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Absence of a strong, deep-reaching Antarctic Circumpolar Current zonal flow across the Tasmanian gateway during the Oligocene to early Miocene (2022)

First Author: Evangelinos D

Attributed to: REVISITING THE NEODYMIUM PARADOX IN THE OCEAN funded by NERC

Abstract

No abstract provided

Bibliographic Information

Digital Object Identifier: http://dx.doi.org/10.1016/j.gloplacha.2021.103718

Publication URI: http://dx.doi.org/10.1016/j.gloplacha.2021.103718

Type: Journal Article/Review

Parent Publication: Global and Planetary Change