A molybdenum isotope record of Eocene Thermal Maximum 2: Implications for global ocean redox during the early Eocene (2012)
Attributed to:
Quantifying seawater redox variations and continental weathering rates through the Paleocene-Eocene Thermal Maximum
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1029/2012pa002346
Publication URI: http://dx.doi.org/10.1029/2012pa002346
Type: Journal Article/Review
Parent Publication: Paleoceanography
Issue: 3