南海西南次海盆柱状沉积物酸类化合物的地球化学特征

王先庆, 陈升, 许兰芳, 彭登. 南海西南次海盆柱状沉积物酸类化合物的地球化学特征[J]. 海洋地质前沿, 2020, 36(7): 17-24. doi: 10.16028/j.1009-2722.2019.170
引用本文: 王先庆, 陈升, 许兰芳, 彭登. 南海西南次海盆柱状沉积物酸类化合物的地球化学特征[J]. 海洋地质前沿, 2020, 36(7): 17-24. doi: 10.16028/j.1009-2722.2019.170
WANG Xianqing, CHEN Sheng, XU Lanfang, PENG Deng. GEOCHEMICAL CHARACTERISTICS OF FATTY ACIDS IN THESOUTHWEST SUB-BASIN OF THE SOUTH CHINA SEA[J]. Marine Geology Frontiers, 2020, 36(7): 17-24. doi: 10.16028/j.1009-2722.2019.170
Citation: WANG Xianqing, CHEN Sheng, XU Lanfang, PENG Deng. GEOCHEMICAL CHARACTERISTICS OF FATTY ACIDS IN THESOUTHWEST SUB-BASIN OF THE SOUTH CHINA SEA[J]. Marine Geology Frontiers, 2020, 36(7): 17-24. doi: 10.16028/j.1009-2722.2019.170

南海西南次海盆柱状沉积物酸类化合物的地球化学特征

  • 基金项目: 国家自然科学基金(91428205,41776056);广东省基础与应用基础研究基金(2020A1515011172)
详细信息
    作者简介: 王先庆(1993—),男,硕士,助理工程师,主要从事海洋地质方面的研究工作. E-mail:wangxq22@mail3.sysu.edu.cn
  • 中图分类号: P736.21

GEOCHEMICAL CHARACTERISTICS OF FATTY ACIDS IN THESOUTHWEST SUB-BASIN OF THE SOUTH CHINA SEA

  • 南海西南次海盆是南海海盆中的一个重要构造单元,了解其沉积物的地球化学信息对于认识南海沉积环境至关重要。采用色谱质谱(GC-MS)方法对南海西南次海盆B3C和C7两个站位沉积柱中的酸类化合物进行研究,结果表明:①南海西南次海盆B3C和C7站位柱状沉积物中的正构脂肪酸呈偶奇优势分布,普遍以n-C16n-C18为主;沉积物主要来源于浮游生物、藻类、细菌等,并有陆源高等植物的贡献。②B3C和B7沉积柱中酸类化合物来源主要以海源为主,总正构脂肪酸含量以及陆源优势正构脂肪酸(n-C24n-C26n-C28)、海源优势正构脂肪酸(n-C12n-C14n-C16)含量在垂向上分布较为稳定,变化波动小,表明该地区的大部分时期沉积环境较为稳定。③总脂肪酸(TFA)和TFA/TOC均表明该区域有机物积累普遍较低,且该处沉积区域处于非透光区和非热液区。

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  • 图 1  采样点位置分布与研究区位置

    Figure 1. 

    图 2  西南次海盆B3C沉积柱正构脂肪酸碳数分布特征

    Figure 2. 

    图 3  西南次海盆C7沉积柱正构脂肪酸碳数分布特征

    Figure 3. 

    图 4  B3C 与C7沉积柱Total n-fatty acids、ΣTer-fatty acids、ΣMar-fatty acids的垂向分布

    Figure 4. 

    表 1  西南次海盆B3C沉积柱正构脂肪酸含量/(ng/g)

    Table 1.  Concentration (ng/g sed. dry weight) of n-fatty acids in B3C core sediments of the Southwest Sub-Basin

    化合物深度/cm
    2060100140180220300340460
    n-C14 494.8 473.1 244.6 377.3 351.3 391.3 274.5 121.1 226.5
    n-C15 196.5 161.9 95.9 129.4 112.5 134.3 102.7 61.6 124.8
    n-C16 3 751.7 2 252.5 2 556.4 2 008.7 1 632.2 1 964.7 7 028.0 686.8 1 082.7
    n-C17 212.1 162.8 114.5 126.5 115.3 130.6 127.3 60.5 96.1
    n-C18 1 922.1 935.9 1714 899.0 831.9 861.9 3 516.8 431.3 646.7
    n-C19 94.7 67.9 49.9 59.1 49.8 54.5 37.4 51.2 76.8
    n-C20 403.5 266.6 258.2 264.5 253.5 201.7 152.9 252.3 586.4
    n-C21 71.6 39.9 37.3 38.4 41.6 102.1 21.1 67.8 123.8
    n-C22 391.5 155.2 205.4 161.4 225.0 13.4 84.0 251.3 485.7
    n-C23 54.6 22.2 26.8 20.8 33.8 37.0 47.9 42.1 149.5
    n-C24 273.9 73.8 134.9 74.9 195.2 N.D. 46.9 154.4 620.5
    n-C25 36.9 10.2 17.3 8.4 25.7 N.D. N.D. 24.2 175.1
    n-C26 192.4 24.5 61.1 20.6 119.6 N.D. N.D. 74.3 563.0
    n-C27 20.6 4.1 5.0 3.1 12.5 N.D. N.D. 13.0 161.6
    n-C28 65.4 7.6 11.3 4.2 27.9 N.D. N.D. 28.3 509.7
    n-C29 N.D. N.D. N.D. N.D. N.D. N.D. N.D. N.D. 124.5
    n-C30 N.D. N.D. N.D. N.D. N.D. N.D. N.D. N.D. 289.0
    n-C31 N.D. N.D. N.D. N.D. N.D. N.D. N.D. N.D. 40.4
    n-C32 N.D. N.D. N.D. N.D. N.D. N.D. N.D. N.D. 75.7
    Total n-fatty acids 8 182.1 4 658.1 5 530.4 4 196.4 4 027.8 3 891.6 1 1439.5 2 320.1 6 158.4
    ΣTer-fatty acids 531.7 105.8 207.3 99.6 342.6 N.D. N.D. 257.0 1 693.2
    ΣMar-fatty acids 4 246.4 2 725.6 2 801.0 2 386.1 1 983.5 2 356.0 7 302.5 808.0 1 309.2
    注:ΣTer-fatty acids— ΣC24+26+28;ΣMar-fatty acids— ΣC12+14+16;N.D.—未检测到
    下载: 导出CSV

