湛江湾-雷州湾海域表层沉积物中底栖有孔虫分布特征及其环境意义

李路路, 鲍宽乐, 张家强, 张德程, 任开文, 代友旭. 湛江湾-雷州湾海域表层沉积物中底栖有孔虫分布特征及其环境意义[J]. 海洋地质前沿, 2024, 40(11): 46-56. doi: 10.16028/j.1009-2722.2024.163
引用本文: 李路路, 鲍宽乐, 张家强, 张德程, 任开文, 代友旭. 湛江湾-雷州湾海域表层沉积物中底栖有孔虫分布特征及其环境意义[J]. 海洋地质前沿, 2024, 40(11): 46-56. doi: 10.16028/j.1009-2722.2024.163
LI Lulu, BAO Kuanle, ZHANG Jiaqiang, ZHANG Decheng, REN Kaiwen, DAI Youxu. Distribution characteristics of benthic foraminifera in surface sediments of Zhanjiang Bay-Leizhou Bay and its environmental significance[J]. Marine Geology Frontiers, 2024, 40(11): 46-56. doi: 10.16028/j.1009-2722.2024.163
Citation: LI Lulu, BAO Kuanle, ZHANG Jiaqiang, ZHANG Decheng, REN Kaiwen, DAI Youxu. Distribution characteristics of benthic foraminifera in surface sediments of Zhanjiang Bay-Leizhou Bay and its environmental significance[J]. Marine Geology Frontiers, 2024, 40(11): 46-56. doi: 10.16028/j.1009-2722.2024.163

湛江湾-雷州湾海域表层沉积物中底栖有孔虫分布特征及其环境意义

  • 基金项目: 中国地质调查局项目“雷州半岛东部海岸带综合地质调查”(DD20208011),“胶东北部海岸带与岛礁综合地质调查”(DD20220990)
详细信息
    作者简介: 李路路(1988—),男,硕士,工程师,主要从事海洋与海岸带地质调查方面的研究工作. E-mail:717104997@qq.com
    通讯作者: 代友旭(1988—),男,硕士,高级工程师,主要从事海洋与海岸带地质调查方面的研究工作. E-mail:daiyouxu1988@126.com
  • 中图分类号: P736.21

Distribution characteristics of benthic foraminifera in surface sediments of Zhanjiang Bay-Leizhou Bay and its environmental significance

More Information
  • 于2020年6月对湛江湾-雷州湾海域89个站位表层沉积物进行底栖有孔虫采样分析,共识别出52属103种,其中,玻璃质壳37属64种,胶结壳10属13种,瓷质壳5属26种。底栖有孔虫分布表现为湾内低、湾外高,由湾内向湾外增加的特点。对底栖有孔虫进行Q型因子分析,划分4个有孔虫组合,组合Ⅰ为Florilus scaphus - Pseudorotalia gaimardi,以暖水种为主,指示受南海暖流影响明显的内陆架浅水环境;组合Ⅱ为Nonion belridgense - Hemirotalia foraminulosa - Elphidium macellum,以咸水种为主,可能反映盐度值明显升高的浅水环境,具有海陆过渡带性质;组合Ⅲ为Hanzawaia convexa - Rosalina bradyi,以浅水种为主,指示受沿岸流与南海暖流共同影响的内陆架浅水环境;组合Ⅳ为Neoconorbina terquemi - Ammonia beccarii,以广盐种为主,反映了受沿岸流影响明显的滨海环境。综合分析影响底栖有孔虫组合分布的各种因素,认为温度、水深为控制研究海域底栖有孔虫分布的主要因素,同时,海流和底质类型也会对底栖有孔虫分布产生一定影响。

  • 加载中
  • 图 1  湛江湾-雷州湾海域采样站位

    Figure 1. 

    图 2  研究区水深(a)、海底水温(b)和盐度(c)分布

    Figure 2. 

    图 3  研究区玻璃质壳(a)、胶结质壳(b)、瓷质壳(c)底栖有孔虫含量分布

    Figure 3. 

    图 4  研究区底栖有孔虫丰度(a)、简单分异度(b)、复合分异度(c)分布

    Figure 4. 

    图 5  研究区底栖有孔虫站位因子荷载值分布

    Figure 5. 

