– This is a long article and you may not be sure you want to read after just reading the teaser section I’ve provided. If you are not sure, go to the end and you’ll find a few quotes from deeper within the article that may pique your interest.
—————————————
by ELIZABETH KOLBERT in The New Yorker magazine
What carbon emissions are doing to the ocean
Pteropods are tiny marine organisms that belong to the very broad class known as zooplankton. Related to snails, they swim by means of a pair of winglike gelatinous flaps and feed by entrapping even tinier marine creatures in a bubble of mucus. Many pteropod species—there are nearly a hundred in all—produce shells, apparently for protection; some of their predators, meanwhile, have evolved specialized tentacles that they employ much as diners use forks to spear escargot. Pteropods are first male, but as they grow older they become female.
Victoria Fabry, an oceanographer at California State University at San Marcos, is one of the world’s leading experts on pteropods. She is slight and soft-spoken, with wavy black hair and blue-green eyes. Fabry fell in love with the ocean as a teen-ager after visiting the Outer Banks, off North Carolina, and took up pteropods when she was in graduate school, in the early nineteen-eighties. At that point, most basic questions about the animals had yet to be answered, and, for her dissertation, Fabry decided to study their shell growth. Her plan was to raise pteropods in tanks, but she ran into trouble immediately. When disturbed, pteropods tend not to produce the mucus bubbles, and slowly starve. Fabry tried using bigger tanks for her pteropods, but the only correlation, she recalled recently, was that the more time she spent improving the tanks “the quicker they died.” After a while, she resigned herself to constantly collecting new specimens. This, in turn, meant going out on just about any research ship that would have her.
Fabry developed a simple, if brutal, protocol that could be completed at sea. She would catch some pteropods, either by trawling with a net or by scuba diving, and place them in one-litre bottles filled with seawater, to which she had added a small amount of radioactive calcium 45. Forty-eight hours later, she would remove the pteropods from the bottles, dunk them in warm ethanol, and pull their bodies out with a pair of tweezers. Back on land, she would measure how much calcium 45 their shells had taken up during their two days of captivity.
In the summer of 1985, Fabry got a berth on a research vessel sailing from Honolulu to Kodiak Island. Late in the trip, near a spot in the Gulf of Alaska known as Station Papa, she came upon a profusion of Clio pyramidata, a half-inch-long pteropod with a shell the shape of an unfurled umbrella. In her enthusiasm, Fabry collected too many specimens; instead of putting two or three in a bottle, she had to cram in a dozen. The next day, she noticed that something had gone wrong. “Normally, their shells are transparent,” she said. “They look like little gems, little jewels. They’re just beautiful. But I could see that, along the edge, they were becoming opaque, chalky.”
Like other animals, pteropods take in oxygen and give off carbon dioxide as a waste product. In the open sea, the CO2 they produce has no effect. Seal them in a small container, however, and the CO2 starts to build up, changing the water’s chemistry. By overcrowding her Cliopyramidata, Fabry had demonstrated that the organisms were highly sensitive to such changes. Instead of growing, their shells were dissolving. It stood to reason that other kinds of pteropods—and, indeed, perhaps any number of shell-building species—were similarly vulnerable. This should have represented a major discovery, and a cause for alarm. But, as is so often the case with inadvertent breakthroughs, it went unremarked upon. No one on the boat, including Fabry, appreciated what the pteropods were telling them, because no one, at that point, could imagine the chemistry of an entire ocean changing.
Since the start of the industrial revolution, humans have burned enough coal, oil, and natural gas to produce some two hundred and fifty billion metric tons of carbon. The result, as is well known, has been a transformation of the earth’s atmosphere. The concentration of CO2 in the air today—three hundred and eighty parts per million—is higher than it has been at any point in the past six hundred and fifty thousand years, and probably much longer. At the current rate of emissions growth, CO2 concentration will top five hundred parts per million—roughly double pre-industrial levels—by the middle of this century. It is expected that such an increase will produce an eventual global temperature rise of between three and a half and seven degrees Fahrenheit, and that this, in turn, will prompt a string of disasters, including fiercer hurricanes, more deadly droughts, the disappearance of most remaining glaciers, the melting of the Arctic ice cap, and the inundation of many of the world’s major coastal cities. But this is only half the story.
Ocean covers seventy per cent of the earth’s surface, and everywhere that water and air come into contact there is an exchange. Gases from the atmosphere get absorbed by the ocean and gases dissolved in the water are released into the atmosphere. When the two are in equilibrium, roughly the same quantities are being dissolved as are getting released. But change the composition of the atmosphere, as we have done, and the exchange becomes lopsided: more CO2 from the air enters the water than comes back out. In the nineteen-nineties, researchers from seven countries conducted nearly a hundred cruises, and collected more than seventy thousand seawater samples from different depths and locations. The analysis of these samples, which was completed in 2004, showed that nearly half of all the carbon dioxide that humans have emitted since the start of the nineteenth century has been absorbed by the sea.
When CO2 dissolves, it produces carbonic acid, which has the chemical formula H2CO3. As acids go, H2CO3 is relatively innocuous—we drink it all the time in Coke and other carbonated beverages—but in sufficient quantities it can change the water’s pH. Already, humans have pumped enough carbon into the oceans—some hundred and twenty billion tons—to produce a .1 decline in surface pH. Since pH, like the Richter scale, is a logarithmic measure, a .1 drop represents a rise in acidity of about thirty per cent. The process is generally referred to as “ocean acidification,” though it might more accurately be described as a decline in ocean alkalinity. This year alone, the seas will absorb an additional two billion tons of carbon, and next year it is expected that they will absorb another two billion tons. Every day, every American, in effect, adds forty pounds of carbon dioxide to the oceans.
Because of the slow pace of deep-ocean circulation and the long life of carbon dioxide in the atmosphere, it is impossible to reverse the acidification that has already taken place. Nor is it possible to prevent still more from occurring. Even if there were some way to halt the emission of CO2 tomorrow, the oceans would continue to take up carbon until they reached a new equilibrium with the air. As Britain’s Royal Society noted in a recent report, it will take “tens of thousands of years for ocean chemistry to return to a condition similar to that occurring at pre-industrial times.”
Humans have, in this way, set in motion change on a geologic scale. The question that remains is how marine life will respond. Though oceanographers are just beginning to address the question, their discoveries, at this early stage, are disturbing.
The complete article is here: ➡
Research thx to LA
Here are a few of LA’s comments on the article:
A recent New Yorker has an article by Elizabeth Kolbert on the
effects of carbon in the oceans. By now we could probably recite the consequences of carbon-loading the atmosphere, but I had never once heard or thought about how it might be affecting the sea. But “nearly half of all the carbon dioxide that humans have emitted since the start of the nineteenth century has been absorbed by the sea.”
This might initially seem like GOOD news. Think what shape the
atmosphere would be in had the oceans not absorbed half the carbon we’ve output! However, the aquatic carbon-loading is far from benign. The main consequence is a change in pH levels. The oceans are alkaline, and the carbon absorption makes them less alkaline, so it’s convenient shorthand (though not strictly accurate) to talk about “ocean acidification.” Research indicates that the changing pH of the oceans will have the following effects:
– Making it more difficult (and at some point impossible) for shellfish to form shells.
– Preventing the growth of coral and endangering the millions of species that depend on coral for habitat
– Killing some kinds of phytoplankton
