Biotic paleothermometry constrains on Arctic plates reconstructions: Carboniferous and Permian (Zhokhov Island, De‐Longa Group Islands, New Siberian Archipelago). Issue 9 (27th September 2016)

• Record Type: Journal Article
• Authors: Davydov, Vladimir I.
• Is Part Of: Tectonics. Volume 35:Issue 9(2016)
• Page Start: 2158
• Page End: 2170
• Publication Date: 2016-09-27
• Subjects: New Siberian Archipelago -- Late Paleozoic biota -- paleothermometry constrains -- paleogeography -- Chukotka and Wrangelia terranes; Geology, Structural -- Periodicals; 551.8
• DOI: 10.1002/2016TC004249
• Languages: English
• ISSNs: 0278-7407

Abstract

Abstract: 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. Key Points: The document in New Siberian Archipelago fusulinid fauna never occurring north from the forbiddance line, i.e., 30–35°N/S The biota paleothermometry provided latitudinal constrains on the paleogeography and tectonics The paleogeography of New Siberian and Wrangelia terranes and surrounding regions reconsidered