Sensitive Grain Size and its Environmental Significance of Modern Mud Patches in Southern and Northern Parts of the Yellow Sea

SHEN Xing; CHU ZhongXin; WANG YueMing; LI YingKun; MIAO AnYang; LIANG YuLei

doi:10.14027/j.cnki.cjxb.2015.01.013

Volume 33 Issue 1

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SHEN Xing, CHU ZhongXin, WANG YueMing, LI YingKun, MIAO AnYang, LIANG YuLei. Sensitive Grain Size and its Environmental Significance of Modern Mud Patches in Southern and Northern Parts of the Yellow Sea[J]. Acta Sedimentologica Sinica, 2015, 33(1): 124-133. doi: 10.14027/j.cnki.cjxb.2015.01.013

Citation:

SHEN Xing, CHU ZhongXin, WANG YueMing, LI YingKun, MIAO AnYang, LIANG YuLei. Sensitive Grain Size and its Environmental Significance of Modern Mud Patches in Southern and Northern Parts of the Yellow Sea[J]. Acta Sedimentologica Sinica, 2015, 33(1): 124-133. doi: 10.14027/j.cnki.cjxb.2015.01.013

Sensitive Grain Size and its Environmental Significance of Modern Mud Patches in Southern and Northern Parts of the Yellow Sea

doi: 10.14027/j.cnki.cjxb.2015.01.013

1.
Ocean University of China, College of Marine Geosciences, Qingdao, Shandong 266100;
2.
The Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of Education, Qingdao, Shandong 266100

Received Date: 2014-01-08
Rev Recd Date: 2014-05-12
Publish Date: 2015-02-10

Abstract

High resolution (0.5 cm) grain size analysis by laser particle size analyzer and ²¹⁰Pb dating of two short cores collected from the mud patches of central part of the southern Yellow Sea (Core YSZD01) and western part of the northern Yellow Sea (Core B45) were performed. Our results show that Core B45, which was deposited from 1913 to 2010, is mainly composed of silt, and its grain size parameters fluctuate vertically. The main sediment of Core YSZD01, which was developed from 1909 to 2012, is mud and sandy mud, and its grain size parameters change little along the core length. Sand fractions in the two cores around 1958, 1971 and 1980 are abruptly increased. We argue that strong cold-air outbreaks probably occurred in the study area, which enhanced ocean hydrodynamics and thereby resulted in abrupt increase in coarse fraction. By the grain size-standard deviation method, we got the environmental sensitive grain size components of Cores B45 and YSZD01, 15.6~71.8 μm and 23.7~500.0 μm, respectively, which are used to indicate variations of the East Asian Monsoon since 1910. The increased percentages of sensitive components during four periods of 1925~1935, 1955~1964, 1974~1977, and 1982~1986, are consistent with significant increase of the East Asian winter monsoon. It seems that the changes in content and fluctuation of sensitive grain size component in the mud patches of the Yellow Sea can be used to indicate variations in intensity and frequency of the East Asian Winter Monsoon.
- Yellow Sea,
- mud patch,
- grain size,
- sensitive grain size component,
- East Asian Monsoon

