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Sedimentary and Benthic Environment Characteristics in Macroalgal Habitats of the Intertidal Zone in Hampyeong Bay

机译:咸平湾潮间带大型藻类栖息地的沉积和底栖环境特征

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摘要

To understand the characteristics of sedimentary and benthic environments in habitats of naturally-occurring intertidal benthic macroalgae, various geochemical parameters of sediment (grain size, ignition loss [IL], chemical oxygen demand [COD], and acid volatile sulfur [AVS]) and pore water (temperature, salinity, pH, and nutrients) were measured in the southern intertidal zone of Hampyeong Bay at two month intervals from April to October 2009. Ecological characteristics including the distribution and biomass of benthic macroalgae were also investigated. Benthic macroalgae were distributed below 4 to 5 m depth from mean sea level near the lower portion of the intertidal zone where air exposure time is relatively short. The distribution area and biomass of benthic macroalgae gradually decreased during the study period. The surface sediments in the benthic algal region were mainly composed of finer sediments, such as slightly gravelly mud and mud. The temperature, salinity, pH, and nutrient concentrations (except dissolved inorganic nitrogen) in pore water did not differ in regions with and without benthic macroalgae, whereas the mean grain size and the concentrations of IL, COD, and AVS in sediments were much higher in regions harboring benthic macroalgae. The correlation between mean grain size and IL in sediments displayed two distinct gradients and the slope was much steeper in regions harboring benthic macroalgae, indicating that the content of organic matter in benthic algal region is not solely dependent on mean grain size. Our results indicate that the benthic macroalgae in the southern intertidal zone of Hampyeong Bay play an important role in the accumulation of organic matter in sediment.
机译:为了了解自然发生的潮间底栖大型藻类栖息地的沉积和底栖环境特征,沉积物的各种地球化学参数(粒度,着火损失[IL],化学需氧量[COD]和酸挥发性硫[AVS])和2009年4月至2009年10月,以每两个月为间隔,对咸平湾南部潮间带的孔隙水(温度,盐度,pH和养分)进行了测量。还研究了底栖大型藻类的生态特征。底栖大型藻类分布在距暴露时间相对较短的潮间带下部较低的平均海平面以下4至5 m的深度处。在研究期间底栖大型藻类的分布面积和生物量逐渐减少。底栖藻类地区的表层沉积物主要由较细的沉积物组成,例如微砾石泥和泥浆。在有和没有底栖大型藻类的地区,孔隙水中的温度,盐度,pH和营养物浓度(溶解的无机氮除外)没有差异,而沉积物中平均粒径和IL,COD和AVS的平均含量要高得多在拥有底栖大型藻类的地区。底栖大型藻类区域平均粒径与沉积物中IL的相关性表现出两个明显的梯度,坡度陡得多,表明底栖藻类区域中有机质的含量不仅取决于平均粒径。我们的结果表明,咸平湾南部潮间带底栖大型藻类在沉积物中有机质的积累中起着重要作用。

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