Orbital and suborbital variability in North Atlantic bottom water temperature obtained from deep-sea ostracod Mg/Ca ratios
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North Atlantic Ocean
Published Version (Please cite this version)10.1016/S0031-0182(00)00104-8
Publication InfoBaker, 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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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.