Revisiting carbonate chemistry controls on planktic foraminifera Mg / Ca: implications for sea surface temperature and hydrology shifts over the Paleocene-Eocene Thermal Maximum and Eocene-Oligocene transition (2016)
Attributed to:
Icehouse tropical climates and plankton evolution
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.5194/cp-12-819-2016
Publication URI: http://dx.doi.org/10.5194/cp-12-819-2016
Type: Journal Article/Review
Parent Publication: Climate of the Past
Issue: 4