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Origin of petroporphyrins. 2. Evidence from stable carbon isotopes

Journal Article · · Energy and Fuels; (USA)
DOI:https://doi.org/10.1021/ef00024a007· OSTI ID:5976310
 [1];  [2]; ;  [3]
  1. Bureau of Mineral Resources, Canberra (Australia)
  2. CSIRO, Menai (Australia)
  3. Indiana Univ., Bloomington (USA)

Compared with the carbon-13 isotopic composition of the ubiquitous C{sub 32}DPEP (DPEP, deoxophylloerythroetioporphyrin) the heavy but equivalent carbon-13 isotopic composition for the porphyrin structures 15(2)-methyl-15,17-ethano-17-nor-H-C{sub 30}DPEP and 15,17-butano-, 13,15-ethano-13(2),17-propano-, and 13(1)-methyl-13,15-ethano-13(2),17-propanoporphyrin suggests a common precursor, presumably chlorophyll c, for these petroporphyrins isolated from the marine Julia Creek oil shale and the lacustrine Condor oil shale. Similarly, the heavy but variable carbon-13 isotopic composition of 7-nor-H-C{sub 31}DPEP compared with C{sub 32}DPEP is consistent with an origin from both chlorophyll b and chlorophyll c{sub 3}. The equivalent carbon-13 isotopic composition for 13(2)-methyl-C{sub 33}DPEP compared with C{sub 32}DPEP suggests a common origin resulting from a weighted average of chlorophyll inputs.

OSTI ID:
5976310
Journal Information:
Energy and Fuels; (USA), Journal Name: Energy and Fuels; (USA) Vol. 4:6; ISSN 0887-0624; ISSN ENFUE
Country of Publication:
United States
Language:
English