印度洋东经90°海岭表层沉积物浮游有孔虫分布特征及其影响因素

胡昱洁, 李小艳, 宋召军, 张彬, 殷征欣, 张辉, 胡倩男, 丁旋. 印度洋东经90°海岭表层沉积物浮游有孔虫分布特征及其影响因素[J]. 海洋地质与第四纪地质, 2023, 43(1): 105-117. doi: 10.16562/j.cnki.0256-1492.2022032102
引用本文: 胡昱洁, 李小艳, 宋召军, 张彬, 殷征欣, 张辉, 胡倩男, 丁旋. 印度洋东经90°海岭表层沉积物浮游有孔虫分布特征及其影响因素[J]. 海洋地质与第四纪地质, 2023, 43(1): 105-117. doi: 10.16562/j.cnki.0256-1492.2022032102
HU Yujie, LI Xiaoyan, SONG Zhaojun, ZHANG Bin, YIN Zhengxin, ZHANG Hui, HU Qiannan, DING Xuan. Distribution and influencing factors of planktonic foraminifera in surface sediments of the Ninetyeast Ridge in Indian Ocean[J]. Marine Geology & Quaternary Geology, 2023, 43(1): 105-117. doi: 10.16562/j.cnki.0256-1492.2022032102
Citation: HU Yujie, LI Xiaoyan, SONG Zhaojun, ZHANG Bin, YIN Zhengxin, ZHANG Hui, HU Qiannan, DING Xuan. Distribution and influencing factors of planktonic foraminifera in surface sediments of the Ninetyeast Ridge in Indian Ocean[J]. Marine Geology & Quaternary Geology, 2023, 43(1): 105-117. doi: 10.16562/j.cnki.0256-1492.2022032102

印度洋东经90°海岭表层沉积物浮游有孔虫分布特征及其影响因素

  • 基金项目: 全球变化与海气相互作用专项“东印度洋 IND-CJ04 区块海底底质和底栖生物调查”(GASI-02-IND-CJ04)
详细信息
    作者简介: 胡昱洁(1999—),女,硕士研究生,主要从事海洋沉积学研究,E-mail:huyujie0216@163.com
    通讯作者: 李小艳(1979—),女,副研究员,研究方向为微体古生物学,古海洋学,E-mail:lixiaoyan@fio.org.cn
  • 中图分类号: P736.21

Distribution and influencing factors of planktonic foraminifera in surface sediments of the Ninetyeast Ridge in Indian Ocean

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  • 对东印度洋90°海岭附近海域82个表层沉积物样品中的浮游有孔虫进行鉴定统计分析,揭示了研究区表层沉积物中浮游有孔虫区域分布特征,并对其影响因素进行了初步探讨。研究表明,东印度洋90°海岭附近海域表层沉积物中浮游有孔虫呈现典型的热带-亚热带组合特征,共鉴定出浮游有孔虫30种。运用聚类分析,得到3个浮游有孔虫组合:组合类群I主要分布在5°~10°N的孟加拉湾南部开阔海域,主要种属包括Globigerinoides sacculiferGlobigerinoides ruberNeogloboquadrina dutertrei,体现了生产力及海水盐度对有孔虫组合的影响;组合类群II主要在5°N至5°S,沿东经90°海岭分布。主要种属包括Globigerinoides ruber,Globorotalia menardii,Neogloboquadrina dutertrei,体现了水深及生产力对有孔虫组合的影响;组合类群III对称分布在组合类群II两侧水深较深的海域,主要种属包括Globorotalia tumidaGloborotalia menardiPulleniatina obliquiloculata,体现了水深对有孔虫组合特征的影响。根据有孔虫组合类群分布特征,推断水深、盐度及生产力是影响本海域浮游有孔虫分布的最主要因素。

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  • 图 1  研究区表层海水盐度及磷酸盐含量分布图

    Figure 1. 

    图 2  研究区表层沉积物取样站位及等深线图

    Figure 2. 

    图 3  浮游有孔虫丰度(a)和底栖有孔虫丰度(b)分布图

    Figure 3. 

    图 4  浮游有孔虫简单分异度(a)和复合分异度分布图(b)

    Figure 4. 

    图 5  表层沉积物中浮游有孔虫碎壳率分布图

    Figure 5. 

