中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Historical changes in nutrient structure and its influences on phytoplantkon composition in Jiaozhou Bay

文献类型:期刊论文

作者Shen, ZL
刊名ESTUARINE COASTAL AND SHELF SCIENCE
出版日期2001-02-01
卷号52期号:2页码:211-224
关键词Nutrients Ratios Historical Changes Nutrient Structure Nutrient Balance Limitation/limiting Phytoplankton Jiaozhou Bay
ISSN号0272-7714
文献子类Article
英文摘要Due to the influence of human activities, nutrient concentrations, nutrient ratios and phytoplankton composition have notably changed in Jiaozhou Bay, China since the 1960s. From the 1960s to the 1990s, nutrient concentrations have increased 1.4 times for PO4-P, 4.3 times for NO3-N, 4.1 times for NH4-N and 3.9 times for DIN. The atomic ratio of DIN:PO4-P increased very rapidly from 15.9 +/- 6.3 for the 1960s, to 37.8 +/- 22.9 for the 1990s. SiO3-Si concentration has remained at a very low level from the 1980s to the 1990s. The high ratio of DIN: PO4-P and low ratios of SiO3-Si:PO4-P (7.6 +/- 8.9) and SiO3-Si:DIN (0.19 +/- 0.15) showed the nutrient structure of Jiaozhou Bay has changed from more balanced to unbalanced during the last 40 years. The possibility that DIN and/or PO4-P as limiting factors of Jiaozhou Bay phytoplankton has been lessened or eliminated and that of SiO3-Si limiting has been increased. The changes in nutrient structure may have led to the decrease of large diatoms and a shift of phytoplankton species composition. It is likely that there is a trend from large diatoms to smaller cells in Jiaozhou Bay. (C) 2001 Academic Press.; Due to the influence of human activities, nutrient concentrations, nutrient ratios and phytoplankton composition have notably changed in Jiaozhou Bay, China since the 1960s. From the 1960s to the 1990s, nutrient concentrations have increased 1.4 times for PO4-P, 4.3 times for NO3-N, 4.1 times for NH4-N and 3.9 times for DIN. The atomic ratio of DIN:PO4-P increased very rapidly from 15.9 +/- 6.3 for the 1960s, to 37.8 +/- 22.9 for the 1990s. SiO3-Si concentration has remained at a very low level from the 1980s to the 1990s. The high ratio of DIN: PO4-P and low ratios of SiO3-Si:PO4-P (7.6 +/- 8.9) and SiO3-Si:DIN (0.19 +/- 0.15) showed the nutrient structure of Jiaozhou Bay has changed from more balanced to unbalanced during the last 40 years. The possibility that DIN and/or PO4-P as limiting factors of Jiaozhou Bay phytoplankton has been lessened or eliminated and that of SiO3-Si limiting has been increased. The changes in nutrient structure may have led to the decrease of large diatoms and a shift of phytoplankton species composition. It is likely that there is a trend from large diatoms to smaller cells in Jiaozhou Bay. (C) 2001 Academic Press.
学科主题Marine & Freshwater Biology ; Oceanography
语种英语
WOS记录号WOS:000167531000006
公开日期2010-12-22
源URL[http://ir.qdio.ac.cn/handle/337002/2835]  
专题海洋研究所_海洋生态与环境科学重点实验室
作者单位Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
推荐引用方式
GB/T 7714
Shen, ZL. Historical changes in nutrient structure and its influences on phytoplantkon composition in Jiaozhou Bay[J]. ESTUARINE COASTAL AND SHELF SCIENCE,2001,52(2):211-224.
APA Shen, ZL.(2001).Historical changes in nutrient structure and its influences on phytoplantkon composition in Jiaozhou Bay.ESTUARINE COASTAL AND SHELF SCIENCE,52(2),211-224.
MLA Shen, ZL."Historical changes in nutrient structure and its influences on phytoplantkon composition in Jiaozhou Bay".ESTUARINE COASTAL AND SHELF SCIENCE 52.2(2001):211-224.

入库方式: OAI收割

来源:海洋研究所

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