The progressive darkening of spores during burial is widely used as a matur
ation parameter in petroleum basins. The use of this parameter is limited b
y the subjective assessment of colour and the poor precision of the data. U
sing a spectral scanning microphotometer the spore colour can be recorded a
s the amount of light transmitted at different wavelengths in the visible s
pectrum. The spore transmittance value (% Sr) is derived from: %St = 100 x
T-550/(T-450 x T-650), where T is the transmission at wavelengths of 450, 5
50 and 650 nm. The % St has been determined from spore colour (SCI) standar
ds, artificially matured spores and pollen, and samples from two wells. The
results show that the spore transmittance is determined by palynormorph ty
pe, and while this increases the range of % St values obtained in a single
sample, the range of % St values obtained from different spore species with
in a sample overlap. The % St values increase with SCI values of spores use
d as SCI standards and with the temperature used in the laboratory maturati
on experiments. In the case of the geological samples the % St value increa
ses with depth. The increase in spore transmittance (% St) with increasing
maturity shows that the method has potential for use as a maturation parame
ter in hydrocarbon exploration. (C) 1999 Published by Elsevier Science Ltd.
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