东海南部内陆架泥质区S05-2孔沉积物4870a BP以来的沉积学记录及其对物源与季风演化指示*

doi:10.11978/2019112

Abstract

Abstract:

For better understanding of the sedimentary process and climate evolution in the East Asian continental shelves, we investigated the core sediments collected from the inner shelf of the East China Sea in terms of aspects of Accelerator Mass Spectrometry (AMS) radiocarbon dating, grain-size, clay minerals, and geochemical element concentrations. The studied sediments were deposited in the last 4870 a BP according to radiocarbon dating. The results show that silt is the dominant component of the sediments from the mud area of the East China Sea. The rivers on Taiwan Island contributed to the deposits in the studied area dominantly, whilst materials from the Yellow River and Yangtze River occurred episodically in the last 4870 a BP. The East Asian winter monsoon could be indicated by element ratio, sensitive grain-size and clay mineral content ratio. It suggests that the East Asian winter monsoon was stable, strengthening, weakening, and re-strengthening from 4870 a BP onward.

Key words: East China Sea inner shelf, mud area, provenance, monsoon, clay minerals, elements, grain size

CLC Number:

P736.31

ZHANG Jie, LI Qi. Sedimentary record from Core S05-2 and its implication of provenance and monsoon evolution in a muddy area of the inner shelf of the Southern East China Sea since 4870 a BP*[J].Journal of Tropical Oceanography, 2020, 39(5): 84-97.

