Their placement in the group is uncertain, some authors have considered them to be members of the modern shark groupGaleomorphi, while others have considered them to represent astem-group to modern sharks,[3][4] with some suggesting that they arebasal to the last common ancestor of modern sharks and rays.[5] There is also disagreement about the relationships betweenTriassic and earlier members of the group, only known from isolated teeth, and those from theJurassic onwards, with the similarity between the two groups possibly being superficial.[6]
The main shared characters of the group relate to teeth anatomy. The teeth roots have a distinctive pseudopolyaulacorhizevascularisation pattern, with a depression on the tooth root to where the nutritive grooves are confined.[4] While Klug (2010) recovered the group asmonophyletic,[4] the monophyly of the group has been doubted by other authors, who suggest that they represent aparaphyletic group,[5] and that the tooth vascularisation patterns do not clearly demonstrate that these sharks are more closely related to each other than to other sharks.[7] One family is unambiguously placed in the order,Palaeospinacidae. The familiesOrthacodontidae,Paraorthacodontidae andPseudonotidanidae, often considered members of the group, have been alternatively considered as members of the modern shark orderHexanchiformes rather than as members of Synechodontiformes.[7][8]
The oldest known synechodontiform remains are teeth ofSynechodus antiquus from the early Permian (Cisuralian) of the Ural Mountains.[9] However, other authors have considered the attribution to the teeth toSynechodus to be questionable.[6]
^C. J. Duffin and D. J. Ward. 1993. The Early Jurassic Palaeospinacid sharks of Lyme Regis, southern England. Belgian Geological Survey, Professional Papers, Elasmobranches et Stratigraphie 264:53-102
^Plamen S. Andreev & Gilles Cuny (2012). "New Triassic stem selachimorphs (Chondrichthyes, Elasmobranchii) and their bearing on the evolution of dental enameloid in Neoselachii".Journal of Vertebrate Paleontology.32 (2):255–266.Bibcode:2012JVPal..32..255A.doi:10.1080/02724634.2012.644646.S2CID84162775.