Late Glacial and Early Holocene Climatic Changes Based on a Multiproxy Lacustrine Sediment Record from Northeast Siberia
Palynological (species assemblage, pollen accumulation rate), geochemical (carbon to nitrogen ratios, organic carbon and biogenic silica content), and sedimentological (particle size, magnetic susceptibility) data combined with improved chronology and greater sampling resolution from a new core from...
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ftosti:oai:osti.gov:965078 2023-07-30T04:07:20+02:00 Late Glacial and Early Holocene Climatic Changes Based on a Multiproxy Lacustrine Sediment Record from Northeast Siberia Kokorowski, H D Anderson, P M Sletten, R S Lozhkin, A V Brown, T A 2021-04-26 application/pdf http://www.osti.gov/servlets/purl/965078 https://www.osti.gov/biblio/965078 https://doi.org/10.1657/1523-0430%2807-036%29%5BKOKOROWSKI%5D2.0.CO%3B2 https://doi.org/10.1657/1523-0430(07-036)[KOKOROWSKI]2.0.CO;2 unknown http://www.osti.gov/servlets/purl/965078 https://www.osti.gov/biblio/965078 https://doi.org/10.1657/1523-0430%2807-036%29%5BKOKOROWSKI%5D2.0.CO%3B2 doi:10.1657/1523-0430(07-036)[KOKOROWSKI]2.0.CO;2 58 GEOSCIENCES 54 ENVIRONMENTAL SCIENCES CARBON CLIMATIC CHANGE MAGNETIC SUSCEPTIBILITY NITROGEN PLANTS POLLEN RESOLUTION SAMPLING SEDIMENTS SHRUBS SIBERIA SILICA TREES TUNDRA 2021 ftosti https://doi.org/10.1657/1523-0430%2807-036%29%5BKOKOROWSKI%5D2.0.CO%3B210.1657/1523-0430(07-036)[KOKOROWSKI]2.0.CO;2 2023-07-11T08:47:42Z Palynological (species assemblage, pollen accumulation rate), geochemical (carbon to nitrogen ratios, organic carbon and biogenic silica content), and sedimentological (particle size, magnetic susceptibility) data combined with improved chronology and greater sampling resolution from a new core from Elikchan 4 Lake provide a stronger basis for defining paleoenvironmental changes than was previously possible. Persistence of herb-dominated tundra, slow expansion of Betula and Alnus shrubs, and low percentages of organic carbon and biogenic silica suggest that the Late-Glacial transition (ca. 16,000-11,000 cal. yr BP) was a period of gradual rather than abrupt vegetation and climatic change. Consistency of all Late-Glacial data indicates no Younger Dryas climatic oscillation. A dramatic peak in pollen accumulation rates (ca. 11,000-9800 cal. yr BP) suggests a possible summer temperature optimum, but finer grain-sizes, low magnetic susceptibility, and greater organic carbon and biogenic silica, while showing significant warming at ca. 11,000 cal. yr BP, offer no evidence of a Holocene thermal maximum. When compared to trends in other paleo-records, the new Elikchan data underscore the apparent spatial complexity of climatic responses in Northeast Siberia to global forcings between ca. 16,000-9000 cal. yr BP. Other/Unknown Material Tundra Siberia SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Elikchan ENVELOPE(156.634,156.634,62.369,62.369) |
institution |
Open Polar |
collection |
SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) |
op_collection_id |
ftosti |
language |
unknown |
topic |
58 GEOSCIENCES 54 ENVIRONMENTAL SCIENCES CARBON CLIMATIC CHANGE MAGNETIC SUSCEPTIBILITY NITROGEN PLANTS POLLEN RESOLUTION SAMPLING SEDIMENTS SHRUBS SIBERIA SILICA TREES TUNDRA |
spellingShingle |
58 GEOSCIENCES 54 ENVIRONMENTAL SCIENCES CARBON CLIMATIC CHANGE MAGNETIC SUSCEPTIBILITY NITROGEN PLANTS POLLEN RESOLUTION SAMPLING SEDIMENTS SHRUBS SIBERIA SILICA TREES TUNDRA Kokorowski, H D Anderson, P M Sletten, R S Lozhkin, A V Brown, T A Late Glacial and Early Holocene Climatic Changes Based on a Multiproxy Lacustrine Sediment Record from Northeast Siberia |
