Chemistry:Eozoon canadense
Eozoön canadense (literally, "dawn animal of Canada") is a pseudofossil.
John William Dawson described the banded structures of coarsely crystalline calcite and serpentine as a gigantic Foraminifera, which was thought to be the oldest known fossil (Dawson 1865). It was found in Precambrian metamorphosed limestone of Canada , at Côte St. Pierre near Grenville (Quebec) in 1863. It was later found in several other localities. Dawson called it "one of the brightest gems in the scientific crown of the Geological Survey of Canada". In 1894, it was shown that the place where it was found was associated with metamorphism (O'Brien 1970; Adelman 2007).
Similar Eozoön structures were subsequently found in metamorphosed limestone blocks erupted from Mount Vesuvius, where high-temperature physical and chemical processes were responsible for their formation (O'Brien 1970).
References
- Adelman, J. (2007). "Eozoön: debunking the dawn animal". Endeavor 31 (3): 94–98. doi:10.1016/j.endeavour.2007.07.002. PMID 17765972.
- Dawson, J. W. (1865). "On the structure of certain organic remains in the Laurentian limestones of Canada". Quart. J. Geol. Soc. 21 (1–2): 51–59. doi:10.1144/GSL.JGS.1865.021.01-02.12.
- Dolan, J. R. (2023). "The saga of the false fossil foram Eozoon". European Journal of Protistology 87 (2): 125955. doi:10.1016/j.ejop.2022.125955.
- O'Brien, C. F. (1970). "Eozoön canadense: 'The dawn animal of Canada'". Isis 61 (2): 206–223. doi:10.1086/350620.
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