Pollen record and age determination of a sediment profile from Lake Teletskoye, Russia ...

A high-resolution pollen record from Lake Teletskoye documents the climate-related vegetation history of the northern Altai Mountain region during the last millennium. Siberian pine taiga with Scots pine, fir, spruce, and birch dominated the vegetation between ca. AD 1050 and 1100. The climate was s...

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Main Authors: Andreev, Andrei A, Pierau, Roberto, Kalugin, Ivan A, Daryin, Andrei V, Smolyaninova, Lyubov G, Diekmann, Bernhard
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2007
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.726702
https://doi.pangaea.de/10.1594/PANGAEA.726702
id ftdatacite:10.1594/pangaea.726702
record_format openpolar
spelling ftdatacite:10.1594/pangaea.726702 2024-09-09T20:03:17+00:00 Pollen record and age determination of a sediment profile from Lake Teletskoye, Russia ... Andreev, Andrei A Pierau, Roberto Kalugin, Ivan A Daryin, Andrei V Smolyaninova, Lyubov G Diekmann, Bernhard 2007 application/zip https://dx.doi.org/10.1594/pangaea.726702 https://doi.pangaea.de/10.1594/PANGAEA.726702 en eng PANGAEA https://dx.doi.org/10.1016/j.yqres.2006.11.004 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Geological profile sampling Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn article Collection Supplementary Publication Series of Datasets 2007 ftdatacite https://doi.org/10.1594/pangaea.72670210.1016/j.yqres.2006.11.004 2024-08-01T10:54:44Z A high-resolution pollen record from Lake Teletskoye documents the climate-related vegetation history of the northern Altai Mountain region during the last millennium. Siberian pine taiga with Scots pine, fir, spruce, and birch dominated the vegetation between ca. AD 1050 and 1100. The climate was similar to modern. In the beginning of the 12th century, birch and shrub alder increased. Lowered pollen concentrations and simultaneous peaks in herbs (especially Artemisia and Poaceae), ferns, and charcoal fragments point to colder and more arid climate conditions than before, with frequent fire events. Around AD 1200, regional climate became warmer and more humid than present, as revealed by an increase of Siberian pine and decreases of dry herb taxa and charcoal contents. Climatic conditions were rather stable until ca. AD 1410. An increase of Artemisia pollen may reflect slightly drier climate conditions between AD 1410 and 1560. Increases in Alnus, Betula, Artemisia, and Chenopodiaceae pollen and in charcoal ... : Supplement to: Andreev, Andrei A; Pierau, Roberto; Kalugin, Ivan A; Daryin, Andrei V; Smolyaninova, Lyubov G; Diekmann, Bernhard (2007): Environmental changes in the northern Altai during the last millennium documented in Lake Teletskoye pollen record. Quaternary Research, 67(3), 394-399 ... Article in Journal/Newspaper permafrost taiga DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Geological profile sampling
Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn
spellingShingle Geological profile sampling
Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn
Andreev, Andrei A
Pierau, Roberto
Kalugin, Ivan A
Daryin, Andrei V
Smolyaninova, Lyubov G
Diekmann, Bernhard
Pollen record and age determination of a sediment profile from Lake Teletskoye, Russia ...
topic_facet Geological profile sampling
Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn
description A high-resolution pollen record from Lake Teletskoye documents the climate-related vegetation history of the northern Altai Mountain region during the last millennium. Siberian pine taiga with Scots pine, fir, spruce, and birch dominated the vegetation between ca. AD 1050 and 1100. The climate was similar to modern. In the beginning of the 12th century, birch and shrub alder increased. Lowered pollen concentrations and simultaneous peaks in herbs (especially Artemisia and Poaceae), ferns, and charcoal fragments point to colder and more arid climate conditions than before, with frequent fire events. Around AD 1200, regional climate became warmer and more humid than present, as revealed by an increase of Siberian pine and decreases of dry herb taxa and charcoal contents. Climatic conditions were rather stable until ca. AD 1410. An increase of Artemisia pollen may reflect slightly drier climate conditions between AD 1410 and 1560. Increases in Alnus, Betula, Artemisia, and Chenopodiaceae pollen and in charcoal ... : Supplement to: Andreev, Andrei A; Pierau, Roberto; Kalugin, Ivan A; Daryin, Andrei V; Smolyaninova, Lyubov G; Diekmann, Bernhard (2007): Environmental changes in the northern Altai during the last millennium documented in Lake Teletskoye pollen record. Quaternary Research, 67(3), 394-399 ...
format Article in Journal/Newspaper
author Andreev, Andrei A
Pierau, Roberto
Kalugin, Ivan A
Daryin, Andrei V
Smolyaninova, Lyubov G
Diekmann, Bernhard
author_facet Andreev, Andrei A
Pierau, Roberto
Kalugin, Ivan A
Daryin, Andrei V
Smolyaninova, Lyubov G
Diekmann, Bernhard
author_sort Andreev, Andrei A
title Pollen record and age determination of a sediment profile from Lake Teletskoye, Russia ...
title_short Pollen record and age determination of a sediment profile from Lake Teletskoye, Russia ...
title_full Pollen record and age determination of a sediment profile from Lake Teletskoye, Russia ...
title_fullStr Pollen record and age determination of a sediment profile from Lake Teletskoye, Russia ...
title_full_unstemmed Pollen record and age determination of a sediment profile from Lake Teletskoye, Russia ...
title_sort pollen record and age determination of a sediment profile from lake teletskoye, russia ...
publisher PANGAEA
publishDate 2007
url https://dx.doi.org/10.1594/pangaea.726702
https://doi.pangaea.de/10.1594/PANGAEA.726702
genre permafrost
taiga
genre_facet permafrost
taiga
op_relation https://dx.doi.org/10.1016/j.yqres.2006.11.004
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.72670210.1016/j.yqres.2006.11.004
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