Greenland’s thaw, which is raising world sea
levels, is also adding about 300,000 metric tonnes of iron a year to the North
Atlantic, based on projections from the study from the muddy melt water of
three glaciers in the southwest. That is similar to the amount of iron blown
into the region as dust by winds. Scientists say that iron is a vital nutrient
and that a lack of the element in parts of the oceans limits growth of
everything from tiny plankton to fish and whales.
“We suggest that glacial runoff serves as a
significant source of bio-available iron to surrounding coastal oceans,” the
scientists, mainly at the US woods Hole Oceanographic Institution (WHOI), wrote
in the journal Nature Geoscience. “We would expect this glacial
contribution of iron to the North Atlantic Ocean
to continue to increase under future warming scenarios”, they added. The
findings show that “as glaciers and ice sheets melt there may be other effects
than just increased sea level,” said Maya Bhatia, who was leader of the study
at WHOI and the Massachusetts Institute of Technology.







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