Two new records from the Amersfoort glacial basin are investigated by means of pollen
analysis. The cores are situated in the deeper part, close to the original Eemian stratotype …

Here we present a multiproxy record (δ 13 C, δ 18 O, major and minor element composition,
mineralogy, and low-resolution biogenic silica content) from a lacustrine succession in the …

We compare multi‐ice core data with δ18O model output for the early last interglacial
Antarctic sea ice minimum. The spatial pattern of δ18O across Antarctica is sensitive to the …

Correlation of individual tephra layers over large areas permits the assessment of eruption
magnitude and synchronization of disparate sedimentary archives. The middle Pleistocene …

Among past interglacial periods, Marine Isotope Stage (MIS) 19 is particularly interesting
because its orbital geometry is very similar to that of the present interglacial. Here we …

Chemical and physical proxy data from a precisely dated early last glacial (∼ 113–110 ka,
MIS5d) Sardinian stalagmite reveal a sub-millennial-scale, cool-dry climate event centered …

Here we investigate the timing of the last glacial loess (L1)-Holocene soil (S0) transition
recorded in loess-paleosol sequences from SE Europe (Ukraine, Romania, Serbia) by …

Although geological and modelling evidence indicate that the last glacial inception in North
America was in NE Canada, little is known about the glacial response of the nearby western …

Relative sea‐level (RSL) evolution during Marine Isotopic Stage (MIS) 5 in the
Mediterranean basin is still not fully understood despite a plethora of morphological …

Our study aims to reconstruct climate changes that occurred at Lake Ohrid (south-western
Balkan Peninsula), the oldest extant lake in Europe, between 160 and 70 ka (covering part …