Neodymium Evidence for Increased Circumpolar Deep Water Flow to the North Pacific During the Middle Miocene Climate Transition (2018)

First Author: Kender S

Abstract

No abstract provided

Bibliographic Information

Digital Object Identifier: http://dx.doi.org/10.1029/2017pa003309

Publication URI: http://dx.doi.org/10.1029/2017pa003309

Type: Journal Article/Review

Parent Publication: Paleoceanography and Paleoclimatology

Issue: 7

ISSN: 2572-4517