Pseudoguembelina palpebra

Pseudoguembelina palpebra

via iDigBio · CC0 · 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
PseudoguembelinaPBDB
Diet
omnivorePBDB, for Foraminifera
Life habit
planktonicPBDB, for Globigerinina
Motility
stationaryPBDB, for Foraminifera
Environment
marinePBDB, for Globigerinina

Time the record covers

At most 45 million years on record.

Every occurrence read is dated to somewhere between 100.5 Mya and 56 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 82 occurrencesLate Cretaceous — about 57 of 82 occurrencesLate CretaceousPaleocene — about 25 of 82 occurrencesPaleoceneEocene — about 0 of 82 occurrences101–100 Mya — about 0.0 occurrences100–98 Mya — about 0.0 occurrences98–97 Mya — about 0.0 occurrences97–95 Mya — about 0.0 occurrences95–94 Mya — about 0.0 occurrences94–92 Mya — about 0.0 occurrences92–91 Mya — about 0.0 occurrences91–89 Mya — about 0.0 occurrences89–88 Mya — about 0.0 occurrences88–86 Mya — about 0.0 occurrences86–84 Mya — about 0.0 occurrences84–83 Mya — about 0.0 occurrences83–81 Mya — about 0.0 occurrences81–80 Mya — about 0.0 occurrences80–78 Mya — about 0.0 occurrences78–77 Mya — about 0.0 occurrences77–75 Mya — about 0.0 occurrences75–74 Mya — about 0.0 occurrences74–72 Mya — about 1 occurrence72–71 Mya — about 14 occurrences71–69 Mya — about 14 occurrences69–67 Mya — about 14 occurrences67–66 Mya — about 14 occurrences66–64 Mya — about 8 occurrences64–63 Mya — about 8 occurrences63–61 Mya — about 6 occurrences61–60 Mya — about 0.3 occurrences60–58 Mya — about 0.3 occurrences58–57 Mya — about 0.3 occurrences57–55 Mya — about 0.1 occurrences101.4 Mya55.1 Mya

82 occurrences of Pseudoguembelina palpebra 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

82 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

El Haria — 36.19°N, 8.71°EEl Haria — 35.95°N, 9.10°EDakhla — 26.35°N, 33.02°EDakhla — 26.52°N, 27.66°ECorsicana — 31.08°N, 96.83°W

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

Pseudoguembelina palpebra and its relatives

Late Cretaceous

Where Pseudoguembelina palpebra and its relatives were recorded in the Late Cretaceous.

Found in the same rock

115 taxa

The Paleobiology Database records 82 sites for Pseudoguembelina palpebra, 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

6 references

Each of the 82 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 Pseudoguembelina palpebra

Source
iDigBio
Credit
via iDigBio
Licence
CC0
Commercial use
the licence allows it

No 3D scan of Pseudoguembelina palpebra 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

Occurrence data from the Paleobiology Database, CC BY 4.0. Bronnimann and Brown 1953