The Earth and Moon underwent a late stage bombardment of sizable impactors that some place at approximately 3.9 billion years ago. This activity is evidence by the basalt-filled basins on the Moon. This final phase of appreciable planetary accretion in the inner solar system may have provided water and organ matter to Earth. A chemical and isotopic record of late-stage impactors to the Earth-Moon system is provided by lunar impact melt rocks, which were generated by the basin-forming events. I will review prior work on these rocks and where future work is heading.
Getting Under Europa’s Skin
Tracing Formation and Evolution of Outer Solar System Bodies Through Stable Isotopes and Noble Gas Abundances
Photosynthesis, a Planetary Revolution
Xenon: King of the Gases