    表 1  研究区底栖有孔虫优势种及环境指示意义

    Table 1.  Dominant benthic foraminifera species in the study area and their environmental significance

    壳质类型 优 势 种 占总含量百分比/% 环境指示意义[1]
    玻璃质壳 Pseudorotalia gaimardi(多疣假轮虫) 20.90 暖水种
    Hanzawaia mantaensis(曼顿半泽虫) 15.02 中外陆架半深水种
    Ammonia beccarii(毕克卷转虫) 6.58 广盐性滨岸种
    Florilus scaphus(船状花朵虫) 4.68 内陆架浅水种
    Elphidium advenum(异地希望虫) 4.11 内陆架浅水种
    Cavarotalia annectens(同现孔轮虫) 3.34 内陆架浅水种
    Elphidium asiaticum(亚洲希望虫) 2.23 内陆架浅水种
    Elphidium limpidum(清晰希望虫) 1.69 内陆架浅水种
    Elphidium hispidulum(茸毛希望虫) 1.26 内陆架浅水种
    Hemirotalia foraminulosa(有孔半轮虫) 1.25 内陆架浅水种
    Pararotalia nipponica(日本纺轮虫) 1.24 内陆架浅水种
    Hanzawaia convexa(隆拱半泽虫) 1.24 中外陆架半深水种
    Ammonia pauciloculata(少室卷转虫) 1.18 内陆架浅水种
    瓷质壳 Quinqueloculina subungeriana(亚恩格五玦虫) 1.61 近岸浅水种
    Quinqueloculina lamarckiana(拉马克五玦虫) 1.29 近岸浅水种
    胶结壳 Textularia foliacea(叶状串珠虫) 12.42 近岸浅水种
    Bigenerina nodosaria(节房双串虫) 6.65 暖水种
    下载: 导出CSV

    表 2  研究区主要底栖有孔虫属种Q型因子分析

    Table 2.  Q-mode factor analysis of major benthic foraminifera species in the study area

    属 种 因子1 因子2 因子3 因子4
    Hanzawaia nipponica −0.032 0.661 0.469 −0.018
    Quinqueloculina argunica −0.056 0.467 0.469 −0.188
    Rosalina bradyi −0.075 0.576 0.739 −0.051
    Cribrononion vitreum −0.150 0.723 0.113 −0.009
    Elphidium macellum −0.088 0.799 0.177 0.017
    Neoconorbina terquemi 0.139 −0.193 0.057 0.819
    Nonion belridgense −0.049 0.941 0.151 −0.018
    Quinqueloculina agglutinans 0.076 0.793 −0.026 −0.026
    Triloculina tricarinata 0.027 0.327 0.235 0.204
    Reussella pluchra 0.593 0.251 0.460 0.330
    Triloculina trigonula 0.040 0.314 −0.006 0.665
    Spiroloculina laevigata 0.132 0.332 −0.113 0.371
    Triloculina disparilis 0.337 −0.081 0.075 0.215
    Ammonia pauciloculata 0.809 0.214 −0.043 0.144
    Hanzawaia convexa −0.031 0.216 0.888 −0.029
    Hemirotalia foraminulosa −0.017 0.84 −0.013 0.042
    Elphidium hispidulum 0.187 −0.069 0.720 0.238
    Quinqueloculina lamarckiana 0.600 −0.153 0.079 0.098
    Elphidium limpidum 0.853 −0.057 0.082 0.341
    Elphidium asiaticum 0.853 −0.006 −0.031 0.321
    Cavarotalia annectens 0.749 −0.066 0.082 −0.134
    Elphidium advenum 0.649 −0.004 0.212 0.490
    Florilus scaphus 0.969 −0.109 −0.063 −0.004
    Ammonia beccarii 0.493 −0.057 0.024 0.717
    Bigenerina nodosaria 0.896 −0.064 0.069 −0.243
    Textularia foliacea 0.896 −0.083 0.019 0.170
    Hanzawaia mantaensis 0.899 −0.127 −0.011 0.242
    Pseudorotalia gaimardi 0.954 −0.114 −0.049 0.073
    注:表中粗体数据为4个主因子组合中的最大值。
    下载: 导出CSV
  • [1]

    汪品先,章纪军,赵泉鸿,等. 东海底质中有孔虫和介形虫[M]. 北京:海洋出版社,1988.

    WANG Pinxian,ZHANG Jijun,ZHAO Quanhong,et al. Foraminifera and Ostracoda in Bottom Sediments of the East China Sea[M]. Beijing:China Ocean Press,1988.

