James Ross Basin workshop

The rocks of the James Ross Basin consist of a 6 km-thick, relatively complete sequence of Early Cretaceous-Eocene marine sediments, which are remarkably well exposed over Seymour, Vega, James Ross, and Snow Hill islands. Throughout most of the sequence, macrofossils and microfossils are extremely a...

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Bibliographic Details
Published in:Antarctic Science
Main Author: Feldmann, Rodney M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1992
Subjects:
Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
Seymour
Antarctic Science
Online Access:http://dx.doi.org/10.1017/s0954102092000361
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102092000361
Description
Summary:The rocks of the James Ross Basin consist of a 6 km-thick, relatively complete sequence of Early Cretaceous-Eocene marine sediments, which are remarkably well exposed over Seymour, Vega, James Ross, and Snow Hill islands. Throughout most of the sequence, macrofossils and microfossils are extremely abundant and diverse.

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