Meristodonoides is an extinct genus of hybodont known from the mid-late Cretaceous, with potential records dating back to the Jurassic. It is one of a number of hybodont genera composed of species formerly assigned to Hybodus.[2]
The genus is primarily known from remains from the Cretaceous of North America and Europe, spanning from the Aptian/Albian to Maastrichtian, making it one of the last surviving hybodont genera, though records of the genus likely extend as far back as the Late Jurassic, based on an undescribed skeleton from the Tithonian of England, and fragmentary teeth from the Kimmeridgian of Poland, England and Switzerland.[3] Other remains of the genus are known from the Coniacian of England, the Aptian-Albian of France,[4] the Campanian of British Columbia, Canada[5] and the Campanian of European Russia.[6]
Taxonomy
The type species is M. rajkovichi, which was originally a species in the genus Hybodus. The species, along with other Hybodus species such as H. butleri and H. montanensis, was reassigned to Meristodonoides by Charlie J. Underwood and Stephen L. Cumbaa in 2010.[2][7]
M. multiplicatus Cicimurri et al., 2014 - Santonian-Campanian of Mississippi[3]
Ecology
The morphology of the teeth suggests an adaptation to tearing prey, with a specialization for restraining fast-swimming prey such as small fish and squid.[3][11] Fossils from the Western Interior Seaway suggest that it preferred nearshore marine environments, being absent from deeper-water areas, with it likely also being able to tolerate brackish and freshwater conditions.[7] In the Gulf Coastal Plain, Meristodonoides teeth are largely found in estuarine deposits. The restriction of Meristodonoides to nearshore habitats, combined with its late occurrence, fits the overall decline in niches occupied by hybodonts throughout the Cretaceous, likely due to them being outcompeted by lamniform sharks in open marine habitats.[11] However, some Meristonoides teeth have also been recovered from deep-water deposits representing open marine environments, such as the Northumberland Formation in Canada.[5]
^Case, G.R.; Cappetta, H. Additions to the elasmobranch fauna from the late Cretaceous of New Jersey (lower Navesink Formation, early Maastrichtian). Palaeovertebrata2004, 33, 1–16