    [2]

    张江勇,汪品先. 深海研究中的底栖有孔虫:回顾与展望[J]. 地球科学进展,2004,19(4):545-550. doi: 10.3321/j.issn:1001-8166.2004.04.009

    ZANG Jiangyong,WANG Pinxian. Benthic foraminifera in deep-sea research:retrospect and prospect[J]. Advances in Earth Science,2004,19(4):545-550. doi: 10.3321/j.issn:1001-8166.2004.04.009

    [3]

    MIAO Q M,THUNELL R C. Late Pleistocene-Holocene distribution of deep-sea benthic foraminifera in the South China Sea and Sulu Sea:paleoceanography implications[J]. Journal of Foraminifera Research,1996,26(1):9-23. doi: 10.2113/gsjfr.26.1.9

    [4]

    GOODAY A J,RATHBURN A E. Temporal variability in living deepsea benthic foraminifera:a review[J]. Earth-Science Reviews,1999,46(1):187-212.

    [5]

    WANG P X,LI Q Y,TIAN J,et al. Monsoon influence on planktonic δ18O records from the South China Sea[J]. Quaternary Science Reviews,2006,142:26-39.

    [6]

    李涛,向荣,李团结. 珠江口表层沉积物底栖有孔虫分布及环境指示[J]. 海洋地质与第四纪地质,2011,31(6):91-98.

    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.

    [7]

    李越,李波,李涛. 南海北部海域表层沉积物底栖有孔虫分布特征及影响因素[J]. 海洋地质前沿,2022,38(2):30-36.

    LI Yue,LI Bo,LI Tao. Distribution pattern and influence factors of benthic foraminifera in the surface sediments of northern South China Sea[J]. Marine Geology Frontiers,2022,38(2):30-36.

    [8]

    方惠瑛. 闽南-台湾浅滩表层沉积物中底栖有孔虫分布及其环境特征[J]. 热带海洋,1992,11(2):54-61.

    FANG Huiying. Benthic foraminifera in the surface sediments of the Minnan-Taiwan bank region and its environmental characteristics[J]. Tropical Geography,1992,11(2):54-61.

    [9]

    袁洁琼,丁旋,邹欣庆. 南黄海辐射沙脊群表层沉积物中底栖有孔虫埋葬群分布特征及其环境意义[J]. 地学前缘,2020,27(6):276-288.

    YUAN Jieqiong,DING Xuan,ZOU Xinqing. Distribution of benthic foraminiferal taphocoenose in surface sediments and the environmental implication in the radial sand ridge of the South Yellow Sea[J]. Earth Science Frontiers,2020,27(6):276-288.

    [10]

    李小艳,石学法,程振波,等. 杭州湾表层沉积物中有孔虫分布特征及其环境意义[J]. 海洋地质与第四纪地质,2015,35(1):121-127.

    LI Xiaoyan,SHI Xuefa,CHENG Zhenbo,et al. Distribution of foraminifera in surface sediments of the Hangzhou Bay and its environmental implication[J]. Marine Geology & Quaternary Geology,2015,35(1):121-127.

    [11]

    李顺,张江勇,钟和贤,等. 南海北部陆坡ZSQD196PC柱状样末次间冰期以来的古海洋学记录:氧同位素、有孔虫和硅藻[J]. 海洋地质前沿,2013,29(11):32-38.

    LI Shun,ZHANG Jiangyong,ZHONG Hexian,et al. Paleoceanographic records of core ZSQD196PC from the northern South China Sea:oxygen isotope,foraminifera and diatom[J]. Marine Geology Frontiers,2013,29(11):32-38.

    [12]

    徐建,黄宝琦,陈荣华,等. 南海东北部表层沉积中有孔虫的分布及其环境意义[J]. 热带海洋学报,2001,20(4):6-13. doi: 10.3969/j.issn.1009-5470.2001.04.002

    XU Jian,HUANG Baoqi,CHEN Ronghua,et al. Distribution of foraminifera in surface sediments of northeastern South China Sea and its environmental implications[J]. Journal of Tropical Oceanography,2001,20(4):6-13. doi: 10.3969/j.issn.1009-5470.2001.04.002

    [13]

    李保华,孔晓敏,王晓燕,等. 北部湾中部海域底质沉积物中的有孔虫[J]. 微体古生物学报,2010,27(2):99-108.

    LI Baohua,KONG Xiaomin,WANG Xiaoyan,et al. Foraminifera in surface sediments of the Tonkin Gulf,northern South China Sea[J]. Acta Micropalaeontologica Sinica,2010,27(2):99-108.

