Griffiths R P, Hayasaka S S, McNamara T M, Morita R Y
Can J Microbiol. 1978 Oct;24(10):1217-26. doi: 10.1139/m78-196.
A total of 91 water, 8 ice, and 50 sediment samples taken from the southwestern Beaufort Sea were analyzed for relative microbial activity, bacterial cell concentrations, and percentage of respiration (mineralization). These samples were taken during three field-study periods (August to September 1975; April 1976; and August 1976). Both the relative microbial activity and the cell concentrations in water and sediment samples were lower during the April (winter) sampling period than in the August-September (summer) studies. The percentage of respiration of labeled glutamic acid was higher in the winter water samples than in the summer samples. The water samples showed higher percentage of respiration values than did sediment samples. The average maximimum potential rate of glutamic acid uptake was as high or higher than those observed in studies made in more temperate waters. Samples of melted sea ice showed levels of relative microbial activity that were about the same as that found in the associated seawater. When 1:1 mixtures of melted ice and seawater were analyzed for altered microbial activity, little effect could be detected.
对从波弗特海西南部采集的91份水样、8份冰样和50份沉积物样本进行了分析,以测定其相对微生物活性、细菌细胞浓度和呼吸(矿化)百分比。这些样本是在三个实地研究期间采集的(1975年8月至9月;1976年4月;以及1976年8月)。在4月(冬季)采样期间,水样和沉积物样本中的相对微生物活性以及细胞浓度均低于8月至9月(夏季)研究期间。冬季水样中标记谷氨酸的呼吸百分比高于夏季样本。水样的呼吸百分比值高于沉积物样本。谷氨酸摄取的平均最大潜在速率与在更温带水域进行的研究中观察到的速率一样高或更高。融化海冰的样本显示出的相对微生物活性水平与相关海水中的水平大致相同。当对融化冰和海水的1:1混合物进行分析以检测微生物活性的变化时,几乎检测不到影响。