Skljarella cracens

No picture of Skljarella cracens 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 Skljarella cracens, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
SkljarellaPBDB
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 4 million years on record.

The one occurrence read is dated to somewhere between 481.1 Mya and 477.1 Mya, which is a dating window rather than a span.

Ordovician — about 1 of 1 occurrenceOrdovician481–481 Mya — about 0.0 occurrences481–481 Mya — about 0.0 occurrences481–481 Mya — about 0.0 occurrences481–480 Mya — about 0.0 occurrences480–480 Mya — about 0.0 occurrences480–480 Mya — about 0.0 occurrences480–480 Mya — about 0.0 occurrences480–480 Mya — about 0.0 occurrences480–480 Mya — about 0.0 occurrences480–479 Mya — about 0.0 occurrences479–479 Mya — about 0.0 occurrences479–479 Mya — about 0.0 occurrences479–479 Mya — about 0.0 occurrences479–479 Mya — about 0.0 occurrences479–479 Mya — about 0.0 occurrences479–478 Mya — about 0.0 occurrences478–478 Mya — about 0.0 occurrences478–478 Mya — about 0.0 occurrences478–478 Mya — about 0.0 occurrences478–478 Mya — about 0.0 occurrences478–478 Mya — about 0.0 occurrences478–477 Mya — about 0.0 occurrences477–477 Mya — about 0.0 occurrences477–477 Mya — about 0.0 occurrences481.6 Mya476.6 Mya

1 occurrence of Skljarella cracens 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

Shineton Shales — 52.63°N, 2.66°W

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

Skljarella cracens and its relatives

Ordovician

Where Skljarella cracens and its relatives were recorded in the Ordovician.

Found in the same rock

16 taxa

The Paleobiology Database records 1 site for Skljarella cracens, 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 doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content0

No picture of Skljarella cracens 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 Skljarella cracens, or no answer at all. This entry cannot say which.

No 3D scan of Skljarella cracens 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 itSkljarella through timeFormations of the OrdovicianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Fortey and Owens 1991