| 南海北部和中部硅藻通量季节性变化及其对季风气候的响应 |
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| 引用本文： | 冉莉华,郑玉龙,陈建芳,陈荣华,郑连福,WIESNERMartin-G.南海北部和中部硅藻通量季节性变化及其对季风气候的响应[J].海洋学报,2011,33(5):139-145. |
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| 作者姓名： | 冉莉华 郑玉龙 陈建芳 陈荣华 郑连福 WIESNERMartin-G |
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| 作者单位： | 1.国家海洋局 第二海洋研究所 浙江 杭州 310012 |
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| 基金项目： | 国家自然科学基金(40676044);国家海洋局青年海洋科学基金重点项目(2010325);国家青年自然科学基金(41006034)。 |
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| 摘 要： | 通过对南海北部和中部两套时间序列沉积物捕获器中的颗粒物样品进行硅藻分析,揭示了南海北部和中部硅藻通量的季节变化规律及其区域差异和各自对东亚季风气候的响应.研究表明在南海北部和中部海域,硅藻通量可以在一定程度上指示海洋初级生产力水平,其中南海北部硅藻通量明显低于中部,这可能与北部颗粒物样品采集期间发生的E1 Ni(n)o...
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| 关 键 词： | 南海 硅藻 季风 沉积物捕获器 |
| 收稿时间： | 2010/1/29 0:00:00 |
The influence of monsoon on seasonal changes of diatom fluxes in the northern and central South China Sea |
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| RAN Li-hu,ZHENG Yu-long,CHEN Jian-fang,CHEN Rong-hu,ZHENG Lian-fu and WIESNER Martin-G.The influence of monsoon on seasonal changes of diatom fluxes in the northern and central South China Sea[J].Acta Oceanologica Sinica (in Chinese),2011,33(5):139-145. |
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| Authors: | RAN Li-hu ZHENG Yu-long CHEN Jian-fang CHEN Rong-hu ZHENG Lian-fu and WIESNER Martin-G |
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| Institution: | 1.The Second Institute of Oceanography, State Oceanic Adminstration,Hangzhou 310012, China2.Institute of Biogeochemistry and Marine Chemistry, University of Hamburg, D-20146 Hamburg, Germany |
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| Abstract: | Diatom analysis of samples from sediment traps deployed in the northern and central South China Sea reveals the seasonal changes of diatom fluxes and their relationships with the East Asia monsoon system. It is shown that the diatom flux can be treated as an indicator of marine primary productivity in the northern and central South China Sea. Especial low diatom fluxes are found in the northern South China Sea, which might be related to the El ni o event during 1987-1988. In the northern South China Sea, apparent increased diatom fluxes are found during the winter monsoon period, which is correlated with stronger sea water vertical mixing and higher aeolian particles input during this period. Relatively high fluxes are also found in the deep water than in the shallow water, indicating possible deep sea lateral advection in the northern South China Sea. Higher diatom fluxes during the summer monsoon period with peak flux in late June to early July are revealed in the central South China Sea, which may be stimulated by higher nutrient input during the summer monsoon. |
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| Keywords: | South China Sea diatom monsoon sediment trap |
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