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Parahelicoprion

From Wikipedia, the free encyclopedia

Parahelicoprion
Temporal range: Early Permian
~298.9–295 Ma
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Chondrichthyes
Subclass: Holocephali
Order: Eugeneodontida
Family: Helicoprionidae
Genus: Parahelicoprion
Karpinsky, 1924
Type species
Helicoprion clerci
Karpinsky, 1916
Species
  • P. clerci (Karpinsky, 1916)
  • P. mariosuarezi Merino-Rodo & Janvier, 1986

Parahelicoprion is an extinct genus of shark-like eugeneodontid holocephalids from the Permian of the Ural Mountains (Russia) and Copacabana Formation, Bolivia.[1] The genus name, from "nearly coiled saw" in Greek, directly refers to Helicoprion, a related holocephalid that shares similar traits to it, including the helical whorl of teeth.

The holotype of Parahelicoprion is based on a poorly preserved material,[1] so its size estimates along with those of some other large eugeneodonts are highly subjective due to their fragmentary fossil remains that cannot provide an empirical basis.[2] While Karpinsky separated the type species from the genus Helicoprion,[3] it has been recently suggested that this genus does represent a junior synonym of Helicoprion.[4]

Description

One of the primary qualities that separate Parahelicoprion from Helicoprion is the shape, thickness, and angle of the tooth whorl. Its teeth protrude outwards not like a tightly coiled saw, but instead a curved arrangement of cutting blades indicating it relied less on crushing slow-moving invertebrates and catching cephalopods, or other small mollusk prey, but inflicting traumatic damage against more durable, faster prey.[5] Their teeth grew at a much slower pace than those of other whorl-tooth sharks, resulting in a depreciated spiral, growing only half of the teeth a Helicoprion would grow in its lifetime. The tooth spiral also was able to indicate the age of the eugeneodontidans in question.[6]

Paleobiology

Parahelicoprion is thought to have been a nektonic carnivore that probably preyed upon a variety of different species, using its blade-like teeth to cut at exposed flesh like a hatchet or wedge.[7]

References

  1. ^ a b Merino-Rodo, Dagmar; et al. (1986). "Chondrichthyan and actinopterygian remains from theLower Permian Copacabana Formation of Bolivia". Geobios. 19 (4): 479–493. Bibcode:1986Geobi..19..479M. doi:10.1016/S0016-6995(86)80005-5.
  2. ^ Maisey, John G.; Bronson, Allison W.; Williams, Robert R.; McKinzie, Mark (2017-05-04). "A Pennsylvanian 'supershark' from Texas". Journal of Vertebrate Paleontology. 37 (3): e1325369. Bibcode:2017JVPal..37E5369M. doi:10.1080/02724634.2017.1325369. ISSN 0272-4634. S2CID 134127771.
  3. ^ Karpinsky, A.P. (1924). "Helicoprion (Parahelicoprion n.g.) clerci". Zapiski Ural'skogo Obshchestva Estestvoispytatelei. 34: 1–10.
  4. ^ Naugolnykh, S.V. (2018). "Artinskian (Early Permian) Sea Basin and Its Biota (Krasnoufimsk, Cis-Urals)". Stratigraphy and Geological Correlation. 26 (7): 734–754. Bibcode:2018SGC....26..734N. doi:10.1134/S0869593818070080. S2CID 135304766.
  5. ^ http://dinonews.net/forum/paleoactus.php?msg=168926 Parahelicoprion and Agassizodontidea
  6. ^ Brad Matsen and Ray Troll (October 25, 2012). "Planet Ocean: A Story of Life, the Sea, and Dancing to the Fossil Record".
  7. ^ "Fossilworks: Parahelicoprion".


This page was last edited on 17 February 2024, at 10:26
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