Figures/Tables 15

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References 49

[1]	陈桥, 刘东艳, 陈颖军, 等, 2013. 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, 41(3):319-325.
	CHEN QIAO, LIU DONGYAN, CHEN YINGJUN, et al, 2013. Comparative analysis of Grade- standard deviation method and factors analysis method for environmental sensitive factor analysis[J]. Earth and Environment, 41(3):319-325 (in Chinese with English abstract).
[2]	程海, 艾思本, 王先锋, 等, 2005. 中国南方石笋氧同位素记录的重要意义[J]. 第四季研究, 25(2):157-163.
	CHENG HAI, AI SIBEN, WANG XIANFENG, et al, 2005. Oxygen isotope records of stalagmites from Southern China[J]. Quaternary Sciences, 25(2):157-163 (in Chinese with English abstract).
[3]	郭志刚, 杨作升, 王兆祥, 1995. 黄、东海海域水团发育对底质沉积物分布的影响[J]. 青岛海洋大学学报, 25(1):75-84.
	GUO ZHIGANG, YANG ZUOSHENG, WANG ZHAOXIANG, 1995. Influence of water masses on the distribution of sea-floor sediments in the Huanghai Sea and the East China Sea[J]. Journal of Ocean University of Qingdao, 25(1):75-84 (in Chinese with English abstract).
[4]	何良彪, 1989. 中国海及其邻近海域的粘土矿物[J]. 中国科学 B辑, (1):75-83 (in Chinese).
[5]	何良彪, 刘秦玉, 1997. 黄河与长江沉积物中粘土矿物的化学特征[J]. 科学通报, 42(7):730-733 (in Chinese).
[6]	贾建军, 高抒, 薛允传, 2002. 图解法与矩法沉积物粒度参数的对比[J]. 海洋与湖沼, 33(6):577-582.
	JIA JIANJUN, GAO SHU, XUE YUNCHUAN, 2002. Grain-size parameters derived from graphic and moment methods: A comparative study[J]. Oceanologia et Limnologia Sinica, 33(6):577-582 (in Chinese with English abstract).
[7]	鞠建廷, 朱立平, 冯金良, 等, 2012. 粒度揭示的青藏高原湖泊水动力现代过程: 以藏南普莫雍错为例[J]. 科学通报, 57(19):1775-1784 (in Chinese).
[8]	蓝先洪, 2001. 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, 17(1):5-7 (in Chinese).
[9]	李传顺, 石学法, 高树基, 等, 2012. 台湾河流沉积物的黏土矿物组成特征与物质来源[J]. 科学通报, 57(2-3):169-177.
	LI CHUANSHUN, SHI XUEFA, GAO SHUJI, et al, 2012. Clay mineral composition and their sources for the fluvial sediments of Taiwanese rivers[J]. Chinese Science Bulletin, 57(2-3):169-177 (in Chinese with English abstract).
[10]	李国刚, 1990. 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, 12(4):470-479 (in Chinese).
[11]	李琰, 于洪军, 易亮, 等, 2014. 渤海南部Lz908孔海陆交互沉积的粒度特征及其对沉积环境的指示[J]. 海洋科学, 38(5):107-113.
	LI YAN, YU HONGJUN, YI LIANG, et al, 2014. Grain-size characteristics and its sedimentary significance of coastal sediments of the borehole Lz908 in the south Bohai Sea (the Laizhou Bay), China[J]. Marine Sciences, 38(5):107-113 (in Chinese with English abstract).
[12]	刘东生, 刘嘉麒, 吕厚远, 1998. 玛珥湖高分辨率古环境研究的新进展[J]. 第四纪研究, (4):289-295.
	LIU DONGSHENG, LIU JIAQI, LV HOUYUAN, 1998. Progress in high-resolution paleoenvironment research from Maar Lake[J]. Quaternary Sciences, (4):289-295 (in Chinese with English abstract).
[13]	刘连文, 陈骏, 陈旸, 等, 2001. 最近130ka以来黄土中Zr/Rb值变化及其对冬季风的指示意义[J]. 科学通报, 47(9):702-706 (in Chinese).
[14]	彭娜娜, 2016. 17000a以来冲绳海槽中部柱状样S10沉积学特征及其物源环境指示[D]. 青岛: 中国科学院海洋研究所.
	PENG NANA, 2016, The characteristics and provenances of core S10 sediments in the Central Okinawa Trough: Constrains on the index of paleoenvironment since 17000a[D]. Qingdao: Institute of Oceanology, Chinese Academy of Sciences (in Chinese with English abstract).
[15]	曲华祥, 黄宝琦, 2019. 南海北部MD12-3232站深海氧同位素MIS6期到MIS5期陆源沉积物元素比值反映的古气候变化[J]. 地学前缘, 26(3):236-242.
	QU HUAXIANG, HUANG BAOQI, 2019. Paleoclimate change reflected by element ratios of terrigenous sediments from deep-sea oxygen isotope MIS6 to MIS5 at MD12-3432 station in northern South China Sea[J]. Earth Science Frontiers, 26(3):236-242 (in Chinese with English abstract).
[16]	时英民, 李坤业, 杨惠兰, 等, 1988. 东海DC-2孔岩芯粘土矿物组合及其分布特征[J]. 海洋科学, (2):13-19.
	SHI YINGMIN, LI YEKUN, YANG HUILAN, et al, 1988. Clay mineral assemblage and their distribution characteristic in sediments in core DC-2 from the East China Sea[J]. Marine Sciences, (2):13-19 (in Chinese with English abstract).
[17]	时英民, 李坤业, 杨惠兰, 1989. 南黄海粘土矿物的分布特征[J]. 海洋科学, (3):32-37.
