Genre
Ichnogenre Éteint

Kalosauropus

Ellenberger 1970

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Plage temporelle
Trias
Jurassique
Crétacé
Paléogène
Néogène
252 201 145 66 0 Ma
Occurrences PBDB
3
Groupe
Dinosaures
Herbivore Vivant au sol Terrestre
Kalosauropus
cliquer pour agrandir
Main evolutionary steps proposed for the morphofunctional and postural changes of the sauropod pedes. (A) Sauropod body mass through time (in metric tons) based on the sauropod body mass estimations of (41) (NB: data lacking for the second half of the Upper Cretaceous so illustrated here faded, in continuity with the data recorded in the Cretaceous). Schematic outlines of selected large specimens illustrated in the curve, including (from left to right) P. engelhardti, Vulcanodon karibaensis, R. brownei, G. brancai, Cedarosaurus weiskopfae, and Notocolossus gonzalezparejasi. (B) Projected evolutionary changes occurring in the sauropod pes associated with trend in body mass, including 1, skeletal and functional digitigrade pedal posture among basal non-sauropod sauropodomorphs with an incipient soft tissue pad (ISP) (see figs. S34 and S35); 2 and 3, expansion of a well-developed soft tissue pad beneath the elevated pedal bones (SP), resulting in a functionally plantigrade pes + retention of skeletal posture within a range of digitigrady; 4, retention of a soft tissue pad and yet undetermined trend toward more elevated bones; 5, conservation of the neomorphic soft tissue pad within all lineages. Selected examples of well-preserved non-sauropod sauropodomorph and sauropod pedal tracks illustrated above the trends, including (from left to right) Evazoum siriguii; Pseudotetrasauropus bipedoida, Eosauropus isp., Lavinipes cheminii; Kalosauropus pollex, Liujianpus shunan, Polyonyx gomesi; Parabrontopodus mcintoshi; Brontopodus birdi; Titanopodus mendozensis; and unnamed Asian sauropod track. Source of adapted drawing and notes are listed in table S9 and data S2. © Andréas Jannel, Steven W. Salisbury, Olga Panagiotopoulou · CC BY 4.0 · Wikimedia
PBDB
Classification
Dinosauria Clade non classé
Saurischia Clade non classé
Sauropodomorpha Clade non classé
Bagualosauria Clade non classé
Plateosauria Clade non classé
Anchisauria Clade non classé
Prosauropoda Clade non classé
Otozoidae Famille
Kalosauropus Genre
Sites de découverte 3 sites géolocalisés
Répartition
Principaux pays
🇱🇸 Lesotho
2
🇵🇱 Pologne
1
Formations géologiques
Zagaje
1
Elliot
1
Distribution temporelle
Pliensbachien (192.9–184.2 Ma)
1
Sinémurien (199.5–192.9 Ma)
1
Hettangien (201.4–199.5 Ma)
1
Espèces (2)
Kalosauropus masitisii 201 Ma
Kalosauropus pollex 201 Ma
Images 1
Bibliographie
Description originale
P. Ellenberger. 1970. Les niveaux paléontologiques de première apparition des mammifères primoridaux en Afrique du Sud et leur ichnologie. Establissement de zones stratigraphiques detaillees dans le Stormberg du Lesotho (Afrique du Sud) (Trias Supérieur à Jurassique) [The paleontological levels of the first appearance of primordial mammals in southern Africa and their ichnology. Establishment of detailed stratigraphic zones in the Stormberg of Lesotho (southern Africa) (Upper Triassic to Jurassic). In: S. H. Haughton (ed.), Second Symposium on Gondwana Stratigraphy and Paleontology, International Union of Geological Sciences. Council for Scientific and Industrial Research, Pretoria
Bibliographie (2)
G. Gierlinski and G. Niedzwiedzki. 2005. New saurischian dinosaur footprints from the Lower Jurassic of Poland. Geological Quarterly 49(1):99-104
P. Ellenberger. 1970. Les niveaux paléontologiques de première apparition des mammifères primoridaux en Afrique du Sud et leur ichnologie. Establissement de zones stratigraphiques detaillees dans le Stormberg du Lesotho (Afrique du Sud) (Trias Supérieur à Jurassique) [The paleontological levels of the first appearance of primordial mammals in southern Africa and their ichnology. Establishment of detailed stratigraphic zones in the Stormberg of Lesotho (southern Africa) (Upper Triassic to Jurassic). In: S. H. Haughton (ed.), Second Symposium on Gondwana Stratigraphy and Paleontology, International Union of Geological Sciences. Council for Scientific and Industrial Research, Pretoria