Johncarteria devia

No picture of Johncarteria devia 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 Johncarteria devia, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
JohncarteriaPBDB
Diet
suspension feederPBDB, for Spiriferida
Life habit
epifaunalPBDB, for Spiriferida
Motility
stationaryPBDB, for Spiriferida
Vision
blindPBDB, for Rhynchonellata
Environment
marinePBDB, for Lophophorata

Time the record covers

At most 2.7 million years on record.

Every occurrence read is dated to somewhere between 266.9 Mya and 264.28 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Permian — about 20 of 20 occurrencesPermian267–267 Mya — about 0.8 occurrences267–267 Mya — about 0.9 occurrences267–267 Mya — about 0.9 occurrences267–266 Mya — about 0.9 occurrences266–266 Mya — about 0.9 occurrences266–266 Mya — about 0.9 occurrences266–266 Mya — about 0.9 occurrences266–266 Mya — about 0.9 occurrences266–266 Mya — about 0.9 occurrences266–266 Mya — about 0.9 occurrences266–266 Mya — about 0.9 occurrences266–265 Mya — about 0.9 occurrences265–265 Mya — about 0.9 occurrences265–265 Mya — about 0.9 occurrences265–265 Mya — about 0.9 occurrences265–265 Mya — about 0.9 occurrences265–265 Mya — about 0.9 occurrences265–265 Mya — about 0.9 occurrences265–265 Mya — about 0.9 occurrences265–265 Mya — about 0.9 occurrences265–264 Mya — about 0.9 occurrences264–264 Mya — about 0.8 occurrences267.4 Mya263.78 Mya

20 occurrences of Johncarteria devia on record, most of them in the Permian. 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

20 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

Amb — 32.50°N, 71.93°EAmb — 32.72°N, 71.75°EAmb — 32.63°N, 71.75°EAmb — 32.75°N, 71.71°EAmb — 32.70°N, 71.68°EAmb — 32.55°N, 71.83°E

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

Johncarteria devia and its relatives

Permian

Where Johncarteria devia and its relatives were recorded in the Permian.

Found in the same rock

79 taxa

The Paleobiology Database records 20 sites for Johncarteria devia, 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 20 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 Johncarteria devia 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 Johncarteria devia, or no answer at all. This entry cannot say which.

No 3D scan of Johncarteria devia 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.

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Occurrence data from the Paleobiology Database, CC BY 4.0. (Reed 1944)