Mid‐Miocene pelagic sedimentary sections can be correlated using intermediate and high
resolution oxygen and carbon isotopic records of benthic foraminifera. Precision of a few …

Abstract 18 O 16 O and 13 C 12 C ratios of Miocene benthic foraminifera from a number of
Atlantic, Pacific and Indian Ocean DSDP sites (71, 77B, 206, 208, 238, 279, 289, 296, 329 …

A search for stable-isotopic signals and biostratigraphic events in Deep Sea Drilling Project
(DSDP) cores to improve chronologic resolution with an aim to reconstruct the …

We have compared detailed planktonic and benthonic foraminiferal carbon and oxygen
isotope records from the Palaeocene and early Eocene successions at DSDP Site 577 …

The middle Miocene δ18O increase represents a fundamental change in the ocean‐
atmosphere system which, like late Pleistocene climates, may be related to deepwater …

Three cycles of δ13C occurred in Oligocene to Miocene benthic and planktonic foraminifera
at western North Atlantic Sites 558 and 563. Intervals of high δ13C occurred at about 35–33 …

High‐resolution stable isotopic records are presented for the epi‐benthic foraminifer
Cibicidoides, the inferred shallow‐dwelling planktonic Globigerinoides quadrilobatus, and …

Benthic foraminiferal oxygen isotopic (δ18O) and carbon isotopic (δ13C) trends, constructed
from compilations of data series from multiple ocean sites, provide one of the primary means …

We examine whether or not a relationship exists between the late Miocene carbon isotope
shift (∼ 7.6–6.6 Ma) and marine productivity at four sites from the Indian and Pacific Oceans …

ABSTRACT ODP Leg 114 recovered sections at four sites east of the Falkland Plateau that
cover a wide range of paleodepths and provide the opportunity to evaluate the response of …