Peponocyathus orientalis

Peponocyathus orientalis

Cairns S, Kitahara M (2012) · CC BY 3.0 · 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
PeponocyathusPBDB
Diet
microcarnivorePBDB, for Turbinoliidae
Life habit
solitaryPBDB, for Turbinoliidae
Motility
stationaryPBDB, for Turbinoliidae
Vision
blindPBDB, for Anthozoa
Environment
marinePBDB, for Scleractinia

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 5.333 Mya to 11.7 ka.

Miocene — about 0 of 11 occurrencesPliocene — about 3 of 11 occurrencesPliocenePleistocene — about 8 of 11 occurrencesPleistoceneHolocene — about 0 of 11 occurrences5.4–5.3 Mya — about 0.1 occurrences5.3–5.1 Mya — about 0.2 occurrences5.1–4.9 Mya — about 0.2 occurrences4.9–4.7 Mya — about 0.2 occurrences4.7–4.5 Mya — about 0.2 occurrences4.5–4.3 Mya — about 0.2 occurrences4.3–4.1 Mya — about 0.2 occurrences4.1–3.9 Mya — about 0.2 occurrences3.9–3.7 Mya — about 0.2 occurrences3.7–3.5 Mya — about 0.2 occurrences3.5–3.3 Mya — about 0.2 occurrences3.3–3.1 Mya — about 0.2 occurrences3.1–2.9 Mya — about 0.2 occurrences2.9–2.7 Mya — about 0.2 occurrences2.7–2.5 Mya — about 0.3 occurrences2.5–2.3 Mya — about 0.4 occurrences2.3–2.1 Mya — about 0.4 occurrences2.1–1.9 Mya — about 0.4 occurrences1.9–1.8 Mya — about 0.4 occurrences1.8–1.6 Mya — about 0.4 occurrences1.6–1.4 Mya — about 0.4 occurrences1.4–1.2 Mya — about 0.4 occurrences1.2–972 ka Mya — about 0.4 occurrences972 ka–778 ka Mya — about 0.4 occurrences778 ka–583 ka Mya — about 0.7 occurrences583 ka–389 ka Mya — about 0.7 occurrences389 ka–194 ka Mya — about 0.7 occurrences194 ka–0 Mya — about 2 occurrences2.58 Mya129 ka5.8 Mya0 Mya

11 occurrences of Peponocyathus orientalis 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

11 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

3 formations

Miaoli — 24.57°N, 120.80°ETonohama — 33.43°N, 133.97°EShimajiri — 26.15°N, 127.72°E

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The named rock units Peponocyathus orientalis 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.

Peponocyathus orientalis and its relatives

Pleistocene

Where Peponocyathus orientalis and its relatives were recorded in the Pleistocene.

Found in the same rock

9 taxa

The Paleobiology Database records 1 site for Peponocyathus orientalis, 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 11 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 Peponocyathus orientalis

Credit
Cairns S, Kitahara M (2012)
Licence
CC BY 3.0
Commercial use
the licence allows it

No 3D scan of Peponocyathus orientalis 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.

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Occurrence data from the Paleobiology Database, CC BY 4.0. (Duncan 1876)