Personally I find the claims of 13000 tonnes to 1 atom of iron somewhat
difficult to comprehend!

A

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Nature doi:10.1038/nature.2012.11028

Dumping iron at sea does sink carbon

Geoengineering hopes revived as study of iron-fertilized algal blooms shows
they deposit carbon in the deep ocean when they die.
Quirin Schiermeier
18 July 2012

In the search for methods to limit global warming, it seems that
stimulating the growth of algae in the oceans might be an efficient way of
removing excess carbon dioxide from the atmosphere after all.

Despite other studies suggesting that this approach was ineffective, a
recent analysis of an ocean-fertilization experiment eight years ago in the
Southern Ocean indicates that encouraging algal blooms to grow can soak up
carbon that is then deposited in the deep ocean as the algae die.

In February 2004, researchers involved in the European Iron Fertilization
Experiment (EIFEX) fertilized 167 square kilometres of the Southern Ocean
with several tonnes of iron sulphate. For 37 days, the team on board the
German research vessel Polarstern monitored the bloom and demise of
single-cell algae (phytoplankton) in the iron-limited but otherwise
nutrient-rich ocean region.

Each atom of added iron pulled at least 13,000 atoms of carbon out of the
atmosphere by encouraging algal growth which, through photosynthesis,
captures carbon. In a paper in Nature today, the team reports that much of
the captured carbon was transported to the deep ocean, where it will remain
sequestered for centuries1 — a 'carbon sink'.

“At least half of the bloom was exported to depths greater than 1,000
metres,” says Victor Smetacek, a marine biologist at the Alfred Wegener
Institute for Polar and Marine Research in Bremerhaven, Germany, who led
the study.

The team used a turbidity meter — a device that measures the degree to
which water becomes less transparent owing to the presence of suspended
particles — to establish the amount of biomass, such as dead algae, that
rained down the water column towards the sea floor. Samples collected
outside the experimental area showed substantially less carbon being
deposited in the deep ocean.
Iron findings

The EIFEX results back up a hypothesis by the late oceanographer John
Martin, who first reported in 1988 that iron deficiency limits
phytoplankton growth in parts of the subarctic Pacific Ocean2. Martin later
proposed that vast quantities of iron-rich dust from dry and sparsely
vegetated continental regions may have led to enhanced ocean productivity
in the past, thus contributing to the drawdown of atmospheric carbon
dioxide during glacial climates3 — an idea given more weight by the EIFEX
findings.

Some advocates of geoengineering think that this cooling mechanism might
help to mitigate present-day climate change. However, the idea of
deliberately stimulating plankton growth on a large scale is highly
controversial. After noting that there were gaps in the scientific
knowledge about this approach, the parties to the London Convention — the
international treaty governing ocean dumping — agreed in 2007 that
‘commercial’ ocean fertilization is not justified (see 'Convention
discourages ocean fertilization').

The finding that ocean fertilization does work, although promising, is not
enough to soothe concerns over potentially harmful side effects on ocean
chemistry and marine ecosystems, says Smetacek. Some scientists fear that
massive ocean fertilization might produce toxic algal blooms or deplete
oxygen levels in the middle of the water column. Given the controversy over
another similar experiment (see 'Ocean fertilization experiment draws
fire'), which critics said should not have been approved in the first
place, the Alfred Wegener Institute will not conduct any further artificial
ocean-fertilization studies, according to Smetacek.

“We just don’t know what might happen to species composition and so forth
if you were to continuously add iron to the sea,” says Smetacek. “These
issues can only be addressed by more experiments including longer-term
studies of natural blooms that occur around some Antarctic islands.”

But some experts argue that artificial ocean-fertilization studies should
not be abandoned altogether. “We are nowhere near the point of recommending
ocean fertilization as a geoengineering tool,” says Ken Buesseler, a
geochemist at the Woods Hole Oceanographic Institution in Massachusetts.
“But just because we don't know all the answers, we shouldn't say no to
further research.”

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