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Report
Warns of Rising Carbon Dioxide Threats to Marine Life Ocean
acidification likely to affect coral, other calcium producers
July 5, 2006
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Corals like these on the
undersea Stetson Bank in the Gulf of Mexico are affected by
the increasing acidity of the oceans. Credit: Frank and
Joyce Burek
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Worldwide emissions of
carbon dioxide from fossil fuel burning are dramatically altering
ocean chemistry and threatening marine organisms, including
corals, that secrete skeletal structures and help support ocean
biodiversity.
A report released today
summarizes the known effects of increased atmospheric carbon
dioxide on these organisms, known as marine calcifiers, and
recommends future research for determining the extent of these
impacts.
"It is clear that seawater
chemistry will change in coming decades and centuries in ways
that will dramatically alter marine life," says Joan
Kleypas, the report's lead author and a scientist at the National
Center for Atmospheric Research in Boulder, Colo.
"We're only beginning to
understand the complex interactions between large-scale chemistry
changes and marine ecology," says Kleypas. "It's vital
to develop research strategies to better understand the long-term
vulnerabilities of sensitive marine organisms to these changes."
The report, Impacts
of Ocean Acidification on Coral Reefs and Other Marine Calcifers,
is funded by the National Science Foundation (NSF) and the
National Oceanic and Atmospheric Administration, and is the
result of a workshop hosted by the U.S. Geological Survey's
Integrated Science Center in St. Petersburg, Fla.
"Increasing carbon dioxide
in the atmosphere has had effects in the ocean, where it's
causing increased acidity," says Phil Taylor, director of
NSF's biological oceanography program, which funded the report.
"This increasing acidity has the potential to disrupt the
calcifying processes that lead to coral reef development, for
example, as well as disrupt those same processes in the
microscopic plankton that form the center of the ocean's food
web."
Oceans are naturally alkaline
and are expected to remain so, but the interaction with carbon
dioxide is making them more acidic. The increased acidity lowers
the amount of carbonate in seawater, a building block of the
calcium carbonate that many marine organisms use to grow their
skeletons and create coral reefs. That means these organisms will
grow more slowly, or their skeletons will become less dense,
similar to osteoporosis in humans. As a result, reefs are
threatened because corals may be unable to build them as fast as
erosion wears them away.
"This threat is hitting
coral reefs at the same time that they are being hit by
warming-induced mass bleaching events," says Chris Langdon
at the University of Miami, one of the report's authors. The mass
bleaching occurs when unusually warm temperatures cause the coral
to expel the colorful microscopic algae that provide the coral
polyps with food.
"This is leading to the
most dramatic changes in marine chemistry in at least the past
650,000 years," says Richard Feely, one of the authors and
an oceanographer at NOAA's Pacific Marine Environmental
Laboratory (PMEL) in Seattle.
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The shells of foraminifera,
members of the ocean's cadre of floating plankton species,
may be a casualty of increasing ocean acidification. Credit:
U.S. Geological Survey
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Many calcifying
organisms--including marine plankton such as pteropods, a
planktonic marine snail--are affected by the chemistry changes.
Shelled pteropods are an important food source for salmon,
mackerel, herring and cod. If calcifying organisms such as
pteropods are unable to sustain their populations, many other
species may be affected.
"Decreased calcification
in marine algae and animals is likely to impact marine food webs
may substantially alter the biodiversity and productivity of the
ocean," says Victoria Fabry of California State University
at San Marcos, one of the report's authors.
Several other major ecosystems
supported by organisms that secrete calcium carbonate shells may
be particularly threatened by ocean acidification. These include
cold-water reefs, which are extensive structures that provide
habitat for many important fish species, particularly in the
coastal waters of Alaska.
The report outlines future
research to understand this unusual consequence of climate
change. While scientists cannot yet fully predict how much marine
calcification rates will change in the future, the report warns
that the more critical question to answer is: "What does
this mean for organism fitness and the future of marine
ecosystems?"
Lisa Robbins of the U.S.
Geological Survey's Center for Coastal and Watershed Studies and
Chris Sabine of NOAA's Pacific Marine Environmental Laboratory
also co-authored the report.
Source
/ Credit: NSF
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