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Source and implication of fatty acids in surface sediments from the Pearl River Mouth Basin, South China Sea

机译:南海珠江口盆地表层沉积物中脂肪酸的来源及其意义

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摘要

Present study consists the fatty acid composition of five samples of Site 4B surface sediment from the Pearl River Mouth Basin in the South China Sea. Total fatty acid (TFA) content of the ranged from 5.14 mu g/g to 8.99 mu g/g (mu g FA/g dry sediment), and the carbon number ranged from C-12 to C-32. The fatty acids detected in the five surface samples include the normal saturated fatty acids, branched-chain fatty acids, monounsaturated fatty acids, polyunsaturated fatty acids, and isoprenoid acids. Short-chain fatty acids in the normal saturated fatty acids were mainly from the marine microorganisms, whereas the long-chain fatty acids were from terrigenous higher plants. The higher concentration of short-chain fatty acids relative to the long-chain fatty acids indicates that the input from marine microorganisms in the surface sediment is far greater than that from terrigenous higher plants. The branched-chain fatty acids i/a15:0, i/a17:0, and 1 Ome16:0 and the monounsaturated fatty acids 18:1(09 and 16:10)9 were mainly synthesized by sulfate-reducing bacteria, whereas 16:1 omega 7 was from the sulfur-oxidizing bacteria. Relative content of the different fatty acids indicate that the surface sediment is dominated by a reductive environment. In addition, eight isoprenoid acids including phytanic acid, 17 beta(H),21 beta(H)-32-bi-homohopanoic acid, and pristane acid were detected in the surface sediment, and they mainly originated from chlorophyll a and bacteria.
机译:目前的研究包括来自南海珠江口盆地的五个站点4B地表沉积物样品的脂肪酸组成。总脂肪酸(TFA)含量为5.14μg/ g至8.99μg/ g(μgFA / g干沉积物),碳数为C-12至C-32。在五个表面样品中检测到的脂肪酸包括正常的饱和脂肪酸,支链脂肪酸,单不饱和脂肪酸,多不饱和脂肪酸和类异戊二烯酸。正常饱和脂肪酸中的短链脂肪酸主要来自海洋微生物,而长链脂肪酸则来自陆生高等植物。相对于长链脂肪酸而言,短链脂肪酸的浓度更高,这表明来自海洋微生物的表面沉积物中的输入远远大于来自陆生高等植物的输入。支链脂肪酸i / a15:0,i / a17:0和1 Ome16:0和单不饱和脂肪酸18:1(09和16:10)9主要由硫酸盐还原菌合成,而16 1:1Ω7来自硫氧化细菌。不同脂肪酸的相对含量表明表面沉积物以还原性环境为主。此外,在表面沉积物中检测到八种类异戊二烯酸,包括植烷酸,17 beta(H),21 beta(H)-32-双-高硼酸和p烷酸,它们主要源自叶绿素a和细菌。

著录项

  • 来源
    《Indian Journal of Marine Sciences》 |2015年第10期|1528-1539|共12页
  • 作者单位

    Chinese Acad Sci, Guangzhou Inst Energy Convers, Key Lab Gas Hydrate, Guangzhou 510640, Guangdong, Peoples R China;

    Chinese Acad Sci, Key Lab Marginal Sea Geol, South China Sea Inst Oceanol, Guangzhou 510301, Guangdong, Peoples R China;

    Zhejiang Univ, Dept Geosci, Hangzhou 310037, Zhejiang, Peoples R China;

    Chinese Acad Sci, Guangzhou Inst Energy Convers, Key Lab Gas Hydrate, Guangzhou 510640, Guangdong, Peoples R China;

    Chinese Acad Sci, Guangzhou Inst Energy Convers, Key Lab Gas Hydrate, Guangzhou 510640, Guangdong, Peoples R China;

    Chinese Acad Sci, Guangzhou Inst Energy Convers, Key Lab Gas Hydrate, Guangzhou 510640, Guangdong, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Fatty acids; Carbon isotopic; South China Sea; Pearl River Mouth Basin;

    机译:脂肪酸;碳同位素;南海;珠江口盆地;

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