Combined variations of insolation and ice sheet led to major global climatic and ecosystem
changes between the Last Glacial Maximum (LGM) and the Holocene. However, little is …

A number of studies proposed a close link between the climate changes in the Asian
summer monsoon (ASM), the Southern Hemisphere (SH), and high latitudes of the Northern …

The glacial-interglacial variability of precipitation and its driving mechanism in monsoonal
regions has long been a subject of debate. However, there are few records of quantitative …

Our knowledge about the Holocene evolution of the East Asian summer monsoon (EASM)
and its relation to human activities remains incomplete. A detailed palynological …

Spatial differences of rainfall in monsoonal China during the last glacial period remain
contentious. Here, we present new 230 Th-dated stalagmite records (δ 13 C and δ 18 O) …

The Asian summer monsoon is a very important climatic component affecting the land
ecosystem on the eastern Asian continent. Here we assess microbe-derived lipid biomarker …

The use of bacterial branched glycerol dialkyl glycerol tetraethers (brGDGTs) to reconstruct
mean annual air temperatures (MAATs) and environmental pH from soils has sparked …

Here we present multiproxy inorganic geochemical records from a peat core (ZK5) from the
Dajiuhu Basin in central China to investigate peatland deposition processes and …

The relationship between monsoon circulation and regional hydrology in the Yangtze River
Basin since the Last Glacial Maximum (LGM) remains unclear. In this study, we present …

Under the dual influences of high‐intensity anthropogenic activity and climate change,
wetland hydrologic connectivity (HC) has decreased significantly, resulting in the severe …