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...
Main Authors: | , , , , , |
---|---|
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 |
_version_ |
1809935215063203840 |