Janke D, Fritsche W
J Basic Microbiol. 1985;25(9):603-19. doi: 10.1002/jobm.3620250910.
Microbial cometabolism, i.e. "transformation of a non-growth substrate in the obligate presence of a growth substrate or another transformable compound" (Dalton and Stirling 1982) is a whole-cell phenomenon physiologically based on coupling of different catabolic pathways at the cellular level. It is frequently observed in transformation of xenobiotic non-growth substrates by individual microbial species. Transformation processes of this type are usually mediated by appropriate non-specific enzymes of the peripheric cellular metabolism able to modify a variety of substances other than their natural substrates. The precise mechanisms of coupling between metabolism of xenobiotic non-growth substrates and of particular additional carbon substrates may be different depending on the substrates and the microbial species involved. However, experimental data indicate that the primary function of the respective additional carbon substrates is to supply either energy, cofactors or metabolites for the different cellular events involved in the transformation process (e.g. uptake of the xenobiotic non-growth substrate, functioning of appropriate degradative enzymes of the peripheric cellular metabolism). Cometabolism of xenobiotics involves nothing special or novel from the standpoint of biochemistry. On the contrary, there are numerous examples where the turnover of particular natural compounds by certain aerobic or anaerobic microorganisms is essentially based on coupling of different catabolic pathways at the cellular level by transfer of hydrogen (i.e. reducing power) and/or energy between two or more enzymatic reactions. Synthetic chemicals which resist total degradation by individual microbial species may undergo mineralization due to complementary catabolic sequences mediated by certain multispecies microbial associations with cometabolic transformations being the initial steps. Although taking place in certain natural habitats (e.g. rhizospheres, sewage), microbial cometabolism of xenobiotics in natural ecosystems occurs with slow rates since the respective cometabolizing populations are generally small and will not increase in number or biomass in response to the introduced chemicals. However, under conditions of axenic microbial cultures, high concentrations of biomass, and appropriate substrate mixtures cometabolism of synthetic chemicals may be a useful technique of considerable practical importance to accumulate biochemical products at high yields. In addition, cometabolic capabilities of wild-type microorganisms may serve as a tool for the construction of microbial strains with a new degradative potential for recalcitrant xenobiotic compounds.
微生物共代谢,即“在生长底物或另一种可转化化合物必然存在的情况下,非生长底物的转化”(道尔顿和斯特林,1982年),是一种全细胞现象,其生理基础是在细胞水平上不同分解代谢途径的偶联。在单个微生物物种对异源非生长底物的转化中经常观察到这种现象。这类转化过程通常由外周细胞代谢中适当的非特异性酶介导,这些酶能够修饰除其天然底物之外的多种物质。异源非生长底物代谢与特定附加碳底物代谢之间偶联的精确机制可能因所涉及的底物和微生物物种而异。然而,实验数据表明,相应附加碳底物的主要功能是为转化过程中涉及的不同细胞事件(例如异源非生长底物的摄取、外周细胞代谢中适当降解酶的功能)提供能量、辅因子或代谢物。从生物化学的角度来看,异源物质的共代谢并没有什么特别或新颖之处。相反,有许多例子表明,某些需氧或厌氧微生物对特定天然化合物的周转基本上是基于通过两个或多个酶促反应之间的氢(即还原力)和/或能量转移,在细胞水平上不同分解代谢途径的偶联。那些能抵抗单个微生物物种完全降解的合成化学物质,可能由于某些多物种微生物联合体介导的互补分解代谢序列而矿化,共代谢转化是初始步骤。尽管微生物对异源物质的共代谢发生在某些自然生境(如根际、污水)中,但在自然生态系统中其发生速率较慢,因为相应的共代谢种群通常较小,并且不会因引入的化学物质而数量或生物量增加。然而,在无菌微生物培养、高生物量浓度和适当底物混合物的条件下,合成化学物质的共代谢可能是一种具有相当实际重要性的有用技术,可用于高产积累生化产物。此外,野生型微生物的共代谢能力可作为构建对难降解异源化合物具有新降解潜力的微生物菌株的工具。