Chidthaisong A, Rosenstock B, Conrad R
Max-Planck-Institut fur Terrestrische Microbiologie, D-35043 Marburg/Lahn, Germany.
Appl Environ Microbiol. 1999 Jun;65(6):2350-5. doi: 10.1128/AEM.65.6.2350-2355.1999.
Degradation of glucose has been implicated in acetate production in rice field soil, but the abundance of glucose, the temporal change of glucose turnover, and the relationship between glucose and acetate catabolism are not well understood. We therefore measured the pool sizes of glucose and acetate in rice field soil and investigated the turnover of [U-14C]glucose and [2-14C]acetate. Acetate accumulated up to about 2 mM during days 5 to 10 after flooding of the soil. Subsequently, methanogenesis started and the acetate concentration decreased to about 100 to 200 &mgr;M. Glucose always made up >50% of the total monosaccharides detected. Glucose concentrations decreased during the first 10 days from 90 &mgr;M initially to about 3 &mgr;M after 40 days of incubation. With the exception at day 0 when glucose consumption was slow, the glucose turnover time was in the range of minutes, while the acetate turnover time was in the range of hours. Anaerobic degradation of [U-14C]glucose released [14C]acetate and 14CO2 as the main products, with [14C]acetate being released faster than 14CO2. The products of [2-14C]acetate metabolism, on the other hand, were 14CO2 during the reduction phase of soil incubation (days 0 to 15) and 14CH4 during the methanogenic phase (after day 15). Except during the accumulation period of acetate (days 5 to 10), approximately 50 to 80% of the acetate consumed was produced from glucose catabolism. However, during the accumulation period of acetate, the rate of acetate production from glucose greatly exceeded that of acetate consumption. Under steady-state conditions, up to 67% of the CH4 was produced from acetate, of which up to 56% was produced from glucose degradation.
葡萄糖的降解与稻田土壤中乙酸盐的产生有关,但葡萄糖的丰度、葡萄糖周转的时间变化以及葡萄糖与乙酸盐分解代谢之间的关系尚不清楚。因此,我们测量了稻田土壤中葡萄糖和乙酸盐的库大小,并研究了[U-14C]葡萄糖和[2-14C]乙酸盐的周转情况。在土壤淹水后的第5至10天,乙酸盐积累至约2 mM。随后,甲烷生成开始,乙酸盐浓度降至约100至200 μM。葡萄糖始终占检测到的总单糖的>50%。葡萄糖浓度在最初的10天内从90 μM降至培养40天后的约3 μM。除了第0天葡萄糖消耗缓慢外,葡萄糖周转时间在几分钟范围内,而乙酸盐周转时间在几小时范围内。[U-14C]葡萄糖的厌氧降解以[14C]乙酸盐和14CO2为主要产物,[14C]乙酸盐的释放速度比14CO2快。另一方面,[2-14C]乙酸盐代谢的产物在土壤培养的还原阶段(第0至15天)为14CO2,在产甲烷阶段(第15天后)为14CH4。除了乙酸盐积累期(第5至10天),消耗的乙酸盐中约50%至80%由葡萄糖分解代谢产生。然而,在乙酸盐积累期,葡萄糖产生乙酸盐的速率大大超过乙酸盐消耗的速率。在稳态条件下,高达67%的CH4由乙酸盐产生,其中高达56%由葡萄糖降解产生。