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Martian meteorite found in the Sahara is 4.1 billion years old

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In short

Researchers analyzing uranium decay in the specimen's zircon crystals determined that Teghaza 001 originated at least 4.1 billion years ago, likely near the southern highlands' Hellas Basin impact crater. Oxygen and hydrogen isotopes trapped inside the rock reveal that liquid water percolated downward from the Martian surface into magma originating from the mantle. While the meteorite confirms early conditions were conducive to microbial life, scientists emphasized that it does not provide definitive evidence that life actually existed.

Key points

  • Chemical signatures within the rock demonstrate that surface water once percolated into t…: Chemical signatures within the rock demonstrate that surface water once percolated into the deeper crust of early Mars.
  • The ancient sample reinforces prevailing scientific theories that the early Martian envir…: The ancient sample reinforces prevailing scientific theories that the early Martian environment was warm, wet, and hospitable to life.
  • Although the specimen verifies that early Mars had life-supporting conditions, it does no…: Although the specimen verifies that early Mars had life-supporting conditions, it does not confirm that living organisms ever formed.

Sources checked by our analysis pipeline: 1

WASHINGTON, Oct 29 : A meteorite found in 2022 in the Sahara in Mali formed in the Martian crust at least 4.1 billion years ago, according to scientists, making the reddish igneous rock perhaps the oldest of the 435 meteorites from Mars known on Earth.

The researchers said the composition of the meteorite, called Teghaza 001, is providing insight into the environment early in the history of Earth's planetary neighbor, with fresh evidence of liquid water on the surface that bolsters the notion that primordial Mars may have been conducive to microbial life.

Planetary scientist Yang Liu of NASA's Jet Propulsion Laboratory in California, which is managed by Caltech, called the meteorite "a witness to a time when Mars was likely warmer and wetter than it has been for most of its history."

The chemistry of the meteorite, a type of coarse-grained rock called gabbro, shows that it experienced interactions with water when it was slowly cooling and crystallizing in the Martian subsurface. It was part of the Martian crust, the planet's outermost layer, but formed from magma originating at…

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