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Phoeniconotius

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Through Extinction and Australia

History

The fossils of Phoeniconotius have been discovered in the Lake Eyre basin of Australia, specifically a layer of mudstone belonging to the Etadunna Formation on the western shore of Lake Palankarinna. The type material consists of three bones, the distal end of the left tarsometatarsus and two phalanges. The material was collected from the surface and were discovered in association with one another, however not articulated. One phalanx, which is thought to represent the third toe, matches well with the corresponding area on the tarsometatarsus while the second known toe bone, likely representing the fourth toe, is thought to stem from the animal's right side. All the material is equally mineralized and shows the same coloration.

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