Conohibolites

Conohibolites

via GBIF · CC BY 4.0 · 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
MesohibolitidaePBDB
Diet
carnivorePBDB, for Cephalopoda
Life habit
nektonicPBDB, for Belemnitida
Motility
fast-movingPBDB, for Cephalopoda
Vision
well-developedPBDB, for Cephalopoda
Environment
marinePBDB, for Cephalopoda

Time the record covers

At least 11 million years on record.

The record covers at least 137.05 Mya to 125.77 Mya. No occurrence read is dated outside 154.8 Mya to 121.4 Mya.

Late Jurassic — about 3 of 12 occurrencesLate JurassicEarly Cretaceous — about 9 of 12 occurrencesEarly Cretaceous155–154 Mya — about 0.1 occurrences154–153 Mya — about 0.3 occurrences153–152 Mya — about 0.3 occurrences152–151 Mya — about 0.3 occurrences151–150 Mya — about 0.3 occurrences150–149 Mya — about 0.3 occurrences149–147 Mya — about 0.3 occurrences147–146 Mya — about 0.3 occurrences146–145 Mya — about 0.3 occurrences145–144 Mya — about 0.3 occurrences144–143 Mya — about 0.3 occurrences143–142 Mya — about 0.3 occurrences142–140 Mya — about 0.3 occurrences140–139 Mya — about 0.3 occurrences139–138 Mya — about 0.3 occurrences138–137 Mya — about 0.3 occurrences133–132 Mya — about 0.0 occurrences132–131 Mya — about 0.2 occurrences131–130 Mya — about 0.2 occurrences130–129 Mya — about 0.2 occurrences129–128 Mya — about 0.2 occurrences128–127 Mya — about 0.2 occurrences127–125 Mya — about 0.7 occurrences125–124 Mya — about 2 occurrences124–123 Mya — about 2 occurrences123–122 Mya — about 2 occurrences122–121 Mya — about 0.7 occurrences137.05 Mya125.77 Mya155.5 Mya120.7 Mya

12 occurrences of Conohibolites on record, most of them in the Early 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

12 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

2 formations

Štramberk Limestone — 49.58°N, 18.12°ELuckovska — 49.03°N, 18.33°E

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The named rock units Conohibolites has been recovered from, largest first. Drawn where the rock is now, not where it formed. 6 occurrences have no formation on record, which is common for older literature.

Conohibolites and its relatives

Early Cretaceous

Where Conohibolites and its relatives were recorded in the Early Cretaceous.

Found in the same rock

70 taxa

The Paleobiology Database records 3 sites for Conohibolites, 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 12 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 Conohibolites

Source
GBIF
Credit
via GBIF
Licence
CC BY 4.0
Commercial use
the licence allows it

No 3D scan of Conohibolites 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 itMesohibolitidae through timeFormations of the Early CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Janssen and Fozy 2005