The maximum limits of the Eurasian ice sheets during four glaciations have been
reconstructed:(1) the Late Saalian (> 140ka),(2) the Early Weichselian (100–80ka),(3) the …

The Eurasian ice-sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …

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 …

While there are numerous hypotheses concerning glacial–interglacial environmental and
climatic regime shifts in the Arctic Ocean, a holistic view on the Northern Hemisphere's late …

Preface the basins of the Arctic Ocean and to present these data in common or parallel
formats. A coherent picture of sediment and organic carbon inputs from the ocean's margins …

The sediment composition of deep-sea cores from the central Arctic Ocean, the Fram Strait,
and the Yermak Plateau was analyzed for several parameters to reconstruct the history of …

Increased public awareness of the global significance of polar regions and opening of the
Russian Arctic to foreign researchers have led to a pronounced intensification of benthic …

Based on field investigations in northern Russia and interpretation of offshore seismic data,
we have made a preliminary reconstruction of the maximum ice‐sheet extent in the Barents …

The pattern of postglacial emergence in the Barents Sea is pivotal to constraining the timing
of deglaciation and extent and thickness of the last ice sheet in northern Eurasia. This review …

It has been proposed that during Pleistocene glaciations, an ice cap of 1 kilometre or greater
thickness covered the Arctic Ocean,,. This notion contrasts with the prevailing view that the …