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首页> 外文期刊>Journal of oceanography >Spatiotemporal changes in meiofaunal composition on soft substrates in the semi-enclosed inner section of the northern Yatsushiro Sea
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Spatiotemporal changes in meiofaunal composition on soft substrates in the semi-enclosed inner section of the northern Yatsushiro Sea

机译:八代海北部半封闭内陆软基底上的名词代名词组成的时空变化

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The Yatsushiro Sea is an inland sea in the southwestern part of Kyushu Island, covering an area of 1,200?km2, and is partly connected to the Ariake Sea to the north and the east China Sea to the south. The innermost part of the sea is semi-enclosed by the Shiranui reclaimed land, which was created in 1967. Coastal fishery operators in the region have suggested that fish stocks have declined due to the accumulation of ‘hedoro’ (sludge) on the sea floor, which increased after the land was reclaimed. This project analyzed spatiotemporal changes in the community structure of the meiofauna, which represent ideal organisms for environment assays and in the environmental factors in sediments at four fixed stations around the inner part of the northern Yatsushiro Sea over 3?years (May 2010–February 2013). The results confirm the site of local deposits in the narrow sub tidal section off the Shiranui reclaimed land, where rich organic matter has accumulated and highly sulfidic conditions above the standard criterion value for fisheries were present, along with clear and significant decreases in meiofaunal abundance during the summer. Multivariate analyses, however, did not reveal any strong association between the meiofaunal composition and any environmental factor in sediments, suggesting the organic and sulfidic conditions were not driving the temporal changes in meiofaunal structure in the area. Instead, the meiofaunal changes could be directly related to the low continuous decline in dissolved oxygen and salinity in the water on the sea floor in summer.
机译:八代海是九州岛西南部的内陆海域,面积为1200平方公里,部分与北部的有明海和南部的东中国海相连。 1967年创建的Shiranui填海区将海洋的最内层半封闭。该地区的沿海渔业经营者认为,由于海床中“ hedoro”(淤泥)的堆积,鱼类种群减少了。 ,这在土地开垦后有所增加。该项目分析了三代(2010年5月至2013年2月)北部八代海内部四个固定站的鱼类群落结构的时空变化,这些时空变化代表了进行环境分析的理想生物以及沉积物中的环境因子。 )。结果证实了在Shiranui填海区附近潮汐区狭窄的局部沉积物的位置,那里积累了丰富的有机物质,并且存在高于渔业标准值的高硫化物条件,并且在此期间淡季的丰度明显而显着降低。夏天。然而,多变量分析并未揭示出动植物的组成与沉积物中的任何环境因素之间的任何强关联,这表明有机和硫化物条件并未驱动该地区动植物的结构随时间变化。取而代之的是,藻类的变化可能直接与夏季海底水中溶解氧和盐度的持续下降较低有关。

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