    图 6  表层沉积物中浮游有孔虫优势种易溶种分布图

    Figure 6. 

    图 7  表层沉积物中浮游有孔虫优势种抗溶种分布图

    Figure 7. 

    图 8  表层沉积物浮游有孔虫属种聚类分区图

    Figure 8. 

    图 9  东印度洋表层沉积物聚类分析谱系图

    Figure 9. 

    图 10  表层沉积物有孔虫丰度及相对含量随水深变化图

    Figure 10. 

    表 1  研究区表层样浮游有孔虫优势种百分含量统计

    Table 1.  Statistical table of relative abundance of dominant planktonic foraminifera in surface sediments in the study area

    属种名最大值/%最小值/%平均值/%
    Globorotalia menardii42.902.4113.64
    Globigerinoides ruber

    31.730.0013.54
    Globigerinoides sacculifer26.160.0012.15
    Neogloboquadrina dutertrei19.280.8310.33
    Globorotalia tumida65.560.0010.20
    Pulleniatina obliquiloculata24.330.009.01
    Globigerinita glutinata16.950.005.21
    下载: 导出CSV

    表 2  各组浮游有孔虫主要种属含量分布

    Table 2.  Content distribution of main species of planktonic foraminifera in each group

    种属组合I组合II组合III
    Globigerinoides ruber16.30%19.68%3.10%
    Globigerinoides sacculifer17.31%15.54%4.80%
    Globorotalia menardii10.04%10.23%21.15%
    Neogloboquadrina dutertrei13.32%10.22%8.87%
    Pulleniatina obliquiloculata9.12%7.21%11.01%
    Globoquadrina conglomerata6.15%6.17%2.23%
    Globigerina bulloides4.79%3.85%1.49%
    Globigerinita glutinata4.68%6.77%2.44%
    Globorotalia tumida1.24%1.26%27.04%
    下载: 导出CSV
  • [1]

    丁旋, 方念乔, 万晓樵. 孟加拉湾晚第四纪的季风气候及其古海洋学记录[J]. 现代地质, 2000, 14(3):295-300 doi: 10.3969/j.issn.1000-8527.2000.03.010

    DING Xuan, FANG Nianqiao, WAN Xiaoqiao. Monsoon climate and its paleoceanographic records of the Bay of Bengal during Late Quaternary [J]. Geoscience, 2000, 14(3): 295-300. doi: 10.3969/j.issn.1000-8527.2000.03.010

    [2]

    吴雨. 安达曼海MIS25期以来浮游有孔虫记录的印度季风演化[D]. 中国地质大学(北京)硕士学位论文, 2020.

    WU Yu. The evolution of Indian monsoon recorded by planktonic foraminifera since the MIS25 Period in the Andaman Sea[D]. Master Dissertation of China University of Geosciences (Beijing), 2020.

    [3]

    宣莉莉. 热带东印度洋上层海洋环流及其与孟加拉湾水交换的季节变化研究[D]. 国家海洋局第三海洋研究所硕士学位论文, 2013.

    XUAN Lili. Seasonal variation of the upper ocean circulation in the eastern tropical Indian Ocean and its water exchange with the Bay of Bengal[D]. Master Dissertation of Third Institute of Oceanography, State Oceanic Administration, 2013.

    [4]

    魏华玲. 3.5Ma来赤道东经90°海岭远洋记录与重大环境事件[D]. 中国地质大学(北京)硕士学位论文, 2006.

    WEI Hualing. Pelagic recards from the equatorial ninetyeast ridge and significant environmental events during past 3.5 million years[D]. Master Dissertation of China University of Geosciences (Beijing), 2006.

    [5]

    丁旋, 方念乔. 东北印度洋区BAR9427岩心末次冰期以来的古季风活动记录[J]. 地球科学:中国地质大学学报, 2006, 31(6):765-772

    DING Xuan, FANG Nianqiao. Records of Paleo-monsoon of core BAR9427 in northeastern Indian Ocean during Last Glaciation [J]. Earth Science:Journal of China University of Geosciences, 2006, 31(6): 765-772.

    [6]

    王颖. 东印度洋中部缺氧区的季节变化特征[D]. 国家海洋局第一海洋研究所硕士学位论文, 2018.

