Boiotremus longitudinalis

Boiotremus longitudinalis

via GBIF · CC BY-NC 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
BoiotremusPBDB
Diet
detritivorePBDB, for Bucaniidae
Life habit
epifaunalPBDB, for Bucaniidae
Motility
actively mobilePBDB, for Bucaniidae
Vision
limitedPBDB, for Gastropoda
Environment
marinePBDB, for Bellerophontida

Time the record covers

At least 8.5 million years on record.

The record covers at least 433.5 Mya to 425 Mya. No occurrence read is dated outside 438.8 Mya to 422.7 Mya.

Silurian — about 14 of 14 occurrencesSilurian439–439 Mya — about 0.0 occurrences439–438 Mya — about 0.4 occurrences438–438 Mya — about 0.5 occurrences438–437 Mya — about 0.5 occurrences437–436 Mya — about 0.5 occurrences436–436 Mya — about 0.5 occurrences436–435 Mya — about 0.5 occurrences435–435 Mya — about 0.5 occurrences435–434 Mya — about 0.5 occurrences434–434 Mya — about 0.5 occurrences434–433 Mya — about 0.3 occurrences433–432 Mya — about 1 occurrence432–432 Mya — about 1 occurrence432–431 Mya — about 1 occurrence431–431 Mya — about 1 occurrence431–430 Mya — about 0.5 occurrences430–430 Mya — about 0.1 occurrences430–429 Mya — about 0.1 occurrences429–428 Mya — about 0.1 occurrences428–428 Mya — about 0.1 occurrences428–427 Mya — about 0.1 occurrences427–427 Mya — about 0.1 occurrences427–426 Mya — about 0.1 occurrences426–426 Mya — about 0.1 occurrences426–425 Mya — about 0.1 occurrences425–424 Mya — about 0.5 occurrences424–424 Mya — about 0.5 occurrences424–423 Mya — about 0.5 occurrences423–423 Mya — about 0.5 occurrences423–422 Mya — about 0.1 occurrences433.5 Mya425 Mya439.3 Mya422.2 Mya

14 occurrences of Boiotremus longitudinalis on record, most of them in the Silurian. 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

14 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

8 formations

Hogklint — 57.50°N, 18.55°ELower Visby — 57.50°N, 18.55°EUpper Visby — 57.50°N, 18.55°EBurgsvik Beds — 57.04°N, 18.28°ERumba — 58.84°N, 24.04°EKlinteberg Beds — 57.53°N, 18.43°EVik — 59.90°N, 10.52°ESlite — 57.74°N, 18.49°E

Loading coastlines…

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

Boiotremus longitudinalis and its relatives

Silurian

Where Boiotremus longitudinalis and its relatives were recorded in the Silurian.

Found in the same rock

134 taxa

The Paleobiology Database records 14 sites for Boiotremus longitudinalis, 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

5 references

Each of the 14 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 Boiotremus longitudinalis

Source
GBIF
Credit
via GBIF
Licence
CC BY-NC 4.0
Commercial use
the licence does not allow it

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

Occurrence data from the Paleobiology Database, CC BY 4.0. (Lindström 1884)