References

[1]	杨旭辉,冯秀丽,褚忠信,等. 中国东部陆架表层沉积物粒度特征及其沉积环境浅析[J]. 中国海洋大学学报:自然科学版,2012,42(7/8):126-134.[Yang Xuhui, Feng Xiuli, Chu Zhongxin, et al. Surface sediment distribution and sedimentary environment on the east China continental shelf[J]. Periodical of Ocean University of China: Natural Science Edition, 2012, 42(7/8): 126-134.]
[2]	蓝先洪,张训华,张志珣. 南黄海沉积物的物质来源及运移研究[J]. 海洋湖沼通报,2005(4):53-60.[Lan Xianhong, Zhang Xunhua, Zhang Zhixun. Material sources and transportation of sediments in the southern Yellow Sea[J]. Transaction of Oceanology and Limnology, 2005(4): 53-60.]
[3]	周晓静,李安春,万世明,等. 东海陆架表层沉积物粘土矿物组成分布特征及来源[J]. 海洋与湖沼,2010,41(5):667-675.[Zhou Xiaojing, Li Anchun, Wan Shiming, et al. Clay minerals in surfacial sediments of the East China Sea shelf: distribution and provenance[J]. Oceanologia et Limnologia Sinica, 2010, 41(5): 667-675.]
[4]	李正刚,初凤友,张富元,等. 南海西北部内陆架表层沉积物的重矿物分布及其控制因素[J]. 海洋地质与第四纪地质,2011,31(4):89-96.[Li Zhenggang, Chu Fengyou, Zhang Fuyuan, et al. Distribution pattern of heavy minerals in the surface sediments on inner shelf, northwest South China Sea and controlling factors[J]. Marine Geology and Quaternary Geology, 2011, 31(4): 89-96.]
[5]	王中波,杨守业,张志珣,等. 东海陆架中北部沉积物粒度特征及其沉积环境[J]. 海洋与湖沼,2012,43(6):1039-1049.[Wang Zhongbo, Yan Shouye, Zhang Zhixun, et al. The grain size compositions of the surface sediments in the East China Sea: indication for sedimentary environments [J]. Oceanologia et Limnologia Sinica, 2012, 43(6): 1039-1049.]
[6]	梅西,张训华,李日辉. 南黄海中部泥质沉积区 DLC70-3 孔稀土元素及环境意义[J]. 地质科技情报,2011,30(4):21-28.[Mei Xi, Zhang Xunhua, Li Rihui. REE of DLC70-3 core sediments from mud areas in the central south Yellow Sea and its environmental significance [J]. Geological Science and Technology Information, 2011, 30(4): 21-28.]
[7]	胡利民,石学法,郭志刚,等. 南黄海柱状沉积物中烃类化合物的地球化学特征及其对沉积环境的指示[J]. 沉积学报,2013,31(1):108-119.[Hu Limin, Shi Xuefa, Guo Zhigang, et al. Geochemical characteristics of hydrocarbons in the core sediments from the south Yellow Sea and its implication for the sedimentary environment [J]. Acta Sedimentologica Sinica, 2013, 31(1): 108-119.]
[8]	王飞飞,丁璇,刘健. 南黄海西部陆架氧同位素3期以来的古沉积环境演化[J]. 微体古生物学报,2012,29(3): 235-252.[Wang Feifei, Ding Xuan, Liu Jian. Paleoenvironmental evolution in the western shelf of the southern Yellow Sea since the marine isotope stage 3[J]. Acta Micropalaeontologica Sinica, 2012, 29(3): 235-252.]
[9]	蓝先洪,申顺喜. 南黄海中部沉积岩芯的微体古生物组合特征及古环境演化[J]. 海洋湖沼通报,2004(3):16-21.[Lan Xianhong, Shen Shunxi. Micropaleontological assemblage characteristics of sediment cores from the centre of the southern Yellow Sea and palaeoenvironmental evolvement [J]. Transaction of Oceanology and Limnology, 2004(3): 16-21.]
[10]	王飞飞,王红,刘健,等. 南黄海西北部SYS-0803孔第四纪晚期底栖有孔虫群落特征及其古环境意义[J]. 海洋地质与第四纪地质,2011,31(4):113-123.[Wang Feifei, Wang Hong, Liu Jian,et al. Late Quaternary benthic foraminifera of Core SYS-0803 from the northwestern south Yellow Sea and their paleoenviromental significance [J]. Marine Geology and Quaternary Geology, 2011, 31(4): 113-123.]
[11]	孙荣涛,李铁刚,常凤鸣. 全新世北黄海泥质区环境演化的底栖有孔虫记录[J]. 海洋地质与第四纪地质,2010,30(5):83-90.[Sun Rongtao, Li Tiegang, Chang Fengming. Distribution of benthic foraminifera and its bearing on marine environmental factors in the north Yellow Sea surface sediments[J]. Marine Geology and Quaternary Geology, 2010, 30(5): 83-90.]
[12]	于非,张志欣,刁新源,等. 黄海冷水团演变过程及其与邻近水团关系的分析[J]. 海洋学报,2006,28(5):26-34.[Yu Fei, Zhang Zhixin, Diao Xinyuan, et al. Analysis of evolution of the Huanghai Sea cold water mass and its relationship with adjacent water masses [J]. Acta Oceanologica Sinica, 2006, 28(5): 26-34.]
[13]	姚志刚,鲍献文,李娜,等. 北黄海冷水团季节变化特征分析[J]. 中国海洋大学学报:自然科学版,2012,42(6):9-15.[Yao Zhigang, Bao Xianwen, Li Na, et al. Seasonal evolution of the northern Yellow Sea cold water mass [J]. Periodical of Ocean University of China: Natural Science Edition, 2012, 42(6): 9-15.]
