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Evidence of iron-eating microbes that existed earlier in Earth’s infancy than previously known offers clues about where and what to look for in seeking signs of life elsewhere in space.

Researchers this week announced the discovery of fossilized remnants that may be the oldest sign of life on Earth, a finding that has implications in the search for life on other planets as well.

Analysis of rock fragments from a rare, primitive piece of Earth’s oceanic crust revealed micrometer-sized tubes and filaments believed to be the remains of iron-eating bacteria that lived between 3.8 billion and 4.3 billion years ago. The bacteria are thought to have lived in hydrothermal vents on the ocean floor, since the fossilized structures resemble those produced by iron-oxidizing bacteria near hydrothermal vents today.

The find, reported in this week’s issue of the journal Nature, pushes back the record of life on Earth to within a few hundred thousand years of the planet’s formation. At that time, Earth likely wasn’t the only planet in solar system that could have supported some form of life.

Scientists have amassed strong evidence that Mars also once had pools of water — perhaps even extensive oceans — as well as a thicker atmosphere and all of the chemical ingredients that are necessary for the development of microbial life.

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“Unlike Earth, and even Venus, there are significant areas on Mars’ ancient surface that are really well preserved and provide great places to search for past habitable environments and the bio-signatures they might contain,” said planetary scientist Jeffrey Johnson with the Johns Hopkins University Applied Physics Lab in Laurel, Maryland.

If the new research holds up to the scrutiny of micropaleontologists, “then it provides an analog for sedimentary systems on Mars where we see silica and iron oxide,” added California Institute of Technology geologist John Grotzinger.

Grotzinger, the former lead scientist for NASA’s Mars Curiosity mission, noted that the rover observed those conditions in what is known as the Murray formation, a geologic layer in Gale Crater that formed from lakebed mud deposits.

“This looks good for Mars,” Grotzinger said.

Finding that ancient life thrived in hydrothermal vents also raises the prospect of life in oceans buried beneath thick layers of ice that cover several moons of Jupiter, Saturn and other giant planets in the outer solar system.

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Jupiter’s Europa and Saturn’s Enceladus, for example, are believed to contain salty oceans in contact with rocky cores — the same sort of chemistry and environmental conditions that may have led to life on Earth.

“Given this new evidence, ancient submarine-hydrothermal vent systems should be viewed as potential sites for the origins of life on Earth, and thus primary targets in the search for extraterrestrial life,” University College London doctoral student Matthew Dodd and colleagues wrote in their Nature article.

While there is no assumption that life beyond Earth, if it exists, would be the same as terrestrial life, it’s a starting point.

“We know how to turn life on Earth into a testable hypothesis,” remarked Shawn Domagal-Goldman, an astrobiologist with NASA’s Goddard Space Flight Center in Greenbelt, at a NASA planetary sciences planning meeting this week.

“The best-known alien biosphere for which we have data is Archean Earth, the ancient Earth,” Domagal-Goldman added. “We now can start to understand how we would look for the signs of life that would have been present on Archean Earth, when there was no oxygen in the atmosphere.”