LI Tao, XIANG Rong, LI Tuanjie. BENTHIC FORAMINIFERAL DISTRIBUTION IN SURFACE SEDIMENTS OF ZHUJIANG ESTUARY AND ITS ENVIRONMENTAL IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2011, 31(6): 91-98. DOI: 10.3724/SP.J.1140.2011.06091
Citation: LI Tao, XIANG Rong, LI Tuanjie. BENTHIC FORAMINIFERAL DISTRIBUTION IN SURFACE SEDIMENTS OF ZHUJIANG ESTUARY AND ITS ENVIRONMENTAL IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2011, 31(6): 91-98. DOI: 10.3724/SP.J.1140.2011.06091
shu

BENTHIC FORAMINIFERAL DISTRIBUTION IN SURFACE SEDIMENTS OF ZHUJIANG ESTUARY AND ITS ENVIRONMENTAL IMPLICATIONS

  • 1 South China Sea Marine Engineering Surveying Center, SOA, Guangzhou 510300, China;

  • 2 South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China

More Information
  • Received Date: May 25, 2011
  • Revised Date: September 29, 2011
    Graphical Abstract
    • Abstract
  • 134 grab surface sediments were collected from the Zhujiang River estuary with the support of projects 908-01-CJ14 and 908-01-CJ15. In the sediment samples discovered are 106 benthic foraminiferal species belonging to 68 genera and 3 suborders, including 65 Hyaline, 21 porcellaneous and 20 agglutinated species. Benthic foraminiferal species at different locations of the Zhujiang River estuary is examined for abundance, number of species and compound diversity H(S). Foraminiferal abundance, number of species and diversity increased rapidly from the estuary to shallow sea. Foraminiferal abundance changes from several to tens of thousands; number of species changes from 1 to 48 and diversity does from 1 to 3. Factor analysis and Pearson correlation matrix was performed on foraminiferal census data of species content higher than 2% which are present in at least three samples. 3 factors were obtained accounting for 87.2% of the total variance. Two benthic foraminiferal subgroups and one group, Ammonia beccarii-Elphidium nakanokawaense subgroup、Ammonia beccarii-Haplophragmoides canariensis subgroup and Hanzawaia nipponica-Elphidium advenum-Ammonia compressiuscula group, were classified according to factor score of foraminiferal genus. Further, there is some kind of relationship between the foraminaferal distribution and environment. Water depth and salinity control foraminiferal distribution and community structure, and sediment type, water dynamics and sedimentary rate affect its ecological structure as well.
    • FullText(HTML)
    • References (21)
  • [1]
    庄丽华, 李铁刚, 常凤鸣, 等. 东海中陆架晚第四纪底栖有孔虫定量分析[J]. 海洋地质与第四纪地质, 2004, 24(1):43-50.

    [ZHUANG Lihua, LI Tiegang, CHANG Fengming, et al. Quantitative analysis on the benthic foraminifer fauna in late Quaternary period in the North continental shelf of the East China Sea[J]. Marine Geology and Quaternary Geology. 2004, 24(1):43-50.]
    [2]
    汪品先, 章纪军, 赵泉鸿. 东海底质中的有孔虫和介形虫[M]. 北京:海洋出版社, 1988.[WANG Pinxian, ZHANG Jijun, ZHAO Quanhong. Foraminifera and Ostracod in Sediments of the East Sea[M]. Beijing:China Ocean Press, 1988.]
    [3]
    王飞飞, 赵全民, 丁旋, 等. 渤海东北海域有孔虫埋葬群特点与沉积环境的关系[J]. 海洋地质与第四纪地质, 2009, 29(2):9-14.

    [WANG Feifei, ZHAO Quanmin, DING Xuan, et al. Characteristics of the foraminiferal taphocoenose in the Northeast Bohai and relationship to the sedimentary envionment[J]. Marine Geology and Quaternary Geology, 2009, 29(2):9-14.]
    [4]
    庄丽华, 常风鸣, 李铁刚, 等. 南黄海EY02-2孔底栖有孔虫群落特征与全新世沉积速率[J]. 海洋地质与第四纪地质,2002, 22(4):7-14.

    [ZHUANG Lihua, CHANG Fengming, LI Tiegang, et al. Foraminiferal faunas and Holocene sedimentation rates of Core EY02-2 in the South Yellow Sea[J]. Marine Geology and Quaternary Geology, 2002, 22(4):7-14.]
    [5]
    李建芬, 裴艳东, 王福, 等. 天津市潮滩活体和埋藏有孔虫群的分布及地质环境意义[J]. 海洋地质与第四纪地质,2009, 29(3):9-21.

