As NASA prepares to launch a new Martian probe, a Florida State University scientist has uncovered what may be the first recognized example of ancient Martian crust.
The work of Munir Humayun — a professor in FSU’s Department of Earth, Ocean and Atmospheric Science and a researcher at the National High Magnetic Field Laboratory (MagLab) — is based on an analysis of a 4.4 billion-year-old Martian meteorite that was unearthed by Bedouin tribesmen in the Sahara desert. The rock (NWA 7533) may be the first recognized sample of ancient Martian crust and holds a wealth of information about the origin and age of the Red Planet’s crust.
Humayun’s groundbreaking discoveries about the crust and what it reveals about the Red Planet’s origins will be published in the journal Nature.
In order to detect minute amounts of chemicals in this meteorite, Humayun and his collaborators performed complex analysis on the meteorite using an array of highly sophisticated mass spectrometers in the MagLab’s geochemistry department. High concentrations of trace metals such as iridium, an element that indicates meteoritic bombardment, showed that this meteorite came from the elusive cratered area of Mars’ southern highlands.
“This cratered terrain has been long thought to hold the keys to Mars’ birth and early childhood,” Humayun said.
While craters cover more than half of Mars, this is the first meteoric sample to come from this area and the first time researchers are able to understand Mars’ early crustal growth.
Using the chemical information found in pieces of soil contained in the meteorite, the researchers were able to calculate the thickness of Mars’ crust. Their calculation aligned with estimates from independent spacecraft measurements and confirms that Mars did not experience a giant impact that melted the entire planet in its early history.
Using a powerful microprobe at Curtin University in Perth, Australia, the team dated special crystals within the meteorite — called zircons — at an astounding 4.4 billion years old.
“This date is about 100 million years after the first dust condensed in the solar system,” Humayun said. “We now know that Mars had a crust within the first 100 million years of the start of planet building, and that Mars’ crust formed concurrently with the oldest crusts on Earth and the Moon.”
Humayun and his collaborators hypothesize that these trailblazing discoveries are just the tip of the iceberg of what continued research on this unique meteorite will uncover. Further studies may reveal more clues about the impact history of Mars, the nature of Martian zircons and the makeup of the earliest sediments on the Red Planet.
Source: Florida State University