First evidence of this mutase reaction was provided by Robinson and coworkers (Gani et
al. 1985; Reynolds et al. 1988), while studying the synthesis of the antibiotic monensin A in
Streptomyces cinnamonensis A3823.5. The carbon backbone of this polyether antibiotic is
assembled from 5 acetate, 1 butyrate and 7 propionate building blocks, indicating the
importance of propionate metabolism. In the course of valine degradation, isobutyrate is
formed and linked to butyrate metabolism by ICM activity. Then, propionate may be
produced either directly by α-oxidation or succinate is formed by ω-oxidation (Reynolds et
al. 1988). The latter can be transformed to propionate via methylmalonyl-CoA. Hence,
monensin A biosynthesis involves both MCM and ICM activities.
In addition to antibiotic production in Streptomyces spp., ICM activity was found to be
involved in the primary metabolism of several anaerobic bacterial strains and enrichment
cultures. As isobutyrate cannot be directly degraded via β-oxidation isomerization to butyrate
seems to be a possible pathway in anoxic environments, enabling growth on isobutyrate
al. 1996; Tholozan et al. 1988; Wu et al. 1994). Although ICM has not been biochemically
and genetically characterized in these anaerobic cultures, the isomerization reaction was
unambiguously proved by 13C labeling experiments, e. g., in Desulforhabdus amnigena DSM
10338 (Oude Elferink et al. 1996) and in a methanogenic enrichment (Tholozan et al. 1988).
In the latter case, syntrophic bacteria living in cooperation with methanogenic species may be
responsible for isobutyrate isomerization, such as the strict anaerobic glutarate-fermenting
bacterium Pelospora glutarica WoG13 (Matthies & Schink 1992; Matthies et al. 2000) and
the thermophilic, fatty acid-oxidizing Synthrophothermus lipocalidus TGB-C1 (Sekiguchi et
al. 2000). Thus, ICM may play a significant role for isobutyrate turnover in biotopes where it
is formed under anoxic conditions, e. g., in the course of anaerobic valine degradation.
Both mutase enzymes, MCM and ICM, have a rather limited substrate spectrum and
al. 1978; Shinichi et al. 1994). However, considering the elegant way by which
methylmalonate and isobutyrate are converted into their corresponding straight-chain
84 Thore Rohwerder and Roland H. Müller
carbonic acids, one might speculate about similar 1,2-rearrangements to be involved in other
pathways. Indeed, this kind of reaction would be suitable for degrading hydrocarbons with
However, until recently other CoA-carbonyl mutases than MCM and ICM have not been
identified and often mutase reactions were not considered when bacterial degradation
pathways were investigated. This conclusion might turn out to be wrong as new findings let
us claim that ICM-like enzymes could perfectly well function in many degradation pathways.
For substantiating this hypothesis, we will present in the following three examples for
possible employment of thus far unknown bacterial CoA-carbonyl mutases; the conversion of
(a) 2-hydroxyisobutyrate, (b) pivalate and (c) carbonic acid intermediates of anaerobic alkane
(a) Isomerization of 2-Hydroxyisobutyrate
The tertiary carbon atom-containing 2-hydroxyisobutyrate (2-HIBA) is rarely found in
nature and only few applications of this branched carbonic acid are known, such as the use of
its complexing properties for analyzing rare earth elements (Raut et al. 2002). In addition, it
is an intermediate and by-product of industrial processes, such as the synthesis of
methacrylate in the classical acetone cyanohydrin process since the mid-1930s (Chisholm
2000). As 2-HIBA seems not to be a widespread contaminant the investigation of its
degradation by bacteria or other microorganisms has not attracted much attention. This
situation changed in the last years since 2-HIBA has been identified as an intermediate in the
degradation pathway of the fuel oxygenate methyl tert-butyl ether (MTBE) (Fayolle et al.
2001). Due to its massive use since the 1990s, the current world production amounts to about
20 Mt/a, MTBE has become a common groundwater contaminant and thus severely threatens
drinking water resources by its suspected carcinogenicity, as well as by its unpleasant odor
and taste (EPA 1997; Moran et al. 2005; Schmidt et al. 2002). Consequently, a main concern
is the environmental fate of the fuel oxygenate and its degradation intermediates. As in situ
biodegradation is the only sustainable sink of MTBE in aquifers extensive research work is
currently undertaken for elucidating its microbial degradation pathway. Aerobically, MTBE
is degraded via tert-butyl alcohol (TBA) and 2-hydroxy-2-methylpropanol to 2-HIBA
(Fayolle et al. 2001; Lopes Ferreira et al. 2006; Steffan et al. 1997) (Figure 1). In the first
investigations on bacterial MTBE degradation, further steps were not identified but only
three possible routes were proposed starting with hydroxylation, dehydration or
decarboxylation of 2-HIBA (Steffan et al. 1997). However, these mechanisms have not been
proved until now. On the contrary, evidence for a fourth pathway involving the activity of a
CoA-carbonyl mutase has been furnished (Rohwerder et al. 2006). The novel ICM-like
mutase catalyzes the conversion of 2-HIBA into 3-hydroxybutyrate (Figure 1) and, thus,
connects the MTBE-specific degradation steps with the common metabolism.
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