FlabelloideaStephen D. Cairns
Representatives of this superfamily occur from the Late Jurassic (135 million years ago) to the Recent, and are widespread in the world oceans and commonly found as fossils on all continents, including Antarctica. All known species are azooxanthellate, and occur at depths of 0-3200 meters. Most species are inconspicuous by virtue of small size (as small as 1 mm calicular diameter) or cryptic and/or deep habitat. Approximately 110 living species in 18 genera have been described (Cairns et al., 1999), and about twice that number of fossil species. All flabelloideans are solitary in growth form; some of them asexually reproduce by transverse division and various forms of budding. Although inconspicuous, some occur in large numbers in certain environments.
The superfamily is characterized by having coralla with a marginothecate wall, as opposed to a septothecal or parathecal wall of the superfamily Caryophyllioidea, or the epithecal wall of the Volzeioidea. Structurally, the marginotheca (Stolarski, 1995) is a primitive, neotenic wall consisting of vertically arranged minitrabeculae that are manufactured from the edge zone of the coral. Additional smooth, non-trabecular calcium carbonate deposits called textura (Stolarski, 1995), literally "plaster" in Latin, are often secreted on the outside of the corallum by the edge zone, and occasionally nontrabecular calcium carbonate is also deposited within the corallum in a structure called stereome. The wall of flabelloids is not epithecate, as previously thought (see Stolarski, 1995), since it consists of trabeculae (epitheca is nontrabecular) and originates from the edge zone (epitheca originates from a lappet cavity). Marginotheca is usually quite smooth, often porcellaneous, but may exhibit low circumferential growth ridges.
No phylogenetic analysis has been performed on the suprageneric taxa of the Caryophylliina. Chevalier (1987) did not acknowledge superfamilies within the suborder Caryophylliina. Most recently, Stolarski (1995, 2000) has examined the wall microstructure of many of the flabelloid genera, which led to a redefinition of some wall terminology and will ultimately lead to the redistribution of some of the genera and even families within this suborder.
Cairns S. D., B. W. Hoeksema, and J. van der Land. 1999. Appendix: List of Extant Stony Corals. Atoll Research Bulletin, 459: 13-46.
Cairns S. D. and S. A. Parker. 1992. Review of the Recent Scleractinia (Stony Corals) of South Australia, Victoria and Tasmania. Records of the South Australian Museum, Monograph Series, 3: 82 pp.
Chevalier, J.-P. 1987. Ordre des Scléractiniares: Systématique. Pp. 679-753 In: Grassé, P. (editor) Traité de Zoologie, 3(3) Masson, Paris.
Stolarski, J. 1995. Ontogenetic development of the thecal structures in caryophylliine scleractinian corals. Acta Palaeontologica Polonica, 40: 19-44.
Stolarski, J. 2000. Origin and phylogeny of Guyniidae (Scleractinia) in the light of microstructural data. Lethaia, 33: 13-38.
Vaughan, T. W. and J. W. Wells. 1943. Revision of the suborders, families, and genera of the Scleractinia. Geological Society of America, Special Papers, 44: 363 pp.
Wells, J. W. 1956. Scleractinia. Pp. F328-F444 In: Moore, R. C. (editor) Treatise on Invertebrate Paleontology, Part F: Coelenterata. University of Kansas Press, Lawrence.
Technical assistance was rendered by Adorian Ardelean.
Correspondence regarding this page should be directed to Stephen D. Cairns at
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- First online 28 October 2002
Citing this page:
Cairns, Stephen D. 2002. Flabelloidea http://tolweb.org/Flabelloidea/19020/2002.10.28 in The Tree of Life Web Project, http://tolweb.org/. Version 28 October 2002.