Pollen data frome Lake Teletskoye, Altai Mountains, south-eastern West Siberia, Russia, with age-depth model

Lake Teletskoye (spanning 51°20′ to 51°47′N and 87°15′ to 87°50′E) is the largest lake in the Altai Mountains and is 77 km long and 330 m deep.The core location (51°44.99′N, 87°37.414′E) was at the deepest part of the lake. The altitude of the mountains surrounding the lake is 1900 m a.s.l. on avera...

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Main Author: Rudaya, Natalia
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2020
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.914490
https://doi.org/10.1594/PANGAEA.914490
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.914490
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.914490 2024-09-15T18:39:49+00:00 Pollen data frome Lake Teletskoye, Altai Mountains, south-eastern West Siberia, Russia, with age-depth model Rudaya, Natalia LATITUDE: 51.749830 * LONGITUDE: 87.623570 2020 application/zip, 4 datasets https://doi.pangaea.de/10.1594/PANGAEA.914490 https://doi.org/10.1594/PANGAEA.914490 en eng PANGAEA Rudaya, Natalia; Nazarova, Larisa B; Novenko, Elena Y; Andreev, Andrei A; Kalugin, Ivan A; Daryin, Andrei V; Babich, Valery V; Li, Hong-Chun; Shilov, Pavel (2016): Quantitative reconstructions of mid- to late holocene climate and vegetation in the north-eastern Altai mountains recorded in lake Teletskoye. Global and Planetary Change, 141, 12-24, https://doi.org/10.1016/j.gloplacha.2016.04.002 https://doi.pangaea.de/10.1594/PANGAEA.914490 https://doi.org/10.1594/PANGAEA.914490 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Altai lake Pollen Western Siberia dataset publication series 2020 ftpangaea https://doi.org/10.1594/PANGAEA.91449010.1016/j.gloplacha.2016.04.002 2024-07-24T02:31:21Z Lake Teletskoye (spanning 51°20′ to 51°47′N and 87°15′ to 87°50′E) is the largest lake in the Altai Mountains and is 77 km long and 330 m deep.The core location (51°44.99′N, 87°37.414′E) was at the deepest part of the lake. The altitude of the mountains surrounding the lake is 1900 m a.s.l. on average. Due to higher annual precipitation at the area, the steppe belt is absencent but it occurs, at least fragmentarily, in other parts of the mountains. Only very small patches along the lakeshore represent steppe-like vegetation. Birch forests mixed with meadows occur at lower altitudes, up to 700 m a.s.l. Unique evergreen (so-called 'dark') coniferous forest grow between 700 and 1700ma.s.l. The mountains above 1700 m are covered by Siberian pine (Pinus sibirica) forest. Above the tree line, at about 1800 m, alpine tundra and alpine meadow communities are widespread. Dating was complicated by the absence of plant macrofossils in the sediments and low bulk TOC. To obtain a more reliable chronology, the 210Pb activity and 137Cs content were also analysed. For more details see Rudaya et al., 2016. Other/Unknown Material Tundra Siberia PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(87.623570,87.623570,51.749830,51.749830)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Altai
lake
Pollen
Western Siberia
spellingShingle Altai
lake
Pollen
Western Siberia
Rudaya, Natalia
Pollen data frome Lake Teletskoye, Altai Mountains, south-eastern West Siberia, Russia, with age-depth model
topic_facet Altai
lake
Pollen
Western Siberia
description Lake Teletskoye (spanning 51°20′ to 51°47′N and 87°15′ to 87°50′E) is the largest lake in the Altai Mountains and is 77 km long and 330 m deep.The core location (51°44.99′N, 87°37.414′E) was at the deepest part of the lake. The altitude of the mountains surrounding the lake is 1900 m a.s.l. on average. Due to higher annual precipitation at the area, the steppe belt is absencent but it occurs, at least fragmentarily, in other parts of the mountains. Only very small patches along the lakeshore represent steppe-like vegetation. Birch forests mixed with meadows occur at lower altitudes, up to 700 m a.s.l. Unique evergreen (so-called 'dark') coniferous forest grow between 700 and 1700ma.s.l. The mountains above 1700 m are covered by Siberian pine (Pinus sibirica) forest. Above the tree line, at about 1800 m, alpine tundra and alpine meadow communities are widespread. Dating was complicated by the absence of plant macrofossils in the sediments and low bulk TOC. To obtain a more reliable chronology, the 210Pb activity and 137Cs content were also analysed. For more details see Rudaya et al., 2016.
format Other/Unknown Material
author Rudaya, Natalia
author_facet Rudaya, Natalia
author_sort Rudaya, Natalia
title Pollen data frome Lake Teletskoye, Altai Mountains, south-eastern West Siberia, Russia, with age-depth model
title_short Pollen data frome Lake Teletskoye, Altai Mountains, south-eastern West Siberia, Russia, with age-depth model
title_full Pollen data frome Lake Teletskoye, Altai Mountains, south-eastern West Siberia, Russia, with age-depth model
title_fullStr Pollen data frome Lake Teletskoye, Altai Mountains, south-eastern West Siberia, Russia, with age-depth model
title_full_unstemmed Pollen data frome Lake Teletskoye, Altai Mountains, south-eastern West Siberia, Russia, with age-depth model
title_sort pollen data frome lake teletskoye, altai mountains, south-eastern west siberia, russia, with age-depth model
publisher PANGAEA
publishDate 2020
url https://doi.pangaea.de/10.1594/PANGAEA.914490
https://doi.org/10.1594/PANGAEA.914490
op_coverage LATITUDE: 51.749830 * LONGITUDE: 87.623570
long_lat ENVELOPE(87.623570,87.623570,51.749830,51.749830)
genre Tundra
Siberia
genre_facet Tundra
Siberia
op_relation Rudaya, Natalia; Nazarova, Larisa B; Novenko, Elena Y; Andreev, Andrei A; Kalugin, Ivan A; Daryin, Andrei V; Babich, Valery V; Li, Hong-Chun; Shilov, Pavel (2016): Quantitative reconstructions of mid- to late holocene climate and vegetation in the north-eastern Altai mountains recorded in lake Teletskoye. Global and Planetary Change, 141, 12-24, https://doi.org/10.1016/j.gloplacha.2016.04.002
https://doi.pangaea.de/10.1594/PANGAEA.914490
https://doi.org/10.1594/PANGAEA.914490
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.91449010.1016/j.gloplacha.2016.04.002
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