Catenipora tapaensis

Catenipora tapaensis

via GBIF · CC BY-NC 4.0 · 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
CateniporaPBDB
Diet
suspension feeder, photosymbioticPBDB, for Tabulata
Life habit
epifaunalPBDB, for Tabulata
Motility
stationary, attachedPBDB, for Tabulata
Vision
blindPBDB, for Anthozoa

Time the record covers

At least 6.4 million years on record.

The record covers at least 449.5 Mya to 443.1 Mya. No occurrence read is dated outside 449.9 Mya to 440.8 Mya.

Ordovician — about 24 of 26 occurrencesOrdovicianSilurian — about 2 of 26 occurrencesSilurian450–450 Mya — about 3 occurrences450–449 Mya — about 5 occurrences449–449 Mya — about 1 occurrence449–449 Mya — about 1 occurrence449–448 Mya — about 1 occurrence448–448 Mya — about 1 occurrence448–448 Mya — about 1 occurrence448–447 Mya — about 1 occurrence447–447 Mya — about 1 occurrence447–447 Mya — about 1 occurrence447–446 Mya — about 1 occurrence446–446 Mya — about 1 occurrence446–446 Mya — about 1 occurrence446–445 Mya — about 1 occurrence445–445 Mya — about 0.6 occurrences443–443 Mya — about 0.1 occurrences443–443 Mya — about 0.3 occurrences443–442 Mya — about 0.3 occurrences442–442 Mya — about 0.3 occurrences442–442 Mya — about 0.3 occurrences442–441 Mya — about 0.3 occurrences441–441 Mya — about 0.3 occurrences441–441 Mya — about 0.2 occurrences449.5 Mya443.1 Mya450.4 Mya440.3 Mya

26 occurrences of Catenipora tapaensis on record, most of them in the Ordovician. 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

26 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

5 formations

Kõrgessaare — 59.17°N, 24.75°EKõrgessaare — 58.95°N, 22.43°EKõrgessaare — 58.98°N, 22.81°EKõrgessaare — 59.02°N, 23.61°EAdila — 58.86°N, 24.08°EAdila — 58.74°N, 24.08°ETaucionys — 56.93°N, 28.46°EMoe — 59.26°N, 26.00°ETamsalu — 58.99°N, 26.35°E

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The named rock units Catenipora tapaensis has been recovered from, largest first. Drawn where the rock is now, not where it formed. 15 occurrences have no formation on record, which is common for older literature.

Catenipora tapaensis and its relatives

Ordovician

Where Catenipora tapaensis and its relatives were recorded in the Ordovician.

Found in the same rock

87 taxa

The Paleobiology Database records 25 sites for Catenipora tapaensis, 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

Each of the 26 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 Catenipora tapaensis

Source
GBIF
Credit
via GBIF
Licence
CC BY-NC 4.0
Commercial use
the licence does not allow it

No 3D scan of Catenipora tapaensis 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 itCatenipora through timeFormations of the OrdovicianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Sokolov 1951