Foraminifera commonly dominate ocean-floor eukaryotic communities. They also are the
most abundant benthic organisms to be preserved in the post-Paleozoic deep-sea fossil …

A compilation of foraminiferal stable isotope measurements from southern high latitude
(SHL) deep-sea sites provides a novel perspective important for understanding Earth's …

The response of the Earth's biota to global change is of fundamental interest to
paleontologists, but patterns of change in paleontologic data are also of interest to a wider …

Abstract CHANGES in the isotope content of the large marine carbon reservoir can force
shifts in that of the smaller carbon pools in the atmosphere and on land. The carbon isotope …

An up-to-date atlas of an important fossil and living group, with the Natural History Museum.
Deep-sea benthic foraminifera have played a central role in biostratigraphic …

Detailed investigations of high latitude sequences recently collected by the Ocean Drilling
Program (ODP) indicate that periods of rapid climate change often culminated in brief …

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 …

An abrupt episode of global warming marked the end of the Paleocene epoch. Oxygen and
carbon isotope records from two widely separated sites support the notion that degassing of …

We present a global synthesis of the evolution of the climate/ocean system from the late
Campanian at approximately 75 Ma to the end of the Maastrichtian at 65 Ma. This study is …

Deep-sea benthic foraminifera live in the largest habitat on Earth, constitute an important
part of its benthic biomass, and form diverse assemblages with common cosmopolitan …