Stable isotope‐size data of four major planktonic foraminifera lineages from the Paleocene‐
Eocene Thermal Maximum (PETM,~ 56 Ma) at two locations (North Atlantic New Jersey shelf …

Abstract The Mid-Pleistocene Transition (MPT) is characterised by cooling and lengthening
glacial cycles from 600–1200 ka, thought to be driven by reductions in glacial CO2 in …

Abstract Changes in North Atlantic sea surface temperature (SST) are regarded as a key
element of the climate during the Quaternary. However, there are relatively few long‐term …

The oxygen and carbon isotopic ratios of 12 multispecimen samples of different extinct
species of planktonic foraminifer are assessed to establish their relative depth ranking in a …

Benthic foraminifera are the most common meiofaunal unicellular deep-sea biota, forming
skeletons used as proxies for past climate change. We aim to increase understanding of …

We combine stable isotope, calcareous nannoplankton, and benthic foraminiferal records for
Ocean Drilling Program Sites 1262 (paleodepth~ 3,500 m) and 1263 (paleodepth~ 1,500 m) …

We use benthic foraminiferal accumulation rates as a proxy for productivity changes during
the mid-Pleistocene climate transition (MPT)(~ 1.2 Ma to 0.4 Ma). Our data are chosen to test …

The mid-Pleistocene climate transition (MPT) is defined by the emergence of high amplitude,
quasi-100ka glacial–interglacial cycles from a prior regime of more subtle 41kacycles. This …

Abstract The Middle Eocene Climatic Optimum (MECO) is an~ 500 kyr interval of
pronounced global warming from which the climate system recovered in< 50 kyr. The deep …

Carbon isotope records across the Latest Palaeocene Thermal Maximum (LPTM) display by
a remarkable delta 13 C excursion of at least-2.5 per mil that occurred within 10X10 3 yrs …