Optically stimulated luminescence (OSL) signals from quartz can be used to determine when
sedimentary archives were deposited. OSL dating uses the accumulation of energy stored in …

Loess formation generally involves the four main stages of production, deflation,
transportation, and deposition of loess particles. Traditionally, loesses are classified as …

Northeastern Siberia has been inhabited by humans for more than 40,000 years but its deep
population history remains poorly understood. Here we investigate the late Pleistocene …

Our understanding of how global climatic changes are translated into ice-sheet fluctuations
and sea-level change is currently limited by a lack of knowledge of the configuration of ice …

We present a new time‐slice reconstruction of the Eurasian ice sheets (British–Irish,
Svalbard–Barents–Kara Seas and Scandinavian) documenting the spatial evolution of these …

To provide a new reconstruction of the deglaciation of the Fennoscandian Ice Sheet, in the
form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we …

Abstract The Land Use and Cover Area frame Statistical survey (LUCAS) aimed at the
collecting harmonised data about the state of land use/cover over the extent of European …

Evolutionary responses are required for tree populations to be able to track climate change.
Results of 250 years of common garden experiments show that most forest trees have …

The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …

The Periglacial Environment, Fourth Edition, is an authoritative overview of the world's cold,
non-glacial environments. First published in 1976 and subsequently revised in 1996 and …