Camosphaeridium williereae

No picture of Camosphaeridium williereae was found. Wikipedia and Wikidata were searched and had none. iDigBio and GBIF were not searched: the Paleobiology Database does not place Camosphaeridium williereae 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 5.7 million years on record.

The one occurrence read is dated to somewhere between 438.6 Mya and 432.9 Mya, which is a dating window rather than a span.

Silurian — about 1 of 1 occurrenceSilurian439–438 Mya — about 0.0 occurrences438–438 Mya — about 0.0 occurrences438–438 Mya — about 0.0 occurrences438–438 Mya — about 0.0 occurrences438–438 Mya — about 0.0 occurrences438–437 Mya — about 0.0 occurrences437–437 Mya — about 0.0 occurrences437–437 Mya — about 0.0 occurrences437–437 Mya — about 0.0 occurrences437–436 Mya — about 0.0 occurrences436–436 Mya — about 0.0 occurrences436–436 Mya — about 0.0 occurrences436–436 Mya — about 0.0 occurrences436–436 Mya — about 0.0 occurrences436–435 Mya — about 0.0 occurrences435–435 Mya — about 0.0 occurrences435–435 Mya — about 0.0 occurrences435–435 Mya — about 0.0 occurrences435–434 Mya — about 0.0 occurrences434–434 Mya — about 0.0 occurrences434–434 Mya — about 0.0 occurrences434–434 Mya — about 0.0 occurrences434–434 Mya — about 0.0 occurrences434–433 Mya — about 0.0 occurrences433–433 Mya — about 0.0 occurrences433–433 Mya — about 0.0 occurrences439.1 Mya432.4 Mya

1 occurrence of Camosphaeridium williereae 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

1 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

1 formation

Agidyl — 67.35°N, 104.04°E

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

Camosphaeridium williereae and its relatives

Silurian

Where Camosphaeridium williereae and its relatives were recorded in the Silurian.

Found in the same rock

80 taxa

The Paleobiology Database records 1 site for Camosphaeridium williereae, 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 1 occurrence 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 Camosphaeridium williereae was found. Wikipedia and Wikidata were searched and had none.

iDigBio and GBIF were not searched: the Paleobiology Database does not place Camosphaeridium williereae 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 Camosphaeridium williereae 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 itFormations of the SilurianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0.