Vertical transferring process of rare elements in coral reef lagoons of Nansha Islands, South China Sea | |
Song, JM; Li, PC | |
刊名 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES |
1998-02-01 | |
卷号 | 41期号:1页码:42-48 |
关键词 | Rare Elements Vertical Flux Transferring Form Coral Reef Ecosystem Of Nansha Islands |
ISSN号 | 1006-9313 |
文献子类 | Article |
英文摘要 | The vertical fluxes and vertical transferring forms of 18 rare elements were studied for the first time in the coral reef ecosystem of Nansha Islands, South China Sea, by deploying sediment traps, The results showed that the vertical transferring flux of most of the measured rare elements in Yongshu lagoon were higher than that in Zhubi lagoon. The vertical transferring forms of rare elements were mainly in the carbonate form, but Ta, As, Th mainly in the ion-exchange form, Ag in iron-manganese oxide form and Sb in the organic matter + sulphide form. None of the 18 rare elements was transferred mainly in the form of detritus silicate to sea floor. This proved that rare elements originating from the earth's crust were redistributed in sinking particulates after they were brought into ocean. The relation between the fluxes and surface seawater temperature (STT) was also studied. The sensitivity of rare elements to SST was in order: Rb>V>As>Ti>U>Zn>Sb>Hf>Ag>Cs.; The vertical fluxes and vertical transferring forms of 18 rare elements were studied for the first time in the coral reef ecosystem of Nansha Islands, South China Sea, by deploying sediment traps, The results showed that the vertical transferring flux of most of the measured rare elements in Yongshu lagoon were higher than that in Zhubi lagoon. The vertical transferring forms of rare elements were mainly in the carbonate form, but Ta, As, Th mainly in the ion-exchange form, Ag in iron-manganese oxide form and Sb in the organic matter + sulphide form. None of the 18 rare elements was transferred mainly in the form of detritus silicate to sea floor. This proved that rare elements originating from the earth's crust were redistributed in sinking particulates after they were brought into ocean. The relation between the fluxes and surface seawater temperature (STT) was also studied. The sensitivity of rare elements to SST was in order: Rb>V>As>Ti>U>Zn>Sb>Hf>Ag>Cs. |
学科主题 | Geosciences, Multidisciplinary |
语种 | 英语 |
WOS记录号 | WOS:000072058100006 |
公开日期 | 2010-12-22 |
内容类型 | 期刊论文 |
源URL | [http://ir.qdio.ac.cn/handle/337002/2857] |
专题 | 海洋研究所_海洋生态与环境科学重点实验室 海洋研究所_海洋生物技术研发中心 |
作者单位 | Acad Sinica, Inst Oceanol, Qingdao 266071, Peoples R China |
推荐引用方式 GB/T 7714 | Song, JM,Li, PC. Vertical transferring process of rare elements in coral reef lagoons of Nansha Islands, South China Sea[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,1998,41(1):42-48. |
APA | Song, JM,&Li, PC.(1998).Vertical transferring process of rare elements in coral reef lagoons of Nansha Islands, South China Sea.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,41(1),42-48. |
MLA | Song, JM,et al."Vertical transferring process of rare elements in coral reef lagoons of Nansha Islands, South China Sea".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 41.1(1998):42-48. |
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