Keichousaurus fossils

Middle Triassic age, Guanling Formation, Xingyi, Guizhou, China.

The matrix is a compacted mix of fine volcanic ash, silt and is intersected by natural calcite mineral formations.

Fossil skeleton (excluding skull & end of tail) has minimal restoration.

Colour variation amongst the bones are the result of fossilization & an artefact of preparation.

Matrix has one repair - white lines are natural calcite mineral veining - the matrix has been tested  & proves genuine.

Reference to the holotype V952 (Institute of Vertebrate Paleontology & Paleoanthropolgy, Beijing, China) & other described specimens GXD7601,GXD7613, GXD7621, Guizhou Province Museum, China (ref; Functional Morphology & Ontogeny of Keichousaurus hui [Reptilia, Sauropterygia] K. Lin, O. Reippel 1998).

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