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Effects of surface current patterns on spatial variations of phytoplankton community and environmental factors in Sunda shelf

机译:Effects of surface current patterns on spatial variations of phytoplankton community and environmental factors in sunda shelf

摘要

Phytoplankton community and environmental factors were investigated in the surface water from eastern Indian Ocean (EIO) to southern South China Sea (SCS) during April-May monsoon transition period both in 2010 and 2011. Our results indicated that the surface current patterns were different in the two cruises. Sea surface salinity (SSS) was lower in Java Sea US), but its salinity front obviously moved to the middle of Sunda Strait when surface waters flowed from JS to EIO in May of 2010. Nutrient concentrations were generally higher in Sunda Strait and JS. Silicate concentrations were significantly lower in EIO suggesting a possibility of silicate limitation for the growth of phytoplankton, which were less than 1 mu mol L-1 in the offshore stations of EIO in May of 2010. Phytoplankton abundance and biodiversity were significant higher in Sunda strait and its adjacent stations, with larger cell-size and higher diatoms proportion. More offshore species were found in Sunda Strait when surface waters flowed from EIO to JS in April of 2011. Nutrient source can be different in Sunda Strait during inflow or outflow of surface waters. The spatial variation of phytoplankton community was greatly determined by Chaetoceros spp., Navicula sp., Pleurosigma affine, Thalassionema frauenfeldii and nano-dinoflagelage. Salinity, nitrate and silicate were the most important environmental factors regulating the variation of phytoplankton community. This study suggests that spatial distribution of phytoplankton and environmental factors are significantly influenced by the surface current patterns and river discharges, and these influences should be greater in dry season. (C) 2014 Published by Elsevier Ltd.
机译:在2010年和2011年的4月至5月季风过渡期,从印度洋东部(EIO)到南海南部(SCS)的地表水进行了浮游植物群落和环境因子的调查。两次巡游。在Java Java US中,海面盐度(SSS)较低,但是2010年5月,当表层水从JS流入EIO时,其盐度前沿明显移至Sun他海峡中部。Sun他海峡和JS中的营养物浓度通常较高。 EIO中的硅酸盐浓度显着较低,表明硅酸盐限制了浮游植物的生长,2010年5月在EIO的近海站浮游植物的硅酸含量低于1μmol L-1。Sun他海峡的浮游植物丰度和生物多样性明显较高。及其邻近的站点,具有更大的细胞大小和更高的硅藻比例。 2011年4月,当地表水从EIO流入JS时,Sun他海峡发现了更多的近海物种。在地表水流入或流出时,source他海峡的营养来源可能有所不同。浮游植物群落的空间变化在很大程度上由Chaetoceros spp。,Navicula sp。,Pleurosigma affine,Thalassionema frauenfeldii和纳米恐龙鞭毛确定。盐度,硝酸盐和硅酸盐是调节浮游植物群落变化的最重要的环境因素。这项研究表明,浮游植物的空间分布和环境因素受地表水流方式和河流流量的显着影响,而在旱季,这些影响应更大。 (C)2014由Elsevier Ltd.出版

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