	SHI YINGMIN, LI YEKUN, YANG HUILAN, 1989. Distributary characteristic of clay mineral in the South Huanghai Sea[J]. Marine Sciences, (3):32-37 (in Chinese with English abstract).
[18]	孙东怀, 鹿化煜, DAVID R, 等, 2000. 中国黄土粒度的双峰分布及其古气候意[J]. 沉积学报, 18(3):327-335.
	SUN DONGHUAI, LU HUAYU, DAVID R, et al, 2000. Bimode Grain-size distribution of Chinese loess and its paleoclimate implication[J]. Acta Sedimentologica Sinica, 18(3):327-335 (in Chinese with English abstract).
[19]	孙庆峰, 陈发虎, COLIN C, 等, 2011. 粘土矿物在气候环境变化研究中的应用进展[J]. 矿物学报, 31(1):146-152.
	SUN QINGFENG, CHEN FAHU, COLIN C, et al, 2011. Application progress of clay minerals in the researches of climate and environment[J]. Acta Mineralogica Sinica, 31(1):146-152 (in Chinese with English abstract).
[20]	孙千里, 周杰, 肖举乐, 2001. 岱海沉积物粒度特征及其古环境意义[J]. 海洋地质与第四纪地质, 21(1):93-95.
	SUN QIANLI, ZHOU JIE, XIAO JULE, 2001. Grain-size characteristics of Lake Daihai sediments and its paleaoenvironment significance[J]. Marine Geology & Quaternary Geology, 21(1):93-95 (in Chinese with English abstract).
[21]	孙有斌, 高抒, 李军, 2003. 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, 48(1):83-86.
	SUN YOUBIN, GAO SHU, LI JUN, 2003. Preliminary analysis of grain-size populations with environmentally sensitive terrigenous components in marginal sea setting[J]. Chinese Science Bulletin, 48(2):184-187 (in Chinese with English abstract).
[22]	王亮, 2014. 东海典型泥质区高分辨沉积记录及其对气候环境变化的响应[D]. 青岛: 中国海洋大学.
	WANG LIANG, 2014. High-resolution sedimentary record in the typical mud areas of East China Sea and its response to climate and environmental changes[D]. Qingdao Ocean University of China (in Chinese with English abstract).
[23]	王中波, 杨守业, 张志珣, 等, 2012. 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, 43(6):1041-1049.
	WANG ZHONGBO, YANG SHOUYE, ZHANG ZHIXUN, et al, 2012. The grain size compositions of the surface sediments in the east China Sea: Indication for sedimentary environments[J]. Oceanologia et Limnologia Sinica, 43(6):1041-1049 (in Chinese with English abstract).
[24]	肖尚斌, 李安春, 2005. 东海内陆架泥区沉积物的环境敏感粒度组分[J]. 沉积学报, 23(1):122-129.
	XIAO SHANGBIN, LI ANCHUN, 2005. A study on environmentally sensitive grain-size population in inner shelf of the East China sea[J]. Acta Sedimentologica Sinica, 23(1):122-129 (in Chinese with English abstract).
[25]	熊应乾, 刘振夏, 杜德文, 等, 2006. 东海陆架EA01孔沉积物常微量元素变化及其意义[J]. 沉积学报, 24(3):356-364.
	XIONG YINGQIAN, LIU ZHENXIA, DU DEWEN, et al, 1988. Variation and its implication of major and trace elements of EA01 from the continental shelf of the East China Sea[J]. Acta Sedimentologica Sinica, 24(3):356-364 (in Chinese with English abstract).
[26]	杨作升, 郭志刚, 王兆祥, 等, 1992. 黄东海陆架悬浮体向其东部深海区输送的宏观格局[J]. 海洋学报, 14(2):81-90 (in Chinese).
[27]	姚檀栋, THOMPSON L G, 施雅风, 等, 1997. 古里雅冰芯中末次间冰期以来气候变化记录研究[J]. 中国科学(D辑), 27(5):447-452.
	YAO TANDONG, THOMPSON L G, SHI YAFENG, et al, 1997. Climate variation since the Last Interglaciation recorded in the Guliya ice core[J]. Science in China Series D: Earth Sciences, 40(6):662-668 (in Chinese with English abstract).
[28]	曾剑, 张强, 王同美, 2010. 东亚冬季风与中国南方冬季降水的关系分析[J]. 高原气象, 29(4):975-981.
	ZENG JIAN, ZHANG QIANG, WANG TONGMEI, 2010. Analysis on Relationship of East-Asian winter monsoon intensity and winter precipitation in Southern China[J]. Plateau Meteorology, 29(4):975-981 (in Chinese with English abstract).
[29]	中华人民共和国国家质量监督检验检疫总局, 中国国家标准化管理委员会, 2008. GB/T 12763.8-2007 海洋调查规范第8部分海洋地质地球物理调查[S]. 北京: 中国标准出版社: 11-12(in Chinese).
[30]	周晓静, 2009. 东海陆架细颗粒沉积物组成分布特征及其物源指示[D]. 青岛: 中国科学院研究生院(海洋研究所).
	ZHOU XIAOJING, 2009. The source and composition of fine-grained sediment deposited on the East China Sea shelf[D]. Qingdao: The Institute of Oceanology, Chinese Academy of Sciences (in Chinese with English abstract).
[31]	周晓静, 李安春, 万世明, 等, 2010. 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, 41(5):667-675. doi: 10.11693/hyhz201005002002
