Cladophyllia excelsa

No picture of Cladophyllia excelsa 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 Cladophyllia excelsa, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
CladophylliaPBDB
Diet
microcarnivore, photosymbioticPBDB, for Scleractinia
Life habit
intermediate-level epifaunal, colonial, clonalPBDB, for Scleractinia
Motility
stationary, attachedPBDB, for Scleractinia
Vision
blindPBDB, for Anthozoa
Environment
marinePBDB, for Scleractinia

Time the record covers

At least 12 million years on record.

The record covers at least 157.9 Mya to 145.06 Mya. No occurrence read is dated outside 159 Mya to 143.1 Mya.

Late Jurassic — about 3 of 3 occurrencesLate JurassicEarly Cretaceous — about 0 of 3 occurrences160–159 Mya — about 0.1 occurrences159–158 Mya — about 0.5 occurrences158–158 Mya — about 0.4 occurrences155–154 Mya — about 0.1 occurrences154–154 Mya — about 0.2 occurrences154–153 Mya — about 0.2 occurrences153–153 Mya — about 0.2 occurrences153–152 Mya — about 0.2 occurrences145–145 Mya — about 0.1 occurrences145–144 Mya — about 0.3 occurrences144–144 Mya — about 0.3 occurrences144–143 Mya — about 0.3 occurrences143–143 Mya — about 0.0 occurrences157.9 Mya145.06 Mya159.5 Mya142.6 Mya

3 occurrences of Cladophyllia excelsa on record, most of them in the Late Jurassic. 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

3 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

Stramberk Limestone — 49.58°N, 18.12°EKorond — 34.17°N, 56.83°EAntalo — 13.64°N, 39.44°E

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

Cladophyllia excelsa and its relatives

Late Jurassic

Where Cladophyllia excelsa and its relatives were recorded in the Late Jurassic.

Found in the same rock

210 taxa

The Paleobiology Database records 3 sites for Cladophyllia excelsa, 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

3 references

Each of the 3 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 content0

No picture of Cladophyllia excelsa 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 Cladophyllia excelsa, or no answer at all. This entry cannot say which.

No 3D scan of Cladophyllia excelsa 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 itCladophyllia through timeFormations of the Late JurassicThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (Koby 1888)