Between a rock and a hard place? A last-ditch approach to slow ocean acidification may involve spreading a mineral along coastlines to suck acidifying protons out of the water.
Earth’s oceans are now 25 per cent more acidic than they were before the industrial revolution, due to excess carbon dioxide in the air dissolving to form carbonic acid. Acidification is threatening a wide range of marine organisms, including corals, mussels, sea urchins and oysters, because it makes it harder for them to build their skeletons and shells.
As a potential solution, Francesc Montserrat of the Royal Netherlands Institute for Sea Research and his colleagues are exploring whether a natural mineral can mop up unwanted acid in seawater.
“We’re trying to put some numbers on the table so that if politicians decide that we need to do this in 10 to 15 years’ time, the research is there and we can say, ‘here are the problems you might be dealing with’,” he says.
Rock to the rescueOlivine is a magnesium silicate mineral that is mainly found in Earth’s subsurface and has been previously suggested as a way to soak up atmospheric CO2. The amounts needed to make a real difference globally are too high, but less of it would be required to reduce ocean acidification locally. When it is placed in seawater, it gradually swaps its magnesium ions for protons, thereby helping to remove acidity.
Montserrat and his colleagues studied this effect in seawater tanks 1 cubic metre in size, which contained living creatures and were designed to mimic the marine ecosystem. When the mineral was ground up and applied as a 1.5 centimetre layer over a base of natural sediment, the pH of the seawater increased by the desired amount, with no adverse effects on life.
However, when a 3 centimetre layer of olivine was used, the lug worms and other marine organisms inhabiting the sediment died. This may be because the pH change was too great, or trace amounts of nickel present in the mineral poisoned the organisms.