    WANG Ying. Seasonal variation of hypoxic zone in the central eastern Indian Ocean[D]. Master Dissertation of the First Institute of Oceanography, State Oceanic Administration, 2018.

    [7]

    Bé A W H. An ecological, zoogeographic and taxonomic review of recent planktonic foraminifera [J]. Oceanic Micropaleontology, 1977, 1: 1-100.

    [8]

    Fairbanks R G, Sverdlove M, Free R, et al. Vertical distribution and isotopic fractionation of living planktonic foraminifera from the Panama Basin [J]. Nature, 1982, 298(5877): 841-844. doi: 10.1038/298841a0

    [9]

    Jian Z M, Wang P X, Saito Y, et al. Holocene variability of the Kuroshio Current in the Okinawa Trough, northwestern Pacific Ocean [J]. Earth and Planetary Science Letters, 2000, 184(1): 305-319. doi: 10.1016/S0012-821X(00)00321-6

    [10]

    吴永华, 程振波, 石学法, 等. 琉球群岛东部海区表层沉积物中浮游有孔虫分布及指示意义[J]. 海洋地质与第四纪地质, 2007, 27(6):1-7

    WU Yonghua, CHENG Zhenbo, SHI Xuefa, et al. Distribution of planktonic foraminifera in surface sediments from sea area East of the Ryukyu Islands and their indications [J]. Marine Geology & Quaternary Geology, 2007, 27(6): 1-7.

    [11]

    张玲芝, 向荣, 唐灵刚, 等. 安达曼海浮游有孔虫群落对全新世海洋环境变化的响应[J]. 热带海洋学报, 2019, 38(6):51-61

    ZHANG Lingzhi, XIANG Rong, TANG Linggang, et al. Response of planktonic foraminifera to Holocene marine environmental changes in the Andaman Sea [J]. Journal of Tropical Oceanography, 2019, 38(6): 51-61.

    [12]

    Thunell R C. Distribution of recent planktonic foraminifera in surface sediments of the Mediterranean Sea [J]. Marine Micropaleontology, 1978, 3(2): 147-173. doi: 10.1016/0377-8398(78)90003-8

    [13]

    Fairbanks R G, Wiebe P H, Bé A W H. Vertical distribution and isotopic composition of living planktonic foraminifera in the western North Atlantic [J]. Science, 1980, 207(4426): 61-63. doi: 10.1126/science.207.4426.61

    [14]

    郑执中, 郑守仪. 南海北部的浮游有孔虫[J]. 海洋与湖沼, 1964, 6(1):38-73

    ZHENG Zhizhong, ZHENG Shouyi. The planktonic foraminifera of the northern South China Sea [J]. Oceanologia et Limnologia Sinica, 1964, 6(1): 38-73.

    [15]

    赵泉鸿, 汪品先. 南海第四纪古海洋学研究进展[J]. 第四纪研究, 1999, 19(6):481-501 doi: 10.3321/j.issn:1001-7410.1999.06.001

    ZHAO Quanhong, WANG Pinxian. Progress in quaternary paleoceanography of the South China sea: A review [J]. Quaternary Sciences, 1999, 19(6): 481-501. doi: 10.3321/j.issn:1001-7410.1999.06.001

    [16]

    涂霞. 南海东北部海区有孔虫的分布及其与海洋环境的关系[J]. 热带海洋, 1983, 2(1):11-19

    TU Xia. Distribution and habitats of foraminifera in bottom sediments of the northeastern South China Sea [J]. Tropical Oceanography, 1983, 2(1): 11-19.

