伶仃洋东岸晚更新世以来硅藻组合及环境意义

彭志远, 陈炽新, 吴聪, 陈芳, 周洋, 余少华, 贾磊, 时翠. 伶仃洋东岸晚更新世以来硅藻组合及环境意义[J]. 海洋地质与第四纪地质, 2021, 41(2): 126-135. doi: 10.16562/j.cnki.0256-1492.2020103001
引用本文: 彭志远, 陈炽新, 吴聪, 陈芳, 周洋, 余少华, 贾磊, 时翠. 伶仃洋东岸晚更新世以来硅藻组合及环境意义[J]. 海洋地质与第四纪地质, 2021, 41(2): 126-135. doi: 10.16562/j.cnki.0256-1492.2020103001
PENG Zhiyuan, CHEN Chixin, WU Cong, CHEN Fang, ZHOU Yang, YU Shaohua, JIA Lei, SHI Cui. Diatom assemblage since late Pleistocene in the east coast of Lingdingyang Bay and its environmental implications[J]. Marine Geology & Quaternary Geology, 2021, 41(2): 126-135. doi: 10.16562/j.cnki.0256-1492.2020103001
Citation: PENG Zhiyuan, CHEN Chixin, WU Cong, CHEN Fang, ZHOU Yang, YU Shaohua, JIA Lei, SHI Cui. Diatom assemblage since late Pleistocene in the east coast of Lingdingyang Bay and its environmental implications[J]. Marine Geology & Quaternary Geology, 2021, 41(2): 126-135. doi: 10.16562/j.cnki.0256-1492.2020103001

伶仃洋东岸晚更新世以来硅藻组合及环境意义

  • 基金项目: 南方海洋科学与工程广东省实验室(广州)人才团队引进重大专项“粤港澳大湾区海岸线及滩涂湿地千年至十年尺度环境演变”(GML2019ZD0209);中国地质调查局二级项目“数字海洋地质工程天然气水合物数据库更新与服务”(DD20190216)
详细信息
    作者简介: 彭志远(1992—),男,硕士,助理工程师,从事海洋微体古生物和古环境研究,E-mail:627917278@qq.com
  • 中图分类号: P736.21

Diatom assemblage since late Pleistocene in the east coast of Lingdingyang Bay and its environmental implications

  • 通过分析伶仃洋东岸sz17QZ-20-3钻孔硅藻分布特征,结合测年、岩性和粒度,重建了该地区晚更新世以来的古环境演化。依据沉积物岩性粒度变化判断,晚更新世时期在23.6~11.0 m层段发育了一套河床相−溺古湾相−岸滩相−冲积相的垂向沉积序列,在花斑黏土层中有海水种Ethmodiscus rex碎片的存在,指示晚更新世海侵海退旋回。早全新世海侵在9000 cal. aBP左右到达研究区,海水种硅藻含量开始迅速增加,发育滨海平原相沉积;在8000 cal. aBP左右达到最高海平面,海水种硅藻含量最高;随后研究区处于海平面停滞状态,并缓慢下降,发育浅海相沉积;中晚全新世4.2~0 m层段为海退时期,发育河口湾相沉积。中全新世4.4~4.2 m层位海水种含量突然增加和4.4~4.6 m层位贝壳碎屑层指示可能有风暴潮事件发生;晚全新世0.3~0 m层段表层沉积物中硅藻丰度异常偏高,受人类活动影响较大。

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  • 图 1  钻孔sz17QZ-20-3地理位置图

    Figure 1. 

    图 2  sz17QZ-20-3钻孔岩性和粒度参数[29]

    Figure 2. 

    图 3  sz17QZ-20-3钻孔硅藻丰度、优势种百分含量、三大类属种和组合特征

    Figure 3. 

