Rapid climate change in the North Atlantic is reflected in the foraminiferal abundance of the Andaman Sea.

G. rubescens minima and maxima in abundance during warm interstadials (D/O events) and cold stadials, respectively.

D/O events are reflected by high abundances of N. dutertrei indicate strengthened summer monsoon and Ayeyarwady outflow.

Planktic foraminiferal evidence for correlative monsoon changes between Andaman Sea and North Atlantic rapid climate change.

Abundance variation of G. rubescens during the last glacial cycle can be a potential proxy for cold and warm climate