Sediment characteristics and paleoenvironmental significance of Core DLW3101 from northern slope of the South China Sea

Zhou Hang; Liu Lejun; Xu Yuanqin; Zhou Qingjie; Gao Shan

doi:10.3969/j.issn.0253-4193.2018.07.009

Article Contents

Article Navigation > Haiyang Xuebao > 2018 > 40(7): 103-115

Zhou Hang, Liu Lejun, Xu Yuanqin, Zhou Qingjie, Gao Shan. Sediment characteristics and paleoenvironmental significance of Core DLW3101 from northern slope of the South China Sea[J]. Haiyang Xuebao, 2018, 40(7): 103-115. doi: 10.3969/j.issn.0253-4193.2018.07.009

Citation:

Zhou Hang, Liu Lejun, Xu Yuanqin, Zhou Qingjie, Gao Shan. Sediment characteristics and paleoenvironmental significance of Core DLW3101 from northern slope of the South China Sea[J]. Haiyang Xuebao, 2018, 40(7): 103-115. doi: 10.3969/j.issn.0253-4193.2018.07.009

Citation:

Zhou Hang, Liu Lejun, Xu Yuanqin, Zhou Qingjie, Gao Shan. Sediment characteristics and paleoenvironmental significance of Core DLW3101 from northern slope of the South China Sea[J]. Haiyang Xuebao, 2018, 40(7): 103-115. doi: 10.3969/j.issn.0253-4193.2018.07.009

PDF( 21668 KB)

Sediment characteristics and paleoenvironmental significance of Core DLW3101 from northern slope of the South China Sea

doi: 10.3969/j.issn.0253-4193.2018.07.009

1.
The First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China
2.
Marine Engineering Environment & Geomatic Center, The First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China
3.
Key Laboratory of Marine Sedimentology and Environmental Geology, The First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China

Received Date: 2017-08-07
Rev Recd Date: 2018-03-05

Abstract

Abstract

Using the oxygen isotope stratigraphy method to establish the age mode of core DLW3101.The bottom of the core is about 306 ka old. Based on this age mode the sediments were used to make grain-size and XRF element scanning test. The conclusion shows that high values of 22.1-63 μm grades may reveal the enhancement of East Asian winter monsoon and the decline of the sea level. High values of 0.35-1.16 μm and 2.32-13.14 μm grades may reveal the enhancement of East Asian summer monsoon and the rise of the sea level. Al/Ti and K/Ti ratio are adopted to reflect chemical weathering degree of sediments source area in order to reveal the strength of East Asian summer monsoon.
- northern slope of the South China Sea,
- grain size,
- geochemical element,
- sea level,
- East Asian monsoon

FullText(HTML)

References(46)

References

金海燕,翦知湣,谢昕,等. 南海北部晚第四纪高分辨率元素比值反映的东亚季风演变[J].第四纪研究,2011,31(2):207-215. Jin Haiyan, Jian Zhimin, Xie Xin, et al. Late quaternary East Asian monsoonal evolution recorded by high resolution elemental ratios in the northern South China Sea[J].Quaternary Research,2011,31(2):207-215.

Wang P X, Prell W L, Blum P, et al. Proceeding of the Ocean Drilling Program, Initial Reports[R]. Texas A & M University, Ocean Drilling Program College Station 184, 2000.

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. Zhao Quanhong, Wang Pinxian. Progress in quaternary paleoceanography of the South China Sea:a review[J]. Quaternary Research, 1999, 19(6):481-501.

业治铮,汪品先. 南海晚第四纪古海洋学研究[M]. 青岛:青岛海洋大学出版社, 1992:1-324. Ye Zhizheng, Wang Pinxian. The Paleoceanographic Study of the Late Quaternary in the South China Sea[M]. Qingdao:Qingdao Ocean University Press, 1992:1-324.

汪品先. 十五万年来的南海[M]. 上海:同济大学出版社, 1995:1-184. Wang Pinxian. The South China Sea for 150000 Years[M]. Shanghai:Tongji University Press, 1995:1-184.

Wei Gangjian, Liu Ying, Li Xianhua. Major and trace element variations of the sediments at ODP Site 1144,South China Sea,during the last 230 ka and their paleoclimate implications[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004, 212:331-342.

