Grain-size characteristics of the surface clastic sediments on the southern margin of the Yap Trench and their provenance implications

CHEN Kang; XU Jishang; LI Guangxue; TIAN Ju; YANG Jichao; ZHOU Shang; SUN Siting

doi:10.16562/j.cnki.0256-1492.2019110601

Marine Geology & Quaternary Geology > 2020 > 40(5): 46-57. > DOI: 10.16562/j.cnki.0256-1492.2019110601

CHEN Kang, XU Jishang, LI Guangxue, TIAN Ju, YANG Jichao, ZHOU Shang, SUN Siting. Grain-size characteristics of the surface clastic sediments on the southern margin of the Yap Trench and their provenance implications[J]. Marine Geology & Quaternary Geology, 2020, 40(5): 46-57. DOI: 10.16562/j.cnki.0256-1492.2019110601

Citation:

PDF (12372 KB)

Grain-size characteristics of the surface clastic sediments on the southern margin of the Yap Trench and their provenance implications

CHEN Kang^1,2,,
XU Jishang^1,2,3,4, ,,
LI Guangxue^1,2,3,4,
TIAN Ju^1,2,
YANG Jichao⁵,
ZHOU Shang^1,2,
SUN Siting^1,2

1.
Key Lab of Submarine Geosciences and Prospecting Techniques, Ocean University of China, Qingdao 266100, China
2.
College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
3.
Engineering Research Center of Marine Petroleum Development and Security Safeguard, Ministry of Education, Qingdao 266100, China
4.
Pilot National Laboratory for Marine Science and Technology, Qingdao 266100, China
5.
National Deep Sea Center, Qingdao 266237, China

More Information

Received Date: November 05, 2019
Revised Date: January 08, 2020
Available Online: October 20, 2020

Graphical Abstract

Abstract

Abstract

The grain size characteristics of the surface detrital sediments near the southern margin of Yap trench and their implications for sediment provenance were studied. Results show that the sediments are dominated by silt and clay in the region. Using the method of grain size component separation, four components, M1, M2, M3 and M4, were separated from fine to coarse. Among them, M1 and M2 are wind dust, which are distributed throughout the study area. M3 and M4 are pyroclast and siliceous bioclast mainly distributed near the Yapu Trench and West Caroline Trough. The detrital particles are rather coarse in the Yap Trench and the West Caroline Trough, whereas the kurtosis figure is small and the sorting is poor, indicating a complex sediment source; the sediments in the West Caroline basin are relatively fine, with low kurtosis and poor sorting, showing a relatively complex material source; whereas the sediments on the West Caroline ridge are the finest with high kurtosis and good sorting, suggesting a rather simple sediment source. From the ridge, basin to the trough and trench, the clastic sediments gradually become coarser, and poorly sorted, with the provenance gradually becoming more complex. It suggests that the distribution of mineral composition of sediments are closely related to the tectonic environment.
- surface sediments,
- mineral detritus,
- grain size,
- provenance,
- Yap trench

FullText(HTML)

References (49)

