Claraia extrema

No picture of Claraia extrema 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 Claraia extrema, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
ClaraiaPBDB
Diet
suspension feederPBDB, for Pectinida
Life habit
epifaunalPBDB, for Pectinida
Motility
stationaryPBDB, for Pectinida
Vision
blindPBDB, for Bivalvia
Environment
marinePBDB, for Pectinida

Time the record covers

At least 300 thousand years on record.

The record covers at least 251.1 Mya to 250.8 Mya. No occurrence read is dated outside 251.902 Mya to 248.6 Mya.

Permian — about 0 of 11 occurrencesEarly Triassic — about 11 of 11 occurrencesEarly Triassic252–252 Mya — about 0.7 occurrences252–252 Mya — about 1 occurrence252–252 Mya — about 1 occurrence252–251 Mya — about 1 occurrence251–251 Mya — about 1 occurrence251–251 Mya — about 1 occurrence251–251 Mya — about 1.0 occurrences251–251 Mya — about 1.0 occurrences251–251 Mya — about 0.2 occurrences251–251 Mya — about 0.1 occurrences251–250 Mya — about 0.1 occurrences250–250 Mya — about 0.1 occurrences250–250 Mya — about 0.1 occurrences250–250 Mya — about 0.1 occurrences250–250 Mya — about 0.1 occurrences250–250 Mya — about 0.1 occurrences250–250 Mya — about 0.1 occurrences250–249 Mya — about 0.1 occurrences249–249 Mya — about 0.1 occurrences249–249 Mya — about 0.1 occurrences249–249 Mya — about 0.1 occurrences249–249 Mya — about 0.1 occurrences249–249 Mya — about 0.1 occurrences249–249 Mya — about 0.0 occurrences251.1 Mya – 250.8 Mya252.4 Mya248.1 Mya

11 occurrences of Claraia extrema on record, most of them in the Early Triassic. 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

11 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

4 formations

Elikah — 30.89°N, 53.21°EKhunamuh — 34.00°N, 75.00°EKhunamuh — 34.08°N, 74.98°EWordie Creek — 74.00°N, 21.49°WThaynes — 42.26°N, 111.43°W

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

Claraia extrema and its relatives

Early Triassic

Where Claraia extrema and its relatives were recorded in the Early Triassic.

Found in the same rock

19 taxa

The Paleobiology Database records 11 sites for Claraia extrema, and this reads all of them. The number is how many of those sites it was catalogued from too.

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

5 references

Each of the 11 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 Claraia extrema 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 Claraia extrema, or no answer at all. This entry cannot say which.

No 3D scan of Claraia extrema 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

Occurrence data from the Paleobiology Database, CC BY 4.0. Spath 1935