[14]	苏纪兰,黄大吉. 黄海冷水团的环流结构[J]. 海洋与湖沼,1995,26(5):1-7.[Su Jilan, Huang Daji. On the current field associated with the Yellow Sea cold water mass [J]. Oceanologia et Limnologia Sinica, 1995, 26(5): 1-7.]
[15]	向荣,杨作升,郭志刚,等. 济州岛西南泥质区粒度组分变化的古环境应用[J]. 地球科学,2005,30(5):582-588.[Xiang Rong, Yan Zuosheng, Guo Zhigang, et al. Paleoenvironmental implications of grain-size component variations in the mud area southwest off Cheju Island, ECS[J].Earth Science, 2005, 30(5): 582-588.]
[16]	孙东怀,安芷生,苏瑞侠,等. 古环境中沉积物粒度组分分离的数学方法及其应用[J]. 自然科学进展,2001,11(3):269-276.[Sun Donghuai, An Zhisheng, Su Ruixia, et al. Mathematical approach to sedimentary component partitioning of polymodal sediments and its applications[J].Progress in Natural Science, 2001, 11(3): 269-276.]
[17]	Sun Donghuai, Bloemendal J, Rea D K, et al. Grain-size distribution function of polymodal sediments in hydraulic and Aeolian environments, and numerical partitioning of the sedimentary components[J]. Sedimentary Geology, 2002, 152(3/4): 263-277.
[18]	向荣,杨作升,Satio Y,等. 济州岛西南泥质区近2300a来环境敏感粒度组分记录的东亚冬季风变化[J]. 中国科学(D 辑):地球科学,2006,36(7):654-662.[Xiang Rong, Yan Zuosheng, Satio Y, et al. Variation of East Asia winter monsoon according grain-size component records in the mud area southwest off Cheju Island for 2300 year recently[J].Science China (Seri. D): Earth Sciences, 2006, 36(7): 654-662.]
[19]	肖尚斌,李安春. 东海内陆架泥区沉积物的环境敏感粒度组分[J]. 沉积学报,2005,23(1):122-129.[Xiao Shangbin, Li Anchun. A study on environmentally sensitive grain-size population in inner shelf of the East China Sea[J]. Acta Sedimentologica Sinica, 2005, 23(1): 122-129.]
[20]	石学法,申顺喜,Yi H I,等. 南黄海现代沉积环境及动力沉积体系[J]. 科学通报,2001,46(增刊):1-6.[Shi Xuefa, Shen Shunxi, Yi H I,et al. Modern sedimentary environments and dynamic depositional systems in the southern Yellow Sea[J]. Chinese Science Bulletin, 2001, 46(Suppl. ): 1-6.]
[21]	Hu Dunxin. Upwelling and sedimentation dynamics [J]. Chinese Journal of Oceanology and Limnology, 1984, 2(1): 12-19.
[22]	Liu J P, Milliman J D, Gao Shu, et al. Holocene development of the Yellow River's subaqueous delta, north Yellow Sea[J]. Marine Geology, 2004, 209(1/4): 45-67.
[23]	Liu J P, Milliman J D, Gao S. The Shandong mud wedge and post-glacial sediment accumulation in the Yellow Sea [J]. Geo-Marine Letters, 2001, 21(4): 212-218.
[24]	高抒. 中国东部陆架全新世沉积体系:过程—产物关系研究进展评述[J]. 沉积学报,2013,31(5):845-855.[Gao Shu. Holocene sedimentary systems over the Bohai,Yellow and East China Sea region: recent progress in the study of process-product relationships[J]. Acta Sedimentologica Sinica, 2013, 31(5): 845-855.]
[25]	Folk R L, Andrews P B, Lewis D W. Detrital sedimentary rock classification and nomenclature for use in New Zealand[J]. New Zealand Journal of Geology and Geophysics, 1970, 13(4): 937-968.
[26]	McManus J. Grain size determination and interpretation[C]//Tucker M. Techniques in Sedimentology. Oxford: Blackwell, 1988:63-85.
[27]	齐君,李凤业,宋金明. 黄海和渤海沉积物²¹⁰Pb活度的分布特征[J]. 地球化学,2005,34(4):351-356.[Qi Jun, Li Fengye, Song Jinming. Distribution of ²¹⁰Pb activity of sediments in the Yellow and Bohai seas [J]. Geochimica, 2005, 34(4): 351-356.]
[28]	秦蕴珊,赵一阳,陈丽蓉,等. 黄海地质[M]. 北京:海洋出版社,1989:289.[Qin Yunshan, Zhao Yiyang, Chen Lirong, et al. Geology of the East China Sea [M]. Beijing: Science Press, 1989: 289.]
[29]	Prins M A, Postma G, Weltje G J. Controls on terrigenous sediment supply to theArabian Sea during the Late Quaternary: the Makran continental slope [J]. Marine Geology, 2000, 169(3): 351-371.
[30]	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.
[31]	Boulay S, Colin C, Trentesaux A,et al. Mineralogy and sedimentology of Pleistocene sediment in the South China Sea (ODP Site 1144)[C]// Prell W L, Wang P, Blum P, et al. Proceedings of the Ocean Drilling Program, Scientific Results, 2003, 184(211): 1-21.
