Abstract
The Paleocene‐Eocene transition is one of the most interesting and intensively investigated time intervals because of the significant changes in global climate and in oceanic circulation that occurred and due to unresolved controversies related to the search for a Global Stratotype Section and Point (GSSP) for the P/E boundary. In order to characterize and understand these changes, numerous sections have been studied in the former Tethys region, an area characterized by sedimentary sequences with fairly continuous sedimentation and rich microfossil contents. The integrated stratigraphy obtained has provided a high-resolution biostratigraphy and important data for paleoenvironmental reconstructions of this time interval. Many of the studied sections are located in Spain (Zumaya, Alamedilla, Caravaca, and Tra
Sign-in/Register to access full text options 
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.
