An abyssal carbonate compensation depth overshoot in the aftermath of the Palaeocene-Eocene Thermal Maximum (2016)
Attributed to:
Ocean circulation and carbon cycling during Eocene 'greenhouse' warmth
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1038/ngeo2757
Publication URI: http://dx.doi.org/10.1038/ngeo2757
Type: Journal Article/Review
Parent Publication: Nature Geoscience
Issue: 8