Tremanotus dilatatus

No picture of Tremanotus dilatatus 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 Tremanotus dilatatus, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
TremanotusPBDB
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 23 million years on record.

The record covers at least 448.8 Mya to 425 Mya. No occurrence read is dated outside 449.2 Mya to 422.7 Mya.

Ordovician — about 1 of 5 occurrencesOrdovicianSilurian — about 4 of 5 occurrencesSilurian450–449 Mya — about 1.0 occurrences449–448 Mya — about 0.0 occurrences443–442 Mya — about 0.6 occurrences442–441 Mya — about 0.7 occurrences441–441 Mya — about 0.7 occurrences441–440 Mya — about 0.0 occurrences431–430 Mya — about 0.0 occurrences430–430 Mya — about 0.2 occurrences430–429 Mya — about 0.2 occurrences429–428 Mya — about 0.2 occurrences428–427 Mya — about 0.2 occurrences427–426 Mya — about 0.0 occurrences426–425 Mya — about 0.0 occurrences425–424 Mya — about 0.4 occurrences424–423 Mya — about 0.4 occurrences423–422 Mya — about 0.2 occurrences448.8 Mya425 Mya449.7 Mya422.2 Mya

5 occurrences of Tremanotus dilatatus 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

5 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

5 formations

Much Wenlock Limestone — 52.50°N, 2.08°WSaugh Hill Grits — 55.25°N, 4.85°WMulloch Hill — 55.24°N, 4.84°WKilley Bridge — 54.60°N, 6.60°WAymestry Limestone — 52.03°N, 2.42°W

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

Tremanotus dilatatus and its relatives

Silurian

Where Tremanotus dilatatus and its relatives were recorded in the Silurian.

Found in the same rock

175 taxa

The Paleobiology Database records 5 sites for Tremanotus dilatatus, 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 5 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 doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content0

No picture of Tremanotus dilatatus 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 Tremanotus dilatatus, or no answer at all. This entry cannot say which.

No 3D scan of Tremanotus dilatatus 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 itTremanotus through timeFormations of the SilurianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (de Sowerby and Murchison 1839)