Smittoidea reticulata

Alison M. Fortunato · CC0 · 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
- SmittoideaPBDB
- 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 4.6 million years on record.
The record covers at least 7.246 Mya to 2.58 Mya. No occurrence read is dated outside 11.63 Mya to 1.8 Mya.
6 occurrences of Smittoidea reticulata on record, most of them in the Miocene. The Paleobiology Database records this as a living group, and the chart stops with its fossils rather than at the present. 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
6 occurrences- Miocene50%
- Pliocene33%
- Pleistocene17%
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 Smittoidea reticulata has been recovered from, largest first. Drawn where the rock is now, not where it formed. 5 occurrences have no formation on record, which is common for older literature.
Smittoidea reticulata and its relatives
MioceneWhere Smittoidea reticulata and its relatives were recorded in the Miocene.
Found in the same rock
159 taxa- Ceriopora palmata5 sites
- Escharoides coccinea5 sites
- Onychocella angulosa5 sites
- Cribrilaria radiata4 sites
- Escharina dutertrei4 sites
- Figularia figularis4 sites
- Schedocleidochasma incisa4 sites
- Schizotheca fissa4 sites
- Smittina cervicornis4 sites
- Therenia montenati4 sites
- Turbicellepora coronopus4 sites
- Adeonella polystomella3 sites
- Biflustra savartii3 sites
- Calloporina decorata3 sites
- Calpensia nobilis3 sites
- Cellaria fistulosa3 sites
- Costazia costazi3 sites
- Diporula verrucosa3 sites
- Escharina vulgaris3 sites
- Escharoides megalota3 sites
- Microporella ciliata3 sites
- Myriapora truncata3 sites
- Reteporella cellulosa3 sites
- Smittina canavarii3 sites
The Paleobiology Database records 6 sites for Smittoidea reticulata, 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
3 references- Les bryozoaires cheilostomes du Néogène bétique (SE Espagne)4
- Celleporid (bryozoan) thickets from the Upper Pliocene of the island of Rhodes, Greece1
- Bryozoaires des milieux récifaux miocénes du sillon sud-rifain au Maroc1
Each of the 6 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 content1

Picture of Smittoidea reticulata
- Source
- Wikidata/Commons
- Credit
- Alison M. Fortunato
- Licence
- CC0
- Commercial use
- the licence allows it
No 3D scan of Smittoidea reticulata 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 itSmittoidea through timeFormations of the MioceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (MacGillivray 1842)