Paleoteius lakui gen. et sp. nov.
Federico L. Agnolín, Mauro Aranciaga-Rolando, Gerardo Álvarez-Herrera, Martín D. Ezcurra, Ana Moreno Rodríguez, Pablo Chafrat, Nahuel Vega, Agustín Scanferla, Krister T. Smith & Fernando E. Novas (2026)
A new late Cretaceous squamate from Patagonia sheds light on Gondwanan diversity
Scientific Reports (advance online publication)
doi:
https://doi.org/10.1038/s41598-026-40914-8https://www.nature.com/articles/s41598-026-40914-8[We are providing an unedited version of this manuscript to give early access to its findings. Before final publication, the manuscript will undergo further editing. Please note there may be errors present which affect the content, and all legal disclaimers apply.]
The fossil record of Mesozoic terrestrial squamates is very poor in the Southern Hemisphere. Currently recognised species represent less than 6% of the number described for Laurasian landmasses. Here, we describe the most complete Late Cretaceous terrestrial squamate known from South America. The specimen was collected in the Maastrichtian Allen Formation of northern Patagonia (Río Negro Province, Argentina) and represents a single individual that preserves a partial skull, vertebrae, and appendicular bones. The skeleton shows a unique combination of character states that allow erecting the new genus and species Paleoteius lakui. Morphological phylogenetic analyses recovered Paleoteius lakui as a Scincomorpha more closely related to Xantusiidae than to other species. When a molecular backbone is applied to those analyses, Paleoteius lakui is found outside Scincomorpha, but within a clade composed of Jurassic to Palaeogene species found as non-crown scincomorphans in previous studies. The affinities of Paleoteius lakui either as a stem-xantusiid or as a more early-diverging clade indicate the presence of a yet unrecognised lineage of squamates in South America. Paleoteius lakui is related to Laurasian forms with a probable cosmopolitan ancestry during the Jurassic–earliest Cretaceous. The new finding helps fill the still poorly known record of Mesozoic Gondwanan squamates.
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Laura Piñuela, Lida Xing, Ángel García-Pérez & José Carlos García-Ramos (2026)
First report of lizard trackways from the Jurassic of Europe
Ichnos (advance online publication)
doi:
https://doi.org/10.1080/10420940.2026.2634103https://www.tandfonline.com/doi/full/10.1080/10420940.2026.2634103 Two well-preserved lizard trackways from the Kimmeridgian Lastres Formation of Asturias (northern Spain) are described. Trackway 1 (T1) consists of seven tracks (four manus and three pes), whereas Trackway 2 (T2) includes six tracks (three manus and three pes). The estimated body lengths of the T1 and T2 trackmakers are slightly below 50 cm and 30 cm, respectively. Both trackways, preserved as natural casts, show asymmetric and ectaxonic manus and pes prints, ranging from tetradactyl to pentadactyl. Digit lengths follow the pattern IV > III > II, with digit V, when present, similar to or slightly longer than digit I. Distinct claw marks are preserved on most digit impressions, particularly in T1. Lizard footprints are uncommon in the Jurassic, and the Upper Jurassic records are especially rare. These new trackways represent the only well-documented lizard trackways from the Upper Jurassic. They are attributed to Rhynchosauroides and constitute the latest occurrence of this ichnogenus in the global record. Experimental comparisons with modern lizards suggest that the tail placement and footprints arrangement in T1 may provide clues to gait and movement patterns in these fossil trackmakers.
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