Neopolypora subovaticellata

No picture of Neopolypora subovaticellata 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 Neopolypora subovaticellata, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
NeopolyporaPBDB
Diet
suspension feederPBDB, for Stenolaemata
Life habit
epifaunalPBDB, for Bryozoa
Motility
stationary, attachedPBDB, for Stenolaemata
Vision
blindPBDB, for Stenolaemata
Environment
marinePBDB, for Lophophorata

Time the record covers

At least 7.5 million years on record.

The record covers at least 274.4 Mya to 266.9 Mya. No occurrence read is dated outside 283.3 Mya to 264.28 Mya.

Permian — about 2 of 2 occurrencesPermian284–283 Mya — about 0.0 occurrences283–282 Mya — about 0.1 occurrences282–282 Mya — about 0.1 occurrences282–281 Mya — about 0.1 occurrences281–280 Mya — about 0.1 occurrences280–280 Mya — about 0.1 occurrences280–279 Mya — about 0.1 occurrences279–278 Mya — about 0.1 occurrences278–278 Mya — about 0.1 occurrences278–277 Mya — about 0.1 occurrences277–276 Mya — about 0.1 occurrences276–276 Mya — about 0.1 occurrences276–275 Mya — about 0.1 occurrences275–274 Mya — about 0.1 occurrences274–274 Mya — about 0.0 occurrences267–266 Mya — about 0.2 occurrences266–266 Mya — about 0.3 occurrences266–265 Mya — about 0.3 occurrences265–264 Mya — about 0.3 occurrences264–264 Mya — about 0.1 occurrences274.4 Mya266.9 Mya283.8 Mya263.8 Mya

2 occurrences of Neopolypora subovaticellata on record, most of them in the Permian. 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

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

2 formations

Qixia — 31.50°N, 117.85°EJiaoga — 29.55°N, 98.73°E

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The named rock units Neopolypora subovaticellata has been recovered from, largest first. Drawn where the rock is now, not where it formed.

Neopolypora subovaticellata and its relatives

Permian

Where Neopolypora subovaticellata and its relatives were recorded in the Permian.

Found in the same rock

9 taxa

The Paleobiology Database records 2 sites for Neopolypora subovaticellata, and this reads all of them. The number is how many of those sites it was catalogued from too.

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

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 Neopolypora subovaticellata 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 Neopolypora subovaticellata, or no answer at all. This entry cannot say which.

No 3D scan of Neopolypora subovaticellata 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 itNeopolypora through timeFormations of the PermianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (Schulga-Nesterenko 1952)