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Ammonites and magnetostratigraphy of the Berriasian–Valanginian boundary deposits from eastern Crimea

In: Geologica Carpathica, vol. 68, no. 6
Vladimir V. Arkadiev - Vladimir A. Grishchenko - Andrei Yu. Guzhikov - Aleksey G. Manikin - Yuliya N. Savelieva - Anna A. Feodorova - Olga V. Shurekova

Details:

Year, pages: 2017, 505 - 516
Language: eng
Keywords:
Mountainous Crimea, Berriasian, Valanginian, ammonites, biostratigraphy, magnetostratigraphy, geomagnetic polarity, correlation
About article:
Euthymi, Crassicostatum and Callisto ammonite subzones, correlable with Paramimounum, Picteti, and Alpillensis subzones and probably with the Late Berriasian Otopeta Subzone of the Boissieri Standard Zone have been recognized in calcareous clays of the Berriasian–Valanginian boundary sequence in the Feodosiya district (eastern Crimea). The ammonite Leptoceras studeri (Ooster) suggests Late Berriasian to Early Valanginian age. Geomagnetic polarity indicates M16–M14r magnetozones. Therefore, the base of the Valanginian sequence in eastern Crimea should be placed within the M14r magnetozone.
How to cite:
ISO 690:
Arkadiev, V., Grishchenko, V., Guzhikov, A., Manikin, A., Savelieva, Y., Feodorova, A., Shurekova, O. 2017. Ammonites and magnetostratigraphy of the Berriasian–Valanginian boundary deposits from eastern Crimea. In Geologica Carpathica, vol. 68, no.6, pp. 505-516. 1335-0552. DOI: https://doi.org/10.1515/geoca-2017-0033

APA:
Arkadiev, V., Grishchenko, V., Guzhikov, A., Manikin, A., Savelieva, Y., Feodorova, A., Shurekova, O. (2017). Ammonites and magnetostratigraphy of the Berriasian–Valanginian boundary deposits from eastern Crimea. Geologica Carpathica, 68(6), 505-516. 1335-0552. DOI: https://doi.org/10.1515/geoca-2017-0033
About edition:
Published: 28. 11. 2017
Rights:
CC BY-NC-ND