Voay, Brochu, 2007
publication ID |
https://doi.org/10.1111/j.1096-3642.2007.00315.x |
publication LSID |
lsid:zoobank.org:pub:894D642D-8EC8-4521-A45F-77508E2317CC |
persistent identifier |
https://treatment.plazi.org/id/231487E6-FFB0-FFA4-2CDB-FA8BD5263541 |
treatment provided by |
Felipe (2021-08-31 17:10:46, last updated by Plazi 2023-11-06 10:31:37) |
scientific name |
Voay |
status |
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OF VOAY
Voay lacks several derived features that characterize the crown genus Crocodylus . These are also absent from Osteolaemus . The maxilla lacks extensive development of blind recesses along the medial surface of the caviconchal recess ( Fig. 6 View Figure 6 ). The anterior ramus of the ectopterygoid forming the posterolateral margin of the suborbital fenestra is not deeply forked ( Fig. 9 View Figure 9 ). The posterior iliac blade is not constricted near its posterior tip ( Fig. 12 View Figure 12 ). The pterygoid of Voay is also tall ventral to the median eustachian foramen, exposing the basisphenoid as a broad sheet ( Fig. 3); in all extant Crocodylus , the pterygoid is much shorter below the median eustachian foramen, limiting exposure of the basisphenoid. The condition seen in Voay is also found in Osteolaemus and Mecistops ( Brochu, 2000) .
The number of unambiguous synapomorphies for Osteolaeminae depends on how basal relationships within the group are resolved. If Rimasuchus is the basalmost osteolaemine or closely related to ‘ C. ’ pigotti and Euthecodon , there are two – extension of the squamosal on to the quadrate ramus and prominent preorbital crests. The former is a subtle character state, and variation in Voay suggests its secondary loss within the group (see below), but it is unique to osteolaemines. The latter is not unique to osteolaemines; most crocodyloid skulls bear nearly parasagittal ridges on the lacrimal, and they become especially prominent in Indopacific species of Crocodylus ( Brazaitis, 1973; Brochu, 2000). They are also anteroposteriorly short in extant Osteolaemus and, in both Osteolaemus and Voay , contiguous with the line along which the lateral surface of the snout is ventrolaterally reflected.
Extension of the squamosal beyond the paroccipital process is unambiguously present in Osteolaemus and the specimens used to code Euthecodon , ‘ C. ’ pigotti, and Rimasuchus . The specific shape of the descending lamina of the squamosal varies in all crocodylian species, but its extension does not vary in Osteolaemus . Nevertheless, variation in this feature in Voay calls utility of this feature into question. Unfortunately, because the other three osteolaemines are each based on single specimens, variation cannot be assessed.
A third character unambiguously diagnoses Osteolaeminae if Rimasuchus is closer to Voay and Osteolaemus – a distinct choanal neck ( Fig. 5 View Figure 5 ). The surface of the pterygoid anterior and lateral to the choana is depressed in most crocodyloids, but this condition is elaborated in osteolaemines such that the choana appears to open at the end of a short tube or ‘neck’. Choanal necks are also seen in some alligatoroids, but these result from deeper depressions lateral and posterior to the choana. This condition is observable in Osteolaemus at all stages of posthatching ontogeny.
This feature is ambiguous because the palate is incomplete in the specimen used to code Rimasuchus lloydi in this study (BMNH r14154) and in the holotype ( Fourtau, 1920), both of which are from the same Burdigalian site in Egypt. Skulls from several sites in Africa have been referred to Rimasuchus lloydi ( Tchernov, 1986; Pickford, 1994, 1996, 2000; Leakey et al., 1996; Llinás Agrasar, 2004), including one that appears to preserve a choanal neck ( Storrs, 2003: 146). However, there is considerable variation in the overall shapes of these skulls ( Tchernov, 1986; C. A. Brochu, pers. observ.) and they derive from several horizons throughout the Miocene and into the Pleistocene. Pending a more complete review of all of this material the condition of the choana in Rimasuchus will remain unknown.
