PEGOPHYSEMINAE, Taylor & Glover & Smith & Dyal & Williams, 2011
publication ID |
https://doi.org/ 10.1111/j.1096-3642.2011.00700.x |
persistent identifier |
https://treatment.plazi.org/id/0E297D4D-FFDF-B82E-B641-8140E6FE4DDE |
treatment provided by |
Valdenar |
scientific name |
PEGOPHYSEMINAE |
status |
subfam. nov. |
PEGOPHYSEMINAE View in CoL – NEW SUBFAMILY
Except for Anodontia alba (type species of Anodontia ), all other species analysed that have been previously classified as Anodontia are separate on a highly supported long branch. Within this clade, the species previously classified into various subgenera of Anodontia , namely Loripinus , Pegophysema , Euanodontia , Cryptophysema , and Cavatidens also lie on long internal branches (most taxa included in 28S tree; Fig. 2 View Figure 2 ). Because of their phylogenetic distinctive- ness we propose a new subfamily Pegophyseminae , and in consideration of the differences from Anodontia alba we elevate the subgenera listed above, together with Afrophysema and Bythosphaera (Taylor & Glover, 2005) , to full generic status. The type species of Pegophysema is Pegophysema schrammi (Crosse, 1876) , and an 18S sequence from this species (donated by D. Distel, specimen from Bermuda) grouped with other pegophysemine species in the analysis of Williams et al. (2004). A closely similar species from the Indo-West Pacific, Pegophysema philippiana , is included in the 28S and 18S trees herein.
Pegophyseminae are united by some unusual morphological characters, including thin, globular, smooth shells, a narrow edentulous hinge with an internal and laterally extended ligament in most species, and, anatomically, the presence of a mantle septum, digitate mantle gills, and extensive posterior mantle fusion ( Taylor & Glover, 2005).
Although the chronogram ( Fig. 5 View Figure 5 ) suggests a late Cretaceous origin, there are no convincing records of Pegophyseminae-like bivalves in pre-Cenozoic rocks. Records for the Cenozoic are frequent, and contemporaneously in the Eocene of the Paris Basin and southern USA ( Cossmann & Pissarro, 1904 –06; Gardner, 1951), there were lucinids with characters of living Pegophyseminae such as Anodontia augustana Gardner, 1951 , ‘ Lucina ’ conili de Raincourt, 1877, and ‘ Lucina ’ parnensis Deshayes, 1857. Pre-Cenozoic species with a superficial resemblance to pegophysemines include the hydrocarbon seep-associated ‘ Cryptolucina ’ kuhnpassetensis Kelly, 2000 from the Cretaceous of Greenland, which is inflated and edentulous ( Kelly et al., 2000). From the Palaeozoic, Boyd & Newell (1979) compared the Permian Gigantocyclus zidensis Termier & Termier, 1977 , from the Permian of Tunisia with Anodontia , and the Devonian Paracyclas species , placed by Johnston (1993) into the family Paracyclidae , are similar in general shape to living taxa. There is insufficient evidence to include any of these genera in the Pegophyseminae .
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