Turborotalia ampliapertura

Turborotalia ampliapertura

via GBIF · CC0 · via GBIF. 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
TurborotaliaPBDB
Diet
omnivorePBDB, for Foraminifera
Life habit
planktonicPBDB, for Globigerinina
Motility
stationaryPBDB, for Foraminifera
Environment
marinePBDB, for Globigerinina

Time the record covers

At least 10 million years on record.

The record covers at least 33.9 Mya to 23.04 Mya. No occurrence read is dated outside 56 Mya to 5.333 Mya.

Paleocene — about 0 of 80 occurrencesEocene — about 16 of 80 occurrencesEoceneOligocene — about 61 of 80 occurrencesOligoceneMiocene — about 3 of 80 occurrencesMiocenePliocene — about 0 of 80 occurrences57–55 Mya — about 0.1 occurrences55–54 Mya — about 0.2 occurrences54–52 Mya — about 0.2 occurrences52–50 Mya — about 0.2 occurrences50–48 Mya — about 0.2 occurrences48–46 Mya — about 0.2 occurrences46–45 Mya — about 0.2 occurrences45–43 Mya — about 0.2 occurrences43–41 Mya — about 0.2 occurrences41–39 Mya — about 0.4 occurrences39–38 Mya — about 0.5 occurrences38–36 Mya — about 6 occurrences36–34 Mya — about 6 occurrences34–32 Mya — about 15 occurrences32–31 Mya — about 15 occurrences31–29 Mya — about 13 occurrences29–27 Mya — about 12 occurrences27–25 Mya — about 4 occurrences25–24 Mya — about 2 occurrences24–22 Mya — about 0.8 occurrences22–20 Mya — about 0.3 occurrences20–18 Mya — about 0.3 occurrences18–17 Mya — about 0.3 occurrences17–15 Mya — about 0.3 occurrences15–13 Mya — about 0.3 occurrences13–11 Mya — about 0.3 occurrences11–9.6 Mya — about 0.3 occurrences9.6–7.8 Mya — about 0.3 occurrences7.8–6.1 Mya — about 0.3 occurrences6.1–4.3 Mya — about 0.1 occurrences33.9 Mya23.04 Mya57 Mya4 Mya

80 occurrences of Turborotalia ampliapertura on record, most of them in the Oligocene. 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

80 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

2 formations

Antigua — 17.03°N, 61.68°WQom — 37.34°N, 44.94°E

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The named rock units Turborotalia ampliapertura has been recovered from, largest first. Drawn where the rock is now, not where it formed. 78 occurrences have no formation on record, which is common for older literature.

Turborotalia ampliapertura and its relatives

Oligocene

Where Turborotalia ampliapertura and its relatives were recorded in the Oligocene.

Found in the same rock

277 taxa

The Paleobiology Database records 80 sites for Turborotalia ampliapertura, 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

20 references

Each of the 80 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. 8 further references are not listed. 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 Turborotalia ampliapertura

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

No 3D scan of Turborotalia ampliapertura was found in MorphoSource and Sketchfab.

Smithsonian Open Access was 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. (Bolli 1957)