Artostrobium tina

No picture of Artostrobium tina 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 Artostrobium tina, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
ArtostrobiumPBDB

Time the record covers

At least 2.1 million years on record.

The record covers at least 85.7 Mya to 83.6 Mya. No occurrence read is dated outside 89.8 Mya to 72.2 Mya.

Late Cretaceous — about 4 of 4 occurrencesLate Cretaceous90–90 Mya — about 0.0 occurrences90–89 Mya — about 0.2 occurrences89–88 Mya — about 0.2 occurrences88–88 Mya — about 0.2 occurrences88–87 Mya — about 0.2 occurrences87–87 Mya — about 0.2 occurrences87–86 Mya — about 0.2 occurrences86–85 Mya — about 0.4 occurrences85–85 Mya — about 0.6 occurrences85–84 Mya — about 0.6 occurrences84–83 Mya — about 0.5 occurrences83–83 Mya — about 0.1 occurrences83–82 Mya — about 0.1 occurrences82–82 Mya — about 0.1 occurrences82–81 Mya — about 0.1 occurrences81–80 Mya — about 0.1 occurrences80–80 Mya — about 0.1 occurrences80–79 Mya — about 0.1 occurrences79–79 Mya — about 0.1 occurrences79–78 Mya — about 0.1 occurrences78–77 Mya — about 0.1 occurrences77–77 Mya — about 0.1 occurrences77–76 Mya — about 0.1 occurrences76–75 Mya — about 0.1 occurrences75–75 Mya — about 0.1 occurrences75–74 Mya — about 0.1 occurrences74–74 Mya — about 0.1 occurrences74–73 Mya — about 0.1 occurrences73–72 Mya — about 0.1 occurrences72–72 Mya — about 0.0 occurrences85.7 Mya – 83.6 Mya90.3 Mya71.7 Mya

4 occurrences of Artostrobium tina 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

4 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

Urakawa — 42.17°N, 142.82°E

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

Artostrobium tina and its relatives

Late Cretaceous

Where Artostrobium tina and its relatives were recorded in the Late Cretaceous.

Found in the same rock

47 taxa

The Paleobiology Database records 4 sites for Artostrobium tina, 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 4 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 the Paleobiology Database's own record for the work.

Media and terms

Media content0

No picture of Artostrobium tina 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 Artostrobium tina, or no answer at all. This entry cannot say which.

No 3D scan of Artostrobium tina 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 itArtostrobium through timeFormations of the Late CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Foreman 1971