Neodutkevitchia

Neodutkevitchia

via GBIF · CC0 · via GBIF. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.

On record

Recorded, not inferred
Sits inside
PseudofusulininaePBDB
Diet
omnivorePBDB, for Foraminifera
Life habit
semi-infaunalPBDB, for Foraminifera
Motility
stationaryPBDB, for Foraminifera
Environment
marinePBDB, for Fusulinoidea

Time the record covers

At most 11 million years on record.

Every occurrence read is dated to somewhere between 293.52 Mya and 283.3 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Permian — about 21 of 21 occurrencesPermian294–293 Mya — about 1 occurrence293–293 Mya — about 2 occurrences293–293 Mya — about 2 occurrences293–292 Mya — about 2 occurrences292–292 Mya — about 2 occurrences292–291 Mya — about 2 occurrences291–291 Mya — about 2 occurrences291–291 Mya — about 2 occurrences291–290 Mya — about 2 occurrences290–290 Mya — about 1 occurrence290–290 Mya — about 0.2 occurrences290–289 Mya — about 0.2 occurrences289–289 Mya — about 0.2 occurrences289–288 Mya — about 0.2 occurrences288–288 Mya — about 0.2 occurrences288–288 Mya — about 0.2 occurrences288–287 Mya — about 0.2 occurrences287–287 Mya — about 0.2 occurrences287–287 Mya — about 0.2 occurrences287–286 Mya — about 0.2 occurrences286–286 Mya — about 0.2 occurrences286–285 Mya — about 0.2 occurrences285–285 Mya — about 0.2 occurrences285–285 Mya — about 0.2 occurrences285–284 Mya — about 0.2 occurrences284–284 Mya — about 0.2 occurrences284–284 Mya — about 0.2 occurrences284–283 Mya — about 0.1 occurrences294 Mya282.8 Mya

21 occurrences of Neodutkevitchia 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

21 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

Khan — 33.83°N, 56.45°EKhan — 33.49°N, 56.26°EKhan — 33.65°N, 56.35°EKhan — 33.26°N, 56.17°EChili — 33.52°N, 56.15°EChili — 33.97°N, 56.47°EQudi — 33.28°N, 87.02°EQudi — 33.09°N, 86.66°EDingjiazhai — 24.36°N, 99.24°E

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

Neodutkevitchia and its relatives

Permian

Where Neodutkevitchia and its relatives were recorded in the Permian.

Found in the same rock

40 taxa

The Paleobiology Database records 15 sites for Neodutkevitchia, 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

6 references

Each of the 21 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 content1

Picture of Neodutkevitchia

Source
GBIF
Credit
via GBIF
Licence
CC0
Commercial use
the licence allows it

No 3D scan of Neodutkevitchia was found in MorphoSource and Sketchfab.

Smithsonian Open Access was 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 itPseudofusulininae through timeFormations of the PermianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Davydov and Arefifard 2007