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270  INTRODUCTION TO PALEOBIOLOGY AND THE FOSSIL RECORD












































                      (a)                                            (b)
                      Figure 11.10  Some archaeocyaths from the Lower Cambrian of Western Mongolia, in thin section:
                      (a) cryptic, solitary individual of Cambrocyathellus showing holdfast structures (×7.5), and (b)
                      branching Cambrocyathellus tuberculatus with skeletal thickening between individuals associated with
                      transverse sections of Rotundocyathus lavigatus (×5). (Courtesy of Rachel Wood.)

                      skeleton is usually buried in the sediment with   material. These groupings have now been

                      a basal flange and roots or holdfasts adding     shown to have little taxonomic value,
                      anchorage and stability. In some taxa, the      refl ecting  rather  ecological   preferences
                      intervallum is partitioned horizontally fi rstly   (Debrenne 2007). Most archaeocyaths are
                      by porous shelves or tabulae or secondly with   “Regulares”, including the orders Ajacicy-
                      aporous, convex dissepiments, often extend-     athida and Coscinocyathida; however the
                      ing into the adjacent central cavity.           apparent abundance of regular genera may be
                        Two main subdivisions have been defi ned       due to excessive taxonomic splitting. There
                      within the group: the “Regulares” and the       are fewer “Irregulares” but this ecogroup
                      “Irregulares”. The regular forms have an        includes the orders Archaeocyathida and
                      initial aporous, single-walled stage lacking    Kazachsetanicyathida.
                      dissepiments; soft tissue fi lled the entire body.
                      The inner and outer walls are punctuated by     Synecology: archaeocyath reefs
                      septa and tabulae developed either singly or
                      together. The irregular forms have initial      The archaeocyaths were exclusively marine,
                      aporous, single-walled stages with dissepi-     probably living at depths of 20–30 m on car-
                      ments. The twin walls have irregular pore       bonate substrates. The phylum developed an
                      structures, always dissepiments, and the skel-  innovative style of growth based on modular
                      eton is asymmetric; soft tissue was restricted   organization (Fig. 11.10). Such modularity
                      by the development of secondary skeletal        permitted encrusting abilities and the possi-
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