It is well established that greenhouse conditions prevailed during the Cretaceous Period (~
145–66 Ma). Determining the exact nature of the greenhouse-gas forcing, climatic warming …

Abstract The Indian Summer Monsoon (ISM) is an inter-hemispheric and highly variable
ocean–atmosphere–land interaction that directly affects the densely populated Indian …

The alkenone‐based U proxy is a cornerstone of paleoclimatology, providing insight into the
temperature history of the Earth's surface ocean. Although the relationship between U and …

The response of the tropical climate in the Indian Ocean realm to abrupt climate change
events in the North Atlantic Ocean is contentious. Repositioning of the intertropical …

The carbon isotopic composition of individual plant leaf waxes (a proxy for C3 vs. C4
vegetation) in a marine sediment core collected from beneath the plume of Sahara-derived …

Abstract The Mg/Ca ratio of planktic foraminifera is a widely used proxy for sea‐surface
temperature but is also sensitive to other environmental factors. Previous work has relied on …

Differential carbon and oxygen stable isotope (δ13C and δ18O) fractionation between
planktonic foraminifera test calcite and sea water related to ecology and life stage confound …

El Niño–Southern Oscillation (ENSO) is a major source of global interannual variability, but
its response to climate change is uncertain. Paleoclimate records from the Last Glacial …

Observed increases in ocean heat content (OHC) and temperature are robust indicators of
global warming during the past several decades. We used high-resolution proxy records …

The eastern equatorial Pacific (EEP) is a source of atmospheric CO2 during the last
deglaciation, but the associated oceanic dynamics in the broader low‐latitude Pacific is not …