Chaetopleura

Chaetopleura is a genus of chitons in the family Chaetopleuridae. The species within this genus are marine molluscs.

Chaetopleura

Seascapeza · CC BY-SA 3.0 · via Wikipedia/Commons. 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
ChaetopleuridaePBDB
Diet
grazerPBDB, for Polyplacophora
Life habit
epifaunalPBDB, for Polyplacophora
Motility
facultatively mobile, attachedPBDB, for Polyplacophora
Vision
limitedPBDB, for Polyplacophora
Environment
marine,brackishPBDB, for Polyplacophora

Time the record covers

At least 15 million years on record.

The record covers at least 15.98 Mya to 129 ka. No occurrence read is dated outside 23.04 Mya to 11.7 ka.

Oligocene — about 0 of 15 occurrencesMiocene — about 3 of 15 occurrencesMiocenePliocene — about 1 of 15 occurrencesPliocenePleistocene — about 11 of 15 occurrencesPleistocene24–23 Mya — about 0.1 occurrences23–22 Mya — about 0.2 occurrences22–21 Mya — about 0.2 occurrences21–20 Mya — about 0.2 occurrences20–20 Mya — about 0.2 occurrences20–19 Mya — about 0.2 occurrences19–18 Mya — about 0.2 occurrences18–17 Mya — about 0.2 occurrences17–16 Mya — about 0.2 occurrences16–16 Mya — about 0.1 occurrences7.8–7.1 Mya — about 0.1 occurrences7.1–6.3 Mya — about 0.4 occurrences6.3–5.5 Mya — about 0.4 occurrences5.5–4.7 Mya — about 0.1 occurrences3.9–3.1 Mya — about 0.5 occurrences3.1–2.4 Mya — about 1 occurrence2.4–1.6 Mya — about 3 occurrences1.6–785 ka Mya — about 3 occurrences785 ka–0 Mya — about 4 occurrences15.98 Mya129 ka23.5 Mya0 Mya

15 occurrences of Chaetopleura on record, most of them in the Pleistocene. The Paleobiology Database records this as a living group. 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

15 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

James City — 35.04°N, 76.99°WQuaternary terrace — 33.75°N, 118.33°WKirkwood — 39.15°N, 74.69°WKirkwood — 39.46°N, 75.30°WBermont — 27.72°N, 82.43°W"Imperial" — 33.95°N, 116.63°W

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The named rock units Chaetopleura has been recovered from, largest first. Drawn where the rock is now, not where it formed. 4 occurrences have no formation on record, which is common for older literature.

Chaetopleura and its relatives

Pleistocene

Where Chaetopleura and its relatives were recorded in the Pleistocene.

Found in the same rock

480 taxa

The Paleobiology Database records 11 sites for Chaetopleura, 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

8 references

Each of the 15 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 Chaetopleura

Credit
Seascapeza
Licence
CC BY-SA 3.0
Commercial use
the licence allows it

No 3D scan of Chaetopleura was found in Smithsonian Open Access and Sketchfab.

MorphoSource was not reached for this taxon, so this list is what the others held rather than everything there is.

The description on this site

Licence
CC BY-SA 4.0

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. Shuttleworth 1853