Environmental Science and Engineering, Oregon Graduate Center, 19600 N.W. Von Neumann Drive, Beaverton, Oregon 97006-1999.
Appl Environ Microbiol. 1989 Jul;55(7):1735-41. doi: 10.1128/aem.55.7.1735-1741.1989.
We calculated the potential H(2) and formate diffusion between microbes and found that at H(2) concentrations commonly found in nature, H(2) could not diffuse rapidly enough to dispersed methanogenic cells to account for the rate of methane synthesis but formate could. Our calculations were based on individual organisms dispersed in the medium, as supported by microscopic observations of butyrate-degrading cocultures. We isolated an axenic culture of Syntrophomonas wolfei and cultivated it on butyrate in syntrophic coculture with Methanobacterium formicicum; during growth the H(2) concentration was 63 nM (10.6 Pa). S. wolfei contained formate dehydrogenase activity (as does M. formicicum), which would allow interspecies formate transfer in that coculture. Thus, interspecies formate transfer may be the predominant mechanism of syntrophy. Our diffusion calculations also indicated that H(2) concentration at the cell surface of H(2)-consuming organisms was low but increased to approximately the bulk-fluid concentration at a distance of about 10 mum from the surface. Thus, routine estimation of kinetic parameters would greatly overestimate the K(m) for H(2) or formate.
我们计算了微生物之间潜在的 H(2) 和甲酸盐扩散,并发现,在自然界中常见的 H(2) 浓度下,H(2) 扩散速度不够快,无法将产甲烷细胞分散开,以解释甲烷合成的速度,但甲酸盐可以。我们的计算基于分散在培养基中的单个生物体,这得到了丁酸降解共培养物的显微镜观察的支持。我们分离了一株专性培养的 S. wolfei,并在与 Methanobacterium formicicum 的共培养物中以丁酸为底物进行培养;在生长过程中,H(2) 浓度为 63 nM(10.6 Pa)。S. wolfei 含有甲酸脱氢酶活性(M. formicicum 也有),这允许在共培养物中进行种间甲酸盐转移。因此,种间甲酸盐转移可能是共营养的主要机制。我们的扩散计算还表明,消耗 H(2) 的生物体细胞表面的 H(2) 浓度较低,但在距离表面约 10 µm 处增加到约与主体流体浓度相同。因此,常规估计动力学参数会大大高估 H(2) 或甲酸盐的 K(m)。