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Upwelling events may cause cyanobacteria blooms in the Baltic Sea

机译:上升事件可能导致波罗的海的蓝细菌绽放

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Cyanobacteria blooms in the Baltic Sea appear after upwelling events, which transport phosphate-rich intermediate water to the surface. The growth potential of diazotrophic cyanobacteria in upwelled water was studied in a mesocosm (tank) experiment in summer 2007. An Anabaena bloom was only induced in the tanks filled with upwelled surface water but not in those filled with surface water from outside the upwelling cell and with intermediate water. The low initial cyanobacteria biomass in the intermediate water could not grow to bloom concentrations within three weeks. It is concluded that mixing of upwelled water with surrounding surface water forms a precondition for a cyanobacteria bloom. An additional mesocosm experiment conducted in 2009 revealed that mixing of intermediate water with surface water had the same stimulating effect on nitrogen fixation and cyanobacteria growth as artificial phosphate input. Phosphate input stimulates the growth of Nodularia and Anabaena more than that of Aphanizomenon. We suggest that the upwelled phosphate-rich intermediate water has to be mixed with the surface water containing physiologically "young" cyanobacteria biomass of at least 20mg/m~3 as an inoculum in order to initiate a cyanobacteria bloom.
机译:上升事件之后,波罗的海的蓝细菌水华出现,这将富含磷酸盐的中间水运到地表。 2007年夏季,通过中膜(水箱)实验研究了重氮营养蓝细菌在上升流中的生长潜力。仅在充满上升流地表水的水箱中诱导了鱼腥藻水华,而在上升流水箱外部未填充地表水的水箱中并没有引起鱼腥藻开花。用中间水。中间水中的初始蓝细菌生物量较低,无法在三周内生长成水华浓度。结论是,上升流水与周围地表水的混合形成了蓝藻水华的前提。 2009年进行的另一项介观试验表明,将中间水与地表水混合具有与人工磷酸盐输入相同的对固氮和蓝细菌生长的刺激作用。磷的输入比Aphanizomenon更加刺激结核和鱼腥藻的生长。我们建议上升流的富含磷酸盐的中间水必须与含有至少20mg / m〜3的生理上“年轻的”蓝细菌生物量的地表水混合作为接种物,以启动蓝细菌开花。

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