Wang Guoguang, Peng Jialin, Hao Ting, Feng Lijuan, Liu Qiaoling, Li Xianguo
Key Laboratory of Marine Chemistry Theory and Technology (Ocean University of China), Ministry of Education, Qingdao 266100, China.
Hunan Vocational College of Science and Technology, Changsha 410004, China.
Environ Pollut. 2017 Nov;230:153-162. doi: 10.1016/j.envpol.2017.06.061. Epub 2017 Jun 23.
As an emerging halogenated organic contaminant, Dechlorane Plus (DP) was scarcely reported in marine environments, especially in China. In this work, 35 surface sediments and a sediment core were collected across the Southern Yellow Sea (SYS) to comprehensively explore the spatio-temporal distribution and possible migration pathway of DP. DP concentrations ranged from 14.3 to 245.5 pg/g dry weight in the surface sediments, displaying a seaward increasing trend with the high levels in the central mud zone. This spatial distribution pattern was ascribed to that fine particles with the elevated DP levels were preferentially transported to the central mud zone under hydrodynamic forcing and/or via long-range atmospheric transportation and deposition. DP concentrations in sediment core gradually increased from the mid-1950s to present, which corresponded well with the historical production and usage of DP, as well as the economic development in China. Significantly positive correlation between DP and total organic carbon (TOC) in both surface sediments and sediment core indicated TOC-dependent natural deposition of DP in the SYS. We used multiple biomarkers, for the first time, to explore the potential effects of terrestrial and marine organic matters (TOM and MOM) on DP deposition. The results showed that competition may occur between TOM and MOM for DP adsorption, and MOM was the predominant contributor in controlling DP deposition in the marine sediments from the SYS.
作为一种新兴的卤代有机污染物,十氯联苯(DP)在海洋环境中鲜有报道,尤其是在中国。在本研究中,我们在南黄海采集了35个表层沉积物和1个沉积岩芯,以全面探究DP的时空分布及可能的迁移路径。表层沉积物中DP的浓度范围为14.3至245.5 pg/g干重,呈现出向海增加的趋势,在中部泥质区含量较高。这种空间分布模式归因于在水动力作用下和/或通过远距离大气传输与沉降,含高浓度DP的细颗粒优先被输送到中部泥质区。沉积岩芯中DP的浓度自20世纪50年代中期至今逐渐增加,这与DP的历史生产和使用情况以及中国的经济发展情况高度吻合。表层沉积物和沉积岩芯中DP与总有机碳(TOC)之间均呈显著正相关,表明在南黄海DP的自然沉积依赖于TOC。我们首次使用多种生物标志物来探究陆地和海洋有机物(TOM和MOM)对DP沉积的潜在影响。结果表明,TOM和MOM在吸附DP方面可能存在竞争,且MOM是控制南黄海海洋沉积物中DP沉积的主要因素。