References

[1]	秦启龙. 深海沉积物细菌和丝状真菌的基因组学研究[D]. 山东大学博士学位论文, 2010. QIN Qilong. Genomic studies of deep-sea sedimentary bacteria and filamentous fungus[D]. Doctor Dissertation of Shandong University, 2010.
[2]	Asahara Y, Tanaka T, Kamioka H, et al. Provenance of the north Pacific sediments and process of source material transport as derived from Rb-Sr isotopic systematics [J]. Chemical Geology, 1999, 158(3): 271-291.
[3]	Mahoney J B. Nd and Sr isotopic signatures of fine-grained clastic sediments: a case study of western Pacific marginal basins [J]. Sedimentary Geology, 2005, 182(1-4): 183-199. doi: 10.1016/j.sedgeo.2005.07.009
[4]	McLaren P. An interpretation of trends in grain size measures [J]. Journal of Sedimentary Research, 1981, 51(2): 611-624.
[5]	McLaren P, Bowles D. The effects of sediment transport on grain-size distributions [J]. Journal of Sedimentary Research, 1985, 55(4): 457-470.
[6]	Shi X F, Liu Y G, Chen Z H, et al. Origin, transport processes and distribution pattern of modern sediments in the Yellow Sea[M]//Li M Z, Sherwood C R, Hill P R. Sediments, Morphology and Sedimentary Processes on Continental Shelves: Advances in Technologies, Research, and Applications. Chichester: John Wiley & Sons, Inc., 2012: 321-350.
[7]	Gao S, Collins M. Net sediment transport patterns inferred from grain-size trends, based upon definition of “transport vectors” [J]. Sedimentary Geology, 1992, 81(1-2): 47-60. doi: 10.1016/0037-0738(92)90055-V
[8]	Gao S, Collins M B. Analysis of grain size trends, for defining sediment transport pathways in marine environments [J]. Journal of Coastal Research, 1994, 10(1): 70-78.
[9]	王伟, 李安春, 徐方建, 等. 北黄海表层沉积物粒度分布特征及其沉积环境分析[J]. 海洋与湖沼, 2009, 40(5):525-531. [WANG Wei, LI Anchun, XU Fangjian, et al. Distribution of surface sediments and sedimentary environment in the North Yellow Sea [J]. Oceanologia et Limnologia Sinica, 2009, 40(5): 525-531. doi: 10.3321/j.issn:0029-814X.2009.05.001
[10]	王汾连, 何高文, 王海峰, 等. 马里亚纳海沟柱状沉积物稀土地球化学特征及其指示意义[J]. 海洋地质与第四纪地质, 2016, 36(4):67-75. [WANG Fenlian, HE Gaowen, WANG Haifeng, et al. Geochemistry of rare earth elements in a core from Mariana trench and its significance [J]. Marine Geology & Quaternary Geology, 2016, 36(4): 67-75.
[11]	付锋, 郑洋, 姚旭莹, 等. 东太平洋CC区西区表层沉积物黏土矿物和地球化学特征[J]. 海洋学研究, 2017, 35(1):55-65. [FU Feng, ZHENG Yang, YAO Xuying, et al. Clay mineral and geochemical analysis of surface sediments in the western region of CC Zone in the East Pacific Ocean [J]. Journal of Marine Sciences, 2017, 35(1): 55-65. doi: 10.3969/j.issn.1001-909X.2017.01.007
[12]	周宇, 蒋富清, 徐兆凯, 等. 近2 Ma帕里西-维拉海盆沉积物中碎屑组分粒度特征及其物源和古气候意义[J]. 海洋科学, 2015, 39(9):86-93. [ZHOU Yu, JIANG Fuqing, XU Zhaokai, et al. Grain-size distribution of detrital sediment in the Parece Vela Basin and its implication of provenance and palaeoclimate over the last 2 Ma [J]. Marine Sciences, 2015, 39(9): 86-93. doi: 10.11759/hykx20140314001
[13]	周烨, 蒋富清, 南青云, 等. 奄美三角盆地晚更新世以来碎屑沉积物粒度特征及其物源和古气候意义[J]. 地球科学进展, 2016, 31(3):298-309. [ZHOU Ye, JIANG Fuqing, NAN Qingyun, et al. Grain-size distribution of detrital sediment in the Amami Sankaku Basin since late pleistocene and its provenance and palaeoclimate implications [J]. Advances in Earth Science, 2016, 31(3): 298-309. doi: 10.11867/j.issn.1001-8166.2016.03.0298.
[14]	张正一, 董冬冬, 张广旭, 等. 板块俯冲侵蚀雅浦岛弧的地形制约[J]. 海洋地质与第四纪地质, 2017, 37(1):41-50. [ZHANG Zhengyi, DONG Dongdong, ZHANG Guangxu, et al. Topographic constraints on the subduction erosion of the Yap arc, Western Pacific [J]. Marine Geology & Quaternary Geology, 2017, 37(1): 41-50.
[15]	瞿洪宝, 郑彦鹏, 刘晨光, 等. 晚始新世以来雅浦海沟-岛弧构造演化模式[J]. 海洋科学进展, 2017, 35(2):249-257. [QU Hongbao, ZHENG Yanpeng, LIU Chenguang, et al. Model of tectonic evolution for Yap Trench-arc since late Eocene [J]. Advances in Marine Science, 2017, 35(2): 249-257. doi: 10.3969/j.issn.1671-6647.2017.02.009
