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 …

This synthesis paper summarizes published proxy climate evidence showing the spatial and
temporal pattern of climate change through the Holocene in Arctic Canada and Greenland …

The rates of subsea permafrost degradation and occurrence of gas-migration pathways are
key factors controlling the East Siberian Arctic Shelf (ESAS) methane (CH4) emissions, yet …

Climate warming threatens to destabilize vast northern permafrost areas, potentially
releasing large quantities of organic carbon that could further disrupt the climate. Here we …

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 …

Multidisciplinary study of a key section on the Laptev Sea Coast (Bykovsky Peninsula, east
Lena Delta) in 1998–2001 provides the most complete record of Middle and Late …

We present a database of late-Quaternary plant macrofossil records for northern Eurasia
(from 23° to 180° E and 46° to 76° N) comprising 281 localities, over 2300 samples and over …

Relative to the past 2,000 years,, the Arctic region has warmed significantly over the past few
decades. However, the evolution of Arctic temperatures during the rest of the Holocene is …

This paper summarizes the results of studies of the Late Weichselian periglacial
environments carried out in key areas of northern Eurasia by several QUEEN teams …