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Foss. Stud., Volume 3, Issue 1 (March 2025) – 5 articles

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12 pages, 3774 KiB  
Article
New Ornithopod Remains from the Upper Barremian (Lower Cretaceous) of Vadillos-1 (Cuenca, Spain)
by Mélani Berrocal-Casero, Fernando Barroso-Barcenilla, Pedro Miguel Callapez, Ricardo Pimentel, María Rosario Alcalde-Fuentes and Irene Prieto
Foss. Stud. 2025, 3(1), 5; https://doi.org/10.3390/fossils3010005 - 13 Mar 2025
Viewed by 1712
Abstract
New ornithopod remains have recently been discovered at the Vadillos-1 paleontological site, in Cuenca Province, Central Spain. These remains were collected in sandy and clayey deposits within “Wealden” alluvial facies, which correspond to an upper Barremian (Lower Cretaceous) alluvial-palustrine muddy floodplain paleoenvironment. The [...] Read more.
New ornithopod remains have recently been discovered at the Vadillos-1 paleontological site, in Cuenca Province, Central Spain. These remains were collected in sandy and clayey deposits within “Wealden” alluvial facies, which correspond to an upper Barremian (Lower Cretaceous) alluvial-palustrine muddy floodplain paleoenvironment. The remains correspond to a part of a sacrum, including three fused sacral vertebral centra with sacral ribs and part of the sacral yoke, together with an isolated unfused sacral vertebra. An incomplete ischium has also been identified, likely belonging to the same individual. The sacral block exhibits a broad sulcus that begins at the most anterior sacral vertebra, continues through the middle vertebra, and ends in the area where the middle and the most posterior vertebrae are fused. The non fused sacral vertebra also displays a ventral sulcus. The incomplete ischium has a curved shaft with a triangular cross section towards the distal end. The combination of the morphological features of the sacrum and ischium allow its attribution to Iguanodon cf. bernissartensis. This species is identified in the area for the first time, adding new valuable data about the dinosaur assemblages from the Lower Cretaceous of Spain. Full article
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24 pages, 18369 KiB  
Article
Giant Bird Tracks (Family Gastornithidae) from the Paleogene Chuckanut Formation, Northwest Washington, USA, with a Review of Gastornis Distribution
by George E. Mustoe
Foss. Stud. 2025, 3(1), 4; https://doi.org/10.3390/fossils3010004 - 27 Feb 2025
Viewed by 1745
Abstract
Giant Paleogene groundbirds named Gastornis have long been known from Europe, with similar fossils from North America being placed in the genus Diatryma. A more recent discovery in China is evidence that these birds had wide geographic distribution. The name Gastornis is [...] Read more.
Giant Paleogene groundbirds named Gastornis have long been known from Europe, with similar fossils from North America being placed in the genus Diatryma. A more recent discovery in China is evidence that these birds had wide geographic distribution. The name Gastornis is now generally considered to be the name that has historical precedence. Historically, Gastornis has been interpreted as being a fierce predator, but anatomical and isotopic evidence suggests that the giant birds were herbivores. Gastornithid tracks preserved in Lower Eocene fluvial sediments of the Chuckanut Formation in northwest Washington State, USA, support the herbivore interpretation. These tridactyl footprints preserve broad triangular toenails rather than talons. The Chuckanut Formation gastornithid tracks have been given the ichnotaxonomic name Rivavipes giganteus Mustoe et al. (2012). In 2024, two important new discoveries were made. These are a trackway that preserves three adult tracks, and two tracks left by a gastornithid chick.The adult bird trackway has stride and pace distances that are consistent with the short lower limb bones (tarsometatarsals) observed in Gastornis skeletal remains. The reproductive strategies of gastornithids remain enigmatic; the evidence consists of numerous egg shell fragments found at sites in France and the newly discovered Chuckanut tracks. Full article
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2 pages, 145 KiB  
Book Review
