The first early interstadial of Zirianian traces (Early Würm) glaciation on Siberia: U / Th date and palaeobotanical data
The application of the U / Th method allowed to reveal traces of an interstadial, which is coeval with the Brørup in the middle stream of the Ob’ River in the well-known Kirias outcrop. Description of a buried peat bog which is coeval with the Brørup interstadial, layers underlying and overlapping t...
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ftlithuaniansrc:oai:elaba:5742295 2023-05-15T17:48:47+02:00 The first early interstadial of Zirianian traces (Early Würm) glaciation on Siberia: U / Th date and palaeobotanical data Sibiro Zirianio (ankstyvojo Viurmio) apledėjimo ankstyvojo tarpstadialo pėdsakai: U / Th data ir paleobotaniniai duomenys Laukhin, Stanislav Arslanov, Khikmatulla A. Maksimov, Fedor E. Kuznetsov, Vladislav Yu. 2007 http://lsmu.lvb.lt/LSMU:ELABAPDB5742295&prefLang=en_US lit eng lit eng http://lsmu.lvb.lt/LSMU:ELABAPDB5742295&prefLang=en_US Geologija, 2007, Nr. 59, p. 47-58 ISSN 1392-110X Pleistocene Uranium-thorium dating Macroflora Palynospectra Western Siberia Zirianian Interglacial info:eu-repo/semantics/article 2007 ftlithuaniansrc 2021-12-02T00:47:32Z The application of the U / Th method allowed to reveal traces of an interstadial, which is coeval with the Brørup in the middle stream of the Ob’ River in the well-known Kirias outcrop. Description of a buried peat bog which is coeval with the Brørup interstadial, layers underlying and overlapping the Kirias section are discussed. The U / Th date was obtained from the peat bog by the methods: leachate alone (L / L) and total sample dissolution (TDS) – 105.5 + 3.6 / –3.3 Ka (L / L) and 104.4 + 4.4 / 3.9 Ka (TSD). The abundant flora (thousands of fruits, seeds, etc.) characteristic of north taiga shows the time of peat bog formation. This flora reflected the local vegetation near the swamp. Palynospectra reflect the zonality in vegetation changes. It characteristics in the beginning of peat bog formation show the development other sub-zones of taiga, followed by forest-tundra. In the layers of loam underlying and overlapping the buried peat bog, palynospectra of the non-forest periglacial vegetation of Zirianian (Early Würm) glacial time were studied. Article in Journal/Newspaper ob river taiga Tundra Siberia LSRC VL (Lithuanian Social Research Centre Virtual Library) |
institution |
Open Polar |
collection |
LSRC VL (Lithuanian Social Research Centre Virtual Library) |
op_collection_id |
ftlithuaniansrc |
language |
Lithuanian English |
topic |
Pleistocene Uranium-thorium dating Macroflora Palynospectra Western Siberia Zirianian Interglacial |
spellingShingle |
Pleistocene Uranium-thorium dating Macroflora Palynospectra Western Siberia Zirianian Interglacial Laukhin, Stanislav Arslanov, Khikmatulla A. Maksimov, Fedor E. Kuznetsov, Vladislav Yu. The first early interstadial of Zirianian traces (Early Würm) glaciation on Siberia: U / Th date and palaeobotanical data |
topic_facet |
Pleistocene Uranium-thorium dating Macroflora Palynospectra Western Siberia Zirianian Interglacial |
description |
The application of the U / Th method allowed to reveal traces of an interstadial, which is coeval with the Brørup in the middle stream of the Ob’ River in the well-known Kirias outcrop. Description of a buried peat bog which is coeval with the Brørup interstadial, layers underlying and overlapping the Kirias section are discussed. The U / Th date was obtained from the peat bog by the methods: leachate alone (L / L) and total sample dissolution (TDS) – 105.5 + 3.6 / –3.3 Ka (L / L) and 104.4 + 4.4 / 3.9 Ka (TSD). The abundant flora (thousands of fruits, seeds, etc.) characteristic of north taiga shows the time of peat bog formation. This flora reflected the local vegetation near the swamp. Palynospectra reflect the zonality in vegetation changes. It characteristics in the beginning of peat bog formation show the development other sub-zones of taiga, followed by forest-tundra. In the layers of loam underlying and overlapping the buried peat bog, palynospectra of the non-forest periglacial vegetation of Zirianian (Early Würm) glacial time were studied. |
format |
Article in Journal/Newspaper |
author |
Laukhin, Stanislav Arslanov, Khikmatulla A. Maksimov, Fedor E. Kuznetsov, Vladislav Yu. |
author_facet |
Laukhin, Stanislav Arslanov, Khikmatulla A. Maksimov, Fedor E. Kuznetsov, Vladislav Yu. |
author_sort |
Laukhin, Stanislav |
title |
The first early interstadial of Zirianian traces (Early Würm) glaciation on Siberia: U / Th date and palaeobotanical data |
title_short |
The first early interstadial of Zirianian traces (Early Würm) glaciation on Siberia: U / Th date and palaeobotanical data |
title_full |
The first early interstadial of Zirianian traces (Early Würm) glaciation on Siberia: U / Th date and palaeobotanical data |
title_fullStr |
The first early interstadial of Zirianian traces (Early Würm) glaciation on Siberia: U / Th date and palaeobotanical data |
title_full_unstemmed |
The first early interstadial of Zirianian traces (Early Würm) glaciation on Siberia: U / Th date and palaeobotanical data |
title_sort |
first early interstadial of zirianian traces (early würm) glaciation on siberia: u / th date and palaeobotanical data |
publishDate |
2007 |
url |
http://lsmu.lvb.lt/LSMU:ELABAPDB5742295&prefLang=en_US |
genre |
ob river taiga Tundra Siberia |
genre_facet |
ob river taiga Tundra Siberia |
op_source |
Geologija, 2007, Nr. 59, p. 47-58 ISSN 1392-110X |
op_relation |
http://lsmu.lvb.lt/LSMU:ELABAPDB5742295&prefLang=en_US |
_version_ |
1766154942600445952 |