Lisboasaurus

Taxobox
name = "Lisbosaurus"
fossil_range = Late Jurassic- Early Cretaceous
regnum = Animalia
phylum = Chordata
classis = Sauropsida
ordo =
genus = "Lisboasaurus"
subdivision_ranks = Species
subdivision =
* "L. estesi " (type)

"Lisboasaurus" is a small (400 mm length) genus of Mesozoic crocodylomorph that lived in fresh water. It is known from fossilized tooth and jaw fragments of Late Jurassic and Early Cretaceous age. Two species have been described. In the past "Lisboasaurus" has been interpreted as a Mid Jurassic avialan, troodontid, or an anguimorph lizard. Both species are currently assigned to Crocodylomorpha, one is reassigned to the genus "Lusitanisuchus".

In the 1960s paleontologists From the Free University Berlin located new vertebrate fossil sites that included the lignite mines of Guimarota, near the town of Leiria, Portugal. These lignites are dated by Milner and Evans, 1991, between Bathonian (middle Jurassic) to Oxfordian (early Late Jurassic) age. Schwarz and Fechner, 2004, date them as Late Jurassic.

Seiffert, (1970, 1973), described "Lisboasaurus" as a genus of anguimorph lepidosaur comprising two species, "L. estesi" and "L. mitracostatus". He subdivided the latter species into two subspecies in the first paper, but not in the second paper. In 1983 Estes listed the material as Lacertilia "incertae sedis". Milner and Evans, 1991, redescribed "L. estesi" as a maniraptoran and, more specifically, as an early avialan or troodontid They also cast doubt on the identification of the more poorly preserved "L. mistracostatus", considering it a "nomen dubium". Buscalioni and Evans "et al." revised this assignment by demonstrating that the material referred to "L. estesi" was closely allied with an Early Cretaceous crocodylomorph (LH 7991) from Las Hoyas, Spain. Buscalioni and Evans supported the "nomen dubium" status of "L. mistracostatus". However, Schwarz and Fechner, 2004, demonstrated that the material referred to "L. mistracostatus" is identical to teeth and fragments found in Porto Dinheiro, and new cranial and mandibular material collected from Guimarota between 1973 and 1982. They referred all "L. mistracostatus" specimens to a new genus they erected, "Lusitanisuchus", creating the new name "Lusitanisuchus mistracostatus".

Schwarz and Fechner (2008) described a new dentary from the Uña coal mine of Cuenca province, Spain. Its teeth demonstrate that it belongs to "Lisboasaurus". This dentary was the first "Lisboasaurus" fossil from the Barremian age of the Early Cretaceous. The new data extracted from the dentary make it more certain that "Lisboasaurus" was a neosuchian crocodylomorph.

References

* Buscalioni, A.D., Ortega, F., Pérez-Moreno, B.P., and Evans, S.E. (1996). "The Upper Jurassic maniraptoran theropod "Lisboasaurus estesi" (Guimarota, Portugal) reinterpreted as a crocodylomorph". "Journal of Vertebrate Paleontology" 16(2): 358–362.

* Estes, R. (1983). Sauria terrestria. Amphisbaenia. In "Handbuch der Paläoherpetologie". Teil 10A. Edited by P. Wellnhofer. Gustav Fischer Verlag, Stuttgart, pp. 1–249.

* Milner, A.R., and Evans, S.E. (1991). "The Upper Jurassic diapsid "Lisboasaurus estesi" — a maniraptoran theropod". "Palaeontology" 34: 503–513.

* Schwarz, D. and Fechner, R. (2004). "Lusitanisuchus", a new generic name for "Lisboasaurus mitracostatus" (Crocodylomorpha: Mesoeucrocodylia), with a description of new remains from the Upper Jurassic (Kimmeridgian) and Lower Cretaceous (Berriasian) of Portugal". "Canadian Journal of Earth Sciences" 41: 1259–1271.

* Seiffert, J. (1970). "Oberjurassische Lacertilier aus der Kohlengrube Guimarota bei Leiria (Mittel Portugal)". Unpublished Inaugural-Dissertation, Freie Universität, Berlin, Germany.

* Seiffert, J. (1973). "Upper Jurassic Lizards from Central Portugal". "Memória dos Servicos Géologicos de Portugal (N.S.)" 22: 7–88.

* Schwarz, D., Fechner, R. (2008). "The first dentary of "Lisboasaurus" (Crocodylomorpha, ?Mesoeucrocodylia) from the Lower Cretaceous of Uña, Cuenca Province, Spain". "Journal of vertebrate Paleontology" 28(1): 264-268.