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| Paleoartistic reconstruction of the Quebrada de Arcas. in Gesualdi, Belvedere, Yurac, ... et Meyer, 2025. Illustration by Joschua Knüppe. |
Highlights:
• New track-bearing surfaces are found in the Chacarilla Fm. in Quebrada des Arca.
• Five morphotypes: one of sauropod and four for different size theropod tracks are defined.
• Huge theropod tracks have been found and identified.
Abstract
We report diverse dinosaur tracks from siltstone to fine-grained sandstone facies of the Chacarilla Formation, Quebrada de Arcas of northeast Chile. Track-bearing surfaces were studied using 3D modelling and false-colour depth maps, derived from UAV photographs. Five morphotypes are identified based on morphology and morphometric criteria. Morphotype I comprises rounded tracks with a consistent narrow-gauge and resembles the sauropod ichnogenus, Parabrontopodus; diplodocids or titanosaurids are probable trackmakers. Morphotype II is assigned to the theropod ichnotaxon Abelichnus astigerrae and comprises some of the largest theropod tracks ever recorded from South America with a maximum footprint length of 51 cm; the trackmaker was most likely a large carcharodontosaurid, such as Giganotosaurus carolinii. Morphotype III is an indeterminate theropod track, which shows a distinctive and prominent metatarsal impression, but does not closely match any ichnotaxon although it bears some morphometrical affinity to Changpeipus carbonicus. The Morphotypes IV and V both belong to small-sized theropod trackmakers, and resemble Grallatoridae and Kayentapus-like forms, respectively. Additional theropod material cannot be assigned to specific morphotypes or trackmakers, due to poor preservation. Our findings show the existence of three distinct size classes (small, medium and large) of theropod morphotypes and point to a high ichnodiversity at the Jurassic-Cretaceous transition in the subtropical arid environments of Gondwana.
Keywords: Dinosaur tracks, Abelichnus astigerrae, Chacarilla Formation, Gondwana, Jurassic-Cretaceous boundary
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| Sedimentary structures in the Chacarilla Fm. Ripple marks (a, d, e), planar lamination (a, c), microbial mats from surface QA12 (b), Ophiomorpha (f) and cross-section dinosaur tracks (c). Scale bars are: 50 cm in (a), 18 cm in (b), 25 cm in (c), 10 cm in (d, e, f). |
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| Paleoartistic reconstruction of the Quebrada de Arcas. Illustration by Joschua Knüppe. |
Vincenzo Gesualdi, Matteo Belvedere, Marko Yurac, Dorothee Hippler, Nejla Hurem, Christian Salazar, Javiera Mendez and Christian A. Meyer. 2025. Diverse Dinosaur Tracks from the Upper Jurassic – Lower Cretaceous Chacarilla Formation of Quebrada de Arcas, northeast Chile: Evidence of high ichnodiversity in an arid palaeoenviroment. Palaeogeography, Palaeoclimatology, Palaeoecology. 113088; In Press. DOI: doi.org/10.1016/j.palaeo.2025.113088 [9 June 2025]
