Tectonic uplift of the Tibetan Plateau (TP) is a major event in the recent geological history of the earth, which produced far-reaching impacts on the Asian and
HDP09 core drilled in Lake Khuvsgul, Mongoria, at 50°52′48″N, 100°26′30″E where the water depth is 222.25 m reached to the depth of ~60 m below lake lfoor
Given the likelihood of future reductions in the strength of the Atlantic Meridional Overturning Circulation (AMOC), it is important to document how changes in
A 13-m long sediment core from Borsog Bay of Lake Khuvsgul, northern Mongolia records hydro-environmental changes during the past 10000 years; three rapid envir