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Please use this identifier to cite or link to this item: http://ntour.ntou.edu.tw:8080/ir/handle/987654321/40903

Title: Trace metal cycling in the deep water of the South China Sea: The composition, sources and fluxes of sinking particles
Authors: Tung-Yuan Ho;Wen-Chen Chou;Hui-Ling Lin;David D. Sheu
Contributors: 國立臺灣海洋大學:海洋環境化學與生態研究所
Date: 2011-07
Issue Date: 2017-02-07T05:57:39Z
Publisher: Limnology and Oceanography
Abstract: Abstract:Moored sediment traps were deployed for 1 yr at depths of 120, 600, and 3500 m in the water column to investigate the trace metal (M) (Al, Ti, V, Cr, Mn, Fe, Co, Ni, Cu, and Zn) composition, sources, and fluxes of deep-water sinking particles. Vertical transport for most of the metals at 120 m was strongly associated with organic matter production, and the major part of many of the metals in the sinking particles was of anthropogenic origin. Although the lithogenic fraction in deeper waters greatly increased with depth, significant proportions of the nonlithogenic and nonintracellular fractions were still observed when using M : Al or M : P ratios as indicators, particularly for Zn, Cu, Ni, Co, and Mn. Because particles from horizontal transport and sediment resuspension are known to be lithogenic in the deep basin, the trace metals in sinking particles in the twilight zone and deep water, which feature significantly elevated M : Al ratios, originate from the downward transport of anthropogenic or authigenic origins. With increasing inputs from anthropogenic aerosols over large oceanic regions globally, the coupling and transport of some trace metals originating from anthropogenic aerosols, such as Zn, Cu, Co, and Ni, with sinking organic particles has become an important pathway for trace metal cycling not only in the euphotic zone, but also in the twilight zone and deeper waters.
Relation: 56(4), pp.1225-1243
URI: http://ntour.ntou.edu.tw:8080/ir/handle/987654321/40903
Appears in Collections:[海洋環境與生態研究所] 期刊論文

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