The discovery of fullerenes in the 1.85 billion-year-old Sudbury meteorite crater

Physics

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Fullerenes, Meteorite Craters, Rocks, Carbon 13, Spectroscopic Analysis, Isotopic Enrichment, Time Of Flight Spectrometers, Mass Spectroscopy, Sulfur, Laser Spectroscopy

Scientific paper

Fullerenes (C(60), C(70)) have been identified by laser time-of-flight and electron-ionization mass spectroscopy in rock samples (black tuff in the Onaping formation) from the crater. They were likely synthesized within the impact plume from carbon contained in the meteorite. The isotopic ratios suggest C-13 enrichment. They are associated with sulfur which may have protected them. This is the largest known deposit of naturally occurring fullerenes.

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