Abstract
Since the beginning of life on Earth, microorganisms have had the remarkable ability to evolve the necessary molecular machinery to cope with and even benefit from high concentrations of toxic metals in the environment. Many metals (in trace amount) play an integral role in biological processes; however, many of the same metals, as well as those not required in biological systems, can be quite harmful.This is most commonly a consequence of the metal concentration; however, speciation and physicochemical form of the element are added factors. Some metals that microorganisms depend on in low concentrations include arsenic, calcium, cobalt, chromium, copper, iron, potassium, magnesium, manganese, sodium, nickel, and zinc; whereas, aluminum, cadmium, gold, lead, mercury, and silver are not known to be part of cellular structures or processes (Bruins et al. 2000; Stolz et al. 2002). The essential metals have been found to be crucial components in redox processes, gene expression, biomolecule activity, cellular osmotic balance, and protein and bacterial cell wall structures (Hughes and Poole 1989; Ji and Silver 1995; Poole and Gadd 1989). Yet, if any of these metals exceed certain concentrations, microorganisms must use resistance mechanisms to survive the ‘metal stress’. Because many environments inhabited by microorganisms have continuously contained poisonous elements, resistance mechanisms most likely developed shortly after the evolution of prokaryotic life.
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Acknowledgements
The authors express their gratitude to the National Science Foundation, the Department of Energy, and the National Aeronautics and Space Administration for funding various aspects of our research on the ecophysiology of arsenic.
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Ledbetter, R.N., Magnuson, T.S. (2010). The Geomicrobiology of Arsenic. In: Barton, L., Mandl, M., Loy, A. (eds) Geomicrobiology: Molecular and Environmental Perspective. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-9204-5_7
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