The provenance of clay minerals in core I8 from the West Philippine Basin

doi:10.3969/j.issn.1001-909X.2015.04.007

Abstract

Abstract: Clay mineral compositions of 35 samples in core I8 recovered from the West Philippine Basin were analyzed by X-ray diffraction (XRD) technique. The results show that the clay mineral assemblages in core I8 consist dominantly of illite (40%), with a lesser abundance of smectite (28%) and chlorite (20%), as well as a low amount of kaolinite (12%), and illite has good crystallinity. The source analysis of clay minerals indicate that the high contents of illite may come from the input of Asian dust, while smectite may be contributed by the nearby ocean bottom volcanoes, and weathering product from Luzon may play the most important role in providing chlorite and kaolinite.

Key words: clay minerals, provenance, the West Philippine Basin

CLC Number:

P736.3

SHU Yu-ting, ZHENG Yu-long, XU Dong, CHU Feng-you. The provenance of clay minerals in core I8 from the West Philippine Basin[J]. Journal of Marine Sciences, 2015, 33(4): 61-69.

References

[1] LAN Xian-hong. Paleoenvironmental significance of clay mineral assemblages in marine sediments [J]. Marine Geology Letters,2001,17(1):5-7.
蓝先洪.海洋沉积物中粘土矿物组合特征的古环境意义[J].海洋地质动态,2001,17(1):5-7.
[2] ZHANG Nai-xian, LI You-qin, ZHAO Hui-min, et al. Research methods of clay mineral [M]. Beijing: China Sciene Publishing & Media LTD,1990.
张乃娴,李幼琴,赵惠敏,等.粘土矿物研究方法[M].北京:科学出版社,1990.
[3] KONG Xiang-le, XIANG Hai-guang. A discussion on the study of clay minerals from ocean sediments and global change[J]. Transactions of Oceanology and Limnology, 2003(1):22-26.
孔祥乐,项海光.海洋沉积粘土矿物与全球变化研究的探讨[J].海洋湖沼通报,2003(1):22-26.
[4] TANG Yan-jie, JIA Jian-ye, XIE Xian-de. Environment significance of clay minerals[J]. Earth Science Frontiers,2002,9(2):337-344.
汤艳杰,贾建业,谢先德.粘土矿物的环境意义[J].地学前缘,2002,9(2):337-344.
[5] SUN Shou-xun, TENG Jun. Climate character of the Philippine Sea[J]. Marine Forecasts,2003,20(3):31-39.
孙守勋,滕军.菲律宾海的气候特征[J].海洋预报,2003,20(3):31-39.
[6] LI Chang-zhen, LI Nai-sheng, LIN Mei-hua. Terrain features of the Philippine Sea[J]. Marine Sciences,2000,24(6):47-51.
李常珍,李乃胜,林美华.菲律宾海的地势特征[J].海洋科学,2000,24(6):47-51.
[7] ZHANG Xuan, YU Mu-geng, JIANG Wei, et al. Hydrologic characteristic of the Philippine Sea and its nearby areas[J]. Marine Science Bulletin,2004,23(1):8-14.
张弦,俞慕耕,江伟,等.菲律宾海及其邻近海区的水文特征[J].海洋通报,2004,23(1):8-14.
[8] XU Zhao-kai, LI Tie-gang, WAN Shi-ming, et al. Evolution of East Asian monsoon: Clay mineral evidence in the western Philippine Sea over the past 700kyr[J]. Journal of Asian Earth Sciences,2012,60:188-196.
[9] SHI Xue-fa. Sedimentation and evolution of sedimentary environment of late Quaternary in the West of Philippine Sea[D]. Qingdao: Institute of Oceanology, Chinese Academy of Sciences,1992.
石学法.西菲律宾海晚第四纪沉积作用和沉积环境演化[D].青岛:中国科学院海洋研究所,1992.
[10] SHI Xue-fa, WANG Zong-liang. Study on minerageny of the clay sediment in the west of Philippine Sea[J]. Marine Geology & Quaternary Geology,1995,15(2):61-72.
