Orbital and suborbital variability in North Atlantic bottom water temperature obtained from deep-sea ostracod Mg/Ca ratios
Type
Journal articleSubject
deep-ocean circulationmagnesium/calcium ratios
North Atlantic Ocean
ostracod
paleoclimate
Quaternary climates
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https://hdl.handle.net/10161/6479Published Version (Please cite this version)
10.1016/S0031-0182(00)00104-8Publication Info
Cronin, TM; Dwyer, GS; Baker, PA; Rodriguez-Lazaro, J; & DeMartino, DM (2000). Orbital and suborbital variability in North Atlantic bottom water temperature obtained
from deep-sea ostracod Mg/Ca ratios. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 162(1-2). pp. 45-57. 10.1016/S0031-0182(00)00104-8. Retrieved from https://hdl.handle.net/10161/6479.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
Paul A. Baker
Professor of Geochemistry
For the past several years, I have been pursuing the goal of understanding climate
change on time-scales from decades to millions of years. I am particularly interested
in what forces natural climate variability, how past climates have influenced the
ecology and diversity of organisms in the tropics, as well as how climate change and
other human activities will affect the eventual fate of these organisms.
Gary S Dwyer
Sr. Research Scientist and Instructor in Earth and Ocean Sciences
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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