JMDMT #2655 Microfossils of Cyanobacteria in Carbonaceous Meteorites

The James M. DuPont Meteorite Collection - En 1989 ; clinopyroxene, Wo 646 En 2970 ; penetrate into the specimen. Unlike known lunar meteorites, this olivine, Fo4888 (Fe/Mn ≈ 87 atom%); accessory minerals are Ti-rich lunar rock is a feldspathic crystalline matrix breccia. The most Mg- chromite, ilmenite (36 wt% MgO), Al-Cr-Zr-rich armalcolite, rutile, rich pyroxene is more Mg-rich than those of common lunar regolith troilite, and FeNi metal (137 wt% Ni; 0.22.3 wt% Co); composition breccias and similar to those of 60019, an Apollo 16 breccia containing of the impact melt matrix is SiO2 = 44.0, TiO2 = 0.15, Al2O3 = 29.8, poikilitic clasts. This lunar meteorite differs from other known lunar Cr2O3 = 0.06, FeO = 3.17, MnO = 0.06, MgO = 4.91, CaO = 17.0, meteorites from the Dhofar region, which