Objective Although extensive lakes and eolian sands within and surrounding the Hunshandake Sandy Land(HSL)are sensitive to paleoenvironmental variations in arid and semi-arid eastern Inner Mongolia(e.g.,Yang et al.,20...Objective Although extensive lakes and eolian sands within and surrounding the Hunshandake Sandy Land(HSL)are sensitive to paleoenvironmental variations in arid and semi-arid eastern Inner Mongolia(e.g.,Yang et al.,2013),these records are commonly confined to the last deglaciation,hampering a complete understanding of展开更多
基金supported by the China Geological Survey (grant no. 121201104000150009)the NSFC (grant no. 41672178)
文摘Objective Although extensive lakes and eolian sands within and surrounding the Hunshandake Sandy Land(HSL)are sensitive to paleoenvironmental variations in arid and semi-arid eastern Inner Mongolia(e.g.,Yang et al.,2013),these records are commonly confined to the last deglaciation,hampering a complete understanding of
