Parasmittina trispinosa

Uncredited · via Wikidata/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
- ParasmittinaPBDB
- Diet
- suspension feederPBDB, for Cheilostomata
- Life habit
- epifaunalPBDB, for Cheilostomata
- Motility
- stationary, attachedPBDB, for Cheilostomata
- Vision
- blindPBDB, for Gymnolaemata
- Environment
- marinePBDB, for Lophophorata
Time the record covers
At least 2.4 million years on record.
The record covers at least 2.58 Mya to 129 ka. No occurrence read is dated outside 3.6 Mya to 11.7 ka.
7 occurrences of Parasmittina trispinosa on record, most of them in the Pleistocene. The Paleobiology Database records this as a living group. 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
7 occurrences- Pliocene14%
- Pleistocene86%
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
6 formations
- Canepatch Formation2
- Gardiners Clay Formation1
- San Diego Formation1
- Santa Barbara Formation1
- Timms Point Silt Formation1
- Lomita Marl Formation1
Loading coastlines…
The named rock units Parasmittina trispinosa has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Parasmittina trispinosa and its relatives
PleistoceneWhere Parasmittina trispinosa and its relatives were recorded in the Pleistocene.
Found in the same rock
359 taxa- Diaperoecia californica4 sites
- Lagenipora punctulata4 sites
- Anadara (Larkinia) transversa3 sites
- Anomia simplex3 sites
- Cauloramphus spiniferum3 sites
- Cellaria diffusa3 sites
- Cellaria mandibulata3 sites
- Crepidula fornicata3 sites
- Elphidium3 sites
- Mercenaria campechiensis3 sites
- Microporella ciliata3 sites
- Opalia borealis3 sites
- Tubulipora tuba3 sites
- Abra aequalis2 sites
- Ammonia2 sites
- Anachis avara translirata2 sites
- Angulus texanus2 sites
- Arca (Arca) sisquocensis2 sites
- Astyris lunata2 sites
- Balanus2 sites
- Callopora corniculifera2 sites
- Chapperia patula2 sites
- Cliona2 sites
- Colletosia radiata2 sites
The Paleobiology Database records 7 sites for Parasmittina trispinosa, 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- Fossil bryozoa from the Pleistocene of Southern California3
- Neogene Stratigraphy of the lower Coast Plain of the Carolinas2
- A Warm-Water Pleistocene Fauna from the Gardiners Clay of Eastern Long Island1
- The geology and paleontology of the marine Pliocene of San Diego, California. Part 2a, Paleontology1
Each of the 7 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 Parasmittina trispinosa
- Source
- Wikidata/Commons
- Credit
- nobody named on the record
- Licence
- not stated by the source
- Commercial use
- cannot be read from the licence given — check the record
No 3D scan of Parasmittina trispinosa 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 itParasmittina through timeFormations of the PleistoceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Johnston 1825)