Phytoliths from Ashed Cedar Bark
                These are phytoliths from ashed Cedar Bark. This is from a
                  section of
                  Cedar bark that was ashed in a muffle furnace.
              
              
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Definition/Function:
                Significance in the Environment:
                Calcareous phytoliths may remain intact as the plant degrades. When the plant containing
                calcium oxalate phytoliths is burned
                the phytoliths go through a series of chemical reactions. First they begin to loose the
                waters of hydration. That begins at about 120 degrees
                Celsius. Next, carbon monoxide is released and calcium carbonate begins to form on the
                surface of the crystal. That begins at a temperature of about
                420 degrees Celsius. At this point the crystal generally still maintains its original
                shape. The crystal shows the effect of the exposure to heat
                but the shape is still consistent with that characteristic of the original plant.
                Continued heating ultimately result in the formation of a calcium
                oxide, begining at about 620 Celsius. Cubical calcium oxide and hydroxide particles are
                common in the plume from the combustion of wood, often
                showing surface modification to the carbonate. The surface modification is evident as a
                birefringent film over part of the particle.
                Characteristic Features:
                Associated Particles:
                References: