留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

南极半岛东北部海域表层沉积物稀土元素特征及物源指示意义

陈志华 黄元辉 唐正 王豪壮 葛淑兰 方习生 韩喜彬 王爱军 武力 朱志敏

陈志华, 黄元辉, 唐正, 王豪壮, 葛淑兰, 方习生, 韩喜彬, 王爱军, 武力, 朱志敏. 南极半岛东北部海域表层沉积物稀土元素特征及物源指示意义[J]. 海洋地质与第四纪地质, 2015, 35(3): 145-155. doi: 10.3724/SP.J.1140.2015.03145
引用本文: 陈志华, 黄元辉, 唐正, 王豪壮, 葛淑兰, 方习生, 韩喜彬, 王爱军, 武力, 朱志敏. 南极半岛东北部海域表层沉积物稀土元素特征及物源指示意义[J]. 海洋地质与第四纪地质, 2015, 35(3): 145-155. doi: 10.3724/SP.J.1140.2015.03145
CHEN Zhihua, HUANG Yuanhui, TANG Zheng, WANG Haozhuang, GE Shulan, FANG Xisheng, HAN Xibin, WANG Aijun, WU Li, ZHU Zhimin. RARE EARTH ELEMENTS IN THE OFFSHORE SURFACE SEDIMENTS OF THE NORTHEASTERN ANTARCTIC PENINSULA AND THEIR IMPLICATIONS FOR PROVENANCE[J]. Marine Geology & Quaternary Geology, 2015, 35(3): 145-155. doi: 10.3724/SP.J.1140.2015.03145
Citation: CHEN Zhihua, HUANG Yuanhui, TANG Zheng, WANG Haozhuang, GE Shulan, FANG Xisheng, HAN Xibin, WANG Aijun, WU Li, ZHU Zhimin. RARE EARTH ELEMENTS IN THE OFFSHORE SURFACE SEDIMENTS OF THE NORTHEASTERN ANTARCTIC PENINSULA AND THEIR IMPLICATIONS FOR PROVENANCE[J]. Marine Geology & Quaternary Geology, 2015, 35(3): 145-155. doi: 10.3724/SP.J.1140.2015.03145

南极半岛东北部海域表层沉积物稀土元素特征及物源指示意义


doi: 10.3724/SP.J.1140.2015.03145
详细信息
    作者简介:

    陈志华(1970-),男,博士,研究员,主要从事海洋地质学研究,Email:chenzia@fio.org.cn

  • 基金项目:

    南北极环境综合考察与评估专项(CHINARE2014-01-02,CHINARE2015-01-02,CHINARE2014-04-01,CHINARE2015-04-01)

    国家自然科学基金项目(40176136,41106166)

  • 中图分类号: P736.4

RARE EARTH ELEMENTS IN THE OFFSHORE SURFACE SEDIMENTS OF THE NORTHEASTERN ANTARCTIC PENINSULA AND THEIR IMPLICATIONS FOR PROVENANCE

More Information
  • 摘要: 通过对南极半岛东北部海域36个表层沉积物样品的稀土元素分析发现:(1)研究区表层沉积物中稀土元素总量(REE)的分布范围为(45.47~183.60)×10-6,平均值为91.36×10-6;稀土元素含量的高低与铝硅酸盐黏土成正比,与生物硅含量成反比;(2)大致以象岛至南极半岛北部的茹安维尔岛为界,研究区西部的布兰斯菲尔德海峡及南设得兰群岛北部岛架-岛坡沉积物稀土含量较低,稀土元素页岩标准化模式与长城站周边土壤/湖泊沉积物、火山岩相一致,表现为重稀土相对富集,铕正异常明显,Sm/Nd分子比值大,推断该区沉积物主要来源于南设德兰群岛中-新生代火山岩分布区与现代火山活动区;(3)研究区东部鲍威尔海盆、南奥克尼群岛岛架和南斯科舍海脊区沉积物稀土元素的页岩标准化配分模式表现为平坦型,轻稀土明显抬升,铕正异常不显著,Sm/Nd分子比值小,稀土元素含量受沉积物中黏土组分含量、硅质生物组分等制约,推断沉积物陆源碎屑主要来源于威德尔海西部和南部,局部受南奥尼克群岛、南斯科舍海脊和南设德兰群岛物质的影响,沉积物的搬运主要受冰筏和海流制约。
  • [1] Vaughan D, Marshall G, Connolley W, et al. Recent rapid regional climate warming on the Antarctic Peninsula[J]. Climate Change, 2003, 60:243-274.
    [2] Steig E, Schneider D, Rutherford S, et al. Warming of the Antarctic Ice-Sheet surface since the 1957 International Geophysical Year[J]. Nature, 2009, 457:459-462.
    [3] Mayewski P, Meredith M, Summerhayes C, et al. State of the Antarctic and Southern Ocean climate system[J]. Reviews of Geophysics, 2009, 47:1-38.
    [4] Cofaigh C ó, Davies B J, Livingstone S J, et al. Reconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial Maximum[J]. Quaternary Science Reviews, 2014, 100:87-110.
    [5] 王先兰. 南极长城湾沉积物中稀土元素的初步研究[J]. 南极研究, 1991, 3(3), 39-44.

