Abstract

Sauropod remains are abundant on the Iberian Peninsula across the Jurassic-Cretaceous transition. Where the osteological record shows a high diversity of this kind of dinosaur, the ichnological findings are mainly limited to sauropod tracks characterized by kidney-shaped manus (with or without pollex impressions) and pes impressions with three claw imprints oriented laterally. Here, we present a new sauropod ichnotaxon, Iniestapodus burgensis, found at several exposures within the Las Sereas megatracksite (Burgos, Spain). These are preserved within lacustrine limestone strata of the Rupelo Formation (Tithonian–Berriasian). Iniestapodus burgensis is characterized by: semicircular manus tracks with small pollex impressions; unusual tetradactyl pes tracks with evidence of four claws oriented anteriorly (I–II) and laterally (III–IV), of variable sizes (short claw I and IV impressions, claw II and III being the largest). The combination of features and comparison with the osteological record allows us to propose a non-titanosaurian titanosauriform as a possible trackmaker. All the Iniestapodus tracks are represented by at least two different size classes of small and medium-sized individuals, and their trackways show different multidirectional orientations. The paleoenvironmental and paleoecological data suggest that Iniestapodus trackmakers were solitary individuals, likely representing different age classes, that crossed and used the Las Sereas shallow lacustrine-palustrine areas as their preferred habitat.

Highlights

  • Sauropod remains are abundant on the Iberian Peninsula across the Jurassic-Cretaceous transition

  • The sauropod tracks studied were impressed in three exposures of the Las Sereas megatracksite, where more than 1000 vertebrate tracks, along 5.6 km, have been identified at ~ 14 sites

  • The sauropod tracks belong to a new ichnotaxon Iniestapodus burgensis

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Summary

Introduction

Sauropod remains are abundant on the Iberian Peninsula across the Jurassic-Cretaceous transition. The Late Jurassic (Kimmeridgian-Tithonian) and Jurassic-Cretaceous (Tithonian–Berriasian) intervals constitute time periods in which most Iberian Peninsula sauropod tracks have been described, with significant sites in the Lusitanian, Asturian, Cameros, and Maestrazgo basins. These track impressions are characterized by a kidney-shaped manus (either with or without a claw impression on digit I) and subtriangular pes with claw impressions generally oriented anterolaterally, and have been associated with the Parabrontopoduslike/Breviparopus-like and Brontopodus-like ­ichnotypes[1,2]. New sauropod tracks and trackways with the same characteristics as this ichnotype, but of two different size classes, have been identified in two further Las Sereas outcrops. These recent discoveries expand the distribution and current information on these specific tracks and their trackmakers

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