Cricotriporites guianensis

No picture of Cricotriporites guianensis was found. Wikipedia, Wikidata and iDigBio were searched and had none. 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 Cricotriporites guianensis, or no answer at all. This entry cannot say which.

On record

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

Time the record covers

At least 36 million years on record.

The record covers at least 48.07 Mya to 11.63 Mya. No occurrence read is dated outside 56 Mya to 5.333 Mya.

Paleocene — about 0 of 6 occurrencesEocene — about 5 of 6 occurrencesEoceneOligocene — about 0 of 6 occurrencesMiocene — about 1 of 6 occurrencesMiocenePliocene — about 0 of 6 occurrences57–55 Mya — about 0.4 occurrences55–54 Mya — about 0.9 occurrences54–52 Mya — about 0.9 occurrences52–50 Mya — about 0.9 occurrences50–48 Mya — about 0.9 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 0.2 occurrences39–38 Mya — about 0.2 occurrences13–11 Mya — about 0.0 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 occurrences48.07 Mya11.63 Mya57 Mya4 Mya

6 occurrences of Cricotriporites guianensis on record, most of them in the Eocene. 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

6 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

4 formations

Arcillas de el Limbo — 4.90°N, 73.02°WMirador — 7.70°N, 72.62°WLa Paz — 7.33°N, 73.33°WChiquimil — 26.83°S, 66.00°W

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

Cricotriporites guianensis and its relatives

Eocene

Where Cricotriporites guianensis and its relatives were recorded in the Eocene.

Found in the same rock

143 taxa

The Paleobiology Database records 6 sites for Cricotriporites guianensis, 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

2 references

Each of the 6 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 content0

No picture of Cricotriporites guianensis was found. Wikipedia, Wikidata and iDigBio were searched and had none.

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 Cricotriporites guianensis, or no answer at all. This entry cannot say which.

No 3D scan of Cricotriporites guianensis 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 itCricotriporites through timeFormations of the EoceneThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Leidelmeyer 1966