The deep-sea as a final global sink of semivolatile persistent organic pollutants? Part I: PCBs in surface and deep-sea dwelling fish of the North and South Atlantic and the Monterey Bay Canyon (California)

被引:111
作者
Froescheis, O
Looser, R
Cailliet, GM
Jarman, WM
Ballschmiter, K
机构
[1] Univ Ulm, Dept Analyt & Environm Chem, D-89081 Ulm, Germany
[2] Moss Landing Marine Labs, Moss Landing, CA 95039 USA
[3] Univ Utah, Civil & Environm Engn Energy & Geosci Inst, Salt Lake City, UT 84108 USA
[4] F Hoffmann La Roche & Co Ltd, Vitamins & Fine Chem Div, CH-4070 Basel, Switzerland
[5] Ctr Technol Assessment Baden Wurttemberg, D-70565 Stuttgart, Germany
关键词
POPs; PCB; deep-sea; Atlantic Ocean; Monterey Bay canyon; bioaccumulation; global sink;
D O I
10.1016/S0045-6535(99)00461-0
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The understanding of the global environmental multiphase distribution of persistent organic pollutants (POPs) as a result of the physico-chemical properties of the respective compounds is well established. We have analysed the results of a vertical transport of POPs from upper water layers (0-200 m) to the deepwater region (>800 m) in terms of the contamination of the biophase in both water layers. The contents of persistent organochlorine compounds like polychlorinated biphenyls (PCBs) in fish living in the upper water layers of the North Atlantic and the South Atlantic, and at the continental shelf of California (Marine Sanctuary Monterey Bay and its deep-sea Canyon) are compared to the levels in deep-sea or bottom dwelling fish within the same geographic area. The deep-sea biota show significantly higher burdens as compared to surface-living species of the same region. There are also indications for recycling processes of POPs - in this case the PCBs - in the biophase of the abyss as well. It can be concluded that the bio- and geo phase of the deep-sea may act similarly as the upper horizons of forest and grasslands on the continents as an ultimate global sink for POPs in the marine environment. (C) 2000 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:651 / 660
页数:10
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