We present planktonic foraminiferal fauna and isotope records from the SE Atlantic that
highlight the nature of millennial‐scale variability over the last 100 kyr. We derive a …

We reconstruct trends in ice volume and deep ocean temperature for the past 108 Myr,
resolving variations on timescales of∼ 2 Myr and longer. We use a sea level record as a …

The carbon dioxide (CO2) content of the atmosphere has varied cyclically between~ 180
and~ 280 parts per million by volume over the past 800,000 years, closely coupled with …

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 …

Different species of benthic Foraminifera taken at the same level in an Atlantic core yielded
different oxygen isotopic values. It was therefore impossible to deduce paleotemperature …

The transition from the extreme global warmth of the early Eocene 'greenhouse'climate∼ 55
million years ago to the present glaciated state is one of the most prominent changes in …

Milankovitch orbital forcing theory has been used to assign time scales to many
paleoclimate records. However, the validity of this theory remains uncertain, and …

Ocean circulation is closely linked to climate change on glacial–interglacial and shorter
timescales. Extensive reorganizations in the circulation of deep and intermediate-depth …

Foraminifera‐based sea surface temperature estimates in the northwest Pacific (Ocean
Drilling Program Site 883; 51° N) varied by 4° C on millennial timescales over the last …

Existing techniques for estimating natural fluctuations of sea level and global ice-volume
from the recent geological past exploit fossil coral-reef terraces or oxygen-isotope records …