Ward D M
Appl Environ Microbiol. 1978 Jun;35(6):1019-26. doi: 10.1128/aem.35.6.1019-1026.1978.
Algal-bacterial mats which grow in the effluent channels of alkaline hot springs provided an environment suitable for studying natural thermophilic methane producing bacteria. Methane was rapidly produced in cores taken from the meat and appeared to be an end product of decomposition of the algal-bacterial organic matter. Formaldehyde prevented production of methane. Initial methanogenic rate was lower and methanogenesis became exponential when samples were permitted to cool before laboratory incubation. Methanogenesis occurred and methanogenic bacteria were present over a range of 68 to 30 degrees C, with optimum methanogenesis near 45 degrees C. The temperature distribution of methanogenesis in the mat is discussed relative to published results on standing crop, primary production, and decomposition in the thermal gradient. The depth distribution of methanogenesis was similar to that of freshwater sediments, with a zone of intense methanogenesis near the mat surface. Methanogenesis in deeper mat layers was very low or undetectable despite large numbers of viable methanogenic bacteria and could not be stimulated by addition of anoxic source water, sulfide, or a macronutrient solution.
生长在碱性温泉排放渠道中的藻菌席提供了一个适合研究天然嗜热产甲烷细菌的环境。从藻菌席中取出的岩芯中迅速产生了甲烷,甲烷似乎是藻菌有机物质分解的最终产物。甲醛抑制了甲烷的产生。当样品在实验室培养前冷却时,初始产甲烷速率较低,产甲烷过程呈指数增长。在68至30摄氏度的范围内发生了产甲烷作用,并且存在产甲烷细菌,产甲烷的最适温度接近45摄氏度。相对于已发表的关于生物量、初级生产和热梯度中分解的结果,讨论了藻菌席中产甲烷作用的温度分布。产甲烷作用的深度分布与淡水沉积物相似,在藻菌席表面附近有一个强烈产甲烷的区域。尽管存在大量活的产甲烷细菌,但藻菌席较深层的产甲烷作用非常低或无法检测到,并且添加缺氧源水、硫化物或大量营养素溶液也无法刺激产甲烷作用。