Processes resulting in the formation of hydrocarbons of carbonaceous c
hondrites and the identity of the interstellar molecular precursors in
volved are an objective of investigations into the origin of the solar
system and perhaps even life on earth. We have combined the resources
and experience of an astronomer and physicists doing laboratory simul
ations with those of a chemical expert in the analysis of meteoritic h
ydrocarbons, in a project that investigated the conversion of polycycl
ic aromatic hydrocarbons (PAHs) formed in stellar atmospheres into alk
anes found in meteorites. Plasma hydrogenation has been found in the U
niversity of Alabama at Birmingham Astrophysics Laboratory to produce
from the precursor PAH naphthalene, a new material having an IR absorp
tion spectrum (Lee, W. and Wdowiak, T.J., Astrophys. J. 417, L49-L51,
1993) remarkably similar to the obtained at Arizona State University o
f the benzene-methanol extract of the Murchison meteorite (Cronin, J.R
. and Pizzarello, S., Geochim. Cosmochim. Acta 54, 2859-2868, 1990). T
here are astrophysical and meteoritic arguments for PAH species from e
xtra-solar sources being incorporated into the solar nebula, where pla
sma hydrogenation is highly plausible. Conversion of PAHs into alkanes
could also have occurred in the interstellar medium. The synthesis of
laboratory analogs of meteoritic hydrocarbons through plasma hydrogen
ation of PAH species is underway, as is chemical analysis of those ana
logs. The objective is to clarify this heretofore uninvestigated proce
ss and to understand its role during the origin of the solar system as
a mechanism of production of hydrocarbon species now found in meteori
tes. Results have been obtained in the form of time-of-flight spectros
copy and chemical analysis of the lab analog prepared from naphthalene
.