Oxysmilia pliocenica
No picture of Oxysmilia pliocenica was found. Wikidata and iDigBio were searched and had none. Wikipedia and 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 Oxysmilia pliocenica, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- OxysmiliaPBDB
- Diet
- microcarnivorePBDB, for Caryophylliidae
- Life habit
- low-level epifaunal, solitary, clonalPBDB, for Caryophylliidae
- Motility
- stationary, attachedPBDB, for Caryophylliidae
- Vision
- blindPBDB, for Anthozoa
- Environment
- marinePBDB, for Scleractinia
Time the record covers
At most 1.1 million years on record.
Every occurrence read is dated to somewhere between 3.6 Mya and 2.58 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
2 occurrences of Oxysmilia pliocenica on record, most of them in the Pliocene. 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 occurrences- Pliocene100%
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
- Cayo Agua Formation · Bocas del Toro Group2
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The named rock units Oxysmilia pliocenica has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Oxysmilia pliocenica and its relatives
PlioceneWhere Oxysmilia pliocenica and its relatives were recorded in the Pliocene.
Found in the same rock
96 taxa- Antillocyathus gracilis2 sites
- Characodoma2 sites
- Cupuladria biporosa2 sites
- Cupuladria canariensis2 sites
- Discoporella2 sites
- Hippoporella gorgonensis2 sites
- Mamillopora2 sites
- Paracyathus adetos2 sites
- Schizoporella cornuta2 sites
- ? Turbonillidae indet.1 site
- Acteocina1 site
- Acteon1 site
- Agatrix1 site
- Alabina1 site
- Anadara (Rasia)1 site
- Ancilla1 site
- Architectonica1 site
- Argopecten1 site
- Cadulus1 site
- Caecidae1 site
- Calliostoma1 site
- Calyptraea1 site
- Carditidae1 site
- Cardium1 site
The Paleobiology Database records 2 sites for Oxysmilia pliocenica, 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- A paleobiotic survey of Caribbean faunas from the Neogene of the Isthmus of Panama1
- New records of azooxanthellate stony corals (Cnidaria: Scleractinia and Stylasteridae) from the Neogene of Panama and Costa Rica1
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 content0
No picture of Oxysmilia pliocenica was found. Wikidata and iDigBio were searched and had none.
Wikipedia and 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 Oxysmilia pliocenica, or no answer at all. This entry cannot say which.
No 3D scan of Oxysmilia pliocenica 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.
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itOxysmilia through timeFormations of the PlioceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Cairns 1995