Biotic paleothermometry constrains on Arctic plates reconstructions: Carboniferous and Permian (Zhokhov Island, De-Longa Group Islands, New Siberian Archipelago)
©2016. American Geophysical Union. All Rights Reserved.A warm-water fauna and flora from a Carboniferous limestone xenolith that was captured during penetration of deep intraplate Cenozoic basalts through a Paleozoic carbonate platform have been found on Zhokhov Island, New Siberian Archipelago (NSA...
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ftkazanuniv:oai:dspace.kpfu.ru:net/142943 2023-05-15T14:17:56+02:00 Biotic paleothermometry constrains on Arctic plates reconstructions: Carboniferous and Permian (Zhokhov Island, De-Longa Group Islands, New Siberian Archipelago) Davydov V. 2016 https://dspace.kpfu.ru/xmlui/handle/net/142943 unknown Tectonics 9 35 2158 http://dspace.kpfu.ru/xmlui/bitstream/net/142943/-1/SCOPUS02787407-2016-35-9-SID84989352604-a1.pdf 0278-7407 https://dspace.kpfu.ru/xmlui/handle/net/142943 SCOPUS02787407-2016-35-9-SID84989352604 Chukotka and Wrangelia terranes Late Paleozoic biota New Siberian Archipelago paleogeography paleothermometry constrains Article 2016 ftkazanuniv 2022-01-01T09:48:43Z ©2016. American Geophysical Union. All Rights Reserved.A warm-water fauna and flora from a Carboniferous limestone xenolith that was captured during penetration of deep intraplate Cenozoic basalts through a Paleozoic carbonate platform have been found on Zhokhov Island, New Siberian Archipelago (NSA). This limestone xenolith contains a very high taxonomic diversity of Moscovian (Middle Pennsylvanian) tropical foraminifera and calcareous algae. As this warm-water biota never occurs north of the forbiddance line, i.e., 30–35°N/S, this fauna and algal flora constrain the paleogeography and interpretation of the paleotectonics in the region. Thus, the location of the most of the New Siberian Archipelago islands at that time must have been within tropics or subtropics. Analyses of the existing data on fusulinid distribution within the Arctic region indicate that Zhokhov and Wrangel Islands were still a part of Alaska-Chukotka composite terrane as late as in the Artinskian. Both fusulinid and detrital zircon provenance data suggest that the Chukotka microplate, NSA, and Wrangel Island probably were close to Arctic Alaska until Triassic time. The fusulinids from the Mankomen Formation and other formations in Wrangelia show a strong affinity with the Uralo-Franklinian province regions including the Sverdrup Basin, Spitsbergen, Barents Sea, and Timan-Pechora and the northern-central Urals rather than with northern Panthalassa. Article in Journal/Newspaper Archipelago Arctic Barents Sea Chukotka Foraminifera* Pechora sverdrup basin Wrangel Island Zhokhov Island Alaska Spitsbergen Kazan Federal University Digital Repository Arctic Barents Sea Wrangel Island ENVELOPE(-179.385,-179.385,71.244,71.244) |
institution |
Open Polar |
collection |
Kazan Federal University Digital Repository |
op_collection_id |
ftkazanuniv |
language |
unknown |
topic |
Chukotka and Wrangelia terranes Late Paleozoic biota New Siberian Archipelago paleogeography paleothermometry constrains |
spellingShingle |
Chukotka and Wrangelia terranes Late Paleozoic biota New Siberian Archipelago paleogeography paleothermometry constrains Davydov V. Biotic paleothermometry constrains on Arctic plates reconstructions: Carboniferous and Permian (Zhokhov Island, De-Longa Group Islands, New Siberian Archipelago) |
topic_facet |
Chukotka and Wrangelia terranes Late Paleozoic biota New Siberian Archipelago paleogeography paleothermometry constrains |
description |
©2016. American Geophysical Union. All Rights Reserved.A warm-water fauna and flora from a Carboniferous limestone xenolith that was captured during penetration of deep intraplate Cenozoic basalts through a Paleozoic carbonate platform have been found on Zhokhov Island, New Siberian Archipelago (NSA). This limestone xenolith contains a very high taxonomic diversity of Moscovian (Middle Pennsylvanian) tropical foraminifera and calcareous algae. As this warm-water biota never occurs north of the forbiddance line, i.e., 30–35°N/S, this fauna and algal flora constrain the paleogeography and interpretation of the paleotectonics in the region. Thus, the location of the most of the New Siberian Archipelago islands at that time must have been within tropics or subtropics. Analyses of the existing data on fusulinid distribution within the Arctic region indicate that Zhokhov and Wrangel Islands were still a part of Alaska-Chukotka composite terrane as late as in the Artinskian. Both fusulinid and detrital zircon provenance data suggest that the Chukotka microplate, NSA, and Wrangel Island probably were close to Arctic Alaska until Triassic time. The fusulinids from the Mankomen Formation and other formations in Wrangelia show a strong affinity with the Uralo-Franklinian province regions including the Sverdrup Basin, Spitsbergen, Barents Sea, and Timan-Pechora and the northern-central Urals rather than with northern Panthalassa. |
format |
Article in Journal/Newspaper |
author |
Davydov V. |
author_facet |
Davydov V. |
author_sort |
Davydov V. |
title |
Biotic paleothermometry constrains on Arctic plates reconstructions: Carboniferous and Permian (Zhokhov Island, De-Longa Group Islands, New Siberian Archipelago) |
title_short |
Biotic paleothermometry constrains on Arctic plates reconstructions: Carboniferous and Permian (Zhokhov Island, De-Longa Group Islands, New Siberian Archipelago) |
title_full |
Biotic paleothermometry constrains on Arctic plates reconstructions: Carboniferous and Permian (Zhokhov Island, De-Longa Group Islands, New Siberian Archipelago) |
title_fullStr |
Biotic paleothermometry constrains on Arctic plates reconstructions: Carboniferous and Permian (Zhokhov Island, De-Longa Group Islands, New Siberian Archipelago) |
title_full_unstemmed |
Biotic paleothermometry constrains on Arctic plates reconstructions: Carboniferous and Permian (Zhokhov Island, De-Longa Group Islands, New Siberian Archipelago) |
title_sort |
biotic paleothermometry constrains on arctic plates reconstructions: carboniferous and permian (zhokhov island, de-longa group islands, new siberian archipelago) |
publishDate |
2016 |
url |
https://dspace.kpfu.ru/xmlui/handle/net/142943 |
long_lat |
ENVELOPE(-179.385,-179.385,71.244,71.244) |
geographic |
Arctic Barents Sea Wrangel Island |
geographic_facet |
Arctic Barents Sea Wrangel Island |
genre |
Archipelago Arctic Barents Sea Chukotka Foraminifera* Pechora sverdrup basin Wrangel Island Zhokhov Island Alaska Spitsbergen |
genre_facet |
Archipelago Arctic Barents Sea Chukotka Foraminifera* Pechora sverdrup basin Wrangel Island Zhokhov Island Alaska Spitsbergen |
op_source |
SCOPUS02787407-2016-35-9-SID84989352604 |
op_relation |
Tectonics 9 35 2158 http://dspace.kpfu.ru/xmlui/bitstream/net/142943/-1/SCOPUS02787407-2016-35-9-SID84989352604-a1.pdf 0278-7407 https://dspace.kpfu.ru/xmlui/handle/net/142943 |
_version_ |
1766289751238770688 |