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We report here a giant microfossil resembling the conidium of an ascomycete fungus (cf. Alternaria alternata). The specimen is preserved in stromatolitic black chert of the Gunflint Iron Formation (Paleoproterozoic Eon, Orosirian Period, ca. 1.9-2.0
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bd37eb344637080dcbc9e5eaa8b7f598
