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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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.726702 2023-05-15T16:37:49+02:00 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 LATITUDE: 51.716600 * LONGITUDE: 87.650000 2007-08-23 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.726702 https://doi.org/10.1594/PANGAEA.726702 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.726702 https://doi.org/10.1594/PANGAEA.726702 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY 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, https://doi.org/10.1016/j.yqres.2006.11.004 AWI_PerDyn Geological profile sampling GEOPRO Lake Teletskoye Altay Mountains Russia Permafrost Research (Periglacial Dynamics) @ AWI Teletskoye Dataset 2007 ftpangaea https://doi.org/10.1594/PANGAEA.726702 https://doi.org/10.1016/j.yqres.2006.11.004 2023-01-20T07:31:29Z 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 particle contents may reflect further deterioration of climate conditions between AD 1560 and 1810, consistent with the Little Ice Age. After AD 1850 the vegetation gradually approached the modern one, in conjunction with ongoing climate warming. Dataset Ice permafrost taiga PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(87.650000,87.650000,51.716600,51.716600) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
AWI_PerDyn Geological profile sampling GEOPRO Lake Teletskoye Altay Mountains Russia Permafrost Research (Periglacial Dynamics) @ AWI Teletskoye |
spellingShingle |
AWI_PerDyn Geological profile sampling GEOPRO Lake Teletskoye Altay Mountains Russia Permafrost Research (Periglacial Dynamics) @ AWI Teletskoye 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 |
AWI_PerDyn Geological profile sampling GEOPRO Lake Teletskoye Altay Mountains Russia Permafrost Research (Periglacial Dynamics) @ AWI Teletskoye |
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 particle contents may reflect further deterioration of climate conditions between AD 1560 and 1810, consistent with the Little Ice Age. After AD 1850 the vegetation gradually approached the modern one, in conjunction with ongoing climate warming. |
format |
Dataset |
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://doi.pangaea.de/10.1594/PANGAEA.726702 https://doi.org/10.1594/PANGAEA.726702 |
op_coverage |
LATITUDE: 51.716600 * LONGITUDE: 87.650000 |
long_lat |
ENVELOPE(87.650000,87.650000,51.716600,51.716600) |
genre |
Ice permafrost taiga |
genre_facet |
Ice permafrost taiga |
op_source |
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, https://doi.org/10.1016/j.yqres.2006.11.004 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.726702 https://doi.org/10.1594/PANGAEA.726702 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.726702 https://doi.org/10.1016/j.yqres.2006.11.004 |
_version_ |
1766028105950953472 |