[16]	宫士奇. 雅浦海山区海底地形及海山形态特征研究与分析[D]. 中国科学院研究生院(海洋研究所)硕士学位论文, 2015. GONG Shiqi. Topographic and geomorphologic features and analyses of the seafloor and seamounts in the Yap seamounts area[D]. Master Dissertation of the Institute of Oceanology, Chinese Academy of Sciences, 2015.
[17]	董冬冬, 张广旭, 钱进, 等. 西太平洋雅浦俯冲带的地貌及地层结构特征[J]. 海洋地质与第四纪地质, 2017, 37(1):23-29. [DONG Dongdong, ZHANG Guangxu, QIAN Jin, et al. Geomorphology and stratigraphic framework of the Yap subduction zone, Western Pacific [J]. Marine Geology & Quaternary Geology, 2017, 37(1): 23-29.
[18]	张晋, 李安春, 万世明, 等. 南海南部表层沉积物粒度分布特征及其影响因素[J]. 海洋地质与第四纪地质, 2016, 36(2):1-10. [ZHANG Jin, LI Anchun, WAN Shiming, et al. Grain size distribution of surface sediments in the southern South China Sea and influencing factors [J]. Marine Geology & Quaternary Geology, 2016, 36(2): 1-10.
[19]	Weissel J K, Anderson R N. Is there a Caroline plate? [J]. Earth and Planetary Science Letters, 1978, 41(2): 143-158. doi: 10.1016/0012-821X(78)90004-3
[20]	Gaina C, Müller D. Cenozoic tectonic and depth/age evolution of the Indonesian gateway and associated back-arc basins [J]. Earth-Science Reviews, 2007, 83(3-4): 177-203. doi: 10.1016/j.earscirev.2007.04.004
[21]	刘子洲, 李培良, 王雪竹, 等. 太平洋气候态环流场的数值模拟及其季节性变化特征[J]. 中国海洋大学学报, 2013, 43(11):17-26. [LIU Zizhou, LI Peiliang, WANG Xuezhu, et al. Climatological simulation of Pacific Ocean circulation and analysis of its seasonal variability [J]. Periodical of Ocean University of China, 2013, 43(11): 17-26.
[22]	Hu D X, Wu L X, Cai W J, et al. Pacific western boundary currents and their roles in climate [J]. Nature, 2015, 522(7556): 299-308. doi: 10.1038/nature14504
[23]	Lukas R, Yamagata T, McCreary J P. Pacific low-latitude western boundary currents and the Indonesian throughflow [J]. Journal of Geophysical Research, 1996, 101(C5): 12209-12216. doi: 10.1029/96JC01204
[24]	Siedler G, Holfort J, Zenk W, et al. Deep-water flow in the Mariana and Caroline basins [J]. Journal of Physical Oceanography, 2004, 34(3): 566-581. doi: 10.1175/2511.1
[25]	Jiang F Q, Zhou Y, Nan Q Y, et al. Contribution of Asian dust and volcanic material to the western Philippine Sea over the last 220 kyr as inferred from grain size and Sr-Nd isotopes [J]. Journal of Geophysical Research, 2016, 121(9): 6911-6928.
[26]	田举. 雅浦海沟南缘及附近海域表层沉积物特征和物源研究[D]. 中国海洋大学硕士学位论文, 2019. TIAN Ju. Properties and Source analysis of the surface sediments in the southern margin of Yapu Trench and adjacent areas[D]. Master Dissertation of Ocean University of China, 2019.
[27]	Mortlock R A, Froelich P N. A simple method for the rapid determination of biogenic opal in pelagic marine sediments [J]. Deep Sea Research Part A. Oceanographic Research Papers, 1989, 36(9): 1415-1426. doi: 10.1016/0198-0149(89)90092-7
[28]	DeMaster D J. The supply and accumulation of silica in the marine environment [J]. Geochimica et Cosmochimica Acta, 1981, 45(10): 1715-1732. doi: 10.1016/0016-7037(81)90006-5
[29]	Demaster D J. Measuring biogenic silica in marine sediments and suspended matter[M]//Hurd D C, Spencer D W. Marine Particles: Analysis and Characterization, Volume 63. Washington: American Geophysical Union, 1991: 363-367.
[30]	Conley D J. An interlaboratory comparison for the measurement of biogenic silica in sediments [J]. Marine Chemistry, 1998, 63(1-2): 39-48. doi: 10.1016/S0304-4203(98)00049-8
[31]	贾建军, 高抒, 薛允传. 图解法与矩法沉积物粒度参数的对比[J]. 海洋与湖沼, 2002, 33(6):577-582. [JIA Jianjun, GAO Shu, XUE Yunchuan. Grain-size parameters derived from graphic and moment methods: a comparative study [J]. Oceanologia et Limnologia Sinica, 2002, 33(6): 577-582. doi: 10.3321/j.issn:0029-814X.2002.06.002
[32]	徐兴永, 易亮, 于洪军, 等. 图解法和矩值法估计海岸带沉积物粒度参数的差异[J]. 海洋学报, 2010, 32(2):80-86. [XU Xingyong, YI Liang, YU Hongjun, et al. The differences of grain-size parameters estimated with graphic and moment methods in coastal sediments [J]. Acta Oceanologica Sinica, 2010, 32(2): 80-86.
[33]	Friedman G M, Johnson K G. Exercises in Sedimentology[M]. New York: Wiley, 1982: 68-83.
