Episodic Ice-Free Arctic Ocean in Pliocene and Pleistocene Time: Calcareous Nannofossil Evidence
THOMAS R. WORSLEY 1 and
YVONNE HERMAN 2
1 Department of Geology, Ohio University, Athens 45701
2 Department of Geology, Washington State University, Pullman 99164
Today's ice cover (2 to 4 meters thick) over the Arctic Ocean provides a shadow that prevents coccolithophorids (photosynthetic, planktonic algae) from living there. Sparse, low-diversity, but indigenous coccolith assemblages in late Pliocene to mid-Pleistocene (but not Holocene) sediments imply deep penetrating warm currents or an ice-free Arctic Ocean, or both, as those layers were being deposited.
Submitted on January 8, 1980
Revised on June 17, 1980