topic_facet |
58 GEOSCIENCES 54 ENVIRONMENTAL SCIENCES CARBON CLIMATIC CHANGE MAGNETIC SUSCEPTIBILITY NITROGEN PLANTS POLLEN RESOLUTION SAMPLING SEDIMENTS SHRUBS SIBERIA SILICA TREES TUNDRA |
description |
Palynological (species assemblage, pollen accumulation rate), geochemical (carbon to nitrogen ratios, organic carbon and biogenic silica content), and sedimentological (particle size, magnetic susceptibility) data combined with improved chronology and greater sampling resolution from a new core from Elikchan 4 Lake provide a stronger basis for defining paleoenvironmental changes than was previously possible. Persistence of herb-dominated tundra, slow expansion of Betula and Alnus shrubs, and low percentages of organic carbon and biogenic silica suggest that the Late-Glacial transition (ca. 16,000-11,000 cal. yr BP) was a period of gradual rather than abrupt vegetation and climatic change. Consistency of all Late-Glacial data indicates no Younger Dryas climatic oscillation. A dramatic peak in pollen accumulation rates (ca. 11,000-9800 cal. yr BP) suggests a possible summer temperature optimum, but finer grain-sizes, low magnetic susceptibility, and greater organic carbon and biogenic silica, while showing significant warming at ca. 11,000 cal. yr BP, offer no evidence of a Holocene thermal maximum. When compared to trends in other paleo-records, the new Elikchan data underscore the apparent spatial complexity of climatic responses in Northeast Siberia to global forcings between ca. 16,000-9000 cal. yr BP. |
author |
Kokorowski, H D Anderson, P M Sletten, R S Lozhkin, A V Brown, T A |
author_facet |
Kokorowski, H D Anderson, P M Sletten, R S Lozhkin, A V Brown, T A |
author_sort |
Kokorowski, H D |
title |
Late Glacial and Early Holocene Climatic Changes Based on a Multiproxy Lacustrine Sediment Record from Northeast Siberia |
title_short |
Late Glacial and Early Holocene Climatic Changes Based on a Multiproxy Lacustrine Sediment Record from Northeast Siberia |
title_full |
Late Glacial and Early Holocene Climatic Changes Based on a Multiproxy Lacustrine Sediment Record from Northeast Siberia |
title_fullStr |
Late Glacial and Early Holocene Climatic Changes Based on a Multiproxy Lacustrine Sediment Record from Northeast Siberia |
title_full_unstemmed |
Late Glacial and Early Holocene Climatic Changes Based on a Multiproxy Lacustrine Sediment Record from Northeast Siberia |
title_sort |
late glacial and early holocene climatic changes based on a multiproxy lacustrine sediment record from northeast siberia |
publishDate |
2021 |
url |
http://www.osti.gov/servlets/purl/965078 https://www.osti.gov/biblio/965078 https://doi.org/10.1657/1523-0430%2807-036%29%5BKOKOROWSKI%5D2.0.CO%3B2 https://doi.org/10.1657/1523-0430(07-036)[KOKOROWSKI]2.0.CO;2 |
long_lat |
ENVELOPE(156.634,156.634,62.369,62.369) |
geographic |
Elikchan |
geographic_facet |
Elikchan |
genre |
Tundra Siberia |
genre_facet |
Tundra Siberia |
op_relation |
http://www.osti.gov/servlets/purl/965078 https://www.osti.gov/biblio/965078 https://doi.org/10.1657/1523-0430%2807-036%29%5BKOKOROWSKI%5D2.0.CO%3B2 doi:10.1657/1523-0430(07-036)[KOKOROWSKI]2.0.CO;2 |
op_doi |
https://doi.org/10.1657/1523-0430%2807-036%29%5BKOKOROWSKI%5D2.0.CO%3B210.1657/1523-0430(07-036)[KOKOROWSKI]2.0.CO;2 |
_version_ |
1772820588315803648 |