Pedogenesis in the Tundra Zone of Coastal Lowlands of Northeastern Siberia

Coastal lowlands of northeastern Siberia are composed of the Pleistocene ice-rich organic-containing loamy sediments of the Ice Complex (yedoma) and products of their transformation in the Holocene. In the tundra zone, three major trends of modern pedogenesis depending on the geomorphic position and...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Eurasian soil science 2020-10, Vol.53 (10), p.1365-1373
Hauptverfasser: Gubin, S. V., Lupachev, A. V.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 1373
container_issue 10
container_start_page 1365
container_title Eurasian soil science
container_volume 53
creator Gubin, S. V.
Lupachev, A. V.
description Coastal lowlands of northeastern Siberia are composed of the Pleistocene ice-rich organic-containing loamy sediments of the Ice Complex (yedoma) and products of their transformation in the Holocene. In the tundra zone, three major trends of modern pedogenesis depending on the geomorphic position and age of particular landforms have been identified. On the interfluves affected by thermokarst processes in the Holocene, somewhat elevated remains of the Late Pleistocene Ice Complex alternate with vast thermokarst depressions (alases) with lakes. Cryozems are developed in automorphic plain positions and on the upper parts of slopes. The profiles of these soils are strongly affected by cycles of frost boiling and cryoturbation; under their influence, specific suprapermafrost accumulative organomineral horizons are formed. Gleyzation predominates in the soils of the low- and middle-level Holocene terraces of alases. Peat accumulation is progressively developed in the bottoms of alas depressions.
doi_str_mv 10.1134/S1064229320100087
format Article
fullrecord <record><control><sourceid>gale_proqu</sourceid><recordid>TN_cdi_proquest_journals_2473804287</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A718451498</galeid><sourcerecordid>A718451498</sourcerecordid><originalsourceid>FETCH-LOGICAL-a378t-6a5f13e6cc0aafb4f7ededf11862cdc88239309ea94e36a2d5bb14924048fcdb3</originalsourceid><addsrcrecordid>eNp1kEtLAzEUhYMoWKs_wF3A9WheM5NZluKTokIriJshk9zUlDapyRTx35sygguRLBLOPd-5Nxehc0ouKeXiak5JJRhrOCOUECLrAzSiZVkVtClfD_M7l4t9_RidpLQihEsp5Ag9PIMJS_CQXMLO4_4d8GLnTVT4LXjAweJpUKlXazwLn2vlTdprjyFmZ9Yhejx3HUSnTtGRVesEZz_3GL3cXC-md8Xs6fZ-OpkViteyLypVWsqh0pooZTthazBgLKWyYtpoKRlvOGlANQJ4pZgpu46KhgkipNWm42N0MeRuY_jYQerbVdhFn1u2TNRcEsFknV2Xg2up1tA6b0Mflc7HwMbp_DXrsj6pqRRljpcZoAOgY0gpgm230W1U_Gopafc7bv_sODNsYFL2-iXE31H-h74BK419Kw</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2473804287</pqid></control><display><type>article</type><title>Pedogenesis in the Tundra Zone of Coastal Lowlands of Northeastern Siberia</title><source>Springer Nature - Complete Springer Journals</source><creator>Gubin, S. V. ; Lupachev, A. V.</creator><creatorcontrib>Gubin, S. V. ; Lupachev, A. V.</creatorcontrib><description>Coastal lowlands of northeastern Siberia are composed of the Pleistocene ice-rich organic-containing loamy sediments of the Ice Complex (yedoma) and products of their transformation in the Holocene. In the tundra zone, three major trends of modern pedogenesis depending on the geomorphic position and age of particular landforms have been identified. On the interfluves affected by thermokarst processes in the Holocene, somewhat elevated remains of the Late Pleistocene Ice Complex alternate with vast thermokarst depressions (alases) with lakes. Cryozems are developed in automorphic plain positions and on the upper parts of slopes. The profiles of these soils are strongly affected by cycles of frost boiling and cryoturbation; under their influence, specific suprapermafrost accumulative organomineral horizons are formed. Gleyzation predominates in the soils of the low- and middle-level Holocene terraces of alases. Peat accumulation is progressively developed in the bottoms of alas depressions.