Chlorobiaceae in Palaeozoic seas revealed by biological markers, isotopes and geology

Roger E. Summons*, Trevor G. Powell

*Corresponding author for this work

    Research output: Contribution to journalArticlepeer-review

    233 Citations (Scopus)


    Biomarker hydrocarbons in oils and sediments have considerable potential for assessing the nature of biological processes in the past, but only a few can be uniquely related to particular organisms. Reef-hosted oils in the Silurian of the Michigan Basin, Canada and the Devonian of Western Canada have high abundances of 1-alkyl-2,3,6-trimethylbenzenes. Their precise structures suggest that they are diagenetic products of aromatic carotenoids of the green sulphur bacteria. Individual components are enriched in 13C by 7-8‰ relative to the saturated hydrocarbons of the same oil. An isotopic anomaly of this magnitude and direction correlates with a component of photosynthetic carbon assimilation by the reductive tricarboxylic acid cycle. These results, together with data on palaeoenvironments, provide compelling evidence for the existence, in ancient restricted seas, of microbial communities containing Chlorobiaceae, organisms with distinctive biochemistry which leave morphologically identifiable remains.

    Original languageEnglish
    Pages (from-to)763-765
    Number of pages3
    Issue number6056
    Publication statusPublished - 1986


    Dive into the research topics of 'Chlorobiaceae in Palaeozoic seas revealed by biological markers, isotopes and geology'. Together they form a unique fingerprint.

    Cite this