Vitreisporites signatus

No picture of Vitreisporites signatus 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 Vitreisporites signatus, or no answer at all. This entry cannot say which.

On record

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

Time the record covers

At least 202 million years on record.

The record covers at least 274.4 Mya to 72.2 Mya. No occurrence read is dated outside 298.9 Mya to 66 Mya.

Carboniferous — about 0 of 27 occurrencesPermian — about 11 of 27 occurrencesPermianEarly Triassic — about 6 of 27 occurrencesMiddle Triassic — about 0 of 27 occurrencesLate Triassic — about 0 of 27 occurrencesEarly Jurassic — about 0 of 27 occurrencesMiddle Jurassic — about 0 of 27 occurrencesLate Jurassic — about 0 of 27 occurrencesEarly Cretaceous — about 0 of 27 occurrencesLate Cretaceous — about 10 of 27 occurrencesLate CretaceousPaleocene — about 0 of 27 occurrences304–295 Mya — about 0.1 occurrences295–287 Mya — about 0.2 occurrences287–279 Mya — about 0.6 occurrences279–271 Mya — about 1 occurrence271–263 Mya — about 1.0 occurrences263–255 Mya — about 5 occurrences255–247 Mya — about 9 occurrences77–69 Mya — about 4 occurrences69–61 Mya — about 6 occurrences274.4 Mya72.2 Mya304 Mya61 Mya

27 occurrences of Vitreisporites signatus on record, most of them in the Permian. 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

27 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

Chorrillo — 50.50°S, 72.56°WCalvoerde — 52.12°N, 10.67°EBernburg — 52.12°N, 10.67°EBuckly — 84.00°S, 162.00°E

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The named rock units Vitreisporites signatus has been recovered from, largest first. Drawn where the rock is now, not where it formed. 9 occurrences have no formation on record, which is common for older literature.

Vitreisporites signatus and its relatives

Permian

Where Vitreisporites signatus and its relatives were recorded in the Permian.

Found in the same rock

241 taxa

The Paleobiology Database records 27 sites for Vitreisporites signatus, 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

5 references

Each of the 27 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 Vitreisporites signatus 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 Vitreisporites signatus, or no answer at all. This entry cannot say which.

No 3D scan of Vitreisporites signatus 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. Leschik 1956