All biological amino acids on Earth appear exclusively in their left-handed form, but the reason underlying this observation is elusive.
Meteorites & Asteroids
A Role For Meteoritic Iron In The Emergence Of Life On Earth
To the best of our current knowledge, life on Earth emerged a mere 400 to 700 million years after the Earth itself had formed.
NASA Support for Planetary Sample Science (SPSS) Cooperative Agreement Notice (CAN) and Questions and Answers (Q&A) Released
CAN/Q&A Release Date: May 11, 2023Number: NNH23ZDA017CStep-1 Proposals Due: June 12, 2023Step-2 Proposals Due: July 24, 2023Number: NNH23ZDA017C
Lightning Strike Creates Phosphorus Material For The First Time On Earth
After lightning struck a tree in a New Port Richey neighborhood, a University of South Florida professor discovered the strike led to the formation of a new phosphorus material. It […]
Two Meteorites Are Providing A Detailed Look Into Astrochemistry
If you’ve ever seen a shooting star, you might have actually seen a meteor on its way to Earth. Those that land here are called meteorites and can be used […]
Searching For Life With Space Dust
Following enormous collisions, such as asteroid impacts, some amount of material from an impacted world may be ejected into space.
Uracil Has Been Found In Asteroid Ryugu Samples
Researchers have analyzed samples of asteroid Ryugu collected by the Japanese Space Agency’s Hayabusa2 spacecraft and found uracil—one of the informational units that make up RNA, the molecules that contain […]
Where Did Earth’s Water Come From? Not Melted Meteorites
Water makes up 71 percent of Earth’s surface, but no one knows how or when such massive quantities of it arrived on Earth.
Origin Of Isotopic Diversity Among Carbonaceous Chondrites
Carbonaceous chondrites are some of the most primitive meteorites and derive from planetesimals that formed a few million years after the beginning of the solar system.
Representation Of S-process Abundances For Comparison To Data From Bulk Meteorites
Analysis of bulk meteorite compositions has revealed small isotopic variations due to the presence of material (e.g., stardust) that preserved the signature of nuclear reactions occurring in specific stellar sites. […]