[32]	董礼先,苏纪兰,王康墡. 黄渤海潮流场及其与沉积物搬运的关系[J]. 海洋学报,1989,11(1):102-114.[Dong Lixian, Su Jilan, Wang Kangshan. Tidal current field and it's effect on sediment transport within Yellow sea and Bohai Sea [J]. Acta Oceanologica Sinica, 1989, 11(1): 102-114.]
[33]	郭志刚,杨作升,雷坤, 等. 东海陆架北部泥质区沉积动力过程的季节性变化[J]. 青岛海洋大学学报:自然科学版,1999,29(3):507-513.[Guo Zhigang, Yang Zuosheng, Lei Kun, et al. Seasonal variation of the sedimentary dynamic processes for the mud area in the northern East China Sea [J]. Journal of Ocean University of Qingdao: Natural Science Edition, 1999, 29(3):507-513.]
[34]	Chu Z X, Sun X G, Zhai S K,et al. Changing pattern of accretion/erosion of the modern Yellow River (Huanghe) subaerial delta, China: Based on remote sensing images [J]. Marine Geology, 2006, 227(1/2): 13-30.
[35]	冯士筰. 风暴潮的研究进展[J]. 世界科技研究与发展,1998,20(4):44-47.[Feng Shizuo. The advance of researches on storm surges [J]. World Sci-Tech R & D, 1998, 20(4): 44-47.]
[36]	王遵娅,丁一汇. 近53年中国寒潮的变化特征及其可能原因[J]. 大气科学,2006, 30(6):1068-1076.[Wang Zuiya, Ding Yihui. Climate change of the cold wave frequency of China in the last 53 years and the possible reasons [J]. Chinese Journal of Atmospheric Sciences, 2006, 30(6): 1068-1076.]
[37]	张秀芝,黄秀芬,李江龙,等. 一百多年来影响黄渤海热带气旋天气气候分析[J]. 海洋预报,1997,14(4):11-21.[Zhang Xiuzhi, Huang Aifeng, Li Jianglong, et al. Weather and climatic analysis of tropical cyclone in the Yellow and Bohai Sea within more than one hundred years [J]. Marine Forecasts, 1997, 14(4): 11-21.]
[38]	孙有斌,高抒,李军. 边缘海陆源物质中环境敏感粒度组分的初步分析[J]. 科学通报,2003,48(1):83-86.[Sun Youbin, Gao Shu, Li Jun. Preliminary analysis of grain-size populations with environmentally sensitive terrigenous components in marginal sea setting [J]. Chinese Science Bulletin, 2003, 48(1): 83-86.]
[39]	肖尚斌,张京穗,陈木宏,等. 从陆架泥质沉积中寻找高分辨率的全新世东亚季风记录[J]. 三峡大学学报:自然科学版,2007,29(4):342-347.[Xiao Shangbin, Zhang Jingsui, Chen Muhong,et al. Exploring high-resolution records of the Holocene East Asian Monsoon from mud sediments on shelves of China marginal seas [J]. Journal of China Three Gorges University: Natural Sciences, 2007, 29(4): 342-347.]
[40]	肖尚斌,李安春,蒋富清,等. 近2ka来东海内陆架的泥质沉积记录及其气候意义[J]. 科学通报,2004,49(21):2233-2238.[Xiao Shangbin, Li Anchun, Jiang Fuqing, et al. The 2 ka record and its climate significance of the mud area of inner shelf of the East China Sea [J]. Chinese Science Bulletin, 2004, 49(21): 2233-2238.]
[41]	肖尚斌,李安春,陈木宏,等. 近8ka东亚冬季风变化的东海内陆架泥质沉积记录[J]. 地球科学,2005,30(5):573-581.[Xiao Shangbin, Li Anchun, Chen Muhong, et al. Recent 8 ka mud records of the East Asian Winter Monsoon from the inner shelf of the East China Sea [J]. Earth Science, 2005, 30(5): 573-581.]
[42]	万世明,李安春,Jan-Berend W S,等. 南海北部ODP1146站粒度揭示的近20Ma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, Jan-Berend W S, et al. East Asia Winter Monsoon change of recent 20Ma from grain size analysis of ODP1146 site from north of South China Sea [J]. Science China(Seri. D): Earth Sciences, 2007, 37(6): 761-770.]
[43]	徐建军,朱乾根. 近百年东亚冬季风的突变性和周期性[J]. 应用气象学报,1999,10(1):1-8.[Xu Jianjun, Zhu Qiangen. Sudden and periodic changes of East Asian Winter Monsoon in the past century [J]. Journal of Applied Meteorological Science, 1999, 10(1): 1-8.]
[44]	郭其蕴,蔡静宁,邵雪梅,等. 1873~ 2000年东亚夏季风变化的研究[J]. 大气科学,2004,28(2):206-215.[Guo Qiyun, Cai Jingning, Shao Xuemei, et al. Studies on the variations of East-Asian Summer Monsoon during A D 1873~2000[J]. Chinese Journal of Atmospheric Sciences, 2004, 28(2): 206-215.]
[45]	陈隆勋,朱乾根,罗会邦,等. 东亚季风[M]. 北京:气象出版社,1991:1-347.[Chen Longxun, Zhu Qiangen, Luo Huibang, et al. The Monsoon of East Asia [M]. Beijing: China Meteorological Press, 1991: 192-244.]
[46]	施能,鲁建军,朱乾根. 东亚冬、夏季风百年强度指数及其气候变化[J]. 南京气象学院学报,1996,19(2):168-177.[Shi Neng, Lu Jianjun, Zhu Qiangen. East Asian Winter/Summer Monsoon intensity indices with their climatic change in 1873–1989[J]. Journal of Nanjing Institute of Meteorology, 1996, 19(2): 168-177.]

