Vertical distribution of pico- and nano-sized Dapi yellow particles at Dyfamed time-series station, NW Mediterranean

Tsuneo Tanaka , Fereidoun Rassoulzadegan
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Abstract

We measured abundance and surface area of pico- and nano-sized organic particles that are stained by 4’6-diamidino-2-phenylindole (Dapi), namely Dapi yellow particles. This study was done monthly from April 1999 to March 2000 from surface down to 2000 m at the French-JGOFS time-series station Dyfamed in the NW Mediterranean. Dapi yellow particles were always observed throughout the water column and the total surface area of Dapi yellow particles 0.2–10 μm ranged from 0.5 to 51.5 mm2 l–1. Dapi yellow particles were generally less abundant in the surface layer, greater between 70 and 500 m and decreased toward 2000 m. During the mixing period, Dapi yellow particles were homogeneous throughout the upper 200 m, suggesting that distribution of Dapi yellow particles was influenced by the hydrological structure. Dapi yellow particles correlated positively with inorganic nutrients (NO3, PO4 and Si) and negatively with dissolved oxygen concentration (P < 0.05). These results suggest that abundant Dapi yellow particles from the bottom of the euphotic layer to the intermediate layer reflect the process of particle degradation in the ocean.

地中海西北部dyfamous时间序列站的皮、纳米尺度大黄颗粒垂直分布
我们测量了4 ' 6-二氨基-2-苯基吲哚(Dapi)染色的微纳米级有机颗粒的丰度和表面积,即Dapi黄色颗粒。本研究于1999年4月至2000年3月在地中海西北部的法国- jgofs时间序列站dyreputation从地表向下至2000 m逐月进行。在整个水柱中均观察到大api黄颗粒,0.2 ~ 10 μm的大api黄颗粒的总表面积为0.5 ~ 51.5 mm2 l-1。大黄颗粒在表层的含量普遍较低,在70 ~ 500 m之间较多,向2000 m方向减少。在混合期,大皮黄颗粒在200 m以上呈均匀分布,表明大皮黄颗粒的分布受水文结构的影响。大皮黄颗粒与无机养分(NO3、PO4和Si)呈正相关,与溶解氧浓度(P <0.05)。这些结果表明,从透光层底部到中间层丰富的大api黄颗粒反映了海洋中颗粒降解的过程。
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