Platyrhizodon barbei
No picture of Platyrhizodon barbei 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 Platyrhizodon barbei, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- PlatyrhizodonPBDB
- Diet
- carnivorePBDB, for Carcharhiniformes
- Life habit
- nektonicPBDB, for Carcharhiniformes
- Motility
- actively mobilePBDB, for Carcharhiniformes
Time the record covers
At most 14 million years on record.
Every occurrence read is dated to somewhere between 85.7 Mya and 72.2 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
4 occurrences of Platyrhizodon barbei 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
4 occurrences- Late Cretaceous100%
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
1 formation
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The named rock units Platyrhizodon barbei has been recovered from, largest first. Drawn where the rock is now, not where it formed. 3 occurrences have no formation on record, which is common for older literature.
Platyrhizodon barbei and its relatives
Late CretaceousWhere Platyrhizodon barbei and its relatives were recorded in the Late Cretaceous.
Found in the same rock
47 taxa- Carcharias adneti4 sites
- Chiloscyllium frequens4 sites
- Eoptolamna supracretacea4 sites
- Nanocorax microserratodon4 sites
- Squalicorax kaupi4 sites
- Squatirhina lonzeensis4 sites
- Anomotodon hermani3 sites
- Pararhincodon crochardi3 sites
- Parasquatina jarvisi3 sites
- Squatina (Cretascyllium) hassei3 sites
- Adnetoscyllium angloparisensis2 sites
- Archaeolamna kopingensis2 sites
- Carcharias latus2 sites
- Cederstroemia havreensis2 sites
- Cretaplatyrhinoidis ornatus2 sites
- Pararhincodon ornatus2 sites
- Paratriakis2 sites
- Paratriakis robustus2 sites
- Platyrhizodon gracilis2 sites
- Pseudocorax laevis2 sites
- Rhinobatos2 sites
- Scapanorhynchus raphiodon2 sites
- Adnetoscyllium1 site
- Agaleorhynchus britannicus1 site
The Paleobiology Database records 4 sites for Platyrhizodon barbei, 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
1 referenceEach of the 4 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 doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.
Media and terms
Media content0
No picture of Platyrhizodon barbei 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 Platyrhizodon barbei, or no answer at all. This entry cannot say which.
No 3D scan of Platyrhizodon barbei 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.
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itPlatyrhizodon through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Guinot et al. 2013