Aegocrioceras

Aegocrioceras is an extinct ammonite genus of cephalopod from the Lower Cretaceous included in the Ammonitida. It is known from northern Europe.

Aegocrioceras

H. Zell · CC BY-SA 3.0 · 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
AegocrioceratidaePBDB
Diet
carnivorePBDB, for Ammonoidea
Life habit
nektonicPBDB, for Ammonoidea
Motility
fast-movingPBDB, for Ammonoidea
Vision
well-developedPBDB, for Cephalopoda
Environment
marinePBDB, for Cephalopoda

Time the record covers

At most 12 million years on record.

Every occurrence read is dated to somewhere between 137.05 Mya and 125.77 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Early Cretaceous — about 2 of 2 occurrencesEarly Cretaceous137–137 Mya — about 0.0 occurrences137–136 Mya — about 0.0 occurrences136–136 Mya — about 0.0 occurrences136–136 Mya — about 0.0 occurrences136–135 Mya — about 0.0 occurrences135–135 Mya — about 0.0 occurrences135–134 Mya — about 0.0 occurrences134–134 Mya — about 0.0 occurrences134–133 Mya — about 0.0 occurrences133–133 Mya — about 0.0 occurrences133–133 Mya — about 0.0 occurrences133–132 Mya — about 0.1 occurrences132–132 Mya — about 0.1 occurrences132–131 Mya — about 0.1 occurrences131–131 Mya — about 0.1 occurrences131–131 Mya — about 0.1 occurrences131–130 Mya — about 0.1 occurrences130–130 Mya — about 0.1 occurrences130–129 Mya — about 0.1 occurrences129–129 Mya — about 0.1 occurrences129–129 Mya — about 0.1 occurrences129–128 Mya — about 0.1 occurrences128–128 Mya — about 0.1 occurrences128–127 Mya — about 0.1 occurrences127–127 Mya — about 0.1 occurrences127–126 Mya — about 0.1 occurrences126–126 Mya — about 0.1 occurrences126–126 Mya — about 0.1 occurrences137.6 Mya125.3 Mya

2 occurrences of Aegocrioceras 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

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

2 formations

Rio Mayer — 47.95°S, 72.12°WZapata — 51.14°S, 73.28°W

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

Aegocrioceras and its relatives

Early Cretaceous

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

Found in the same rock

14 taxa

The Paleobiology Database records 2 sites for Aegocrioceras, and this reads all of them. The number is how many of those sites it was catalogued from too.

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

2 references

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. 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 Aegocrioceras

Credit
H. Zell
Licence
CC BY-SA 3.0
Commercial use
the licence allows it

No 3D scan of Aegocrioceras was found in MorphoSource and Sketchfab.

Smithsonian Open Access was 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. Spath 1924