26 Soils, Geomorphology, and Quaternary Geology (Posters)
Friday, 1 April 2016
8:00 AM - 5:30 PM
Exhibit Hall
PRELIMINARY MINERALOGY AND GEOMICROBIOLOGY OF CHEROKEE CAVERNS, A UNIQUE DOLOMITE CAVE IN EAST TENNESSEE
Paper number: 26-1
Program: Technical Sessions
Time: 8:00 AM – 5:30 PM
Authors
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Garry D. PennycuffPellissippi State Community College, Knoxville, TN
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Paul A. GiestingUniversity of Tennessee, Knoxville, TN
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Minoo D.F. AskariPellissippi State Community College, Knoxville, TN
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Sven HolbikFlorida International University, Miami, FL
Abstract
In some places in the cave, anthodites extend from crusty orange bacteria-rich clay attached to grey dolomite bedrock. SEM/EDS images and spectral analyses indicate the side of the crusty orange clay adjacent to the dolomite bedrock is populated with numerous ten-micron spheres of unknown origin, and with crystals that look degraded. Holes in one crystal are one micron in diameter, the size of some bacteria. The crusty clay side away from the dolomite bedrock, from which anthodites protrude, lacks these features.
Elsewhere, ephemeral ceiling fibers similar to snottites have gypsum attached to carbon-rich fibers while sprays of carbonates are attached to fibers associated with stalagmites. One remarkable SEM/EDS image shows microbes attached to a 15-micron iron-rich sphere, possibly oxidizing the iron to gain energy in the dark confines of the cave. In Cherokee Caverns, minerals and bacteria are intimately related.
Geological Society of America Abstracts with Programs. Vol. 48, No. 3
doi: 10.1130/abs/2016SE-273127
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