    [WANG Xianlan. A preliminary study on REE in the sediments of the Great Wall Bay, Antarctica[J]. Antarctic Research, 1991, 3(3):39-44.]
    [6] 王先兰. 南极长城湾沉积物的地球化学特征与分区[J].南极研究, 1993, 5(1), 24-30.

    [WANG Xianlan. Geochemical characteristics and divisions of the sediments in the Great Wall Bay, Antarctica[J]. Antarctic Research, 1993, 5(1):24-30.]
    [7] Kim D, Park B K, Yoon H I, et al. Geochemical evidence for Holocene paleoclimatic changes in Maxwell Bay of South Shetland Islands, West Antarctica[J]. Geosciences Journal, 1999, 3(1):55-62.
    [8] Santos I R, Fávaro D I T, Schaefer C E G R, et al. Sediment geochemistry in coastal maritime Antarctica (Admiralty Bay, King George Island):Evidence from rare earths and other elements[J]. Marine Chemistry, 2007, 107:464-474.
    [9] 李芝君, 王大锐, 陈永武. 南极半岛西部海域表层沉积中有孔虫的初步研究[J]. 海洋地质与第四纪地质, 1987, 7(4):67-79.

    [LI Zhijun, WANG Darui, CHEN Yongwu. A preliminary study on foraminerfa in surface sediments the Great Wall Bay, Antarctica[J]. Antarctic Research, 1991, 3(3):39-44.]
    [10] 詹玉芬.南极半岛西北海域表层沉积物中硅藻的初步研究[J]. 南极研究, 1988, 1(2):37-43.

    [ZHAN Yufen. A preliminary study on diatom in surface sediments in the area to west of Antarctica Peninsula[J]. Antarctic Research, 1988, 1(2):37-43.]
    [11] 吴能友, 段威武, 蔡秋蓉, 2002. 南极布兰斯菲尔德海峡冰海沉积环境与沉积模式初探[J]. 南海地质研究, 13(1):1-8.[WU Nengyou, DUAN Weiwu, CAI Qiurong. Preliminary discussion the sedimentary envrironment and sedimentation model of the Bransfield Strait, Antarctica[J]. South China Sea Research, 2002

    , 13(1):1-8.]
    [12] 卢冰, 唐运千, 眭良仁. 南极布兰斯菲尔德海峡表层沉积物生物标志化合物[J]. 极地研究, 1997, 9(3):198-206.

    [LU Bing, TANG Yunqian, SUI Liangren. The biomarker compounds in surfacial sediments from the Bransfield Strait, Antarctica[J]. Chinese Journal of Polar Research, 1997, 9(3):198-206.]
    [13] 潘建明, 张海生, 程先豪, 等, 1998. 西南极海沉积硒的地球化学状态[J]. 海洋与湖沼, 29(4),424-430.[PAN Jianming, ZHANG Haisheng, CENG Xianhao, et al. Geochemical state of sedimentary selenium in western Antarctic ocean[J]. Oceanologia et Limnologia Sinica, 1998

    , 29(4):424-430.]
    [14] Duan Weiwu, Zhong Hexian, Li Yang. Late Quaternary glacial-marine sedimentation in the Bransfield Strait off northeast Antarctic Peninsula[J]. Antarctic Research, 1996, 7(1):19-33.
    [15] 王春娟, 陈志华, 李全顺, 等. 南极半岛周边海域表层沉积物粒度分布特征及其环境指示意义[J]. 极地研究, 2014, 26(1):128-138.