石学法,王宗良.西菲律宾海西部海域粘土沉积物的成因矿物学研究[J].海洋地质与第四纪地质,1995,15(2):61-72.
[11] WAN Shi-ming, YU Zhao-jie, CLIFT P D, et al. History of Asian eolian input to the West Philippine Sea over the last one million years[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2012,326-328(2):152-159.
[12] WAN Shi-ming, LI An-chun, XU Ke-hui, et al. Characteristics of clay minerals in the northern South China Sea and its implications for evolution of east Asian monsoon since Miocene[J]. Earth Science: Journal of China University of Geosciences,2008,33(3):289-300.
万世明,李安春,胥可辉,等.南海北部中新世以来粘土矿物特征及东亚古季风记录[J].地球科学:中国地质大学学报,2008,33(3):289-300.
[13] CHI Ye, LI An-chun, JIANG Fu-qing, et al. Assemblage and provenance of clay minerals off the east of Luzon Island[J]. Marine Sciences,2009,33(9):80-88.
池野,李安春,蒋富清,等.吕宋岛东部海域黏土矿物组合特征及物源分析[J].海洋科学,2009,33(9):80-88.
[14] SEO I, LEE Y I, YOO C M, et al. Sr-Nd isotope composition and clay mineral assemblages in eolian dust from the central Philippine Sea over the last 600 kyr: Implications for the transport mechanism of Asian dust[J]. Journal of Geophysical Research: Atmospheres,2014,119(19):11 492-11 504.
[15] XIONG Zhi-fang, LI Tie-gang, ZHAI Bin, et al. Clay mineral characteristics of Ethmodiscus rex diatom mats from low-latitude Western Pacific during the last glacial and implications for their formation[J]. Earth Science: Journal of China University of Geosciences,2010,35(4):551-562.
熊志方,李铁刚,翟滨,等.低纬度西太平洋末次冰期Ethmodiscus rex硅藻席粘土矿物特征及形成机制启示[J].地球科学:中国地质大学学报,2010,35(4):551-562.
[16] MING Jie, LI An-chun, MENG Qing-yong, et al. Quaternary assemblage characteristic and provenance of clay minerals in the Parecevela Basin of the east Philippine Sea[J]. Marine Geology & Quaternary Geology,2012,32(4):139-148.
明洁,李安春,孟庆勇,等.东菲律宾海帕里西维拉海盆第四纪黏土矿物组合特征及物源分析[J].海洋地质与第四纪地质,2012,32(4):139-148.
[17] MING Jie, LI An-chun, HUANG Jie, et al. Assemblage characteristics of clay minerals and its implications to evolution of eolian dust input to the Parece Vela Basin since 1.95 Ma[J]. Chinese Journal of Oceanology and Limnology,2014,32(1):174-186.
[18] ZHAI Bin, LI Tie-gang, XIONG Zhi-fang, et al. Diatom records inferred from the diatom mat deposits from low-latitude Western Pacific in the last glacial period[J]. Journal of Tropical Oceanography,2012,31(4):75-82.
翟滨,李铁刚,熊志方,等.末次冰期低纬度西太平洋硅藻席沉积中的硅藻记录[J].热带海洋学报,2012,31(4):75-82.
[19] JIN Ning, LI An-chun, LIU Hai-zhi, et al. Clay minerals in surface sediment of the northwest Parecevela Basin: Distribution and provenance[J]. Oceanologia et Limnologia Sinica,2008,38(6):504-511.
靳宁,李安春,刘海志,等.帕里西维拉海盆西北部表层沉积物中黏土矿物的分布特征及物源分析[J].海洋与湖沼,2008,38(6):504-511.
[20] ZHANG De-yu. Clay mineral composition and distribution in the Mariana Trough[J]. Journal of Oceanography of Huanghai & Bohai Seas,1994,12(2):32-39.
张德玉.马里亚纳海槽区粘土矿物组成及分布特征[J].黄渤海海洋,1994,12(2):32-39.
[21] ZHANG De-yu. Clay mineralogy of the sediments deposited since the Pleistocene in the Mariana Trough and the West Philippine Basin[J]. Acta Sedimentologica Sinaca,1993,11(1):111-120.
