Kindbladia affinis

Kindbladia affinis

Conroy, E. A.; Rowell, Albert J. · CC BY 4.0 · via GBIF. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.

On record

Recorded, not inferred
Sits inside
KindbladiaPBDB
Diet
carnivorePBDB, for Trilobita
Life habit
low-level epifaunalPBDB, for Trilobita
Motility
fast-movingPBDB, for Trilobita
Vision
well-developedPBDB, for Dokimokephalidae
Environment
marinePBDB, for Trilobita

Time the record covers

At most 11 million years on record.

Every occurrence read is dated to somewhere between 497 Mya and 486.85 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Cambrian — about 13 of 13 occurrencesCambrianOrdovician — about 0 of 13 occurrences497–497 Mya — about 0.7 occurrences497–496 Mya — about 1 occurrence496–496 Mya — about 1 occurrence496–496 Mya — about 1 occurrence496–495 Mya — about 1 occurrence495–495 Mya — about 1 occurrence495–495 Mya — about 1 occurrence495–494 Mya — about 1 occurrence494–494 Mya — about 1 occurrence494–493 Mya — about 0.9 occurrences493–493 Mya — about 0.1 occurrences493–493 Mya — about 0.1 occurrences493–492 Mya — about 0.1 occurrences492–492 Mya — about 0.1 occurrences492–492 Mya — about 0.1 occurrences492–491 Mya — about 0.1 occurrences491–491 Mya — about 0.1 occurrences491–490 Mya — about 0.1 occurrences490–490 Mya — about 0.1 occurrences490–490 Mya — about 0.1 occurrences490–489 Mya — about 0.1 occurrences489–489 Mya — about 0.1 occurrences489–489 Mya — about 0.1 occurrences489–488 Mya — about 0.1 occurrences488–488 Mya — about 0.1 occurrences488–487 Mya — about 0.1 occurrences487–487 Mya — about 0.1 occurrences487–487 Mya — about 0.1 occurrences497.5 Mya486.4 Mya

13 occurrences of Kindbladia affinis on record, most of them in the Cambrian. 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

13 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

6 formations

Davis — 37.77°N, 90.52°WCorset Spring Shale — 38.52°N, 114.97°WCorset Spring Shale — 38.87°N, 114.32°WDunderberg Shale — 39.97°N, 114.88°WWindfall — 39.45°N, 115.97°WNopah — 39.00°N, 116.00°WOrr — 38.70°N, 113.44°W

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The named rock units Kindbladia affinis has been recovered from, largest first. Drawn where the rock is now, not where it formed. 1 occurrence has no formation on record, which is common for older literature.

Kindbladia affinis and its relatives

Cambrian

Where Kindbladia affinis and its relatives were recorded in the Cambrian.

Found in the same rock

23 taxa

The Paleobiology Database records 13 sites for Kindbladia affinis, 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

4 references

Each of the 13 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. Entries link to doi.org where the Paleobiology Database holds an identifier, and to its own record where it does not. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content1

Picture of Kindbladia affinis

Source
GBIF
Credit
Conroy, E. A.; Rowell, Albert J.
Licence
CC BY 4.0
Commercial use
the licence allows it

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

Occurrence data from the Paleobiology Database, CC BY 4.0. (Walcott 1884)