刘坚,陆红锋,苏新,等. 南海北部BY1钻孔沉积物元素地球化学特征及其古环境意义[J]. 热带海洋学报, 2012, 31(5):6-11. Liu Jian, Lu Hongfeng, Su Xin, et al. Element geochemistry of Core BY1 from the northern South China Sea and its paleoenvironmental implication[J]. Journal of Tropical Oceanography, 2012, 31(5):6-11.

赵宏樵,韩喜彬,陈荣华,等. 南海北部191柱状沉积物主元素特征及其古环境意义[J]. 海洋学报, 2008, 30(6):85-93. Zhao Hongqiao, Han Xibin, Chen Ronghua, et al. Charicteristics of main elements and their paleoenvironment significance of Core 191 in the northern South China Sea[J]. Haiyang Xuebao, 2008, 30(6):85-93.

梅西,张训华,郑洪波,等. 南海南部120 ka以来元素地球化学记录的东亚夏季风变迁[J]. 矿物岩石地球化学通报, 2010, 29(2):134-141. Mei Xi, Zhang Xunhua, Zheng Hongbo, et al. Element geochemistry record in southern South China Sea sediments during the past 120 ka and its implications for East Asian summer monsoon variation[J]. Bulletin of Mineralogy,Petrology and Geochemistry Bull Mineral,Petrol Geochem, 2010, 29(2):134-141.

王成,龚庆杰,李刚,等. 从南海沉积物中的主量元素比值变化看沉积物源区化学侵蚀变化[J]. 海洋地质动态, 2007, 23(1):1-5. Wang Cheng, Gong Qingjie, Li Gang, et al. Study on chemical erosion variations in source area of the sediment from the South China Sea sediments' main element ratio[J]. Marine Geology Letters, 2007, 23(1):1-5.

郑洪波,陈国成,谢昕,等. 南海晚第四纪陆源沉积:粒度组成、动力控制及反映的东亚季风演化[J]. 第四纪研究, 2008, 29(3):414-424. Zheng Hongbo, Chen Guocheng, Xie Xin, et al. Grain size distribution and dynamic control of late quaternary terrigenous sediments in the South China Sea and their impalication for East Asian monsoon evolution[J]. Quaternary Research, 2008, 29(3):414-424.

万世明,李安春. 南海北部ODP1146站粒度揭示的近20 Ma以来东亚季风演化[J]. 中国科学D辑:地球科学, 2007, 37(6):761-770. Wan Shiming, Li Anchun. The evolution of East Asian monsoon since nearly 20 Ma revealed from granularity of ODP1146 station in the north of the South China Sea[J]. Science in China Series D:Earth Science, 2007,37(6):761-770.

杨文光, 郑洪波, 王可,等. 南海东北部MD05-2905站36 ka BP以来的陆源碎屑沉积特征与东亚季风的演化[J]. 地球科学进展, 2007, 22(10):1012-1018. Yang Wenguang, Zheng Hongbo, Wang Ke, et al. Sedimentary characteristic of terrigenous clast of Site MD05-2905 in the northeastern part of South China Sea after 36 ka and evolution of East Asian monsoon[J]. Advances in Earth Science, 2007, 22(10):1012-1018.

李小洁, 梁莲姬, 吴枫,等. 南海北部沉积物常量元素变化、碳酸盐旋回及其古环境意义[J]. 第四纪研究, 2015, 35(2):411-421. Li Xiaojie, Liang Lianji, Wu Feng, et al. Variations of major elements and carbonate cycle of the northern South China Sea sediments and their paleoenvironmental significance[J]. Quaternary Research, 2015, 35(2):411-421.

陈宇亮,郑洪波. XRF岩心扫描在第四纪沉积物研究中的应用[J]. 海洋地质前沿,2014,30(4):51-59. Chen Yuliang, Zheng Hongbo. The application of XRF core scanning to quatermaty sediments[J]. Marine Geology Frontiers, 2014,30(4):51-59.

张晓楠,张灿,吴铎,等. 基于XRF岩心扫描的中国西部湖泊沉积物元素地球化学特征[J]. 海洋地质与第四纪地质,2015,35(1):163-174. Zhang Xiaonan, Zhang Can, Wu Duo, et al. Element geochemistry of lake deposits measured by X-Ray fluorescence core scanner in northwest China[J]. Marine Geology & Quaternary Geology, 2015,35(1):163-174.

