Polyopesia angustata

Yale Peabody Museum · CC0 · via GBIF. 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
- PolyopesiaPBDB
- Diet
- suspension feederPBDB, for Hexactinosa
- Life habit
- epifaunalPBDB, for Hexactinosa
- Motility
- stationary, attachedPBDB, for Hexactinosa
- Vision
- blindPBDB, for Hexactinellida
- Environment
- marinePBDB, for Hexactinellida
Time the record covers
At least 49 million years on record.
The record covers at least 132.6 Mya to 83.6 Mya. No occurrence read is dated outside 137.05 Mya to 72.2 Mya.
14 occurrences of Polyopesia angustata 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
14 occurrencesThese 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
3 formations
- Ahlen Formation4
- "Cuvieri-Pläner" Formation1
- Upper Chalk Formation · Chalk Group1
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The named rock units Polyopesia angustata has been recovered from, largest first. Drawn where the rock is now, not where it formed. 8 occurrences have no formation on record, which is common for older literature.
Polyopesia angustata and its relatives
Late CretaceousWhere Polyopesia angustata and its relatives were recorded in the Late Cretaceous.
Found in the same rock
290 taxa- Aulaxinia sulcifera5 sites
- Ventriculites radiatus5 sites
- Aphrocallistes cylindrodactylus4 sites
- Belemnitella mucronata4 sites
- Coeloscyphia racemosa4 sites
- Coscinopora infundibuliformis4 sites
- Hoploscaphites4 sites
- Laocoetis fittoni4 sites
- Laocoetis virgatula4 sites
- Leiostracosia angustata4 sites
- Leptophragma micropora4 sites
- Micraster glyphus4 sites
- Pachydiscus4 sites
- Periphragella plicata4 sites
- Spirolophia tortuosa4 sites
- Sporadoscinia alcyonoides4 sites
- Sporadoscinia stirps4 sites
- Sporadoscinia venosa4 sites
- Verrucocoelia tubulata4 sites
- Astropegma3 sites
- Callopegma acaule3 sites
- Cassianella gryphaeata3 sites
- Cataceramus balticus3 sites
- Echinocorys ovatus3 sites
The Paleobiology Database records 13 sites for Polyopesia angustata, 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
5 references- Die Großfauna der Mukronatenkreide (unteres Obercampan) im östlichen Münsterland4
- Hexactinellid sponges from the Santonian deposits of the Krakow area (southern Poland)3
- Contribution a l'etude des spongiaires siliceux du Cretace inferieur3
- Die Kieselspongien der oberen Kreide von Nordwestdeutschland, Teil 2 Triaxonia (Hexactinellida) [Upper Cretaceous sponges from north-western Germany, part 2 Triaxonia (Hexactinellida)]3
- Hexactinellid faunas in the chalk of England and Ireland1
Each of the 14 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 Polyopesia angustata
- Source
- GBIF
- Credit
- Yale Peabody Museum
- Licence
- CC0
- Commercial use
- the licence allows it
No 3D scan of Polyopesia angustata 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 itPolyopesia through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Schrammen 1902)