Ancyloceratina
The Ancyloceratina were a diverse suborder of ammonite most closely related to the ammonites of order Lytoceratina. They evolved during the Late Jurassic but were not very common until the Cretaceous period, when they rapidly diversified and became one of the most distinctive components of Cretaceous marine faunas. They have been recorded from every continent and many are used as zonal or index fossils. The most distinctive feature of the majority of the Ancyloceratina is the tendency for most of them to have shells that are not regular spirals like most other ammonites. These irregularly-coiled ammonites are called heteromorph ammonites, in contrast to regularly coiled ammonites, which are called homomorph ammonites.

Neale Monks at English Wikipedia · 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
- AmmonitidaPBDB
- 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 least 102 million years on record.
The record covers at least 168.2 Mya to 66 Mya. No occurrence read is dated outside 170.9 Mya to 56 Mya.
7,938 occurrences of Ancyloceratina on record, most of them in the Late Cretaceous. The Paleobiology Database records this as a living group, and the chart stops with its fossils rather than at the present. 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
7,938 occurrences- Middle Jurassicunder 1%
- Late Jurassicunder 1%
- Early Cretaceous38%
- Late Cretaceous61%
- Paleoceneunder 1%
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
484 formations
- Pierre Shale Formation · Montana Group368
- Grès verts helvétiques Formation256
- Prairie Bluff Formation · Selma Group201
- Fox Hills Formation189
- Mancos Shale Formation131
- La Peña Formation120
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The named rock units Ancyloceratina has been recovered from, largest first. Drawn where the rock is now, not where it formed. 460 further formations hold fewer occurrences each and are not listed. 2,020 occurrences have no formation on record, which is common for older literature.
Ancyloceratina and its relatives
Late CretaceousWhere Ancyloceratina and its relatives were recorded in the Late Cretaceous.
Found in the same rock
725 taxa- Bryozoa54 sites
- Inoceramus38 sites
- Hoploscaphites35 sites
- Cataceramus subcompressus26 sites
- Barremites24 sites
- Phyllopachyceras infundibulum21 sites
- Cheloniceras20 sites
- Baculites gregoryensis18 sites
- Baculites perplexus18 sites
- Tropaeum17 sites
- Nuculana16 sites
- Deshayesites15 sites
- Resatrix15 sites
- Baculites14 sites
- Baculites gilberti14 sites
- Douvilleiceras mammillatum14 sites
- Hypacanthoplites14 sites
- Phylloceras (Hypophylloceras) ponticuli14 sites
- Euspira13 sites
- Baculites eliasi12 sites
- Entolium orbiculare12 sites
- Exogyra12 sites
- Holcodiscus12 sites
- Karsteniceras12 sites
The Paleobiology Database records at least 917 sites for Ancyloceratina, and this reads 240 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
659 references- Les grès verts helvétiques (Aptien moyen-Albien supérieur) de Haute-Savoie, Valais et Vaud (Alpes occidentales franco-suisses)345
- The stratigraphical palaeontology of the Lower Greensand226
- Upper Cretaceous ammonites of California. Part III205
- Lower Barremian ammonite biostratigraphy in the Subbetic Domain (Betic Cordillera, southern Spain)201
- Upper Cretaceous (Maestrichtian) Mollusca from the Haustator bilira Assemblage Zone in the East Gulf Coastal Plain199
- Scaphitid ammonites of the Upper Cretaceous (Maastrichtian) Fox Hills Formation in South Dakota and Wyoming186
- The Red Bird Section of the Upper Cretaceous Pierre Shale in Wyoming186
- Turrilitidy pozdnego Al'ba i Cenomana yuga SSSR127
- Geologie de Madagascar I. Les Terrains Sedimentaires125
- The larger invertebrate fossils of the Navarro group of Texas121
- Ammonite biostratigraphy of two stratigraphic sections of the La Peña Formation (Aptian, Lower Cretaceous) in Nuevo León State, northeast Mexico109
- Ammonite families Phylloceratidae, Gaudryceratidae, Oppeliidae and Desmoceratidae from Kopet Dagh Basin NE of Iran; palaeobiogeographical and palaeoecological application97
Each of the 7,938 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. 647 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 content1
Picture of Ancyloceratina
- Source
- Wikipedia/Commons
- Credit
- Neale Monks at English Wikipedia
- Licence
- CC BY-SA 3.0
- Commercial use
- the licence allows it
No 3D scan of Ancyloceratina 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.
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
What may have been alongside itAmmonitida through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Wiedmann 1966