[34]	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]. 中国科学院研究生院(海洋研究所)博士学位论文, 2013. MING Jie. The characeristics and provenance of the sediment in the Parece Vela Basin since the Quaternary and their environmental implications[D]. Doctor Dissertation of the Institute of Oceanology, Chinese Academy of Science, 2013.
[35]	张富元, 章伟艳, 杨群慧. 南海东部海域沉积物粒度分布特征[J]. 沉积学报, 2003, 21(3):452-460. [ZHANG Fuyuan, ZHANG Weiyan, YANG Qunhui. Characteristics of grain size distributions of surface sediments in the eastern South China sea [J]. Acta Sedimentologica Sinica, 2003, 21(3): 452-460. doi: 10.3969/j.issn.1000-0550.2003.03.014
[36]	Qin X G, Cai B G, Liu T S. Loess record of the aerodynamic environment in the east Asia monsoon area since 60,000 years before present [J]. Journal of Geophysical Research, 2005, 110(B1): B01204.
[37]	Wan S M, Yu Z J, 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: 152-159. doi: 10.1016/j.palaeo.2012.02.015
[38]	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, 2014, 119(19): 11492-11504.
[39]	于兆杰, 万世明, 孙晗杰, 等. 近百万年来亚洲风尘在西菲律宾海的沉积物粒度记录[J]. 地球环境学报, 2012, 3(2):792-800. [YU Zhaojie, WAN Shiming, SUN Hanjie, et al. Grain-size records of Asian eolian input to the West Philippine Sea over the last one million years [J]. Journal of Earth Environment, 2012, 3(2): 792-800. doi: 10.7515/JEE201202005
[40]	Leinen M. Quartz content of northwest Pacific Hole 576A and implications for Cenozoic eolian transport[R]. Initial Reports of the Deep Sea Drilling Proiect, 1985, 86: 581-588.
[41]	孙东怀, 安芷生, 苏瑞侠, 等. 最近2.6 Ma中国北方季风环流与西风环流演变的风尘沉积记录[J]. 中国科学(D辑), 2003, 46(10):1049-1059. [SUN Donghuai, AN Zhisheng, SU Ruixia, et al. Eolian sedimentary records for the evolution of monsoon and westerly circulations of northern China in the last 2.6 Ma [J]. Science in China Series D: Earth Sciences, 2003, 46(10): 1049-1059. doi: 10.1007/BF02959400
[42]	Ohara Y, Fujioka K, Ishizuka O, et al. Peridotites and volcanics from the Yap arc system: implications for tectonics of the southern Philippine Sea Plate [J]. Chemical Geology, 2002, 189(1-2): 35-53. doi: 10.1016/S0009-2541(02)00062-1
[43]	Yang Y M, Wu S G, Gao J W, et al. Geology of the Yap Trench: new observations from a transect near 10°N from manned submersible Jiaolong [J]. International Geology Review, 2018, 60(16): 1941-1953. doi: 10.1080/00206814.2017.1394226
[44]	Taira K, Kitagawa S, Yamashiro T, et al. Deep and bottom currents in the Challenger Deep, Mariana Trench, measured with super-deep current meters [J]. Journal of Oceanography, 2004, 60(6): 919-926. doi: 10.1007/s10872-005-0001-y
[45]	Turnewitsch R, Falahat S, Stehlikova J, et al. Recent sediment dynamics in hadal trenches: evidence for the influence of higher-frequency (tidal, near-inertial) fluid dynamics [J]. Deep Sea Research Part I: Oceanographic Research Papers, 2014, 90: 125-138. doi: 10.1016/j.dsr.2014.05.005
[46]	Luo M, Gieskes J, Chen L Y, et al. Provenances, distribution, and accumulation of organic matter in the southern Mariana Trench rim and slope: implication for carbon cycle and burial in hadal trenches [J]. Marine Geology, 2017, 386: 98-106. doi: 10.1016/j.margeo.2017.02.012
[47]	蒋富清, 李安春, 李铁刚. 冲绳海槽南部柱状沉积物地球化学特征及其古环境意义[J]. 海洋地质与第四纪地质, 2002, 22(3):11-17. [JIANG Fuqing, LI Anchun, LI Tiegang. Geochemical characteristics for core sediments of the southern Okinawa Trough and their paleoenvironment implication [J]. Marine Geology & Quaternary Geology, 2002, 22(3): 11-17.
[48]	李传顺. 冲绳海槽西南端中全新世以来的沉积特征及其物源与环境意义[D]. 中国科学院研究生院(海洋研究所)博士学位论文, 2009. LI Chuanshun. The characteristics and provenance of the sediment in the southwestern Okinawa Trough since the mid-Holocene and their environmental implications[D]. Doctor Dissertation of the Institute of Oceanology, Chinese Academy of Science, 2009.
[49]	何起祥. 海洋沉积作用的物源控制[J]. 海洋地质前沿, 2011, 27(1):8-13. [HE Qixiang. Sediment source and its bearing on marine sedimentation [J]. Marine Geology Frontiers, 2011, 27(1): 8-13.

