Palaeolake evolution history has been used to reconstruct the Late Quaternary
environmental and climatic conditions in East Asian monsoon area. In this study, based on …

Climate models suggest that Asian paleoenvironments, monsoons and continental
aridification were primarily governed by tectonic uplift and sea retreat since the Eocene with …

Zhuyeze palaeolake is a terminal lake situated in the arid northern China in the East Asian
monsoon margin. In order to examine the Holocene palaeoclimatic change in the East Asian …

The cold and warm intervals during the Plio‐Pleistocene provide an opportunity to assess
the response of the Asian summer monsoon (ASM) to different levels of global warming. In …

Modern pollen samples from lake sediments, moss polsters or surface soils are commonly
used to interpret fossil pollen records. An increasing number of Holocene pollen records has …

Arid and semi-arid ecosystems are increasingly recognized as important carbon storage
sites. In these regions, extensive sequestration of dissolved inorganic carbon can occur in …

The desert and arid steppes of Mongolia and northern China were geographically central to
the spread of pastoralism and the rise of pastoralist states, but research on the …

Located at the modern junction of the Asian Summer Monsoon and the Westerlies, the
northeastern Tibetan Plateau and western Chinese Loess Plateau are in distinct climatic …

Holocene climate records obtained from the Asian summer monsoon domain suggest a
regionally-delineated response to changing summer monsoon. The interaction between the …

Reconstructing changes in altitudinal vegetation belts is crucial for comprehending
vegetation response to past environmental changes in arid alpine regions, however, proxy …