Thick polygonal peatlands in continuous permafrost zone of West Siberia
The study focuses on the structure of thick peatlands with syngenetic ice wedges in the Yamal and Gydan Peninsulas (northern West Siberia). Thick polygonal peatlands formed in floodplains and laidas or in lacustrine-palustrine inliers within hypsometrically higher terraces. Peat accumulated at rates...
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2020
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.919617 https://doi.org/10.1594/PANGAEA.919617 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.919617 2024-09-15T17:52:00+00:00 Thick polygonal peatlands in continuous permafrost zone of West Siberia Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna MEDIAN LATITUDE: 69.663255 * MEDIAN LONGITUDE: 72.308030 * SOUTH-BOUND LATITUDE: 66.950000 * WEST-BOUND LONGITUDE: 66.850000 * NORTH-BOUND LATITUDE: 72.001667 * EAST-BOUND LONGITUDE: 81.710984 2020 application/zip, 3 datasets https://doi.pangaea.de/10.1594/PANGAEA.919617 https://doi.org/10.1594/PANGAEA.919617 en eng PANGAEA Vasil'chuk, Yurij K; Vasil'chuk, Alla Constantinovna (2016): Thick polygonal peatlands in continuous permafrost zone of West Siberia. KRIOSFERA ZEMLI, (4), 3-15, https://doi.org/10.21782/KZ1560-7496-2016-4(3-15) Batuyev, V I; Ganul, A G; Novikov, S M (2015): The Age of "relict" Bogs of the northern Part of West Siberia. Tomsk State Pedagogical University Bulletin, 2(155), 185-191 Vasil'chuk, Alla Constantinovna; Vasil'chuk, Yurij K (2018): Pollen of the Matyuisale Holocene polygonal ice wedge complex, the north of the Gydan Peninsula. Arktika i Antarktika (Arctic and Antarctic), 2, 29-47, https://doi.org/10.7256/2453-8922.2018.2.26725 Vasil'chuk, Yurij K; Jungner, Höegne; Vasil'chuk, Alla Constantinovna (2001): ¹⁴C Dating of Peat and δ¹⁸O-δD in Ground Ice From Northwest Siberia. Radiocarbon, 43(2B), 527-540, https://doi.org/10.1017/S0033822200041187 Vasil'chuk, Yurij K; Petrova, E A; Vasil'chuk, Alla Constantinovna (1983): Some Holocene palaeogeography aspects of Yamal Peninsula. n Commission of the Study of the Quaternary by the USSR Academy of Sciences, Bulletin. Moscow, Nauka: 73-89 Vasil'chuk, Yurij K; Vasil'chuk, Alla Constantinovna; Jungner, H; Geyh, M A; van der Plicht, Johannes; Sonninen, Eloni; Budantseva, Nadine A (2003): Southern limit of syngenetic ice-wedge formation during the Holocene climatic optimum in north-west Siberia. Earth Cryosphere. Special Issue. Russian Academy of Sciences and Scott Polar Research Institute, University of Cambridge, 19-31 https://doi.pangaea.de/10.1594/PANGAEA.919617 https://doi.org/10.1594/PANGAEA.919617 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Holocene Ice wedges northern West Siberia peat accumulation rate peatlands radiocarbon Stable isotope dataset bundled publication 2020 ftpangaea https://doi.org/10.1594/PANGAEA.91961710.21782/KZ1560-7496-2016-4(3-1510.7256/2453-8922.2018.2.2672510.1017/S0033822200041187 2024-07-24T02:31:21Z The study focuses on the structure of thick peatlands with syngenetic ice wedges in the Yamal and Gydan Peninsulas (northern West Siberia). Thick polygonal peatlands formed in floodplains and laidas or in lacustrine-palustrine inliers within hypsometrically higher terraces. Peat accumulated at rates of several mm per year so the peatland reached thicknesses of 4-5 m in 700-1000 years. The presence of Boreal (Holocene) tree macrofossils at the base of many peat sections confirms the tree line advance as far as the contemporary tundra during the Holocene optimum. Other/Unknown Material Arctic Ice permafrost Polar Research Tundra wedge* Siberia PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(66.850000,81.710984,72.001667,66.950000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Holocene Ice wedges northern West Siberia peat accumulation rate peatlands radiocarbon Stable isotope |
spellingShingle |
