakin V.N., Romanenko F.A., Molochaev A.V., Rogacheva E.V., Syroechkovskiy E.E. Gydan nature reserve. Zapovedniki Rossii: Zapovedniki Sibiri. Natural reserves of Russia: Natural reserves of Siberia. V. 2. Moscow: Logata, 2000: 47–55. [In Russian]. Kaplin P.A., Selivanov A.O. Izmeneniya urovney morey Rossii i razvitie beregov: proshloe, nastoyashchee, budushchee. Changes of sea level in Russia and evolution of beaches: past, present and future. Moscow: GEOS, 1999: 299 p. [In Russian]. Karpov E.G. On the origin of massive ground ice in the lower course of Yenissei River [In Russian]. Geologiya i geofizika. Geology and Geophysics. 1984, 1: 118–122. Levitan M.A., Lavrushin Yu.A., Stein R. Ocherki istorii sedimentatsii v Severnom Ledovitom okeane i moryakh Suaerktiki v techenie poslednikh 130 tysyach let. On the history of sedimentation in the Arctic Ocean and Subarctic seas during the last 130 thousand years. Moscow: GEOS, 2007: 404 p. [In Russian]. Nikolaev V.I., Mikhalev D.V., Romanenko F.A., Brilli M. Reconstruction of the permafrost formation conditions in the North-East of Russia based on the results of isotope studies of reference sections in Kolyma lowland. Led i Sneg. Ice and Snow. 2010; 4 (112): 79–90. [In Russian]. Svitoch A.A. Morskoy pleystotsen pobereziy Rossii. Marine Pleistocene of beaches in Russia. Moscow: GEOS, 2003: 362 p. [In Russian]. Streletskaya I.D., Vasiliev A.A. Isotope composition of polygonal ground ice in the West Taimyr Kriosfera Zemli. Earth Cryosphere. 2009, 13 (3): 59–69. [In Russian]. Streletskaya I.D., Vasiliev A.A., Slagoda E.A., Opokina O.L., Oblogov G.E. Polygonal ground ice at the Sibiryakov Island, Kara Sea. Vestnik MGU. Ser. 5. Geografiya. Herald of the Moscow State University. Ser. 5. Geography. 2012, 3: 57–63. [In Russian]. Suslova M.Yu., Parfenova V.V., Pavlova O.N., Kostornova T.Ya., Fedotov A.P. Diversity and distribution of the cultivate microbe association in the regions of Lover Yenisei and shelf of Kara Sea). Kriosfera Zemli. Earth Cryosphere. 2011, 15 (4): 106–109. [In Russian]. Wetterich S., Rudaya N., Tumskoy V., Andreev A., Opel T., Schirrmeister L., Meyer H. Last Glacial Maximum records in permafrost of the East Siberian Arctic. Quaternary Science Reviews. 2011, 30: 3139–3151. |
| op_rights | Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal 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 are able to 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 acknowledgement 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). Авторы, публикующие статьи в данном журнале, соглашаются на следующее:Авторы сохраняют за собой авторские права и предоставляют журналу право первой публикации работы, которая по истечении 6 месяцев после публикации автоматически лицензируется на условиях Creative Commons Attribution License , что позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Редакция журнала будет размещать принятую для публикации статью на сайте журнала до выхода её в свет (после утверждения к печати редколлегией журнала). Авторы также имеют право размещать их работу в сети Интернет (например в институтском хранилище или персональном сайте) до и во время процесса рассмотрения ее данным журналом, так как это может привести к продуктивному обсуждению и большему количеству ссылок на данную работу (См. The Effect of Open Access). |
| op_source | Ice and Snow; Том 54, № 2 (2014); 82-90 Лёд и Снег; Том 54, № 2 (2014); 82-90 2412-3765 2076-6734 10.15356/2076-6734-2014-2 |
| publishDate | 2015 |
| publisher | IGRAS |
| record_format | openpolar |
| spelling | ftjias:oai:oai.ice.elpub.ru:article/43 2025-04-06T14:41:32+00:00 Sea level fluctuations and their signature in the composition and structure of polygonal wedge ice in the Yenisei River lower reaches колебания уровня моря и их отражение в составе и строении полигонально-жильных льдов в низовьях Енисея O. Opokina L. E. Slagoda A. I. Tomberg B. M. Suslova Yu. A. Firsova D. T. Khodzher V. N. Zhuchenko A. О. Опокина Л. Е. Слагода А. И. Томберг В. М. Суслова Ю. А. Фирсова Д. Т. Ходжер В. Н. Жученко А. 2015-03-26 https://ice-snow.igras.ru/jour/article/view/43 https://doi.org/10.15356/2076-6734-2014-2-82-90 ru rus IGRAS Antipina Z.N., Are F.E., Voichenko V.V., Molochushkin E.N. Cryolithozone of the Asian Arctic shelf. Pozdnechetvertichnaya istoriya i sedimentogenez okrainnykh i bnutrennikh morey. Late Pleistocene history and sedimentogenesis of the adjacent and enclosed seas). Moscow: Nauka, 1979; 183–189. [In Russian]. Astakhov V.I. On chronostratigraphic subdivisions of the Upper Pleistocene of Siberia Geologiya i geofizika. Geology and Geophysics. 