Sources of polycyclic aromatic hydrocarbons in marine sediments from southern and northern areas of the Norwegian continental shelf

被引:38
|
作者
Boitsov, Stepan [1 ]
Petrova, Vera [2 ]
Jensen, Henning K. B. [3 ]
Kursheva, Anna [2 ]
Litvinenko, Ivan [2 ]
Klungsoyr, Jarle [1 ]
机构
[1] IMR, N-5817 Bergen, Norway
[2] Academician IS Gramberg All Russia Res Inst Geol, St Petersburg, Russia
[3] Geol Survey Norway NGU, Trondheim, Norway
关键词
PAH; Sediments; Biomarkers; Hopanes; Skagerrak; Barents Sea; WESTERN BARENTS SEA; FRASER-RIVER BASIN; POLYAROMATIC HYDROCARBONS; RISK-ASSESSMENT; BALTIC SEA; PAH; SAMPLES; BIOACCUMULATION; IDENTIFICATION; CONTAMINANTS;
D O I
10.1016/j.marenvres.2013.03.006
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Variability in levels and sources of polycyclic aromatic hydrocarbons (PAM) in sediments from one large sea area off the coast of northern Norway ("North area", NA) have been compared to similar data from another large area off the coast of southern Norway ("South area", SA). Samples from NA were collected at the Norwegian continental shelf in south-western Barents Sea and north-eastern Norwegian Sea. Samples from SA were from the Norwegian Trench and the Skagerrak. Sediment cores have been dated, characterised by grain size distribution (GS) and organic carbon content (TOC), and the composition of PAH and geochemical biomarkers (alkanes and triterpanes) studied to provide an insight into the different sources of PAH. Generally, PAH levels are higher in sediments from SA compared to NA. A mixture of pyrogenic and petrogenic sources contribute to PAH levels in SA, while the contents of petrogenic PAH is negligible in surface sediments in NA. At some locations in NA, petrogenic PAH levels are elevated in the deepest sediment layers from pre-industrial times, indicating a natural input of petroleum through seepage. Occurrence of elevated levels of microbial hopanoids (hopenes) in the deepest sediment layers at some locations both in the north and the south indicate the presence of petroleum. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:73 / 84
页数:12
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