Palaeoneilo fecunda

No picture of Palaeoneilo fecunda 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 Palaeoneilo fecunda, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
PalaeoneiloPBDB
Diet
deposit feederPBDB, for Nuculanoidea
Life habit
infaunalPBDB, for Nuculanoidea
Motility
facultatively mobilePBDB, for Nuculanoidea
Vision
blindPBDB, for Bivalvia

Time the record covers

At least 61 million years on record.

The record covers at least 449.6 Mya to 387.95 Mya. No occurrence read is dated outside 450.2 Mya to 382.31 Mya.

Ordovician — about 6 of 16 occurrencesOrdovicianSilurian — about 0 of 16 occurrencesDevonian — about 10 of 16 occurrencesDevonian452–449 Mya — about 2 occurrences449–447 Mya — about 2 occurrences447–444 Mya — about 1 occurrence395–393 Mya — about 0.1 occurrences393–390 Mya — about 0.4 occurrences390–388 Mya — about 0.4 occurrences388–386 Mya — about 4 occurrences386–383 Mya — about 4 occurrences383–381 Mya — about 2 occurrences449.6 Mya387.95 Mya452 Mya381 Mya

16 occurrences of Palaeoneilo fecunda on record, most of them in the Devonian. 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

16 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

8 formations

Moscow — 42.88°N, 78.42°WMoscow — 42.77°N, 77.82°WMoscow — 42.81°N, 77.90°WMoscow — 42.70°N, 78.95°WMoscow — 42.78°N, 77.33°WBrainard — 42.94°N, 91.71°WMaquoketa — 42.94°N, 91.71°WMaquoketa — 43.28°N, 91.37°WBills Creek Shale — 43.42°N, 83.95°WLudlowville — 42.96°N, 78.13°WMahantango — 40.42°N, 77.00°WScales — 42.48°N, 90.87°WBokkeveld Beds — 33.98°S, 18.60°E

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The named rock units Palaeoneilo fecunda has been recovered from, largest first. Drawn where the rock is now, not where it formed. 2 occurrences have no formation on record, which is common for older literature.

Palaeoneilo fecunda and its relatives

Devonian

Where Palaeoneilo fecunda and its relatives were recorded in the Devonian.

Found in the same rock

199 taxa

The Paleobiology Database records 14 sites for Palaeoneilo fecunda, 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

7 references

Each of the 16 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 Palaeoneilo fecunda 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 Palaeoneilo fecunda, or no answer at all. This entry cannot say which.

No 3D scan of Palaeoneilo fecunda 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. (Hall 1862)