Mid-Pliocene sea level and continental ice volume based on coupled benthic Mg/Ca palaeotemperatures and oxygen isotopes
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http://hdl.handle.net/10161/6586Published Version (Please cite this version)
10.1098/rsta.2008.0222Publication Info
(2009). Mid-Pliocene sea level and continental ice volume based on coupled benthic Mg/Ca palaeotemperatures and oxygen isotopes. PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 367(1886). pp. 157-168. 10.1098/rsta.2008.0222. Retrieved from http://hdl.handle.net/10161/6586.This is constructed from limited available data and may be imprecise. To cite this
article, please review & use the official citation provided by the journal.
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Show full item recordScholars@Duke
Gary Dwyer
Research Scientist, Senior
Dwyer's experience lies in the development of tracers and indicators of environmental
change, and their application to modern and ancient environmental systems. Research
areas include paleoceanography, paleoclimatology, carbonate sedimentology, marine
geology and environmental geochemistry.
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