CAS Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, PR China; Laboratory for Marine Ecology and Environmental Sciences, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, PR China; University of Chinese Academy of Sciences, Beijing 100049, PR China; Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, PR China.
CAS Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, PR China; Laboratory for Marine Ecology and Environmental Sciences, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, PR China; University of Chinese Academy of Sciences, Beijing 100049, PR China; Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, PR China.
Ecotoxicol Environ Saf. 2019 Jan 15;167:259-268. doi: 10.1016/j.ecoenv.2018.10.011. Epub 2018 Oct 18.
The composition, distribution, indexes and budget of saturated lipid biomarker aliphatic hydrocarbons (AHs) in sediments of the East China Sea (ESC) were analyzed to identify their indications and sources. The resolved n-alkane (R) contents were 0.70-2.89 μg/g, with long-chain n-alkanes as the dominant composition in the ECS. The high R values mainly appeared at south inner shelf and north outer upwelling area, corresponding to the high mud, total organic carbon (TOC) and Chl a contents there. The composition, distribution pattern, combined with indexes of AHs, suggested no petroleum contamination and predominant biogenic sources in the ECS. The biogenic sources mainly were the mixed terrestrial higher plant, marine plankton and bacteria and aquatic macrophyte origins. Biotic source apportionment suggested that terrestrial higher plants were the dominant source of AHs, followed by marine planktons, with the lowest of submerged/floating macrophytes. Quantitative evaluation of R sources suggested that the Changjiang River input was the primary terrestrial contributor, accounting for 67.9% of total terrestrial input. The burial flux of R was 1.11 × 10 t/yr, with inner shelf and estuary as main accumulation areas. Although there was a huge amount of R influx from terrestrial and marine sources, only 9.8% could be preserved in sediments.
分析了东海(ESC)沉积物中饱和脂质生物标志物脂肪族烃(AHs)的组成、分布、指标和预算,以确定其指示物和来源。解析烷烃(R)含量为 0.70-2.89μg/g,长链烷烃是 ESC 的主要组成部分。高 R 值主要出现在南内架和北外上升流区,与那里的高泥、总有机碳(TOC)和 Chl a 含量相对应。AHs 的组成、分布模式以及指标表明,东海没有石油污染,主要是生物来源。生物来源主要来自混合陆地高等植物、海洋浮游生物和细菌以及水生大型植物。生物源分配表明,陆地高等植物是 AHs 的主要来源,其次是海洋浮游生物,水生大型植物的来源最低。R 源的定量评估表明,长江输入是主要的陆地贡献者,占总陆地输入的 67.9%。R 的埋藏通量为 1.11×10 t/yr,以内架和河口为主要堆积区。尽管有大量的 R 从陆地和海洋来源输入,但只有 9.8%可以在沉积物中保存下来。