Calyptraea (Galerus) vancouverensis

No picture of Calyptraea (Galerus) vancouverensis was found. Wikipedia, Wikidata and Smithsonian Open Access were searched and had none. iDigBio and GBIF were not searched: the Paleobiology Database does not place Calyptraea (Galerus) vancouverensis 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.

Time the record covers

At most 4.3 million years on record.

Every occurrence read is dated to somewhere between 27.3 Mya and 23.04 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Oligocene — about 2 of 2 occurrencesOligoceneMiocene — about 0 of 2 occurrences27–27 Mya — about 0.0 occurrences27–27 Mya — about 0.1 occurrences27–27 Mya — about 0.1 occurrences27–27 Mya — about 0.1 occurrences27–27 Mya — about 0.1 occurrences27–26 Mya — about 0.1 occurrences26–26 Mya — about 0.1 occurrences26–26 Mya — about 0.1 occurrences26–26 Mya — about 0.1 occurrences26–26 Mya — about 0.1 occurrences26–26 Mya — about 0.1 occurrences26–25 Mya — about 0.1 occurrences25–25 Mya — about 0.1 occurrences25–25 Mya — about 0.1 occurrences25–25 Mya — about 0.1 occurrences25–25 Mya — about 0.1 occurrences25–24 Mya — about 0.1 occurrences24–24 Mya — about 0.1 occurrences24–24 Mya — about 0.1 occurrences24–24 Mya — about 0.1 occurrences24–24 Mya — about 0.1 occurrences24–24 Mya — about 0.1 occurrences24–23 Mya — about 0.1 occurrences23–23 Mya — about 0.1 occurrences23–23 Mya — about 0.1 occurrences23–23 Mya — about 0.0 occurrences27.8 Mya22.5 Mya

2 occurrences of Calyptraea (Galerus) vancouverensis on record, most of them in the Oligocene. The Paleobiology Database records this as a living group, and the chart stops with its fossils rather than at the present. 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

Pysht — 48.17°N, 123.94°WBlakeley — 47.95°N, 122.07°W

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The named rock units Calyptraea (Galerus) vancouverensis has been recovered from, largest first. Drawn where the rock is now, not where it formed.

Calyptraea (Galerus) vancouverensis and its relatives

Oligocene

Where Calyptraea (Galerus) vancouverensis and its relatives were recorded in the Oligocene.

Found in the same rock

31 taxa

The Paleobiology Database records 2 sites for Calyptraea (Galerus) vancouverensis, 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 the Paleobiology Database's own record for the work.

Media and terms

Media content0

No picture of Calyptraea (Galerus) vancouverensis was found. Wikipedia, Wikidata and Smithsonian Open Access were searched and had none.

iDigBio and GBIF were not searched: the Paleobiology Database does not place Calyptraea (Galerus) vancouverensis 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.

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

What may have been alongside itFormations of the OligoceneThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Clark and Arnold 1923