INTERVIEW-Southern Ocean being "strangled" by greenhouse
gases
Source: Reuters
By
Michael Byrnes
SYDNEY, Feb 22 (Reuters) - The pristine Southern Ocean, which swirls
around the Antarctic and absorbs vast amounts of carbon dioxide from the
atmosphere, is slowly losing a fight against industrial gases responsible for
global warming, scientists say.
The Southern Ocean's unique wind and storm conditions make it the world's
greatest carbon "sink"; the earth's oceans absorb a third of the carbon dioxide
in the atmosphere, and the Southern Ocean absorbs a third of that.
But the waters that surround Antarctica are becoming more acidic as they
absorb increasing amounts of carbon dioxide produced by nations burning fossil
fuels such as oil, coal and natural gas.
Deforestation and slash-and-burn farming also releases vast amounts of
carbon dioxide stored in timber or peat bogs.
The more acidic an ocean gets, the less carbon dioxide it can soak up.
"It is becoming more difficult for the Southern Ocean to absorb the
excess carbon dioxide," said Dr Will Howard of Australia's Antarctic Climate and
Ecosystems Cooperative Research Centre.
Howard has just returned to the Australian Antarctic and Southern Ocean
Research Programme's base in southern Tasmania state after leading a team of 60
international scientists on a five-week expedition to gather evidence on how
ocean systems are struggling to cope with the build-up of greenhouse gases.
"I would not say it's being killed," Howard said in a telephone
interview. But it is being changed. "And once the system is altered ... it's
going to be a different ecosystem," he said.
Rising acidification of the Southern Ocean has already begun to affect
the ability of plankton -- microscopic marine plants, animals and bacteria -- to
absorb carbon dioxide, scientists have found.
In the sea as on land, plants absorb carbon dioxide from the atmosphere
through photosynthesis. Oceans soak up carbon dioxide from the air and sink it
to the depths.
CHEMISTRY
Microscopic marine organisms also form tiny shells of calcium carbonate,
which sink when they die to also move carbon to the bottom of the sea.
Projections by the Antarctic Climate & Ecosystems Cooperative
Research Centre indicate that some organisms will not be able to make shells
within the next 100 years, Howard said.
"We're talking about timescales of decades to perhaps a century before at
least some of these shell-making organisms are facing an ocean chemistry that
they cannot make shells in."
Scientists from Australia, France, Belgium, the United States and New
Zealand on board the research ship Aurora Australis have just returned from
gathering extensive seawater samples from east of Tasmania, where the warm, east
Australian current mixes with colder Southern Ocean waters.
This is also an area that carries iron-bearing dust blown off the vast,
arid Australian continent into the sea. And iron is seen as part of a possible
solution.
Scientists have discovered that phytoplankton in the Southern Ocean are
deficient in iron, and that some parts of the Southern Ocean are persistently
more fertile than others, probably because they receive extra iron.
So should Australia, the world's largest exporter of iron ore for the
steel mills of Asia, throw its iron ore into the sea to help plankton absorb
excess carbon dioxide?
"It's not so easy to manipulate," Howard said.
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