The record of oxygen isotopic variations in foraminifer shells from deep-sea cores preserves
a continuous record of ice volume and sea level oscillations. To extract the ice volume …

Planktonic foraminifer tests are major archives of environmental change and provide a
multitude of proxies in paleoceanography and paleoclimatology. The application of such …

Variations in the strength of the North Atlantic Ocean thermohaline circulation have been
linked to rapid climate changes during the last glacial cycle through oscillations in North …

Stable isotope data from eastern equatorial Pacific (EEP) core TR163‐19 (2° 15′ N, 90°
57′ W, 2348 m) are presented for the surface‐dwelling foraminifers Globigerinoides ruber …

The Milankovitch paradigm links the timing (phase) of ice volume minima to summer
insolation maxima in the hemisphere where ice volume dominates; consistent application of …

Abstract The Mg/Ca ratio in foraminiferal calcite is one of the principal proxies used for
paleoceanographic temperature reconstructions, but recent core-top sediment observations …

Evidence is emerging that the tropical climate system played a major role in global climate
change during the last deglaciation. However, existing studies show that deglacial warming …

The Pliocene was characterized by a gradual shift of global climate toward cooler and drier
conditions. This shift fundamentally reorganized Earth's climate from the Miocene state …

Particulate organic matter collected during a 2‐year period, as part of an ongoing sediment
trap study, and a high‐resolution sediment record from 1850 to 1987 AD from the Santa …

In order to consistently approximate the thermal vertical structure of past upper water
columns, Mg/Ca ratios of eight planktonic foraminiferal species with different preferential …