Evidence for Porphyrins in the Orgueil Meteorite

@article{Hodgson1964EvidenceFP,
  title={Evidence for Porphyrins in the Orgueil Meteorite},
  author={Gordon W. Hodgson and Bruce L. Baker},
  journal={Nature},
  year={1964},
  volume={202},
  pages={125-131}
}
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AQUEOUS, LOW TEMPERATURE ENVIRONMENT OF THE ORGUEIL METEORITE PARENT BODY
TLDR
The Orgueil meteorite, the principal object of the present investigation, fell a t 8 P.M. on May 14, 1864 and was observed to fall, while the appearance of the luminous meteor, the subsequent detonations and the fall were observed by the local residents. Expand
EVIDENCE IN METEORITES OF FORMER LIFE: THE ORGANIC COMPOUNDS IN CARBONACEOUS CHONDRITES ARE SIMILAR TO THOSE FOUND IN MARINE SEDIMENTS
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Investigations do not support the view that a loss of volatile compounds leads to a depletion of C13 in sedimental organic matter, and it is found that ecology exerts the principal control on terrestrial, organic C13 contents. Expand
Electron Probe Microanalysis of Organized Elements in the Orgueil Meteorite
Electron probe x-ray microanalysis of organized elements in the orgueil carbonaceous meteorite
FURTHER OBSERVATIONS ON THE PROPERTIES OF THE “ORGANIZED ELEMENTS” IN CARBONACEOUS CHONDRITES
TLDR
It is suggested that the Orgueil, Ivuna, Tonk, and Alais carbonaceous meteorites contain indigenous, organic microstructures that seem to be of biogenic origin. Expand
Long-chain fatty acids from the orgueil meteorite
A series of long-chain fatty acids, C 14 −C 30 has been isolated from the Orgueil carbonaceous meteorite. The analysis consisted of the vapor-phase chromatographic separations of the urea adducts ofExpand
OBSERVATIONS ON THE NATURE OF THE “ORGANIZED ELEMENTS” IN CARBONACEOUS CHONDRITES
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