The possible origin of the characteristic compositions of pyrolysates of or
ganic fossil leaf cuticles has been investigated by heat treatment of cutic
les of recent Kalanchoe glandiflora followed by flash pyrolysis-gas chromat
ography. Dewaxed cuticles, whether heat-treated or not, yield mainly cyclic
compounds from adventitious cell-wall material together with cutin monomer
s. The pyrolysate of waxy cuticle includes the same compounds but is domina
ted by wax components which are simply desorbed unchanged under the conditi
ons of pyrolysis. However prior heat treatment of waxy cuticle transforms t
he pyrolysate so that its chromatogram shows a prominent series of alkene-a
lkane peaks from C-8 to C-34, typical of fossil leaf cuticles. It is conclu
ded that leaf waxes, instead of or in addition to cutan, are a principal so
urce of the aliphatic constituents of organic fossil leaf cuticles. (C) 200
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