</description><identifier>ISSN: 1064-2293</identifier><identifier>EISSN: 1556-195X</identifier><identifier>DOI: 10.1134/S1064229320100087</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Earth and Environmental Science ; Earth Sciences ; Genesis and Geography of Soils ; Geomorphology ; Geotechnical Engineering &amp; Applied Earth Sciences ; Holocene ; Lakes ; Landforms ; Lowlands ; Peat ; Pleistocene ; Sediments ; Sediments (Geology) ; Soil ; Soil formation ; Soils ; Terraces ; Tundra</subject><ispartof>Eurasian soil science, 2020-10, Vol.53 (10), p.1365-1373</ispartof><rights>Pleiades Publishing, Ltd. 2020</rights><rights>COPYRIGHT 2020 Springer</rights><rights>Pleiades Publishing, Ltd. 2020.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a378t-6a5f13e6cc0aafb4f7ededf11862cdc88239309ea94e36a2d5bb14924048fcdb3</citedby><cites>FETCH-LOGICAL-a378t-6a5f13e6cc0aafb4f7ededf11862cdc88239309ea94e36a2d5bb14924048fcdb3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1064229320100087$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1064229320100087$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51297</link.rule.ids></links><search><creatorcontrib>Gubin, S. V.</creatorcontrib><creatorcontrib>Lupachev, A. V.</creatorcontrib><title>Pedogenesis in the Tundra Zone of Coastal Lowlands of Northeastern Siberia</title><title>Eurasian soil science</title><addtitle>Eurasian Soil Sc</addtitle><description>Coastal lowlands of northeastern Siberia are composed of the Pleistocene ice-rich organic-containing loamy sediments of the Ice Complex (yedoma) and products of their transformation in the Holocene. In the tundra zone, three major trends of modern pedogenesis depending on the geomorphic position and age of particular landforms have been identified. On the interfluves affected by thermokarst processes in the Holocene, somewhat elevated remains of the Late Pleistocene Ice Complex alternate with vast thermokarst depressions (alases) with lakes. Cryozems are developed in automorphic plain positions and on the upper parts of slopes. The profiles of these soils are strongly affected by cycles of frost boiling and cryoturbation; under their influence, specific suprapermafrost accumulative organomineral horizons are formed. Gleyzation predominates in the soils of the low- and middle-level Holocene terraces of alases. Peat accumulation is progressively developed in the bottoms of alas depressions.</description><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Genesis and Geography of Soils</subject><subject>Geomorphology</subject><subject>Geotechnical Engineering &amp; Applied Earth Sciences</subject><subject>Holocene</subject><subject>Lakes</subject><subject>Landforms</subject><subject>Lowlands</subject><subject>Peat</subject><subject>Pleistocene</subject><subject>Sediments</subject><subject>Sediments (Geology)</subject><subject>Soil</subject><subject>Soil formation</subject><subject>Soils</subject><subject>Terraces</subject><subject>Tundra</subject><issn>1064-2293</issn><issn>1556-195X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp1kEtLAzEUhYMoWKs_wF3A9WheM5NZluKTokIriJshk9zUlDapyRTx35sygguRLBLOPd-5Nxehc0ouKeXiak5JJRhrOCOUECLrAzSiZVkVtClfD_M7l4t9_RidpLQihEsp5Ag9PIMJS_CQXMLO4_4d8GLnTVT4LXjAweJpUKlXazwLn2vlTdprjyFmZ9Yhejx3HUSnTtGRVesEZz_3GL3cXC-md8Xs6fZ-OpkViteyLypVWsqh0pooZTthazBgLKWyYtpoKRlvOGlANQJ4pZgpu46KhgkipNWm42N0MeRuY_jYQerbVdhFn1u2TNRcEsFknV2Xg2up1tA6b0Mflc7HwMbp_DXrsj6pqRRljpcZoAOgY0gpgm230W1U_Gopafc7bv_sODNsYFL2-iXE31H-h74BK419Kw</recordid><startdate>20201001</startdate><enddate>20201001</enddate><creator>Gubin, S. V.</creator><creator>Lupachev, A. V.</creator><general>Pleiades Publishing</general><general>Springer</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QL</scope><scope>7ST</scope><scope>7T7</scope><scope>7U9</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H94</scope><scope>H96</scope><scope>L.G</scope><scope>M7N</scope><scope>P64</scope><scope>SOI</scope></search><sort><creationdate>20201001</creationdate><title>Pedogenesis in the Tundra Zone of Coastal Lowlands of Northeastern Siberia</title><author>Gubin, S. V. ; Lupachev, A. V.