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

Baker, PA; Cronin, TM; DeMartino, DM; Dwyer, Gary; Rodriguez-Lazaro, J

doi:10.1016/S0031-0182(00)00104-8

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.

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.

Collections

Scholarly Articles

More Info

Show full item record

Scholars@Duke

Gary S Dwyer

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.

Articles written by Duke faculty are made available through the campus open access policy. For more information see: Duke Open Access Policy

Rights for Collection: Scholarly Articles