	ZHOU XIAOJING, LI ANCHUN, WAN SHIMING, et al, 2010. Clay minerals in surfacial sediments of the East China Sea shelf: distribution and provenance[J]. Oceanologia et Limnologia Sinica, 41(5):667-675 (in Chinese with English abstract). doi: 10.11693/hyhz201005002002
[32]	ALLEY R B, 2000. The Younger Dryas cold interval as viewed from central Greenland[J]. Quaternary Science Reviews, 19(1-5):213-226.
[33]	DYKOSKI C A, EDWARDS R L, CHENG HAI, et al, 2005. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China[J]. Earth and Planetary Science Letters, 233(1-2):71-86.
[34]	DYPYJK H, HARRIS N B, 2001. Geochemical facies analysis of fine-grained siliciclastics using Th/U, Zr/Rb and (Zr+Rb)/Sr ratios[J]. Chemical Geology 181 (1-4):131-146.
[35]	FRIEDMAN G M, 1979. Address of the retiring president of the international association of sedimentologists: differences in size distributions of populations of particles among sands of various origins[J]. Sedimentology, 26(1):3-32.
[36]	INGRAM B L, SLOAN D, 1992. Strontium isotopic composition of estuarine sediments as paleosalinity paleoclimate indicator[J]. Science, 255(5040):68-72. doi: 10.1126/science.255.5040.68 pmid: 17739916
[37]	LIU ZHIFEI, TRENTESAUX A, CLEMENS S C, et al, 2003. Clay mineral assemblages in the northern South China Sea: implications for East Asian monsoon evolution over the past 2 million years[J]. Marine Geology, 201(1-3):133-146.
[38]	MCLAREN P, BOWLES D, 1985. The effects of sediment transport on grain-size distributions[J]. Journal of Sedimentary Research, 55(4):457-470.
[39]	MCMANUS J, 1988. Grain size determination and interpretation[M]// TUCKER M. Techniques in Sedimentology. Oxford, UK: Blackwell Scientific Publications: 63-85.
[40]	MILLIMAN J D, BEARDSLEY R C, YANG ZUOSHENG, et al, 1985. Modern Huanghe-derived muds on the outer shelf of the East China Sea: identification and potential transport mechanisms[J]. Continental Shelf Research, 4(1-2):175-188.
[41]	TU LUYAO, ZHOU XIN, CHENG WENHAN, et al, 2016. Holocene East Asian winter monsoon changes reconstructed by sensitive grain size of sediments from Chinese coastal seas: A review[J]. Quaternary International, 440:82-90.
[42]	VISHER G S, 1969. Grain size distributions and depositional processes[J]. Journal of Sedimentary Research, 39(3):1074-1106.
[43]	WAN SHIMING, TIAN JUN, STEINKE S, et al, 2010. Evolution and variability of the East Asian summer monsoon during the Pliocene: Evidence from clay mineral records of the South China Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 293(1-2):237-247.
[44]	WANG L, SARNTHEIN M, ERLENKEUSER H, et al, 1999. East Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the South China Sea[J]. Marine Geology, 156(1-4):245-284.
[45]	WEI GANGJIAN, LIU YING, LI XIANHUA, et al, 2004. 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, 212(3-4):331-342. doi: 10.1016/S0031-0182(04)00329-3
[46]	XIAO SHANGBIN, LI ANCHUN, LIU J P, et al, 2006. Coherence between solar activity and the East Asian winter monsoon variability in the past 8000 years from Yangtze River-derived mud in the East China Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 237(2-4):293-304. doi: 10.1016/j.palaeo.2005.12.003
[47]	YANCHEVA G, NOWACZYK N R, MINGRAM J, et al, 2007. Influence of the intertropical convergence zone on the East Asian monsoon[J]. Nature, 445(7123):74-77. doi: 10.1038/nature05431 pmid: 17203059
[48]	YANG SHOUYE, JUNG H S, CHOI M S, et al, 2002. The rare earth element compositions of the Changjiang (Yangtze) and Huanghe (Yellow) river sediments[J]. Earth and Planetary Science Letters, 201(2):407-419. doi: 10.1016/S0012-821X(02)00715-X
[49]	YURETICH R, MELLES M, SARATA B, et al, 1999. Clay minerals in the sediments of Lake Baikal; a useful climate proxy[J]. Journal of Sedimentary Research, 69(3):588-596.

