Allomorone burlesonis
No picture of Allomorone burlesonis was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Allomorone burlesonis, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- AllomoronePBDB
- Motility
- actively mobilePBDB, for Osteichthyes
Time the record covers
At least 7 million years on record.
The record covers at least 48.07 Mya to 41.03 Mya. No occurrence read is dated outside 56 Mya to 33.9 Mya.
22 occurrences of Allomorone burlesonis on record, most of them in the Eocene. 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 occurrences- Eocene100%
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
10 formations
- Weches Formation · Claiborne Group4
- Cook Mountain Formation · Claiborne Group4
- Stone City Formation3
- Bashi Formation2
- Nanjemoy Formation2
- Lisbon Formation1
Loading coastlines…
The named rock units Allomorone burlesonis has been recovered from, largest first. Drawn where the rock is now, not where it formed. 2 occurrences have no formation on record, which is common for older literature.
Allomorone burlesonis and its relatives
EoceneWhere Allomorone burlesonis and its relatives were recorded in the Eocene.
Found in the same rock
202 taxa- Brazosiella kokeni15 sites
- Bauzaia12 sites
- Jefitchia copelandi11 sites
- Ekokenia eporrecta10 sites
- Lactarius amplus10 sites
- Paraconger10 sites
- Preophidion petropolis10 sites
- Sciaena9 sites
- Signata stenzeli9 sites
- Pterothrissus umbonatus8 sites
- Bregmaceros troelli7 sites
- Caproidarum serratus7 sites
- Preophidion7 sites
- Sparus elegantulus7 sites
- Symmetrosulcus7 sites
- Bauzaia lamberi6 sites
- Bauzaia melrosensis6 sites
- Carapus smithvillensis6 sites
- Conger6 sites
- Brazosiella moseleyi5 sites
- Clupeidae5 sites
- Corvina intermedia5 sites
- Glyptophidium stringeri5 sites
- Haemulon5 sites
The Paleobiology Database records 22 sites for Allomorone burlesonis, 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
4 references- Middle and late Eocene fish otoliths from the eastern and southern USA9
- Otoliths of some early Cenozoic fishes of the Gulf Coast6
- Early Eocene fish otoliths from the eastern and southern USA5
- Community structure and evaluation of trophic analysis in paleoecology Stone City Formation (Middle Eocene, Texas)2
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 content0
No picture of Allomorone burlesonis was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none.
GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Allomorone burlesonis, or no answer at all. This entry cannot say which.
No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itAllomorone through timeFormations of the EoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Frizzell and Dante 1965)