Over the past 3.5 million years, there have been several intervals when climate conditions
were warmer than during the pre-industrial Holocene. Although past intervals of warming …

Ancient lakes are among the best archivists of past environmental change, having
experienced more than one full glacial cycle, a wide range of climatic conditions, tectonic …

The last interglaciation (LIG, 129 to 116 thousand years ago) was the most recent time in
Earth's history when global mean sea level was substantially higher than it is at present …

Although detailed age models exist for some marine sediment records of the last glacial
cycle (0–150 ka), age models for many cores rely on the stratigraphic correlation of benthic …

Considerable ambiguity remains over the extent and nature of millennial/centennial-scale
climate instability during the Last Interglacial (LIG). Here we analyse marine and terrestrial …

Sea-level histories during the two most recent deglacial–interglacial intervals show
substantial differences,–despite both periods undergoing similar changes in global mean …

The last interglaciation (~ 130 to 116 ka) is a time period with a strong astronomically
induced seasonal forcing of insolation compared to the present. Proxy records indicate a …

Aim Reconstructing megafauna diversity in the past before anthropogenic impacts is crucial
for develo** targeted restoration strategies. We estimated the diversity and functional …

Few continental palaeoenvironmental sedimentary sequences from Southern Europe are
long enough to span the last interglacial period (Marine Isotopic Stage-MIS 5), the last …

A period of continental ice growth between about 80,000 and 70,000 years ago was
controlled by a decrease in summer insolation, and was among the four largest ice …