    [WANG Chunjuan,CEN Zhihua,LI Quanshun, et al. Distributions of surface sediments surrounding the Antarctic Peninsula and its environmental significance[J]. Chinese Journal of Polar Research, 2014, 26(1):128-138.]
    [16] 刘忠诚, 陈志华, 金秉福, 等. 南极半岛东北部海域碎屑矿物特征与物源分析[J]. 极地研究, 2014, 26(1):139-150.

    [LIU Zhongcheng, CHEN Zhihua, JIN Bingfu, et al. Characteristics and provenance of clastic minerals in surface sediments in the waters northeast of the Antarctic Peninsula[J]. Chinese Journal of Polar Research, 2014, 26(1):128-138.]
    [17] 王中刚,于学元,赵振华.稀土元素地球化学[M].北京:科学出版社,1989.[WANG Zhonggang, YU Xueyuan, ZHAO Zhenhua. Geochemistry of Rare Earth Elements[M]. Beijing, Science Press, 1989.]
    [18] 赵一阳, 鄢明才.中国浅海沉积物地球化学[M].北京:科学出版社,1994,130-150.[ZHAO Yiyang, YAN Mincai. Sediment Geochemistry of Chinese Epicontiental Seas[M]. Beijing, Science Press, 1994, 130

    -150.]
    [19] 王银喜,沈炎彬. 南极乔治王岛晚白垩世火山岩Rb-Sr同位素定年及微量元素、稀土元素地球化学特征[C]//南极乔治王岛菲尔德斯半岛地层及古生物研究.北京,科学出版社,1994:109-131.[WANG Yinbin, SHEN Yanbi. Rb-Sr isotopic dating and trace element, REE geochemistry of Late Cretaceous volcanic rocks from King George Island, Antarctica[C]//SHEN Yanbin, ed. Stratigraphy and Paleontology of Fildes Peninsula, King George Island, Antarctica. Beijing:Science Press, 1994:109

    -131.]
    [20] Liu Xiaodong, Liguang Sun, Dan Li, et al. Rare earth elements in the ornithogenic sediments from the Maritime Antarctic:A potential new palaeoecology proxy[J]. Geochemical Journal, 2011, 45:15-26.
    [21] 王先兰,赵云龙.南极半岛西北部海区重矿物及其中稀土、微量元素的统计分析[J]. 南极研究, 1989, 1(3):34-43.

    [WANG Xianlan, ZHAO Yunlong. Mathematical statistics of heavy minerals and their REE and trace elements in the northwestern sea area of Antarctic Peninsula[J]. Antarctic Research, 1989, 1(3):34-43.]
    [22] Lee J I, Park B K, Jwa Y J, et al. Geochemical characteristics and the provenance of sediments in the Bransfield Strait, West Antarctica[J]. Marine Geology, 2005, 219:81-98.
    [23] Eaglesa G, Livermore R A. Opening history of Powell Basin, Antarctic Peninsula[J]. Marine Geology, 2002, 185:195-205.
    [24] Jiang M, Charette M A, Measures C I, et al. Seasonal cycle of circulation in the Antarctic Peninsula and the off-shelf transport of shelf waters into southern Drake Passage and Scotia Sea[J]. Deep-Sea Research Ⅱ, 2013, 90:15-30.
    [25] Maldonado A, Barnolas A, Bohoyo F, et al. Contourite deposits in the central Scotia Sea:the importance of the Antarctic Circumpolar Current and the Weddell Gyre flows[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2003, 198(1-2):187-221.
    [26] Howe J A, Livermore R A, Maldonado A. Mudwave activity and current-controlled sedimentation in Powell Basin, northern Weddell Sea, Antarctica[J]. Marine Geology, 1998, 149:229-241.
    [27] Sangra P, Gordo C, Hernandez-Arencibia M. The Bransfield current system[J]. Deep-Sea Research I, 2011, 58:390-402.
    [28] Schodlok M P, Hellmer H H, Rohardt G, et al. Weddell Sea iceberg drift:five years of observations[J]. J. Geophys. Res., 2006, 111:C06018. doi:10.1029/2004JC002661.
    [29] Diekmann B, Kuhn G. Provenance and dispersal of glacial-marine surface sediments in the Weddell Sea and adjoining areas, Antarctica:ice-rafting versus current transport[J]. Marine Geology, 1999, 158:209-231.
    [30] Byrne R H, Sholkovitz E R. The marine chemistry and geochemistry of the lanthanides[M]//The Handbook of the Physics and Chemistry of Rare Earths. Elsevier, 1996:497-593.
    [31] 中国南极考察队. 南大洋考察报告(南极半岛西北部海区), 1984-1985[R]. 北京:海洋出版社, 1987:289-293.[Chinese National Antarctic Research Expedition. Observational Report on the Southern Ocean Research (the Sea Area Northwest of the Antarctic Peninsula), 1984-1985

