Dajiuhu, a rare peatland in Central China, has attracted several studies. There are
differences in the interpretations of its Holocene record, and little has been written on …

The evolution of the East Asian Summer Monsoon (EASM) and its mechanism since the
Holocene remains controversial. Here, we investigate four eolian sediment sequences in the …

South-west China is an important area for determining variability of the SW Asian Monsoon;
it is, however, also tectonically very active. Palaeolimnological studies in this region …

The investigation of two profiles (DYS1 and DYS5) from the Daiyun Mountains in
southeastern China sheds new light on the history of regional climate changes and the …

Hydroclimatic changes over arid central Asia (ACA) are not fully understood, primarily due to
the paucity of accurate, high-resolution climatic records. Here we reconstruct hydroclimatic …

Abstract The East Asian summer monsoon (EASM) significantly influences the precipitation
and vegetation dynamics in that region. Previous studies have assessed the spatial and …

Reconstructing the Mid-Holocene climate change in arid and semiarid areas can help
predict regional moisture availability and resultant lake evolution and vegetation changes …

Reconstructing environmental changes for the last glacial-interglacial cycles in central
China plays a key role in deciphering vegetation history and the evolution of the East Asia …

The interactions between past climate, human activity and environmental change in
subtropical mountainous areas are poorly understood due to the lack of reliable records in …

A 76.7 m-thick section of aeolian sediment is exposed in the transition zone between the Mu
Us Desert and the Loess Plateau of northern China. The aeolian sediments contain sand …