--> ABSTRACT: Carbonate Petrography and Geochemistry of Middle Pennsylvanian Coal Balls (Herrin Coal): Evidence Regarding Coal-Ball Formation And Fossil Plant Preservation, by Siewers, Fredrick D., Tom L. Phillips; #90026 (2004)
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Siewers, Fredrick D.1, Tom L. Phillips2 
(1) Western Kentucky University, Bowling Green, KY 
(2) University of Illinois, Urbana, IL

ABSTRACT: Carbonate Petrography and Geochemistry of Middle Pennsylvanian Coal Balls (Herrin Coal): Evidence Regarding Coal-Ball Formation And Fossil Plant Preservation

Coal-ball concretions provide important insights into the plant composition and ecological structure of Pennsylvanian coal swamps; however, the processes leading to coal-ball formation and fossil plant preservation are still poorly understood. An investigation of coal balls from the Herrin Coal (Middle Pennsylvanian), Illinois Basin indicates initial coal-ball formation occurred by the precipitation of two distinct carbonate phases: a composite crystalline Previous HitphaseNext Hit of fibrous Mg-enriched carbonate and a monocrystalline Previous HitphaseNext Hit of equant, low magnesian calcite. The composite crystalline Previous HitphaseNext Hit occurs primarily as radiating fans and spherulites of acicular fibers, many of which pass through plant remains without significant disruption of anatomical structures. Individual fibers have a distinctive trigonal prism morphology and a microbulk composition of 9 to 14 mol. % MgCO3. The monocrystalline Previous HitphaseNext Hit fills intercrystalline pore spaces, voids within some cell lumens and some of the extra-cellular pore space. This Previous HitphaseNext Hit occurs as a primary precipitate and as void-fill replacements after precursor fibrous carbonate. 
The composite crystalline Previous HitphaseNext Hit was typically first to precipitate and was most involved in the initial permineralization of the peat. Although now composed of a cryptocrystalline mixture of low magnesium calcite and dolomite, the composite crystalline Previous HitphaseTop originally precipitated as high magnesian calcite. Precipitation was likely triggered by CO2 degassing, flowing porewaters and an abundant supply of chemical reactants. The composite crystals grew by the addition of submicron crystallites along principal growth axes, a growth mechanism that enhanced the preservation of delicate plant structures.

 

AAPG Search and Discovery Article #90026©2004 AAPG Annual Meeting, Dallas, Texas, April 18-21, 2004.