    [R]. Beijing:Ocean Publications, 1987:289-293.]
    [32] German C R, Masuzawa T, Greaves M J, et al. Dissolved rare earth elements in the Southern Ocean:Cerium oxidation and the influence of hydrography[J]. Geochimica et Cosmochimica Acta, 1995, 59(8):1551-1558.
    [33] Comiso J C, Cavalieri D J, Markus T. Sea ice concentration, ice temperature, and snow depth using AMSR-E data[J]. Geoscience and Remote Sensing, 2003, 41(2):243-252.
    [34] Anderson J B. Antarctic Marine Geology[M]. Cambridge University Press, 1999.
    [35] Caggianelli A, Fiore S, Mongelli G, et al. REE distribution in the clay fraction of pelites from the southern Apennines, Italy[J]. Chem. Geol., 1992, 99:253-263.
    [36] 杨杰东, 徐士进. 同位素与全球环境变化[M]. 北京:地质出版社, 2007:141-147.[YANG Jiedong,XU Shijin. Isotopes and Global Environmental Changes[M]. Beijing:Geological Publications, 2007:141

    -147.]
    [37] 刘嘉麒,张雯华,郭正府.南极南设得兰群岛中-新生代火山作用与地质环境[J]. 极地研究, 2002, 14(1):1-11.

    [LIU Jiaqi, ZHANG Wenhua, GUO Zhengfu, et al. Mesozoic-Cenozoic volcanism and geological environment in the South Shetland Islands, Antarctica[J]. Chinese Journal of Polar Research, 2002, 14(1):1-11.]
    [38] 匡福祥,金庆民.乔治王岛菲尔德斯半岛火山岩地球化学及生成与演化[J].中国地质科学院南京地质矿产所所刊, 1989, 10(1):1-11.

    [KUANG Fuxiang, JIN Qingmin. Geochemistry, origin and evolution of the volcanic rocks in Fildes Peninsula, King George Island[J]. Bull. Nanjing Inst. Geol. M. R., Chinese Acad. Geol. Sci., 1989, 10(1):1-11.]
    [39] 聂森艳,王汝建,肖文申.南极半岛Bransfield海峡约6000年以来的陆源组分记录及其古环境意义[J]. 第四纪研究, 2014, 34(3):590-599.

