Abstract
Abstract The Paleocene-Eocene boundary is defined on the basis of planktonic foraminifera. The Globorotalia parva zone, the uppermost Paleocene zone, represents the Thanetian, at least in part, or Landenian stage, including the lower part of the Ilerdian stage of Hottinger and Schaub (1960). The G. subbotinae zone, the lowermost Eocene zone, is equivalent to the lower part of the Ypresian, Sparnacian, or Londonian stage, which includes the middle and upper parts of the Ilerdian stage.
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.
