Orbital and suborbital variability in North Atlantic bottom water temperature obtained from deep-sea ostracod Mg/Ca ratios

Date
2000-09-15
Authors
Baker, PA
Cronin, TM
DeMartino, DM
Dwyer, Gary
Rodriguez-Lazaro, J
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Type
Journal article
Subject
deep-ocean circulation
magnesium/calcium ratios
North Atlantic Ocean
ostracod
paleoclimate
Quaternary climates
Permalink
https://hdl.handle.net/10161/6479
Published Version (Please cite this version)
10.1016/S0031-0182(00)00104-8
Publication Info
Baker, PA; Cronin, TM; DeMartino, DM; Dwyer, Gary; & Rodriguez-Lazaro, J (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.
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Scholars@Duke

Dwyer

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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