Page 396 - Introduction to Paleobiology and The Fossil Record
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ECDYSOZOA: ARTHROPODS      383





















                                                            (b)






















             (a)                                            (c)

             Figure 14.21  Carboniferous shrimps: (a) Tealliocaris woodwardi from the Gullane Shrimp Bed, near
             Edinburgh (×4); (b) Waterstonella grantonensis from the Granton Shrimp Bed, near Edinburgh (×2);
             (c) Crangopsis socialis and Waterstonella grantonensis from the Granton Shrimp Bed (×2). (Courtesy of
             Euan Clarkson.)


             described from the Granton Shrimp Bed by        structions and, at some levels in the strati-
             Euan Clarkson (University of Edinburgh) and     graphic record, have been used for correlation.
             his colleagues (Fig. 14.21).                      Ostracodes have weak segmentation with a
                                                             poorly defined head, thorax and abdomen;

                                                             the animal is contained within the two shells,
             Ostracodes
                                                             with the carapace united dorsally by an elastic
             Ostracodes are crustacean arthropods, abun-     ligament and a variably developed hinge.
             dant and widespread in aquatic environments.    Growth is by periodic ecdysis or molting. Fol-
             They have small bivalved carapaces, hinged      lowing each molt phase the carapace initially
             along the dorsal margin (Fig. 14.22a). The      develops as a pair of chitinous valves enclos-
             carapace is perforate and completely covers     ing the animal; most of the carapace is

             the entire animal when closed. Most ostra-      then calcified, except the dorsal margin that
             codes are benthic, swimming, crawling or        remains as a chitinous ligament forcing the
             burrowing at the sediment–water interface in    valves apart when the internal adductor
             muds or silts with abundant organic material.   muscles relax. The central muscle scars vary
             A few, such as the myodocopids, are plank-      across the class (Fig. 14.22b), from complex
             tonic and some are commensal or parasitic.      patterns in the Leperditicopida to a single scar
             They are very useful for environmental recon-   in some members of the Palaeocopida.
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