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Sensitive Grain Size and its Environmental Significance of Modern Mud Patches in Southern and Northern Parts of the Yellow Sea

1. Ocean University of China, College of Marine Geosciences, Qingdao, Shandong 266100;

2. The Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of Education, Qingdao, Shandong 266100

Received Date: 2014-01-08

Rev Recd Date: 2014-05-12

Publish Date: 2015-02-10

Key words:

Abstract: High resolution (0.5 cm) grain size analysis by laser particle size analyzer and ²¹⁰Pb dating of two short cores collected from the mud patches of central part of the southern Yellow Sea (Core YSZD01) and western part of the northern Yellow Sea (Core B45) were performed. Our results show that Core B45, which was deposited from 1913 to 2010, is mainly composed of silt, and its grain size parameters fluctuate vertically. The main sediment of Core YSZD01, which was developed from 1909 to 2012, is mud and sandy mud, and its grain size parameters change little along the core length. Sand fractions in the two cores around 1958, 1971 and 1980 are abruptly increased. We argue that strong cold-air outbreaks probably occurred in the study area, which enhanced ocean hydrodynamics and thereby resulted in abrupt increase in coarse fraction. By the grain size-standard deviation method, we got the environmental sensitive grain size components of Cores B45 and YSZD01, 15.6~71.8 μm and 23.7~500.0 μm, respectively, which are used to indicate variations of the East Asian Monsoon since 1910. The increased percentages of sensitive components during four periods of 1925~1935, 1955~1964, 1974~1977, and 1982~1986, are consistent with significant increase of the East Asian winter monsoon. It seems that the changes in content and fluctuation of sensitive grain size component in the mud patches of the Yellow Sea can be used to indicate variations in intensity and frequency of the East Asian Winter Monsoon.

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Reference (46)

