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Science 17 July 1964: Vol. 145. no. 3629, pp. 262 - 263 DOI: 10.1126/science.145.3629.262
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Articles
Biological Remnants in a Precambrian Sediment
W. G. Meinschein 1,
E. S. Barghoorn 2, and
J. W. Schopf 2
1 Esso Research and Engineering Company, Linden, New Jersey
2 Department of Biology, Harvard University, Cambridge, Massachusetts
A billion-year-old shale from the Nonesuch formation at White Pine Mine, Michigan, contains microfossils, porphyrins, and optically active alkanes. Pristane and phytane, which are isoprenoid hydrocarbons found in living plants and animals, are constituents of the ancient alkanes in the Nonesuch shale; the presence of porphyrins in this Precambrian sediment suggests that photosynthetic organisms have existed for more than a billion years.
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- Electron Microscopy of Fossil Bacteria Two Billion Years Old.
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149, 1365-1367
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- Organic Pigments: Their Long-Term Fate.
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149, 722-726
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- Paleobiology of a Precambrian Shale: Geology, organic geochemistry, and paleontology are applied to the problem of detection of ancient life.
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148, 461-472
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- Hydrocarbons of Biological Origin in Sediments about Two Billion Years Old.
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148, 77-79
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