Early Pleistocene enamel proteome sequences from Dmanisi resolve Stephanorhinus phylogeny.
Jazmin Ramos Madrigal,
Anna K. Fotakis,
Victor J. Moreno Mayar,
Rosa Rakownikow Jersie-Christensen,
Marc R. Dickinson,
Yvonne L. Chan,
Senthilvel KSS Nathan,
Peter D. Heintzman,
Joshua D. Kapp,
Marcela Sandoval Velasco,
Mikkel-Holger S. Sinding,
Christian D. Kelstrup,
Morten E. Allentoft,
M. Thomas P. Gilbert,
Posted 10 Sep 2018
bioRxiv DOI: 10.1101/407692
Posted 10 Sep 2018
Ancient DNA (aDNA) sequencing has enabled unprecedented reconstruction of speciation, migration, and admixture events for extinct taxa. Outside the permafrost, however, irreversible aDNA post-mortem degradation has so far limited aDNA recovery within the ~0.5 million years (Ma) time range. Tandem mass spectrometry (MS)-based collagen type I (COL1) sequencing provides direct access to older genetic information, though with limited phylogenetic use. In the absence of molecular evidence, the speciation of several Early and Middle Pleistocene extinct species remain contentious. In this study, we address the phylogenetic relationships of the Eurasian Pleistocene Rhinocerotidae using ~1.77 million years (Ma) old dental enamel proteome sequences of a Stephanorhinus specimen from the Dmanisi archaeological site in Georgia (South Caucasus). Molecular phylogenetic analyses place the Dmanisi Stephanorhinus as a sister group to the woolly (Coelodonta antiquitatis) and Merck's rhinoceros (S. kirchbergensis) clade. We show that Coelodonta evolved from an early Stephanorhinus lineage and that this genus includes at least two distinct evolutionary lines. As such, the genus Stephanorhinus is currently paraphyletic and its systematic revision is therefore needed. We demonstrate that Early Pleistocene dental enamel proteome sequencing overcomes the limits of ancient collagen- and aDNA-based phylogenetic inference, and also provides additional information about the sex and the taxonomic assignment of the specimens analysed. Dental enamel, the hardest tissue in vertebrates, is highly abundant in the fossil record. Our findings reveal that palaeoproteomic investigation of this material can push biomolecular investigation further back into the Early Pleistocene.
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