[1]	杨旭辉,冯秀丽,褚忠信,等. 中国东部陆架表层沉积物粒度特征及其沉积环境浅析[J]. 中国海洋大学学报:自然科学版,2012,42(7/8):126-134.[Yang Xuhui, Feng Xiuli, Chu Zhongxin, et al. Surface sediment distribution and sedimentary environment on the east China continental shelf[J]. Periodical of Ocean University of China: Natural Science Edition, 2012, 42(7/8): 126-134.]
[2]	蓝先洪,张训华,张志珣. 南黄海沉积物的物质来源及运移研究[J]. 海洋湖沼通报,2005(4):53-60.[Lan Xianhong, Zhang Xunhua, Zhang Zhixun. Material sources and transportation of sediments in the southern Yellow Sea[J]. Transaction of Oceanology and Limnology, 2005(4): 53-60.]
[3]	周晓静,李安春,万世明,等. 东海陆架表层沉积物粘土矿物组成分布特征及来源[J]. 海洋与湖沼,2010,41(5):667-675.[Zhou Xiaojing, Li Anchun, Wan Shiming, et al. Clay minerals in surfacial sediments of the East China Sea shelf: distribution and provenance[J]. Oceanologia et Limnologia Sinica, 2010, 41(5): 667-675.]
[4]	李正刚,初凤友,张富元,等. 南海西北部内陆架表层沉积物的重矿物分布及其控制因素[J]. 海洋地质与第四纪地质,2011,31(4):89-96.[Li Zhenggang, Chu Fengyou, Zhang Fuyuan, et al. Distribution pattern of heavy minerals in the surface sediments on inner shelf, northwest South China Sea and controlling factors[J]. Marine Geology and Quaternary Geology, 2011, 31(4): 89-96.]
[5]	王中波,杨守业,张志珣,等. 东海陆架中北部沉积物粒度特征及其沉积环境[J]. 海洋与湖沼,2012,43(6):1039-1049.[Wang Zhongbo, Yan Shouye, Zhang Zhixun, et al. The grain size compositions of the surface sediments in the East China Sea: indication for sedimentary environments [J]. Oceanologia et Limnologia Sinica, 2012, 43(6): 1039-1049.]
[6]	梅西,张训华,李日辉. 南黄海中部泥质沉积区 DLC70-3 孔稀土元素及环境意义[J]. 地质科技情报,2011,30(4):21-28.[Mei Xi, Zhang Xunhua, Li Rihui. REE of DLC70-3 core sediments from mud areas in the central south Yellow Sea and its environmental significance [J]. Geological Science and Technology Information, 2011, 30(4): 21-28.]
[7]	胡利民,石学法,郭志刚,等. 南黄海柱状沉积物中烃类化合物的地球化学特征及其对沉积环境的指示[J]. 沉积学报,2013,31(1):108-119.[Hu Limin, Shi Xuefa, Guo Zhigang, et al. Geochemical characteristics of hydrocarbons in the core sediments from the south Yellow Sea and its implication for the sedimentary environment [J]. Acta Sedimentologica Sinica, 2013, 31(1): 108-119.]
[8]	王飞飞,丁璇,刘健. 南黄海西部陆架氧同位素3期以来的古沉积环境演化[J]. 微体古生物学报,2012,29(3): 235-252.[Wang Feifei, Ding Xuan, Liu Jian. Paleoenvironmental evolution in the western shelf of the southern Yellow Sea since the marine isotope stage 3[J]. Acta Micropalaeontologica Sinica, 2012, 29(3): 235-252.]
[9]	蓝先洪,申顺喜. 南黄海中部沉积岩芯的微体古生物组合特征及古环境演化[J]. 海洋湖沼通报,2004(3):16-21.[Lan Xianhong, Shen Shunxi. Micropaleontological assemblage characteristics of sediment cores from the centre of the southern Yellow Sea and palaeoenvironmental evolvement [J]. Transaction of Oceanology and Limnology, 2004(3): 16-21.]
[10]	王飞飞,王红,刘健,等. 南黄海西北部SYS-0803孔第四纪晚期底栖有孔虫群落特征及其古环境意义[J]. 海洋地质与第四纪地质,2011,31(4):113-123.[Wang Feifei, Wang Hong, Liu Jian,et al. Late Quaternary benthic foraminifera of Core SYS-0803 from the northwestern south Yellow Sea and their paleoenviromental significance [J]. Marine Geology and Quaternary Geology, 2011, 31(4): 113-123.]
[11]	孙荣涛,李铁刚,常凤鸣. 全新世北黄海泥质区环境演化的底栖有孔虫记录[J]. 海洋地质与第四纪地质,2010,30(5):83-90.[Sun Rongtao, Li Tiegang, Chang Fengming. Distribution of benthic foraminifera and its bearing on marine environmental factors in the north Yellow Sea surface sediments[J]. Marine Geology and Quaternary Geology, 2010, 30(5): 83-90.]
[12]	于非,张志欣,刁新源,等. 黄海冷水团演变过程及其与邻近水团关系的分析[J]. 海洋学报,2006,28(5):26-34.[Yu Fei, Zhang Zhixin, Diao Xinyuan, et al. Analysis of evolution of the Huanghai Sea cold water mass and its relationship with adjacent water masses [J]. Acta Oceanologica Sinica, 2006, 28(5): 26-34.]
[13]	姚志刚,鲍献文,李娜,等. 北黄海冷水团季节变化特征分析[J]. 中国海洋大学学报:自然科学版,2012,42(6):9-15.[Yao Zhigang, Bao Xianwen, Li Na, et al. Seasonal evolution of the northern Yellow Sea cold water mass [J]. Periodical of Ocean University of China: Natural Science Edition, 2012, 42(6): 9-15.]
