Parvicingula matura

No picture of Parvicingula matura 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 Parvicingula matura, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
ParvicingulaPBDB

Time the record covers

At least 3.8 million years on record.

The record covers at least 174.7 Mya to 170.9 Mya. No occurrence read is dated outside 182.9 Mya to 168.2 Mya.

Early Jurassic — about 1 of 10 occurrencesEarly JurassicMiddle Jurassic — about 9 of 10 occurrencesMiddle Jurassic183–183 Mya — about 0.0 occurrences183–182 Mya — about 0.1 occurrences182–182 Mya — about 0.1 occurrences182–181 Mya — about 0.1 occurrences181–181 Mya — about 0.1 occurrences181–180 Mya — about 0.1 occurrences180–180 Mya — about 0.1 occurrences180–179 Mya — about 0.1 occurrences179–179 Mya — about 0.1 occurrences179–178 Mya — about 0.1 occurrences178–178 Mya — about 0.1 occurrences178–177 Mya — about 0.1 occurrences177–177 Mya — about 0.1 occurrences177–176 Mya — about 0.1 occurrences176–176 Mya — about 0.1 occurrences176–175 Mya — about 0.1 occurrences175–175 Mya — about 0.0 occurrences171–171 Mya — about 0.2 occurrences171–170 Mya — about 2 occurrences170–170 Mya — about 2 occurrences170–169 Mya — about 2 occurrences169–169 Mya — about 2 occurrences169–168 Mya — about 1.0 occurrences168–168 Mya — about 0.0 occurrences174.7 Mya170.9 Mya183.4 Mya167.7 Mya

10 occurrences of Parvicingula matura on record, most of them in the Middle Jurassic. 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

10 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

Graham Island — 53.40°N, 132.28°WSnowshoe — 44.00°N, 119.50°WPhantom Creek — 53.42°N, 132.27°W

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

Parvicingula matura and its relatives

Middle Jurassic

Where Parvicingula matura and its relatives were recorded in the Middle Jurassic.

Found in the same rock

97 taxa

The Paleobiology Database records 10 sites for Parvicingula matura, 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 10 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 Parvicingula matura 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 Parvicingula matura, or no answer at all. This entry cannot say which.

No 3D scan of Parvicingula matura 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.

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Occurrence data from the Paleobiology Database, CC BY 4.0. Pessagno and Whalen 1982