    表 1  sz17QZ-20-3钻孔测年数据

    Table 1.  Chronology of the borehole sz17QZ-20-3

    样品编号实验室编号 取样深度/m测年物质AMS14C年代/aBP校正后年代/cal. aBP
    sz17QZ-20-3-1Beta-502459 2.10~2.20木屑1570±301534~1394
    sz17QZ-20-3-2Beta-502460 4.80~4.90贝壳7420±307954~7806
    sz17QZ-20-3-3Beta-502461 8.40~8.50贝壳7690±308257~8037
    sz17QZ-20-3-4Beta-502462 9.75~9.95木屑7580±308420~8350
    sz17QZ-20-3-5Beta-502463 10.50~10.60木屑7840±308715~8547
    sz17QZ-20-3-6Beta-502464 20.60~20.85木屑>43500
    sz17QZ-20-3-7Beta-502465 21.75~21.90木屑>43500
    下载: 导出CSV

    表 2  硅藻属种划分

    Table 2.  Classification of diatoms

    硅藻生态类型主要硅藻种类
    海水种Actinocyclus ehrenbergii(爱氏辐环藻)、Nitzschia cocconeiformis(卵菱形藻)、Coscinodiscus excentricus(偏心圆筛藻)、Coscinodiscus lineatus(线性圆筛藻)、Coscinodiscus oculatus(小眼圆筛藻)、Thalassiosira oestrupii(厄氏海链藻)、Tryblioptychus cocconeisformis(卵形褶盘藻)、Ethmodiscus rex(斑盘藻)、Coscinodiscus subaulacodiscoidalis(亚沟圆筛藻)
    半咸水种Cyclotella striata(条纹小环藻)、Cyclotella stylorum(柱状小环藻)、Coscinodiscus divisus(多束圆筛藻)、Coscinodiscus subtilis(细弱圆筛藻)、Paralia sulcata(具槽帕拉藻)、Coscinodiscus radiatus(辐射圆筛藻)、Actinoptychus undulatus(环状辐裥藻)、Coscinodiscus argus(蛇目圆筛藻)、Coscinodiscus curvatulus(弓束圆筛藻)
    淡水种Achnanthes crenulata(波缘曲壳藻)、Cymbella tumida(膨胀桥弯藻)、Cyclotella meneghiniana(梅尼小环藻)
    下载: 导出CSV
  • [1]

    小泉格. 硅藻[M]. 王开发, 郭蓄民, 译. 北京: 地质出版社, 1984.

    KOIZUMI G. Diatom Analysis[M]. WANG Kaifa, GUO Xumin, trans. Beijing: Geological Publishing House, 1984.

    [2]

    金德祥, 陈金环, 黄凯歌. 中国海洋浮游硅藻类[M]. 上海: 上海科学技术出版社, 1965.

    JIN Dexiang, CHEN Jinhuan, HUANG Kaige. China Marine Planktonic Diatoms[M]. Shanghai: Shanghai Science and Technology Press, 1965.

    [3]

    金德祥, 程兆第, 林均民, 等. 中国海洋底栖硅藻类(上卷)[M]. 北京: 海洋出版社, 1982.

    JIN Dexiang, CHENG Zhaodi, LIN Junmin, et al. China Marine Benthic Diatoms (The First Volume)[M]. Beijing: Ocean Press, 1982.

    [4]

    金德祥, 程兆第, 刘师成, 等. 中国海洋底栖硅藻类(下卷)[M]. 北京: 海洋出版社, 1992.

    JIN Dexiang, CHENG Zhaodi, LIU Shicheng, et al. China Marine Benthic Diatoms (The Second Volume)[M]. Beijing: Ocean Press, 1992.

    [5]

    王开发, 蒋辉, 冯文科. 南海深海盆地硅藻组合的发现及其地质意义[J]. 海洋学报, 1985, 7(5):590-599

    WANG Kaifa, JIANG Hui, FENG Wenke. Discovery of the diatom assemblages in abyssal basin of South China Sea and their geological significance [J]. Acta Oceanologica Sinica, 1985, 7(5): 590-599.

    [6]

    王开发, 蒋辉, 张玉兰. 南海及沿岸地区第四纪孢粉藻类与环境[M]. 上海: 同济大学出版社, 1990.

    WANG Kaifa, JIANG Hui, ZHANG Yulan. Quaternary Spores, Pollen and Algae from the South China Sea and the Coastal Region and their Environment[M]. Shanghai: Tongji University Press, 1990.

    [7]

    蓝东兆, 程兆第, 刘师成. 南海晚第四纪沉积硅藻[M]. 北京: 海洋出版社, 1995.

    LAN Dongzhao, CHENG ZHAODI, LIU Shicheng. Diatoms in Late Quaternary Sediments from the South China Sea[M]. Beijing: Ocean Press, 1995.

