Cantioscyllium
Cantioscyllium is an extinct genus of nurse shark from the Mesozoic era. It is known mainly from isolated teeth, but was named on a partial skeleton from the Late Cretaceous of England. It is a widespread and diverse genus, currently containing 10 species. They are uncommon but present throughout the late cretaceous of the eastern United States, including the Severn Formation of Maryland, the Tar Heel and Peedee formations of North Carolina, and Campanian of New Jersey. It is also known from the Western Interior Seaway and western Europe. C. hashimiaensis is known from the Santonian of Jordan. C. alhaulfi is from the Barremian.
No picture of Cantioscyllium was found. Wikipedia, Wikidata and iDigBio were searched and had none. Smithsonian Open Access did not answer, so this is what the others held rather than everything there is. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Cantioscyllium, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- GinglymostomatidaePBDB
- Diet
- carnivorePBDB, for Orectolobiformes
- Life habit
- nektobenthicPBDB, for Orectolobiformes
- Motility
- actively mobilePBDB, for Orectolobiformes
Time the record covers
At least 72 million years on record.
The record covers at least 145.06 Mya to 72.2 Mya. No occurrence read is dated outside 152.21 Mya to 66 Mya.
51 occurrences of Cantioscyllium on record, most of them in the Late Cretaceous. Bar height is expected occurrences, not a count: each fossil is spread across the span it is dated to, so a tall narrow bar means tight dating and a low wide one means loose.
When
51 occurrencesThese are dates about fossils, not the animal: the record can only begin after it arose and end before it died out, so either end may reach further. Shares are expected occurrences: a fossil dated to a span is counted partly in each period it straddles. More on what this infers.
Found in
25 formations
- Hell Creek Formation · Montana Group5
- Carlile Shale Formation · Colorado Group4
- Iron Springs Formation3
- Point Lookout Formation2
- Eutaw Formation2
- Straight Cliffs Formation1
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The named rock units Cantioscyllium has been recovered from, largest first. Drawn where the rock is now, not where it formed. One further formation holds fewer occurrences and is not listed. 15 occurrences have no formation on record, which is common for older literature.
Cantioscyllium and its relatives
Late CretaceousWhere Cantioscyllium and its relatives were recorded in the Late Cretaceous.
Found in the same rock
671 taxa- Cretalamna appendiculata16 sites
- Pseudohypolophus mcnultyi16 sites
- Hybodus14 sites
- Chiloscyllium greeni13 sites
- Ischyrhiza mira13 sites
- Pseudoscapanorhynchus compressidens12 sites
- Squalicorax kaupi12 sites
- Cretodus semiplicatus11 sites
- Dromaeosauridae11 sites
- Ptychotrygon triangularis11 sites
- Rhinobatos11 sites
- Squalicorax11 sites
- Haimirichia amonensis10 sites
- Ptychotrygon10 sites
- Squalicorax falcatus10 sites
- Chiloscyllium9 sites
- Scapanorhynchus minimus9 sites
- Scapanorhynchus raphiodon9 sites
- Texatrygon avonicola9 sites
- Lepisosteidae8 sites
- Protolamna8 sites
- Scapanorhynchus texanus8 sites
- Cenocarcharias tenuiplicatus7 sites
- Cretoxyrhina mantelli7 sites
The Paleobiology Database records 49 sites for Cantioscyllium, and this reads all of them. The number is how many of those sites it was catalogued from too. The 24 sharing the most are listed.
This is not a list of everything alive at the time. It is only what has come out of the same ground as this animal and been written down.
Entered from
34 references- New sharks and rays from the Cenomanian and Turonian of Charentes, France5
- Late Cretaceous Elasmobranchs from the Eutaw Formation at Luxapalila Creek, Lowndes County, Mississippi3
- Vertebrates of the Iron Springs Formation, Upper Cretaceous, southwestern Utah3
- Additions aux faunes de sélaciens du Crétacé du Texas (Albien supérieur-Campanien)3
- Les sélaciens des terrains néocrétacés and paléocènes de Belgique and des contrées limitrophes. Eléments d'une biostratigraphie intercontinentale3
- Euselachian diversity through the uppermost Cretaceous Hell Creek Formation of Garfield County, Montana, USA, with implications for the Cretaceous-Paleogene mass extinction in freshwater environments2
- Ein weiteres Exemplar von Cantioscyllum decipiens Woodward aus den Plattenkalken (Oberkreide) von Hakel (Haqil) im Libanon2
- Sharks (Elasmobranchii: Euselachii) from the Late Cretaceous of France and the UK2
- Elasmobranchs from Upper Cretaceous freshwater facies in southern Utah2
- Non-dinosaurian lower vertebrates across the Cretaceous-Tertiary boundary in northeastern Montana2
- Fossil marine vertebrates from the Blue Hill Shale Member (Middle Turonian) of the Upper Cretaceous Carlile Shale in northeastern Nebraska1
- Vertebrate Paleontology and Stratigraphy of the Late Cretaceous Holmdel Park Site, Monmouth County, New Jersey1
Each of the 51 occurrences read was entered from one of these publications, ordered by how many each accounts for. This is not a search for papers mentioning the name. 22 further references are not listed. Entries link to doi.org where the Paleobiology Database holds an identifier, and to its own record where it does not. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.
Media and terms
Media content0
No picture of Cantioscyllium was found. Wikipedia, Wikidata and iDigBio were searched and had none.
Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.
GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Cantioscyllium, or no answer at all. This entry cannot say which.
No 3D scan of Cantioscyllium was found in Sketchfab.
Smithsonian Open Access and MorphoSource were not reached for this taxon, so this list is what the others held rather than everything there is.
The description on this site
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itGinglymostomatidae through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Woodward 1889