Millennial-scale climate oscillations of the last ice age registered in Greenland and Antarctic
ice cores did not always vary in unison. A striking example is that the strongest Antarctic …

Abstract The European Alps and their forelands provide a range of different archives and
climate proxies for develo** climate records in the time interval 60–8 thousand years (ka) …

This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …

The reasons for the early Holocene temperature discrepancy between northern hemispheric
model simulations and paleoclimate reconstructions—known as the Holocene temperature …

Terrestrial records of past climatic conditions, such as lake sediments and speleothems,
provide data of great importance for understanding environmental changes. However, unlike …

Little is known about the timing and the vegetation dynamics shortly after the Last Glacial
Maximum (LGM) on the Swiss Plateau 19,000–15,000 cal bp. Subsequent Late Glacial and …

High-resolution pollen analyses made on the same samples on which the ratios of oxygen
isotopes were measured that provided the time scale and a temperature proxy after …

It is widely recognised that natural disasters emerge in the interplay between extreme
geophysical events and the human communities affected by them. Whilst detailed natural …

Abstract The Cuerpo de Hombre paleoglacier occupies the upper sector of the Cuerpo de
Hombre river basin, located on the northwest slope of the Sierra de Béjar Mountains (Iberian …

Abstract The Pleistocene-Holocene transition reveals a short and abrupt climatic sequence
from the warming conditions of the Greenland Interstadial-1 (GI-1), followed by the …