How does rising atmospheric CO2 affect marine organisms?

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Northwestern Arabian Sea
Reference
Gupta, A.K., Das, M. and Anderson, D.M. 2005. Solar influence on the Indian summer monsoon during the Holocene. Geophysical Research Letters 32: doi:10.1029/2005GL022685.

Description
A high-resolution record of variations in the Indian summer monsoon derived from relative abundances of the planktic foraminifer Globigerina bulloides obtained from a sediment core off the coast of Oman in the northwestern Arabian Sea (18°03.08'N, 57°36.56'E) indicated that southwest monsoon winds were stronger during the Medieval Warm Period (AD 800-1300), coincident with a period of high solar activity.