    [14]

    杨毅,徐艳东,王发云,等. 粤西沿岸流和物质输移模型研究及应用[J]. 科学技术与工程,201,15(19):80-85.

    YANG Yi,XU Yandong,WANG Fayun,et al. A numerical hydrodynamic and transport model in the west coast of Guangdong Province[J]. Science Technology and Engineering,2015,15(19):80-85.

    [15]

    郝连成,远继东,郑立龙,等. 湛江湾海域表层沉积物粒度特征及沉积环境[J]. 海洋地质前沿,2022,38(8):1-10.

    HAO Liancheng,YUAN Jidong,ZHENG Lilong,et al. Grain-size characteristics of surface sediment and sedimentary environment in Zhanjiang Bay[J]. Marine Geology Frontiers,2022,38(8):1-10.

    [16]

    李栓虎. 湛江湾外航道二侧浅滩冲淤变化的成因分析[J]. 科学技术与工程,2013,13(35):10595-10599.

    LI Shuanhu. Cause analysis of erosion and deposition two side of channel sandbar outside of Zhanjiang Bay[J]. Science Technology and Engineering,2013,13(35):10595-10599.

    [17]

    陈新庚. 湛江港和雷州湾的生态环境分析与污染现状评价[J]. 中山大学学报论丛,1989(3):210-225.

    CHEN Xingeng. Ecological environment analysis and assessment of the present state of pollution in Zhanjiang Harbor and Leizhou Bay[J]. Sun Yatsen University Forum,1989(3):210-225.

    [18]

    陈春亮,张才学. 雷州湾浮游植物群落结构特征及其环境影响分析[J]. 应用海洋学学报,2016,35(2):174-182. doi: 10.3969/J.ISSN.2095-4972.2016.02.004

    CHEN Chunliang,ZHANG Caixue. Community structure of phytoplankton in the coastal waters of Leizhou Bay with its relationships to environmental factors[J]. Journal of Applied Oceanography,2016,35(2):174-182. doi: 10.3969/J.ISSN.2095-4972.2016.02.004

    [19]

    何炎,胡兰英. 广东雷州半岛上新世有孔虫[M]. 合肥:中国科学技术大学出版社,2001:1-189.

    HE Yan,HU Lanying. Pliocene Foraminifera from Leizhou Peninsula,Guangdong Province[M]. Hefei:University of Science and Technology of China Press,2011:1-189.

    [20]

    IJIRIA A,WANG L,OBA T,et al. Paleoenvironmental changes in the northern area of the East China Sea during the past 42 000 years[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,2005,219:239-261.

    [21]

    CULVER S. New foraminiferal depth zonation of the northwestern Gulf of Mexico[J]. Palaios,1988,3:69-85. doi: 10.2307/3514545

    [22]

    JIAN Z M,WANG L J. Late Quaternary benthic foraminifera and deep-water paleoceanography in the South China Sea[J]. Mar Micropaleontol,1997,32:127-154. doi: 10.1016/S0377-8398(97)00017-0

    [23]

    汪品先,闵秋宝. 我国第四纪海侵研究中的几个基本问题[J]. 海洋地质与第四纪地质,1985,5(1):15-25.

    WANG Pinxian,MIN Qiubao. Quaternary marine transgressions in China:some basic questions[J]. Marine Geology & Quaternary Geology,1985,5(1):15-25.

    [24]

    周洋,陈芳,孙桂华,等. 台湾海峡西北部平潭岛海域表层沉积物中底栖有孔虫分布及其环境控制因素[J]. 微体古生物学报,2014,31(1):54-63.

    ZHOU Yang,CHEN Fang,SUN Guihua,et al. Benthic foraminiferal distribution in surface sediments of the northwest Taiwan strait near the Pingtan Island and its environmental controlling factors[J]. Acta Micropalaeontologica Sinica,2014,31(1):54-63.

    [25]

    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.

    [26]

    汪品先,闵秋保,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[C]//海洋微体古生论文集, 北京:海洋出版社,1980:61-83.

    WANG Pinxian,MIN Qiubao,BIAN Yunhua. Distribution and geological significance of foraminifera and ostracoda in the sediment of northwest South Yellow Sea[C]//Proceedings of Marine Micropaleozoic,Beijing:China Ocean Press,1980:61-83.

  • 加载中

(5)

(2)

计量
  • 文章访问数:  158
  • PDF下载数:  18
  • 施引文献:  0
出版历程
收稿日期:  2024-07-14
刊出日期:  2024-11-28

目录