The NASA-sponsored ICESCAPE expedition that discovered the bloom was led
by Stanford
environmental Earth system science Professor Kevin Arrigo.
(Photo: Gert van Dijken)
A massive phytoplankton bloom has been found underneath the Arctic
pack ice in the Chukchi Sea. The under-ice bloom, previously thought
impossible, will require a complete rethinking of Arctic ecosystems –
and is a potent indicator of global warming's effects on the far north.
The 2011 NASA-sponsored ICESCAPE expedition that discovered the bloom was led by Stanford environmental Earth system science Professor Kevin Arrigo. The paper announcing the find appeared today in Science.
Under-ice discovery
Unlike most Arctic research teams, ICESCAPE headed deep into the
Chukchi Sea ice pack, north of the Bering Strait. The research cruise,
consisting of prominent scientists in the fields of oceanography,
biology, chemistry and optics, was intended to improve NASA's remote
monitoring of the Arctic's changing conditions.
"Suddenly, the fluorometer" – the fluorescence-measuring device used
to estimate the algal content of water – "went nuts," Arrigo said. "We
thought there was something wrong with the instrument."
Most models of biological production in the Arctic Ocean assume a
value of zero below pack ice. Sea ice and snow cover have historically
reflected incoming solar radiation, leaving no sunlight for plankton in
the water below.
"Not only was the value not zero," said Arrigo, "production was higher there than it was in open water."
Based on samples from surrounding water and on the species of algae
in the bloom, the scientists confirmed that the phytoplankton had not
drifted under the ice from elsewhere.
Instead, changing ice conditions now allow light to penetrate large
swaths of Arctic sea ice.
Thick "multi-year" ice, which requires several
seasons to accumulate, is on the decline, while warming temperatures
favor thinner "first-year ice." Additionally, the melt pools that now
commonly form on top of Arctic sea ice decrease the ice pack's ability
to reflect light.
The resulting under-ice environment is ideal for Arctic
phytoplankton. The thin ice lets in light while protecting the algae
from ultraviolet radiation.
"Grow rates under the ice are higher than I thought was possible for
Arctic phytoplankton," Arrigo said. Algal cells that would normally take
three days to divide were doubling more than once a day.
A shifting Arctic
While the discovery marks the first direct observation of an
under-ice bloom, the conditions that allow for it in the Chukchi Sea
exist over a large area of the Arctic.
"We suspect that this is a lot more widespread than we realize," said Arrigo.
The appearance of under-ice blooms may presage wholesale shifts in
the ecosystem of the Arctic. Colder-water phytoplankton production, as
with under-ice algae, may cause organic matter to drop to the ocean
floor sooner. The effect would benefit bottom-feeding species, to the
detriment of species that feed in the water column.
And, as algal blooms are able to occur earlier in the year, animals
that depend on timing their behavior to "pulses" in algal productivity
may be left out in the cold.
One piece of seemingly good news is an increase in the Arctic's
ability to sequester carbon. As the Arctic Ocean's productivity
increases, so should its carbon capture rate. But, Arrigo says, the
effect is unlikely to make much difference.
"Even if the amount of CO2 going into the Arctic Ocean doubled, it's a blip on a global scale," he said.
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