Reconstructions of last interglacial (LIG, MIS 5e,∼ 127–117 ka) climate offer insights into the
natural response and variability of the climate system during a period partially analogous to …

Abstract In Eastern Europe Marine Isotope Stage (MIS) 3 represents a period characterised
by severe climate change of very rapid onset, which is recorded in the regional sedimentary …

Proximal evidence of the surface ocean response to size reduction of the Greenland Ice
Sheet (GIS) during the Last Interglacial (MIS5e) and preceding glacial termination (T2) …

Abstract Intensification of the Agulhas Leakage (AL) during glacial terminations has long
been proposed as a necessary mechanism for reverting the Atlantic Meridional Overturning …

Warmer than present Antarctic and Southern Ocean temperatures during the last
interglacial, approximately 128,000 years ago, have been attributed to changes in north …

Last Interglacial (LIG), stable water isotope values (δ 18 O) measured in Greenland deep ice
cores are at least 2.5‰ higher compared to the present day. Previous isotopic climate …

This study explores the climatic variability in the Iberian Peninsula (IP) and its surrounding
seas from 140 to 65 kyr BP. Marine sediment cores and cave speleothems are used to …

Wolbach et al. published two papers on the Younger Dryas Impact Hypothesis (YDIH)—the
paleoenvironmental effects of a purported cosmic impact at the beginning of the Younger …

The current rapid change of the Earth's climate has resulted in an increasing interest for the
past warm periods as potential long-term scenarios of the effects of the present global …

Millennial-scale oscillations are known to be important in the climatic evolution of the Atlantic
basin, but which internal processes originates these oscillations are still uncertain. In this …