Holocene Ice wedges northern West Siberia peat accumulation rate peatlands radiocarbon Stable isotope Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna Thick polygonal peatlands in continuous permafrost zone of West Siberia |
topic_facet |
Holocene Ice wedges northern West Siberia peat accumulation rate peatlands radiocarbon Stable isotope |
description |
The study focuses on the structure of thick peatlands with syngenetic ice wedges in the Yamal and Gydan Peninsulas (northern West Siberia). Thick polygonal peatlands formed in floodplains and laidas or in lacustrine-palustrine inliers within hypsometrically higher terraces. Peat accumulated at rates of several mm per year so the peatland reached thicknesses of 4-5 m in 700-1000 years. The presence of Boreal (Holocene) tree macrofossils at the base of many peat sections confirms the tree line advance as far as the contemporary tundra during the Holocene optimum. |
format |
Other/Unknown Material |
author |
Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna |
author_facet |
Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna |
author_sort |
Vasil'chuk, Yurij K |
title |
Thick polygonal peatlands in continuous permafrost zone of West Siberia |
title_short |
Thick polygonal peatlands in continuous permafrost zone of West Siberia |
title_full |
Thick polygonal peatlands in continuous permafrost zone of West Siberia |
title_fullStr |
Thick polygonal peatlands in continuous permafrost zone of West Siberia |
title_full_unstemmed |
Thick polygonal peatlands in continuous permafrost zone of West Siberia |
title_sort |
thick polygonal peatlands in continuous permafrost zone of west siberia |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.919617 https://doi.org/10.1594/PANGAEA.919617 |
op_coverage |
MEDIAN LATITUDE: 69.663255 * MEDIAN LONGITUDE: 72.308030 * SOUTH-BOUND LATITUDE: 66.950000 * WEST-BOUND LONGITUDE: 66.850000 * NORTH-BOUND LATITUDE: 72.001667 * EAST-BOUND LONGITUDE: 81.710984 |
long_lat |
ENVELOPE(66.850000,81.710984,72.001667,66.950000) |
genre |
Arctic Ice permafrost Polar Research Tundra wedge* Siberia |
genre_facet |
Arctic Ice permafrost Polar Research Tundra wedge* Siberia |
op_relation |
Vasil'chuk, Yurij K; Vasil'chuk, Alla Constantinovna (2016): Thick polygonal peatlands in continuous permafrost zone of West Siberia. KRIOSFERA ZEMLI, (4), 3-15, https://doi.org/10.21782/KZ1560-7496-2016-4(3-15) Batuyev, V I; Ganul, A G; Novikov, S M (2015): The Age of "relict" Bogs of the northern Part of West Siberia. Tomsk State Pedagogical University Bulletin, 2(155), 185-191 Vasil'chuk, Alla Constantinovna; Vasil'chuk, Yurij K (2018): Pollen of the Matyuisale Holocene polygonal ice wedge complex, the north of the Gydan Peninsula. Arktika i Antarktika (Arctic and Antarctic), 2, 29-47, https://doi.org/10.7256/2453-8922.2018.2.26725 Vasil'chuk, Yurij K; Jungner, Höegne; Vasil'chuk, Alla Constantinovna (2001): ¹⁴C Dating of Peat and δ¹⁸O-δD in Ground Ice From Northwest Siberia. Radiocarbon, 43(2B), 527-540, https://doi.org/10.1017/S0033822200041187 Vasil'chuk, Yurij K; Petrova, E A; Vasil'chuk, Alla Constantinovna (1983): Some Holocene palaeogeography aspects of Yamal Peninsula. n Commission of the Study of the Quaternary by the USSR Academy of Sciences, Bulletin. Moscow, Nauka: 73-89 Vasil'chuk, Yurij K; Vasil'chuk, Alla Constantinovna; Jungner, H; Geyh, M A; van der Plicht, Johannes; Sonninen, Eloni; Budantseva, Nadine A (2003): Southern limit of syngenetic ice-wedge formation during the Holocene climatic optimum in north-west Siberia. Earth Cryosphere. Special Issue. Russian Academy of Sciences and Scott Polar Research Institute, University of Cambridge, 19-31 https://doi.pangaea.de/10.1594/PANGAEA.919617 https://doi.org/10.1594/PANGAEA.919617 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.91961710.21782/KZ1560-7496-2016-4(3-1510.7256/2453-8922.2018.2.2672510.1017/S0033822200041187 |
_version_ |
1810294080572227584 |