Page 47 - Atlas of Sedimentary Rocks Under The Microscope
P. 47

Carbonate rocks                                         90, 91, 92
                                                                        B  i o c l asts

                                                                        B  r achiopods
























                                                                        The articulate brachiopods are important constituents of
                                                                        Palaeozoic  and  Mesozoic limestones. They  were  origin­
                                                                        ally calcite and so their shell structures are weB-preserved.
                                                                        Typically, brachiopods have a thick inner layer of calcite
                                                                        fibres  aligned  with  their  length  at  a  low  angle  to  the
                                                                        shell  wall. A thin outer prismatic layer may be preserved.
                                                                          90 shows a broken brachiopod of which parts of both
                                                                        valves arc present and surrounded by a micrite envelope
                                                                        (p.  54).  The  fibrous  structure  is  clearly  visible,  as  are
                                                                        tine tubes at right angles to the shell wall. filled with blue­
                                                                        �taincd fer roan calcite cement. These are endopunctae and
                                                                        they  characterize  some  groups  of  brachiopods.  The
                                                                        sample also shows a good example of coarse. blue-stained
                                                                        f c rroan calcite cement.
                                                                          91  shows two  large fragments of pseudopunctate  bra-
                                                                        chiopods.  In  these.  the  fibrous  wa11  structure  is  inter­
                                                                        rupted.  not by open tubes but by calcite rods. The left­
                                                                        hand  fragment  shows  the pseudopunctae sectioned  par­
                                                                        allel  to  their length.  Note  the  wavy  nature of the  fibres
                                                                        adjacent to the pseudopunctae. The right-hand fragment
                                                                        is a section of a shell showing the pseudopunctae in cross­
                                                                        section.
                                                                          92  illustrates  a  brachiopod  fragment  with  its  outer
                                                                        prismatic layer preserved. The f o liated nature of the inner
                                                                        part  of  the  wall  is  also  well  shown.  The  shape  of  the
                                                                        fragment suggests that it is part of a ribbed shell. It is also
                                                                        illlfllllltlllte.  lacking either endopunctac or pscudopunc­
                                                                        tae.  These  factors  in  an  Upper  Jurassic  brachiopod
                                                                        indicate that it  is part of a rhynchonellid. The fine-grained
                                                                        calcite  matrix  contains  abundant  colourless  fine  sand­
                                                                        and silt-size quartz.









                                                                        90: Swi11ed tlti11 section.  I n f erior  Oolite.  Middle Jurassic.
                                                                        l.ec� hampton  Hill.  Glm1c�srersltire.  England:  magnific­
                                                                        ation x 32. PPL.
                                                                        91: Stained tltin  section.  Monsal  Dale  Limestone.  Lmrer
                                                                        Carhon(f' erous.  Cressbrook  Dale.  Derbyshire.  England:
                                                                        lllliKII(/ication x  16. PPL.
                                                                        92:  Stained tltin section.  Upper Jurassic.  Jehel  Amsilf<'ll.
                                                                        Morocco: magnification x 40.  PPL.

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