Strephinia convoluta

Strephinia convoluta

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
StrephiniaPBDB
Diet
suspension feederPBDB, for Hexactinellida
Life habit
intermediate-level epifaunalPBDB, for Hexactinellida
Motility
stationary, attachedPBDB, for Hexactinellida
Vision
blindPBDB, for Hexactinellida
Environment
marinePBDB, for Hexactinellida

Time the record covers

At least 20 million years on record.

The record covers at least 110.1 Mya to 89.8 Mya. No occurrence read is dated outside 113.2 Mya to 85.7 Mya.

Early Cretaceous — about 2 of 6 occurrencesEarly CretaceousLate Cretaceous — about 4 of 6 occurrencesLate Cretaceous114–113 Mya — about 0.1 occurrences113–112 Mya — about 0.3 occurrences112–111 Mya — about 0.3 occurrences111–110 Mya — about 0.3 occurrences107–106 Mya — about 0.0 occurrences106–105 Mya — about 0.2 occurrences105–104 Mya — about 0.2 occurrences104–103 Mya — about 0.2 occurrences103–102 Mya — about 0.2 occurrences102–101 Mya — about 0.2 occurrences101–100 Mya — about 0.2 occurrences100–99 Mya — about 0.3 occurrences99–98 Mya — about 0.3 occurrences98–98 Mya — about 0.3 occurrences98–97 Mya — about 0.3 occurrences97–96 Mya — about 0.3 occurrences96–95 Mya — about 0.3 occurrences95–94 Mya — about 0.3 occurrences94–93 Mya — about 0.2 occurrences93–92 Mya — about 0.2 occurrences92–91 Mya — about 0.2 occurrences91–90 Mya — about 0.2 occurrences90–89 Mya — about 0.2 occurrences89–88 Mya — about 0.2 occurrences88–87 Mya — about 0.2 occurrences87–86 Mya — about 0.2 occurrences86–85 Mya — about 0.1 occurrences110.1 Mya89.8 Mya113.8 Mya85.2 Mya

6 occurrences of Strephinia convoluta on record, most of them in the Late Cretaceous. 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

6 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

West Melbury Marly Chalk — 51.58°N, 1.47°W

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The named rock units Strephinia convoluta has been recovered from, largest first. Drawn where the rock is now, not where it formed. 5 occurrences have no formation on record, which is common for older literature.

Strephinia convoluta and its relatives

Late Cretaceous

Where Strephinia convoluta and its relatives were recorded in the Late Cretaceous.

Found in the same rock

57 taxa

The Paleobiology Database records 4 sites for Strephinia convoluta, 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

4 references

Each of the 6 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 Strephinia convoluta

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

No 3D scan of Strephinia convoluta 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

What may have been alongside itStrephinia through timeFormations of the Late CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Hinde 1883