Chirocentrites
Chirocentrites is an extinct genus of marine ray-finned fish in the order Ichthyodectiformes. It contains a single species, C. coroninii, from the Late Cretaceous (Cenomanian) of Slovenia. A potential specimen is also known from the Albian-aged Pietraroja Plattenkalk of southern Italy, but it has been suggested that this specimen actually represents Cladocyclus.

Creator: Dmitry Bogdanov - dmitrchel@mail.ru · CC BY-SA 3.0 · 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- Sits inside
- CladocyclidaePBDB
- Diet
- carnivorePBDB, for Ichthyodectiformes
- Life habit
- nektonicPBDB, for Ichthyodectiformes
- Motility
- actively mobilePBDB, for Ichthyodectiformes
Time the record covers
At least 9.6 million years on record.
The record covers at least 110.1 Mya to 100.5 Mya. No occurrence read is dated outside 113.2 Mya to 93.9 Mya.
2 occurrences of Chirocentrites on record, most of them in the Early 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
2 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
1 formation
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The named rock units Chirocentrites 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.
Chirocentrites and its relatives
Early CretaceousWhere Chirocentrites and its relatives were recorded in the Early Cretaceous.
Found in the same rock
35 taxa- Anaethalion1 site
- Belonostomus1 site
- Brachyphyllum1 site
- Celtedens megacephalus1 site
- Chometokadmon fitzingeri1 site
- Cladocyclus1 site
- Clupavus1 site
- Costapycnodus costae1 site
- Costasaurus rusconi1 site
- Derasmosaurus pietrarojae1 site
- Diplomystus1 site
- Eichstaettisaurus gouldi1 site
- Glossodus heckelii1 site
- Heckelichthys microdon1 site
- Hemielopopsis suessi1 site
- Holcodon lesinaensis1 site
- Hypsospondylus bassanii1 site
- Hyptius sebastiani1 site
- Lepidotes1 site
- Leptolepis neumayri1 site
- Notagogus pentlandi1 site
- Ocloedus1 site
- Ophirachis deperditus1 site
- Opsigonus megaluriformis1 site
The Paleobiology Database records 2 sites for Chirocentrites, 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
2 references- Scipionyx samniticus (Theropoda: Compsognathidae) from the Lower Cretaceous of Italy: osteology, ontogenetic assessment, phylogeny, soft tissue anatomy, taphonomy and palaeobiology1
- Palaeoichtyoložki prilozi1
Each of the 2 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. Each entry links to the Paleobiology Database's own record for the work.
Media and terms
Media content1
Picture of Chirocentrites
- Source
- Wikipedia/Commons
- Credit
- Creator: Dmitry Bogdanov - dmitrchel@mail.ru
- Licence
- CC BY-SA 3.0
- Commercial use
- the licence allows it
No 3D scan of Chirocentrites 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 itCladocyclidae through timeFormations of the Early CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0.