    [8]

    汪桂荣. 珠江三角洲全新世硅藻[J]. 古生物学报, 1998, 37(3):305-325

    WANG Guirong. Holocene diatoms from the delta of Pearl River, South China [J]. Acta Palaeontologica Sinica, 1998, 37(3): 305-325.

    [9]

    黄镇国, 李平日, 张仲英, 等. 珠江三角洲形成发育演变[M]. 广州: 科学普及出版社广州分社, 1982.

    HUANG Zhenguo, LI Pingri, ZHANG Zhongying, et al. Formation, Development and Evolution of the Pearl River Delta[M]. Guangzhou: Science Popularization Press Guangzhou Branch, 1982.

    [10]

    龙云作. 珠江三角洲沉积地质学[M]. 北京: 地质出版社, 1997.

    LONG Yunzuo. Sedimentary Geology of Pearl River Delta[M]. Beijing: Geological Publishing House, 1997.

    [11]

    李平日, 乔彭年, 郑洪汉, 等. 珠江三角洲一万年来环境演变[M]. 北京: 海洋出版社, 1991.

    LI Pingri, QIAO Pengnian, ZHENG Honghan, et al. The Environment Evolution of the Zhujiang Delta in the Last 10000 Years[M]. Beijing: Ocean Press, 1991.

    [12]

    陈炽新, 吴聪, 谢叶彩, 等. 珠江三角洲中山地区ZK201-2钻孔硅藻组合及古环境意义[J]. 微体古生物学报, 2014, 31(4):335-346

    CHEN Chixin, WU Cong, XIE Yecai, et al. Diatom assemblages from borehole ZK201-2 in Zhongshan area of the Zhujiang River delta Guangdong, S. China and their paleoenvironment significance [J]. Acta Micropalaeontologica Sinica, 2014, 31(4): 335-346.

    [13]

    谢叶彩, 王强, 龙桂, 等. 珠江口小榄镇-万顷沙地区晚更新世以来的海侵层序[J]. 古地理学报, 2014, 16(6):835-852 doi: 10.7605/gdlxb.2014.06.067

    XIE Yecai, WANG Qiang, LONG Gui, et al. Transgressive sequence since the Late Pleistocene in Xiaolan Town-Wanqingsha area, Zhujiang River estuary [J]. Journal of Palaeogeography, 2014, 16(6): 835-852. doi: 10.7605/gdlxb.2014.06.067

    [14]

    蓝先洪. 珠江三角洲晚第四纪沉积特征[J]. 沉积学报, 1996, 14(2):155-161

    LAN Xianhong. Sedimentary characteristics of the Late Quaternary in the Zhujiang River delta [J]. Acta Sedimentologica Sinica, 1996, 14(2): 155-161.

    [15]

    徐明广, 马道修, 周青伟, 等. 珠江三角洲地区第四纪海平面变化[J]. 海洋地质与第四纪地质, 1986, 6(3):93-102

    XU Mingguang, MA Daoxiu, ZHOU Qingwei, et al. Quaternary sea-level fluctuation in Zhujiang river delta area [J]. Marine Geology & Quaternary Geology, 1986, 6(3): 93-102.

    [16]

    余素华, 张玉兰, 杨晓强, 等. 深圳湾北岸新民孔岩心晚更新世以来的环境记录[J]. 海洋地质与第四纪地质, 2003, 23(2):9-18

    YU Suhua, ZHANG Yulan, YANG Xiaoqiang, et al. Environmental records in the Xinmin core since the Late pleistocene in the Northern Coast of the Shenzhen Bay [J]. Marine Geology & Quaternary Geology, 2003, 23(2): 9-18.