Cited By

Cited by

Periodical cited type(10)

1.	杨名名，张一帆，李杏筠，周圆. 华南岬湾海滩冲淤演变特征及其机制分析——以南澳岛前江湾为例. 海洋技术学报. 2024(02): 43-57 .
2.	李华勇，袁俊英，杨艺萍，梁志姣，李智慧，吴帅虎，张虎才. 山东弥河流域现代洪水沉积特征与水动力过程反演. 海洋地质与第四纪地质. 2022(02): 178-189 . 本站查看
3.	李华勇，赵楠，杨艺萍，于正松，孙启发，吴帅虎，张曼，张虎才. 山东丹河2018年洪水沉积特征、物源分析及水文过程重建. 地质力学学报. 2022(02): 226-236 .
4.	李平，杜军，张志卫，徐国强. 粤东南澳岛青澳海滩侵蚀退化风险评价及其安全调控. 海洋科学进展. 2020(01): 171-181 .
5.	李华勇，唐倩玉，张虎才，李婷，段立曾. MS2000激光粒度仪测量第四纪沉积物粒度的定量进样研究. 海洋地质与第四纪地质. 2020(02): 200-207 . 本站查看
6.	张桂华，刘洪妍，介冬梅，刘颖，蒙萌，王江永，高桂在，李德晖，李楠楠，牛洪昊，冷程程. 科尔沁沙地不同类型沙丘表土有机质与粒度特征差异分析. 生态环境学报. 2020(11): 2223-2230 .
7.	杨文卿，孙立广，杨仲康，高抒，高月嵩，邵达，梅衍俊，臧晶晶，王玉宏，谢周清. 南澳宋城:被海啸毁灭的古文明遗址. 科学通报. 2019(01): 107-120 .
8.	李强，张学华. 基于遗传算法的BP神经网络模型在预测海洋沉积物烧失量中的应用. 冶金分析. 2019(04): 25-30 .
9.	刘勇，潘雪花，向莉芳，袁智郴，杨作治，李正西，赵增友. 贵州西部高原末次冰消期气候记录及古环境意义. 绿色科技. 2019(24): 174-178 .
10.	刘璇，张永战，夏非，王嵘，任珊，WüNNEMANN Bernd. 北海南部Lunden湾全新世沉积环境演变. 地理研究. 2017(11): 2261-2276 .

Other cited types(19)

Get Citation

PDF

XML

Article views (2130) PDF downloads (52) Cited by(29)

Turn off MathJax

Article Contents

Abstract

References

Grain-size characteristics of the surface clastic sediments on the southern margin of the Yap Trench and their provenance implications