Windermeria Explained

Windermeria aitkeni (named after Windermere, British Columbia, Canada) is a Precambrian organism from the Blueflower Formation of Sekwi Brook North, in the Northwest Territories of Canada. Only one specimen has been found. Windermeria is a small (16.4 × 7.9 mm) segmented elongated oval fossil with eight nearly equal-sized segments arranged transverse to medial furrow in opposite arrangement.^[1] Windermeria superficially resembles a diminutive Dickinsonia and as such is the only possible dickinsoniid proarticulatan known exclusively from outside of Australia and East Europe.^[2]

See also

• List of Ediacaran genera

External links

• Queen's University Department of Geological Sciences and Geological Engineering Museum archived from the original

Notes and References

1. Fedonkin M.A., Gehling J.G., Grey K., Narbonne G.M., Vickers-Rich P. (2007). "The Rise of Animals: Evolution and Diversification of the Kingdom Animalia", Johns Hopkins University Press. pp. 292
2. Narbonne G.M. (2007). "Chapter 10. The Canadian Cordillera". In: Fedonkin M.A., Gehling J.G., Grey K., Narbonne G.M., Vickers-Rich P. "The Rise of Animals: Evolution and Diversification of the Kingdom Animalia", Johns Hopkins University Press. pp. 180