Late quaternary insects and freshwater invertebrates of the alaskan north slope and paleoenvironmental reconstructions in arctic Alaska

© INVERTEBRATE ZOOLOGY, 2019. A large series (26 samples) of fossil insect assemblages were excavated from riverbank exposures at two localities at Ikpikpuk and Titaluk Rivers on the North Slope of Alaska, U.S.A. Climatic conditions were reconstructed for the Late Pleistocene and early Holocene base...

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Main Authors: Kuzmina S., Elias S., Kotov A.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2019
Subjects:
Online Access:https://openrepository.ru/article?id=199298
id ftneicon:oai:rour.neicon.ru:rour/199298
record_format openpolar
spelling ftneicon:oai:rour.neicon.ru:rour/199298 2023-05-15T15:05:29+02:00 Late quaternary insects and freshwater invertebrates of the alaskan north slope and paleoenvironmental reconstructions in arctic Alaska Kuzmina S. Elias S. Kotov A. 2019 https://openrepository.ru/article?id=199298 unknown Invertebrate Zoology 2 16 89 http://rour.neicon.ru:80/xmlui/bitstream/rour/199298/1/nora.pdf 1812-9250 https://openrepository.ru/article?id=199298 SCOPUS18129250-2019-16-2-SID85070756481 Beetles Beringia Cladocera Fossil insects Holocene Pleistocene Steppetundra Article 2019 ftneicon 2020-07-21T12:06:11Z © INVERTEBRATE ZOOLOGY, 2019. A large series (26 samples) of fossil insect assemblages were excavated from riverbank exposures at two localities at Ikpikpuk and Titaluk Rivers on the North Slope of Alaska, U.S.A. Climatic conditions were reconstructed for the Late Pleistocene and early Holocene based on the fossil insect assemblage data. Insects indicate the continuous existence of a steppe-tundra community on the Alaskan North Slope during the end of the Pleistocene and the beginning of the Holocene. The invasion of poplar during the Early Holocene occurred within the context of the steppe-tundra community. The insect faunas indicate plant communities dominated by grasses and other herbs, with the local presence of tall shrubs and dwarf willows. The composition of the North Slope insect communities during the study interval was affected by the high latitude of the localities, periglacial winds coming off Brooks Range glaciers, and the close proximity of eolian sand and silt. The North Slope environment differed from those in more southerly localities in Eastern Beringia, reflecting ancient climatic and vegetational zonation. Article in Journal/Newspaper Arctic Brooks Range glaciers north slope Tundra Alaska Beringia NORA (National aggregator of open repositories of Russian universities) Arctic
institution Open Polar
collection NORA (National aggregator of open repositories of Russian universities)
op_collection_id ftneicon
language unknown
topic Beetles
Beringia
Cladocera
Fossil insects
Holocene
Pleistocene
Steppetundra
spellingShingle Beetles
Beringia
Cladocera
Fossil insects
Holocene
Pleistocene
Steppetundra
Kuzmina S.
Elias S.
Kotov A.
Late quaternary insects and freshwater invertebrates of the alaskan north slope and paleoenvironmental reconstructions in arctic Alaska
topic_facet Beetles
Beringia
Cladocera
Fossil insects
Holocene
Pleistocene
Steppetundra
description © INVERTEBRATE ZOOLOGY, 2019. A large series (26 samples) of fossil insect assemblages were excavated from riverbank exposures at two localities at Ikpikpuk and Titaluk Rivers on the North Slope of Alaska, U.S.A. Climatic conditions were reconstructed for the Late Pleistocene and early Holocene based on the fossil insect assemblage data. Insects indicate the continuous existence of a steppe-tundra community on the Alaskan North Slope during the end of the Pleistocene and the beginning of the Holocene. The invasion of poplar during the Early Holocene occurred within the context of the steppe-tundra community. The insect faunas indicate plant communities dominated by grasses and other herbs, with the local presence of tall shrubs and dwarf willows. The composition of the North Slope insect communities during the study interval was affected by the high latitude of the localities, periglacial winds coming off Brooks Range glaciers, and the close proximity of eolian sand and silt. The North Slope environment differed from those in more southerly localities in Eastern Beringia, reflecting ancient climatic and vegetational zonation.
format Article in Journal/Newspaper
author Kuzmina S.
Elias S.
Kotov A.
author_facet Kuzmina S.
Elias S.
Kotov A.
author_sort Kuzmina S.
title Late quaternary insects and freshwater invertebrates of the alaskan north slope and paleoenvironmental reconstructions in arctic Alaska
title_short Late quaternary insects and freshwater invertebrates of the alaskan north slope and paleoenvironmental reconstructions in arctic Alaska
title_full Late quaternary insects and freshwater invertebrates of the alaskan north slope and paleoenvironmental reconstructions in arctic Alaska
title_fullStr Late quaternary insects and freshwater invertebrates of the alaskan north slope and paleoenvironmental reconstructions in arctic Alaska
title_full_unstemmed Late quaternary insects and freshwater invertebrates of the alaskan north slope and paleoenvironmental reconstructions in arctic Alaska
title_sort late quaternary insects and freshwater invertebrates of the alaskan north slope and paleoenvironmental reconstructions in arctic alaska
publishDate 2019
url https://openrepository.ru/article?id=199298
geographic Arctic
geographic_facet Arctic
genre Arctic
Brooks Range
glaciers
north slope
Tundra
Alaska
Beringia
genre_facet Arctic
Brooks Range
glaciers
north slope
Tundra
Alaska
Beringia
op_source SCOPUS18129250-2019-16-2-SID85070756481
op_relation Invertebrate Zoology
2
16
89
http://rour.neicon.ru:80/xmlui/bitstream/rour/199298/1/nora.pdf
1812-9250
https://openrepository.ru/article?id=199298
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