[14]	苏纪兰,黄大吉. 黄海冷水团的环流结构[J]. 海洋与湖沼,1995,26(5):1-7.[Su Jilan, Huang Daji. On the current field associated with the Yellow Sea cold water mass [J]. Oceanologia et Limnologia Sinica, 1995, 26(5): 1-7.]
[15]	向荣,杨作升,郭志刚,等. 济州岛西南泥质区粒度组分变化的古环境应用[J]. 地球科学,2005,30(5):582-588.[Xiang Rong, Yan Zuosheng, Guo Zhigang, et al. Paleoenvironmental implications of grain-size component variations in the mud area southwest off Cheju Island, ECS[J].Earth Science, 2005, 30(5): 582-588.]
[16]	孙东怀,安芷生,苏瑞侠,等. 古环境中沉积物粒度组分分离的数学方法及其应用[J]. 自然科学进展,2001,11(3):269-276.[Sun Donghuai, An Zhisheng, Su Ruixia, et al. Mathematical approach to sedimentary component partitioning of polymodal sediments and its applications[J].Progress in Natural Science, 2001, 11(3): 269-276.]
[17]	Sun Donghuai, Bloemendal J, Rea D K, et al. Grain-size distribution function of polymodal sediments in hydraulic and Aeolian environments, and numerical partitioning of the sedimentary components[J]. Sedimentary Geology, 2002, 152(3/4): 263-277.
[18]	向荣,杨作升,Satio Y,等. 济州岛西南泥质区近2300a来环境敏感粒度组分记录的东亚冬季风变化[J]. 中国科学(D 辑):地球科学,2006,36(7):654-662.[Xiang Rong, Yan Zuosheng, Satio Y, et al. Variation of East Asia winter monsoon according grain-size component records in the mud area southwest off Cheju Island for 2300 year recently[J].Science China (Seri. D): Earth Sciences, 2006, 36(7): 654-662.]
[19]	肖尚斌,李安春. 东海内陆架泥区沉积物的环境敏感粒度组分[J]. 沉积学报,2005,23(1):122-129.[Xiao Shangbin, Li Anchun. A study on environmentally sensitive grain-size population in inner shelf of the East China Sea[J]. Acta Sedimentologica Sinica, 2005, 23(1): 122-129.]
[20]	石学法,申顺喜,Yi H I,等. 南黄海现代沉积环境及动力沉积体系[J]. 科学通报,2001,46(增刊):1-6.[Shi Xuefa, Shen Shunxi, Yi H I,et al. Modern sedimentary environments and dynamic depositional systems in the southern Yellow Sea[J]. Chinese Science Bulletin, 2001, 46(Suppl. ): 1-6.]
[21]	Hu Dunxin. Upwelling and sedimentation dynamics [J]. Chinese Journal of Oceanology and Limnology, 1984, 2(1): 12-19.
[22]	Liu J P, Milliman J D, Gao Shu, et al. Holocene development of the Yellow River's subaqueous delta, north Yellow Sea[J]. Marine Geology, 2004, 209(1/4): 45-67.
[23]	Liu J P, Milliman J D, Gao S. The Shandong mud wedge and post-glacial sediment accumulation in the Yellow Sea [J]. Geo-Marine Letters, 2001, 21(4): 212-218.
[24]	高抒. 中国东部陆架全新世沉积体系:过程—产物关系研究进展评述[J]. 沉积学报,2013,31(5):845-855.[Gao Shu. Holocene sedimentary systems over the Bohai,Yellow and East China Sea region: recent progress in the study of process-product relationships[J]. Acta Sedimentologica Sinica, 2013, 31(5): 845-855.]
[25]	Folk R L, Andrews P B, Lewis D W. Detrital sedimentary rock classification and nomenclature for use in New Zealand[J]. New Zealand Journal of Geology and Geophysics, 1970, 13(4): 937-968.
[26]	McManus J. Grain size determination and interpretation[C]//Tucker M. Techniques in Sedimentology. Oxford: Blackwell, 1988:63-85.
[27]	齐君,李凤业,宋金明. 黄海和渤海沉积物²¹⁰Pb活度的分布特征[J]. 地球化学,2005,34(4):351-356.[Qi Jun, Li Fengye, Song Jinming. Distribution of ²¹⁰Pb activity of sediments in the Yellow and Bohai seas [J]. Geochimica, 2005, 34(4): 351-356.]
[28]	秦蕴珊,赵一阳,陈丽蓉,等. 黄海地质[M]. 北京:海洋出版社,1989:289.[Qin Yunshan, Zhao Yiyang, Chen Lirong, et al. Geology of the East China Sea [M]. Beijing: Science Press, 1989: 289.]
[29]	Prins M A, Postma G, Weltje G J. Controls on terrigenous sediment supply to theArabian Sea during the Late Quaternary: the Makran continental slope [J]. Marine Geology, 2000, 169(3): 351-371.
[30]	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.
[31]	Boulay S, Colin C, Trentesaux A,et al. Mineralogy and sedimentology of Pleistocene sediment in the South China Sea (ODP Site 1144)[C]// Prell W L, Wang P, Blum P, et al. Proceedings of the Ocean Drilling Program, Scientific Results, 2003, 184(211): 1-21.
[32]	董礼先,苏纪兰,王康墡. 黄渤海潮流场及其与沉积物搬运的关系[J]. 海洋学报,1989,11(1):102-114.[Dong Lixian, Su Jilan, Wang Kangshan. Tidal current field and it's effect on sediment transport within Yellow sea and Bohai Sea [J]. Acta Oceanologica Sinica, 1989, 11(1): 102-114.]
