Eustatic variations during the Paleocene-Eocene greenhouse world
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منابع مشابه
Early Eocene deep-sea benthic foraminiferal faunas: Recovery from the Paleocene Eocene Thermal Maximum extinction in a greenhouse world
The early Eocene greenhouse world was marked by multiple transient hyperthermal events. The most extreme was the Paleocene-Eocene Thermal Maximum (PETM, ~56 Ma), linked to the extinction of the globally recognised deep-sea benthic foraminiferal Velasco fauna, which led to the development of early Eocene assemblages. This turnover has been studied at high resolution, but faunal development into ...
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ژورنال
عنوان ژورنال: Paleoceanography
سال: 2008
ISSN: 0883-8305
DOI: 10.1029/2008pa001615