SENSITIVE GRAIN SIZE OF THE MUD DEPOSITS OFFSHORE QINGDAO AND ITS IMPLICATIONS FOR SEDIMENTARY ENVIRONMENTS
-
摘要: 通过对青岛南部近岸泥质区3个岩心(Z14、Z16、QDZ03)进行粒度分析和AMS14C年龄测试,研究了沉积物粒度组成并提取了敏感粒级,探讨了敏感粒级的搬运机制及其环境指示意义。研究表明:研究区岩心沉积物以粉砂和黏土质粉砂为主,包含3个敏感粒级(敏感粒级1、敏感粒级2、敏感粒级3),分别对应粒度细端组分、中端组分和粗端组分,以悬浮和跳跃搬运为主,少量以滚动、推移方式搬运;沉积物主要受沿岸流输运的影响,粒度组分自东北向西南逐渐变细,反映了水动力条件自东北向西南逐渐减弱的趋势;其中,敏感粒级2对东亚冬季风增强事件具有较好的反映:利用QDZ03孔上部3.94 m岩心沉积物敏感粒级获得了近3 ka以来5个明显的东亚冬季风增强事件(230~370、1 050~1 180、1 400~1 550、1 850~1 950和2 250~2 350 aBP),对古气候记录具有较好的指示作用。Abstract: Three cores (Z14, Z16 and QDZ03) retrieved from the Qingdao offshore mud area were analyzed for grain size distribution and AMS 14C dating in order to study the grain size distribution pattern and their sensitive components for revealing of the transporting mechanism and their environmental implications. The sediments in the three cores are mostly composed of silt and clayey silt. Observed are three sensitive grain sizes, i.e. the sensitive grain size 1, the sensitive grain size 2 and the sensitive grain size 3, respectively corresponding to the components of the fine end, medium-grained and coarse end in the particle size distribution. The sediment mainly consists of suspended load and saltation load, with a little bed load. It is mainly transported by the nearshore currents and the particle sizes are gradually getting smaller from northeast to southwest. It means that the hydrodynamics is gradually weakened from northeast to southwest. Among the three, the sensitive grain size 2 represents the record of the enhanced winter monsoon event. The sensitive grain size (15.63-210μm) in the upper part (0-3.94m) of the Core QDZ03 reveals that there are five enhanced events of East Asian Winter Monsoon (230-370a BP, 1050-1180a BP, 1400-1550a BP, 1850-1950a BP and 2250-2350a BP) over the past 3ka. The case proves that the sensitive grain size could be used as a good indicator of paleoclimate records.
-
-
[1] 涂路遥, 周鑫, 刘毅,等. 近海泥质沉积物敏感粒径作为冬季风强度指标的再研究:与器测数据的对比[J]. 第四纪研究, 2015, 35(6):1393-1401. [TU Luyao,ZHOU Xin, LIU Yi, et al. Re-analysis of sensitive grain size of coastal muddy sediments as proxy of winter monsoon strength:comparison with instrumental Data[J]. Quaternary Sciences, 2015, 35(6):1393-1401.]
[2] 沈星, 褚忠信, 王玥铭,等. 北黄海西部与南黄海中部泥质区岩心敏感粒级及其环境意义[J]. 沉积学报, 2015, 33(01):124-133. [SHEN Xing, CHU Zhongxin, WANG Yueming, et al. 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(01):124-133.]
[3] Hu B Q, Yang Z S, Zhao M X, et al. Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area, China[J]. Science China Earth Science, 2012, 55(10):1656-1668.
[4] Xiao S, Li A, Liu J P, et al. 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, 2006, 237(2-4):293-304.
[5] 徐方建, 李安春, 万世明,等. 东海内陆架泥质区中全新世环境敏感粒度组分的地质意义[J]. 海洋学报, 2009, 31(03):95-102. [XU Fangjian, LI Anchun, WAN Shiming, et al. The geological significance of environmental sensitive grain-size populations in the mud wedge of the East China Sea during the mid-Holocene[J]. Acta Oceanologica Sinica, 2009, 31(03):95-102.]
[6] Zhou X, Yang W, Xiang R, et al. Re-examining the potential of using sensitive grain size of coastal muddy sediments as proxy of winter monsoon strength[J]. Quaternary International, 2014, 333(4):173-178.
