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With Speed and Violence Fred Pearce - Global Commons Institute

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THE ACID BATH<br />

What carbon dioxide does to the oceans<br />

The oceans are the ultimate sink for most of the heat from the sun <strong>and</strong> also<br />

for most of the greenhouse gases we are pouring into the atmosphere. The<br />

atmosphere may be the place in which we live <strong>and</strong> breathe, but for long-term<br />

planetary systems it is just a holding bay. At any one time, there is fifty times<br />

as much carbon dioxide dissolved in ocean waters as there is in the<br />

atmosphere. Given time, the oceans can absorb most of what we can throw<br />

into the atmosphere. But time is what we do not have, <strong>and</strong> the oceans'<br />

patience with our activities may be limited.<br />

Carbon dioxide moves constantly between the oceans' surface <strong>and</strong> the<br />

atmosphere, as the two environments share out the gas. And, because of<br />

ever-rising concentrations in the atmosphere, the oceans currently absorb in<br />

excess of 2 billion tons more a year than they release. Much of that surplus<br />

eventually finds its way to the ocean floor after being absorbed by growing<br />

marine organisms—a process often called the biological pump. Sometimes<br />

there are so many skeletons falling to the depths that biologists call it marine<br />

snow.<br />

Though they are the ultimate sink for most carbon dioxide, the oceans do<br />

not simply absorb any spare carbon dioxide left in the atmosphere. The<br />

relationship is much more dynamic—<strong>and</strong> much less reliable. In the long run,

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