ARE COAL BALLS RARE? A CYCLOSTRATIGRAPHIC ANALYSIS
Through the Desmoinesian/Missourian boundary interval, North American paleotropical climates became drier and tree ferns replaced lycopsids as the dominant plants in paleomires. Significantly more cycles dominated by lycopsids or cordaiteans have coal balls than cycles dominated by tree ferns. Overall, 44% of cycles (18/41) with lycopsid or cordaitean dominance have coal balls, whereas 21% (9/43) of cycles with tree fern dominance have coal balls (p < 0.01). While 25% (5/20) of minor cycles with lycopsid or cordaitean dominance have coal balls, no minor cycle with tree fern dominance has coal balls.
This pattern may reflect the relative abundance of coal in latest Atokan – Desmoinesian vs Missourian – Virgilian cycles, with drier paleotropical climates leading to less paleotropical coal and fewer coal balls. Rygel et al. (2008) reported increased erosional relief in clastic facies of Missourian-Virgilian cycles, which would have increased the amplitude and rate of sea-level change during each glacial-eustatic cycle. Faster sea-level rise could affect coal-ball abundance, particularly if coal balls formed in marine paleomires, with rapid sea-level rise leading to thinner coals, or freshwater coals directly overlain by marine sediments. Conversely, as antecedent topography filled with sediment in the Missourian-Virgilian, producing a broader flatter shelf, similar amounts of glacial-eustatic sea-level rise may have mimicked the effect of increasing the amplitude and rate of sea-level rise.