张德玉.马里亚纳海槽和西菲律宾海盆更新世以来沉积物中的粘土矿物[J].沉积学报,1993,11(1):111-120.
[22] KOLLA V, NADLER L, BONATTI E. Clay mineral distributions in surface sediments of the Philippine Sea [J].Oceanologyca Acta,1980,3(2):245-250.
[23] ZHANG Bin, LI Guang-xue, HUANG Ji-feng. The tectonic geomorphology of the Philippine Sea[J]. Marine Geology & Quaternary Geology,2014,34(2):79-88.
张斌,李广雪,黄继峰.菲律宾海构造地貌特征[J].海洋地质与第四纪地质,2014,34(2):79-88.
[24] LEE I, OGAWA Y. Bottom-current deposits in the Miocene-Pliocene Misaki Formation, Izu forearc area, Japan[J]. Island Arc,1998,7(3):315-329.
[25] BISCAYE P E. Mineralogy and sedimentation of recent deep sea clay in the Atlantic Ocean and adjacent sea and oceans[J]. Bulletin of the Geological Society of Amercia,1965,76(7):803-832.
[26] XU Zhao-kai, LI An-chun, JIANG Fu-qing,et al. Grain-size and clay mineral characteristics of sediments under deep water ferromanganese crusts in the eastern Philippine Sea[J]. Acta Oceanologica Sinica,2007,29(2):150-155.
徐兆凯,李安春,蒋富清,等.东菲律宾海深水铁锰结壳发育站位沉积物的粒度及黏土矿物学特征[J].海洋学报,2007,29(2):150-155.
[27] LIU Zhi-fei, TRENTESAUX A, CLEMENS S C, et al. Clay mineral records in ODP1146 of the northern South China Sea slope since the Quaternary: Currents transport and evolution of East Asian Monsoon[J]. Science in China Ser. D: Earth Sciences,2003,33(3):271-280.
刘志飞,TRENTESAUX A, CLEMENS S C, et al. 南海北坡 ODP1146 站第四纪粘土矿物记录: 洋流搬运与东亚季风演化[J]. 中国科学 D 辑,2003,33(3):271-280.
[28] GINGELE F X. Holocene climatic optimum in Southwest Africa—Evidence from the marine clay mineral record[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,1996,122(1):77-87.
[29] EHRMANN W. Implications of late Eocene to early Miocene clay mineral assemblages in McMurdo Sound (Ross Sea, Antarctica) on paleoclimate and ice dynamics[J]. Palaeogeography Palaeoclimatology Palaeoecology,1998,139(3):213-231.
[30] CHAMLEY H. Clay sedimentology[M]. Springer-Verlag,1989.
[31] LIU Zhi-fei, LI Xia-jing, Discussion on smectite formation in South China Seasediments[J]. Quaternary Sciences,2011,31(2):199-206.
刘志飞,李夏晶.南海沉积物中蒙脱石的成因探讨[J].第四纪研究,2011,31(2):199-206.
[32] MING Jie. The characteristics and provenance of the sediment in the Parece Vela Basin since the Quaternary and their environmental implications[D].Qingdao: University of Chinese Academy of Sciences(Institute of Oceanology),2013.
明洁.东菲律宾海帕里西维拉海盆第四纪沉积特征和物质来源及其古环境意义[D].青岛:中国科学院研究生院(海洋研究所),2013.
[33] YU Zhao-jie. Research on Asian eolian input to the West Philippine Sea over the last one million years[D]. Qingdao: University of Chinese Academy of Sciences(Institute of Oceanology),2013.
于兆杰.近百万年以来西菲律宾海风尘沉积研究[D].青岛:中国科学院研究生院(海洋研究所),2013.
[34] SHI Xue-fa, CHEN Li-rong, MA Jian-guo, et al. REE Geochemistry of sediments from West Philippine sea [J]. Acta Mineralogica Sinica,1996,16(3):260-267.
石学法,陈丽蓉,马建国,等.西菲律宾海沉积物稀土元素地球化学[J].矿物学报,1996,16(3):260-267.
[35] SHI Yu-xin, DAI Xue-rong, SONG Zhi-guang, et al. Characteristics of clay mineral assanblages and their spatial distribution of Chinese Loess in different climatic Zones[J]. Acta Sedmentologica Sinica,2006,23(4):690-695.
