Absence of a strong, deep-reaching Antarctic Circumpolar Current zonal flow across the Tasmanian gateway during the Oligocene to early Miocene (2022)
Attributed to:
Dynamics of the Oligocene cryosphere: mid-to-high latitude climate variability and ice sheet stability
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