Following the early Eocene climatic optimum some 50 million years ago, the marine
paleoclimate record indicates that a long interval of global cooling took place, punctuated by …

Lake hydrological change and its driving mechanisms in the Eocene warmhouse climate are
important to evaluating environmental and ecological changes induced by global warming …

In order to study how the Holocene Central Asian climate is coupled to the global climate
system, a 4.24 m long lake core from western Inner Mongolia in China was studied using a …

The middle to late Eocene marked a key transition from greenhouse to coolhouse. However,
a lack of high-resolution and temporally well-constrained continental records hinders our …

Abstract Orbital-scale East Asian summer monsoon (EASM) variability has been extensively
investigated in Pliocene-Quaternary loess and marine sediments. In recent years, middle …

The extent to which climate variability in Central Asia is causally linked to large-scale
changes in the Asian monsoon on varying timescales remains a longstanding question …

East Asian summer monsoon (EASM) precipitation received by northern China over the past
800 thousand years (ky) is characterized by dominant 100-ky periodicity, mainly attributed to …

Orbital-scale global climatic changes during the late Quaternary are dominated by high-
latitude influenced~ 100,000-year global ice-age cycles and monsoon influenced~ 23,000 …

Millennial-scale climate variability has not been well documented in arid northwest China
due to the scarcity of high-resolution, well-dated paleoclimate records. Here we present …

We review Late Cenozoic climate and environment changes in the western interior of China
with an emphasis on lacustrine records from Lake Qinghai. Widespread deposition of red …