样品编号	实验室样品编号	深度/cm	样品类型	δ¹³C/‰	AMS¹⁴C年龄/(a BP)	校正后日历年龄/(cal a BP)	概率
S05-2-166	503269	166	有孔虫	-0.3	3260 ± 30	3660 ± 30	0.95
S05-2-340	509424	340	有孔虫	-0.6	4470 ± 30	4870 ± 30	0.95

分层	年龄范围	项目	平均粒径/μm	分选系数	偏态	峰态
层段 Ⅳ (0~92cm)	3660a BP 以来后期阶段	平均值	6.76	1.88	0.08	2.36
		最大值	7.02	2.11	0.26	3.26
		最小值	6.36	1.76	-0.46	2.14
层段 Ⅲ (92~166cm)	3660a BP 以来早期阶段	平均值	6.86	1.80	0.16	2.48
		最大值	7.08	2.07	0.35	2.83
		最小值	6.42	1.70	-0.20	2.30
层段 Ⅱ (166~254cm)	4870a BP—3660a BP 后期阶段	平均值	6.76	1.80	0.26	2.49
		最大值	7.08	2.04	0.56	2.83
		最小值	6.33	1.61	-0.10	2.27
层段 Ⅰ (254~340cm)	4870a BP—3660a BP 早期阶段	平均值	6.88	1.71	0.23.	2.63
		最大值	7.12	2.03	0.38.	3.50
		最小值	6.43	1.60	-0.35	2.44

	蒙脱石	伊利石	高岭石	绿泥石
最大值	38.750	81.549	9.221	31.137
最小值	0.003	47.716	1.188	9.021
平均值	4.610	75.066	4.043	16.282

元素名称	最大值	最小值	平均值
Ti	3524.61	1991.32	2954.97
V	374.87	0	175.02
Mn	516.21	287.63	396.67
Fe	41146.78	25900.92	34157.56
Ni	55.42	15.34	29.06
Rb	113.33	78.62	95.44
Zr	157.82	103.32	123.87
Sr	220.74	88.05	109.61

样品	蒙脱石	伊利石	高岭石	绿泥石
S05-2 层段Ⅰ	4.80	76.43	3.00	15.76
S05-2 层段Ⅱ	11.47	70.46	3.22	14.85
S05-2 层段Ⅲ	0.03	78.30	4.56	17.11
S05-2 层段Ⅳ	0.75	76.61	5.17	17.46
长江	6.85	67.95	12.62	14.14
黄河	17.52	61.58	8.73	12.17
古黄河	21.49	60.28	8.49	10.01
黄海泥质区	23.67	52.89	10.33	12.89
台湾岛东部河流	0	70.82	2.45	26.64
台湾岛西部河流	0	69.40	3.40	27.40

Sedimentary record from Core S05-2 and its implication of provenance and monsoon evolution in a muddy area of the inner shelf of the Southern East China Sea since 4870 a BP*

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[13]	Lianghong LÜ, Xiaotong ZHENG. The effect of Indian Ocean Basin mode on Indian Summer Monsoon Rainfall in decaying year of El Niño [J]. Journal of Tropical Oceanography, 2017, 36(2): 1-11.
[14]	Tao LIU, Ying LIU, Yuanfu YUE. Response of mangrove swamp sedimentation rate to climate change [J]. Journal of Tropical Oceanography, 2017, 36(2): 40-47.
[15]	YAN Yi, ALMATARI Ali Ahmed Ali, TIAN Zhixian, QIAN Kun. Basin-mountain evolution, thermo-tectonic history and surface crustal recycling processes of the northern margin of the South China Sea [J]. Journal of Tropical Oceanography, 2016, 35(6): 46-57.