Conaspis

Conaspis

via iDigBio · via iDigBio. 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
DokimokephalidaePBDB
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 6 of 6 occurrencesCambrianOrdovician — about 0 of 6 occurrences497–497 Mya — about 0.1 occurrences497–496 Mya — about 0.1 occurrences496–496 Mya — about 0.1 occurrences496–496 Mya — about 0.1 occurrences496–495 Mya — about 0.1 occurrences495–495 Mya — about 0.1 occurrences495–495 Mya — about 0.1 occurrences495–494 Mya — about 0.1 occurrences494–494 Mya — about 0.1 occurrences494–493 Mya — about 0.2 occurrences493–493 Mya — about 0.4 occurrences493–493 Mya — about 0.4 occurrences493–492 Mya — about 0.4 occurrences492–492 Mya — about 0.4 occurrences492–492 Mya — about 0.4 occurrences492–491 Mya — about 0.4 occurrences491–491 Mya — about 0.4 occurrences491–490 Mya — about 0.4 occurrences490–490 Mya — about 0.4 occurrences490–490 Mya — about 0.4 occurrences490–489 Mya — about 0.4 occurrences489–489 Mya — about 0.4 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

6 occurrences of Conaspis 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

6 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

5 formations

Gatesburg — 41.38°N, 75.46°WFranconia — 44.52°N, 89.57°WDavis — 37.93°N, 90.73°WBison Creek — 51.50°N, 116.20°WHoney Creek Limestone — 34.39°N, 97.12°W

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

Conaspis and its relatives

Cambrian

Where Conaspis and its relatives were recorded in the Cambrian.

Found in the same rock

19 taxa

The Paleobiology Database records 6 sites for Conaspis, 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 6 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 Conaspis

Source
iDigBio
Credit
via iDigBio
Licence
not stated by the source
Commercial use
cannot be read from the licence given — check the record

No 3D scan of Conaspis 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

What may have been alongside itDokimokephalidae through timeFormations of the CambrianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Hall 1863