    [17]

    孙荣涛, 李铁刚, 曹奇原, 等. 冲绳海槽北部表层沉积物中浮游有孔虫的分布与海洋环境[J]. 海洋与湖沼, 2003, 34(5):511-518 doi: 10.3321/j.issn:0029-814X.2003.05.006

    SUN Rongtao, LI Tiegang, CAO Qiyuan, et al. Planktonic Foraminifera distributions in surface sediments of the northern Okinawa trough and their marine environment interpretation [J]. Oceanologia et Limnologia Sinica, 2003, 34(5): 511-518. doi: 10.3321/j.issn:0029-814X.2003.05.006

    [18]

    Berger W H. Planktonic Foraminifera: selective solution and paleoclimatic interpretation [J]. Deep Sea Research and Oceanographic Abstracts, 1968, 15(1): 31-43. doi: 10.1016/0011-7471(68)90027-2

    [19]

    齐泽坤, 徐继尚, 李广雪, 等. 热带西太平洋碳酸盐溶跃深度及其变化规律[J]. 地质学报, 2020, 94(12):3852-3863 doi: 10.3969/j.issn.0001-5717.2020.12.022

    QI Zekun, XU Jishang, LI Guangxue, et al. The variation of carbonate lysocline depth in the western tropical Pacific Ocean [J]. Acta Geologica Sinica, 2020, 94(12): 3852-3863. doi: 10.3969/j.issn.0001-5717.2020.12.022

    [20]

    郑连福, 陈荣华. 浮游有孔虫与深海碳酸盐溶解作用[J]. 海洋石油, 1982, 2(5):41-49

    ZHENG Lianfu, CHEN Ronghua. Planktonic foraminifera and deep-sea carbonate dissolution [J]. Offshore Oil, 1982, 2(5): 41-49.

    [21]

    张江勇, 赵利, 李波, 等. 南海与台湾岛东部海域浅地层碳酸盐旋回[J]. 中国地质, 2020, 47(5):1486-1500

    ZHANG Jiangyong, ZHAO Li, LI Bo, et al. Carbonate cycle in sub-bottom strata in the South China Sea and the East Sea area of Taiwan Island [J]. Geology in China, 2020, 47(5): 1486-1500.

    [22]

    丁旋, 方念乔, 陈萍. 等. 孟加拉湾深海氧同位素2、3期上升流活动: 北印度洋冬季风的实证[J]. 第四纪研究, 2003, 23(1):53-59 doi: 10.3321/j.issn:1001-7410.2003.01.006

    DING Xuan, FANG Nianqiao, CHEN Ping, et al. Upwelling actions in the Bay of Bengal during marine isotope stages 2 and 3: evidence for Indian winter monsoon [J]. Quaternary Sciences, 2003, 23(1): 53-59. doi: 10.3321/j.issn:1001-7410.2003.01.006

    [23]

    Ding X, Bassinot F, Guichard F, et al. Distribution and ecology of planktonic foraminifera from the seas around the Indonesian Archipelago [J]. Marine Micropaleontology, 2006, 58(2): 114-134. doi: 10.1016/j.marmicro.2005.10.003

    [24]

    魏华玲, 方念乔, 丁旋, 等. 赤道东经90°海岭3.5Ma以来远洋记录反映的重大环境事件[J]. 地质通报, 2007, 26(12):1627-1632 doi: 10.3969/j.issn.1671-2552.2007.12.016

    WEI Hualing, FANG Nianqiao, DING Xuan, et al. Major environmental events reflected by pelagic records since 3.5 Ma BP in the Ninetyeast Ridge at the equator [J]. Geological Bulletin of China, 2007, 26(12): 1627-1632. doi: 10.3969/j.issn.1671-2552.2007.12.016

    [25]

    刘勇勤. 晚中新世以来东北印度洋赤道海岭的远洋沉积记录及其环境意义[D]. 中国地质大学(北京)硕士学位论文, 2003.

    LIU Yongqin. Pelagic sedimentary records and its palaeoenvironmental implication in Ninetyeast Ridge of the NE Indian Ocean since Middle Miocene[D]. Master Dissertation of China University of Geosciences (Beijing), 2003.

    [26]

    Symphonia T, Nathan D S. Planktonic Foraminifera from the Offshore segment between Chennai and Cuddalore, Bay of Bengal, India [J]. International Journal of Science and Research, 2014, 3(8): 1222-1225.

    [27]

    Gandhi M S, Solai A. Statistical studies and ecology of benthic foraminifera from the depositional environment; a case study between Mandapam and Tuticorin, South East Coast of India [J]. International Journal of Research and Reviews, 2010, 5(1): 86-94.

