Orectolobiformes
Carpet sharks are sharks classified in the order Orectolobiformes. Sometimes the common name "carpet shark" is used interchangeably with "wobbegong", which is the common name of sharks in the family Orectolobidae. Carpet sharks have five gill slits, two spineless dorsal fins, and a small mouth that does not extend past the eyes. Many species have barbels.

Richard Ling · CC BY-SA 2.0 · via Wikipedia/Commons. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.
On record
Recorded, not inferred- Also called
- carpet sharkPBDB
- Sits inside
- GaleomorphiPBDB
- Diet
- carnivorePBDB
- Life habit
- nektobenthicPBDB
- Motility
- actively mobilePBDB
Time the record covers
At least 227 million years on record.
The record covers at least 227.3 Mya to 129 ka. No occurrence read is dated outside 237 Mya to 11.7 ka.
1,144 occurrences of Orectolobiformes on record, most of them in the Late Cretaceous. The Paleobiology Database records this as a living group. 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
1,144 occurrences- Late Triassicunder 1%
- Early Jurassic4%
- Middle Jurassic4%
- Late Jurassicunder 1%
- Early Cretaceous6%
- Late Cretaceous46%
- Paleocene8%
- Eocene25%
- Oligocene1%
- Miocene4%
- Plioceneunder 1%
- Pleistoceneunder 1%
These 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
211 formations
- Mesaverde Formation29
- Matam Formation28
- Hell Creek Formation · Montana Group22
- Marnes de Donzacq Formation21
- Hunstanton Formation21
- Couche II Formation20
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The named rock units Orectolobiformes has been recovered from, largest first. Drawn where the rock is now, not where it formed. 187 further formations hold fewer occurrences each and are not listed. 401 occurrences have no formation on record, which is common for older literature.
Orectolobiformes and its relatives
Late CretaceousWhere Orectolobiformes and its relatives were recorded in the Late Cretaceous.
Found in the same rock
3,558 taxa- Myledaphus bipartitus40 sites
- Teleostei39 sites
- Squalicorax kaupi37 sites
- Ischyrhiza mira35 sites
- Archaeolamna kopingensis34 sites
- Crocodylia32 sites
- Myliobatis31 sites
- Rhinobatos31 sites
- Hybodus30 sites
- Carcharias28 sites
- Cretalamna appendiculata28 sites
- Dasyatis28 sites
- Trionychidae28 sites
- Hemipristis serra27 sites
- Squatina25 sites
- Aves23 sites
- Meristodonoides montanensis23 sites
- Protoplatyrhina renae23 sites
- Scyliorhinus23 sites
- Lepisosteus22 sites
- Odontaspis aculeatus22 sites
- Restesia americana22 sites
- Carcharhinus21 sites
- Texatrygon avonicola21 sites
The Paleobiology Database records 589 sites for Orectolobiformes, and this reads 240 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
276 references- Les Orectolobiformes, Carcharhiniformes et Myliobatiformes (Elasmobranchii, Neoselachii) des bassins à phosphate du Maroc (Maastrichtien-Lutétien basal). Systématique, biostratigraphie, évolution et dynamique des faunes107
- Sharks (Elasmobranchii: Euselachii) from the Late Cretaceous of France and the UK67
- Late Cretaceous and Danian neoselachians from southern Sweden55
- Toarcian shark and ray faunas (Chondrichthyans) from Luxembourg and Belgium in the aftermath of the T-OAE38
- Nouvelle faunes de sélaciens (Elasmobranchii, Neoselachii) de l'Eocène moyen des Landes (Sud-Ouest, France). Implication dans la connaissance des communautés de sélaciens d'eau profondes35
- The selachian fauna (sharks and rays) of the phosphate series of Ndendouri-Ouali Diala (Matam, Western Senegal): Dating and paleoenvironmental interests28
- A new selachian fauna from the late Campanian of Wyoming (Teapot Sandstone Member, Mesaverde Formation, Big Horn Basin)26
- Albian and Cenomanian selachian assemblages from north-east England25
- Les poissons fossiles du Bas-Congo et des régions voisines24
- Shark and ray faunas in the Middle and Late Eocene of the Fayum Area, Egypt22
- Les sélaciens des terrains néocrétacés and paléocènes de Belgique and des contrées limitrophes. Eléments d'une biostratigraphie intercontinentale21
- The Selsey Division (Bracklesham Group) at Lee-on-the-Solent, Gosport, (Hants)13
Each of the 1,144 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. 264 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 content1
Picture of Orectolobiformes
- Source
- Wikipedia/Commons
- Credit
- Richard Ling
- Licence
- CC BY-SA 2.0
- Commercial use
- the licence allows it
No 3D scan of Orectolobiformes was found in MorphoSource and Sketchfab.
Smithsonian Open Access was 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 itGaleomorphi through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Applegate 1972