Studies of Cenozoic lacustrine cyclostratigraphy in northeastern Tibet have been successful
in reconstructing the history of precipitation and aridification at astronomical (Milankovitch) …

Reconstructing Cenozoic lacustrine astrochronology is essential for understanding climatic
and environmental change around northeastern Tibetan Plateau. Existing models attribute …

The relationship between the uplift of the Tibetan Plateau and the aridification of eastern
Asia during the middle to late Eocene is still controversial, primarily due to the lack of high …

Abstract The East Asian summer monsoon (EASM) variability on orbital time scale has been
extensively investigated in Quaternary loess and speleothems. However, EASM variability …

Abstract The Early Eocene Climatic Optimum (EECO) may be a potentially useful analog for
future global warming under high CO2 concentrations. However, a paucity of orbital‐scale …

Abstract Knowledge of the variations of aridification during past warm periods can help
predict future aridification trends. However, the variation of aridity during the warm Pliocene …

This study focuses on Holocene monsoon dynamics on the central Tibetan Plateau (TP)
inferred using a sediment record from Lake Nam Co. A high-resolution (decadal) multi-proxy …

Previous climate modeling studies suggest that the surface uplift of the Himalaya–Tibetan
plateau (TP) is a crucial parameter for the onset and intensification of the East Asian …

Variations in the strength of the Asian monsoon during Holocene time are thought to have
been associated with widespread changes in precipitation across much of Tibet. Local …

Qaidam Basin existed as a paleolake at least as early as the Oligocene, which was quite
different from the present-day desert landscape. The paleolake in the basin evolved from its …