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The imagery on this page is the basis for a paper entitled The Oldest Platypus and its Bearing on Divergence Timing of the Platypus and Echidna Clades, by T. Rowe, T.H. Rich, P. Vickers-Rich, M. Springer and M.O. Woodburne (Proceedings of the National Academy of Sciences 105:1238-1242, 2008). The abstract is as follows:
Monotremes have left a poor fossil record, and paleontology has been virtually mute during two decades of discussion about molecular clock estimates of the timing of divergence between the platypus and echidna clades. We describe new evidence from high-resolution X-ray computed tomography indicating that Teinolophos, an Early Cretaceous fossil from Australia’s Flat Rocks locality (121-112.5 Ma), lies within the crown clade Monotremata, as a basal platypus. Strict molecular clock estimates of the divergence between platypus and echidnas range from 17-80 Ma, but Teinolophos suggests that the two monotreme clades were already distinct in the Early Cretaceous, and that their divergence may predate even the oldest strict molecular estimates by at least 50%. We generated relaxed molecular clock models using three different datasets, but only one yielded a date overlapping with the age of Teinolophos. Morphology suggests that Teinolophos is a platypus in both phylogenetic and ecological aspects, and tends to contradict the popular view of rapid Cenozoic monotreme diversification. Whereas the monotreme fossil record is still sparse and open to interpretation, the new data are consistent with much slower ecological, morphological, and taxonomic diversification rates for monotremes than in their sister taxon, the therian mammals. This alternative view of a deep geological history for monotremes suggests that rate heterogeneities may have affected mammalian evolution in such a way as to defeat strict molecular clock models and to challenge even relaxed molecular clock models when applied to mammalian history at a deep temporal scale.
About the Species
This specimen, a right dentary, was collected from the Wonthaggi Formation, Bunarong Marine Park, Victoria, Australia. It was made available to The University of Texas High-Resolution X-ray CT Facility for scanning by Dr. Thomas Rich of Museum Victoria. Funding for scanning and image processing was provided by a National Science Foundation Digital Libraries Initiative grant to Dr. Timothy Rowe of The University of Texas at Austin.
About this Specimen
This specimen was scanned by Matthew Colbert on 10 October 2005 along the coronal axis for a total of 1122 slices. Each 1024x1024 pixel slice is 0.012 mm thick, with an interslice spacing of 0.012 mm and a field of reconstruction of 11.84 mm.
About the Scan
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Literature & Links
None available.
Additional Imagery
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