Much of the carbon dioxide we are spewing into the atmosphere is certain to become part of the oceans through some of the same mechanisms. The only question was, When will we see the effects? It is, after all, something of a feat to change the chemistry of something so large as the Pacific Ocean. We are talking about a seriously large body of water here.
On September 11, the Seattle Times published a multimedia masterpiece called Sea Change: The Pacific's Perilous Turn. Apparently, we have managed to pump enough carbon into the atmosphere to change the chemistry of the Pacific.
Ocean acidification, the lesser-known twin of climate change, threatens to scramble marine life on a scale almost too big to fathom.Story by CRAIG WELCH
Photographs by STEVE RINGMAN
"Sea Change" was produced, in part, with funding from the Pulitzer Center on Crisis Reporting.
NORMANBY ISLAND, Papua New Guinea — Katharina Fabricius plunged from a dive boat into the Pacific Ocean of tomorrow.
She kicked through blue water until she spotted a ceramic tile attached to the bottom of a reef.
A year earlier, the Australian ecologist had placed this small square near a fissure in the sea floor where gas bubbles up from the earth. She hoped the next generation of baby corals would settle on it and take root.
Fabricius yanked a knife from her ankle holster, unscrewed the plate and pulled it close. Even underwater the problem was clear. Tiles from healthy reefs nearby were covered with budding coral colonies in starbursts of red, yellow, pink and blue. This plate was coated with a filthy film of algae and fringed with hairy sprigs of seaweed.
Instead of a brilliant new coral reef, what sprouted here resembled a slimy lake bottom.
Isolating the cause was easy. Only one thing separated this spot from the lush tropical reefs a few hundred yards away.
In fact, the water chemistry here is exactly what scientists predict most of the seas will be like in 60 to 80 years.
That makes this isolated splash of coral reef a chilling vision of our future oceans.
‘High rates of extinction’ to come?
Imagine every person on Earth tossing a hunk of CO2 as heavy as a bowling ball into the sea. That’s what we do to the oceans every day.
Burning fossil fuels, such as coal, oil and natural gas, belches carbon dioxide into the air. But a quarter of that CO2 then gets absorbed by the seas — eight pounds per person per day, about 20 trillion pounds a year.
Scientists once considered that entirely good news, since it removed CO2 from the sky. Some even proposed piping more emissions to the sea.
But all that CO2 is changing the chemistry of the ocean faster than at any time in human history. Now the phenomenon known as ocean acidification — the lesser-known twin of climate change — is helping push the seas toward a great unraveling that threatens to scramble marine life on a scale almost too big to fathom, and far faster than first expected.
Here’s why: When CO2 mixes with water it takes on a corrosive power that erodes some animals’ shells or skeletons. It lowers the pH, making oceans more acidic and sour, and robs the water of ingredients animals use to grow shells in the first place.
Acidification wasn’t supposed to start doing its damage until much later this century.
Instead, changing sea chemistry already has killed billions of oysters along the Washington coast and at a hatchery that draws water from Hood Canal. It’s helping destroy mussels on some Northwest shores. It is a suspect in the softening of clam shells and in the death of baby scallops. It is dissolving a tiny plankton species eaten by many ocean creatures, from auklets and puffins to fish and whales — and that had not been expected for another 25 years.
And this is just the beginning.
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