Mid-cretaceous sedimentary core (IMAGE) Northwestern University Caption Sediment core from the eastern Indian Ocean, offshore of southwest Australia. Lighter colored sedimentary rocks (below right) are rich in carbonate microfossils deposited before the ocean acidification event, and darker mudstones (left) represent the time interval when ocean acidification occurred. These stones are darker due to the absence of carbonate microfossils caused by more corrosive seawater during the acidification event. Credit Matt Jones Usage Restrictions Add credit License Original content Disclaimer: AAAS and EurekAlert! are not responsible for the accuracy of news releases posted to EurekAlert! by contributing institutions or for the use of any information through the EurekAlert system.