Tainoceratoidea Hyatt, 1883
publication ID |
https://doi.org/10.5852/ejt.2025.1017.3065 |
publication LSID |
lsid:zoobank.org:pub:BFD619DA-1648-440D-BF28-4BF0724CA6A0 |
DOI |
https://doi.org/10.5281/zenodo.17252502 |
persistent identifier |
https://treatment.plazi.org/id/03BF2F39-FFAE-6503-7025-BCEE8CF1F95D |
treatment provided by |
Plazi |
scientific name |
Tainoceratoidea Hyatt, 1883 |
status |
|
Superfamily Tainoceratoidea Hyatt, 1883
Diagnosis
Superfamily of the suborder Tainoceratina with a discoidal to pachyconic, subinvolute or subevolute conch. Whorl profile always with midventral longitudinal groove; in early species subquadrate with a distinct ventrolateral shoulder and a distinct umbilical margin, in derived species polygonal with divergent or convergent flanks. Dorsal whorl zone always very small. Sculpture with rows of ventrolateral nodes, in some species with rows of nodes on the flank. Septa simply domed; suture line depending on the whorl profile, usually with shallow lobes and low saddles.
Included family
Tainoceratidae Hyatt, 1883 (Late Carboniferous to Early Triassic; 23 Palaeozoic genera, 89 Palaeozoic species).
Remarks
The superfamily Tainoceratoidea as used here corresponds to the family Tainoceratidae as employed by earlier authors. It is generally regarded as one of the most important Late Carboniferous to Triassic nautiloid clades. Its family composition and internal classification have been discussed repeatedly over the last 90 years, and various concepts for the differentiation of the genera have been presented. As many of the other families of the suborder are placed within the Pleuronautiloidea , only one family is accepted here:
Tainoceratidae Hyatt, 1883 – Forms with usually octagonal whorl profile; sculpture usually with several rows of nodes ( Fig. 30 View Fig ).
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.