1987
DOI: 10.17741/bgsf/59.2.001
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Fossil bacterial forms in Early Proterozoic dolomite at Kiihtelysvaara in eastern Finland

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(13 citation statements)
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“…Therefore, we used part of the original specimen and prepared a new HF-HC1 acid residue, which was mounted on epoxy and polished for analysis by electron microprobe. Figure 1 shows that the microfossil-like objects analysed from the new grain mount correspond to the description and figures in Tynni and Sarapää (1987). In figure 2 these objects are seen between crossed polarizers in the original grain mount (GSF-760) studied by Tynni and Sarapää (1987).…”
Section: Geologic Setting and Sample Materialsmentioning
confidence: 58%
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“…Therefore, we used part of the original specimen and prepared a new HF-HC1 acid residue, which was mounted on epoxy and polished for analysis by electron microprobe. Figure 1 shows that the microfossil-like objects analysed from the new grain mount correspond to the description and figures in Tynni and Sarapää (1987). In figure 2 these objects are seen between crossed polarizers in the original grain mount (GSF-760) studied by Tynni and Sarapää (1987).…”
Section: Geologic Setting and Sample Materialsmentioning
confidence: 58%
“…Microfossil-like objects discovered by Tynni and Sarapää (1987) occur in chert nodules within a dolomitic unit of the Viistola Formation (Pekkarinen and Lukkarinen 1991), which forms part of the early Proterozoic cover sequence deposited on the Archean platform. The geology of the area has been described by Pekkarinen (1979) and Pekkarinen and Lukkarinen (1991).…”
Section: Geologic Setting and Sample Materialsmentioning
confidence: 99%
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