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首页> 外文期刊>Applied and Environmental Microbiology >Bacterioplankton in Antarctic Ocean Waters During Late Austral Winter: Abundance, Frequency of Dividing Cells, and Estimates of Production
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Bacterioplankton in Antarctic Ocean Waters During Late Austral Winter: Abundance, Frequency of Dividing Cells, and Estimates of Production

机译:南极冬季晚期南极海洋水域中的浮游细菌:丰度,分裂细胞的频率和产量估算

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Bacterioplankton productivity in Antarctic waters of the eastern South Pacific Ocean and Drake Passage was estimated by direct counts and frequency of dividing cells (FDC). Total bacterioplankton assemblages were enumerated by epifluorescent microscopy. The experimentally determined relationship between in situ FDC and the potential instantaneous growth rate constant (μ) is best described by the regression equation ln μ = 0.081 FDC ? 3.73. In the eastern South Pacific Ocean, bacterioplankton abundance (2 × 105 to 3.5 × 105 cells per ml) and FDC (11%) were highest at the Polar Front (Antarctic Convergence). North of the Subantarctic Front, abundance and FDC were between 1 × 105 to 2 × 105 cells per ml and 3 to 5%, respectively, and were vertically homogeneous to a depth of 600 m. In Drake Passage, abundance (10 × 105 cells per ml) and FDC (16%) were highest in waters south of the Polar Front and near the sea ice. Subantarctic waters in Drake Passage contained 4 × 105 cells per ml with 4 to 5% FDC. Instantaneous growth rate constants ranged between 0.029 and 0.088 h?1. Using estimates of potential μ and measured standing stocks, we estimated productivity to range from 0.62 μg of C per liter · day in the eastern South Pacific Ocean to 17.1 μg of C per liter · day in the Drake Passage near the sea ice.
机译:通过直接计数和分裂细胞的频率(FDC)估算南太平洋东部南极水域和德雷克海峡中的浮游细菌生产力。通过落射荧光显微镜对总的浮游细菌集合进行计数。通过回归方程lnμ= 0.081 FDC?最好地描述了实验确定的原位FDC与潜在瞬时生长速率常数(μ)之间的关系。 3.73。在南太平洋东部,极地锋(南极收敛)的浮游细菌丰度(每毫升2×105至3.5×105个细胞)和FDC(11%)最高。在亚南极锋的北部,丰度和FDC分别为每毫升1×105至2×105个细胞和3至5%,并且垂直均匀,深度为600 m。在德雷克海峡,丰度(每毫升10×105个细胞)和FDC(16%)在极地锋以南和海冰附近的水中最高。德雷克海峡的亚极南极水每毫升含有4×105个细胞,FDC为4%至5%。瞬时生长速率常数在0.029至0.088 h?1之间。使用潜在μ的估计值和测得的固定存量,我们估计生产率范围从南太平洋东部的0.62μg/升·天到海冰附近的Drake通道的17.1μg/升·天。

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