[7] 向荣, 杨作升, Saito 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:, 2006, 36(7):654-662. [XIANG Rong, YANG Zuosheng, Saito Y, et al. East Asia Winter Monsoon change o frecent 2300 a recorded by environmental sensitive grain-size population change in the mud area southwest off Cheju Island, ECS[J]. Science in China (Series D), 2006, 36(7):654-662.]
[8] 孙晓燕, 李广雪, 刘勇,等. 东海北部泥质区敏感粒度组分对东亚季风演变的响应[J]. 海洋地质与第四纪地质, 2008, 13(04):11-17. [SUN Xiaoyan, LI Guangxue, LIU Yong, et al. Response of environmental sensitive grain size group in core FJ04 from mud area in the north of East China Sea to East Asian winter monsoon evolvement[J].Marine Geology and Quaternary Geology, 2008, 13(04):11-17.]
[9] 杨作升, 郭志刚, 王兆祥,等. 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, 1992(02):81-90.[YANG Zuosheng, GUO Zhigang, WANG Zhaoxiang, et al. Basic pattern of transport of suspended matter from the Yellow Sea and East China Sea to the eastern deep seas[J]. Acta Oceanological Siniea, 1992 , 14(2):81-90.]
[10] 郭志刚, 杨作升. 东海陆架北部泥质区沉积动力过程的季节性变化[J]. 中国海洋大学学报(自然科学版), 1999(03):507-513.[GUO Zhigang, YANG Zuosheng. Seasonal variation of the sedimentary dynamic processes for the mud area in the northern East China Sea[J]. Journal of Ocean University of Qingdao, 1999(7),29(3):507-513.] [11] 孙效功, 方明, 黄伟. 黄、东海陆架区悬浮体输运的时空变化规律[J]. 海洋与湖沼, 2000, 31(06):581-587. [SUN Xiaogong, FANG Ming, HUANG Wei, et al. Spatial and temporal variations in suspended particulate mater transport on the Yellow and East China Sea shelf[J]. Oceanology and Limnology, 2000, 31(6):581-587.]
[12] 王可, 郑洪波, Maarten Prins,等. 东海内陆架泥质沉积反映的古环境演化[J]. 海洋地质与第四纪地质, 2008, 28(04):1-10. [WANG Ke, ZHENG Hongbo, Maarten Prins, et al. High-resolution paleoenvironmental record of the mud sediments of the East China Sea inner shelf[J]. Marine Geology and Quaternary Geology, 2008, 28(04):1-10.]
[13] 杨作升, 陈晓辉. 百年来长江口泥质区高分辨率沉积粒度变化及影响因素探讨[J]. 第四纪研究, 2007, 27(05):690-699. [YANG Zuosheng, CHEN Xiaohui. Centurial high resolution records of sediment grain-size variation in the mud area off The Changjiang (Yangtze river) estuary and its influencial factors[J]. Quaternary Research, 2007, 27(05):690-699.]
[14] Wu X, Bi N, Kanai Y, et al. Sedimentary records off the modern Huanghe (Yellow River) delta and their response to deltaic river channel shifts over the last 200 years[J]. Journal of Asian Earth Sciences, 2015, 108:68-80.
[15] Qiu J, Liu J, Saito Y, et al. Sedimentary evolution of the Holocene subaqueous clinoform off the southern Shandong Peninsula in the Western South Yellow Sea[J]. Journal of Ocean University of China, 2014, 13(5):747-760.
[16] Zhang X, Shipu Bi, Zhang Y, et al. Provenance analysis of surface sediments in the Holocene mud area of the southern coastal waters off Shandong Peninsula,China[J]. Acta Oceanologica Sinica -English Edition-, 2016, 35(5):124-133.
[17] 张晓波, 张勇, 孔祥淮,等.山东半岛南部近岸海域表层沉积物稀土元素的物源指示[J]. 海洋地质与第四纪地质, 2014(03):57-66.[ZHANG Xiaobo, ZHANG Yong, KONG Xianghuai, et al. Rare earth elements analysis for provenance study of surface sediments off south Shandong peninsula[J]. Marine Geology and Quaternary Geology, 2014 , (3):57-66.]
