Basic info | Taxonomic history | Classification | Included Taxa |
Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Taphrosphys sulcatus
Taxonomy
Platemys sulcatus was named by Leidy (1856) [Locality and Horizon. "Tinton Falls, N.J." (Leidy, 1865, p. 109). No further information is available. The locality has not been relocated and the horizon of the type is not known.]. Its type specimen is AMNH 2522, a partial shell (fifth, sixth, and seventh left peripherals and left xiphiplastron), and it is a 3D body fossil. Its type locality is Tinton Falls (Greensand), which is in a Maastrichtian marine sandstone in the Hornerstown Formation of New Jersey. It is the type species of Taphrosphys.
It was recombined as Prochonias sulcatus by Cope (1869); it was recombined as Taphrosphys sulcatus by Hay (1902), Hay (1908), Hay (1930), Wood (1975), Gaffney (1975), Lapparent de Broin and Werner (1998), Gaffney et al. (2006).
It was recombined as Prochonias sulcatus by Cope (1869); it was recombined as Taphrosphys sulcatus by Hay (1902), Hay (1908), Hay (1930), Wood (1975), Gaffney (1975), Lapparent de Broin and Werner (1998), Gaffney et al. (2006).
Synonyms
|
Synonymy list
Year | Name and author |
---|---|
1856 | Platemys sulcatus Leidy p. 303 |
1865 | Platemys sulcatus Leidy p. 109 figs. Fig. 4, Plate 19 |
1869 | Prochonias sulcatus Cope |
1870 | Taphrosphys enodis Cope |
1870 | Taphrosphys molops Cope p. 159 |
1870 | Taphrosphys longinuchus Cope p. 162 |
1870 | Taphrosphys leslianus Cope pp. 166-166-A |
1902 | Taphrosphys leslianus Hay p. 438 |
1902 | Taphrosphys longinuchus Hay p. 438 |
1902 | Taphrosphys molops Hay p. 438 |
1902 | Taphrosphys sulcatus Hay p. 439 |
1908 | Amblypeza antellius Hay |
1908 | Taphrosphys sulcatus Hay p. 106 figs. Teit-figs. 98-100 |
1908 | Taphrosphys longinuchus Hay p. 108 figs. Test-figs. 101, 102 |
1908 | Taphrosphys leslianus Hay p. 111 figs. hrosphys leslianus Cope. Text-figs. 105-106 |
1908 | Taphrosphys molops Hay p. 115 figs. Figs. 112-120 |
1930 | Taphrosphys leslianus Hay p. 75 |
1930 | Taphrosphys longinuchus Hay p. 75 |
1930 | Taphrosphys molops Hay p. 75 |
1930 | Taphrosphys sulcatus Hay p. 75 |
1955 | Taphrosphys longinuchus Miller |
1975 | Taphrosphys sulcatus Gaffney pp. 2-3 |
1975 | Taphrosphys sulcatus Wood |
1998 | Taphrosphys sulcatus Lapparent de Broin and Werner p. 41 |
2006 | Taphrosphys sulcatus Gaffney et al. pp. 97-100 |
Is something missing? Join the Paleobiology Database and enter the data
|
|
If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Taphrosphys sulcatus Leidy 1856
show all | hide all
Invalid names: Amblypeza antellius Hay 1908 [synonym], Prochonias longinuchus Cope 1870 [synonym], Taphrosphys enodis Cope 1870 [synonym], Taphrosphys leslianus Cope 1870 [synonym], Taphrosphys molops Cope 1870 [synonym]
Diagnosis
Reference | Diagnosis | |
---|---|---|
E. S. Gaffney 1975 | Plastron relatively narrower than in T. olssoni; xiphiplastral notch shallower and not so circular as in T. olssoni; anterior plastral lobe relatively longer than in T. olssoni; xiphiplastral points more lateral compared with T. olssoni. | |
E. S. Gaffney et al. 2006 | A bothremydid pleurodire of the genus Taphrosphys distinguished from the other two species as follows: from T. congolensis: premaxilla labial ridge shallow not deep; rostrum basisphenoidale short and flat, barely defined; sella turcica shallow and wide; dorsum sellae low; processus clinoideus small; processus inferior parietalis farther from midline than in T. congolensis. Distinguished from T. ippolitoi: quadrate shelf not expanded laterally; sulcus eustachii opens ventrally rather than posteroventrally; fossa precolumellaris absent; sulcus eustachii without lateral process; premaxilla narrow; fenestra postotica not subdivided; tuberculum basioccipitale smaller; cavum tympani shallow rather than deep. Shell distinguished from ‘‘Taphrosphys’’ olssoni by plastron relatively narrower than in ‘‘T.’’ olssoni; xiphiplastral notch shallower and not as circular as in ‘‘T.’’ olssoni; anterior plastral lobe relatively longer than in ‘‘T.’’ olssoni; xiphiplastral points more lateral compared with ‘‘T.’’ olssoni. |
Measurements
No measurements are available
|
|
||||
|
|
||||
|
|
||||
|
|
||||
Source: subo = suborder, c = class, subp = subphylum | |||||
References: Hendy et al. 2009, Carroll 1988, Uetz 2005, Kiessling 2004 |
Age range: base of the Late/Upper Maastrichtian to the top of the Early/Lower Paleocene or 72.20000 to 61.66000 Ma
Collections (9 total)
Time interval | Ma | Country or state | Original ID and collection number |
---|---|---|---|
Late/Upper Maastrichtian | USA (New Jersey) | Platemys sulcatus (type locality: 129264) Taphrosphys leslianus (88034) Taphrosphys molops, Taphrosphys leslianus, Taphrosphys enodis (167780) Taphrosphys sulcatus (127082) Taphrosphys sulcatus, Taphrosphys molops (48570) | |
Late/Upper Maastrichtian - Early/Lower Paleocene | USA (New Jersey) | Taphrosphys longinuchus (128429) Taphrosphys molops (128428) Taphrosphys sulcatus, Taphrosphys molops (26819) | |
Danian | USA (New Jersey) | Holops pneumaticus (70857) |