Twenty deep-sea sediment cores from the western Pacific between 30° N and 30° S provide
evidence of sea-surface temperature (SST) changes throughout the tropics and subtropics …

Oxygen-isotope compositions of fossilised planktonic and benthic foraminifera tests are
used as proxies for surface-and deep-ocean paleotemperatures, providing a continuous …

Abstract We present a Southwest Pacific Ocean paleothermometry transect using new and
existing foraminiferal Mg/Ca data from six Eocene locations from eastern New Zealand to …

An attempt is made to unravel the dual influences of seawater temperature and isotopic
composition upon the oxygen-isotope records of benthic foraminifers from the deep Pacific …

Sea surface temperature (SST) is a critical variable in the Earth's climate system since it
influences atmospheric circulation, the hydrological cycle and, via ocean surface density …

High resolution (∼ 200 yr sample spacing) records of sea surface temperature for the past
15,000 yr have been inferred from planktonic foraminiferal assemblages in a sediment core …

Mg sea surface temperature (SST) records from different planktonic foraminifera (G.
sacculifer and G. ruber), size fractions, and core depths (1600 and 2600 m) suggest similar …

This study represents an attempt to extract paleoclimatic data from the deep‐sea record by
analyzing foraminiferal shells individually. Using the oxygen (δ18O) and carbon (δ13C) …

Re-examination of sediment cores from Deep Sea Drilling Project (DSDP) Site 277 on the
western margin of the Campbell Plateau (paleolatitude of~ 65° S) has identified an intact …

We present Holocene and last glacial maximum (LGM) oxygen and carbon isotope
measurements on Planulina wuellerstorfi in six southeast Pacific cores. Sedimentation rates …