师育新,戴雪荣,宋之光,等.我国不同气候带黄土中粘土矿物组合特征分析[J].沉积学报,2006,23(4):690-695.
[36] LI Guo-gang. Composition, distribution and geological significance of clay mineral in Chinese Offshore surface sediments[J]. Acta Oceanologica Sinica,1990,12(4):470-479.
李国刚.中国近海表层沉积物中粘土矿物的组成,分布及其地质意义[J].海洋学报:中文版,1990,12(4):470-479.
[37] LIU Zhi-fei, TUO Shou-tiong, COION C, et al. Detrital fine-grained sediment contribution from Taiwan to the northern South China Sea and its relation to regional ocean circulation[J]. Marine Geology,2008,255(3):149-155.
[38] YU Xu, CHAO Hua. Studie of modern marine sedimentary minerals and their X-ray diffraction[M]. Beijing: China Sciene Publishing & Media LTD,1984.
俞旭,超华.现代海洋沉积矿物及其X射线衍射研究[M].北京:科学出版社,1984.
[39] GRIFFIN J J, WINDOM H, GOLDBERG E D. The distribution of clay minerals in the World Ocean[J]. Deep Sea Research & Oceanographic Abstracts,1968,15(4):433-459.
[40] YANG Xian-zhong. Illite crystallinity and its geological significances[J]. Acta Sedimentologica Sinica,1993,11(4):92-98.
杨献忠.伊利石的结晶度及其地质意义综述[J].沉积学报,1993,11(4):92-98.
[41] SKONIECZNY C, BORY A, BOUT-ROUMAZEILLES V, et al. The 7-13 March 2006 major Saharan outbreak: Multiproxy characterization of mineral dust deposited on the West African margin[J]. Journal of Geophysical Research,2011,116(D18):597-616.
[42] SRINE C, ANNIE G, LAURENT G, et al. Saharan dust: Clay ratio as a relevant tracer to assess the origin of soil-derived aerosols[J]. Geophysical Research Letters,1998,25(7):983-986.
[43] GINGELE F X, DECKKER P D, HILLENBRAD C D. Clay mineral distribution in surface sediments between Indonesia and NW Australia-source and transport by ocean currents[J]. Marine Geology,2001,179(3):135-146.
[44] GINGELE F X, DECKKER P D. Fingerprinting Australias rivers with clay minerals and the application for the marine record of climate change[J]. Australian Journal of Earth Sciences,2004,51(3):339-348.
[45] LEINEN M, PROSPERO J M, ARNOLD E, et al. Mineralogy of aeolian dust reaching the North Pacific Ocean: 1. Sampling and analysis[J]. Journal of Geophysical Research,1994,99(D10):21 017-21 023.
[46] ARNOLD E, MERRILL J, LEINEN M, et al. The effect of source area and atmospheric transport on mineral aerosol collected over the North Pacific Ocean, Global Planet[J]. Change,1998,18(3-4):137-159.
[47] BISCAYE P E, GROUSSET F E, REVEL M, et al. Asian provenance of glacial dust (stage 2) in the Greenland Ice Sheet Project 2 Ice Core, Summit, Greenland[J]. J Geophys Res,1997,102(C12):26 765-26 781.
[48] ZHANG Yong-shuang, QU Yong-xin. Quantitative research on clay mineral composition of the Malan Loess from the Loess Plateau in China[J]. Geological Review,2005,50(5):530-537.
张永双,曲永新.黄土高原马兰黄土粘土矿物的定量研究[J].地质论评,2005,50(5):530-537.
[49] GERVASIO F C. Age and nature of orogenesis of the Philippines[J]. Tectonophysics,1967,4(4):379-402.
[50] GIBBS R J. Clay mineral segregation in the marine environment[J]. Journal of Sedimentary Research,1977,47(1):237-243.