| Yttrium and rare earth element partitioning in seawaters from the Bay of Bengal | |
Yu, Zhaojie1; Colin, Christophe1; Douville, Eric2; Meynadier, Laure3; Duchamp-Alphonse, Stephanie1; Sepulcre, Sophie1; Wan, Shiming4,5; Song, Lina6 ; Wu, Qiong7; Xu, Zhaokai4; Bassinot, Frank2
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| 2017-04-01 | |
| 发表期刊 | GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
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| 卷号 | 18期号:4页码:1388-1403 |
| 文章类型 | Article |
| 摘要 | The dissolved yttrium (Y) and rare earth element (REE) concentrations of seawater samples collected along a north-south hydrological transect within the Bay of Bengal (BoB) have been analyzed to estimate contributions of the Ganges and Brahmaputra (G-B) river inputs to the dissolved REE distribution of the Northern Indian Ocean. Surface water masses of the BoB are characterized by Y/Ho ratios (84) intermediate between the G-B river suspended sediment (41) and water mass from the South Indian Ocean (93). Covariation of MREE (middle REE, Sm) and LREE (light REE, La) concentrations suggests that the dissolved REEs in surface waters (upper 100 m depth) of the BoB (Sm/La=0.21) appear to derive mainly from the freshwater discharge of the G-B river system. In contrast, values obtained in the intermediate and deep waters (Sm/La=0.14) suggest a mixing of dissolved REEs deriving from the release of G-B river suspended particles (Sm/La=0.16) and the contribution of Antarctic Bottom Water (AABW) (Sm/La=0.12). Consequently, we propose that MREE/MREE* ratios in the BoB waters could be an accurate proxy to trace lithogenic inputs from the G-B river system. The dissolved and particle remineralization Nd fluxes from G-B river system are calculated to constitute about 9% and 4% of the global dissolved river discharge and "boundary inputs" flux. Our estimation indicates that the massive G-B river system inputs could greatly alter the dissolved REEs distribution in the BoB and contribute to the dissolved REEs budget in the ocean. |
| DOI | 10.1002/2016GC006749 |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000403478500005 |
| 引用统计 | |
| 文献类型 | 期刊论文 |
| 版本 | 出版稿 |
| 条目标识符 | http://ir.qdio.ac.cn/handle/337002/137120 |
| 专题 | 海洋地质与环境重点实验室 海洋环流与波动重点实验室 |
| 作者单位 | 1.Univ Paris Saclay, Univ Paris Sud, CNRS, UMR 8148,Lab GEOsci Paris Sud, Orsay, France 2.Univ Paris Saclay, UVSQ, CNRS, CEA,Lab Sci Climat & Environm,LSCE IPSL, Gif Sur Yvette, France 3.Univ Paris Diderot, Inst Phys Globe Paris, UMR 7154, Equipe Geochim & Cosmochim,Sorbonne Paris Cite, Paris, France 4.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China 5.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Peoples R China 6.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China 7.Tongji Univ, State Key Lab Marine Geol, Shanghai, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yu, Zhaojie,Colin, Christophe,Douville, Eric,et al. Yttrium and rare earth element partitioning in seawaters from the Bay of Bengal[J]. GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,2017,18(4):1388-1403. |
| APA | Yu, Zhaojie.,Colin, Christophe.,Douville, Eric.,Meynadier, Laure.,Duchamp-Alphonse, Stephanie.,...&Bassinot, Frank.(2017).Yttrium and rare earth element partitioning in seawaters from the Bay of Bengal.GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,18(4),1388-1403. |
| MLA | Yu, Zhaojie,et al."Yttrium and rare earth element partitioning in seawaters from the Bay of Bengal".GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS 18.4(2017):1388-1403. |
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| 文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
| Yttrium and rare ear（4566KB） | 期刊论文 | 出版稿 | 限制开放 | CC BY-NC-SA | 浏览 | |
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