Establishing tropical sea surface temperature (SST) during the Last Glacial Maximum (LGM) is important for constraining equilibrium climate sensitivity to radiative forcing. Until now, there has been little data from central equatorial Pacific in global compilations, with foraminiferal assemblage-based estimates suggesting region was within 1°C of modern temperatures LGM. This stark contrast mu...

Our study focuses on European loess sequences, particularly the eolian intervals in between observed pedogenic units. The classical concept of soil formation from parent material is reformulated to estimate duration and associated sedimentation rate (SR) mass accumulation (MAR) these paleodust intervals. We show that Greenland Stadial (GS) deposits includes thickness overlying unit, which fact ...