    [17]

    黄镇国, 蔡福祥. 珠江口晚第四纪埋藏风化层及其环境意义[J]. 第四纪研究, 2007, 27(5):828-833 doi: 10.3321/j.issn:1001-7410.2007.05.024

    HUANG Zhenguo, CAI Fuxiang. Buried weathering layers of the Late Quaternary and their environmental significance in the Zhujiang River estuary [J]. Quaternary Sciences, 2007, 27(5): 828-833. doi: 10.3321/j.issn:1001-7410.2007.05.024

    [18]

    陈国能, 张珂, 贺细坤, 等. 珠江三角洲晚更新世以来的沉积—古地理[J]. 第四纪研究, 1994, 14(1):67-74 doi: 10.3321/j.issn:1001-7410.1994.01.007

    CHEN Guoneng, ZHANG Ke, HE Xikun, et al. Paleo-geographic evolution of the Pearl River Delta since the Late Pleistocene [J]. Quaternary Sciences, 1994, 14(1): 67-74. doi: 10.3321/j.issn:1001-7410.1994.01.007

    [19]

    方国祥, 李平日, 黄光庆. 珠江三角洲8000年来海平面变化[J]. 地理研究, 1991, 10(4):1-11

    FANG Guoxiang, LI Pingri, HUANG Guangqing. Sea level changes in Zhujiang Delta during the past 8000 years [J]. Georaphical Research, 1991, 10(4): 1-11.

    [20]

    余少华, 陈芳, 谢叶彩, 等. 珠江口万顷沙晚第四纪沉积及古环境重建[J]. 热带地理, 2016, 36(3):374-387

    YU Shaohua, CHEN Fang, XIE Yecai, et al. Paleoenvironment Reconstruction and Sedimentary Record in the Wanqingsha Area of the Pearl River Estuary [J]. Tropical Geography, 2016, 36(3): 374-387.

    [21]

    吴月琴, 刘春莲, 杨小强, 等. 珠江三角洲中部全新世以来的微体动物群记录与古环境重建[J]. 海洋地质与第四纪地质, 2019, 39(2):31-43

    WU Yueqin, LIU Chunlian, YANG Xiaoqiang, et al. Holocene microfaunal records in the central Pearl River Delta and implications for palaeoenvironmental change [J]. Marine Geology and Quaternary Geology, 2019, 39(2): 31-43.

    [22]

    王建华, 曹玲珑, 王晓静, 等. 珠江三角洲万顷沙地区晚第四纪沉积相与古环境演变[J]. 海洋地质与第四纪地质, 2009, 29(6):37-41

    WANG Jianhua, CAO Linglong, WANG Xiaojing, et al. Evolution of sedimentary facies and paleoenvironment during the late quaternary in Wanqingsha area of the Pearl River delta [J]. Marine Geology & Quaternary Geology, 2009, 29(6): 37-41.

    [23]

    时翠, 甘华阳, 马胜中, 等. 晚更新世以来内伶仃洋河口湾的地层层序和沉积演化[J]. 海洋地质前沿, 2015, 31(10):8-18

    SHI Cui, GAN Huayang, MA Shengzhong, et al. Late quaternary evolution and sequence stratigraphy of the Lingdingyang Eatuary in south China [J]. Marine Geology Frontiers, 2015, 31(10): 8-18.

    [24]

    时翠, 甘华阳, 夏真, 等. 珠江口内伶仃洋表层沉积物粒度特征及其运移趋势[J]. 海洋地质与第四纪地质, 2015, 35(1):13-20

    SHI Cui, GAN Huayang, XIA Zhen, et al. Characteristics and transport trend of surface sediments in inner Lingdingyang Firth of the Pearl River estuary [J]. Marine Geology and Quaternary Geology, 2015, 35(1): 13-20.

    [25]

    赵信文, 陈双喜, 黄长生, 等. 珠江三角洲陈村钻孔剖面沉积特征及有机碳同位素古环境意义[J]. 地质通报, 2014, 33(10):1635-1641 doi: 10.3969/j.issn.1671-2552.2014.10.023

    ZHAO Xinwen, CHEN Shuangxi, HUANG Changsheng, et al. The sedimentary characteristics of core section from Chencun Village in Pearl River Delta, and their organic carbon isotopic palaeoenvironmental implications [J]. Geological Bulletin of China, 2014, 33(10): 1635-1641. doi: 10.3969/j.issn.1671-2552.2014.10.023

    [26]

    陈木宏, 赵焕庭, 温孝胜, 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 & Quaternary Geology, 1994, 14(1): 11-22.

    [27]

    陶慧, 王建华, 陈慧娴, 等. 伶仃洋ZK19孔全新统有机物δ13C和C/N值特征及东亚季风演变记录[J]. 中山大学学报(自然科学版), 2019, 58(3):1-12

    TAO Hui, WANG Jianhua, CHEN Huixian, et al. Characteristics of δ13C and C/N in the Holocene organic material of borehole ZK19 in Lingdingyang bay and the records of east Asian Monsoon variation [J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 2019, 58(3): 1-12.

