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A new study by researchers at the University of Bristol and Plymouth Marine Laboratory has shed light on how different species of marine organisms are reacting to ocean acidification.
Since the Industrial Revolution, nearly 30 per cent of all the carbon dioxide produced by manmade emissions has been absorbed by the ocean, causing a drop in pH of ocean surface waters: ocean acidification.
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The current rate of CO2 emissions is unprecedented in the past 65 million years and there are considerable risks for the marine ecosystem all over the globe. The related risks for marine life and the associated consequences for humanity will be discussed at the upcoming Washington Ocean Summit, chaired by US Secretary of State, John Kerry on 16-17 June.
The difficulties in predicting the future of our oceans is, among others, the different response to ocean acidification in closely related species and therefore the inability to generalize physiological effects.
Dr Sophie McCoy (Plymouth) and Dr Federica Ragazzola (Bristol) compared historical material and recent material from crustose coralline algae from a location with fast acidification on the west coast of the United States.
They found that the reaction to ocean acidification in some organisms is driven by their morphology (that is, the form and structure of the organisms and their specific structural features) and therefore, organisms with the same morphology will react the same independently of how closely related the species are.
Photo credit R Greenway, ENN.
Read more at University of Bristol.
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