Hematite-coated microfossils: primary ecological fingerprint or taphonomic oddity of the Paleoproterozoic?

Microfossils belonging to the 1.88-billion-year-old ‘Gunflint-biota ’ are preserved as carbonaceous and hematitic filaments and spheres that are believed to represent ancient chemolithoautotrophic Fe(II) oxidiz-ing bacteria that grew above a chemocline where ferruginous seawater upwelled into shallow, oxygenated waters. This ‘biological ’ model posits that hematite formed during burial from dewatering of the precursor ferric oxyhydroxides that encrusted Fe(II)-oxidizing bacteria. Here, we present an alternate ‘taphonomic’ model in which iron-rich groundwaters discharged into buried stromatolites; thus, the mineralization reac-tions are more informative of diagenetic processes than they are for primary marine conditions. We sam-pled centimeter-scale columnar stromatolites from both the lower and upper stromatolite horizons of the Biwabik and Gunflint formations, across a range of metamorphic gradients including unaltered to prehnite-pumpellyite taconite, supergene altered ore, and amphibolite-pyroxene grade contact-metamorphic zones. Fossils are rare to very rare and comprise curved filaments that exist in clusters with similar orientations. The filaments from throughout the Biwabik are similar to well-preserved carbonaceous Gunflintia from Ontario. Spheres of Huroniospora are also found in both formations. Microfossils from the least altered sec-tions are preserved as carbon. Prehnite-pumpellyite samples are composed of either carbon or hematit