Comophyllia corrugata
No picture of Comophyllia corrugata was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Comophyllia corrugata, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- ComophylliaPBDB
- Diet
- photosymbiotic, suspension feederPBDB, for Latomeandridae
- Life habit
- colonial, clonalPBDB, for Latomeandridae
- Motility
- stationary, attachedPBDB, for Scleractinia
- Vision
- blindPBDB, for Anthozoa
- Environment
- marinePBDB, for Scleractinia
Time the record covers
At least 5.6 million years on record.
The record covers at least 154.8 Mya to 149.2 Mya. No occurrence read is dated outside 161.5 Mya to 145.06 Mya.
5 occurrences of Comophyllia corrugata 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
5 occurrences- Late Jurassic100%
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
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The named rock units Comophyllia corrugata has been recovered from, largest first. Drawn where the rock is now, not where it formed. 2 occurrences have no formation on record, which is common for older literature.
Comophyllia corrugata and its relatives
Late JurassicWhere Comophyllia corrugata and its relatives were recorded in the Late Jurassic.
Found in the same rock
194 taxa- Amphiastrea basaltiformis2 sites
- Aplosmilia semisulcata2 sites
- Calamophylliopsis flabellum2 sites
- Dimorphastrea dubia2 sites
- Heliocoenia (Decaheliocoenia) variabilis2 sites
- Ovalastrea michelini2 sites
- Pruvostastraea labyrinthiformis2 sites
- Psammogyra choffati2 sites
- Stylina excelsa2 sites
- Acrosmilia1 site
- Acrosmilia depressa1 site
- Acrosmilia robusta1 site
- Actinaraea1 site
- Actinaraea granulata1 site
- Actinastrea1 site
- Actinastrea furcata1 site
- Actinostreon gregarea1 site
- Actinostromaria tokadiensis1 site
- Adelocoenia limbata1 site
- Adelocoenia pistillum1 site
- Allocoenia trochiformis1 site
- Aplosmilia1 site
- Aplosmilia aspera1 site
- Aplosmilia distans1 site
The Paleobiology Database records 3 sites for Comophyllia corrugata, 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- Etude stratigraphique et paléontologique des formations à madréporaires du Jurassique supérieur du Jura et de l'est du Bassin de Paris3
- Die oberjurassische Korallenfazies von Algarve (Südportugal) [The Upper Jurassic coral facies of Algarve (Southern Portugal)]1
- Die oberjurassische Korallenfauna von Württemberg1
Each of the 5 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 Comophyllia corrugata was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none.
GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Comophyllia corrugata, or no answer at all. This entry cannot say which.
No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itComophyllia through timeFormations of the Late JurassicThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Milne-Edwards and Haime 1849)