    表 2  西南次海盆C7沉积柱正构脂肪酸含量/(ng/g)

    Table 2.  Concentration (ng/g sed.dry weight) of n-fatty acids in C7 core sediments of the Southwest Sub-Basin

    化合物深度/cm
    20 60 100 140 180 220 260 300 340 380 420 460
    n-C14 834.1 459.5 436.8 397.5 382.9 387.1 312.8 267.0 481.6 478.4 422.2 609.4
    n-C15 172.4 111.1 129.7 134.8 106.4 117.0 92.1 72.1 128.7 247.7 137.4 150.3
    n-C16 4 425.7 1 888.2 5 529.6 2 344.5 2 245.6 2 446.0 3 365.2 2 818.3 2 842.8 2 561.6 2 523.3 3 279.3
    n-C17 193.5 134.4 172.4 150.7 114.7 138.6 131.6 84.9 167.9 314.1 137.6 185.4
    n-C18 2 911.5 1 218.8 4 009.5 1 195.9 1 141.8 1 390.5 2 461.2 1 874.4 1 857.2 1 689.8 1 228.6 2 013.9
    n-C19 86.3 68.7 50.6 63.6 49.7 62.7 54.4 31.4 65.7 110.2 49.9 67.5
    n-C20 286.6 292.6 147.3 291.3 280.1 296.4 308.9 148.4 291.0 396.1 188.3 264.4
    n-C21 54.6 53.9 21.5 41.8 40.1 45.3 36.2 19.5 51.7 83.0 31.4 45.8
    n-C22 335.1 367.9 77.4 190.0 276.8 293.8 188.1 95.8 336.2 524.3 121.0 262.0
    n-C23 29.6 42.0 10.7 25.8 34.6 40.3 18.4 12.2 42.5 78.7 16.2 28.4
    n-C24 118.3 176.1 27.4 105.1 159.5 146.7 60.0 42.8 204.8 270.3 52.3 104.1
    n-C25 13.7 19.3 N.D. 13.1 17.1 31.6 N.D. N.D. 38.0 37.2 6.3 13.0
    n-C26 16.6 52.1 N.D. 52.7 56.3 54.3 N.D. N.D. 164.3 115.7 13.7 29.5
    n-C27 4.7 4.2 N.D. N.D. N.D. N.D. N.D. N.D. 20.3 N.D. N.D. N.D.
    n-C28 7.9 7.9 N.D. N.D. N.D. N.D. N.D. N.D. 50.1 N.D. N.D. N.D.
    Total n-fatty acids 9 490.5 4 896.9 10 613.2 5 006.9 4 905.7 5 450.4 7 028.8 5 466.7 6 742.8 6 907.3 4 928.0 7 052.9
    ΣTer-fatty acids 142.8 236.1 27.4 157.9 215.8 201.0 60.0 42.8 419.2 386.1 66.0 133.6
    ΣMar-fatty acids 5 259.7 2 347.7 5 966.4 2 742.0 2628.6 2 833.1 3 678.0 3 085.3 3 324.3 3 040.0 2 945.5 3 888.7
    注:ΣTer-fatty acids— ΣC24+26+28;ΣMar-fatty acids— ΣC12+14+16;N.D.—未检测到
    下载: 导出CSV
  • [1]

    姚伯初. 南海南部地区的新生代构造演化[J]. 南海地质研究,1994(6):1-15.

    [2]

    姚伯初. 南海西南海盆的海底扩张及其构造意义[J]. 南海地质研究,1997(9):20-36.

    [3]

    李家彪. 南海大陆边缘动力学: 科学实验与研究进展[J]. 地球物理学报,2011,54(12):2993-3003. doi: 10.3969/j.issn.0001-5733.2011.12.002

    [4]

    李家彪,丁巍伟,吴自银,等. 南海西南海盆的渐进式扩张[J]. 科学通报,2012,57(20):1896-1905.

