Pradeep Ram A S, Nair Shanta, Chandramohan D
Centre for Ecological Research, Kyoto University, 2-509-3 Hirano, Otsu, Shiga, Japan.
Microb Ecol. 2007 May;53(4):591-9. doi: 10.1007/s00248-006-9124-y. Epub 2007 Mar 14.
Bacterial growth efficiency (BGE) is a key factor in understanding bacterial influence on carbon flow in aquatic ecosystems. We report intra-annual variability in BGE, and bacteria-mediated carbon flow in the tropical Mandovi and Zuari estuaries (southwest India) and the adjoining coastal waters (Arabian Sea). BGE ranged from 3% to 61% and showed clear temporal variability with significantly (ANOVA, p < 0.01) higher values in the estuaries (mean, 28 +/- 14%) than coastal waters (mean, 12 +/- 6%). The greater variability of BGE in the estuaries than coastal waters suggest some systematic response to nutrient composition and the variability of dissolved organic matter pools, as BGE was governed by bacterial secondary production (BP). Monsoonal rains and its accompanied changes brought significant variability in BGE and bacterial productivity/primary productivity (BP/PP) ratio when compared to nonmonsoon seasons in the estuaries and coastal waters. High BP/PP ratio (>1) together with high carbon flux through bacteria (>100% of primary productivity) in the estuarine and coastal waters suggests that bacterioplankton consumed dissolved organic carbon in excess of the amount produced in situ by phytoplankton of this region, which led to the mismatch between primary production of carbon and amount of carbon consumed by bacteria. Despite the two systems being subsidized by allochthonous inputs, the low BGE in the coastal waters may be attributable to the nature and time interval in the supply of allochthonous carbon.
细菌生长效率(BGE)是理解细菌对水生生态系统碳流影响的关键因素。我们报告了印度西南部热带曼多维河和祖阿里河河口及其毗邻沿海水域(阿拉伯海)BGE的年内变化以及细菌介导的碳流情况。BGE范围为3%至61%,呈现出明显的时间变化,河口地区(平均值为28±14%)的BGE值显著高于沿海水域(平均值为12±6%)(方差分析,p<0.01)。河口地区BGE的变化大于沿海水域,这表明其对营养成分和溶解有机物库的变化存在一些系统性响应,因为BGE受细菌次级生产(BP)的控制。与河口和沿海水域非季风季节相比,季风降雨及其伴随的变化使BGE和细菌生产力/初级生产力(BP/PP)比值产生了显著变化。河口和沿海水域较高的BP/PP比值(>1)以及通过细菌的高碳通量(超过初级生产力的100%)表明,浮游细菌消耗的溶解有机碳超过了该区域浮游植物原位产生的量,并导致了碳的初级生产与细菌消耗的碳量之间的不匹配。尽管这两个系统都受到陆源输入的补贴,但沿海水域较低的BGE可能归因于陆源碳供应的性质和时间间隔。