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Abstract In 1946 Gilmore observed that the Hell Creek Formation component of the late Maastrichtian TT-zone contained more tyrannosaur taxa than just titanic Tyrannosaurus rex , based on a small, ontogenetically mature skull with a higher tooth count than the tyrant lizard. Over four decades later the skull was assigned to its own genus, Nanotyrannus lancensis . Also tagged shortly after was the taxon Stygivenator molnari . At the last turn of the century it was contended that all TT-zone tyrannosaurs are adult or juvenile T. rex , a view that became accepted by many. Because of the unusual morphological alterations that this hypothesis requires, it was consequently proposed that during ontogeny T. rex experienced a peculiar fish like metamorphosis. This conservative analysis rejects radical ontogenetic speculations, in favour of Tyrannosaurus having shared much the same average amniote/diapsid conventional growth observed in its fellow tyrannosaurids and especially tyrannosaurins. Actual juvenile Tyrannosaurus s pecimens show the same tooth count and other osteological features observed in the adults, negating the need for the metamorphosis not observed in any amniotes. This option has become widely accepted. The most extensive phylogenetic analysis to date confirms that the comparative anatomical analysis that most TT-zone mini tyrannosaurs possess a number of features that indicate they are not only not Tyrannosaurus , but represent an array of basal eutyrannosaur taxa that are neither Nanotyrannus nor Stygivenato r, with high tooth counts, and at least in some examples elongated hands, prominent dentary grooves and other features. Two new taxa are correspondingly named at the species and/or genus level, Gilmoretyrannus lethaeus and Larsonvenator elegans . These are postulated to represent at least in part the migration of basal eutyrannosaurs from former Appalachia into the Laramidia region via the new Laralachia land bridge. The total number of tyrannosaur taxa now known to have inhabited the TT-zone for over 1 MA is seven species in five genera from multiple subfamilies, with a smaller portion of this collection extant at any given stratigraphic level.