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3<br />

Role of Microorganisms<br />

in Wear Down of Rocks and Minerals<br />

Anna A. Gorbushina 1 ,W.E.Krumbein 1<br />

1<br />

Rock Weathering or Rock Wear Down?<br />

Rock weathering is an awkward term. Near and below the Earth’s surface,<br />

physical and chemical processes operate under direct or indirect control of<br />

living matter. Weathering, however, strongly relates to physical and chemical<br />

changes produced by the weather and its long-term average, the climate.<br />

Meteorological connotation of the term ignores the importance of biological<br />

interactions in the process of rock and material alteration. Terms like<br />

biotransfer, biocorrosion, biodeterioration, bioabrasion, bioerosion, biodenudation,<br />

or biokarst closely connect the physical and chemical processes<br />

related to mineral and rock destruction with biological phenomena and<br />

processes, as indicated by the prefix. Therefore, in this chapter, it was deliberately<br />

decided to avoid the term rock weathering as much as possible.<br />

Krumbein and Dyer (1985) suggested dividing the processes of rock and<br />

mineral destruction into physical and chemical transfer reactions. Physical<br />

transfer includes biological and abiological processes through which<br />

particles are mechanically disconnected from a bulk material and transferred<br />

into the hydrosphere, atmosphere or pedosphere as particulates,<br />

colloids and aerosols. Chemical transfer embraces all biologically or abiologically<br />

driven reactions through which ions are removed from rock<br />

and mineral and transformed into gases, solutes, colloids. It can also yield<br />

solid particles after precipitation of intermediate gaseous or liquid compounds.<br />

Krumbein (1969, 1988, 1993, 1996, 1998) and Krumbein and Dyer (1985)<br />

described the physical and chemical biotransfer actions in an embracing<br />

definition, which introduces “wear down” as a generalized term. In a geological<br />

context, wear down was perhaps used for the first time in 1885<br />

concerning sponge spicules transformed into powder. The original use of<br />

this term, however, stems from 1729. It described the weight loss of silver<br />

coins due to use and exposure to environmental conditions.<br />

1 AG Geomikrobiologie, ICBM, Carl von Ossietzky Universität, Postfach 2503, 26111 Oldenburg,<br />

Germany, e-mail: a.gorbushina@uni-oldenburg.de, Tel: +49-441-7983393, Fax: +49-<br />

441-7983384<br />

Soil Biology, Volume 3<br />

Microorganisms in Soils: Roles in Genesis and Functions<br />

(ed. by F. Buscot and A. Varma)<br />

c○ Springer-Verlag Berlin Heidelberg 2005

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