Carcharhinus perezi
The Caribbean reef shark is a species of requiem shark, belonging to the family Carcharhinidae. It is found in the tropical waters of the western Atlantic Ocean from Florida to Brazil, and is the most commonly encountered reef shark in the Caribbean Sea. With a robust, streamlined body typical of the requiem sharks, this species is difficult to tell apart from other large members of its family such as the dusky shark and the silky shark. Distinguishing characteristics include dusky-colored fins without prominent markings, a short free rear tip on the second dorsal fin, and tooth shape and number.

Albert Kok3 · CC0 · 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
- Caribbean reef sharkPBDB
- Sits inside
- CarcharhinusPBDB
- Diet
- carnivorePBDB, for Carcharhiniformes
- Life habit
- nektonicPBDB, for Carcharhiniformes
- Motility
- actively mobilePBDB, for Carcharhiniformes
Time the record covers
At least 12 million years on record.
The record covers at least 15.98 Mya to 3.6 Mya. No occurrence read is dated outside 23.04 Mya to 2.58 Mya.
22 occurrences of Carcharhinus perezi on record, most of them in the Miocene. The Paleobiology Database records this as a living group, and the chart stops with its fossils rather than at the present. 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
22 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
11 formations
- Pirabas Formation5
- Esbarrondadoiro Formation3
- Cantaure Formation3
- Gatun Formation2
- Arenas de Huelva Formation2
- Castillo Formation1
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The named rock units Carcharhinus perezi has been recovered from, largest first. Drawn where the rock is now, not where it formed. 1 occurrence has no formation on record, which is common for older literature.
Carcharhinus perezi and its relatives
MioceneWhere Carcharhinus perezi and its relatives were recorded in the Miocene.
Found in the same rock
1,143 taxa- Hemipristis serra15 sites
- Rhizoprionodon12 sites
- Rhinoptera11 sites
- Carcharhinus leucas10 sites
- Carcharhinus plumbeus9 sites
- Otodus megalodon9 sites
- Galeocerdo mayumbensis8 sites
- Mustelus8 sites
- Sphyrna laevissima8 sites
- Nebrius7 sites
- Pseudocarcharias kamoharai7 sites
- Raja7 sites
- Carcharhinus ackermannii6 sites
- Carcharodon hastalis6 sites
- Dasyatis6 sites
- Galeocerdo aduncus6 sites
- Mobula6 sites
- Physogaleus contortus6 sites
- Aetobatus5 sites
- Aetomylaeus5 sites
- Alopias vulpinus5 sites
- Carcharhinus brachyurus5 sites
- Carcharias cuspidatus5 sites
- Isurus oxyrinchus5 sites
The Paleobiology Database records 22 sites for Carcharhinus perezi, 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
12 references- A new Early Miocene (Aquitanian) Elasmobranchii assemblage from the la Guajira Peninsula, Colombia3
- Chondrichthyan fauna from the Pirabas Formation, Miocene of Northern Brazil, with comments on paleobiogeography3
- Sélaciens du Miocène terminal du bassin d'Alvalade (Portugal) Essai de synthèse3
- Neogene sharks and rays from the Brazilian 'Blue Amazon'2
- Sharks and Rays (Chondrichthyes, Elasmobranchii) from the late Miocene Gatun Formation of Panama2
- Los tiburones Carcharhiniformes (Chondrichthyes, Galeomorphii) del Plioceno inferior de la Formación Arenas de Huelva, suroeste de la cuenca del Guadalquivir, España2
- The Neogene sharks, rays, and bony fishes from Lee Creek Mine, Aurora, North Carolina2
- Underwater paleontology inside cenotes reveals the Miocene-Pliocene fish diversity in the Yucatan Peninsula, southeast Mexico1
- Sharks and rays (Chondrichthyes: Elasmobranchii) from the Peace River and Tamiami formations (Late Miocene–Early Pliocene) on the submerged continental shelf1
- A small fossil fish fauna, rich in Chlamydoselachus teeth, from the Late Pliocene of Tuscany (Siena, central Italy)1
- A new near-shore marine fauna and flora from the early Neogene of northwestern Venezuela1
- The Early Miocene fish fauna from the Pollock Farm Site, Delaware1
Each of the 22 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. 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 Carcharhinus perezi
- Source
- Wikipedia/Commons
- Credit
- Albert Kok3
- Licence
- CC0
- Commercial use
- the licence allows it
No 3D scan of Carcharhinus perezi 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 itCarcharhinus through timeFormations of the MioceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Poey 1876)