2006, 47 (11): 1207–1220. [In Russian]. Vasil’chuk A.K. Reflection of Heinrich’ events on the pollen diagrams of massive wedge ice dated by radiocarbon and included the edoma deposits in the lower course of Kolyma River. Kriosfera Zemli. Earth Cryosphere. 2003, 7 (4): 3–138. [In Russian]. Vasil’chuk A.K. Povtorno-zhil’nye l’dy: geterotsiklichnost’, geterokhronnostt’, geterogennost’. Massive wedge ice. Moscow: Moscow State University, 2006: 404 p. [In Russian]. Vtyurin B.I. Podzemnye l’dy SSSR. Ground ice in the USSR. Moscow: Nauka, 1975: 215 p. [In Russian]. Grosswald M.G. Evraziyskie gidrosfernye katastrofy i oledenenie Arktiki. Eurasian hydrosphere catastrophes and glaciation in Arctic. Moscow: Scientific World, 1999: 120 p. [In Russian]. Gusev E.A., Arslanov H.A., Maksimov F.E., Molod’kov A.N., Kuznetsov V.Yu., Smirnov S.B., Chernov S.B., Zherebtsov I.E., Levchenko S.B. New geochronological data on neoPleistocene-Holocene deposits in the lower course of Yenissei River. Problemy Arktiki i Antarktiki. Problems of Arctic and Antarctic. 2011, 2: 36–44. [In Russian]. Gusev E.A., Molod’kov A.N. Structure of deposits in the final stage of Kazantsev transgression (MIS 5) at the North of West Siberia. Doklady Akademii Nauk. Proc. of the Academy of Sciences. 2012, 443 (6): 707–710. [In Russian]. Danilov I.D. Evolution of Arctic shelf in Late Cainozoik and cryogenic-glaciogenic processes within its limits. Kriosfera Zemli. Earth Cryosphere. 1997, 1 (2): 36–41. [In Russian]. Ivanov A.V. Kriogennaya metamorfizhatsiya khimicheskogo sostava prirodnykh l’dov, zamerzayushchikh i talykh vod. Cryogenic metamorphism of the chemical composition of nature ice, freezing and melting water. Khabarovsk: Dalnauka, 1998: 164 p. [In Russian]. Kalyakin V.N., Romanenko F.A., Molochaev A.V., Rogacheva E.V., Syroechkovskiy E.E. Gydan nature reserve. Zapovedniki Rossii: Zapovedniki Sibiri. Natural reserves of Russia: Natural reserves of Siberia. V. 2. Moscow: Logata, 2000: 47–55. [In Russian]. Kaplin P.A., Selivanov A.O. Izmeneniya urovney morey Rossii i razvitie beregov: proshloe, nastoyashchee, budushchee. Changes of sea level in Russia and evolution of beaches: past, present and future. Moscow: GEOS, 1999: 299 p. [In Russian]. Karpov E.G. On the origin of massive ground ice in the lower course of Yenissei River [In Russian]. Geologiya i geofizika. Geology and Geophysics. 1984, 1: 118–122. Levitan M.A., Lavrushin Yu.A., Stein R. Ocherki istorii sedimentatsii v Severnom Ledovitom okeane i moryakh Suaerktiki v techenie poslednikh 130 tysyach let. On the history of sedimentation in the Arctic Ocean and Subarctic seas during the last 130 thousand years. Moscow: GEOS, 2007: 404 p. [In Russian]. Nikolaev V.I., Mikhalev D.V., Romanenko F.A., Brilli M. Reconstruction of the permafrost formation conditions in the North-East of Russia based on the results of isotope studies of reference sections in Kolyma lowland. Led i Sneg. Ice and Snow. 2010; 4 (112): 79–90. [In Russian]. Svitoch A.A. Morskoy pleystotsen pobereziy Rossii. Marine Pleistocene of beaches in Russia. Moscow: GEOS, 2003: 362 p. [In Russian]. Streletskaya I.D., Vasiliev A.A. Isotope composition of polygonal ground ice in the West Taimyr Kriosfera Zemli. Earth Cryosphere. 2009, 13 (3): 59–69. [In Russian]. Streletskaya I.D., Vasiliev A.A., Slagoda E.A., Opokina O.L., Oblogov G.E. Polygonal ground ice at the Sibiryakov Island, Kara Sea. Vestnik MGU. Ser. 5. Geografiya. Herald of the Moscow State University. Ser. 5. Geography. 2012, 3: 57–63. [In Russian]. Suslova M.Yu., Parfenova V.V., Pavlova O.N., Kostornova T.Ya., Fedotov A.P. Diversity and distribution of the cultivate microbe association in the regions of Lover Yenisei and shelf of Kara Sea). Kriosfera Zemli. Earth Cryosphere. 2011, 15 (4): 106–109. [In Russian]. Wetterich S., Rudaya N., Tumskoy V., Andreev A., Opel T., Schirrmeister L., Meyer H. Last Glacial Maximum records in permafrost of the East Siberian Arctic. Quaternary Science Reviews. 2011, 30: 3139–3151. Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal 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 are able to 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 acknowledgement 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). Авторы, публикующие статьи в данном журнале, соглашаются на следующее:Авторы сохраняют за собой авторские права и предоставляют журналу право первой публикации работы, которая по истечении 6 месяцев после публикации автоматически лицензируется на условиях Creative Commons Attribution License , что позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Редакция журнала будет размещать принятую для публикации статью на сайте журнала до выхода её в свет (после утверждения к печати редколлегией журнала). Авторы также имеют право размещать их работу в сети Интернет (например в институтском хранилище или персональном сайте) до и во время процесса рассмотрения ее данным журналом, так как это может привести к продуктивному обсуждению и большему количеству ссылок на данную работу (См. The Effect of Open Access). Ice and Snow; Том 54, № 2 (2014); 82-90 Лёд и Снег; Том 54, № 2 (2014); 82-90 2412-3765 2076-6734 10.15356/2076-6734-2014-2 Chemistry and microbiology of ice;Holocene;Kara Sea;polygon-wedge ice;regression;transgression Голоцен;Карское море;полигонально-жильный лёд;регрессия;трансгрессия;химия и микробиология льда info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftjias https://doi.org/10.15356/2076-6734-2014-2-82-9010.15356/2076-6734-2014-2 2025-03-10T11:00:05Z Late Pleistocene and Holocene polygonal-wedge ice is studied in the lower course of the Yenisei River. Ice distribution, features of the formation, chemical and microbiological composition were determined. It was established that ice wedges were formed on the slopes of the depression, in coastal-marine lagoons and in thermokarst during Holocene. The evidence of thermoabrasion and thermokarst in sediments as well as the marine signal in composition of polygonal-wedge ice allowed clarifying the southern limit of the Holocene transgression. В низовьях р. Енисей изучены сартанские и голоценовые полигонально-жильные льды и вмещающие отложения. Проведён анализ их химического и микробиологического состава. Установлено, что голоценовые полигонально-жильные льды формировались в разных условиях: на склонах депрессий; в мелководных прибрежно-морских лагунах; на первой морской террасе; в термокарстовых понижениях. Показано, что осадконакопление и рост полигонально-жильных льдов в низовьях р. Енисей коррелирует с уровнем моря в голоцене. Article in Journal/Newspaper Arctic Kara Sea Thermokarst термокарст* Ice and Snow Kara Sea Yenisei River ENVELOPE(84.738,84.738,69.718,69.718) Ice and Snow 126 2 82 |
| spellingShingle | Chemistry and microbiology of ice;Holocene;Kara Sea;polygon-wedge ice;regression;transgression Голоцен;Карское море;полигонально-жильный лёд;регрессия;трансгрессия;химия и микробиология льда O. Opokina L. E. Slagoda A. I. Tomberg B. M. Suslova Yu. A. Firsova D. T. Khodzher V. N. Zhuchenko A. О. Опокина Л. Е. Слагода А. И. Томберг В. М. Суслова Ю. А. Фирсова Д. Т. Ходжер В. Н. Жученко А. Sea level fluctuations and their signature in the composition and structure of polygonal wedge ice in the Yenisei River lower reaches |
| title | Sea level fluctuations and their signature in the composition and structure of polygonal wedge ice in the Yenisei River lower reaches |
| title_full | Sea level fluctuations and their signature in the composition and structure of polygonal wedge ice in the Yenisei River lower reaches |
| title_fullStr | Sea level fluctuations and their signature in the composition and structure of polygonal wedge ice in the Yenisei River lower reaches |
| title_full_unstemmed | Sea level fluctuations and their signature in the composition and structure of polygonal wedge ice in the Yenisei River lower reaches |
| title_short | Sea level fluctuations and their signature in the composition and structure of polygonal wedge ice in the Yenisei River lower reaches |
| title_sort | sea level fluctuations and their signature in the composition and structure of polygonal wedge ice in the yenisei river lower reaches |
| topic | Chemistry and microbiology of ice;Holocene;Kara Sea;polygon-wedge ice;regression;transgression Голоцен;Карское море;полигонально-жильный лёд;регрессия;трансгрессия;химия и микробиология льда |
| topic_facet | Chemistry and microbiology of ice;Holocene;Kara Sea;polygon-wedge ice;regression;transgression Голоцен;Карское море;полигонально-жильный лёд;регрессия;трансгрессия;химия и микробиология льда |
| url | https://ice-snow.igras.ru/jour/article/view/43 https://doi.org/10.15356/2076-6734-2014-2-82-90 |