    [LI Jianfen, PEI Yandong. WANG Fu. et al. Distribution and environmental significance of living foraminiferal assemblages and taphocoenose in Tianjin intertidal zone, the west coast of Bohai Bay[J]. Marine Geology and Quaternary Geology, 2009, 29(3):9-21.]
    [6]
    Jayaraju N, Reddy B C S R, Reddy K R. Deep-sea benthic foraminiferal distribution in south west Indian Ocean:implications to paleoecology[J]. International Journal of Geosciences, 2010, 1:79-86.
    [7]
    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]. IJRRAS, 2010, 5(1):86-94.
    [8]
    Ijiria A, Wang L, Oba T, et al. Paleoenvironmental changes in the northern area of the East China Sea during the past 42000 years[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2005, 219:239-261.
    [9]
    Ohkushi K, Thomas E, Kawahata H. Abyssal benthic foraminifera from the northwestern Pacific (Shatsky Rise) during the last 298 kyr[J]. Marine Micropaleontology, 2000, 38:119-147.
    [10]
    汪品先, 闵秋宝, 卞云华, 等. 河口有孔虫的搬运及其古环境意义(I)[J]. 海洋地质与第四纪地质,1986, 6(2):53-65.

    [WANG Pinxian, MIN Qiubao, BIA Yunhua, et al. Transport of foraminiferal tests in estuaries and its paleoenvironmental implications[J]. Marine Geology and Quaternary Geology,1986, 6(2):53-65.]
    [11]
    汪品先, 闵秋宝, 卞云华, 等. 河口有孔虫的搬运及其古环境意义(Ⅱ)[J]. 海洋地质与第四纪地质,1986, 6(3):83-90.

    [WANG Pinxian, MIN Qiubao, BIAN Yunhua, et al. Transport of foraminiferal tests in estuaries and its paleoenvironmental implications[J]. Marine Geology and Quaternary Geology, 1986, 6(3):83-90.]
    [12]
    李淑鸾. 珠江口底质中有孔虫埋葬群的分布规律[J]. 海洋地质与第四纪地质,1985, 5(2):83-104.

    [LI Shuluan. Distribution of the foraminiferal thanatocoenosis of Pearl River Estuary[J]. Marine Geology and Quaternary Geology, 1985, 5(2):83-104.]
    [13]
    李淑鸾. 珠江口底质沉积中浮游有孔虫的分布规律[J]. 北京大学学报:自然科学版,1987, 6:109-121.[LI Shuluan. Distribution of the planktonic foraminifera of Pearl River Estuary[J].Acta Scientiarum Naturalium Universitaries Pekinensis, 1987

    , 6:109-121.]
    [14]
    李淑鸾. 珠江口底质中胶结壳有孔虫的分布规律[J]. 海洋与湖沼,1988, 19(2):187-196.

    [LI Shuluan. Distribution of agglutinated foraminifera in bottom sediments of the Zhujiang River estuary[J]. Oceanologia et Limnologia Sinica, 1988, 19(2):187-196.]
    [15]
    陈木宏. 珠江崖门口沉积物中有孔虫分布的定量分析[C]//南海海洋科学集刊(第9集).北京:科学出版社, 1989.[CHEN Muhong. A Quantitative Study of the Distribution of foraminifera and its environmental controls in Yamen estuary, Zhujiang River[C]//Nanhai Studia Marina Sinica(No.9). Beijing:China Science Press, 1989.]
    [16]
    罗宪林, 李春初, 牟崇键. 伶仃洋有孔虫生物群和埋葬群的比较及河口沉积作用分析[J]. 海洋学报,2001, 23(4):69-74.

    [LUO Xianlin, LI Chunchu, MOU Chongjian. Difference in environmental explanation from analysis of living and dead foraminifera in the Lingdingyang estuary[J]. Acta Oceanologica Sinica,2001, 23(4):69-74.]
    [17]
    陈木宏, 赵焕庭, 温考胜, 等. 伶仃洋L2和L16孔第四纪有孔虫群与孢粉化石带特征及其地质意义[J]. 海洋地质与第四纪地质,1994, 14(1):11-22.

    [CHEN Muhong, ZHAO Huanting, WEN Xiaosheng, et al. Quaternary foraminiferal group and sporopollen zones in Cores L2 and L16 in the Lingdingyang estuary[J]. Marine Geology and Quaternary Geology, 1994, 14(1):11-22.]
    [18]
    汪品先, 闵秋宝, 卞云华. 南黄海西北部底质中有孔虫、介形虫分布规律及其地质意义[M]. 北京:海洋出版社, 1980.[WANG Pinxian,MIN Qiubao,BIAN Yunhua. Distribution of Foraminifera and Ostracod in Sediments of the Northwest South Yellow Sea and Its Geological Significance[M]. Beijing:China Ocean Press, 1980.]
    [19]
    汪品先, 闵秋宝, 卞云华, 等. 我国若干河口的有孔虫、介形虫埋葬群特征及其地质意义[C]//汪品先.海洋微体古生物论文集.北京:海洋出版社, 1980.[WANG Pinxian,MIN Qiubao,BIAN Yunhua,et al. Characteristics of foraminiferal and ostracod thanatocoenoses from some Chinese estuaries and their geological significance[C]//WANG Pinxian. Marine Micropaleontology of China. Beijing:China Ocean Press,1980.]
    [20]
    陈荣华. 浙江海岸带表层沉积物中有孔虫的分布及其影响因子[J]. 东海海洋, 1990, 8(3):35-48.

