Page 311 - Introduction to Paleobiology and The Fossil Record
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298  INTRODUCTION TO PALEOBIOLOGY AND THE FOSSIL RECORD


                      What do lampshells, moss animals and the        (microns in length) to the massive gigantopro-
                      rare tube-dwelling phoronids, or horseshoe      ductids (nearly 0.5 m wide). Although only
                      worms, have in common? They may look very       about 120 genera of brachiopods, also known
                      different, but these three phyla, the Brachiop-  as lampshells, survive today, they occupy a
                      oda, Bryozoa and Phoronida, all possess a       wide range of habitats from the intertidal
                      complex feeding organ, the lophophore, and      zone to the abyssal depths. The brachiopods
                      have similar body cavities or celoms. Never-    are entirely marine, bilaterally symmetric
                      theless the relationships among the three are   animals with a ciliated feeding organ, or loph-
                      not yet fully resolved, although the phoronids   ophore, contained within a pair of shells or
                      probably lie close to or may even be part of    valves. Internal structures such as  teeth and
                      the group, the bryozoans are more distantly     sockets, cardinal processes and various muscle
                      related. Our understanding has not changed      scars are all associated with the opening and
                      much since 1890, but new molecular studies      closing of the two valves during feeding cycles.
                      may help resolve these uncertainties in the     Brachiopods have featured in many paleoeco-
                      next 10 years.                                  logical studies of Paleozoic faunas, when they
                        The phoronids are tube-dwelling, worm-        dominated life on the seabed in terms of
                      like lophophorates, with the 10 or so described   numbers of both individuals and species.
                      species divided between two genera, Phoronis    Their use in paleobiogeographic analysis is
                      and Phoronopsis. These animals lack a min-      well documented (see Chapter 4). Neverthe-
                      eralized skeleton and pursue burrowing or       less brachiopods have also been widely used
                      boring life strategies with near-cosmopolitan   in regional biostratigraphy and, during the
                      distributions. The phylum has a long though     Silurian, a number of orthide, pentameride
                      questionable geological history, as some        and rhynchonellide lineages show good pros-
                      authors suggest that Precambrian and Lower      pects for international correlation.
                      Paleozoic records of the vertical burrow          Despite their relative low diversity today,
                      Skolithos (see p. 523) may possibly be the      living brachiopods are actually quite wide-
                      work of phoronids. The ichnogenus Talpina,      spread, represented mainly by forms attached
                      present as borings in both Cretaceous belem-    by pedicles to a variety of substrates across a
                      nite rostra and Tertiary mollusk shells, may    spectrum of water depths. At high latitudes
                      also have been constructed by phoronids.        brachiopods range from intertidal to basinal
                                                                      environments at depths of over 6000 m. They
                                                                      are most common in fjord settings in Canada,
                                                                      Norway and Scotland and in the seas around
                      BRACHIOPODA
                                                                      Antarctica and New Zealand. The associa-
                        It is no valid objection to this conclusion,   tion of the brachiopod  Terebratulina  retusa
                        that certain brachiopods have been but        growing on the horse mussel, Modiolus modi-

                        slightly modified from an extremely            olus, a bivalve, is widespread in the northern
                        remote geological epoch; and that certain     hemisphere. In the tropics, however, many
                        land and fresh-water shells have remained     species are minute, exploiting cryptic habi-
                        nearly the same, from the time when, as       tats, hiding in reef crevices or in the shade of
                        far as is known, they fi rst appeared.         corals and sponges. Larger forms live in
                                                                      deeper-water environments, out of the range
                                         Charles Darwin (1859)        of predators, like sea urchins, that graze on
                                       On the Origin of Species       the sumptuous meadows of newly attached
                                                                      larvae.
                        The brachiopods are one of the most suc-
                      cessful invertebrate phyla in terms of abun-
                      dance and diversity. They appeared fi rst in the   Morphology: brachiopod animal
                      Early Cambrian and diversifi ed  throughout      The brachiopod soft parts are enclosed by
                      the Paleozoic to dominate the low-level, sus-   two morphologically different shells or valves
                      pension-feeding benthos; a wide range of        that are opened and closed by a variety
                      shell morphologies and sizes characterize       of muscles; this arrangement is modifi ed
                      the phylum, from the tiny acrotretides          differently across the three subphyla – the
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