    [NIE Sunyan, WANG Ruijian, XIAO Wenshen et al. A 6000 year record of terrigeneous compositions from the Bransfield Strait, Antarctic Peninsula:responses to climate change[J]. Quaternary Sciences, 2014, 34(3):590-599.]
    [40] Gabrielli P, Wegner A, Petit J R. A major glacial-interglacial change in aeolian dust composition inferred from Rare Earth Elements in Antarctic ice[J]. Quaternary Science Reviews, 2010, 29:265-273.
    [41] Gallet S, Jahn B, Lanoe B V V, et al. Loess geochemistry and its implications for particle origin and composition of the upper continental crust[J]. Earth and Planetary Science Letters, 1998, 156:157-172.
  • [1] 密蓓蓓, 张勇, 梅西, 王忠蕾, 窦衍光.  南黄海表层沉积物稀土元素分布特征及其物源指示意义 . 海洋地质与第四纪地质, 2022, 42(6): 93-103. doi: 10.16562/j.cnki.0256-1492.2022072901
    [2] 齐文菁, 李小艳, 范德江, 张辉, 殷征欣, 刘升发.  印度洋东经90°海岭现代沉积物稀土元素组成及其物源示踪意义 . 海洋地质与第四纪地质, 2022, 42(2): 92-100. doi: 10.16562/j.cnki.0256-1492.2021050701
    [3] 孙兴全, 刘升发, 李景瑞, 曹鹏, 张辉, 赵广涛, SomkiatKhokiattiwong, NarumolKornkanitnan, 石学法.  孟加拉湾南部表层沉积物稀土元素组成及其物源指示意义 . 海洋地质与第四纪地质, 2020, 40(2): 80-89. doi: 10.16562/j.cnki.0256-1492.2019102801
    [4] 杨木壮, 何韵.  南极半岛西侧别林斯高晋海陆缘含水合物系统及资源潜力 . 海洋地质与第四纪地质, 2019, 39(4): 136-147. doi: 10.16562/j.cnki.0256-1492.2018111202
    [5] 林刚, 陈琳莹, 罗敏, 陈多福.  西太平洋新不列颠海沟表层沉积物的地球化学特征及其物源指示 . 海洋地质与第四纪地质, 2019, 39(3): 12-27. doi: 10.16562/j.cnki.0256-1492.2018060701
    [6] 胡思谊, 曾志刚, 殷学博, 朱博文, 方雪, 齐海燕.  冲绳海槽岩心沉积物稀土元素特征及物源指示 . 海洋地质与第四纪地质, 2019, 39(1): 69-82. doi: 10.16562/j.cnki.0256-1492.2017082301
    [7] 苏妮, 毕磊, 郭玉龙, 杨守业.  木兰溪河口及邻近海域表层沉积物稀土元素组成与物源判别 . 海洋地质与第四纪地质, 2018, 38(1): 150-159. doi: 10.16562/j.cnki.0256-1492.2018.01.015
    [8] 郭玉龙, 杨守业, 苏妮, 印萍, 王中波.  中国东南入海河流沉积物的稀土元素地球化学特征 . 海洋地质与第四纪地质, 2018, 38(1): 139-149. doi: 10.16562/j.cnki.0256-1492.2018.01.014
    [9] 邬黛黛, 杨飞, 黄霞, 潘梦迪, 孙甜甜, 刘丽华, 吴能友.  南海东沙海域冷泉渗漏区沉积物稀土元素地球化学特征 . 海洋地质与第四纪地质, 2017, 37(5): 59-69. doi: 10.16562/j.cnki.0256-1492.2017.05.006
    [10] 仇建东, 王双, 刘健, 张勇, 孔祥淮.  山东半岛南部滨浅海区QDZ03孔稀土元素组成与物源判别 . 海洋地质与第四纪地质, 2016, 36(6): 143-151. doi: 10.16562/j.cnki.0256-1492.2016.06.017
    [11] 郭敏, 徐利强.  巢湖沉积物稀土元素地球化学特征及环境意义 . 海洋地质与第四纪地质, 2016, 36(4): 137-144. doi: 10.16562/j.cnki.0256-1492.2016.04.016
    [12] 李景瑞, 刘升发, 冯秀丽, 孙兴全, 石学法.  孟加拉湾中部表层沉积物稀土元素特征及其物源指示意义 . 海洋地质与第四纪地质, 2016, 36(4): 41-50. doi: 10.16562/j.cnki.0256-1492.2016.04.005
    [13] 曹鹏, 石学法, 李巍然, 刘升发, 朱爱美, 杨刚, Somkiat Khokiattiwong, Narumol Kornkanitnan.  安达曼海东南部海域表层沉积物稀土元素特征及其物源指示意义 . 海洋地质与第四纪地质, 2015, 35(5): 57-67. doi: 10.16562/j.cnki.0256-1492.2015.05.007
    [14] 张晓波, 张勇, 孔祥淮, 李安龙, 刘珊珊, 褚宏宪, 林曼曼.  山东半岛南部近岸海域表层沉积物稀土元素的物源指示 . 海洋地质与第四纪地质, 2014, 34(3): 57-66. doi: 10.3724/SP.J.1140.2014.03057
    [15] 徐兆凯, 李铁刚, 李安春.  东菲律宾海表层沉积物来源的稀土证据 . 海洋地质与第四纪地质, 2013, 33(2): 1-7. doi: 10.3724/SP.J.1140.2013.02001
    [16] 徐刚, 刘健, 孔祥淮, 张军强, 仇建东.  南黄海西部陆架区表层沉积物稀土元素及其物源分析 . 海洋地质与第四纪地质, 2012, 32(1): 11-17. doi: 10.3724/SP.J.1140.2012.01011
    [17] 朱爱美, 刘季花, 张辉, 白亚之, 崔菁菁, 刘升发.  东海内陆架泥质区表层沉积物稀土元素的分布特征 . 海洋地质与第四纪地质, 2012, 32(1): 1-10. doi: 10.3724/SP.J.1140.2012.01001
    [18] 蔡观强, 邱燕, 彭学超, 钟和贤.  南海西南海域表层沉积物微量和稀土元素地球化学特征及其意义 . 海洋地质与第四纪地质, 2010, 30(5): 53-62. doi: 10.3724/SP.J.1140.2010.05053
    [19] 赵青芳, 龚建明, 李双林, 贺行良, 付少英.  南海神狐海域表层沉积物稀土元素地球化学 . 海洋地质与第四纪地质, 2010, 30(1): 65-70. doi: 10.3724/SP.J.1140.2010.01065
    [20] 孔祥淮, 刘健, 李巍然, 张宪军, 梁源.  山东半岛东北部滨浅海区表层沉积物的稀土元素及其物源判别 . 海洋地质与第四纪地质, 2007, 27(3): 51-59.
  • 加载中
计量
  • 文章访问数:  2121
  • HTML全文浏览量:  260
  • PDF下载量:  19
  • 被引次数: 0
出版历程
  • 收稿日期:  2015-04-10
  • 修回日期:  2015-04-24

