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首页> 外文期刊>Estuarine Coastal and Shelf Science >Dynamics of heterotrophic dinoflagellates off the Pearl River Estuary, northern South China Sea
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Dynamics of heterotrophic dinoflagellates off the Pearl River Estuary, northern South China Sea

机译:南海北部珠江口外异养鞭毛体的动态

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摘要

Variations in abundance, biomass, vertical profile and cell size of heterotrophic dinoflagellates (HDFs) between summer and winter and its controlling factors were studied in the northern South China Sea (SCS). It was found that HDF abundance and carbon biomass were 4-102 × 10~3 cells L~(-1) and 0.34-12.3 mgCL~(-1) in winter (February 2004), respectively, while they were 2-142 × 10~3 cells L~(-1) and 0.22-31.4 μg CL~(-1) in summer (July, 2004), respectively, in the northern SCS. HDF abundance and carbon biomass decreased from the estuary to inshore and then offshore. Vertical profiles of HDF abundance were heterogeneous, which accorded well with that of chlorophyll a (Chl.a). Higher abundance of HDFs was often observed at a depth of 30-70 m offshore waters, matching well with the Chl.a maximum, while it showed high abundance at the surface in some coastal and estuary stations. Small HDFs (≤20 μm) dominated the assemblage in term of abundance accounting for more than 90%. However, large HDFs (>20 μm) generally-contributed equally in terms of carbon biomass, accounting for 47% on average. HDFs showed different variation patterns for the different study regions; in the estuarine and continental shelf regions, abundance and biomass values were higher in summer than those in winter, while it was the reverse pattern for the slope waters. Hydrological factors (e.g. water mass, river outflow, monsoon and eddies) associated with biological factors, especially the size-fractionated Chl.a, seemed to play an important role in regulating HDF distribution and variations in the northern South China Sea.
机译:研究了南海北部(SCS)夏季和冬季之间异养鞭毛藻(HDFs)的丰度,生物量,垂直剖面和细胞大小的变化及其控制因素。发现冬季(2004年2月)的HDF丰度和碳生物量分别为4-102×10〜3个细胞L〜(-1)和0.34-12.3 mgCL〜(-1),而它们为2-142×夏季(2004年7月),北半球10〜3个细胞L〜(-1)和0.22-31.4μgCL〜(-1)。 HDF的丰度和碳生物量从河口到近海再到近海减少。 HDF丰度的垂直分布是异质的,与叶绿素a(Chl.a)的分布非常吻合。经常在离岸水域30-70 m的深度观察到HDF的丰度较高,与Chl.a最大值相吻合,而在某些沿海和河口站地表则显示出较高的HDF丰度。小型HDF(≤20μm)以丰富度占主导地位,占90%以上。但是,大型HDF(> 20μm)通常在碳生物量方面的贡献均等,平均占47%。 HDF在不同的研究区域显示出不同的变化模式;在河口和大陆架地区,夏季的丰度和生物量值高于冬季,而坡度水的丰度和生物量值则相反。与生物因素有关的水文因素(例如水量,河流流出,季风和涡流),特别是大小分级的Chl.a,似乎在调节南海北部的HDF分布和变化中起着重要作用。

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  • 来源
    《Estuarine Coastal and Shelf Science》 |2009年第3期|421-429|共9页
  • 作者单位

    State Key Laboratory of Marine Environmental Science, Environmental Science Research Center, Xiamen University, Xiamen, PR China Marine Environmental Monitoring Center of Beihai, Bureau of Environmental Protection of Guangxi, Beihai, PR China;

    State Key Laboratory of Marine Environmental Science, Environmental Science Research Center, Xiamen University, Xiamen, PR China;

    State Key Laboratory of Marine Environmental Science, Environmental Science Research Center, Xiamen University, Xiamen, PR China;

    Second Institute of Oceanography, State Oceanic Administration, Hangzhou, PR China;

    State Key Laboratory of Marine Environmental Science, Environmental Science Research Center, Xiamen University, Xiamen, PR China;

    State Key Laboratory of Marine Environmental Science, Environmental Science Research Center, Xiamen University, Xiamen, PR China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    heterotrophic dinoflagellates; temporal and spatial variations; anticyclonic (warm) eddy; northern South China Sea;

    机译:异养藻鞭毛虫;时空变化;反气旋(暖)涡流;南海北部;

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