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 …

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 …

We report the first high resolution stalagmite record from Indian Central Himalaya by using a
combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the …

Stable isotope records from speleothems provide information on past climate changes, most
particularly information that can be used to reconstruct past changes in precipitation and …

The last glacial period is characterized by abrupt climate oscillations, also known as
Dansgaard-Oeschger (DO) cycles. However, DO cycles remain poorly documented in …

During glacial terminations, massive iceberg discharges and meltwater pulses in the North
Atlantic triggered a shutdown of the Atlantic Meridional Overturning Circulation (AMOC) …

A number of studies proposed a close link between the climate changes in the Asian
summer monsoon (ASM), the Southern Hemisphere (SH), and high latitudes of the Northern …

Cave monitoring is crucial for the interpretation of climatic and environmental significances
of various geological proxies in speleothem. Therefore, the hydrochemical and stable …

The scientific explanation of speleothem δ 18 O in Chinese monsoon region is a greatly
debated issue. Modern cave monitoring combined with instrument observation maybe is an …

摘要石笋是洞穴次生碳酸盐的一种, 是由含Ca 2+ 和HCO3 的洞穴滴水滴到洞穴地面后,
水中碳酸钙在一定条件下过饱和析出, 经年复一年沉积形成. 石笋是古气候研究的重要地质材料 …