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- W2417966467 abstract "We describe crocodylian remains from the Early Miocene (MN4) site of Els Casots (Subirats, Vallès-Penedès Basin, NE of the Iberian Peninsula). Referral to Diplocynodon (Alligatoroidea: Diplocynodontidae) is justified by several cranial and postcranial features, including: (1) the subequal and confluent alveoli of the maxilla (fourth and fifth) and dentary (third and fourth); (2) the position of the foramen aëreum on the quadrate; (3) the small and ventrally reflected medial hemicondyle of the quadrate; (4) the distinct dorsoventral step on the frontal; and (5) the bipartite ventral osteoderms. Multiple morphological features are consistent with an attribution to Diplocynodon ratelii, previously known from the Early Miocene (MN2) of France, and discount an alternative attribution to other species of the genus, including Diplocynodon ungeri from the Middle Miocene (MN5) of Austria. The described material from Els Casots is smaller in size than the French material of D. ratelii, possibly reflecting an earlier ontogenetic stage. The described remains constitute the first report of D. ratelii and the youngest record of Diplocynodon in the Iberian Peninsula, where only Diplocynodon muelleri and Diplocynodon tormis have been previously reported. The presence of Diplocynodon further supports the lacustrine depositional environment previously inferred for Els Casots and also indicates a relatively high temperature. Nous décrivons les restes de crocodiliens du site du Miocène inférieur (MN4) d’Els Casots (Subirats, bassin de Vallès-Penedès, Nord-Est de la péninsule Ibérique). Une attribution à Diplocynodon (Alligatoroidea : Diplocynodontidae) est justifiée par plusieurs caractéristiques crâniennes et postcrâniennes, comprenant : (1) les alvéoles subégales et confluentes du maxillaire (quatrième et cinquième) et dentaires (troisième et quatrième) ; (2) la position du foramen aëreum sur le carré ; (3) l’hémicondyle média du carré, petit et ventralement réfléchi ; (4) l’étape dorsoventrale distincte sur le frontal ; (5) les ostéodermes ventrales bipartites. Plusieurs caractères morphologiques sont compatibles avec une attribution à Diplocynodon ratelii, déjà connu au Miocène inférieur (MN2) en France, et permettent de prévoir une attribution alternative à d’autres espèces du genre, y compris Diplocynodon ungeri du Miocène moyen (MN5) d’Autriche. Le matériel décrit à Els Casots est de plus petite taille que le matériel français de D. ratelii, reflétant probablement un stade ontogénétique antérieur. Les restes décrits constituent le premier rapport sur D. ratelii et le plus récent enregistrement de Diplocynodon dans la péninsule Ibérique, où seuls Diplocynodon muelleri et Diplocynodon tormis ont été précédemment signalés. La présence de Diplocynodon plaide encore plus en faveur de l’environnement sédimentaire lacustre précédemment inféré pour Els Casots et indique également une température relativement élevée." @default.
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- W2417966467 date "2017-01-01" @default.
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- W2417966467 title "New remains of Diplocynodon (Crocodylia: Diplocynodontidae) from the Early Miocene of the Iberian Peninsula" @default.
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- W2417966467 doi "https://doi.org/10.1016/j.crpv.2015.11.003" @default.
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