StarTalk: OSIRIS‑REx, Bennu, and Ingredients for Life 🚀🪨
Hosts & Guest
- Neil deGrasse Tyson (host)
- Chuck Nice (co-host)
- Harold Connolly Jr. — Professor of Geology, Rowan University; Mission Sample Scientist (OSIRIS‑REx)
Episode Focus
- How asteroids/comets preserve early Solar System materials.
- What OSIRIS‑REx found at asteroid Bennu and implications for origins-of-life research.
- Sample-return mission challenges, contamination control, and interdisciplinary science between geologists, chemists, biologists, and astronomers.
OSIRIS‑REx Mission Overview 🛰️
- Acronym: Origins, Spectral Interpretation, Resource Identification, Security/regolith Explorer (tortured acronym).
- Mission type: NASA New Frontiers sample-return.
- Target: Near‑Earth carbonaceous asteroid Bennu (rubble‑pile, ~500 m across, Earth‑crossing → accessible).
- Collection: Touch‑and‑go sampling using nitrogen gas to mobilize surface grains into a collection head.
- Returned to Earth: Sample Return Capsule landed in Utah; total recovered ≈ 121.6 g (goal ≥ 60 g).
Why Sample Asteroids? 🕰️
- Asteroids/comets are time capsules: largely unaltered since Solar System formation (~4.567 billion years).
- Meteorites on Earth are often contaminated (weather, microbes, terrestrial chemicals). Pristine returned samples allow cleaner analyses.
- Carbonaceous chondrite–like bodies contain:
- Volatiles (water, hydrated minerals)
- Organic/prebiotic compounds (amino acids, organics)
- Evaporite minerals (salts) indicating aqueous alteration
Bennu’s Surface & Sampling Challenges ⚠️
- Bennu is a rubble pile with large boulders (some ~11 stories tall), not the fine‑gravel surface expected.
- Sampling incident: some stones jammed the sample head flap and caused sample loss; mission team stowed sample sooner to preserve material.
- The spacecraft penetrated deeper (~48 cm) than anticipated, revealing fresher subsurface material.
Sample Handling & Contamination Control 🧪
- Samples processed in nitrogen‑filled environments to minimize terrestrial contamination.
- Nitrogen chosen due to known purity/isotopic composition and low reactivity with typical minerals.
- Initial examination: visual inspection → microscopy → thin sections → electron microscopy → chemical/organic analyses. Context (rock type, geology) is critical before destructive tests.
Key Scientific Findings & Themes 🔬
- Organic inventory:
- Numerous organic compounds and many amino acids detected (e.g., reports indicate 14–15 of the 20 proteinogenic amino acids).
- RNA‑sugar (ribose) detections reported elsewhere bolster prebiotic chemistry findings.
- Minerals:
- Evaporite minerals (salts) and phosphate minerals found → evidence of aqueous fluids and evaporative concentration processes.
- Discovery of certain minerals (e.g., magnetite/pyrrhotite pathway minerals) informs oxygen‑availability history.
- Geological context matters: aqueous alteration inside parent bodies produced prebiotic chemistry; evaporative processes can concentrate organics (salting out).
Broader Implications for Origin of Life 🌊→🧬
- Asteroids likely delivered prebiotic ingredients (water, organics, phosphates) to early Earth and possibly Mars (lithopanspermia discussions).
- Debate: Are organics on planets produced locally abiotically, or delivered/extraterrestrial? Evidence suggests both are possible; meteoritic/asteroidal inputs are important pieces.
- Making complex biomolecules (e.g., DNA) remains more challenging than producing amino acids; context and repeated geologic processing influence outcomes.
Relation to Other Missions & Samples 🌏🇯🇵
- Hayabusa2 (JAXA) returned samples from carbonaceous asteroid Ryugu (smaller mass returned than Bennu). Cross‑team collaboration and shared findings accelerated interpretations.
- Meteorites on Earth bias sample availability; returned samples (Bennu, Ryugu) provide less-contaminated, context‑rich material.
Planetary Protection & Safety 🛡️
- Asteroid samples considered non‑biological risk (exposed to space radiation for billions of years). Planetary protection protocols primarily prevent sample contamination (not to guard against extraterrestrial pathogens).
- Bennu has a nonzero impact probability in the future (historically cited ~1 in 2,700 chance in 2182); knowing composition helps mitigation planning.
Interdisciplinary Science Takeaway 🤝
- Understanding prebiotic chemistry requires geologists (context), organic chemists (molecules), biologists (life‑process interpretation), and astronomers (target selection & orbital dynamics).
- Shared samples, international collaboration, and peer‑reviewed publications drive robust scientific conclusions.
Miscellanea & Human Notes 🎙️
- Total returned sample mass ≈ 121.6 g (a “cup” of particles) — scientifically valuable despite small mass.
- Samples archived by NASA; ~70% reserved for curation; remaining aliquots distributed to the scientific community after an exclusive analysis period.
- Harold Connolly Jr. to spend time at the Natural History Museum (London) analyzing meteorite collections and lecturing.
Further Resources & Where to Follow Updates
- NASA / JPL mission pages (OSIRIS‑REx) for official updates.
- Peer‑reviewed journals for detailed findings (papers on amino acids, organics, minerals).
- Harold Connolly Jr.’s site: haroldconnolly.wordpress.com (updates/lectures).
Key message: OSIRIS‑REx’s Bennu samples provide high‑quality, context‑preserved material showing water‑related minerals and abundant organics—crucial evidence for understanding prebiotic chemistry and the early Solar System, highlighting the necessity of cross‑disciplinary science.