Placoseris eturbensis

No picture of Placoseris eturbensis was found. Wikipedia and Wikidata were searched and had none. iDigBio and GBIF were not searched: the Paleobiology Database does not place Placoseris eturbensis firmly enough to tell it from something else bearing the same name, and a search on the name alone returns whichever of them was photographed. Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.

On record

Recorded, not inferred
Sits inside
PlacoserisPBDB

Time the record covers

At least 12 million years on record.

The record covers at least 113.2 Mya to 100.5 Mya. No occurrence read is dated outside 121.4 Mya to 93.9 Mya.

Early Cretaceous — about 1 of 16 occurrencesEarly CretaceousLate Cretaceous — about 15 of 16 occurrencesLate Cretaceous122–121 Mya — about 0.0 occurrences121–120 Mya — about 0.1 occurrences120–119 Mya — about 0.1 occurrences119–118 Mya — about 0.1 occurrences118–117 Mya — about 0.1 occurrences117–116 Mya — about 0.1 occurrences116–115 Mya — about 0.1 occurrences115–114 Mya — about 0.1 occurrences114–113 Mya — about 0.1 occurrences113–112 Mya — about 0.0 occurrences101–100 Mya — about 1 occurrence100–99 Mya — about 2 occurrences99–98 Mya — about 2 occurrences98–97 Mya — about 2 occurrences97–96 Mya — about 2 occurrences96–95 Mya — about 2 occurrences95–94 Mya — about 2 occurrences94–93 Mya — about 0.9 occurrences113.2 Mya100.5 Mya122 Mya93.3 Mya

16 occurrences of Placoseris eturbensis on record. 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

16 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

5 formations

Korycany — 50.27°N, 14.48°EKorycany — 50.28°N, 14.33°EKorycany — 50.20°N, 14.43°EDölzschen — 51.03°N, 13.70°ELangshan — 33.45°N, 79.70°EBranderfleck — 47.63°N, 11.67°EAltamira — 43.38°N, 4.22°W

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The named rock units Placoseris eturbensis has been recovered from, largest first. Drawn where the rock is now, not where it formed. 1 occurrence has no formation on record, which is common for older literature.

Found in the same rock

129 taxa

The Paleobiology Database records 4 sites for Placoseris eturbensis, 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

7 references

Each of the 16 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 Placoseris eturbensis was found. Wikipedia and Wikidata were searched and had none.

iDigBio and GBIF were not searched: the Paleobiology Database does not place Placoseris eturbensis firmly enough to tell it from something else bearing the same name, and a search on the name alone returns whichever of them was photographed.

Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.

No 3D scan of Placoseris eturbensis 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 itPlacoseris through timeThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (Fromentel 1857)