Wednesday, June 04, 2014

Modern Ocean Acidification Is Outpacing Ancient Upheaval:  Rate May Be Ten Times Faster

Ocean acidification in the modern ocean may already be affecting some marine life, as shown by the partly dissolved shell of this planktic snail, or pteropod, caught off the Pacific Northwest. (Credit: Nina Bednaršedk/NOAA) Click to enlarge.
Scientists estimate that surface ocean acidity increased by about 100 percent during the Paleocene-Eocene Thermal Maximum in a few thousand years or more, and stayed that way for the next 70,000 years. 

Scientists have long suspected that ocean acidification caused the crisis -- similar to today, as humanmade CO2 combines with seawater to change its chemistry.  Now, for the first time, scientists have quantified the extent of surface acidification from those ancient days, and the news is not good: the oceans are on track to acidify at least as much as they did then, only at a much faster rate.

Modern Ocean Acidification Is Outpacing Ancient Upheaval:  Rate May Be Ten Times Faster

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