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Temporal changes in effects of ambient UV radiation on natural communities of Antarctic marine protists

机译:环境紫外线辐射对南极海洋生物的自然群落影响的时间变化

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ABSTRACT: The effects of ambient solar UV radiation (280 to 400 nm) were determined using 3 natural marine protist communities incubated in 650 l tanks (minicosms) for 13  to 14 d over the summer of 2002–2003 at Davis Station, Antarctica. Minicosms were exposed to ambient light that was variously attenuated to give treatments of photosynthetically active radiation (PAR, ≥385 nm wavelength), PAR + UV-A radiation (315 to 385 nm), and PAR + UV-A + 4 different treatments of UV-B radiation (280 to 315 nm) that simulated a range of equivalent depths (ED) in the water column from 4.43 to 7.15 m. Results showed a seasonal progression in the response of microbial communities to UV radiation exposure. The first experiment in November showed that the microbial community was significantly inhibited in the PAR + UV-A-exposed treatment but this inhibition declined with increasing addition of UV-B radiation. The second experiment in December showed that UV-A or UV-B radiation had few significant effects. Like in Expt 1, some taxa were inhibited by PAR + UV-A or promoted by UV-B, but most were inhibited at the highest UV-B irradiances (≤4.43 m ED). The last experiment in January showed UV-B induced inhibition of all but one of the dominant taxa. The seasonal transition in UV wavelengths responsible for inhibition of protists may be due to ozone reduction, the light history of protists, and/or changes in species composition. The increasing UV-B-induced inhibition we observed over the summer corresponded to a decline in ozone concentrations over Davis. This recurrent decline in ozone over Antarctica between January and April coincides with blooms of diatoms that appear to have low UV-B tolerance but are responsible for ~47% of annual primary production in Antarctic waters.
机译:摘要:2002年至2003年夏天,在南极州戴维斯站的3个自然海洋生物社区中,在650 l罐(微型)中孵化了13到14 d,确定了周围太阳紫外线辐射(280至400 nm)的影响。将缩影暴露于各种衰减的环境光下,以进行光合有效辐射(PAR,≥385nm波长),PAR + UV-A辐射(315至385 nm)和PAR + UV-A + 4种不同处理UV-B辐射(280至315 nm)模拟了水柱中4.43至7.15 m的等效深度(ED)范围。结果表明,微生物群落对紫外线辐射的响应呈季节性变化。 11月的第一个实验表明,在暴露于PAR + UV-A的处理中,微生物群落受到显着抑制,但是随着添加的UV-B辐射的增加,这种抑制作用减弱。十二月的第二个实验表明,UV-A或UV-B辐射几乎没有显着影响。像在Expt 1中一样,一些类群被PAR + UV-A抑制或被UV-B促进,但是大多数在最高UV-B辐照度(≤4.43m ED)下受到抑制。一月份的最后一个实验表明,UV-B可以抑制除一个优势类群之外的所有其他类群。负责抑制原生生物的紫外线波长的季节性转变可能是由于臭氧减少,原生生物的光历史和/或物种组成的变化。我们在整个夏天观察到的UV-B诱导的抑制作用增加,这与戴维斯地区臭氧浓度的下降相对应。一月至四月之间,南极洲臭氧的反复下降与硅藻的开花相吻合,这些硅藻似乎对UV-B的耐受性较低,但约占南极水域年初级产量的47%。

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