The First Record of a Representative of the Toarcian–Early Aalenian Belemnites in Kimberlites of the Obnazhennaya Pipe (Northeastern Siberian Platform)
A rostrum fragment of a representative of the Toarcian–Early Aalenian (the latest Early Jurassic–the earliest Middle Jurassic) belemnites Arcobelus cf. krimholzi (Sachs, 1970) was found for the first time in kimberlites of the Obnazhennaya pipe of the Kuoika kimberlite field (northeastern Siberian P...
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Published in: | Doklady earth sciences Vol. 513; no. 2; pp. 1344 - 1348 |
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Main Authors: | , , , |
Format: | Journal Article |
Language: | English |
Published: |
Moscow
Pleiades Publishing
01-12-2023
Springer Nature B.V |
Subjects: | |
Online Access: | Get full text |
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Summary: | A rostrum fragment of a representative of the Toarcian–Early Aalenian (the latest Early Jurassic–the earliest Middle Jurassic) belemnites
Arcobelus
cf.
krimholzi
(Sachs, 1970) was found for the first time in kimberlites of the Obnazhennaya pipe of the Kuoika kimberlite field (northeastern Siberian Platform, Olenek Uplift). It was shown that the belemnite records previously known here and dated to the Late Jurassic or Early Cretaceous may be of Bajocian–Bathonian (Middle Jurassic) age. The stage of kimberlite magmatism of 177 ± 1.5 Ma, recently established in the northeastern part of the Siberian craton according to U–Pb geochronological data, falls on the time of the existence of belemnites of the genus
Arcobelus
. The estimated Late Bajocian–Early Bathonian age of the representative of the genus
Pachyteuthis,
previously found in kimberlites of the Obnazhennaya pipe, is consistent with the
40
Ar/
39
Ar age (167 Ma), as well as with the age based on some paleomagnetic data (168 ± 11 Ma) reported for the pipe. Taking into consideration the new data on belemnites, the internal part of the shelf should be extended to the territory of the Kuoika kimberlite field in the paleogeographic schemes of the northeastern part of the Siberian Platform during the Toarcian–Early Bathonian. |
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ISSN: | 1028-334X 1531-8354 |
DOI: | 10.1134/S1028334X23601876 |