Research Details and Recent Findings
by Penny Boston, Associate
Professor of Cave and Karst Science
Major questions that my work addresses:
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How much impact do subsurface microorganisms have on the Earth’s lithosphere
on short timescales, and over geological time?
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How dependent are subsurface microbe/mineral communities on surface inputs
of nutrients, weathering effects, and hydrology?
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How independent are subsurface microbial communities from surface microorganisms
and how does this vary between separate subsurface systems?
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What are the original sources of cave microflora: Organisms in groundwater?
Air transport of surface organisms? Indigenous aquifer inhabitants? Or
cells entombed in the parent rock during the original deposition of sediments?
Significant recent findings include
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discovery of unique Mn minerals in secondary cave deposits and laboratory
demonstration of microbial precipitation of these minerals
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microbial involvement in concentration of Mn above background by 4 orders
of magnitude & concentration of Fe above background by 3 orders of
magnitude in secondary mineral deposits
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demonstration of high bacterial metabolic activity levels (55-80%) in parent
rock, leached corroded punk rock, and detrital deposits
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distinctive d 34 S signatures produced by microbial mats living deep within
the rock piping of hydrogen sulfide emitting springs in a volcano-influenced
tropical cave
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in situ bacterial precipitation of gypsum and sulfur within unique exopolysaccharide/bacterial
strings in a hydrogen sulfide cave
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development of new non-consumptive exoenzyme assays for microorganism detection
on rocks, buildings/monuments, unconsolidated materials, and waters.