Greenland ice cores are high-resolution archives of atmospheric dust loadings, and a better
understanding of the driving factors for Greenland ice core dust concentration changes …

Different origins of loess deposits in northern and southern Central Asia are not only
associated with Central Asian topography, but also with aeolian dust dynamics. However …

Our understanding of the climatic teleconnections that drove ice-age cycles has been limited
by a paucity of well-dated tropical records of glaciation that span several glacial–interglacial …

The study of the cultural materials associated with the Neanderthal physical remains from
the sites in the Caucasus, Central Asia and Siberian Altai and adjacent areas documents …

Abstract Marine Isotope Stage (MIS) 4 (ca. 71–57 ka; within the Middle Weichselian
Substage) is considered a significant Pleistocene glaciation, but it remains poorly …

Milankovitch orbital parameters control cycles of insolation, a primary pacer of long term
changes in climate, but exactly how insolation signals are transmitted around the globe in …

Glacial landforms formed by multiple glaciations are well-preserved in the valleys around
Karlik Mountain in the easternmost Tianshan range, Central Asia. These landforms are …

Constraining the timing and extent of past glaciations can help understand how glaciers
respond to climate change as well as study past changes in atmospheric circulation …

The late Quaternary glacier advances in the Himalayan orogen exhibit a complex interplay
of insolation induced changes in summer monsoon and winter westerlies. However, the …

Reconstruction of Pleistocene glacial cycles from oxygen isotope records identifies dramatic
changes in both global climate state and ice sheet size. The Mid-Pleistocene Transition …