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第1段

1 .This is Scientific American 60-Second Earth. I'm David Biello. Your minute begins now.

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2 .The oceans are turning acidic.

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3 .Surface waters absorb carbon dioxide produced by the burning of fossil fuels.

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4 .And those CO2 molecules react with the seawater to make carbonic acid.

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5 . Voilà,a more acidic ocean.

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6 .That's big trouble for tiny plants and animals in the sea that make shells.

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7 .Because acidic water makes it harder to produce those shells.

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8 .And once the shells do form, the acidic water also corrodes the shells.

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9 .Many marine biologists have thus been anxious that climate change may mean an end to coral reefs.

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10 .But a set of experiments undertaken in Hawaii, Moorea and Okinawa give new hope, at least in the Pacific.

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11 .Four common corals and algae were subjected to conditions that mimic oceans if CO2 concentrations in the atmosphere reached 1000 ppm, more than double the levels today.

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12 .And three out of the four could still easily form their hard calcium shells even in such an acid ocean.

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13 .That doesn't mean ocean acidification won't be bad for corals and algae.

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14 .But it does mean that across the Pacific some of these organisms can tough it out.

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15 .Whether other organisms, including us humans, could thrive in such a 1000 ppm CO2 world is whole another question.

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16 .Your minute is up, for Scientific American 60-Second Earth. I'm David Biello.

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