Asteroid Bennu reveals a new pathway to life’s chemistry

by Chief Editor

Asteroid Bennu’s Secrets: Rewriting the Story of Life’s Origins

When NASA’s OSIRIS-REx mission delivered samples from asteroid Bennu to Earth in 2023, it wasn’t just a scientific triumph – it was a potential revolution in our understanding of how life began. Initial analysis confirmed the presence of amino acids, the fundamental building blocks of proteins, and DNA. But modern research is challenging long-held assumptions about where and how these crucial molecules formed.

Beyond Warm Water: A New Perspective on Amino Acid Formation

For decades, the prevailing theory suggested amino acids arose through processes like Strecker synthesis, requiring liquid water and moderate temperatures. Still, a recent study led by Penn State scientists, published in the Proceedings of the National Academy of Sciences, suggests a far more diverse and harsher origin story. The chemical signatures within Bennu’s samples indicate amino acids may have formed in extremely cold, radioactive conditions during the solar system’s earliest stages.

Allison Baczynski, assistant research professor of geosciences at Penn State, explains, “Our results flip the script on how we have typically thought amino acids formed in asteroids. It now looks like there are many conditions where these building blocks of life can form, not just when there’s warm liquid water.”

Isotope Analysis: Unlocking Bennu’s Past

The Penn State team focused on glycine, the simplest amino acid, analyzing isotopes – variations in atomic mass – within a teaspoon-sized sample of Bennu material. These subtle differences reveal the conditions under which molecules were created. Their findings suggest glycine on Bennu didn’t originate in warm, watery environments, but rather in frozen ice exposed to radiation in the outer solar system.

This discovery was made possible by specialized instrumentation developed at Penn State, capable of measuring incredibly low abundances of organic compounds. As Baczynski notes, “Without advances in technology and investment in specialized instrumentation, we would have never made this discovery.”

Bennu vs. Murchison: A Tale of Two Asteroids

To contextualize their findings, researchers compared Bennu’s amino acids to those found in the Murchison meteorite, a well-studied carbon-rich space rock that fell in Australia in 1969. The comparison revealed significant differences. Murchison’s amino acids appear to have formed in environments with liquid water and moderate temperatures, conditions also present on early Earth.

Ophélie McIntosh, a postdoctoral researcher at Penn State, highlights the implications: “What’s a real surprise is that the amino acids in Bennu demonstrate a much different isotopic pattern than those in Murchison, and these results suggest that Bennu and Murchison’s parent bodies likely originated in chemically distinct regions of the solar system.”

The Mystery of Mirror Images

The study also uncovered a puzzling anomaly. Amino acids exist in two mirror-image forms. Scientists expected both forms to share the same isotopic signature, but the two versions of glutamic acid in Bennu’s samples exhibited dramatically different nitrogen values. The reason for this discrepancy remains unknown and is a focus of ongoing research.

Future Trends: Expanding the Search for Life’s Building Blocks

The OSIRIS-REx mission and the analysis of Bennu’s sample are just the beginning. Several key trends are emerging in the search for the origins of life:

  • Increased Focus on Diverse Environments: Scientists are now broadening their search beyond traditional “habitable zones” to include icy moons, radiation-exposed regions, and other seemingly inhospitable environments.
  • Advanced Isotope Analysis: Continued development of sophisticated instrumentation will allow for more precise analysis of isotopic signatures, revealing even more subtle clues about the origins of organic molecules.
  • Sample Return Missions: Future missions, like the planned Dragonfly mission to Titan, will bring back samples from other potentially prebiotic environments for detailed study.
  • Comparative Planetology: Comparing the chemistry of different asteroids, comets, and planetary bodies will help scientists understand the distribution of life’s building blocks throughout the solar system.

As Baczynski concludes, “We have more questions now than answers. We hope that we can continue to analyze a range of different meteorites to seem at their amino acids. We want to know if they continue to look like Murchison and Bennu, or maybe there is even more diversity in the conditions and pathways that can create the building blocks of life.”

Frequently Asked Questions

Q: What is the significance of the OSIRIS-REx mission?
A: It’s the first U.S. Mission to collect a sample from an asteroid and return it to Earth, providing scientists with pristine material to study the origins of the solar system and the building blocks of life.

Q: What are amino acids and why are they important?
A: Amino acids are essential molecules that form proteins and are central to nearly every biological process. They are considered fundamental building blocks of life.

Q: What is isotope analysis?
A: It’s a technique used to measure slight differences in the mass of atoms, which can reveal how and where molecules were formed.

Q: What is the Murchison meteorite?
A: A carbon-rich meteorite that fell in Australia in 1969, containing a variety of organic molecules, including amino acids.

Did you know? The sample returned by OSIRIS-REx is the largest extraterrestrial sample returned to Earth since the Apollo missions to the Moon.

Pro Tip: Keep an eye on NASA’s OSIRIS-APEX mission, the repurposed OSIRIS-REx spacecraft, as it prepares to explore asteroid Apophis in 2029.

Want to learn more about the search for life beyond Earth? Explore The Planetary Society’s website for the latest news and discoveries.

Share your thoughts on these groundbreaking findings in the comments below!

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