Erratencrinurus uncatus

No picture of Erratencrinurus uncatus 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 Erratencrinurus uncatus, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
ErratencrinurusPBDB
Diet
carnivorePBDB, for Trilobita
Life habit
low-level epifaunalPBDB, for Trilobita
Motility
fast-movingPBDB, for Trilobita
Environment
marinePBDB, for Trilobita

Time the record covers

At most 3.5 million years on record.

The one occurrence read is dated to somewhere between 457.3 Mya and 453.8 Mya, which is a dating window rather than a span.

Ordovician — about 1 of 1 occurrenceOrdovician457–457 Mya — about 0.0 occurrences457–457 Mya — about 0.0 occurrences457–457 Mya — about 0.0 occurrences457–457 Mya — about 0.0 occurrences457–457 Mya — about 0.0 occurrences457–456 Mya — about 0.0 occurrences456–456 Mya — about 0.0 occurrences456–456 Mya — about 0.0 occurrences456–456 Mya — about 0.0 occurrences456–456 Mya — about 0.0 occurrences456–456 Mya — about 0.0 occurrences456–456 Mya — about 0.0 occurrences456–455 Mya — about 0.0 occurrences455–455 Mya — about 0.0 occurrences455–455 Mya — about 0.0 occurrences455–455 Mya — about 0.0 occurrences455–455 Mya — about 0.0 occurrences455–455 Mya — about 0.0 occurrences455–455 Mya — about 0.0 occurrences455–454 Mya — about 0.0 occurrences454–454 Mya — about 0.0 occurrences454–454 Mya — about 0.0 occurrences454–454 Mya — about 0.0 occurrences454–454 Mya — about 0.0 occurrences457.8 Mya453.3 Mya

1 occurrence of Erratencrinurus uncatus on record, most of them in the Ordovician. 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

1 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

1 formation

Oranda — 38.52°N, 78.89°W

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

Erratencrinurus uncatus and its relatives

Ordovician

Where Erratencrinurus uncatus and its relatives were recorded in the Ordovician.

Found in the same rock

16 taxa

The Paleobiology Database records 1 site for Erratencrinurus uncatus, and this reads all of them. The number is how many of those sites it was catalogued from too.

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

1 reference

Each of the 1 occurrence 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 Erratencrinurus uncatus 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 Erratencrinurus uncatus, or no answer at all. This entry cannot say which.

No 3D scan of Erratencrinurus uncatus 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 itErratencrinurus through timeFormations of the OrdovicianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (Evitt and Tripp 1977)