Deep water inflow slowed offshore expansion of the West Antarctic Ice Sheet at the Eocene-Oligocene transition (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/10.1038/s43247-022-00369-x
Publication URI: http://dx.doi.org/10.1038/s43247-022-00369-x
Type: Journal Article/Review
Parent Publication: Communications Earth & Environment
Issue: 1