Categorized | Sci-Tech

Oceans reveal further impacts of climate change


UAB biologist Jim McClintock, Ph.D., discusses the impacts of ocean acidification.

MEDIA RELEASE / Newswise

The increasing acidity of the world’s oceans – and that acidity’s growing threat to marine species – are definitive proof that the atmospheric carbon dioxide that is causing climate change is also negatively affecting the marine environment, says world-renowned Antarctic marine biologist Jim McClintock, Ph.D., professor in the University of Alabama at Birmingham (UAB) Department of Biology.

“The oceans are a sink for the carbon dioxide that is released into the atmosphere,” says McClintock, who has spent more than two decades researching the marine species off the coast of Antarctica. Carbon dioxide is absorbed by oceans, and through a chemical process hydrogen ions are released to make seawater more acidic.

“Existing data points to consistently increasing oceanic acidity, and that is a direct result of increasing carbon dioxide levels in the atmosphere; it is incontrovertible,” McClintock says. “The ramifications for many of the organisms that call the water home are profound.”

A substance’s level of acidity is measured by its pH value; the lower the pH value, the more acidic is the substance. McClintock says data collected since the pre-industrial age indicates the mean surface pH of the oceans has declined from 8.2 to 8.1 units with another 0.4 unit decline possible by century’s end. A single whole pH unit drop would make ocean waters 10 times more acidic, which could rob many marine organisms of their ability to produce protective shells – and tip the balance of marine food chains.

“There is no existing data that I am aware of that can be used to debate the trend of increasing ocean acidification,” he says.

McClintock and three co-authors collected and reviewed the most recent data on ocean acidification at high latitudes for an article in the December 2009 issue of Oceanography magazine, a special issue that focuses on ocean acidification worldwide.

McClintock also recently published research that revealed barnacles grown under acidified seawater conditions produce weaker adult shells.

ANTARCTICA AS GROUND ZERO FOR CLIMATE CHANGE

McClintock says the delicate balance of life in the waters that surround the frozen continent of Antarctica is especially susceptible to the effects of acidification. The impact on the marine life in that region will serve as a bellwether for global climate-change effects, he says.

“The Southern Ocean is a major global sink for carbon dioxide. Moreover, there are a number of unique factors that threaten to reduce the availability of abundant minerals dissolved in polar seawater that are used by marine invertebrates to make their protective shells,” McClintock says.

“In addition, the increased acidity of the seawater itself can literally begin to eat away at the outer surfaces of shells of existing clams, snails and other calcified organisms, which could cause species to die outright or become vulnerable to new predators.”

One study McClintock recently conducted with a team of UAB researchers revealed that the shells of post-mortem Antarctic marine invertebrates evidenced erosion and significant loss of mass within only five weeks under simulated acidic conditions.

McClintock says acidification also could exert a toll on the world’s fisheries, including mollusks and crustaceans. He adds that the potential loss of such marine populations could greatly alter the oceans’ long-standing food chains and produce negative ripple effects on human industries or food supplies over time.

“So many fundamental biological processes can be influenced by ocean acidification, and the change in the oceans’ makeup in regions such as Antarctica are projected to occur over a time period measured in decades,” McClintock says.

“Evolution simply may be unable to keep up, because it typically takes marine organisms longer periods, hundreds or even thousands of years to naturally adapt,” he says. “But ocean acidification is simply happening too quickly for many species to survive unless we reverse the trend of increasing anthropogenically generated carbon dioxide that is in large part driving climate change.”

An expert on Antarctica who has logged more than two dozen trips to the continent, McClintock’s ongoing research explores the chemical defenses of polar marine organisms and impacts of ocean acidification on marine invertebrates. McClintock Point, located at the entrance of a three-mile stretch of land known as Explorers Cove in Antarctica, was named for the biologist in 1998.

Follow McClintock, fellow UAB research biologist Charles Amsler, Ph.D., and their research team’s upcoming visit to Antarctica from February through May at www.antarctica.uab.edu. Later in 2010 McClintock will lead his third Climate Challenge Education Mission cruise to Antarctica.

One Response to “Oceans reveal further impacts of climate change”

  1. Shame on Dr. McClintock for trying to whip up more climate hysteria now that the whole theory is in retreat. Our harmless emissions of trifling quantities of carbon dioxide cannot possibly acidify the oceans.

    Paper after paper after learned paper in the peer-reviewed literature makes that quite plain. IDSO cites some 150 scientific sources, nearly all of them providing hard evidence, by measurement and experiment, that there is no basis for imagining that we can acidify the oceans to any extent large enough to be measured even by the most sensitive instruments. And, as Richard Feynman used to say, no matter how elegant your t

    heory, no matter how smart you are, if experiment proves you wrong then you need another theory.

    Why can’t rising atmospheric CO2 acidify the oceans?

    First, because it has not done so before. During the Cambrian era, 550 million years ago, there was 20 times as much CO2 in the atmosphere as there is today: yet that is when the calcite corals first achieved algal symbiosis. During the Jurassic era, 175 million years ago, there was again 20 times as much CO2 as there is today: yet that is when the delicate aragonite corals first came into being.

    Secondly, ocean acidification, as a notion, suffers from the same problem of scale as “global warming”. Just as the doubling of CO2 concentration expected this century will scarcely change global mean surface temperature because there is so little CO2 in the atmosphere in the first place, so it will scarcely change the acid-base balance of the ocean, because there is already 70 times as much CO2 in solution in the oceans as there is in the atmosphere. Even if all of the additional CO2 we emit were to end up not in the atmosphere (where it might in theory cause a very little warming) but in the ocean (where it would cause none), the quantity of CO2 in the oceans would rise by little more than 1%, a trivial and entirely harmless change.

    Thirdly, to imagine that CO2 causes “ocean acidification” is to ignore the elementary chemistry of bicarbonate ions. Quantitatively, CO2 is only the seventh-largest of the substances in the oceans that could in theory alter the acid-base balance, so that in any event its effect on that balance would be minuscule. Qualitatively, however, CO2 is different from all the other substances in that it acts as the buffering mechanism for all of them, so that it does not itself alter the acid-base balance of the oceans at all.

    Fourthly, as Professor Ian Plimer points out in his excellent book Heaven and Earth (Quartet, London, 2009), the oceans slosh around over vast acreages of rock, and rocks are pronouncedly alkaline. Seen in a geological perspective, therefore, acidification of the oceans is impossible. McClintock should look for a better scare story if he want to illicit grant funds.

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