Conflicting reconstructions of Holocene variability of the East Asian summer monsoon
(EASM) from speleothem versus other types of proxy records have yielded widely divergent …

Stalagmite is one kind of secondary carbonates formed in limestone caves (speleothem).
After cave water droplets containing Ca 2+ and HCO _3^-HCO 3− drip onto floor, carbonate …

The Liangzhu culture in the Yangtze River Delta (YRD) was among the world's most
advanced Neolithic cultures. Archeological evidence suggests that the Liangzhu ancient city …

Characterizing the temporal uncertainty in palaeoclimate records is crucial for analysing
past climate change, correlating climate events between records, assessing climate …

In the last two decades, stalagmite oxygen isotope (δ 18 O) records have been widely used
to study the evolution of the paleomonsoon. Nevertheless, interpreting cave δ 18 O records …

Asian summer monsoon (ASM) variability significantly affects hydro-climate, and thus socio-
economics, in the East Asian region, where nearly one-third of the global population resides …

The anthropogenic warming of the Earth's atmosphere is causing dynamical and
thermodynamical changes in the ocean and atmosphere circulation, including the Asian …

Tree-ring cellulose oxygen isotope (δ 18 O) in monsoon Asia (MA) is affected collectively by
local hydroclimate and remote oceanic-atmospheric variations. Variations of tree-ring δ 18 O …

Knowing the behavior of the Asian summer monsoon (ASM) and its global correlation help
understand roles of the ASM in global climate change. Here we synthesize a stalagmite δ 18 …

Although the collapses of several Neolithic cultures in China are considered to have been
associated with abrupt climate change during the 4.2 ka BP event (4.2–3.9 ka BP), the timing …