Late Maastrichtian Paleocene chronostratigraphy from Seymour Island, James Ross Basin, Antarctic Peninsula: Eustatic controls on sedimentation

The Paleocene (66–56 Ma) was a critical time interval for understanding the geological history in high palaeolatitudes after the end of Cretaceous event (recovery from mass extinction, palaeoclimate, global sea level changes, among others). The sedimentary succession from Seymour Island (Antarctic P...

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Bibliographic Details
Main Authors: Montes, Manuel, Beamud, Elisabet, Nozal, Francisco, Santillana, Sergio
Format: Article in Journal/Newspaper
Language:English
Published: Polar Research Institute of China - PRIC 2019
Subjects:
Online Access:http://library.arcticportal.org/2699/
http://library.arcticportal.org/2699/1/A1903009.pdf