Trochocyathus taylorensis

No picture of Trochocyathus taylorensis 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 Trochocyathus taylorensis, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
TrochocyathusPBDB
Diet
microcarnivorePBDB, for Trochocyathus
Life habit
low-level epifaunalPBDB, for Trochocyathus
Motility
stationary, attachedPBDB, for Trochocyathus
Vision
blindPBDB, for Anthozoa
Environment
marinePBDB, for Scleractinia

Time the record covers

At most 12 million years on record.

The one occurrence read is dated to somewhere between 83.6 Mya and 72.2 Mya, which is a dating window rather than a span.

Late Cretaceous — about 1 of 1 occurrenceLate Cretaceous84–83 Mya — about 0.0 occurrences83–83 Mya — about 0.0 occurrences83–82 Mya — about 0.0 occurrences82–82 Mya — about 0.0 occurrences82–82 Mya — about 0.0 occurrences82–81 Mya — about 0.0 occurrences81–81 Mya — about 0.0 occurrences81–80 Mya — about 0.0 occurrences80–80 Mya — about 0.0 occurrences80–80 Mya — about 0.0 occurrences80–79 Mya — about 0.0 occurrences79–79 Mya — about 0.0 occurrences79–78 Mya — about 0.0 occurrences78–78 Mya — about 0.0 occurrences78–77 Mya — about 0.0 occurrences77–77 Mya — about 0.0 occurrences77–77 Mya — about 0.0 occurrences77–76 Mya — about 0.0 occurrences76–76 Mya — about 0.0 occurrences76–75 Mya — about 0.0 occurrences75–75 Mya — about 0.0 occurrences75–75 Mya — about 0.0 occurrences75–74 Mya — about 0.0 occurrences74–74 Mya — about 0.0 occurrences74–73 Mya — about 0.0 occurrences73–73 Mya — about 0.0 occurrences73–73 Mya — about 0.0 occurrences73–72 Mya — about 0.0 occurrences84.1 Mya71.7 Mya

1 occurrence of Trochocyathus taylorensis 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

1 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

1 formation

Taylor Marl — 30.32°N, 97.63°W

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

Trochocyathus taylorensis and its relatives

Late Cretaceous

Where Trochocyathus taylorensis and its relatives were recorded in the Late Cretaceous.

Found in the same rock

The Paleobiology Database records no fossil sites for Trochocyathus taylorensis, so there is nothing to compare it with.

Entered from

1 reference

Each of the 1 occurrence 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 Trochocyathus taylorensis 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 Trochocyathus taylorensis, or no answer at all. This entry cannot say which.

No 3D scan of Trochocyathus taylorensis 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 itTrochocyathus through timeFormations of the Late CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Wells 1933