Monday, July 4, 2011

Antarctic Krill: study finds krill releases iron, a part of the CO2 absorption process

Krill is one of the primary foundations in the ocean's food chain. And iron is an important component of sea water, involved in the complicated process of absorption of carbon dioxide (CO2) by microscopic plants. These two elements, krill and iron, were brought together in a press release released today from the British Antarctic Survey:

"A new discovery reveals that the shrimp-like creature at the heart of the Antarctic food chain could play a key role in fertilizing the Southern Ocean with iron – stimulating the growth of phytoplankton (microscopic plant-like organisms). This process enhances the ocean's capacity for natural storage of carbon dioxide.

Reporting this month in the journal Limnology and Oceanography, an international team of researchers describe how Antarctic krill (Euphausia superba), once thought to live mostly in surface waters, regularly feed on iron-rich fragments of decaying organisms on the sea floor. They swim back to the surface with stomachs full of iron, releasing it into the water.

Antarctic krill is the staple diet for fish, penguins, seals and whales; and is harvested by commercial fisheries for human consumption.

Lead author from British Antarctic Survey, Dr Katrin Schmidt says, 'We are really excited to make this discovery because the textbooks state krill live mainly in surface waters. We knew they make occasional visits to the sea floor but these were always thought as exceptional. What surprises us is how common these visits are – up to 20% of the population can be migrating up and down the water column at any one time.'

The scientists painstakingly examined the stomach contents of over 1000 krill collected from 10 Antarctic research expeditions. They found that the krill, caught near the surface, had stomachs full of iron-rich material from the seabed. The team also studied photographs of krill on the sea floor, acoustic data and net samples. All these provided strong evidence that these animals frequently feed on the sea floor.

This finding has implications for managing commercial krill fisheries and will lead to a better understanding of the natural carbon cycle in the Southern Ocean."

Iron is known to enter the seas through the upwellings of deep sediments, run-off and wind-blown dust from land, and melting icebergs. Iron stimulates plankton growth which, in turn, takes in CO2. Dying plankton settle on the bottom thereby capturing and holding the CO2 - and the iron. This new study indicates that krill may also be a vital component in the recycling of iron, thereby stimulating plankton growth, and the CO2 absorption cycle is further stimulated.

The need for managing commercial krill fisheries to ensure a healthy food cycle for a variety of sealife in the Southern Ocean is now given extra importance based on what disruptions could occur to the carbon cycle should krill be over-harvested.

Read the press release from the British Antarctic Survey.

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