Spinilingula

Spinilingula

Rowell, Albert J.; Krause, F. F. · 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
ObolinaePBDB
Diet
suspension feederPBDB, for Obolidae
Life habit
low-level epifaunalPBDB, for Obolidae
Motility
stationary, attachedPBDB, for Obolidae
Vision
blindPBDB, for Lingulata
Environment
marinePBDB, for Lophophorata

Time the record covers

At least 17 million years on record.

The record covers at least 477.1 Mya to 459.7 Mya. No occurrence read is dated outside 486.85 Mya to 457.3 Mya.

Cambrian — about 0 of 7 occurrencesOrdovician — about 7 of 7 occurrencesOrdovician487–486 Mya — about 0.1 occurrences486–485 Mya — about 0.2 occurrences485–484 Mya — about 0.2 occurrences484–483 Mya — about 0.2 occurrences483–482 Mya — about 0.2 occurrences482–481 Mya — about 0.2 occurrences481–480 Mya — about 0.2 occurrences480–479 Mya — about 0.2 occurrences479–478 Mya — about 0.2 occurrences478–477 Mya — about 0.2 occurrences477–476 Mya — about 0.0 occurrences472–471 Mya — about 0.0 occurrences471–470 Mya — about 0.1 occurrences470–469 Mya — about 0.1 occurrences469–468 Mya — about 0.1 occurrences468–467 Mya — about 0.2 occurrences467–466 Mya — about 0.2 occurrences466–465 Mya — about 0.2 occurrences465–464 Mya — about 0.2 occurrences464–463 Mya — about 0.2 occurrences463–462 Mya — about 0.2 occurrences462–461 Mya — about 0.7 occurrences461–460 Mya — about 1.0 occurrences460–459 Mya — about 1.0 occurrences459–458 Mya — about 0.7 occurrences458–457 Mya — about 0.0 occurrences477.1 Mya459.7 Mya487.4 Mya456.7 Mya

7 occurrences of Spinilingula 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

7 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

Fillmore — 38.87°N, 113.35°WPratt Ferry — 33.02°N, 87.08°WUzunbulak — 43.83°N, 75.33°EGullhögen — 58.38°N, 13.82°EFurudal — 62.97°N, 14.48°EFolkeslunda Limestone — 62.97°N, 14.48°E

Loading coastlines…

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

Spinilingula and its relatives

Ordovician

Where Spinilingula and its relatives were recorded in the Ordovician.

Found in the same rock

118 taxa

The Paleobiology Database records 7 sites for Spinilingula, 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

4 references

Each of the 7 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 Spinilingula

Source
GBIF
Credit
Rowell, Albert J.; Krause, F. F.
Licence
CC BY 4.0
Commercial use
the licence allows it

No 3D scan of Spinilingula 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 itObolinae through timeFormations of the OrdovicianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Cooper 1956