[18] 刘金庆, 张勇, 印萍,等.青岛近岸海域表层沉积物重矿物分布及物源[J]. 海洋地质与第四纪地质, 2016(01):69-78.[LIU Jinqing, ZHANG Yong, YIN Ping, et al. Disribution And Provenance Of Heavy Minerals Insurface Sediments Of The Qingdao Off Shore Area[J]. Marine Geology and Quaternary Geology, 2016 (01):69-78.]
[19] Folk R L, Ward W C. Brazos River bar:a study in the significance of grain size parameters[J]. Journal of Sedimentary Research, 1957, 27(1):215-220.
[20] Visher G S.Grain size distributions and depositional processes[J]. Journal of Sedimentary Petrology,1969,39:1074-1106.
[21] Glaister R P,Nelson H W.Grain-size distributions, an aid in facies identification[J]. Bulletin of Canada Petroleum Geology,1974,22(3):203-240.
[22] 郑俊茂, 王德发, 孙永传. 黄骅坳陷几种砂体的粒度分布特征及其水动力条件的初步分析[J]. 石油实验地质,1980,2:9-20.[ZHENG Junmao,WANG Defa,SUN Yongchuan. The grain size distribution characteristic of some sandbody in Huanghua Depression and its hydrodynamic conditions analysis[J]. Experimental Petroleum Geology, 1980 ,2:9-20.]
[23] 袁静, 杨学君, 路键勇,等. 东营凹陷盐22块沙四上亚段砂砾岩粒度概率累积曲线特征[J]. 沉积学报, 2011, 29(5):815-824. [YUAN Jing, YANG Xuejun, LU Zhiyong, et al. Probability Cumulative Grain Size Curves in Sandy Conglomerate of the Upper Es4in Yan 22 Block,Dongying Depression[J]. Acta Sedimentologica Sinica, 2011, 29(5):815-824.]
[24] Gao S, Collins M. Modelling exchange of natural trace sediments between an estuary and adjacent continental shelf[J]. Journal of Sedimentary Research, 1992(1):35-40.
[25] Gao S, Collins M, Mclaren P, et al. A critique of the "McLaren Method" for defining sediment transport paths; discussion and reply[J]. Journal of Sedimentary Research, 1991, 61(1):143-147.
[26] 高抒. 沉积物粒径趋势分析:原理与应用条件[J]. 沉积学报, 2009, 27(05):826-836. [GAO Shu. Grain size trend analysis:principle and applicabilit[J]. Acta Sedimentologica Sinica, 2009, 27(05):826-836.]
[27] 李淑玲. 鳌山湾水动力环境及泥沙运动特征研究[D]. 中国海洋大学,2012.[LI Shuling. Study on the hydrodynamic environment and sediment movement characteristics in Aoshan Bay[D]. Ocean University of China, 2012.] [28] 王文海,夏东兴,高兴辰,等.中国海湾志第4分册-山东半岛南部和江苏省海湾[M].北京:海洋出版社,1993:1-448.[WANG Wenhai, XIA Dongxing, GAO Xingchen, et al. The Fourth volume of the China Gulf Chronicle the gulf of southern Shandong Peninsula and Jiangsu Province[M]. Beijing:China Ocean Press,1993:1 -448.]
[29] 徐丹亚, 赵保仁. 青岛-石岛近海反气旋中尺度涡旋存在证据及数值模拟[J]. 海洋学报, 1999, 21(02):18-26. [XU Danya, ZHAO Baoren. Existential proof and numerical study of a mesoscale anticyclonic eddy in the Qingdao-Shidao offshore[J]. Acta Oceanologica Sinica,1999,21(2):18-26.]
[30] 施雅风, 孔昭宸. 中国全新世大暖期的气候波动与重要事件[J]. 中国科学(B辑), 1992, 22(12):1300-1308.[SHI yafeng, KONG zhaocheng. Climates and Environments of the Holocene Mega thermal Maximum in China[J]. Science in China (Ser. B), 1992, 22(12):1300-1308.] [31] 王绍武. 小冰期气候的研究[J]. 第四纪研究, 1995, 15(03):202-212. [WANG Shaowu. Research on the Little Ice Age climate[J]. Quaternary Research, 1995, (3):202-212.]
