Dynamics of sediment flux to a bathyal continental margin section through the Paleocene-Eocene Thermal Maximum (2018)
Attributed to:
Reducing Greenhouse Climate Proxy Uncertainty
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.5194/cp-14-1035-2018
Publication URI: http://dx.doi.org/10.5194/cp-14-1035-2018
Type: Journal Article/Review
Parent Publication: Climate of the Past
Issue: 7
ISSN: 18149332 18149324