Mercury in water and biomass of microbial communities in hot springs of Yellowstone National Park, USA
Susan A. King, Sabrina Behnke, Kim Slack, David P. Krabbenhoft, D. Kirk Nordstrom, Mark D. Burr, Robert G. Striegl
Applied Geochemistry, 2006
Abstract
Ultra-clean sampling methods and approaches typically used in pristine environments were applied to quantify concentrations
of Hg species in water and microbial biomass from hot springs of Yellowstone National Park, features that are
geologically enriched with Hg. Microbial populations of chemically-diverse hot springs were also characterized using modern
methods in molecular biology as the initial step toward ongoing work linking Hg speciation with microbial processes.
Molecular methods (amplification of environmental DNA using 16S rDNA primers, cloning, denatured gradient gel electrophoresis
(DGGE) screening of clone libraries, and sequencing of representative clones) were used to examine the dominant
members of microbial communities in hot springs. Total Hg (THg), monomethylated Hg (MeHg), pH, temperature,
and other parameters influential to Hg speciation and microbial ecology are reported for hot springs water and associated
microbial mats.
Several hot springs indicate the presence of MeHg in microbial mats with concentrations ranging from 1 to 10 ng g-1 (dry
weight). Concentrations of THg in mats ranged from 4.9 to 120,000 ng g-1 (dry weight). Combined data from surveys of
geothermal water, lakes, and streams show that aqueous THg concentrations range from l to 600 ng L-1. Species and concentrations
of THg in mats and water vary significantly between hot springs, as do the microorganisms found at each site.
NOTE: the article text supplied here is for educational purposes only.
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