Ammonites and magnetostratigraphy of the Berriasian–Valanginian boundary deposits from eastern Crimea
2017; De Gruyter Open; Volume: 68; Issue: 6 Linguagem: Inglês
10.1515/geoca-2017-0033
ISSN1336-8052
AutoresArkadiev Vladimir V., Grishchenko Vladimir A., A. Yu. Guzhikov, A. G. Manikin, Savelieva Yuliya N., Carlos A. Ferreira, O. V. Shurekova,
Tópico(s)Geology and Paleoclimatology Research
ResumoAbstract 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.
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