DOI: 10.1002/2017GB005711
Scopus记录号: 2-s2.0-85030871614
论文题名: Distribution of Dissolved Zinc in the Western and Central Subarctic North Pacific
作者: Kim T ; , Obata H ; , Nishioka J ; , Gamo T
刊名: Global Biogeochemical Cycles
ISSN: 8866236
出版年: 2017
卷: 31, 期: 9 起始页码: 1454
结束页码: 1468
语种: 英语
英文关键词: GEOTRACES
; subarctic North Pacific
; trace metal
; zinc
Scopus关键词: biogeochemical cycle
; cruise report
; dissolved matter
; intermediate water
; open ocean
; phosphorus
; reactive transport
; silicate
; trace metal
; Pacific Ocean
; Pacific Ocean (North)
英文摘要: We investigated the biogeochemical cycling of dissolved zinc (Zn) in the western and central subarctic North Pacific during the GEOTRACES GP 02 cruise. The relationship between dissolved Zn and silicate in the subarctic North Pacific plotted as a concave curve. Values of Zn* were strongly positive in the intermediate waters (26.6–27.5 σθ) of both the western and the central subarctic North Pacific. There was a distinct kink in the relationship between dissolved Zn and soluble reactive phosphorus (SRP) at the transition from shallow to intermediate water, which is similar to what has been reported for other open oceans. The high Zn:SRP ratio and high Zn* in the intermediate water suggest that intermediate water masses play an important role in the decoupling of dissolved Zn and silicate in the subarctic North Pacific, which implies that the biogeochemical processes that control dissolved Zn and silicate in the intermediate water are different from those in other oceanic regions. ©2017. American Geophysical Union. All Rights Reserved.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/77708
Appears in Collections: 气候变化事实与影响
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作者单位: Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, Japan; Institute of Low Temperature Science, Hokkaido University, Sapporo, Japan
Recommended Citation:
Kim T,, Obata H,, Nishioka J,et al. Distribution of Dissolved Zinc in the Western and Central Subarctic North Pacific[J]. Global Biogeochemical Cycles,2017-01-01,31(9)