Paleogene cooling (55-30 MA) as inferred from oxygen isotope variation within mollusc shells /

Paleogene cooling (c. 50-30 Ma) started sometime in the early-middle Eocene. This was a time when high-latitude and deep-sea temperatures were significantly warmer than today. This cooling culminated during the earliest Oligocene marked by the sudden appearance of a major continental glacier on An...

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Bibliographic Details

Main Author:	Kobashi, Takuro, 1974-
Format:	Thesis eBook
Language:	English
Published:	[Place of publication not identified] : [publisher not identified] ; 2001.
Subjects:	Major geology.
Online Access:	Link to OAKTrust copy