    [5]

    Hamilton W B. Tectonics of the Indonesia region[J]. US Geological Survey Professional Paper,1979:1078.

    [6]

    Tapponnier P,Peltzer G,Le Dain A Y,et al. Propagating extrusion tectonics in Asia: new insights from simple experiments with plasticine[J]. Geology,1982,10(12):611.

    [7]

    Duan Y. Organic geochemistry of recent marine sediments from the Nansha Sea,China[J]. Organic Geochemistry,2000,31(2/3):159-167. doi: 10.1016/S0146-6380(99)00135-7

    [8]

    Hu J F,Peng P,Chivas A R. Molecular biomarker evidence of origins and transport of organic matter in sediments of the pearl river estuary and adjacent south china sea[J]. Applied Geochemistry,2009,24(9):1666-1676.

    [9]

    Tahir N M,Pang S Y,Simoneit B R T. Distribution and sources of lipid compound series in sediment cores of the southern South China Sea[J]. Environ-mental Science and Pollution Research,2015,22(10):7557-7568.

    [10]

    徐 行,姚永坚,彭 登,等. 南海西南次海盆的地热流特征与分析[J]. 地球物理学报,2018,61(7):2915-2925. doi: 10.6038/cjg2018L0223

    [11]

    Meyers P A,Lallier-Vergés E. Lacustrine sedimentary organic matter records of late quaternary paleoclimates[J]. Journal of Paleolimnology,1999,21(3):345-372. doi: 10.1023/A:1008073732192

    [12]

    Meyers P A. Applications of organic geochemistry to paleolimnological reconstructions: a summary of examples from the laurentian great lakes[J]. Organic Geochemistry,2003,34(2):261-289. doi: 10.1016/S0146-6380(02)00168-7

    [13]

    Cranwell P A. Lipids of aquatic sediments and sedimenting particulates[J]. Progress in Lipid Research,1982,21(4):271-308. doi: 10.1016/0163-7827(82)90012-1

    [14]

    Kattner G,Gercken G,Eberlein K. Development of lipids during a spring plankton bloom in the northern North Sea: I. Particulate fatty acids[J]. Marine Chemistry,1983,14(2):149-162. doi: 10.1016/0304-4203(83)90038-5

    [15]

    Zegouagh Y,Derenne S,Largeau C,et al. Organic matter sources and early diagenetic alterations in Arctic surface sediments (Lena River delta and Laptev Sea, Eastern Siberia,Ⅱ. Molecular and isotopic studies of hydrocarbons[J]. Organic Geochemistry,1998,28(9/10):571-583.

    [16]

    Chuecas L,Riley J P. Component fatty acids of the total lipids of some marine phytoplankton[J]. Journal of the Marine Biological Association of the United Kingdom,1969,49(1):97-116. doi: 10.1017/S0025315400046439

    [17]

    Heras X,Grimalt J O,Albaiges J,et al. Origin and diagenesis of the organic matter in Miocenefreshwater lacustrine phosphates (Cerandya Basin, Eastern Pyrencos)[J]. Organic Geochemistry,1989,14:667-677. doi: 10.1016/0146-6380(89)90046-6

    [18]

    Riebesell U,Revill A T,Holdsworth D G,et al. The effects of varying CO2 concentration on lipid composition and carbon isotope fractionation in Emiliania huxleyi[J]. Geochimica Et Cosmochimica Acta,2000,64(24):4179-4192. doi: 10.1016/S0016-7037(00)00474-9

    [19]

    Ratnayake N P,Suzuki N,Matsubara M. Sources of long chain fatty acids in deep sea sediments from the bering sea and the north pacific ocean[J]. Organic Geochemistry,2005,36(4):531-541.

    [20]

    Naraoka H,Ishiwatari R. Molecular and isotopic abundances of long-chainn-fatty acids in open marine sediments of the western North Pacific[J]. Chemical Geology,2000,165(1):23-36.

    [21]

    Harvey, Rodger H. Fatty acids and sterols as source markers of organic matter in sediments of the North Carolina continental slope[J]. Deep Sea Research Part II: Topical Studies in Oceanography,1994,41(4/6):783-796. doi: 10.1016/0967-0645(94)90048-5

    [22]

    Wakeham S G,Hedges J I,Lee C,et al. Compositions and transport of lipid biomarkers through the water column and surficial sediments of the equatorial Pacific Ocean[J]. Deep Sea Research Part 2:Topical Studies in Oceanography,1997,44(9/10):2131-2162.

    [23]

    Ohkouchi N. Lipids as Biogeochemical Tracers in the Late Quaternary[D].Tokyo: University Tokyo, 2012.

    [24]

    Hedrick D B,Pledger R D,White D C,et al. In situ microbial ecology of hydrothermal vent sediments[J]. FEMS Microbiology Letters,1992,101(1):1-10.

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收稿日期:  2019-08-12
刊出日期:  2020-07-28

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