John Inge Svendsen

TL;DR: In this paper, the maximum limits of the Eurasian ice sheets during four glaciations have been reconstructed: (1) the Late Saalian (>140 ka), (2) the Early Weichselian (100-80 ka),(3) the Middle Weichsellian (60-50 ka), and (4) the late Weichselsian (25-15 ka) based on satellite data and aerial photographs combined with geological field investigations in Russia and Siberia, and with marine seismic and sediment core data.

TL;DR: In this paper, the authors 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 interconnected ice sheets every 1000 years from 25 to 10 years and at four selected time periods back to 40 years.

TL;DR: This paper reviewed the geological observations and interpretations regarding the size and timing of the Late Weichselian Barents ice sheet, combined with numerical modelling of its formation in order to produce a reconstruction of ice sheet extent and behaviour.

TL;DR: In this article, the authors reconstructed large ice-dammed lakes with reversed outlets, e.g. toward the Caspian Sea, based on numerous optically stimulated luminescence (OSL) dates for the periods 90-80 and 60-50 ka.

TL;DR: In this article, the authors made a preliminary reconstruction of the maximum ice-sheet extent in the Barents and Kara Sea region during the Early/Middle Weichselian and the Late Weichsellian.