雅浦海沟北部深渊沉积物中脂肪酸的分布特征

Distribution characteristics of fatty acids in the abyssal sediments of the northern Yap Trench

  • 摘要: 本研究测定了雅浦海沟北部深渊4 435 m(西侧崖壁, D109站位)和4 568 m(东侧崖壁, S02站位)两个柱状沉积物样品中脂肪酸生物标志物的组成和浓度,分析了其来源和分布特征。结果表明,两个沉积物样品中均鉴定出25种脂肪酸,碳原子数为12~24,以中链和短链脂肪酸为主。两个站位沉积物中不同种类和存在形态的脂肪酸的分布特征差异显著,西侧D109站位沉积物的总脂肪酸含量较高,平均浓度为88.4 μg/g,主要以结合态形式存在;东侧S02站位沉积物总脂肪酸的平均含量为66.7 μg/g,主要以游离态形式存在。两个站位表层沉积物脂肪酸的浓度最高,18∶0和16∶0是其中最丰富的脂肪酸。两个站位沉积物的脂肪酸均来源于海洋,包括藻源、细菌源和浮游动物来源等。D109站位和S02站位沉积物脂肪酸的δ13C值低至−136.48‰和−78.83‰,显示存在以甲烷作为碳源进行的微生物生物化学过程。深渊西侧D109站位沉积物中18∶ 1ω7含量较高,受深海热液影响更加显著,脂肪酸在总有机碳中的占比随深度增加而增加,沉积物更加新鲜。两个站位沉积物样品中脂肪酸的含量变化均受到海沟“漏斗效应”、碳酸盐补偿深度变化以及脂肪酸降解等因素的影响。本研究提供了雅浦海沟北部深渊环境中脂肪酸生物标志物的基本信息,有助于更深入地了解有机碳的生物地球化学循环。

     

    Abstract: In this study, the composition and concentration of fatty acid biomarkers in columnar sediment samples at depths of 4 435 m (western cliff, station D109) and 4 568 m (eastern cliff, station S02) from the abyss of the northern Yap Trench were determined, and the sources of the fatty acids and distribution characteristics in the sediment samples were analyzed. The results showed that 25 fatty acids were identified at both sediment samples, with a carbon number of 12-24, mainly in medium-chain and short-chain fatty acids. The distribution characteristics of different types and forms of fatty acids in the sediments of the two stations were significantly different. The total fatty acid content in the sediment from station D109 on the west side was higher, with an average concentration of 88.41 μg/g, mainly in bound form; and the total fatty acid content in the sediment of S02 station on the east side was 66.68 μg/g, mainly in free form. The concentrations of fatty acids in the surface sediments of the two stations were the highest, and 18∶0 and 16∶0 were the most abundant fatty acids. The fatty acids of the sediment from the two stations were derived from the ocean, including algal sources, bacterial sources and zooplankton sources. δ13C values of the fatty acids reached as low as −136.48‰ and −78.83‰ in the sediment from the two stations, indicating the existence of microbial biochemical processes using methane as a carbon source. The content of 18∶1ω7 in the sediments of station D109 on the west side of the abyss was higher, which were more significantly affected by deep-sea hydrothermal fluid, and the proportion of fatty acids in total organic carbon increases with the increase of depth, therefore the sediments of station D109 were fresher. The variations of fatty acid content in the two sediment samples were affected by “funnel effect” of the trench, change of carbonate compensation depth and fatty acid degradation. This study would provide basic information on fatty acid biomarkers in the abyssal environment of the northern Yap Trench, which is helpful for deeper understanding of the biogeochemical cycle of deep-sea organic carbon.

     

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