Rare earth element distributions in the West Pacific: Trace element sources and conservative vs. non-conservative behavior

被引:30
作者
Behrens, Melanie K. [1 ]
Pahnke, Katharina [1 ]
Paffrath, Ronja [1 ]
Schnetger, Bernhard [2 ]
Brumsack, Hans-Juergen [2 ]
机构
[1] Carl von Ossietzky Univ Oldenburg, Inst Chem & Biol Marine Environm ICBM, Max Planck Res Grp Marine Isotope Geochem, Carl von Ossietzky Str 9-11, D-26129 Oldenburg, Germany
[2] Carl von Ossietzky Univ Oldenburg, Microbiogeochem, Inst Chem & Biol Marine Environm ICBM, Carl von Ossietzky Str 9-11, D-26129 Oldenburg, Germany
关键词
rare earth elements; West Pacific; GEOTRACES; EQUATORIAL PACIFIC; NEODYMIUM ISOTOPES; GEOTRACES INTERCALIBRATION; ATLANTIC SECTOR; SOUTH-PACIFIC; DISSOLVED ND; WATER; OCEAN; SEAWATER; CIRCULATION;
D O I
10.1016/j.epsl.2018.01.016
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Recent studies suggest that transport and water mass mixing may play a dominant role in controlling the distribution of dissolved rare earth element concentrations ([REE]) at least in parts of the North and South Atlantic and the Pacific Southern Ocean. Here we report vertically and spatially high-resolution profiles of dissolved REE concentrations ([REE]) along a NW-SE transect in the West Pacific and examine the processes affecting the [REE] distributions in this area. Surface water REE patterns reveal sources of trace element (TE) input near South Korea and in the tropical equatorial West Pacific. Positive europium anomalies and middle REE enrichments in surface and subsurface waters are indicative of TE input from volcanic islands and fingerprint in detail small-scale equatorial zonal eastward transport of TEs to the iron-limited tropical East Pacific. The low [REE] of North and South Pacific Tropical Waters and Antarctic Intermediate Water are a long-range (i.e., preformed) laterally advected signal, whereas increasing [REE] with depth within North Pacific Intermediate Water result from release from particles. Optimum multiparameter analysis of deep to bottom waters indicates a dominant control of lateral transport and mixing on [REE] at the depth of Lower Circumpolar Deep Water (>3000 m water depth: 75-100% explained by water mass mixing), allowing the northward tracing of LCDW to 28 N in the Northwest Pacific. In contrast, scavenging in the hydrothermal plumes of the Lau Basin and Tonga-Fiji area at 1500-2000 m water depth leads to [REE] deficits (similar to 40-60% removal) and marked REE fractionation in the tropical West Pacific. Overall, our data provide evidence for active trace element input both near South Korea and Papua New Guinea, and for a strong lateral transport component in the distribution of dissolved REEs in large parts of the West Pacific. (C) 2018 Elsevier B.V. All rights reserved.
引用
收藏
页码:166 / 177
页数:12
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