    [28]

    李日辉, 孙荣涛, 陈晓辉. 渤海南部表层沉积物有孔虫埋藏群组合特征与海洋环境[J]. 海洋地质与第四纪地质, 2017, 37(3):17-27

    LI Rihui, SUN Rongtao, CHEN Xiaohui. Comparison of foraminiferal taphocoenose assemblages with marine environmental parameters of the surface sediments from southern Bohai sea [J]. Marine Geology & Quaternary Geology, 2017, 37(3): 17-27.

    [29]

    张洁. 西南印度洋晚更新世以来的浮游有孔虫组合及其环境意义[D]. 中国地质大学(北京)硕士学位论文, 2017.

    ZHANG Jie. Foraminiferal Assemblages in the Southwest Indian ocean sediments and their paleoenrivonmental implications since Late Pleistocene[D]. Master Dissertation of China University of Geosciences (Beijing), 2017.

    [30]

    Anbuselvan N, Senthil Nathan D. Distribution and environmental implications of planktonic foraminifera in the surface sediments of southwestern part of Bay of Bengal, India [J]. Journal of Sedimentary Environments, 2021, 6(2): 213-235. doi: 10.1007/s43217-021-00053-8

    [31]

    Kennet J P, Srinivasan M S. Neogene Planktonic Foraminifera: A Phylogenetic Atlas[M]. Hutchinson Ross Publishing Company, 1983: 265.

    [32]

    Le J N, Shackleton N J. Carbonate dissolution fluctuations in the western equatorial Pacific during the Late Quaternary [J]. Paleoceanography, 1992, 7(1): 21-42. doi: 10.1029/91PA02854

    [33]

    Oda M, Takemoto A. Planktonic foraminifera and paleoceanography in the domain of the Kuroshio current around Japan during the last 20, 000 years [J]. The Quaternary Research (Daiyonki Kenkyu), 1992, 31(5): 341-357. doi: 10.4116/jaqua.31.341

    [34]

    Kawahata H, Nishimura A, Gagan M K. Seasonal change in foraminiferal production in the western equatorial Pacific warm pool: evidence from sediment trap experiments [J]. Deep Sea Research Part II:Topical Studies in Oceanography, 2002, 49(13-14): 2783-2800. doi: 10.1016/S0967-0645(02)00058-9

    [35]

    李两全, 涂霞, 罗又郎, 等. 南海表层沉积物中浮游有孔虫的定量分析[J]. 中国科学B辑, 1992(9):966-971

    LI Liangquan, TU Xia, LUO Youlang, et al. Quantitative analysis of planktonic foraminifera in surface sediments of the South China Sea [J]. Scientia Sinica(Series B), 1992(9): 966-971.

    [36]

    刘志学. 印度洋东经90°海岭更新世晚期的上层海水性质及其古气候意义[D]. 中国地质大学(北京)硕士学位论文, 2016

    LIU Zhixue. Charateristic of the upper sea water in Ninetyeast Ridge and Paleoclimatic implication in the Late Pleistocene[D]. Master Dissertation of China University of Geosciences (Beijing), 2016.

    [37]

    张振芳. 孟加拉湾上新世以来沉积记录及古气候演化[D]. 中国地质大学(北京)博士学位论文, 2003.

    ZHANG Zhenfang. Sedimentary records and paleoclimate evolution of bay of Bengal since Pliocene Time[D]. Doctor Dissertation of China University of Geosciences (Beijing), 2003.

    [38]

    Huber B T. Modern planktonic foraminifera [J]. Journal of Foraminiferal Research, 1990, 20(1): 90-91. doi: 10.2113/gsjfr.20.1.90

    [39]

    赵其渊. 海洋地球化学[M]. 北京: 地质出版社, 1989.

    ZHAO Qiyuan. Marine Geochemistry[M]. Beijing: Geological Publishing House, 1989.

    [40]

    刘振尤. 中印度洋海盆南部中新世以来CCD的演变及意义: 来自微体化石组合和元素地球化学的证据[D]. 南京大学硕士学位论文, 2020.

    LIU Zhenyou. CCD evolution and implications since the Miocene: evidence from nannofossils assemblage and element geochemistry in the south part of Central Indian Ocean Basin[D]. Master Dissertation of Nanjing University, 2020.

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收稿日期:  2022-03-21
修回日期:  2022-05-30
录用日期:  2022-05-30
刊出日期:  2023-02-28

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