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Evidence for polar porphyrins of bacterial and algal origin in oil shale

Conference · · Am. Chem. Soc., Div. Pet. Chem., Prepr.; (United States)
OSTI ID:5602566
The major part of the porphyrins of the immature Messel oil shale is composed of monocarboxylic acids (C/sub 30/-C/sub 36/) essentially complexed with nickel. These acids were separated as methyl esters by reverse phase h.p.l.c. and nine components characterized by mass and NMR spectroscopy. Structural assignments were supported by synthesis of several members and nuclear Overhauser effect experiments. Besides a major component of the DPEP series, this fraction contained other members belonging to the phyllo- and etioporphyrin series, as well as to a novel chlorophyll C derived series typical of algae. Furthermore the identification of several higher homologues (C/sub 34/-C/sub 36/) of the DPEP series, structurally related to the bacteriochlorophylls, reflects the bacterial input. The characterization of a series of petroporphyrinic acids from the polar fraction of the Messel oil shale confirms the chlorophyllic (a+b,c) origin of these porphyrins. It furthermore implies that most of the characterized petroporphyrins and the survival of carboxylic functions in this class of compounds under mild diagenetic conditions. It furthermore implies that most of the characterized petroporphyrins in Messel shale originate from photosynthetic bacteria and microscopic algae.
Research Organization:
Departement de Chimie, Universite Louis Pasteur 1, rue Blaise Pascal, 67008 Strasbourg
OSTI ID:
5602566
Report Number(s):
CONF-860425-
Conference Information:
Journal Name: Am. Chem. Soc., Div. Pet. Chem., Prepr.; (United States) Journal Volume: 31:2
Country of Publication:
United States
Language:
English