Life's history in iron

Life’s history in iron
BIF from the Nuvvuagittuq Supracrustal Belt in Quebec, Canada. This belt contains the oldest supracrustals (sedimentary and volcanic rocks) thus far reported. Credit: Ernesto Percoits

A new study examines how Earth's oldest iron formations could have been formed before oxygenic photosynthesis played a role in oxidizing iron.

Geology tells us a great deal about the history and evolution of on our planet. By studying formations in the , astrobiologists can uncover important clues about the history of habitability on Earth.

Of particular interest to astrobiologists are iron formations, which existed on Earth at key periods in the of life. These are made of layers of material that contain at least 15% iron, which is mixed into layers of quartz or carbonate. Geologists recognize two types of iron formations: the Algoma-type and the larger Superior-type.

Algoma-type formations are linked to volcanism deep in the oceans, whereas Superior-type formations were formed near the shore in continental shelf environments and contain few volcanic rocks.

Superior-type formations first appear on Earth in the Late Archean (2.7 billion years ago) – at the same time the continents began to rise. These formations were huge and prevailed until 2.4 billion years ago (the Early Paleoproterozoic).

At this time, the Earth was undergoing big changes, including oxygenation of the atmosphere. Because the Earth was changing so much, the ways in which superior-type formations were created between 2.7-2.4 billion years ago may have also varied – particularly in respect to the time periods before and after the atmosphere became rich in oxygen and photosynthesis became a dominant process on Earth.

After the rise of oxygen, oxygenic photosynthetic bacteria are thought to have played a big role in the creation of iron formations. But how were iron formations made before advent of oxygenic photosynthesis?

The new study addresses this question by examining how iron deposition could have occurred without biology (a process known as abiological iron deposition).

One mechanism for abiological iron deposition is a reaction in the atmosphere that creates (a well-known powerful oxidant), which can then oxidize ferrous iron in seawater. Researchers modeled how much hydrogen peroxide could have been produced in the Eoarchean atmosphere of the Earth in order to see if this process could have played a major role in creating ancient iron formations.

According to the paper, published in Geobiology, the amount of hydrogen peroxide simply wasn't enough to account for the iron formations we now see in the geological record.

"What we concluded is that, by discounting hydrogen peroxide oxidation, anoxygenic photosynthetic micro-organisms are the most likely mechanism responsible for Earth's oldest ," Ernesto Pecoits of the Université Paris Diderot and lead author on the study told

Microorganisms that photosynthesize in the absence of oxygen assimilate carbon by using iron oxide (Fe(II)) as an electron donor instead of water. While oxygenic photosynthesis produces oxygen in the atmosphere (in the form of dioxygen), anoxygenic adds an electron to Fe(II) to produce Fe(III).

"In other words, they oxidize the iron," explains Pecoits. "This finding is very important because it implies that this metabolism was already active back in the early Archean (ca. 3.8 Byr-ago)."

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More information: Pecoits et al. (2014) "Atmospheric hydrogen peroxide and Eoarchean iron formations." Geobiology, DOI: 10.1111/gbi.12116

This story is republished courtesy of NASA's Astrobiology Magazine. Explore the Earth and beyond at .

Citation: Life's history in iron (2014, November 7) retrieved 14 October 2019 from
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Nov 07, 2014
"What we concluded is that, by discounting hydrogen peroxide oxidation, anoxygenic photosynthetic micro-organisms are the most likely mechanism responsible for Earth's oldest iron formations,"

i don't believe this by a long shot. primordial iron chemistry is probably something far from discoverable with any meaningful level of certainty.

consider that the current leading theory of HYDROCARBON formation is biogenic, and then consider that we've never ruled out life on titan, but yet, we seem to agree that the massive hydrocarbon ocean/atmosphere of tital --extremely rich in hydrocarbons ----was created abiogenically.

primordial abiogenic chemistry is mysterious. the chemistry that occurred was likely predetermined by the unique starting conditions of our particular solar system composition
planetary science is just starting as a field ; we need to learn more about the spectrum of extrasolar planet system chemistry---to be more certain

Nov 08, 2014

The Nuvvuagittuq Supracrustal Belt is (arguably) dated to ~ 4.3 billion years ago [ http://en.wikiped...oarchean ]. This is a full 100 million years after the oldest Jack Hill zircon of ~ 4.4 billion years ago showed a cold early Earth with oceans. And if the Nice 2 model is correct, the survivable impact ratio from the forming planet system would be survivable sometimes before 4.35 billion years ago.

Having anoxygenic photosynthesis (or more likely, a distributed phototrophy that used Fe(II)) that far back ties well in with the evolution over the more soluble Mn when Fe became scarce to today's Mn catalytic photosynthesis. It is also consistent with previous microanalysis that shows that early BIFs were produced that way. [ http://www.scienc...1200711X ]

Nov 08, 2014
@teslaberry: "primordial iron chemistry is probably something far from discoverable with any meaningful level of certainty."

Yet that is what this paper has done, as well as earlier ones. And here is even earlier iron observations mentioned today: .

Nov 09, 2014
Uh oh...The earth's timeline is off again.. Wild guessing to make the numbers jive.
"Quantum" Kudos for a piece that isn't about "Climate Change". Kind of a loser's trophy though, now that the funding to study how believable it is, is going to be dropped ..

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