The history (45–0 ka BP) of the aquatic vegetation composition of the shallow alpine Lake
Luanhaizi from the NE Tibetan Plateau is inferred from aquatic plant macrofossil frequencies …

Genggahai Lake, a small, shallow water body on the northeastern Qinghai–Tibetan Plateau,
is presently occupied by dense aquatic vegetation. The distribution of macrophytes is …

The influence of the mid-latitude westerlies (MLW) competing with the Asian summer
monsoons (ASM) over the Tibetan Plateau (TP) remains a matter of discussion on how and …

Holocene lake level fluctuations were reconstructed from a 2.7-m sediment core from Nam
Co, Central Tibet, China dating to> 7.2 cal ka BP. Results were compared to existing lake …

Climatic and environmental changes in the northeastern Tibetan Plateau are controlled by
the Asian summer monsoon (ASM) and the westerlies, two key circulation components of the …

Two sediment cores (length 13.94 and 12.93 m) have been drilled from the small alpine
Lake Luanhaizi in the eastern central Qilian Mountains and correlated by means of magnetic …

A multi-proxy investigation of two sediment cores from the large closed-basin Lake Qinghai
provides evidence of abrupt changes in paleolimnological conditions across the late …

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 …

Lake level fluctuations are important features in paleo-reconstructions that can be linked to
past climate changes. Closed-basin lakes on the south-central Tibetan Plateau record the …

The eastern Juyanze palaeolake in hyperarid north-western China (41.75–42° N, 101.5–
102° E) provides evidence of a complex hydrological pattern during the Holocene …