Clisocolus corrugatus

Clisocolus corrugatus

via iDigBio · CC BY · 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
ClisocolusPBDB
Diet
chemosymbioticPBDB, for Lucinoidea
Life habit
infaunalPBDB, for Lucinoidea
Motility
facultatively mobilePBDB, for Lucinoidea
Vision
blindPBDB, for Bivalvia

Time the record covers

At most 17 million years on record.

Every occurrence read is dated to somewhere between 106.3 Mya and 89.8 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Early Cretaceous — about 0 of 16 occurrencesEarly CretaceousLate Cretaceous — about 16 of 16 occurrencesLate Cretaceous107–106 Mya — about 0.0 occurrences106–106 Mya — about 0.0 occurrences106–105 Mya — about 0.0 occurrences105–104 Mya — about 0.0 occurrences104–104 Mya — about 0.0 occurrences104–103 Mya — about 0.0 occurrences103–103 Mya — about 0.0 occurrences103–102 Mya — about 0.0 occurrences102–102 Mya — about 0.0 occurrences102–101 Mya — about 0.0 occurrences101–100 Mya — about 0.1 occurrences100–100 Mya — about 0.2 occurrences100–99 Mya — about 0.2 occurrences99–99 Mya — about 0.2 occurrences99–98 Mya — about 0.2 occurrences98–97 Mya — about 0.2 occurrences97–97 Mya — about 0.2 occurrences97–96 Mya — about 0.2 occurrences96–96 Mya — about 0.2 occurrences96–95 Mya — about 0.2 occurrences95–95 Mya — about 0.2 occurrences95–94 Mya — about 0.2 occurrences94–93 Mya — about 2 occurrences93–93 Mya — about 2 occurrences93–92 Mya — about 2 occurrences92–92 Mya — about 2 occurrences92–91 Mya — about 2 occurrences91–90 Mya — about 2 occurrences90–90 Mya — about 2 occurrences90–89 Mya — about 0.3 occurrences106.8 Mya89.3 Mya

16 occurrences of Clisocolus corrugatus on record, most of them in the Late Cretaceous. 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

16 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

Ladd — 33.75°N, 117.68°WLadd — 33.75°N, 117.64°WLadd — 33.75°N, 117.64°WGalala — 29.27°N, 34.72°EHalal — 30.37°N, 34.45°E

Loading coastlines…

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

Clisocolus corrugatus and its relatives

Late Cretaceous

Where Clisocolus corrugatus and its relatives were recorded in the Late Cretaceous.

Found in the same rock

74 taxa

The Paleobiology Database records 14 sites for Clisocolus corrugatus, 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

5 references

Each of the 16 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 Clisocolus corrugatus

Source
iDigBio
Credit
via iDigBio
Licence
CC BY
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

What may have been alongside itClisocolus through timeFormations of the Late CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Popenoe 1937