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Science 24 February 1967:
Vol. 155. no. 3765, pp. 1003 - 1005
DOI: 10.1126/science.155.3765.1003
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Articles

Fossil Actinomycetes in Middle Precambrian Glacial Varves

Togwell A. Jackson 1

1 Department of Geology, University of Missouri, Columbia

Fossil actinomycetes and other bacteria have been found in sulfide minerals from "varved" argillites in the middle Precambrian Cobalt Series of Canada. The fossils consist of branched and unbranched nonseptate hyphae and chains of rod-shaped cells. The presence of actinomycetes is consistent with the theory that the argillites are lacustrine desposits.


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Stable isotope variations in the Neoproterozoic Beck Spring Dolomite and Mesoproterozoic Mescal Limestone paleokarst: Implications for life on land in the Precambrian.
R. Kenny and L. P. Knauth (2001)
Geological Society of America Bulletin 113, 650-658
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Science. ISSN 0036-8075 (print), 1095-9203 (online)