| Silicon limitation on primary production and its destiny in Jiaozhou Bay, China——Ⅶ： The complementary mechanism of the earth ecosystem |
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| 引用本文： | 杨东方,高振会,杨应斌,孙培艳,王鑫平.Silicon limitation on primary production and its destiny in Jiaozhou Bay, China——Ⅶ： The complementary mechanism of the earth ecosystem[J].中国海洋与湖沼学报,2006,24(4):401-412. |
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| 作者姓名： | 杨东方 高振会 杨应斌 孙培艳 王鑫平 |
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| 作者单位： | College of Fishery Science Shanghai Fisheries University，Beihai Monitoring Center State Oceanic Administration，Beihai Monitoring Center State Oceanic Administration，Beihai Monitoring Center State Oceanic Administration，Beihai Monitoring Center State Oceanic Administration，Shanghai 200090 China Beihai Monitoring Center State Oceanic Administration Qingdao 266033 China，Qingdao 266033 China，Qingdao 266033 China，Qingdao 266033 China，Qingdao 266033 China |
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| 基金项目： | Supported by the Director’s Foundation of the Beihai Monitoring Cen-ter, the State Oceanic Administration, and Chinese Academy of Sciences (KZCX 2-207). |
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| 摘 要： | 1 INTRODUCTION In marine waters, water temperature and nutrient Si control the temporal and spatial variation of the phytoplankton growth (Yang et al., 2006). The effect of nutrient Si and water temperature on the mecha- nism of phytoplankton growth has p…
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| 关 键 词： | 胶洲湾 海洋生态 浮游植物 硅 |
| 收稿时间： | 2005-01-24 |
| 修稿时间： | 2005-08-25 |
Silicon limitation on primary production and its destiny in Jiaozhou Bay, China |
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| Yang Dongfang,Gao Zhenhui,Yang Yingbin,Sun Peiyan,Wang Xinping.Silicon limitation on primary production and its destiny in Jiaozhou Bay, China[J].Chinese Journal of Oceanology and Limnology,2006,24(4):401-412. |
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| Authors: | Yang Dongfang Gao Zhenhui Yang Yingbin Sun Peiyan Wang Xinping |
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| Institution: | (1) College of Fishery Science, Shanghai Fisheries University, 200090 Shanghai, China;(2) Beihai Monitoring Center, State Oceanic Administration, 266033 Qingdao, China |
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| Abstract: | In this paper, the phenomenon that the variation in nutrient and water temperature could cause changes in phytoplankton growth and structure is examined; and the question of how a marine eco-system make up the earth ecosystem step by step to auto-sustain the balance between phytoplankton and nutrient supply especially Si is discussed. Three major complementary mechanisms of the earth ecosys-tem for nutrient Si, water temperature and carbon were put forward. Understanding the mechanisms nowadays would explain the why the El Nio and La Nia occurred, and forecast the trend of hu-man-impacted the earth, which would alert us with proactive countermeasures. |
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| Keywords: | nutrient Si phytoplankton marine ecosystem earth ecosystem complementary mechanism |
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