Equatorward phytoplankton migration during a cold spell within the Late Cretaceous super-greenhouse

Oceanic Anoxic Event 2 (OAE2), a  ∼  600 kyr episode close to the Cenomanian–Turonian boundary (ca. 94 Ma), is characterized by relatively widespread marine anoxia and ranks amongst the warmest intervals of the Phanerozoic. The early stages of OAE2 are, however, marked by an episode of widespread tr...

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Bibliographic Details
Main Authors: N. A. G. M. van Helmond, A. Sluijs, N. M. Papadomanolaki, A. G. Plint, D. R. Gröcke, M. A. Pearce, J. S. Eldrett, J. Trabucho-Alexandre, I. Walaszczyk, B. van de Schootbrugge, H. Brinkhuis
Format: Article
Language:English
Published: Copernicus Publications 2016-05-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/13/2859/2016/bg-13-2859-2016.pdf