The transition on North America from the warm humid Pliocene to the glaciated Quaternary traced by eolian dust deposition at a benchmark North Atlantic Ocean drill site (2014)
Attributed to:
Timing, Causes and Consequences of the Decline in Pliocene pCO2
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1016/j.quascirev.2014.04.005
Publication URI: http://dx.doi.org/10.1016/j.quascirev.2014.04.005
Type: Journal Article/Review
Parent Publication: Quaternary Science Reviews