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)

First Author: Lang D
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