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a378t-6a5f13e6cc0aafb4f7ededf11862cdc88239309ea94e36a2d5bb14924048fcdb3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Genesis and Geography of Soils</topic><topic>Geomorphology</topic><topic>Geotechnical Engineering &amp; Applied Earth Sciences</topic><topic>Holocene</topic><topic>Lakes</topic><topic>Landforms</topic><topic>Lowlands</topic><topic>Peat</topic><topic>Pleistocene</topic><topic>Sediments</topic><topic>Sediments (Geology)</topic><topic>Soil</topic><topic>Soil formation</topic><topic>Soils</topic><topic>Terraces</topic><topic>Tundra</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Gubin, S. V.</creatorcontrib><creatorcontrib>Lupachev, A. V.</creatorcontrib><collection>CrossRef</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Virology and AIDS Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>AIDS and Cancer Research Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Environment Abstracts</collection><jtitle>Eurasian soil science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Gubin, S. V.</au><au>Lupachev, A. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Pedogenesis in the Tundra Zone of Coastal Lowlands of Northeastern Siberia</atitle><jtitle>Eurasian soil science</jtitle><stitle>Eurasian Soil Sc</stitle><date>2020-10-01</date><risdate>2020</risdate><volume>53</volume><issue>10</issue><spage>1365</spage><epage>1373</epage><pages>1365-1373</pages><issn>1064-2293</issn><eissn>1556-195X</eissn><abstract>Coastal lowlands of northeastern Siberia are composed of the Pleistocene ice-rich organic-containing loamy sediments of the Ice Complex (yedoma) and products of their transformation in the Holocene. In the tundra zone, three major trends of modern pedogenesis depending on the geomorphic position and age of particular landforms have been identified. On the interfluves affected by thermokarst processes in the Holocene, somewhat elevated remains of the Late Pleistocene Ice Complex alternate with vast thermokarst depressions (alases) with lakes. Cryozems are developed in automorphic plain positions and on the upper parts of slopes. The profiles of these soils are strongly affected by cycles of frost boiling and cryoturbation; under their influence, specific suprapermafrost accumulative organomineral horizons are formed. Gleyzation predominates in the soils of the low- and middle-level Holocene terraces of alases. Peat accumulation is progressively developed in the bottoms of alas depressions.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1064229320100087</doi><tpages>9</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1064-2293
ispartof Eurasian soil science, 2020-10, Vol.53 (10), p.1365-1373
issn 1064-2293
1556-195X
language eng
recordid cdi_proquest_journals_2473804287
source Springer Nature - Complete Springer Journals
subjects Earth and Environmental Science
Earth Sciences
Genesis and Geography of Soils
Geomorphology
Geotechnical Engineering & Applied Earth Sciences
Holocene
Lakes
Landforms
Lowlands
Peat
Pleistocene
Sediments
Sediments (Geology)
Soil
Soil formation
Soils
Terraces
Tundra
title Pedogenesis in the Tundra Zone of Coastal Lowlands of Northeastern Siberia
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-23T16%3A33%3A30IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Pedogenesis%20in%20the%20Tundra%20Zone%20of%20Coastal%20Lowlands%20of%20Northeastern%20Siberia&rft.jtitle=Eurasian%20soil%20science&rft.au=Gubin,%20S.%20V.&rft.date=2020-10-01&rft.volume=53&rft.issue=10&rft.spage=1365&rft.epage=1373&rft.pages=1365-1373&rft.issn=1064-2293&rft.eissn=1556-195X&rft_id=info:doi/10.1134/S1064229320100087&rft_dat=%3Cgale_proqu%3EA718451498%3C/gale_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2473804287&rft_id=info:pmid/&rft_galeid=A718451498&rfr_iscdi=true