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Engonoceratidae ✝
Description | Engonoceratidae is a family of typically compressed, more or less flat sided and involute ammonites (cephalopod order Ammonitida) from the mid Cretaceous belonging to the Hoplitoidea. shells have flat sided outer rims (venters), at least in some stage. Single or branching irregular ribs and variably placed tubercles may occur. Sutures have numerous auxiliary and adventive elements of similar form, in general radially arranged. Forwardly divergent saddles tend to be simple, without subdivision. Lobes, pointing apically, may be simple and undivided or may be frilled with short irregular serrations. From Wikipedia article at https://en.wikipedia.org/wiki/Engonoceratidae, which is released under the Creative Commons Attribution-Share-Alike License 3.0. | ||||||||||||||||||||||||||||||||||||||||||||||||
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Source Data |
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Rank | family | ||||||||||||||||||||||||||||||||||||||||||||||||
Taxonomy (GBIF) | Life : Animalia : Mollusca : Cephalopoda : Ammonoidea : Engonoceratidae | ||||||||||||||||||||||||||||||||||||||||||||||||
Taxonomy (PBDB) | Life : Animalia : Mollusca : Cephalopoda : Ammonitida : Engonoceratidae | ||||||||||||||||||||||||||||||||||||||||||||||||
Taxonomic Status (GBIF) | accepted | ||||||||||||||||||||||||||||||||||||||||||||||||
Classification (PBDB,GBIF) |
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Scientific Name | Engonoceratidae | ||||||||||||||||||||||||||||||||||||||||||||||||
Opinions (PBDB) |
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Status (PBDB) | extinct | ||||||||||||||||||||||||||||||||||||||||||||||||
Taxon Size (PBDB) | 37 | ||||||||||||||||||||||||||||||||||||||||||||||||
First Recorded Appearance | 122 - 112 Ma Early/Lower Cretaceous | ||||||||||||||||||||||||||||||||||||||||||||||||
Last Recorded Appearance | 93.5 - 89.3 Ma Late/Upper Cretaceous | ||||||||||||||||||||||||||||||||||||||||||||||||
Motility | fast-moving (based on Ammonoidea) | ||||||||||||||||||||||||||||||||||||||||||||||||
Vision | well-developed (based on Cephalopoda) | ||||||||||||||||||||||||||||||||||||||||||||||||
Diet | carnivore (based on Ammonoidea) | ||||||||||||||||||||||||||||||||||||||||||||||||
Taphonomy | aragonite (based on Ammonoidea) | ||||||||||||||||||||||||||||||||||||||||||||||||
Primary Reference (PBDB) | W. J. Kennedy and M. D. Simmons. 1991. Mid-Cretaceous ammonites and associated microfossils from the Central Oman Mountains. Newsletters on Stratigraphy 25(3):127-154 | ||||||||||||||||||||||||||||||||||||||||||||||||
Wikipedia | https://en.wikipedia.org/wiki/Engonoceratidae |
Fossil Distribution
Subtaxa
Name | Status | Common Name(s) | Fossil Occurrences | Oldest | Youngest |
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Engonoceras ✝ genus | accepted (GBIF) listed (PBDB) | 42 | 113 Ma Early/Lower Cretaceous | 99.6 Ma Late/Upper Cretaceous | |
Metengonoceras ✝ genus | accepted (GBIF) listed (PBDB) | 49 | 122 Ma Early/Lower Cretaceous | 93.5 Ma Late/Upper Cretaceous | |
Neolobites ✝ genus | accepted (GBIF) listed (PBDB) | 40 | 101 Ma Late/Upper Cretaceous | 99.6 Ma Late/Upper Cretaceous | |
Platiknemiceras ✝ genus | accepted (GBIF) listed (PBDB) | 5 | 112 Ma Early/Lower Cretaceous | 112 Ma Early/Lower Cretaceous | |
Protengonoceras ✝ genus | accepted (GBIF) listed (PBDB) | 3 | 109 Ma Early/Lower Cretaceous | 105 Ma Early/Lower Cretaceous | |
Engohoplitoides zumoffeni species | accepted (GBIF) | No associated record in PBDB |
Synonymy List
Year | Name and Author |
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1900 | Engonoceratidae Hyatt |
1991 | Engonoceratidae Kennedy and Simmons p. 132 |
1992 | Engonoceratidae Meister et al. p. 59 |
1994 | Engonoceratidae Kennedy p. 221 |
1994 | Engonoceratidae Meister et al. p. 191 |
1998 | Engonoceratidae Kennedy et al. p. 7 |
Year | Name and Author |
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1998 | Engonoceratidae Lucas and Estep p. 78 |
2005 | Engonoceratidae Kennedy p. 357 |
2008 | Engonoceratidae Aly et al. p. 46 |
2010 | Engonoceratidae Bulot |
2018 | Engonoceratidae El Qot p. 156 |
2018 | Engonoceratidae Robert et al. p. 9 |
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
Vagos, Aveiro, Portugal