The choana is not preserved in Euthecodon arambourgii ( Ginsburg & Buffetaut, 1978; C. A. Brochu, pers. observ.). More complete specimens of other species of Euthecodon not included in this study clearly show a strongly depressed pterygoid around the choana ( Tchernov, 1986; Storrs, 2003). Given the distribution of this feature in other crocodylids, its presence in Euthecodon arambourgii is predicted.
Two character states unambiguously unite Voay and Osteolaemus – a short palatine process that does not extend far beyond the anterior margins of the suborbital fenestrae and constricted supratemporal fenestrae. Both might be related to snout shape – in both cases, the skull is dorsoventrally deep relative to snout length (see below). In addition, Voay and O. tetraspis (but not O. osborni ) have short flanges that extend from the lateral margins of the palatines into the suborbital fenestra, another feature that might reflect overall skull shape.
Brazaitis P. 1973. The identification of living crocodilians. Zoologica 59: 59 - 88.
Brochu CA. 2000. Phylogenetic relationships and divergence timing of Crocodylus based on morphology and the fossil record. Copeia 2000: 657 - 673.
Fourtau R. 1920. Contribution a l'Etude des Vertebres Miocenes de l'Egypte. Cairo: Egypt Survey Department.
Ginsburg L, Buffetaut E. 1978. Euthecodon arambourgii n. sp. et l'evolution du genre Euthecodon, crocodilien du Neogene d'Afrique. Geologie Mediterraneene 5: 291 - 302.
Leakey MG, Feibel CS, Bernor RL, Harris JM, Cerling TE, Stewart KM, Storrs GW, Walker A, Werdelin L, Winkler AJ. 1996. Lothagam: a record of faunal change in the late Miocene of East Africa. Journal of Vertebrate Paleontology 16: 556 - 570.
Llinas Agrasar E. 2004. Crocodile remains from the Burdigalian (lower Miocene) of Gebel Zelten (Libya). Geodiversitas 26: 309 - 321.
Pickford M. 1994. Late Cenozoic crocodiles (Reptilia: Crocodylidae) from the Western Rift. Uganda geology and palaeobiology of the Albertine rift valley, Uganda-Zaire, Vol. II. Palaeobiology. In: Senut B, Pickford M, eds. Orleans: CIFEG Occasional Publications, 137 - 155.
Pickford M. 1996. Fossil crocodiles (Crocodylus lloydi) from the Lower and Middle Miocene of southern Africa. Annales de Paleontologie 82: 235 - 250.
Pickford M. 2000. Crocodiles from the Beglia Formation, Middle / Late Miocene boundary, Tunisia, and their significance for Saharan palaeoclimatology. Annales de Paleontologie 86: 59 - 67.
Storrs GW. 2003. Late Miocene - Early Pliocene crocodilian fauna of Lothagam, southwest Turkana Basin, Kenya. In: Leakey MG, Harris JM, eds. Lothagam: the dawn of humanity in eastern Africa. New York: Columbia University Press, 137 - 159.
Tchernov E. 1986. Evolution of the crocodiles in east and north Africa. Paris: CNRS.
Figure 5. Internal choana, ventral view. A, AMNH 3101, Voay robustus. B, TMM m-1786, Crocodylus niloticus. C, AMNH 10083, Osteolaemus osborni (holotype). Scale = 1 cm.
Figure 6. Right maxillae, medial view, showing medial wall of caviconchal recess (ccr). A, BMNH r2193, Voay robustus. B, UCMP 140795, Crocodylus niloticus. C, UF 34784, Osteolaemus tetraspis. Scale = 1 cm.
Figure 9. Right suborbital fenestra, lateral oblique view, showing condition of the anterior ramus of the ectopterygoid (ear). A, BMNH uncategorized, Voay robustus. B, TMM m-1786, Crocodylus niloticus. Scale = 1 cm.
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Kingdom |
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Order |
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Family |
Voay
Brochu, Christopher A. 2007 |
Voay
Brochu 2007 |
Voay
Brochu 2007 |
Voay
Brochu 2007 |
Voay
Brochu 2007 |
Voay
Brochu 2007 |
Osteolaeminae
Brochu 2003 |
Rimasuchus
Storrs 2003 |
Euthecodon
Fourtau 1920 |