Rebbachisauridae

Rebbachisauridae

Bilateria

Rebbachisaurids
Temporal range: Early Cretaceous
Limaysaurus tessonei skeleton restoration
Scientific classification e
Phylum: Chordata
Class: Reptilia
Superorder: Dinosauria
Order: Saurischia
Suborder: Sauropodomorpha
Infraorder: Sauropoda
Superfamily: Diplodocoidea
Family: Rebbachisauridae
Bonaparte, 1997
Genera

Rebbachisauridae is a family of sauropod dinosaurs known from fragmentary fossil remains from the Cretaceous of South America, Africa, and Europe.

Taxonomy

Sauropod specialist Jack McIntosh in 1990 included the first known genus, the giant North African sauropod Rebbachisaurus in the family Diplodocidae, subfamily Dicraeosaurinae, on the basis of skeletal details. With the discovery in subsequent years of a number of additional forms, it was realised that the rebbachisaurs constitute a distinct group of dinosaurs, and in 1997 the Argentine paleontologist José Bonaparte named the family Rebbachisauridae. Whitlock, 2011 defined two new subfamilies Nigersaurinae and Limaysaurinae within Rebbachisauridae. Cladogram of the Rebbachisauridae after Whitlock, 2011.[3]

Rebbachisauridae

Histriasaurus




Rebbachisaurus



Nigersaurinae

Zapalasaurus




Demandasaurus ("Spanish rebbachisaurid")



Nigersaurus




Limaysaurinae

Cathartesaura



Limaysaurus






Cladogram based on Carballido et al. (2010)[4] and Sereno et al. (2007):[2]

Rebbachisauridae

Histriasaurus




Rebbachisaurus





Demandasaurus ("Spanish rebbachisaurid")



Nigersaurus





Zapalasaurus





Cathartesaura



Rayososaurus





England taxon



Limaysaurus








Evolutionary relationships and characteristics

Nigersaurus taqueti teeth

Although all authorities agree that the rebbachisaurids are members of the superfamily Diplodocoidea, they lack the bifid (divided) cervical neural spines that characterise the diplodocids and dicraeosaurids, and for this reason are considered more primitive than the latter two groups. It is not yet known whether they share the distinctive whip-tail of the latter two taxa.

Rebbachisaurids are distinguished from other sauropods by their distinctive teeth, which have low angle, internal wear facets and asymmetrical enamel.

Unique among sauropods, at least some rebbachisaurids (such as Nigersaurus) are characterised by the presence of tooth batteries, similar to those of hadrosaur and ceratopsian dinosaurs. Such a feeding adaptation has thus developed independently three times among the dinosaurs.

So far, rebbachisaurids are known only from the middle and early part of the Late Cretaceous. Unless the nemegtosaurids are in fact diplodocoids (rather than titanosaurs), then the rebbachisaurids represent the last known representatives of this clade, and lived alongside the titanosaurs until fairly late in the Cretaceous. So far, no rebbachisaurids are known from the very end of the Cretaceous period.

References

  1. ^ Fidel Torcida Fernández-Baldor, José Ignacio Canudo, Pedro Huerta, Diego Montero, Xabier Pereda Suberbiola and Leonardo Salgado (2011). "Demandasaurus darwini, a new rebbachisaurid sauropod from the Early Cretaceous of the Iberian Peninsula". Acta Palaeontologica Polonica in press. doi:10.4202/app.2010.0003. http://www.app.pan.pl/article/item/app20100003.html. 
  2. ^ a b Paul C. Sereno, Jeffrey A. Wilson, Lawrence M. Witmer, John A. Whitlock, Abdoulaye Maga, Oumarou Ide, Timothy A. Rowe (2007). Kemp, Tom. ed. "Structural Extremes in a Cretaceous Dinosaur". PLoS ONE 2 (11): e1230. doi:10.1371/journal.pone.0001230. PMC 2077925. PMID 18030355. http://www.plosone.org/article/info:doi/10.1371/journal.pone.0001230. 
  3. ^ John A. Whitlock (2011). "A phylogenetic analysis of Diplodocoidea (Saurischia: Sauropoda)". Zoological Journal of the Linnean Society 161 (4): 872–915. doi:10.1111/j.1096-3642.2010.00665.x. 
  4. ^ José L. Carballido, Alberto C. Garrido, José I. Canudo and Leonardo Salgado (2010). "Redescription of Rayososaurus agrioensis Bonaparte (Sauropoda, Diplodocoidea), a rebbachisaurid from the early Late Cretaceous of Neuquén". Geobios 43 (5): 493–502. doi:10.1016/j.geobios.2010.01.004. 
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