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The soils of the area are described by Gunn (1972a). Additional features of the physical environment are contained in Lucas and De Keyser (1965), De Keyser and Lucas (1968) and Whitaker and Gibson (1977). Climate This area of Cape York Peninsula has a subhumid to humid tropical climate with marked with wet and dry seasons. According to Nix and Kalma (1972), shifts of the intertropical convergence zone dominate the climate of the region. During the dry season (May to October) whilst southeasterly Trade winds prevail, the intertropical convergence zone is well to the north of the Australian continent and dry relatively cool weather and only very light rainfalls occur.

Relative Quadrat Density (%) = Number of individuals of one species x 100 Number of individuals of all species in that quadrat For each quadrat, this parameter equals 100% and it measures the density of each species in relation to the other species in the same quadrat. H. H. = girth at breast height). / ; ........ 'I -\ Cer; ps -- - - Brug ulerc / i'-.. •. 10 20 \ / 30 Q -- \\ \ 40 V7 ,,/ / / so I \ ,' ,/ ,. / ~ r--.... T 110 , , \ , " f. ) , ,, , \ \' '. -~ --- , I: '" '- § Q . - ... ~ Sonn erat ~ '

In: Interdisciplinary Studies of Peat and Coal Origins. pp. 18-49, Geol. Soc. America Microform Pub. 7. A. I. F. Laughan. 1974. Fossil plants and coal: patterns of change in Pennsylvanian coal swamps of the Illinois Basin. Science 184: 1367-1369. L. I. DeMaris. 1980. Stratigraphic patterns of Pennsylvanian coal swamps in Midcontinent and Appalachian regions of the United States. GSA Abst. with Progs. Vo. 12:498-499. L. In press. Stratigraphic Ranges of Miospores in Coals of the Des Moines Series of Southern Iowa.

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