Page 43 - Atlas of Sedimentary Rocks Under The Microscope
P. 43

Carbonate rocks                                        8 1 , 82, 83
                                                                         P  i s o  i d s  a n d   O  n c o  i d s



























                                                                        The  nomenclature  of carbonate grains which arc  larger
                                                                        than  2 mm  in  diameter  and  have  an  outer  layer  with
                                                                        concentric  laminae,  depends  to  a  certain  extent  on  an
                                                                        interpretation  of their  origin.  Thus  the  term pisoid  or
                                                                        pi.wlith  usually  refers to grains presumed to have formed
                                                                        inorganically, usually in a subaerial environment. On  the
                                                                        other  hand,  oncoids.  or oncoliflrs,  are  presumed  to  be
                                                                        biogenic. blue-green algae on the grain surfaces, trapping
                                                                        and binding fine sediment particles.
                                                                          81  is a photograph of a polished rock surface showing
                                                                        oncoids.  Note  the  size  of the  grains,  the  asymmetrical
                                                                        growth  and  the wavy nature  of many of the laminae,  all
                                                                        f e atures characteristic of oncoids. The bluish-grey areas
                                                                        arc sparry calcite and  the orange-brown areas arc stained
                                                                        with iron oxides.
                                                                          82 and 83 show concentrically-laminated grains whose
                                                                        origins  are  more  difficult  to  interpret.  82  shows  grains
                                                                        which arc about 2 mm in diameter. The outer surfaces arc
                                                                        not  as  smooth  as  most  ooids,  although  the  concentric
                                                                        lamination is very regular. Grains in the upper right show
                                                                        irregular outer coats of micrite and  some  particles have
                                                                        apparently grown together to form compound grains (e.g.
                                                                        lower left). This latter f e ature is unlikely to occur in ooids,
                                                                        where  precipitated  carbonate  laminae  are  formed while
                                                                        the grain is held in suspension. These grains are therefore
                                                                        interpreted  as  oncoids.  The  cement  is  sparite.  This
                                                                        photograph is of a thin section made by Sorby in 1849 and
                                                                        illustrates the  high  quality of his sections.
                                                                          83 shows grains with a regular. well-defined concentric
                                                                        layering. in  grains  up to 5 mm in diameter. This is typical
                                                                        of  inorganic  growth  and  these  grains  may  be  pisoids.
                                                                        Pisoid� are commonly fractured or broken. Broken pieces
                                                                        can  be seen  towards the  top  right of the  photograph.









                                                                        81:  Polis/red s w f ace.  L/anel�r  F o rmation.  Lower  Carbo­
                                                                        niferous. Blaen Onneu, South  Wales: magnification x I .8.
                                                                        82:  Unstai11ed thin  section.  Wenlock  Limestone.  Silurian,
                                                                        Mafl•em  Hills.  En�land: magnification x 13.  PPL.
                                                                        83: Stai11ed tlli11 section, L01rer Jurassic. Greece: magn(/ic­
                                                                        atioll x  I I .   PPI�.

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