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زمینشناسی و معدن::
میکروفسیل
hypothesis, since the oldest microfossil occurrences have been found in rocks formed in deep water hydrothermal settings.
Putative hematite tubes and filamentous microfossils have been identified in the 3.7 Ga rocks of the Nuvvuagittuq supracrustal
The filamentous microfossils were tested as fluid flow products of precipitation reactions and self-assembly structures.
microfossils of the Nuvvuagittuq units are considered iron-metabolizing filamentous bacteria and remain as one of the oldest
once figured as Eoarchean microfossils (Isuasphaera isua Pflug, 1978), these structures have recently been subjected to detailed
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