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Anthropogenic Activities Have Contributed Moderately to Increased Inputs of Organic Materials in Marginal Seas off China

机译:人为活动已在一定程度上促进了中国沿海海域有机物质的增加输入

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摘要

Sediment has been recognized as a gigantic sink of organic materials and therefore can record temporal input trends. To examine the impact of anthropogenic activities on the marginal seas off China, sediment cores were collected from the Yellow Sea, the inner shelf of the East China Sea (ECS), and the South China Sea (SCS) to investigate the sources and spatial and temporal variations of organic materials, i.e., total organic carbon (TOC) and aliphatic hydrocarbons. The concentration ranges of TOC were 0.5-1.29, 0.63-0.83, and 0.33-0.85%, while those of Σn-C_(14-35) (sum of n-alkanes with carbon numbers of 14-35) were 0.08-1.5, 0.13-1.97, and 0.35-0.96 μg/g dry weight in sediment cores from the Yellow Sea, ECS inner shelf, and the SCS,respectively. Terrestrial higher plants were an important source of aliphatic hydrocarbons in marine sediments off China. The spatial distribution of Σn-C_(14-35) concentrations and source diagnostic ratios suggested a greater load of terrestrial organic materials in the Yellow Sea than in the ECS and SCS. Temporally, TOC and Σn-C_(14-35) concentrations increased with time and peaked at either the surface or immediate subsurface layers. This increase was probably reflective of elevated inputs of organic materials to marginal seas off China in recent years, and attributed partly to the impacts of intensified anthropogenic activities in mainland China. Source diagnostics also suggested that aliphatic hydrocarbons were mainly derived from biogenic sources, with a minority in surface sediment layers from petroleum sources, consistent with the above-mentioned postulation.
机译:沉积物被认为是有机材料的巨大汇,因此可以记录时间输入趋势。为了研究人为活动对中国沿海海域的影响,从黄海,东海内陆架(ECS)和南海(SCS)收集了沉积物芯,以调查其来源,空间和有机材料的时间变化,即总有机碳(TOC)和脂族烃。 TOC的浓度范围为0.5-1.29、0.63-0.83和0.33-0.85%,而Σn-C_(14-35)(碳原子数为14-35的正构烷烃之和)的浓度范围为0.08-1.5,黄海,ECS内陆架和南海的沉积物芯干重分别为0.13-1.97和0.35-0.96μg/ g干重,陆生高等植物是中国海洋沉积物中脂肪烃的重要来源。 Σn-C_(14-35)浓度和源诊断率的比重表明,黄海中的陆地有机物质的负荷比ECS和SCS更大,暂时,TOC和Σn-C_(14-35)的浓度随时间和这种增加可能反映了近年来中国大陆边缘海域有机物质输入的增加,部分原因是中国大陆人为活动加剧的影响。碳氢化合物主要来自生物来源,石油来源的表层沉积物层很少,与上述假设一致。

著录项

  • 来源
    《Environmental Science & Technology》 |2013年第20期|11414-11422|共9页
  • 作者单位

    State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, People's Republic of China University of the Chinese Academy of Sciences, Beijing 100049, People's Republic of China;

    State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, People's Republic of China University of the Chinese Academy of Sciences, Beijing 100049, People's Republic of China;

    State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, People's Republic of China;

    State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, People's Republic of China;

    Department of Environmental Studies and Sciences and Department of Chemistry, Richardson College for the Environment,University of Winnipeg, Winnipeg, Manitoba, R3B 2E9 Canada;

    State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences,Beijing 100012, People's Republic of China;

    State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, People's Republic of China;

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