Abstract
Diverse epidermal appendages including grouped filaments closely resembling primitive feathers in non-avian theropods, are associated with skeletal elements in the primitive ornithischian dinosaur Kulindadromeus zabaikalicus from the Kulinda locality in south-eastern Siberia. This discovery suggests that “feather-like” structures did not evolve exclusively in theropod dinosaurs, but were instead potentially widespread in the whole dinosaur clade. The dating of the Kulinda locality is therefore particularly important for reconstructing the evolution of “feather-like” structures in dinosaurs within a chronostratigraphic framework. Here we present the first dating of the Kulinda locality, combining U-Pb analyses (LA-ICP-MS) on detrital zircons and monazites from sedimentary rocks of volcaniclastic origin and palynological observations. Concordia ages constrain the maximum age of the volcaniclastic deposits at 172.8 ± 1.6 Ma, corresponding to the Aalenian (Middle Jurassic). The palynological assemblage includes taxa that are correlated to Bathonian palynozones from western Siberia, and therefore constrains the minimum age of the deposits. The new U-Pb ages, together with the palynological data, provide evidence of a Bathonian age—between 168.3 ± 1.3 Ma and 166.1 ± 1.2 Ma—for Kulindadromeus. This is older than the previous Late Jurassic to Early Cretaceous ages tentatively based on local stratigraphic correlations. A Bathonian age is highly consistent with the phylogenetic position of Kulindadromeus at the base of the neornithischian clade and suggests that cerapodan dinosaurs originated in Asia during the Middle Jurassic, from a common ancestor that closely looked like Kulindadromeus. Our results consequently show that Kulindadromeus is the oldest known dinosaur with “feather-like” structures discovered so far.
Highlights
In 2010, a new Konservat-Lagerstätte was discovered in the Kulinda locality by geologists from the Institute of Natural Resources, Ecology, and Cryology, SB RAS (Chita, Russia)
206Pb/238U data obtained for the granite and two volcaniclastic samples are given in Table S2. 206Pb/238U ages of individual zircons and monazites range between 171.1 ± 1.5 Ma and 189.3 ± 1.5 Ma, with the highest age probability around 172–173 Ma (Fig. 3)
Results of 206Pb/238U dating of the three samples have been plotted on three distinct concordia curves (Figs. 4A–4C), one for each sample
Summary
According to Alifanov & Saveliev (2014) and Alifanov & Saveliev (2015), the dinosaur fauna at Kulinda comprises three new taxa: the ‘hypsilophodontian’ ornithopods Kulindapteryx ukureica and Daurosaurus olovus (Alifanov & Saveliev, 2014), and the ‘nqwebasaurid’ ornithomimosaur Lepidocheirosaurus natalis (Alifanov & Saveliev, 2015). We consider these three taxa as nomina dubia, and very likely synonyms of Kulindadromeus zabaikalicus (see Supplementary Information for a brief discussion on the composition of the Kulinda dinosaur fauna)
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