In the late Paleocene to early Eocene, deep sea benthic foraminifera suffered their only
global extinction of the last 75 million years and diversity decreased worldwide by 30–50 …

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 …

The oxygen isotope record in Paleogene benthic Foraminifera shows that at the base of the
Paleogene the ocean deep waters had a temperature of about 10° C, rising to about 12° C …

Oxygen and carbon isotope ratios in Eocene and Oligocene planktonic and benthic
foraminifera have been investigated from Atlantic, Indian, and Pacific Ocean locations. The …

ABSTRACT Upper Maashichtian through lowermost Eocene deep-sea benthic foraminiferal
records from Maud Rise (Weddell Sea, Antarctica) demonstrate that there was no mass …

A major extinction of intermediate‐water (500–1000 m) benthic foraminiferal species
coincided with a major decrease in δ13C (2.8‰) of terrestrial organic matter (n‐C29 alkane) …

ABSTRACT A mass extinction of deep-sea benthic foraminifera has been documented
globally, coeval with the negative carbon isotope excursion (CIE) at the Paleocene-Eocene …

The Palaeocene–Eocene thermal maximum (PETM) is characterized by a global negative
carbon isotope excursion (CIE) and widespread dissolution of seafloor carbonate …

The last major turnover in deep-sea benthic foraminifera (the Stilostomella extinction) is
documented in detail in six DSDP and ODP sites around New Zealand, South-west Pacific …

Oxygen and carbon isotope measurements on paleontologically inferred" planktonic" and"
benthonic" foraminifera of Late Cretaceous and Early Tertiary age have shown that the" …