Page 55 - Atlas of Sedimentary Rocks Under The Microscope
P. 55

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            Carbonate rocks                                      112, 113,  1 4
                                                                              B  i o c l asts
                                                                             Algae


















                                                                             Those algae in which all or part of  the skeleton b e c o mes
                                                                             calcified arc known as  the skeletal calcareous algae. They
                                                                             arc  important  contributors  to  carbonate  sediments
                                                                             throughout the Phanerozoic and exhibit a wide diversity
                                                                             of  fo rms.  Green  algae  arc  one  of the  most  important
                                                                             groups and the photographs on this page illustrate three
                                                                             examples.  one  from  each  of  the  major  groups,  the
                                                                             Codiaceae,  Dasycladaceae  and  Charophyceae.  For de·
                                                                             tails of calcareous algae see Johnson (1961), Wray (1977)
                                                                             and t=l tigel ( 1982).
                                                                               1 1 2    shows segments of one of the common f o r m s   of
                                                                             codiacean  alga,  Halimeda.  which  still  occurs  toda)
                                                                             Living examples contain organic filaments embedded in
                                                                             aragonite.  The  example  shown  is  from  a  poorl)·
                                                                             consolidated  Quaternary  sediment  which  had  to  be
                                                                             impregnated with resin before a peel could be made. The
                                                                             grey areas between  the algal segments and in the holes
                                                                             originally occupied by the filaments are the imprcgnat mg
                                                                             medium.  In this sample the Halimeda  segments arc sull
                                                                             aragonite, although the wall structure cannot be seen at
                                                                             this magnification. Halimeda fragments are often poorly­
                                                                             preserved because of the loss of microstructure during the
                                                                             replacement of aragonite by calcite.
                                                                               113 shows two types of algae. The large fragment with
                                                                             the honeycomb structure and walls of fine-grained calcite
                                                                             is  the  common  Carboniferous  dasycladacean  alga
                                                                             Koninckopora.  Several algal segments of a different  type
                                                                             can  be  seen  below  the  Koninckopora.  At  the  level  of
                                                                             viewing here they have no  discernible wall structure and
                                                                             there is a slight resemblance to echinoderm fragments. In
                                                                             fact they have a fine fibrous wall structure and hence arc
                                                                             not  !>inglc  crystals.  They  may  show  branching and an
                                                                             example of Y-branching can  be seen  in  the  lower-right
                                                                             part  of the  photograph.  These  belong  to a  problematic
                                                                             group. often  referred  to  as ancestral coralline algae, but
                                                                             sometimes classified with  the  f o raminifera or stromato·
                                                                             poroids.
                                                                              The  third  group  of green algae arc  the charophyte1.
                                                                            although these are sometimes classified separately. ThC)
                                                                            arc  frc!>hwater  plants.  occurring  in  the  Mesozoic  and
                                                                            Cenozoic. and usually only the reproductive parts (oogo­
                                                                             n•a) arc calcified. These are small egg-shaped bodies 11ith
                                                                            vanou!> ornaments.  1 1 4  shows  three  oogonia  in cr�.
                                                                            section.
                                                                             112: Swinecl ace/ate peel.  Quaternary.  Mombasa. Kenya,
                                                                            magniftcation x  13.  PPL.
                                                                             113: Stained thin  section.  Chee  Tor  Rock,  Lmrer Carbo·
                                                                            ni/erou.\,  Tunstead  Quarry,  Derbyshire.  England: magm(
                                                                            ication  x  17. PPL.
                                                                             114: Swined thin section. lggui el Behar F o r marion. U p pt r
                                                                            Jurassic,   Wesrem   High   A rlas,   Morocco:  magn(fi(
                                                                            arion x 56. PPL.
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