Craticularia parallela

Craticularia parallela

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
CraticulariaPBDB
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 12 million years on record.

The record covers at least 161.5 Mya to 149.2 Mya. No occurrence read is dated outside 165.3 Mya to 143.1 Mya.

Middle Jurassic — about 1 of 21 occurrencesMiddle JurassicLate Jurassic — about 20 of 21 occurrencesLate JurassicEarly Cretaceous — about 0 of 21 occurrences166–165 Mya — about 0.1 occurrences165–164 Mya — about 0.2 occurrences164–163 Mya — about 0.2 occurrences163–163 Mya — about 0.2 occurrences163–162 Mya — about 0.2 occurrences162–161 Mya — about 0.2 occurrences161–160 Mya — about 0.1 occurrences160–160 Mya — about 0.1 occurrences160–159 Mya — about 0.5 occurrences159–158 Mya — about 2 occurrences158–157 Mya — about 2 occurrences157–157 Mya — about 2 occurrences157–156 Mya — about 2 occurrences156–155 Mya — about 2 occurrences155–154 Mya — about 0.9 occurrences154–153 Mya — about 0.7 occurrences153–153 Mya — about 0.7 occurrences153–152 Mya — about 1 occurrence152–151 Mya — about 2 occurrences151–150 Mya — about 2 occurrences150–150 Mya — about 2 occurrences150–149 Mya — about 0.9 occurrences149–148 Mya — about 0.3 occurrences148–147 Mya — about 0.3 occurrences147–146 Mya — about 0.3 occurrences146–146 Mya — about 0.3 occurrences146–145 Mya — about 0.2 occurrences145–144 Mya — about 0.1 occurrences144–143 Mya — about 0.1 occurrences143–143 Mya — about 0.0 occurrences161.5 Mya149.2 Mya165.8 Mya142.6 Mya

21 occurrences of Craticularia parallela on record, most of them in the Late Jurassic. 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

La Manga — 35.95°S, 69.98°WPeral — 37.12°N, 8.18°WCalcaires Lites — 45.78°N, 5.52°ECouches de Birmensdorf — 46.25°N, 5.67°E

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The named rock units Craticularia parallela has been recovered from, largest first. Drawn where the rock is now, not where it formed. 16 occurrences have no formation on record, which is common for older literature.

Craticularia parallela and its relatives

Late Jurassic

Where Craticularia parallela and its relatives were recorded in the Late Jurassic.

Found in the same rock

211 taxa

The Paleobiology Database records 20 sites for Craticularia parallela, 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

10 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 Craticularia parallela

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

No 3D scan of Craticularia parallela 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 itCraticularia through timeFormations of the Late JurassicThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (Goldfuss 1826)