Linking the distribution of 210Po and 210Pb with plankton community along Line P, Northeast Subarctic Pacific

被引:8
|
作者
Choi, Hiu Yan [1 ,2 ]
Stewart, Gillian M. [1 ,2 ]
Lomas, Michael W. [3 ]
Kelly, Roger P. [4 ]
Moran, S. Bradley [4 ]
机构
[1] CUNY, Queens Coll, Flushing, NY 11367 USA
[2] CUNY, Grad Ctr, Flushing, NY 11367 USA
[3] Bermuda Inst Ocean Sci, Biol Stn 17, St Georges 01, GE, France
[4] Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA
基金
美国国家科学基金会;
关键词
Polonium; Plankton; Ocean Station Papa; Particle export; ORGANIC-MATTER TRANSPORT; ATLANTIC TIME-SERIES; FECAL PELLETS; EQUATORIAL PACIFIC; CARBON FLUXES; POC EXPORT; PO-210/PB-210; DISEQUILIBRIA; INTERANNUAL VARIABILITY; SEASONAL PATTERNS; PARTICLE EXPORT;
D O I
10.1016/j.jenvrad.2014.02.009
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Depth profiles of Po-210 and Pb-210 activity and phytoplankton and zooplankton abundance were collected during two cruises along the Canadian time-series Line P in the Northeast Subarctic Pacific (ranging from 48o39 N to 50o00 N and 126040 W to 145o00 W) in August 2010 and February 2011 to evaluate connections between the planktonic community and distributions of these radionuclides in the upper 500 m of the water column. Statistical analysis indicates that Po-210 is more effectively removed from the surface ocean when large (>0.1 mg ind(-1) dry wt) zooplankton dominate, and is less effectively scavenged when the picoplankton Synechococcus is present at high concentrations (>1 x 10(5) cells ml(-1)). While the zooplankton field data are consistent with previous lab studies and field observations, the phytoplankton results seem to conflict with recent evidence that small cells may contribute significantly to export in other oligotrophic regions. Differences in ecosystem mechanisms between the Subarctic Pacific and other oligotrophic systems that limit the contribution of small cells to sinking flux remain to be identified. (C) 2014 Elsevier Ltd. All rights reserved.
引用
收藏
页码:390 / 401
页数:12
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