Conulariida

Conulariida

James St. John · CC BY 2.0 · via Wikidata/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
ConulataePBDB
Diet
suspension feederPBDB
Life habit
epifaunalPBDB
Motility
stationary, attachedPBDB
Vision
blindPBDB, for Scyphozoa

Time the record covers

At least 333 million years on record.

The record covers at least 538.8 Mya to 205.7 Mya. No occurrence read is dated outside 635 Mya to 201.4 Mya.

Cambrian — about 26 of 596 occurrencesCambrianOrdovician — about 199 of 596 occurrencesOrdovicianSilurian — about 79 of 596 occurrencesDevonian — about 90 of 596 occurrencesDevonianCarboniferous — about 86 of 596 occurrencesCarboniferousPermian — about 99 of 596 occurrencesPermianEarly Triassic — about 1 of 596 occurrencesMiddle Triassic — about 1 of 596 occurrencesLate Triassic — about 13 of 596 occurrencesEarly Jurassic — about 0 of 596 occurrences644–629 Mya — about 0.1 occurrences629–614 Mya — about 0.3 occurrences614–599 Mya — about 0.3 occurrences599–584 Mya — about 0.3 occurrences584–569 Mya — about 0.3 occurrences569–553 Mya — about 0.3 occurrences553–538 Mya — about 0.5 occurrences538–523 Mya — about 14 occurrences523–508 Mya — about 10 occurrences508–493 Mya — about 2 occurrences493–478 Mya — about 8 occurrences478–463 Mya — about 30 occurrences463–448 Mya — about 125 occurrences448–433 Mya — about 62 occurrences433–418 Mya — about 56 occurrences418–403 Mya — about 32 occurrences403–388 Mya — about 29 occurrences388–373 Mya — about 18 occurrences373–358 Mya — about 8 occurrences358–343 Mya — about 10 occurrences343–328 Mya — about 15 occurrences328–313 Mya — about 18 occurrences313–298 Mya — about 43 occurrences298–283 Mya — about 35 occurrences283–268 Mya — about 21 occurrences268–253 Mya — about 38 occurrences253–238 Mya — about 7 occurrences238–223 Mya — about 5 occurrences223–208 Mya — about 2 occurrences208–193 Mya — about 6 occurrences538.8 Mya205.7 Mya644 Mya193 Mya

596 occurrences of Conulariida on record, most of them in the Ordovician. 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

596 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

255 formations

Graham — 32.73°N, 98.64°WGraham — 33.26°N, 98.12°WGraham — 33.24°N, 98.08°WGraham — 33.17°N, 98.16°WGraham — 33.13°N, 98.16°WGraham — 33.10°N, 98.40°WGraham — 33.12°N, 98.30°WGraham — 33.00°N, 98.54°WOlive Series — 32.70°N, 72.96°EOlive Series — 32.80°N, 73.09°EZahorany — 50.00°N, 14.00°EGydo — 33.30°S, 21.83°EGydo — 33.52°S, 24.74°EGydo — 32.64°S, 19.41°EGydo — 33.31°S, 22.43°EGydo — 34.01°S, 23.46°EPonta Grossa — 24.25°S, 49.70°WPonta Grossa — 26.07°S, 52.58°WPonta Grossa — 25.08°S, 50.15°WPonta Grossa — 24.50°S, 50.40°WLiben — 50.00°N, 14.00°ELiben — 49.74°N, 13.54°ELiben — 49.72°N, 13.57°ELiben — 49.80°N, 13.63°ELiben — 49.82°N, 13.75°EVinice — 50.00°N, 14.00°ELetna — 50.00°N, 14.00°ERed River — 52.13°N, 97.52°WRed River — 52.09°N, 97.88°WRed River — 52.42°N, 97.98°WRed River — 52.06°N, 97.44°WVerulam — 44.60°N, 78.97°WVerulam — 44.45°N, 78.70°WVerulam — 44.52°N, 78.97°WVerulam — 44.43°N, 78.78°WVerulam — 44.48°N, 78.95°WMaidiping — 29.53°N, 103.39°EBohdalec — 50.00°N, 14.00°EBohdalec — 50.00°N, 14.38°EMuldraugh — 40.04°N, 86.87°WMuldraugh — 40.06°N, 86.90°WRochester Shale — 43.15°N, 77.62°WRochester Shale — 43.10°N, 79.06°WRochester Shale — 39.65°N, 78.76°WMount Ida — 36.77°S, 144.77°EMotol — 49.95°N, 12.93°EMotol — 50.00°N, 17.78°EMotol — 49.97°N, 14.13°ENavas de Estena — 39.00°N, 4.00°WHunsrück Slate — 49.89°N, 7.47°EHunsrück Slate — 49.83°N, 7.37°EPimenteira — 7.00°S, 42.00°WPimenteira — 6.33°S, 41.42°WPimenteira — 8.82°S, 48.40°WPimenteira — 8.38°S, 48.00°WMara — 21.74°S, 165.69°EMara — 21.75°S, 165.70°EMara — 21.98°S, 166.05°ECampile — 53.44°N, 7.23°WCampile — 53.22°N, 7.93°WCampile — 53.45°N, 7.17°WBarfield — 25.21°S, 150.22°ESolvik — 59.92°N, 10.75°ESyracuse — 43.05°N, 76.15°WSyracuse — 43.07°N, 76.33°WSyracuse — 43.05°N, 76.15°W

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The named rock units Conulariida has been recovered from, largest first. Drawn where the rock is now, not where it formed. 231 further formations hold fewer occurrences each and are not listed. 51 occurrences have no formation on record, which is common for older literature.

Conulariida and its relatives

Ordovician

Where Conulariida and its relatives were recorded in the Ordovician.

Found in the same rock

3,514 taxa

The Paleobiology Database records 473 sites for Conulariida, and this reads 240 of them. Of that, one read hit the database's own return limit, so every count below is a floor rather than a total. 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

237 references

Each of the 596 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. 225 further references are not listed. 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 content2

Picture of Conulariida

Credit
James St. John
Licence
CC BY 2.0
Commercial use
the licence allows it

3D model

Source
Sketchfab
Licence
CC Attribution
Commercial use
cannot be read from the licence given — check the record

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. Miller and Gurley 1896