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              The branching coral Madracis mirabilis 
              occasionally forms large thickets. These assemblages can be 
              well over 500m2. The architecture of these branching corals leads 
              to sediment falling out between their branches. Any structure in 
              the path of water flow will slow down the water flow, thus increased 
              the amount of sediment trapped between the branches. Over time, 
              this process starts burring the corals. These in turn keep growing 
              and as long as the growth rate outruns the sedimentation rate the 
              reef continues to grow.  
            Although 
              dominated by M. mirabilis, Porites porites is another common 
              branching species interspersed in these ologi-specific aggregations. 
              The largest and most impressive ones run perpendicular to the shoreline 
              near Mero where individual ridges reach dimensions of up 
              to 1000 m2. The local dive site where these reefs are found is called 
              Maggie's Point. Smaller formations are found throughout the west 
              coast where reef accretion has take place. At Cachacrou (Scott's 
              Head) only a few remnants of large formations of this kind are alive, 
              due to the heavy use of this reef. In 2007 our survey team also 
              identified small patches of up to approx. 25m2 in the southern region 
              of Dominica near Fond Saint Jean.  
            The 
              2005 bleaching episode severely affected the abundance of P. 
              porites, which in 2006 had virtually disappeared from many sites. 
              This was also very evident in the M. mirabilis assemblages, 
              previously containing substantial amounts of P. porites. 
            SCCS1107 
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