Eozoon canadense Pseudofossil
Summary:
Originally this fossil was identified in 1864 or 1865 by John William Dawson as a Precambrian foraminifera. As it turns out it was metamorphosed bands of calcite and serpentine thus a pseudofossil. Specimen can be seen at the Museo di Paleontologia at Sapienza University of Rome Italy.
Image was taken in June 2014.
Learn more at:
http://en.wikipedia.org/wiki/Eozoon_canadense
Content analysis:
Stratigraphic context:
Recognized stratigraphic terms [n]: | Precambrian [1]
|
Agenames chronostratigraphy [rating]: | Precambrian [0.1] |
Geographic context:
Location | Country | Latitude | Longitude |
Rome | IT | 41.8984 | 12.4956 |
Keywords:
bands, calcite, canada, canadense Pseudofossil Originally, Eozoon, Image, John William Dawson, Museo, Paleontologia, Precambrian foraminifera, Rome Italy, Sapienza University, Specimen