Pseudo-Oolites in Rocks of the Ulundi Formation, Lower Part of the Archaean Fig Tree Group (South Africa)
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[1] L. Margulis,et al. Primary productivity in an early Archean microbial ecosystem , 1979 .
[2] D. Lowe,et al. The Oldest Marine Carbonate Ooids Reinterpreted as Volcanic Accretionary Lapilli, Onverwacht Group, South Africa , 1978 .
[3] T. Reimer,et al. A sedimentary barite deposit from the Archean Fig Tree Group of the Barberton Mountain Land (South Africa) , 1977 .
[4] D. Lowe,et al. Sedimentology of the Onverwacht Group (3.4 Billion Years), Transvaal, South Africa, and Its Bearing on the Characteristics and Evolution of the Early Earth , 1977, The Journal of Geology.
[5] A. Knoll,et al. Archean microfossils showing cell division from the swaziland system of South Africa. , 1977, Science.
[6] T. Reimer. Paleogeographic significance of the oldest known oolite pebbles in the Archaean Swaziland Supergroup (South Africa) , 1975 .
[7] T. Reimer,et al. Petrology and Geochemistry of Early Precambrian Graywackes from the Fig Tree Group, South Africa , 1970 .
[8] J. Schopf,et al. Alga-Like Fossils from the Early Precambrian of South Africa , 1967, Science.
[9] J. Oró,et al. Aliphatic Hydrocarbons in Pre-Cambrian Rocks , 1967, Nature.
[10] J. Schopf,et al. Microorganisms Three Billion Years Old from the Precambrian of South Africa , 1966, Science.
[11] D. L. Peck,et al. Accretionary Lapilli in Volcanic Rocks of the Western Continental United States , 1962, The Journal of Geology.
[12] J. Ramsay. Structural investigations in the Barberton Mountian land, Eastern Transvaal , 1963 .