首页> 外文期刊>Journal of oceanography >Year-round accumulation of particulate organic matter in the estuarine turbidity maximum: comparative observations in three macrotidal estuaries (Chikugo, Midori, and Kuma Rivers), southwestern Japan
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Year-round accumulation of particulate organic matter in the estuarine turbidity maximum: comparative observations in three macrotidal estuaries (Chikugo, Midori, and Kuma Rivers), southwestern Japan

机译:在河口浊度最大值中的全年颗粒有机物积累:日本西南部三个巨潮河口(筑后,绿通和熊马河)的比较观测

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The inner part of the Ariake Sea is one of the most productive estuarine systems in Japan. To examine potential food items for estuarine organisms, we conducted monthly observations of the dynamics of particulate organic matter along the macrotidal Chikugo River estuary in 2005 and 2006. In the neighboring macrotidal Midori and Kuma River estuaries, comparative observations were made. High turbidity and strong vertical mixing were observed only at low salinities (<10) in the Chikugo River estuary. In contrast, the Midori and Kuma River estuaries were characterized by less turbid and less mixed waters. Concentrations of particulate organic carbon often exceeded 5?mg?l?1 in or close to the estuarine turbidity maximum (ETM) of the Chikugo River estuary. However, such high concentrations were rarely observed in the other two estuaries. The observed differences could be attributable to different hydrodynamic processes related to the different lengths of tidal reaches: 23, 8, and 6?km in the Chikugo, Midori, and Kuma Rivers, respectively. In the Chikugo River estuary, spatiotemporal changes of chlorophyll a suggested that phytoplankton occurred abundantly up- and/or downstream from the ETM especially during the warm season. In contrast, pheophytin (i.e., plant detritus) always accumulated in or close to the ETM. Carbon stable isotope ratios and carbon to nitrogen ratios indicated that the plant detritus was derived from phytoplankton and terrestrial plants. The Chikugo River estuary has a high potential to support the production of estuarine organisms through abundant plant detritus in the well-developed ETM all the year round.
机译:有明海的内部是日本生产力最高的河口系统之一。为了检查河口生物的潜在食物,我们在2005年和2006年沿大潮汐筑后河河口进行了颗粒有机物动力学的月度观测。在邻近的巨潮Midori和Kuma河口进行了对比观测。在筑后河河口,只有在低盐度(<10)时才观察到高浊度和强垂直混合。相比之下,Midori河和Kuma河河口的特点是浑浊较少,水质较少。在筑后河河口最大浊度(ETM)中或接近该浓度时,颗粒有机碳的浓度通常超过5?mg?l?1。但是,在其他两个河口很少观察到如此高的浓度。所观察到的差异可能归因于潮汐长度不同的不同水动力过程:在筑后河,绿道河和久马河分别为23、8和6公里。在筑后河河口,叶绿素a的时空变化表明浮游植物大量出现在ETM的上下游,特别是在暖季。相反,脱镁叶绿素(即植物碎屑)总是积累在ETM中或附近。碳稳定同位素比和碳氮比表明植物碎屑来自浮游植物和陆生植物。筑后河河口全年通过发达的ETM中丰富的植物碎屑来支持河口生物的生产。

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