Clavaspidella

Clavaspidella

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
DolichometopidaePBDB
Diet
carnivorePBDB, for Corynexochida
Life habit
nektobenthicPBDB, for Corynexochida
Motility
actively mobilePBDB, for Corynexochida
Environment
marinePBDB, for Trilobita

Time the record covers

At least 8.3 million years on record.

The record covers at least 505.3 Mya to 497 Mya. No occurrence read is dated outside 509.7 Mya to 486.85 Mya.

Cambrian — about 7 of 7 occurrencesCambrianOrdovician — about 0 of 7 occurrences510–509 Mya — about 0.1 occurrences509–509 Mya — about 0.2 occurrences509–508 Mya — about 0.2 occurrences508–507 Mya — about 0.2 occurrences507–506 Mya — about 0.2 occurrences506–505 Mya — about 0.2 occurrences505–505 Mya — about 0.1 occurrences505–504 Mya — about 0.2 occurrences504–503 Mya — about 0.3 occurrences503–502 Mya — about 0.3 occurrences502–501 Mya — about 0.3 occurrences501–501 Mya — about 0.3 occurrences501–500 Mya — about 0.3 occurrences500–499 Mya — about 0.3 occurrences499–498 Mya — about 0.3 occurrences498–497 Mya — about 0.3 occurrences497–497 Mya — about 0.3 occurrences497–496 Mya — about 0.2 occurrences496–495 Mya — about 0.2 occurrences495–494 Mya — about 0.2 occurrences494–494 Mya — about 0.2 occurrences494–493 Mya — about 0.2 occurrences493–492 Mya — about 0.2 occurrences492–491 Mya — about 0.2 occurrences491–490 Mya — about 0.2 occurrences490–490 Mya — about 0.2 occurrences490–489 Mya — about 0.2 occurrences489–488 Mya — about 0.2 occurrences488–487 Mya — about 0.2 occurrences487–486 Mya — about 0.1 occurrences505.3 Mya497 Mya510.2 Mya486.4 Mya

7 occurrences of Clavaspidella 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

7 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

3 formations

Langston — 42.19°N, 112.25°WLangston — 42.32°N, 111.45°WMuav Limestone — 35.82°N, 113.65°WMuav Limestone — 35.99°N, 113.82°WMuav Limestone — 36.08°N, 112.13°WBright Angel — 35.99°N, 113.82°W

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

Clavaspidella and its relatives

Cambrian

Where Clavaspidella and its relatives were recorded in the Cambrian.

Found in the same rock

56 taxa

The Paleobiology Database records 7 sites for Clavaspidella, 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

4 references

Each of the 7 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 Clavaspidella

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 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 itDolichometopidae through timeFormations of the CambrianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Poulson 1927