The demise of the early Eocene greenhouse – Decoupled deep and surface water cooling in the eastern North Atlantic

Author:

Bornemann André,D'haenens Simon,Norris Richard D.,Speijer Robert P.ORCID

Funder

NSF

Deutsche Forschungsgemeinschaft

Fonds Wetenschappelijk Onderzoek

KU Leuven

NSF-OCE

Publisher

Elsevier BV

Subject

Oceanography,Global and Planetary Change

Reference93 articles.

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2. An interpretation of Cretaceous and Tertiary biota in polar-regions;Axelrod;Palaeogeogr. Palaeoclimatol. Palaeoecol.,1984

3. A revised tropical to subtropical Paleogene planktonic foraminiferal zonation;Berggren;J. For. Res.,2005

4. Data report: stable isotope ratios of foraminifers from ODP Leg 207, Sites 1257, 1259, and 1260, and a cleaning procedure for foraminifers in organic-rich shales;Bice;Proc. Ocean Drill. Program Sci. Results,2005

5. Late Paleocene Arctic Ocean shallow-marine temperatures from mollusc stable isotopes;Bice;Paleoceanography,1996

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