Chinese stalagmite δ18O controlled by changes in the Indian monsoon during a simulated Heinrich event

FSR Pausata, DS Battisti, KH Nisancioglu… - Nature Geoscience, 2011 - nature.com
Carbonate cave deposits in India and China are assumed to record the intensity of monsoon
precipitation, because the δ18O of the carbonate tracks the isotopic signature of …

The chemical index of alteration (CIA) as a proxy for climate change during glacial-interglacial transitions in Earth history

P Wang, Y Du, W Yu, TJ Algeo, Q Zhou, Y Xu, L Qi… - Earth-Science …, 2020 - Elsevier
The glacial-interglacial transitions of ice ages are associated with large, rapid changes in
climate, which potentially can be reconstructed from stratigraphic profiles of the chemical …

East Asian hydroclimate modulated by the position of the westerlies during Termination I

H Zhang, ML Griffiths, JCH Chiang, W Kong, S Wu… - Science, 2018 - science.org
Speleothem oxygen isotope records have revolutionized our understanding of the paleo
East Asian monsoon, yet there is fundamental disagreement on what they represent in terms …

Holocene East Asian summer monsoon records in northern China and their inconsistency with Chinese stalagmite δ18O records

J Liu, J Chen, X Zhang, Y Li, Z Rao, F Chen - Earth-Science Reviews, 2015 - Elsevier
Monsoon precipitation over China exhibits large spatial differences. It has been found that a
significantly enhanced East Asian summer monsoon (EASM) is characterized by increased …