A Zen discovery: Unrusted iron in ocean

A Zen discovery: Unrusted iron in ocean
Iron spewed from hydrothermal vents and carried away by seawater does not rust. Credit: Nicolle Rager-Fuller, National Science Foundation

Iron dust, the gold of the oceans and rarest nutrient for most marine life, can be washed down by rivers or blown out to sea or - a surprising new study finds - float up from the sea floor. The discovery, published online Feb. 8 in Nature Geoscience, connects life at the surface to events occurring at extreme depths and pressures.

The two worlds were long assumed to have little interaction.

A team from the University of Southern California, Woods Hole Oceanographic Institution and Lawrence Berkeley National Laboratory took samples from the East Pacific Rise, a volcanic mid-ocean ridge.

The group found that organic compounds capture some iron spewed by hydrothermal vents, enabling it to be carried away in seawater.

Iron trapped in this way does not rust.

For the scientists, discovering shiny iron in the ocean was like fishing a dry sponge out of a bath.

"Everything we know about the chemical properties of iron tells us that it should be oxidized. It should be rusted," said team leader Katrina Edwards of USC.

The metal's purity has practical value. Aquatic organisms metabolize pure iron much more easily than its rusted form, Edwards said.

How much captured iron floats into surface waters remains unknown. But any that does would nourish ocean life more efficiently than the oxidized iron from regular sources.

"This is one potential mechanism of creating essentially a natural iron fertilization mechanism that's completely unknown," Edwards said.

Some marine scientists have called for iron fertilization because of the metal's crucial place in the aquatic food chain. Iron is the limiting nutrient in most parts of the oceans, meaning that its scarcity is the only thing standing in the way of faster growth.

Iron's equivalent on land is nitrogen. Crop yields rose dramatically during the 20th century in part because of increased nitrogen fertilization.

The expedition team discovered the phenomenon of iron capture serendipitously. Edwards and her collaborators were studying deep-sea bacteria that catalyze the iron rusting reaction.

Of the possible reactions that support microbial communities on rocks, iron oxidation is one of the most important, Edwards explained.

Unfortunately, she added, "it's probably the least well understood major metabolic pathway in the microbial world."

The bacteria involved do not grow well in culture, so the researchers are using a range of molecular techniques to search for genes related to iron oxidation.

One major question involves the importance of bacteria-catalyzed oxidation versus the conventional rusting process. How much of the world's iron is deposited with bacterial help? And how much escapes both bacteria and the natural oxidation process?

The sea floor holds the answer.

The samples were collected continuously using a remote sampling device deployed and retrieved from the research vessel Atlantis between May 16 and June 27, 2006.

Source: University of Southern California


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Feb 08, 2009
Hey! Giant OTEC machines could suction up water from the depths of the ocean and spread nutrients to the top layers of the ocean where iron will fertilize the plankton that can absorb carbon dioxide. Dropping depth charges into the deep oceans will stir up iron laden sediments also. My bet; you heard it here first. contact me at protn7@att.net

Feb 08, 2009
Another argument to use against those who say that fertilization of the oceans with iron is a risky unnatural experiment. We cannot wait for natural process to remove the excessive CO2 we've allowed to accumulate in our atmosphere, even if we stop emitting it tomorrow. We must set up artificial processes to remove the carbon from circulation and iron fertilization of the oceans is emerging as the best way to do this.

Feb 08, 2009
The article fails to make it clear that the 'Woods Hole Oceanographic Institute' is an entirely separate entity , and part of the study.


Feb 09, 2009
anyone find the original article. I am quite skeptical about "pure iron". maybe an iron chelate?

I had thought that iron sulphate breakdown by bacteria had been studied for decades. iron oxidation is of immense economic significance. If bacteria play an important part is is difficult to imagine how or why it has not been studied to date.

KBK
Feb 09, 2009
Alchemy 101.

If you find such a comment either unfathomable, bizarre, or outside your ability to take seriously, then you are not ready for the subject.

When you are serious and real then it will be revealed to you, if you put yourself into it.

It is purposely pitched that way to keep those who do not yet posses the psychology to deal with it - out of it.

What it requires is a stable psychological condition. Dump the monkey-and you may then possibly reach the answers it has always inherently held.

Feb 09, 2009
I'm curious; the AGW naysayers position is that it is not possible for humans to have any appreciable effect on the warming of the earth via CO2 emissions or any other means. If this is so, why are the naysayers not jumping in here to point out how silly it is to think that human action could spread enough billions of tons of iron fertilizer around the vast oceans to have any significant impact whatsoever on CO2 in the atmosphere?

Feb 09, 2009
Lari,
Maybe because the idea of fertilizing the oceans is ludicrous enough not to need naysayers? I don't think you really need to address the CO2 implications of this experiment, the staggering cost of fertilization.

Let's start with some fun math. Volume of the ocean = 1.35 X10^21 Liters of water. lets say a low level fertilization and aim for 10ppm. Or 10mg/L 1.35 X 10^15 Kilograms, For reference that's 1.35 quadrillion kilograms. Or 1,350 billion metric tons.

For those of you keeping track, if we divert the total of the Worlds iron production annually direct to the oceans, then we will have increased the iron content of the oceans by 10 parts per million by 3010AD give or take a couple decades, assuming we don%u2019t run out first.. This does not factor in settling and deposition, or the fact that 10ppm is not really enough to make a difference over the next millenia. If AGW is right the 1000 years might be a little bit long on the time scale don'tcha think?

And to the first tree stump to say we don't need 10ppm, ok, at 100ppb we're still talking about a 10 year project costing the value of the entire world production of iron plus the cost of processing and transportation. For the record 1,350 billion metric tons is going to run in the neighborhood of US$300 Trillion give or take several Trillion, it's hard to be accurate when the rounding error is geting as large as a small countries entire GNP.

Feb 09, 2009
Roach's assumption that the iron level will have to be raised throughout the entire ocean volume is false. Fertilization would only need to take place in the top meter or so of selected areas where iron content is low. Careful targeting would be needed.

Feb 09, 2009
Iron Floats? At a specific gravity of 1.6(ferric sulfate)? That's a neat trick, but Going you are absolutely right, in order to raise the top by the amount that would make a difference we'd probably have to over load the lower portions of the oceans, everything below the top 1 meter by at least double to keep diffusion on our side? Since the majority is below that 1 meter then we can safely say we actually need to dump iron at a rate closer to 1.5 to 2 times the annual global production of iron in order to meet the timeline of 1000 years.

Feb 10, 2009
Microscopic iron dust particles don't float but their viscosity in water will mean they will stay in the top few meters long enough to have an effect on biology. This already happens naturally with wind blown dust particles, a phenomenon that can be studied to ensure we understand the physical processes involved.

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