Craigia

Craigia is a genus of flowering plants in the family Malvaceae sensu lato or Tiliaceae.

A picture published with the record for Craigia. What it shows has not been checked.

Kevmin · CC BY-SA 4.0 · via Wikipedia/Commons. 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
PlantaePBDB

Time the record covers

At least 26 million years on record.

The record covers at least 37.71 Mya to 11.63 Mya. No occurrence read is dated outside 48.07 Mya to 5.333 Mya.

Eocene — about 2 of 13 occurrencesEoceneOligocene — about 10 of 13 occurrencesOligoceneMiocene — about 1 of 13 occurrencesMiocenePliocene — about 0 of 13 occurrences49–47 Mya — about 0.1 occurrences47–46 Mya — about 0.1 occurrences46–44 Mya — about 0.1 occurrences44–43 Mya — about 0.1 occurrences43–42 Mya — about 0.1 occurrences42–40 Mya — about 0.4 occurrences40–39 Mya — about 0.6 occurrences39–37 Mya — about 0.3 occurrences34–33 Mya — about 2 occurrences33–31 Mya — about 2 occurrences31–30 Mya — about 2 occurrences30–28 Mya — about 2 occurrences28–27 Mya — about 1 occurrence27–25 Mya — about 0.3 occurrences25–24 Mya — about 0.3 occurrences24–22 Mya — about 0.2 occurrences12–10 Mya — about 0.2 occurrences10–8.9 Mya — about 0.2 occurrences8.9–7.4 Mya — about 0.2 occurrences7.4–6.0 Mya — about 0.2 occurrences6.0–4.5 Mya — about 0.1 occurrences37.71 Mya11.63 Mya48.9 Mya4.5 Mya

13 occurrences of Craigia on record, most of them in the Oligocene. The Paleobiology Database records this as a living group, and the chart stops with its fossils rather than at the present. 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

13 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

John Day — 44.64°N, 120.30°WJohn Day — 45.00°N, 120.20°WJohn Day — 44.95°N, 120.33°WJohn Day — 44.14°N, 120.27°WJohn Day — 44.57°N, 119.63°WJohn Day — 44.94°N, 120.40°WSalmon City — 45.18°N, 113.88°WHuazhige — 23.02°N, 104.38°E

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The named rock units Craigia has been recovered from, largest first. Drawn where the rock is now, not where it formed. 5 occurrences have no formation on record, which is common for older literature.

Craigia and its relatives

Oligocene

Where Craigia and its relatives were recorded in the Oligocene.

Found in the same rock

357 taxa

The Paleobiology Database records 5 sites for Craigia, 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

8 references

Each of the 13 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. Entries link to doi.org where the Paleobiology Database holds an identifier, and to its own record where it does not. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content1

Picture of Craigia

Credit
Kevmin
Licence
CC BY-SA 4.0
Commercial use
the licence allows it

No 3D scan of Craigia 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.

The description on this site

Licence
CC BY-SA 4.0

This is what the site found, which is not the same as what exists.

Keep going

What may have been alongside itPlantae through timeFormations of the OligoceneThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Smith and Evans 1921