Planktic foraminiferal assemblages have been analyzed quantitatively in six DSDP sites in
the Atlantic (Site 363), Pacific (Sites 292, 77B, 277), and Indian Ocean (Sites 219, 253) in …

Quantitative faunal analyses and oxygen isotope ranking of individual planktic foraminiferal
species from deep sea sequences of three oceans are used to make paleoceanographic …

A detailed paleoclimatic investigation was performed on planktonic foraminiferal
assemblages spanning the interval from Zone P21a (late Oligocene) to Zone N5 (early …

Publisher Summary This chapter discusses the key terminal Eocene to Early Oligocene
events. These events were the result of the modification and/or elimination of specialized …

The Paleogene evolutionary records of planktonic foraminifera and larger benthic
foraminifera show parallel patterns in development that may, in part, reflect changes in …

Eocene-Oligocene deep-sea benthonic foraminifera in DSDP Site 277 in the southwest
Pacific have been analyzed to determine the benthonic foraminiferal response to the …

The late middle Eocene is marked by accelerated global cooling, representing part of the
long transitional interval separating the early Eocene 'greenhouse'and later Oligocene …

Reconstruction of Atlantic Ocean vertical and meridional water characteristics is based on
combined synoptic fossil census data, stable isotope records, and measurements of …

ABSTRACT The" Terminal Eocene Event" in the marine realm is comprised of a sequence of
events that record the climate transition from peak early Eocene warmth to cold, glaciated …

The evolution of planktonic foraminifera during the Late Cretaceous is marked in the
Santonian by the disappearance of complex morphotypes (the marginotruncanids), and the …