The Upper Triassic of northern Middle Siberia: stratigraphy and palynology
The Lower Carnian succession in northern Middle Siberia includes continental and marine deposits. Bivalves, nautiloids and ammonites in the marine units provide biostratigraphic control for a palynological study of three important sections. Palynomorph associations from the base of the succession in...
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Norwegian Polar Institute
2008
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ftjpolarres:oai:journals.openacademia.net:article/2896 2023-05-15T14:59:40+02:00 The Upper Triassic of northern Middle Siberia: stratigraphy and palynology Ilyina, Natalya V. Egorov, Alexander Y. 2008-12-01 application/pdf https://polarresearch.net/index.php/polar/article/view/2896 https://doi.org/10.3402/polar.v27i3.6195 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2896/6523 https://polarresearch.net/index.php/polar/article/view/2896 doi:10.3402/polar.v27i3.6195 Copyright (c) 2018 Polar Research Polar Research; Vol. 27 No. 3 (2008): Special issue: The Boreal Triassic; 372-392 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2008 ftjpolarres https://doi.org/10.3402/polar.v27i3.6195 2021-11-11T19:13:21Z The Lower Carnian succession in northern Middle Siberia includes continental and marine deposits. Bivalves, nautiloids and ammonites in the marine units provide biostratigraphic control for a palynological study of three important sections. Palynomorph associations from the base of the succession include forms that have previously been reported only from Norian and Rhaetian deposits in the Tethyan and Boreal realms. This suggests that, in comparison with other areas, the palynoflora of Siberia was more uniform throughout the Late Triassic, and that the Carnian and Norian stages have a miospore assemblage that is recognizable in a wide belt through Arctic Canada and northern Eurasia. Article in Journal/Newspaper Arctic Polar Research Siberia Polar Research (E-Journal) Arctic Canada Polar Research 27 3 |
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Open Polar |
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Polar Research (E-Journal) |
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ftjpolarres |
language |
English |
description |
The Lower Carnian succession in northern Middle Siberia includes continental and marine deposits. Bivalves, nautiloids and ammonites in the marine units provide biostratigraphic control for a palynological study of three important sections. Palynomorph associations from the base of the succession include forms that have previously been reported only from Norian and Rhaetian deposits in the Tethyan and Boreal realms. This suggests that, in comparison with other areas, the palynoflora of Siberia was more uniform throughout the Late Triassic, and that the Carnian and Norian stages have a miospore assemblage that is recognizable in a wide belt through Arctic Canada and northern Eurasia. |
format |
Article in Journal/Newspaper |
author |
Ilyina, Natalya V. Egorov, Alexander Y. |
spellingShingle |
Ilyina, Natalya V. Egorov, Alexander Y. The Upper Triassic of northern Middle Siberia: stratigraphy and palynology |
author_facet |
Ilyina, Natalya V. Egorov, Alexander Y. |
author_sort |
Ilyina, Natalya V. |
title |
The Upper Triassic of northern Middle Siberia: stratigraphy and palynology |
title_short |
The Upper Triassic of northern Middle Siberia: stratigraphy and palynology |
title_full |
The Upper Triassic of northern Middle Siberia: stratigraphy and palynology |
title_fullStr |
The Upper Triassic of northern Middle Siberia: stratigraphy and palynology |
title_full_unstemmed |
The Upper Triassic of northern Middle Siberia: stratigraphy and palynology |
title_sort |
upper triassic of northern middle siberia: stratigraphy and palynology |
publisher |
Norwegian Polar Institute |
publishDate |
2008 |
url |
https://polarresearch.net/index.php/polar/article/view/2896 https://doi.org/10.3402/polar.v27i3.6195 |
geographic |
Arctic Canada |
geographic_facet |
Arctic Canada |
genre |
Arctic Polar Research Siberia |
genre_facet |
Arctic Polar Research Siberia |
op_source |
Polar Research; Vol. 27 No. 3 (2008): Special issue: The Boreal Triassic; 372-392 1751-8369 |
op_relation |
https://polarresearch.net/index.php/polar/article/view/2896/6523 https://polarresearch.net/index.php/polar/article/view/2896 doi:10.3402/polar.v27i3.6195 |
op_rights |
Copyright (c) 2018 Polar Research |
op_doi |
https://doi.org/10.3402/polar.v27i3.6195 |
container_title |
Polar Research |
container_volume |
27 |
container_issue |
3 |
_version_ |
1766331776332988416 |