Eocryptaenia singularis

No picture of Eocryptaenia singularis was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Eocryptaenia singularis, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
EocryptaeniaPBDB
Diet
detritivorePBDB, for Eotomarioidea
Life habit
epifaunalPBDB, for Eotomarioidea
Motility
slow-movingPBDB, for Eotomarioidea
Vision
limitedPBDB, for Eotomarioidea
Environment
coastal,marinePBDB, for Murchisoniina

Time the record covers

At most 6.4 million years on record.

Every occurrence read is dated to somewhere between 449.5 Mya and 443.1 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Ordovician — about 2 of 2 occurrencesOrdovicianSilurian — about 0 of 2 occurrences450–449 Mya — about 0.0 occurrences449–449 Mya — about 0.0 occurrences449–449 Mya — about 0.0 occurrences449–449 Mya — about 0.0 occurrences449–448 Mya — about 0.0 occurrences448–448 Mya — about 0.0 occurrences448–448 Mya — about 0.0 occurrences448–448 Mya — about 0.0 occurrences448–447 Mya — about 0.0 occurrences447–447 Mya — about 0.0 occurrences447–447 Mya — about 0.0 occurrences447–447 Mya — about 0.0 occurrences447–446 Mya — about 0.0 occurrences446–446 Mya — about 0.0 occurrences446–446 Mya — about 0.0 occurrences446–446 Mya — about 0.0 occurrences446–445 Mya — about 0.0 occurrences445–445 Mya — about 0.1 occurrences445–445 Mya — about 0.2 occurrences445–445 Mya — about 0.2 occurrences445–444 Mya — about 0.2 occurrences444–444 Mya — about 0.2 occurrences444–444 Mya — about 0.2 occurrences444–444 Mya — about 0.2 occurrences444–443 Mya — about 0.2 occurrences443–443 Mya — about 0.2 occurrences450 Mya442.6 Mya

2 occurrences of Eocryptaenia singularis 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

2 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

Boda Limestone — 60.17°N, 14.70°EÄrina — 59.19°N, 26.19°E

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

Eocryptaenia singularis and its relatives

Ordovician

Where Eocryptaenia singularis and its relatives were recorded in the Ordovician.

Found in the same rock

60 taxa

The Paleobiology Database records 2 sites for Eocryptaenia singularis, 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

1 reference

Each of the 2 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. Each entry links to the Paleobiology Database's own record for the work.

Media and terms

Media content0

No picture of Eocryptaenia singularis was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none.

GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Eocryptaenia singularis, or no answer at all. This entry cannot say which.

No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.

This is what the site found, which is not the same as what exists.

Keep going

What may have been alongside itEocryptaenia through timeFormations of the OrdovicianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Koken and Perner 1925