Axosmilia infundibuliformis

No picture of Axosmilia infundibuliformis was found. Wikipedia, Wikidata and iDigBio were searched and had none. 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 Axosmilia infundibuliformis, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
AxosmiliaPBDB
Diet
microcarnivorePBDB, for Axosmiliidae
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 39 million years on record.

The record covers at least 152.21 Mya to 113.2 Mya. No occurrence read is dated outside 154.8 Mya to 110.1 Mya.

Late Jurassic — about 12 of 13 occurrencesLate JurassicEarly Cretaceous — about 1 of 13 occurrencesEarly Cretaceous156–154 Mya — about 2 occurrences154–153 Mya — about 4 occurrences153–151 Mya — about 1 occurrence151–149 Mya — about 0.3 occurrences149–148 Mya — about 1.0 occurrences148–146 Mya — about 1 occurrence146–145 Mya — about 1 occurrence145–143 Mya — about 2 occurrences143–142 Mya — about 0.2 occurrences114–112 Mya — about 0.3 occurrences112–111 Mya — about 0.5 occurrences111–109 Mya — about 0.2 occurrences152.21 Mya113.2 Mya155.7 Mya109.2 Mya

13 occurrences of Axosmilia infundibuliformis 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

13 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

2 formations

Massenkalk — 48.68°N, 10.22°EStramberk Limestone — 49.58°N, 18.12°E

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The named rock units Axosmilia infundibuliformis has been recovered from, largest first. Drawn where the rock is now, not where it formed. 11 occurrences have no formation on record, which is common for older literature.

Axosmilia infundibuliformis and its relatives

Late Jurassic

Where Axosmilia infundibuliformis and its relatives were recorded in the Late Jurassic.

Found in the same rock

444 taxa

The Paleobiology Database records 13 sites for Axosmilia infundibuliformis, 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

6 references

Each of the 13 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 Axosmilia infundibuliformis was found. Wikipedia, Wikidata and iDigBio were searched and had none.

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 Axosmilia infundibuliformis, or no answer at all. This entry cannot say which.

No 3D scan of Axosmilia infundibuliformis 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

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