Sanguinolites woolnoughi

No picture of Sanguinolites woolnoughi 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 Sanguinolites woolnoughi, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
SanguinolitesPBDB
Diet
suspension feederPBDB, for Bivalvia
Life habit
deep infaunalPBDB, for Sanguinolites
Motility
facultatively mobilePBDB, for Bivalvia
Vision
blindPBDB, for Bivalvia

Time the record covers

At least 4.7 million years on record.

The record covers at least 323.4 Mya to 318.7 Mya. No occurrence read is dated outside 330.3 Mya to 307.4 Mya.

Carboniferous — about 2 of 2 occurrencesCarboniferous331–330 Mya — about 0.0 occurrences330–329 Mya — about 0.1 occurrences329–328 Mya — about 0.1 occurrences328–328 Mya — about 0.1 occurrences328–327 Mya — about 0.1 occurrences327–326 Mya — about 0.1 occurrences326–325 Mya — about 0.1 occurrences325–324 Mya — about 0.1 occurrences324–324 Mya — about 0.1 occurrences324–323 Mya — about 0.0 occurrences319–318 Mya — about 0.1 occurrences318–317 Mya — about 0.1 occurrences317–316 Mya — about 0.1 occurrences316–316 Mya — about 0.1 occurrences316–315 Mya — about 0.1 occurrences315–314 Mya — about 0.1 occurrences314–313 Mya — about 0.1 occurrences313–312 Mya — about 0.1 occurrences312–312 Mya — about 0.1 occurrences312–311 Mya — about 0.1 occurrences311–310 Mya — about 0.1 occurrences310–309 Mya — about 0.1 occurrences309–308 Mya — about 0.1 occurrences308–308 Mya — about 0.1 occurrences308–307 Mya — about 0.0 occurrences323.4 Mya318.7 Mya330.8 Mya306.9 Mya

2 occurrences of Sanguinolites woolnoughi on record, most of them in the Carboniferous. 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

2 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

2 formations

Booral — 31.02°S, 152.67°EPoperima — 24.98°S, 151.37°E

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

Sanguinolites woolnoughi and its relatives

Carboniferous

Where Sanguinolites woolnoughi and its relatives were recorded in the Carboniferous.

Found in the same rock

21 taxa

The Paleobiology Database records 2 sites for Sanguinolites woolnoughi, and this reads all of them. The number is how many of those sites it was catalogued from too.

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 2 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 Sanguinolites woolnoughi 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 Sanguinolites woolnoughi, or no answer at all. This entry cannot say which.

No 3D scan of Sanguinolites woolnoughi 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. Campbell 1962