Whether or not millennium-scale climate events had occurred in the tropical continent of East Asia during the last glacial period has been a long-term puzzle. In addition, whether those events were affected by the high-latitude atmospheric conditions in the northern hemisphere, or driven by low-latitude oceanic conditions, remains uncertain.
Click here for original story, Phytolith reveals seasonal drought conditions of tropical East Asia during the last 60,000 years
Source: Phys.org