Originally published June 26, 2024 at NASA.gov. Edits by EarthSky.
- A type of rock mirroring that found at Earthly mid-ocean ridges has been found via analysis of the asteroid Bennu sample returned by NASA’s OSIRIS-REx mission in September 2023.
- The magnesium-sodium phosphate found in the sample hints that the asteroid could have splintered off from a small, ancient, primitive ocean world.
- Japan’s Hayabusa2 mission also delivered an asteroid sample back to Earth, in 2020. It came from asteroid Ryugu, and it revealed a similar phosphate.
Scientists have eagerly awaited the opportunity to dig into the 4.3-ounce (121.6-gram) pristine asteroid Bennu sample collected by NASA’s OSIRIS-REx spacecraft since it was delivered to Earth last fall. They hoped the material would hold secrets of the solar system’s past and the prebiotic chemistry that might have led to life on Earth. An early analysis of the Bennu sample demonstrates this excitement was warranted. A type of rock in the sample hints that the asteroid could have splintered off from a long-gone, tiny, primitive ocean world.
The OSIRIS-REx Sample Analysis Team found that Bennu contains the original ingredients that formed our solar system. The asteroid’s dust is rich in carbon and nitrogen, as well as organic compounds, all of which are essential components for life as we know it. The sample also contains magnesium-sodium phosphate, which was a surprise to the research team, because it wasn’t seen in the remote sensing data collected by the spacecraft at Bennu. Its presence suggests an ocean world origin.
The journal Meteoritics & Planetary Science published this new work on June 26, 2024.
OSIRIS-REx is the first U.S. mission to collect a sample from an asteroid. It was launched on September 8, 2016. The spacecraft traveled to near-Earth asteroid Bennu and collected a sample of rocks and dust from the surface. It delivered the sample to Earth on September 24, 2023.
The spacecraft is currently on its way to infamous asteroid Apophis, which it will reach in April, 2029, just as the asteroid is sweeping past Earth.
Asteroid Bennu sample reveals a phosphate surprise
Analysis of the Bennu sample unveiled intriguing insights into the asteroid’s composition. Dominated by clay minerals, particularly serpentine, the sample mirrors the type of rock found at mid-ocean ridges on Earth, where material from the mantle, the layer beneath Earth’s crust, encounters water.
This interaction doesn’t just result in clay formation; it also gives rise to a variety of minerals like carbonates, iron oxides, and iron sulfides. But the most unexpected discovery is the presence of water-soluble phosphates. These compounds are components of biochemistry for all known life on Earth today.
While a similar phosphate was found in the asteroid Ryugu sample delivered by JAXA’s (Japan Aerospace Exploration Agency) Hayabusa2 mission in 2020, the magnesium-sodium phosphate detected in the Bennu sample stands out for its purity — that is, the lack of other materials in the mineral — and the size of its grains, unprecedented in any meteorite sample.
The finding of magnesium-sodium phosphates in the Bennu sample raises questions about the geochemical processes that concentrated these elements and provides valuable clues about Bennu’s historic conditions. Dante Lauretta, co-lead author of the paper and principal investigator for OSIRIS-REx at the University of Arizona, Tucson, said:
The presence and state of phosphates, along with other elements and compounds on Bennu, suggest a watery past for the asteroid. Bennu potentially could have once been part of a wetter world. Although, this hypothesis requires further investigation.
Jason Dworkin, a co-author on the paper and the OSIRIS-REx project scientist at NASA’s Goddard Space Flight Center in Greenbelt, Maryland, said:
OSIRIS-REx gave us exactly what we hoped: a large pristine asteroid sample rich in nitrogen and carbon from a formerly wet world.
From a young solar system
Despite its possible history of interaction with water, Bennu remains a chemically primitive asteroid, with elemental proportions closely resembling those of our sun. Lauretta said:
The sample we returned is the largest reservoir of unaltered asteroid material on Earth right now.
This composition offers a glimpse into the early days of our solar system, over 4.5 billion years ago. These rocks have retained their original state, having neither melted nor resolidified since their inception, affirming their ancient origins.
Hints at life’s building blocks
The team has confirmed the asteroid is rich in carbon and nitrogen. These elements are crucial in understanding the environments where Bennu’s materials originated, and the chemical processes that transformed simple elements into complex molecules, potentially laying the groundwork for life on Earth. Lauretta said:
These findings underscore the importance of collecting and studying material from asteroids like Bennu — especially low-density material that would typically burn up upon entering Earth’s atmosphere.
This material holds the key to unraveling the intricate processes of solar system formation and the prebiotic chemistry that could have contributed to life emerging on Earth.
What’s next?
Dozens more labs in the United States and around the world will receive portions of the Bennu sample from NASA’s Johnson Space Center in Houston in the coming months. And many more scientific papers describing analyses of the Bennu sample are expected in the next few years from the OSIRIS-REx Sample Analysis Team. Harold Connolly, co-lead author on the paper and OSIRIS-REx mission sample scientist at Rowan University in Glassboro, New Jersey, said:
The Bennu samples are tantalizingly beautiful extraterrestrial rocks. Each week, analysis by the OSIRIS-REx Sample Analysis Team provides new and sometimes surprising findings that are helping place important constraints on the origin and evolution of Earth-like planets.
Bottom line: NASA’s OSIRIS-REx mission delivered a sample of asteroid Bennu to Earth in late 2023. Analysis of the sample shows a type of rock mirroring that found at Earthly mid-ocean ridges.