Protoseris

Protoseris

Choffat, Paul · CC BY 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
CalamophylliidaePBDB
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 33 million years on record.

The record covers at least 154.8 Mya to 121.4 Mya. No occurrence read is dated outside 161.5 Mya to 113.2 Mya.

Middle Jurassic — about 0 of 21 occurrencesLate Jurassic — about 13 of 21 occurrencesLate JurassicEarly Cretaceous — about 8 of 21 occurrencesEarly Cretaceous162–161 Mya — about 0.1 occurrences161–159 Mya — about 0.3 occurrences159–157 Mya — about 0.4 occurrences157–156 Mya — about 0.8 occurrences156–154 Mya — about 0.9 occurrences154–152 Mya — about 0.9 occurrences152–151 Mya — about 0.4 occurrences151–149 Mya — about 0.5 occurrences149–147 Mya — about 2 occurrences147–146 Mya — about 2 occurrences146–144 Mya — about 3 occurrences144–142 Mya — about 2 occurrences142–141 Mya — about 0.2 occurrences141–139 Mya — about 0.2 occurrences139–137 Mya — about 0.2 occurrences137–136 Mya — about 2 occurrences136–134 Mya — about 2 occurrences134–132 Mya — about 2 occurrences122–121 Mya — about 0.1 occurrences121–119 Mya — about 0.2 occurrences119–117 Mya — about 0.2 occurrences117–116 Mya — about 0.2 occurrences116–114 Mya — about 0.2 occurrences114–112 Mya — about 0.1 occurrences154.8 Mya121.4 Mya162 Mya112 Mya

21 occurrences of Protoseris 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

21 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

6 formations

Slivnitsa — 42.77°N, 22.75°EMassenkalk — 48.68°N, 10.22°EStramberk Limestone — 49.58°N, 18.12°ESteeple Ashton Coral Bed — 51.33°N, 1.83°WAmaral — 39.02°N, 9.12°WSwarzow Limestone — 50.18°N, 20.95°E

Loading coastlines…

The named rock units Protoseris has been recovered from, largest first. Drawn where the rock is now, not where it formed. 7 occurrences have no formation on record, which is common for older literature.

Protoseris and its relatives

Late Jurassic

Where Protoseris and its relatives were recorded in the Late Jurassic.

Found in the same rock

397 taxa

The Paleobiology Database records 9 sites for Protoseris, 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

11 references

Each of the 21 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 Protoseris

Source
GBIF
Credit
Choffat, Paul
Licence
CC BY 4.0
Commercial use
the licence allows it

No 3D scan of Protoseris 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

Occurrence data from the Paleobiology Database, CC BY 4.0. Milne-Edwards and Haime 1851