Parafusulina

Searched as Parafusulina cf. shaksgamensis crassimarginata. The Paleobiology Database treats Parafusulina as the accepted name.

Parafusulina is a genus of foraminifera included in the fusulinoidean family Schwagerinidae that were extant during the Permian.

Parafusulina

JJonahJackalope · CC BY-SA 4.0 · via Wikipedia/Commons. 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
SchwagerinidaePBDB
Diet
omnivorePBDB, for Foraminifera
Life habit
semi-infaunalPBDB, for Foraminifera
Motility
stationaryPBDB, for Foraminifera
Environment
marinePBDB, for Fusulinoidea

Time the record covers

At most 8.9 million years on record.

Every occurrence read is dated to somewhere between 283.3 Mya and 274.4 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Permian — about 2 of 2 occurrencesPermian283–283 Mya — about 0.0 occurrences283–283 Mya — about 0.1 occurrences283–282 Mya — about 0.1 occurrences282–282 Mya — about 0.1 occurrences282–282 Mya — about 0.1 occurrences282–281 Mya — about 0.1 occurrences281–281 Mya — about 0.1 occurrences281–281 Mya — about 0.1 occurrences281–281 Mya — about 0.1 occurrences281–280 Mya — about 0.1 occurrences280–280 Mya — about 0.1 occurrences280–280 Mya — about 0.1 occurrences280–279 Mya — about 0.1 occurrences279–279 Mya — about 0.1 occurrences279–279 Mya — about 0.1 occurrences279–278 Mya — about 0.1 occurrences278–278 Mya — about 0.1 occurrences278–278 Mya — about 0.1 occurrences278–277 Mya — about 0.1 occurrences277–277 Mya — about 0.1 occurrences277–277 Mya — about 0.1 occurrences277–276 Mya — about 0.1 occurrences276–276 Mya — about 0.1 occurrences276–276 Mya — about 0.1 occurrences276–275 Mya — about 0.1 occurrences275–275 Mya — about 0.1 occurrences275–275 Mya — about 0.1 occurrences275–274 Mya — about 0.0 occurrences283.8 Mya273.9 Mya

2 occurrences of Parafusulina 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

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

1 formation

Bird Spring — 35.09°N, 115.86°W

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

Parafusulina and its relatives

Permian

Where Parafusulina and its relatives were recorded in the Permian.

Found in the same rock

369 taxa

The Paleobiology Database records 251 sites for Parafusulina, and this reads 240 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

1 reference

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 doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content2

Picture of Parafusulina

Credit
JJonahJackalope
Licence
CC BY-SA 4.0
Commercial use
the licence allows it

3D model

Source
Sketchfab
Licence
CC0 Public Domain
Commercial use
the licence allows it

Smithsonian Open Access and MorphoSource were not reached for this taxon, so this list is what the others held rather than everything there is.

The description on this site

Licence
CC BY-SA 4.0

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. Dunbar and Skinner 1931