    [28]

    周洋, 谢叶彩, 陈芳, 等. 珠江三角洲ZK201-2孔晚更新世以来微体生物群与古环境[J]. 海洋地质与第四纪地质, 2015, 35(4):113-123

    ZHOU Yang, XIE Yecai, CHEN Fang, et al. Microfaunas in hole ZK201-2 at Zhujiang River Delta since Late Pleistocene and their Implications for Paleoenvironments [J]. Marine Geology & Quaternary Geology, 2015, 35(4): 113-123.

    [29]

    广州海洋地质调查局. 深圳西岸科学用海区环境地质工程地质调查成果报告[M]. 广州: 广州洋地质调查, 2019.

    Guangzhou Marine Geological Survey. Report on Geological Survey Results of Environmental Geology and Engineering in the Scientific Seas Area on the West Bank of Shenzhen[M]. Guangzhou: Guangzhou Marine Geological Survey, 2019.

    [30]

    Abrantes F. Assessing the Ethmodiscus ooze problem: new perspective from a study of an eastern equatorial Atlantic core [J]. Deep Sea Research Part I: Oceanographic Research Papers, 2001, 48(1): 125-135. doi: 10.1016/S0967-0637(00)00041-8

    [31]

    Dong Y X, Liu C L, Yin J R, et al. Late Quaternary microfaunas and paleoenvironmental changes recorded in core sediments of the Pearl River Delta, South China [J]. Vertebrata Palasiatica, 2007, 45(2): 162-173.

    [32]

    ZongY, Huang G, Switzer A D, et al. An evolutionary model for the Holocene formation of the Pearl River delta, China [J]. The Holocene, 2009, 19(1): 129-142. doi: 10.1177/0959683608098957

    [33]

    Fairbridge R W. Eustatic changes in sea level [J]. Physics and Chemistry of the Earth, 1961, 4: 99-185. doi: 10.1016/0079-1946(61)90004-0

    [34]

    Siddall M, Rohling E J, Almogi-Labin A, et al. Sea-level fluctuations during the last glacial cycle [J]. Nature, 2003, 423(6942): 853-858. doi: 10.1038/nature01690

    [35]

    赵信文, 罗传秀, 陈双喜, 等. 基于孢粉数据的珠江三角洲QZK6孔全新世气候定量重建[J]. 地质通报, 2014, 33(10):1621-1628 doi: 10.3969/j.issn.1671-2552.2014.10.020

    ZHAO Xinwen, LUO Chuanxiu, CHEN Shuangxi, et al. Quantitative re-construction of Holocene climate based on pollen data from drill hole QZK6 in Pearl River Delta [J]. Geological Bulletin of China, 2014, 33(10): 1621-1628. doi: 10.3969/j.issn.1671-2552.2014.10.020

    [36]

    刘春莲, FÜRSICH F T, 董艺辛, 等. 珠江三角洲PRD05孔的高分辨率介形类记录与晚第四纪古环境重建[J]. 古地理学报, 2008, 10(3):313-322 doi: 10.7605/gdlxb.2008.03.011

    LIU Chunlian, FÜRSICH F T, DONG Yixin, et al. High resolution outraced records of borehole PRD05 and the Late Quaternary palaeoenvironment in Pearl River delta [J]. Journal of Palaeogeography, 2008, 10(3): 313-322. doi: 10.7605/gdlxb.2008.03.011

    [37]

    廖梦娜, 于革, 桂峰. 长江三角洲-辐射沙脊群YZ07钻孔晚更新世以来海侵事件的古生态学记录[J]. 第四纪研究, 2018, 38(3):732-745 doi: 10.11928/j.issn.1001-7410.2018.03.18

    LIAO Mengna, YU Ge, GUI Feng. Paleoecological records of transgressions in Core YZ07 from Changjiang River delta-radial sand ridges of the South Yellow Sea since the Late Pleistocene [J]. Quaternary Sciences, 2018, 38(3): 732-745. doi: 10.11928/j.issn.1001-7410.2018.03.18

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