首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Aliphatic hydrocarbon concentrations in short sediment cores from the southern Okinawa Trough: Implications for lipid deposition in a complex environment
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Aliphatic hydrocarbon concentrations in short sediment cores from the southern Okinawa Trough: Implications for lipid deposition in a complex environment

机译:冲绳海槽南部短沉积岩心中的脂肪烃浓度:对复杂环境中脂质沉积的影响

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摘要

Seven short sediment cores from the southern Okinawa Trough were collected and analyzed for the aliphatic hydrocarbon concentrations by capillary gas chromatography to explore the deposition of hydrocarbons to this area. For all cores studied, ratios of Σhydrocarbons/TOC, (nC_(27)+nC_(29)+nC_(31))/TOC, terrigenous/aquatic, and diploptene/ΣC_(25–33) n-alkanes fluctuated around a mean value with coefficients of variation ranging from 9.0% to 19.7%, 4.9% to 20.0%, 27.3% to 129%, and 3.8% to 163%, respectively. For the nC_(31)/(nC_(27)+nC_(29)+nC_(31)) ratio, only station 21 showed fluctuation. Moreover, the carbon preference indexes in the C25–C33 n-alkane range also exhibited fluctuating values with coefficients of variation of 1.9–14.4%. These results indicate that concentrations of hydrocarbon inputs to the sampling sites vary with time; this may result from complex current flow and sediment transport, leading to variable lipid deposition. In addition, significant correlation between diploptene (hop-22(29)-ene) and higher plant n-alkanes was found for cores 21, 42 and 46, indicating that diploptene was predominantly from higher plant sources. However, no correlation between diploptene and higher plant n-alkanes was found for cores 20, 36, 43 and 44; autochthonous sources of diploptene in these cores were quite probable.
机译:收集了来自冲绳海槽南部的七个短沉积岩心,并通过毛细管气相色谱分析了脂肪烃的浓度,以探索该地区的碳氢化合物沉积。对于所有研究的岩心,Σ烃/ TOC,(nC_(27)+ nC_(29)+ nC_(31))/ TOC,陆源/水生和二萜/ΣC_(25-33)正构烷烃之比均值波动变异系数分别为9.0%至19.7%,4.9%至20.0%,27.3%至129%和3.8%至163%。对于nC_(31)/(nC_(27)+ nC_(29)+ nC_(31))的比率,仅站21出现波动。此外,C25–C33正构烷烃范围内的碳偏好指数也表现出波动值,变异系数为1.9–14.4%。这些结果表明,输入到采样点的碳氢化合物的浓度随时间变化。这可能是由于复杂的电流和沉积物传输所致,从而导致脂质沉积变化。此外,发现核心21、42和46的二萜烯(hop-22(29)-ene)与高级植物正构烷烃之间存在显着相关性,这表明二萜烯主要来自高级植物。然而,对于核心20、36、43和44,没有发现二萜与高级植物正构烷烃之间的相关性。这些岩心中双萜的自生来源很可能。

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