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首页> 外文期刊>Journal of oceanography >Phytoplankton Pigment Change as a Photoadaptive Response to Light Variation Caused by Tidal Cycle in Ariake Bay Japan
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Phytoplankton Pigment Change as a Photoadaptive Response to Light Variation Caused by Tidal Cycle in Ariake Bay Japan

机译:浮游植物色素的变化对日本有明湾潮汐周期引起的光变的光适应性响应

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Underwater light environment and photosynthetic accessory pigments were investi-gated in Ariake Bay in order to understand how change of the pigments occurs in response to the tidal-induced changes in underwater light conditions. We hypothesize that phytoplankton increases photo-protective pigments and decreases light-harvest-ing pigments under higher light condition in the mixed layer caused by tidal cycle. Contribution rates of non-phytoplankton particles (a_(nph)(400-700)) for light attenua-tion coefficient (K_d) was highest (32-85%), and those of phytoplankton particles (a_(ph)(400-700)), dissolved organic matter (a_g(400-700)) and water were 6-32,6-21 and 5-23%, respectively. Mean K_d was higher during the spring tide (0.55 ± 0.23 m~(-1)) than the neap tide (0.44 ± 0.16 m~(-1)), and the K_d difference was caused by the sub-stances resuspension due to the tidal current. In contrast, ratios of photo-protective pigments (diadinoxanthin and diatoxanthin) per chlorophyll a ((DD+DT)/Chl a) were higher during the neap tide (0.10 ± 0.03 mg mg-Chl a~(-1)) than the spring tide (0.08 ± 0.03 mg mg-Chl a~(-1)). And there was significant positive correlation between (DD+DT)/ Chl a and mean relative PAR in the mixed layer (I_(mix) ). Moreover, there was signifi-cant negative correlation between ratios of light-harvesting pigments (fucoxanthin) per Chl a (Fuco/Chl a) and I_(mix) . These results suggested that phytoplankton in Ariake Bay increase photo-protective pigments and decrease light-harvesting pigments in the higher light condition of less turbid, shallower mixed layer during neap tide than spring tide.
机译:为了了解潮汐引起的水下光变化,如何在有明湾进行水下光环境和光合辅助色素的研究。我们假设浮游植物在潮汐循环引起的混合层中在较高光照条件下会增加光保护性色素并减少光吸收性色素。非浮游植物颗粒(a_(nph)(400-700))对光衰减系数(K_d)的贡献率最高(32-85%),而浮游植物颗粒(a_(ph)(400-700) ),溶解的有机物(a_g(400-700))和水分别为6-32、6-21和5-23%。春季潮时的平均K_d(0.55±0.23 m〜(-1))高于潮汐时的平均K_d(0.44±0.16 m〜(-1)),K_d的差异是由于水体重新悬浮造成的。潮流。相比之下,在退潮期间,每叶绿素a的光保护性颜料(二恶黄质和重黄质黄质)的比例((DD + DT)/ Chl a)要更高(0.10±0.03 mg mg-Chl a〜(-1))。春季潮(0.08±0.03 mg mg-Chl a〜(-1))。并且(DD + DT)/ Chla与混合层中的平均相对PAR(I_(mix))之间存在显着的正相关。此外,每Chla(Fuco / Chl a)和I_(mix)的光采颜料(岩藻黄质)的比例之间存在显着的负相关。这些结果表明,与潮汐相比,有潮时浮游植物增加了光保护性色素,而在潮汐较少混浊,浅层的较高光照条件下,光吸收色素减少了。

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