Physogaleus aduncus (Agassiz, 1843)

Cicimurri, David J. & Knight, James L., 2009, Late Oligocene sharks and rays from the Chandler Bridge Formation, Dorchester County, South Carolina, USA, Acta Palaeontologica Polonica 54 (4), pp. 627-647 : 632-633

publication ID

https://doi.org/ 10.4202/app.2008.0077

publication LSID

lsid:zoobank.org:pub:3D85D369-7A74-44B6-9766-7C4B8B26705B

persistent identifier

https://treatment.plazi.org/id/03A6C023-FF83-4E1B-1D24-FC1FFCDBF8D2

treatment provided by

Felipe

scientific name

Physogaleus aduncus (Agassiz, 1843)
status

 

Physogaleus aduncus (Agassiz, 1843)

Fig. 5E, F View Fig .

Referred specimens.—BCGM 9063–9066, SC 2009.18.7.

Comments.—The teeth within in this sample include morphotypes traditionally identified as Galeocerdo contortus Gibbes, 1849 and G. aduncus Agassiz, 1843 . Our studies of Oligocene and Miocene elasmobranch assemblages from the Atlantic Coastal plain confirm the observations of Purdy et al. (2001) and Ward and Bonavia (2001) that the two morphotypes occur together and in nearly equal numbers (see also Case 1980; Kent 1994). The morphologies could represent two coeval species, the teeth might be conspecific and represent dignathic heterodonty in a single species, (upper and lower teeth), or the teeth may be conspecific and represent gynandric heterodonty (male and female teeth).

Leriche (1927) illustrated what appear to be the “ G. contortus ” and “ G. aduncus ” morphologies under the name Galeocerdo aduncus (pl. 14: 1–8). Applegate (1978, 1992) discussed the possibility that the two morphologies represent dignathic heterodonty within a single species, “ G. ” aduncus , with palatoquadrates (upper jaws) bearing the “ G. aduncus ” morphotype and the Meckel’s cartilages (lower jaws) the “ G. contortus ” morphotype. Gottfried (1993) followed Applegate (1978) when describing a dentigerous partial right Meckel’s cartilage from the Miocene of Maryland, and Manning (2006) also advocated this relationship. Treating the morphologies as separate species, Purdy et al. (2001) suggested that “ G. aduncus ” fed on larger animals, whereas “ G. contortus ” was piscivorous.

Ward and Bonavia (2001) consider the “ G. contortus ” and “ G. aduncus ” morphologies to represent the same species (“ G. aduncus ”), but they also believe these are sufficiently similar to another carcharhiniform shark, Physogaleus Cappetta, 1980 , to warrant placement in that genus. Reinecke et al. (2005) assigned the contortus morphology to Physogaleus , but they referred the G. aduncus morphology to Galeocerdo , citing differences in tooth morphology and the paucity or complete lack of the G. contortus morphology in deposits yielding the G. aduncus morphology (see also Reinecke and Hoedemakers 2006). Physogaleus exhibits gynandric heterodonty ( Cappetta 1987), and according to Ward and Bonavia’s (2001) taxonomy the typical G. aduncus morphology represents teeth of females and upper teeth of males ( Fig. 5E View Fig ), whereas the G. contortus morphology represents teeth in the lower dentition of males ( Fig. 5F View Fig ). The taxonomic questions raised by the G. contortus / G. aduncus associations may not be answered without the aid of numerous crania with articulated dentitions (showing the range of gynandric/dignathic heterodonty).

Stratigraphic and geographic range.—Oligocene to Pliocene, Europe, USA (Atlantic Coastal Plain), Japan, Equador, Zaire.

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