Book Review: Laurin, M. The Advent of PhyloCode: The Continuing Evolution of Biological Nomenclature; CRC Press: Boca Raton, FL, USA; Abingdon, UK, 2024; ISBN: 978-0-367-55288-6 (hbk), 978-0-367-55210-7 (pbk), 978-1-003-09282-7 (ebk)
by Sandra J. Carlson
Foss. Stud. 2025, 3(1), 3; https://doi.org/10.3390/fossils3010003 - 18 Feb 2025
Viewed by 734
Abstract
Birds are dinosaurs! Elementary school children will eagerly share this exciting bit of news with us these days [...] Full article
10 pages, 20679 KiB  
Communication
Bioerosion Structures on Dinosaur Bones Probably Made by Multituberculate Mammals and Dermestid Beetles (Guichón Formation, Late Cretaceous of Uruguay)
by Daniel Perea, Mariano Verde, Valeria Mesa, Matías Soto and Felipe Montenegro
Foss. Stud. 2025, 3(1), 2; https://doi.org/10.3390/fossils3010002 - 20 Jan 2025
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Abstract
We describe the first fossil traces from the skeletal remains of dinosaurs from Uruguay, from the Upper Cretaceous Guichón Formation. We describe the first biting/gnawing fossil traces reported for Uruguay, Machichnus bohemicus Mikulás et al., 2006, probably made by small tetrapods, such as multituberculate [...] Read more.
We describe the first fossil traces from the skeletal remains of dinosaurs from Uruguay, from the Upper Cretaceous Guichón Formation. We describe the first biting/gnawing fossil traces reported for Uruguay, Machichnus bohemicus Mikulás et al., 2006, probably made by small tetrapods, such as multituberculate mammals. Moreover, traces likely made by sarcosaprophagous beetles, namely Cubiculum Roberts et al., 2007, cf. Cubiculum, and cf. Osteocallis Roberts et al., 2007, are described. The presence of Cubiculum and Osteocallis supports previously proposed depositional conditions in a warm and arid to semi-arid continental environment for the referred stratigraphical unit. All traces would indicate a certain period of subaerial exposure before the definitive burial of the bones. Full article
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24 pages, 12711 KiB  
Article
The Largest Mesosaurs Ever Known: Evidence from Scanty Records
by Graciela Piñeiro, Pablo Núñez Demarco and Michel Laurin
Foss. Stud. 2025, 3(1), 1; https://doi.org/10.3390/fossils3010001 - 25 Dec 2024
Viewed by 3255
Abstract
Mesosaurs have long been considered to be small to mid-sized aquatic to semiaquatic amniotes that lived in Gondwana during the Early Permian or Late Carboniferous, according to recent research that showed their ghost range extending back to the Pennsylvanian. Previous morphometric analyses based [...] Read more.
Mesosaurs have long been considered to be small to mid-sized aquatic to semiaquatic amniotes that lived in Gondwana during the Early Permian or Late Carboniferous, according to recent research that showed their ghost range extending back to the Pennsylvanian. Previous morphometric analyses based on several hundred mesosaur specimens, including materials from Uruguay, Brazil, South Africa, Namibia, and the Paris National History Museum, provided a comprehensive understanding of mesosaur ontogeny, documented from fetus to adults. As a result, it was possible to determine the approximate size of any individual, measuring just one isolated limb bone, vertebrae, or even cranial elements. Herein, we describe large, poorly preserved and incomplete skulls, as well as axial and appendicular bones, from the Mangrullo Formation Konservat-Lagerstätte of Uruguay that suggest the existence of gigantism in mature mesosaurs reaching more than twice the size of previously described adults and type specimens. The sporadic occurrence of these giant individuals contrasts sharply with the abundant remains of young mesosaurs and, in general, with what is commonly found in the fossil record of vertebrates. The poor preservation of the mature individuals and their presence in coastal areas of the basin is consistent with the hypothesis that older mesosaurs have spent more time near the coast. An alternative hypothesis suggesting pelagic lifestyles is less supported by the available data. Given the preservation of unborn and hatchlings, as well as early juvenile, mature and very mature individuals, the mesosaur record is considered exceptional among early amniotes. Full article
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