Slide show of putative Archean microfossils discovered from the Farrel Quartzite (>2.97 Ga) at the Mount Goldsworthy – Mount Grant area in the northeastern Pilbara Craton. Many of them are characterized by unusual shape, but are actually present in chert matrix in Archean age. Please contact to me (sugi@info.human.nagoya-u.ac.jp) for details (size, abundance, interpretations, etc...)
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