Pentlandina lewisii lewisii

No picture of Pentlandina lewisii lewisii was found. Wikipedia and Wikidata were searched and had none. iDigBio and GBIF were not searched: the Paleobiology Database does not place Pentlandina lewisii lewisii firmly enough to tell it from something else bearing the same name, and a search on the name alone returns whichever of them was photographed. Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.

Time the record covers

At most 2.3 million years on record.

Every occurrence read is dated to somewhere between 432.9 Mya and 430.6 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Silurian — about 2 of 2 occurrencesSilurian433–433 Mya — about 0.0 occurrences433–433 Mya — about 0.1 occurrences433–433 Mya — about 0.1 occurrences433–433 Mya — about 0.1 occurrences433–432 Mya — about 0.1 occurrences432–432 Mya — about 0.1 occurrences432–432 Mya — about 0.1 occurrences432–432 Mya — about 0.1 occurrences432–432 Mya — about 0.1 occurrences432–432 Mya — about 0.1 occurrences432–432 Mya — about 0.1 occurrences432–432 Mya — about 0.1 occurrences432–432 Mya — about 0.1 occurrences432–431 Mya — about 0.1 occurrences431–431 Mya — about 0.1 occurrences431–431 Mya — about 0.1 occurrences431–431 Mya — about 0.1 occurrences431–431 Mya — about 0.1 occurrences431–431 Mya — about 0.1 occurrences431–431 Mya — about 0.1 occurrences431–431 Mya — about 0.1 occurrences431–431 Mya — about 0.0 occurrences433.4 Mya430.1 Mya

2 occurrences of Pentlandina lewisii lewisii 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

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

Slite Beds — 57.72°N, 18.80°EUpper Visby — 57.63°N, 18.30°E

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

Pentlandina lewisii lewisii and its relatives

Silurian

Where Pentlandina lewisii lewisii and its relatives were recorded in the Silurian.

Found in the same rock

64 taxa

The Paleobiology Database records 2 sites for Pentlandina lewisii lewisii, 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 doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content0

No picture of Pentlandina lewisii lewisii was found. Wikipedia and Wikidata were searched and had none.

iDigBio and GBIF were not searched: the Paleobiology Database does not place Pentlandina lewisii lewisii firmly enough to tell it from something else bearing the same name, and a search on the name alone returns whichever of them was photographed.

Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.

No 3D scan of Pentlandina lewisii lewisii was found in MorphoSource and Sketchfab.

Smithsonian Open Access was 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 itFormations of the SilurianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0.