贺子丁,刘志飞,李建如,等. 南海西部54万年以来元素地球化学记录及其反映的古环境演变[J]. 地球科学进展,2012,27(3):327-336. He Ziding, Liu Zhifei, Li Jianru, et al. Elemental geochemical records in the western South China Sea since 540 ka and their paleoenvironmental implications[J]. Advances in Earth Science, 2012,27(3):327-336.

周航. 南海北部陆坡DLW3101孔沉积物特征及古环境意义[D]. 青岛:国家海洋局第一海洋研究所,2016. Zhou Hang. Sediment characteristics and paleoenvironmental significance of Core DLW3101 from northern slope of South China Sea[D]. Qingdao:The First Institute of Oceanography, State Oceanic Administration,2016.

Wang P X. Glacial carbonate cycles in western pacific marginal seas[J]. Marine Geology & Quaternary Geology, 1998, 18(1):1-11.

李学杰, 刘坚, 陈芳,等. 南海北部晚更新世以来的碳酸盐旋回[J]. 第四纪研究, 2008, 28(3):431-436. Li Xuejie, Liu Jian, Chen Fang, et al. Carbonate cycles since late Pleistocene in the northern South China Sea[J]. Quaternary Research, 2008, 28(3):431-436.

Syvitski J P M. Factor analysis of size frequency distributions:significance of factor solutions based on simulation experiments[M]//Principles, Methods and Applications Particle Size Analysis. Cambridge:Cambridge University Press, 1991:249-263.

Prins M A, Postma G, Weltje G. Controls on the terrigenous sediment supply to the Arabian Sea during the late Quaternary:The Makran continental slope[J]. Marine Geology, 2000,169(3/4):351-371.

薛积彬,钟巍. 干旱区湖泊沉积物粒度组分记录的区域沙尘活动历史:以新疆巴里刊湖为例[J]. 沉积学报,2008, 26(4):647-654. Xue Jibin, Zhong Wei. Variations in dust event reflected by grain-size component of lacustrine records in droughty area:a case study on Barkol Lake, Xinjiang, China[J]. Acta Sedimentologica Sinica,2008, 26(4):647-654.

陈桥,刘东艳,陈颖军,等. 粒级-标准偏差法和主成分因子分析法在粒度敏感因子提取中的对比[J]. 地球与环境,2013,41(3):319-325. Chen Qiao, Liu Dongyan, Chen Yingjun, et al. Comparative analysis of grade-standard deviation method and factors analysis method for environmental sensitive factor analysis[J]. Earth and Environment, 2013,41(3):319-325.

Yang Shouye, Jung H S, Lim D. A review on the provenance discrimination of sediments in the Yellow Sea[J]. Earth-Science Reviews, 2003,63(1/2):93-120.

Yang Shouye, Youn J S. Geochemical compositions and provenance discrimination of the central south Yellow Sea sediments[J]. Marine Geology, 2007, 243(1/4):229-241.

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. Zhao yiyang, Yan Mingcai. Sediment Geochemistty of the China Shelf Sea[M]. Beijing:Science Press, 1994.

肖尚斌,李安春,蒋富清,等. 近2 ka来东海内陆架泥质沉积物地球化学特征[J]. 地球化学, 2005, 34(6):595-604. Xiao Shangbin, Li Anchun, Jiang Fuqing, et al. Geochemical characteristics of recent 2 ka mud on the inner shelf of the East China Sea[J]. Geochimica, 2005, 34(6):595-604.

刘建国,李安春,陈木宏,等. 全新世渤海泥质沉积物地球化学特征[J]. 地球化学, 2007, 36(6):559-568. Li Jianguo, Li Anchun, Chen Muhong, et al. Geochemical characteristics of sediments in the Bohai Sea mud area during Holocene[J]. Geochimica, 2007, 36(6):559-568.

杜德文,石学法,孟宪伟,等. 黄海沉积物地球化学的粒度效应[J]. 海洋科学进展, 2003, 21(1):78-82. Du Dewen, Shi Xuefa, Meng Xianwei, et al. Geochemical granularity effect of sediment in the Yellow Sea[J]. Advances in Marine Science, 2003, 21(1):78-82.

徐方建,李安春,万世明,等. 东海内陆架陆源物质矿物组成对粒度和地球化学成分的制约[J]. 地球科学:中国地质大学学报, 2009, 34(4):613-622. Xu Fangjian, Li Anchun, Wan Shiming, et al. Terrigenous mineral constrains on the grain-size distribution and geochemical composition of sediments in the inner shelf of the East China Sea[J]. Earth Science:Journal of China University of Geosciences, 2009, 34(4):613-622.