    [CHEN Ronghua. Distribution of foraminifera in surface sediments of the coastal zone of Zhejiang Province and its influencing factors[J]. Donghai Marine Science, 1990, 8(3):35-48.]
    [21]
    朱晓东. 影响沉积物中有孔虫丰度的生态因素探讨[J]. 南京大学学报,1993, 29(4):680-689.

    [ZHU Xiaodong. Ecological factors responsible for foraminiferal abundance in sediments:A comprehensive consideration[J]. Journal of Nanjing University(Natural Sciences Edition), 1993, 29(4):680-689.]
    • Related Articles

  • Related Articles

    [1]ZHANG Lixue, CHEN Aiqing, CHEN Qing, LAI Peixin. Late Quaternary clay minerals in the inner Lingdingyang of the Pearl River Estuary, southern China: Implications for paleoclimate changes at the provenance[J]. Marine Geology & Quaternary Geology, 2021, 41(5): 202-209. DOI: 10.16562/j.cnki.0256-1492.2020121002
    [2]ZHANG Jing, HU Gang, MA Guorong, HUI Jianguo, ZHANG Mingzhen, ZHANG Yong, DU Baoxia. Distribution of benthic forminifera in the surficial sediments of Changjiang distal delta and its environmental implications[J]. Marine Geology & Quaternary Geology, 2020, 40(4): 127-138. DOI: 10.16562/j.cnki.0256-1492.2019101401
    [3]MA Benjun, QIN Zhiliang, WU Shiguo, MI Lijun, GAO Wei, WANG Lei. Types and genesis of the mixed deposits in the Pearl River Mouth Basin of South China Sea[J]. Marine Geology & Quaternary Geology, 2018, 38(6): 149-158. DOI: 10.16562/j.cnki.0256-1492.2018.06.015
    [4]ZHANG Liang, CUI Zhenang, WANG Yaping, GAO Jianhua, XIA Zhen, MA Shengzhong. GRAIN SIZE VARIATION AND HEAVY METALS DISTRIBUTION DURING LAST HUNDRED YEARS UNDER THE IMPACT OF HUMAN ACTIVITIES IN THE INNER LINGDINGYANG BAY OF THE PEARL RIVER ESTUARY[J]. Marine Geology & Quaternary Geology, 2016, 36(1): 27-41. DOI: 10.16562/j.cnki.0256-1492.2016.01.003
    [5]LI Shanshan, PENG Song, DENG Yong, WEI Changfei, LI Hui, ZHAN Yeping. UPPER OLIGOCENE-EARLY LOWER MIOCENE SEDIMENTARY FACIES AND RESERVOIR DISTRIBUTION PATTERN IN WENCHANG H ZONE IN THE WESTERN PEARL RIVER MOUTH BASIN[J]. Marine Geology & Quaternary Geology, 2015, 35(5): 103-110. DOI: 10.16562/j.cnki.0256-1492.2015.05.012
    [6]GAN Huayang, LIANG Kai, ZHENG Zhichang. TRACE ELEMENTS GEOCHEMICAL CHARACTERISTICS OF THE SURFACE SEDIMENTS OF PEAR RIVER ESTUARY[J]. Marine Geology & Quaternary Geology, 2010, 30(4): 131-139. DOI: 10.3724/SP.J.1140.2010.04131
    [7]ZHU Yanhe, ZHU Weilin, XU Qiang, WANG Yingmin, LÜ Ming. SEDIMENTARY CHARACTERISTICS AND SEQUENCE FRAMEWORK OF THE ZHUHAI-ZHUJIANG FORMATION IN THE MIDDLE AREA OF PEARL RIVER MOUTH BASIN[J]. Marine Geology & Quaternary Geology, 2009, 29(4): 77-83. DOI: 10.3724/SP.J.1140.2009.04077
    [8]JIANG Hua, WANG Hua, LI Junliang, CHEN Shaoping, LIN Zhengliang, FANG Xinxin, CAI Jia. ANALYSIS ON SEQUENCE FORMATION STYLES OF ZHU-3 DEPRESSION IN PEARL RIVER MOUTH BASIN[J]. Marine Geology & Quaternary Geology, 2009, 29(1): 87-93. DOI: 10.3724/SP.J.1140.2009.01087
    [9]REN Zhen-huan, SUN Chong-chi, HUANG Jian-tao, LIAO Gui-jin, LIU Tian-you, QIAO Ji-hua, WEI wei, LIU Da-wei. INTERPRETATION OF THE GRAVIMETRY AND MAGNETOMETRY DATA OF THE SEGMENT OF THE COASTAL FRACTURE ZONE IN THE ZHUJIANG (PEARL) RIVER MOUTH[J]. Marine Geology & Quaternary Geology, 2008, 28(3): 61-66.
    [10]SHI Xiao-jun, CHEN Te-gu, YU Ke-fu. SEA-LEVEL CHANGES IN ZHUJIANG ESTUARY OVER LAST 40 YEARS[J]. Marine Geology & Quaternary Geology, 2008, 28(1): 127-134.

Catalog

    Get Citation
    PDF
    XML
    Article views (1942) PDF downloads (39) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzdsjdz@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return