Fukuda R, Ogawa H, Nagata T, Koike I
Ocean Research Institute, University of Tokyo, Nakano, Tokyo 164-8639, Japan.
Appl Environ Microbiol. 1998 Sep;64(9):3352-8. doi: 10.1128/AEM.64.9.3352-3358.1998.
In order to better estimate bacterial biomass in marine environments, we developed a novel technique for direct measurement of carbon and nitrogen contents of natural bacterial assemblages. Bacterial cells were separated from phytoplankton and detritus with glass fiber and membrane filters (pore size, 0.8 &mgr;m) and then concentrated by tangential flow filtration. The concentrate was used for the determination of amounts of organic carbon and nitrogen by a high-temperature catalytic oxidation method, and after it was stained with 4',6-diamidino-2-phenylindole, cell abundance was determined by epifluorescence microscopy. We found that the average contents of carbon and nitrogen for oceanic bacterial assemblages were 12.4 +/- 6.3 and 2.1 +/- 1.1 fg cell-1 (mean +/- standard deviation; n = 6), respectively. Corresponding values for coastal bacterial assemblages were 30.2 +/- 12.3 fg of C cell-1 and 5.8 +/- 1.5 fg of N cell-1 (n = 5), significantly higher than those for oceanic bacteria (two-tailed Student's t test; P < 0.03). There was no significant difference (P > 0.2) in the bacterial C:N ratio (atom atom-1) between oceanic (6.8 +/- 1.2) and coastal (5.9 +/- 1.1) assemblages. Our estimates support the previous proposition that bacteria contribute substantially to total biomass in marine environments, but they also suggest that the use of a single conversion factor for diverse marine environments can lead to large errors in assessing the role of bacteria in food webs and biogeochemical cycles. The use of a factor, 20 fg of C cell-1, which has been widely adopted in recent studies may result in the overestimation (by as much as 330%) of bacterial biomass in open oceans and in the underestimation (by as much as 40%) of bacterial biomass in coastal environments.
为了更好地估算海洋环境中的细菌生物量,我们开发了一种直接测量天然细菌群落碳和氮含量的新技术。使用玻璃纤维和膜过滤器(孔径0.8μm)将细菌细胞与浮游植物和碎屑分离,然后通过切向流过滤进行浓缩。浓缩物用于通过高温催化氧化法测定有机碳和氮的含量,在用4',6-二脒基-2-苯基吲哚染色后,通过落射荧光显微镜测定细胞丰度。我们发现,海洋细菌群落的碳和氮平均含量分别为12.4±6.3和2.1±1.1 fg cell-1(平均值±标准差;n = 6)。沿海细菌群落的相应值为30.2±12.3 fg C cell-1和5.8±1.5 fg N cell-1(n = 5),显著高于海洋细菌(双尾学生t检验;P < 0.03)。海洋(6.8±1.2)和沿海(5.9±1.1)群落之间的细菌C:N比(原子比)没有显著差异(P > 0.2)。我们的估算结果支持了之前的观点,即细菌对海洋环境中的总生物量有很大贡献,但也表明,在不同的海洋环境中使用单一的转换因子可能会在评估细菌在食物网和生物地球化学循环中的作用时导致较大误差。最近的研究中广泛采用的20 fg C cell-1这个因子,可能会导致公海中细菌生物量被高估(高达330%),而在沿海环境中细菌生物量被低估(高达40%)。