Yang Shouye, Li Congxian, Cai Jingong. Geochemical compositions of core sediments in eastern China:Implication for Late Cenozoic palaeoenvironmental changes[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 229(4):287-302.

Liu Jianguo, Steinke S, Vogt C, et al. Temporal and spatial patterns of sediment deposition in the northern South China Sea over the last 50,000 years[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2016,465:212-224.

Xun Xiangjun, Luo Yunli, Huang Fei, et al. Deep-sea pollen from the South China Sea:Pleistocene indicators of East Asian Monsoon[J]. Marine Geology,2003,201(1/3):97-118.

罗运利,陈怀成,吴国瑄,等. 南海最近3个冰期旋回中的天然火与气候——ODP1144孔深海沉积中的炭屑记录[J]. 中国科学,2001,31(10):854-860. Luo Yunli, Chen Huaicheng, Wu Guoxuan, et al. Natural fire and climate change in the last 3 glacial cycles in the South China Sea-carbon dioxide records in deep sea sediments of ODP1144 station[J]. Scientia Sinica, 2001,31(10):854-860.

Boulay S, Colin C, Trentesaux A. et al. Mineralogy and sedimentology of pleistocene sediment of the South China Sea(ODP1144)[J]. Proceedings of the Ocean Drilling Program Scientific Results,2003,184:1-21.

Wang L, Sarnthein M, Erlenkeuser H, et al. East Asian monsoon climate during the Late Pleistocene:high resolution sediment records from the South China Sea[J]. Marine Geology,1999,156(1/4):245-284.

Tamburini F, Adatte T, Föllmi K, et al. Investigating the history of East Asian monsoon and climate during the last glacial-interglacial period (0-140000 years):mineralogy and geochemistry of ODP Sites 1143 and 1144, South China Sea[J]. Marine Geology, 2003, 201(1/3):147-168.

黄镇国, 张伟强, 江璐明. 中国热带MIS 3气候特征探讨[J]. 第四纪研究, 2003, 23(1):77-82. Huang Zhenguo, Zhang Weiqiang, Jiang Luming. Climatic characteristics in tropic areas of China during MIS3[J]. Quaternary Sciences, 2003, 23(1):77-82.

刘东生, 安芷生, 孙东怀,等. 最近0.6 Ma南、北半球古气候对比初探[J]. 中国科学D辑:地球科学, 1996, 26(2):97-102. Liu Dongsheng, An Zhisheng, Sun Donghuai, et al. A preliminary study of paleoclimate comparison in the southern and northern hemispheres of 0.6Ma[J]. Science in China Series D:Earth Science,1996, 26(2):97-102.

Dansgaard W, White J W C, Johnsen S J. The abrupt termination of the Younger Dryas climate event[J]. Nature, 1989, 339:532-534.

Alley R B, Marotzke J, Nordhaus W D. Abrupt climate change[J]. Science, 2003, 299(5615):2005-2010.

郑洪波,杨文光,贺娟,等. 南海的氧同位素3期[J]. 第四纪研究, 2008, 29(1):68-78. Zheng Hongbo, Yang Wenguang, He Juan, et al. Marine isotope stage (MIS3) of South China Sea[J]. Quaternary Sciences, 2008, 29(1):68-78.

Zhang P Z, Molnar P, Downs W. Increased sedimentation rates and grain size 2-4 Myr ago due to the influence of climate changes on erosion rates[J]. Nature,2001,410:891-897.

梅西. 南海南部晚第四纪以来沉积与地球化学记录及古环境意义[D]. 上海:同济大学,2008. Mei Xi. Sedimentary and geochemical records and paleoenvironmental significance of the southern South China Sea since Late Quaternary[D]. Shanghai:Tongji University, 2008.

汪品先,翦知湣,赵泉鸿,等. 南海演变与季风历史的深海证据[J]. 科学通报, 2003, 48(21):2228-2239. Wang Pinxian, Jian Zhimin, Zhao Quanhong, et al. The evolution of the South China Sea and the monsoon history from the deep sea evidence[J].Chinese Science Bulletin, 2003, 48(21):2228-2239.

Relative Articles

Supplements(0)

Cited By

Proportional views