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THE BASAL METAZOANS: SPONGES AND CORALS  283





                        Box 11.5  Rugosan life strategies

               Despite the apparent simplicity of rugosan architecture, these corals may have pursued a number of
               different life strategies (Fig. 11.24). A number of corals, for example Dokophyllum, probably sat
               upright in the sediment rooted by fine holdfasts extending from the epitheca. Other taxa, such as

               Holophragma, were initially attached to a patch of hard substrate but subsequently toppled over to
               rest on the seabed. Grewingkia was cemented to areas of hard substrate. The small discoidal Pal-
               aeocyclus, however, may have been mobile, creeping over the substrate on its tentacles. A number
               of strongly curved rugosans, for example Aulophyllum, probably lay within the substrate, concave
               upwards. Successive increments of growth were directed more or less vertically giving the coral
               exterior a stepped appearance. Many other solitary corals exhibit a similar terraced theca, which
               may be due to changes in growth direction associated with adjustments following toppling of the
               corallum during slight turbulence or storms.











                            Attached to clast                                Recumbent








                                                    Fixosessile
                                                                             Recumbent
                                 Rhizosessile

               Figure 11.24  Rugose solitary life strategies displaying attached, fi xosessile, rhizosessile and
                recumbent life modes. (Based on Neuman; B.E.E. 1988. Lethaia 21.)





             phaceloid Syringopora, with long, thin, cylin-  sans. Secondary septa are inserted in all six
             drical corallites, characterize the coral faunas   spaces between the primary or cardinal septa.
             of the period. By the Late Permian the group    In further contrast to septal insertion in the
             was very much in decline following a long       rugosans, each cycle of six is fully completed
             period of deterioration after the Frasnian      before the next cycle of insertion commences.

             extinctions; only five families survived to the   Tabulae are absent, although dissepiments
             end of the period.                              and dissepimentaria are developed. Moreover
                                                             the scleractinian skeleton, although relatively
             Scleractinian corals                            light and porous, has the stability of a basal
                                                             plate which aids anchorage in the substrate.
             The scleractinians are elegant zoantharian      Additionally, the scleractinian polyp can
             corals with relatively light, porous skeletons   secrete aragonite on the exterior of the coral-
             composed of aragonite (Fig. 11.29). Both soli-  lite, often in the form of attachment struc-
             tary and colonial modes exist with even more    tures. Both adaptations provided a much
             varied architectures than those of the rugo-    greater potential for reef building than the less
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