Longapertites vaneendenburgi

No picture of Longapertites vaneendenburgi was found. Wikidata and iDigBio were searched and had none. Wikipedia and Smithsonian Open Access did not answer, so this is what the others held rather than everything there is. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Longapertites vaneendenburgi, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
LongapertitesPBDB
Diet
"photoautotroph"PBDB, for Angiospermae

Time the record covers

At least 6.7 million years on record.

The record covers at least 66 Mya to 59.24 Mya. No occurrence read is dated outside 72.2 Mya to 56 Mya.

Late Cretaceous — about 3 of 40 occurrencesLate CretaceousPaleocene — about 37 of 40 occurrencesPaleoceneEocene — about 0 of 40 occurrences73–72 Mya — about 0.0 occurrences72–72 Mya — about 0.3 occurrences72–71 Mya — about 0.3 occurrences71–70 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 occurrences68–67 Mya — about 0.3 occurrences67–66 Mya — about 0.3 occurrences66–66 Mya — about 0.7 occurrences66–65 Mya — about 2 occurrences65–65 Mya — about 2 occurrences65–64 Mya — about 2 occurrences64–64 Mya — about 2 occurrences64–63 Mya — about 2 occurrences63–62 Mya — about 2 occurrences62–62 Mya — about 2 occurrences62–61 Mya — about 1 occurrence61–61 Mya — about 0.9 occurrences61–60 Mya — about 0.9 occurrences60–60 Mya — about 0.9 occurrences60–59 Mya — about 2 occurrences59–58 Mya — about 4 occurrences58–58 Mya — about 4 occurrences58–57 Mya — about 4 occurrences57–57 Mya — about 4 occurrences57–56 Mya — about 4 occurrences56–56 Mya — about 0.5 occurrences66 Mya59.24 Mya72.7 Mya55.5 Mya

40 occurrences of Longapertites vaneendenburgi on record, most of them in the Paleocene. 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

40 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

Guasare — 11.00°N, 72.38°WMirador — 11.00°N, 72.38°WMirador — 10.88°N, 72.38°WLefipán — 42.67°S, 69.83°W

Loading coastlines…

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

Longapertites vaneendenburgi and its relatives

Paleocene

Where Longapertites vaneendenburgi and its relatives were recorded in the Paleocene.

Found in the same rock

The Paleobiology Database records no fossil sites for Longapertites vaneendenburgi, so there is nothing to compare it with.

Entered from

3 references

Each of the 40 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 content0

No picture of Longapertites vaneendenburgi was found. Wikidata and iDigBio were searched and had none.

Wikipedia and Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.

GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Longapertites vaneendenburgi, or no answer at all. This entry cannot say which.

No 3D scan of Longapertites vaneendenburgi 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. Geermerad et al. 1968