Scale microfossils

Apatitic scale microfossils are a group of reticulate phosphatic plates found in the Neoproterozoic (810 million years ago) strata of the Fifteenmile Group, Yukon, Canada. They represent some of the earliest examples of biologically-induced biomineralization, using the mineral hydroxyapatite.[1]

Scale microfossils
Temporal range: 810 Ma
Scientific classification
Domain: Eukaryota
(unranked): Apatitic scale microfossils

References

  1. Cohen, Phoebe A.; Strauss, Justin V.; Rooney, Alan D.; Sharma, Mukul; Tosca, Nicholas (2017). "Controlled hydroxyapatite biomineralization in an ~810 million-year-old unicellular eukaryote". Science Advances. 3 (6): e1700095. Bibcode:2017SciA....3E0095C. doi:10.1126/sciadv.1700095. PMC 5489269. PMID 28782008.


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