Cretaceous microfossils as indicators of cooling episodes (Boreal and Peri-Tethyan Russia)
S4. Palaeogeographic sketch for Early Campanian. Distribution of the foraminifera and radiolaria in the EEP and in the Crimea–Caucasus area. White colour—land, area of denudation or erosian; blue colour—marine sediments. 1— Oxytoma teniucostata (Roemer), boreal bivalve migrant from Western Siberia;...
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ftgeosoclonfig:oai:figshare.com:article/11359097 2023-05-15T18:00:17+02:00 Cretaceous microfossils as indicators of cooling episodes (Boreal and Peri-Tethyan Russia) V. S. Vishnevskaya L. F. Kopaevich 2019-12-12T14:02:19Z https://doi.org/10.6084/m9.figshare.11359097.v1 https://figshare.com/articles/Cretaceous_microfossils_as_indicators_of_cooling_episodes_Boreal_and_Peri-Tethyan_Russia_/11359097 unknown doi:10.6084/m9.figshare.11359097.v1 https://figshare.com/articles/Cretaceous_microfossils_as_indicators_of_cooling_episodes_Boreal_and_Peri-Tethyan_Russia_/11359097 CC BY 4.0 CC-BY Geology boreal S 4. Palaeogeographic sketch Globotruncana arca beds EEP Cretaceous microfossils Planktonic foraminifera radiolaria Western Siberia Globotruncanita elevata Zone Peri-Tethyan Russia cooling episodes Mangyshlak MTS Pseudogavelinella clementiana Zone Crimea Tethys area colour Calcareous benthic foraminifera Image Figure 2019 ftgeosoclonfig https://doi.org/10.6084/m9.figshare.11359097.v1 2020-02-21T07:20:00Z S4. Palaeogeographic sketch for Early Campanian. Distribution of the foraminifera and radiolaria in the EEP and in the Crimea–Caucasus area. White colour—land, area of denudation or erosian; blue colour—marine sediments. 1— Oxytoma teniucostata (Roemer), boreal bivalve migrant from Western Siberia; 2— Marsupites testudinarius Schlotheim, crinoids from Tethys area. Calcareous benthic foraminifera of the Pseudogavelinella clementiana Zone: 3— P. clementiana (d'Orbigny); 4— Bolivinoides decoratus Jones. Planktonic foraminifera of Globotruncana arca beds on Mangyshlak MTS: 5— Globotruncana arca (Cushman); planktonic foraminifera of Globotruncanita elevata Zone in Crimea–Caucasus area: 6— Globotruncanita elevata (Brotzen). Radiolaria: 7—boreal radiolaria Prunobrachidae . Still Image Planktonic foraminifera Siberia Geological Society of London: Figshare |
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Geological Society of London: Figshare |
op_collection_id |
ftgeosoclonfig |
language |
unknown |
topic |
Geology boreal S 4. Palaeogeographic sketch Globotruncana arca beds EEP Cretaceous microfossils Planktonic foraminifera radiolaria Western Siberia Globotruncanita elevata Zone Peri-Tethyan Russia cooling episodes Mangyshlak MTS Pseudogavelinella clementiana Zone Crimea Tethys area colour Calcareous benthic foraminifera |
spellingShingle |
Geology boreal S 4. Palaeogeographic sketch Globotruncana arca beds EEP Cretaceous microfossils Planktonic foraminifera radiolaria Western Siberia Globotruncanita elevata Zone Peri-Tethyan Russia cooling episodes Mangyshlak MTS Pseudogavelinella clementiana Zone Crimea Tethys area colour Calcareous benthic foraminifera V. S. Vishnevskaya L. F. Kopaevich Cretaceous microfossils as indicators of cooling episodes (Boreal and Peri-Tethyan Russia) |
topic_facet |
Geology boreal S 4. Palaeogeographic sketch Globotruncana arca beds EEP Cretaceous microfossils Planktonic foraminifera radiolaria Western Siberia Globotruncanita elevata Zone Peri-Tethyan Russia cooling episodes Mangyshlak MTS Pseudogavelinella clementiana Zone Crimea Tethys area colour Calcareous benthic foraminifera |
description |
S4. Palaeogeographic sketch for Early Campanian. Distribution of the foraminifera and radiolaria in the EEP and in the Crimea–Caucasus area. White colour—land, area of denudation or erosian; blue colour—marine sediments. 1— Oxytoma teniucostata (Roemer), boreal bivalve migrant from Western Siberia; 2— Marsupites testudinarius Schlotheim, crinoids from Tethys area. Calcareous benthic foraminifera of the Pseudogavelinella clementiana Zone: 3— P. clementiana (d'Orbigny); 4— Bolivinoides decoratus Jones. Planktonic foraminifera of Globotruncana arca beds on Mangyshlak MTS: 5— Globotruncana arca (Cushman); planktonic foraminifera of Globotruncanita elevata Zone in Crimea–Caucasus area: 6— Globotruncanita elevata (Brotzen). Radiolaria: 7—boreal radiolaria Prunobrachidae . |
format |
Still Image |
author |
V. S. Vishnevskaya L. F. Kopaevich |
author_facet |
V. S. Vishnevskaya L. F. Kopaevich |
author_sort |
V. S. Vishnevskaya |
title |
Cretaceous microfossils as indicators of cooling episodes (Boreal and Peri-Tethyan Russia) |
title_short |
Cretaceous microfossils as indicators of cooling episodes (Boreal and Peri-Tethyan Russia) |
title_full |
Cretaceous microfossils as indicators of cooling episodes (Boreal and Peri-Tethyan Russia) |
title_fullStr |
Cretaceous microfossils as indicators of cooling episodes (Boreal and Peri-Tethyan Russia) |
title_full_unstemmed |
Cretaceous microfossils as indicators of cooling episodes (Boreal and Peri-Tethyan Russia) |
title_sort |
cretaceous microfossils as indicators of cooling episodes (boreal and peri-tethyan russia) |
publishDate |
2019 |
url |
https://doi.org/10.6084/m9.figshare.11359097.v1 https://figshare.com/articles/Cretaceous_microfossils_as_indicators_of_cooling_episodes_Boreal_and_Peri-Tethyan_Russia_/11359097 |
genre |
Planktonic foraminifera Siberia |
genre_facet |
Planktonic foraminifera Siberia |
op_relation |
doi:10.6084/m9.figshare.11359097.v1 https://figshare.com/articles/Cretaceous_microfossils_as_indicators_of_cooling_episodes_Boreal_and_Peri-Tethyan_Russia_/11359097 |
op_rights |
CC BY 4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.11359097.v1 |
_version_ |
1766169328915316736 |