Clavulinoides

Searched as Clavulinoides trilaterus. The Paleobiology Database treats Clavulinoides as the accepted name.

Clavulinoides

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
PseudogaudryininaePBDB
Diet
detritivorePBDB, for Textulariina
Life habit
infaunalPBDB, for Textulariina
Motility
stationaryPBDB, for Foraminifera

Time the record covers

At most 11 million years on record.

Every occurrence read is dated to somewhere between 72.2 Mya and 61.66 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Late Cretaceous — about 5 of 6 occurrencesLate CretaceousPaleocene — about 1 of 6 occurrencesPaleocene72–72 Mya — about 0.2 occurrences72–72 Mya — about 0.3 occurrences72–71 Mya — about 0.3 occurrences71–71 Mya — about 0.3 occurrences71–70 Mya — about 0.3 occurrences70–70 Mya — about 0.3 occurrences70–70 Mya — about 0.3 occurrences70–69 Mya — about 0.3 occurrences69–69 Mya — about 0.3 occurrences69–68 Mya — about 0.3 occurrences68–68 Mya — about 0.3 occurrences68–68 Mya — about 0.3 occurrences68–67 Mya — about 0.3 occurrences67–67 Mya — about 0.3 occurrences67–67 Mya — about 0.3 occurrences67–66 Mya — about 0.3 occurrences66–66 Mya — about 0.2 occurrences66–65 Mya — about 0.1 occurrences65–65 Mya — about 0.1 occurrences65–65 Mya — about 0.1 occurrences65–64 Mya — about 0.1 occurrences64–64 Mya — about 0.1 occurrences64–63 Mya — about 0.1 occurrences63–63 Mya — about 0.1 occurrences63–63 Mya — about 0.1 occurrences63–62 Mya — about 0.1 occurrences62–62 Mya — about 0.1 occurrences62–62 Mya — about 0.1 occurrences72.7 Mya61.2 Mya

6 occurrences of Clavulinoides on record, most of them in the Late Cretaceous. The Paleobiology Database records this as a living group, and the chart stops with its fossils rather than at the present. 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

1 formation

Dakhla — 26.52°N, 27.66°E

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

Clavulinoides and its relatives

Late Cretaceous

Where Clavulinoides and its relatives were recorded in the Late Cretaceous.

Found in the same rock

91 taxa

The Paleobiology Database records 9 sites for Clavulinoides, 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

1 reference

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. Each entry links to doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content1

Picture of Clavulinoides

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 Clavulinoides was found in Sketchfab.

Smithsonian Open Access and MorphoSource were 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 itPseudogaudryininae through timeFormations of the Late CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Cushman 1936