Abstract
Determines the Sr isotopic composition of seawater during the last 40 Ma. Foraminiferal recrystallization was assessed through scanning electron microscopy (SEM) and Sr/Ca ratios. Foraminifers were shown to be well preserved. Results document that the seawater 87Sr/86Sr has increased continuously but not uniformly, since the latest Eocene. -from Authors
Cite
CITATION STYLE
Hess, J., & Schilling, J. G. (1986). 87Sr/86Sr ratios of planktonic foraminifers and interstitial waters, Deep Sea Drilling Project, Leg 90, Site 593. Initial Reports DSDP, Leg 90, Noumea, New Caledonia to Wellington, New Zealand. Part 2, 1257–1260. https://doi.org/10.2973/dsdp.proc.90.133.1986
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.