[33]	郭志刚,杨作升,雷坤, 等. 东海陆架北部泥质区沉积动力过程的季节性变化[J]. 青岛海洋大学学报:自然科学版,1999,29(3):507-513.[Guo Zhigang, Yang Zuosheng, Lei Kun, et al. Seasonal variation of the sedimentary dynamic processes for the mud area in the northern East China Sea [J]. Journal of Ocean University of Qingdao: Natural Science Edition, 1999, 29(3):507-513.]
[34]	Chu Z X, Sun X G, Zhai S K,et al. Changing pattern of accretion/erosion of the modern Yellow River (Huanghe) subaerial delta, China: Based on remote sensing images [J]. Marine Geology, 2006, 227(1/2): 13-30.
[35]	冯士筰. 风暴潮的研究进展[J]. 世界科技研究与发展,1998,20(4):44-47.[Feng Shizuo. The advance of researches on storm surges [J]. World Sci-Tech R & D, 1998, 20(4): 44-47.]
[36]	王遵娅,丁一汇. 近53年中国寒潮的变化特征及其可能原因[J]. 大气科学,2006, 30(6):1068-1076.[Wang Zuiya, Ding Yihui. Climate change of the cold wave frequency of China in the last 53 years and the possible reasons [J]. Chinese Journal of Atmospheric Sciences, 2006, 30(6): 1068-1076.]
[37]	张秀芝,黄秀芬,李江龙,等. 一百多年来影响黄渤海热带气旋天气气候分析[J]. 海洋预报,1997,14(4):11-21.[Zhang Xiuzhi, Huang Aifeng, Li Jianglong, et al. Weather and climatic analysis of tropical cyclone in the Yellow and Bohai Sea within more than one hundred years [J]. Marine Forecasts, 1997, 14(4): 11-21.]
[38]	孙有斌,高抒,李军. 边缘海陆源物质中环境敏感粒度组分的初步分析[J]. 科学通报,2003,48(1):83-86.[Sun Youbin, Gao Shu, Li Jun. Preliminary analysis of grain-size populations with environmentally sensitive terrigenous components in marginal sea setting [J]. Chinese Science Bulletin, 2003, 48(1): 83-86.]
[39]	肖尚斌,张京穗,陈木宏,等. 从陆架泥质沉积中寻找高分辨率的全新世东亚季风记录[J]. 三峡大学学报:自然科学版,2007,29(4):342-347.[Xiao Shangbin, Zhang Jingsui, Chen Muhong,et al. Exploring high-resolution records of the Holocene East Asian Monsoon from mud sediments on shelves of China marginal seas [J]. Journal of China Three Gorges University: Natural Sciences, 2007, 29(4): 342-347.]
[40]	肖尚斌,李安春,蒋富清,等. 近2ka来东海内陆架的泥质沉积记录及其气候意义[J]. 科学通报,2004,49(21):2233-2238.[Xiao Shangbin, Li Anchun, Jiang Fuqing, et al. The 2 ka record and its climate significance of the mud area of inner shelf of the East China Sea [J]. Chinese Science Bulletin, 2004, 49(21): 2233-2238.]
[41]	肖尚斌,李安春,陈木宏,等. 近8ka东亚冬季风变化的东海内陆架泥质沉积记录[J]. 地球科学,2005,30(5):573-581.[Xiao Shangbin, Li Anchun, Chen Muhong, et al. Recent 8 ka mud records of the East Asian Winter Monsoon from the inner shelf of the East China Sea [J]. Earth Science, 2005, 30(5): 573-581.]
[42]	万世明,李安春,Jan-Berend W S,等. 南海北部ODP1146站粒度揭示的近20Ma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, Jan-Berend W S, et al. East Asia Winter Monsoon change of recent 20Ma from grain size analysis of ODP1146 site from north of South China Sea [J]. Science China(Seri. D): Earth Sciences, 2007, 37(6): 761-770.]
[43]	徐建军,朱乾根. 近百年东亚冬季风的突变性和周期性[J]. 应用气象学报,1999,10(1):1-8.[Xu Jianjun, Zhu Qiangen. Sudden and periodic changes of East Asian Winter Monsoon in the past century [J]. Journal of Applied Meteorological Science, 1999, 10(1): 1-8.]
[44]	郭其蕴,蔡静宁,邵雪梅,等. 1873~ 2000年东亚夏季风变化的研究[J]. 大气科学,2004,28(2):206-215.[Guo Qiyun, Cai Jingning, Shao Xuemei, et al. Studies on the variations of East-Asian Summer Monsoon during A D 1873~2000[J]. Chinese Journal of Atmospheric Sciences, 2004, 28(2): 206-215.]
[45]	陈隆勋,朱乾根,罗会邦,等. 东亚季风[M]. 北京:气象出版社,1991:1-347.[Chen Longxun, Zhu Qiangen, Luo Huibang, et al. The Monsoon of East Asia [M]. Beijing: China Meteorological Press, 1991: 192-244.]
[46]	施能,鲁建军,朱乾根. 东亚冬、夏季风百年强度指数及其气候变化[J]. 南京气象学院学报,1996,19(2):168-177.[Shi Neng, Lu Jianjun, Zhu Qiangen. East Asian Winter/Summer Monsoon intensity indices with their climatic change in 1873–1989[J]. Journal of Nanjing Institute of Meteorology, 1996, 19(2): 168-177.]

Sensitive Grain Size and its Environmental Significance of Modern Mud Patches in Southern and Northern Parts of the Yellow Sea

doi: 10.14027/j.cnki.cjxb.2015.01.013

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