Cupressinoxylon artabeae

No picture of Cupressinoxylon artabeae was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Cupressinoxylon artabeae, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
CupressinoxylonPBDB
Diet
"photoautotroph"PBDB, for Streptophyta

Time the record covers

At most 22 million years on record.

Every occurrence read is dated to somewhere between 83.6 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 1 of 2 occurrencesLate CretaceousPaleocene — about 1 of 2 occurrencesPaleocene84–83 Mya — about 0.0 occurrences83–83 Mya — about 0.0 occurrences83–82 Mya — about 0.0 occurrences82–81 Mya — about 0.0 occurrences81–80 Mya — about 0.0 occurrences80–80 Mya — about 0.0 occurrences80–79 Mya — about 0.0 occurrences79–78 Mya — about 0.0 occurrences78–77 Mya — about 0.0 occurrences77–76 Mya — about 0.0 occurrences76–76 Mya — about 0.0 occurrences76–75 Mya — about 0.0 occurrences75–74 Mya — about 0.0 occurrences74–73 Mya — about 0.0 occurrences73–73 Mya — about 0.0 occurrences73–72 Mya — about 0.0 occurrences72–71 Mya — about 0.0 occurrences71–70 Mya — about 0.0 occurrences70–70 Mya — about 0.0 occurrences70–69 Mya — about 0.0 occurrences69–68 Mya — about 0.0 occurrences68–67 Mya — about 0.0 occurrences67–67 Mya — about 0.0 occurrences67–66 Mya — about 0.1 occurrences66–65 Mya — about 0.2 occurrences65–64 Mya — about 0.2 occurrences64–63 Mya — about 0.2 occurrences63–63 Mya — about 0.2 occurrences63–62 Mya — about 0.2 occurrences62–61 Mya — about 0.1 occurrences84.1 Mya61.2 Mya

2 occurrences of Cupressinoxylon artabeae 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

2 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

Salamanca — 45.07°S, 66.98°WPuntudo Chico — 44.10°S, 67.93°W

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

Cupressinoxylon artabeae and its relatives

Late Cretaceous

Where Cupressinoxylon artabeae and its relatives were recorded in the Late Cretaceous.

Found in the same rock

7 taxa

The Paleobiology Database records 2 sites for Cupressinoxylon artabeae, and this reads all of them. The number is how many of those sites it was catalogued from too.

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

2 references

Each of the 2 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 Cupressinoxylon artabeae was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none.

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

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 itCupressinoxylon through timeFormations of the Late CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Ruiz et al. 2017