Abstract
The calcareous nannoplankton of the Upper Paleocene and Eocene deposits from the Bakhchisaray district of the Southwest Crimea has been studied. It has been compared with the coeval complexes studied earlier and the following zones have been identified: the Kacha Formation corresponds to zones NP6–NP8 (?), the Bakhchisaray Formation is NP12, and the Simferopol Formation is NP13–NP14. According to the species composition, calcareous nannoplankton inhabited the normal salty shelf sea in the tropical belt.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
