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Microfossils Bitter Springs

Fig. 3-6 Microfossils of several filamentous microorganisms. Bitter Springs Formation, Central Australia. Dated at 0.85 Gyr. (Courtesy William Schopf.)... Fig. 3-6 Microfossils of several filamentous microorganisms. Bitter Springs Formation, Central Australia. Dated at 0.85 Gyr. (Courtesy William Schopf.)...
Fig. 10.1 Cellular, petrified, filamentous microfossils (cyanobacteria) from the Bitter Springs geological formation in central Australia they are about 850 million years old. With kind permission of J. W. Schopf... Fig. 10.1 Cellular, petrified, filamentous microfossils (cyanobacteria) from the Bitter Springs geological formation in central Australia they are about 850 million years old. With kind permission of J. W. Schopf...
Southgate P. (1986) Depositional environment and preservation of microfossils, upper Proterozoic Bitter Springs Formation, Australia. Geology 14, 683-686. [Pg.3578]

Fig. 2. Carbon isotopic values (with error bars) of individual Precambrian microfossils from single stratigraphic horizons of three geologic units measured by ion microprobe mass spectrometry compared with those of the carbonate and total organic carbon measured in bulk samples of the same geologic units. Values plotted for carbonate and total organic carbon are from Strauss and Moore (1992) for microfossils from the Bitter Springs and Gunflint Formations, from House et al (2000) and those for microfossils from the Dresser Formation, from Ueno et al. (2001). Fig. 2. Carbon isotopic values (with error bars) of individual Precambrian microfossils from single stratigraphic horizons of three geologic units measured by ion microprobe mass spectrometry compared with those of the carbonate and total organic carbon measured in bulk samples of the same geologic units. Values plotted for carbonate and total organic carbon are from Strauss and Moore (1992) for microfossils from the Bitter Springs and Gunflint Formations, from House et al (2000) and those for microfossils from the Dresser Formation, from Ueno et al. (2001).

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