The genus Ptychodus is represented in the fossil records of Asia, Europe, Africa and the Americas. In North America, they are generously represented in Texas and the Western Interior Seaway. Welton &: Farish (1993) ascribed ten species to the Cretaceous of Texas:

  • Ptychodus anonymus WILLISTON 1900 (Cenomanian-Turonian),
  • P. connellyi MACLEOD & LAUGHTER 1980 (Campanian),
  • P. decurrens AGASSIZ 1843 (Albian-Cenomanian),
  • P. latissimus AGASSIZ 1843 (Coniacian-Campanian),
  • P. mammillaris AGASSIZ 1835 (Coniacian),
  • P. mortoni AGASSIZ 1839 ( Coniacian-Santonian),
  • P. occidentalis LEIDY 1868 (Cenomanian-Turonian),
  • P. polygyrus AGASSIZ 1839 (Turonian),
  • P. rugosus DIXON 1850 (Santonian) and
  • P. whipplei MARCOU 1858 (Turonian-Coniacian)
    In addition to some of the above, the Kansas chalk also yields P. martini WILLISTON 1898 from Coniacian exposures.

    Ptychodid sharks have been a puzzle since they were first described in the mid-1880s and it is still uncertain whether they are more closely related to sharks or rays. Generally, they are known only from isolated teeth in late Cretaceous (Albian through Campanian) deposits. Several more or less complete jaw plates, consisting of a hundred or more teeth, have also been found. In a few cases, the teeth are associated with vertebrae and dermal scales that are very similar to those of Squalicorax. The current view of the family Ptychodontidae is that they are related to hybodont sharks.

    The teeth of Ptychodus are arranged parallel, interlocking rows which form a broad crushing surface on both the upper and lower jaws. The largest teeth are found in the upper medial tooth row. The crown of the tooth ranges from nearly flat in some species, to a strongly developed cusp in others. The crown is expanded to cover the weakly bilobate root on all faces and always bears a series of distinctively radiating or transverse enameloid ridges surrounded by a marginal area of varying width. Species of Ptychodus are defined on the basis of crown shape and cusp development. According to Cappetta (1987), the flatter teeth of Ptychodus latissimus and P. polygyrus formed grindstone-like plates that were ideal for crushing benthic mollusks with thick shells. By elevating the cusp above the basal surface of the tooth, Ptychodus rugosus and P. mortoni may have been better equipped to attack less well protected prey such as ammonites. Wear patterns on P. mortoni teeth show that they were used to crush hard-shelled prey. Coprolite-like structures composed of the finely crushed shells of immature inoceramids in the Smoky Hill Chalk suggest that ptychodids may have preferred these small mollusks to the thicker shelled adults.


     

    For additional Ptychodus species, see the Ptychodids of the Tropic Shale webpage.

    For more information on Kansas ptychodids, visit the Oceans of Kansas webpage on ptychodid dentitions or Tom Caggiano's page on a Ptychodus anonymus dentition from the chalk.