南极半岛东北部海域表层沉积物稀土元素特征及物源指示意义

doi: 10.3724/SP.J.1140.2015.03145
    作者简介:

    陈志华(1970-),男,博士,研究员,主要从事海洋地质学研究,Email:chenzia@fio.org.cn

基金项目:

南北极环境综合考察与评估专项(CHINARE2014-01-02,CHINARE2015-01-02,CHINARE2014-04-01,CHINARE2015-04-01)

国家自然科学基金项目(40176136,41106166)

  • 中图分类号: P736.4

摘要: 通过对南极半岛东北部海域36个表层沉积物样品的稀土元素分析发现:(1)研究区表层沉积物中稀土元素总量(REE)的分布范围为(45.47~183.60)×10-6,平均值为91.36×10-6;稀土元素含量的高低与铝硅酸盐黏土成正比,与生物硅含量成反比;(2)大致以象岛至南极半岛北部的茹安维尔岛为界,研究区西部的布兰斯菲尔德海峡及南设得兰群岛北部岛架-岛坡沉积物稀土含量较低,稀土元素页岩标准化模式与长城站周边土壤/湖泊沉积物、火山岩相一致,表现为重稀土相对富集,铕正异常明显,Sm/Nd分子比值大,推断该区沉积物主要来源于南设德兰群岛中-新生代火山岩分布区与现代火山活动区;(3)研究区东部鲍威尔海盆、南奥克尼群岛岛架和南斯科舍海脊区沉积物稀土元素的页岩标准化配分模式表现为平坦型,轻稀土明显抬升,铕正异常不显著,Sm/Nd分子比值小,稀土元素含量受沉积物中黏土组分含量、硅质生物组分等制约,推断沉积物陆源碎屑主要来源于威德尔海西部和南部,局部受南奥尼克群岛、南斯科舍海脊和南设德兰群岛物质的影响,沉积物的搬运主要受冰筏和海流制约。

English Abstract

参考文献 (41)

目录

    /

    返回文章
    返回