[32] 洪业汤, 李汉鼎. 近5ka温度的金川泥炭δ18O记录[J]. 中国科学(D辑), 1997(6 ):525-530.[HONG Yetang, JIANG Hongbo. Temperature record of Jinchuan peat δ18O over the last 5000a[J]. Science in China(Series D), 1997, 27(6):525-530.]
[33] 徐海, 洪业汤, 林庆华,等. 红原泥炭纤维素氧同位素指示的距今6 ka温度变化[J]. 科学通报, 2002, 47(15):1181-1186. [XU Hai, HONG Yetang, LIN Qinghua, et al. Temperature change over the past 6000 a from cellulose oxygen isotope of Hongyuan peat[J]. Chinese Science Bulletin, 2002, 47(15):1181-1186.]
[34] 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(中国地质大学学报), 2005, 30(05):582-588.[XIANG Rong, YANG Zuosheng, GUO Zhigang, et al. Paleoenvironmental implications of grain-size component variations in the mud area Southwest off Cheju Island,ECS[J]. Earth Science Journal of China University of Geoscienees, 2005, 30(5):582-588.] [35] 刘晓宏, 秦大河, 邵雪梅,等. 祁连山中部过去近千年温度变化的树轮记录[J]. 中国科学(D辑), 2004, 34(1):89-95.[LIU Xiaohong, QIN Dahe, SHAO Xuemei, et al. Temperature variations recovered from tree-rings in the middle Qilian Mountain over the last millennium[J]. Science in China(Ser.D), 2004, 34(1):89-95.] [36] 曹建廷, 金章东, 沈吉,等. 近800年来内蒙古岱海地区古气温的定量重建[J]. 地理科学, 2003, 23(03):298-303. [CAO Jianting, JIN Zhangdong, SHEN Ji, et al. An 800-year temperature reconstruction in Daihai Lake area of Inner Mongolia[J]. Scientia Geographica Sinica, 2003, 23(03):298-303.]
[37] Jacoby G C, D'Arrigo R. Reconstructed Northern Hemisphere annual temperature since 1671 based on high-latitude tree-ring data from North America[J]. Climatic Change, 1989, 14(1):39-59.
[38] Stuiver M, Grootes P M, Braziunas T F. The GISP2 δ18O Climate Record of the Past 16,500 Years and the Role of the Sun, Ocean, and Volcanoes[J]. Quaternary Research, 1995, 44(3):341-354.
[39] Wang S W. Reconstruction of temperature series of north China from 1380s to 1980s[J]. Science in China, 1991, 34(6):751-759.
[40] 吴宏岐, 党安荣. 隋唐时期气候冷暖特征与气候波动[J]. 第四纪研究, 1998(01):31-38.[WU Hongqi, DANG Anrong. Fluctuation of climatic change in temperature of Tang Dynasty[J]. Quaternary Research,1998 (1):31-38.]
[41] 葛全胜, 满志敏. 过去2000a中国东部冬半年温度变化序列重建及初步分析[J]. 地学前缘, 2002, 9(01):169-181. [GE Quansheng, MAN Zhimin, et al. Recons truction and analysis on the series of winter half year temperature changes over the past 2000 years in eastern China[J]. Earth Science Frontiers, 2002, 9(1):169-181.]
[42] 徐方建. 东海内陆架泥质区EC2005孔沉积特征及古环境记录[D]. 中国科学院研究生院(海洋研究所), 2009.[XU Fangjian. Sedimentary characteristics and paleoenvironmental records of Core EC2005 in the mud area on the inner shelf of the East China Sea[D].Institute of Oceanology,Chinese Academy of Sciences, 2009.] [43] 郑景云, 满志敏, 方修琦,等. 魏晋南北朝时期的中国东部温度变化[J]. 第四纪研究, 2005, 25(02):129-140. [ZHENG Jingyun, MAN Zhimin, FANG Xiuqi, et al. Temperature variation in the Eastern China during Wei, Jin and south-north Dynasties(220~580a. D.)[J]. Quaternary Sciences, 2005, 25(02):129-140.]
[44] 刘升发, 石学法, 刘焱光,等. 近2ka以来东海内陆架泥质区记录的高分辨率古气候演化[J]. 海洋学报, 2011, 33(03):85-93. [LIU Shengfa, SHI Xuefa, LIU Yanguang, et al. Recent 2000 a climatic record of mud area on the inner shelf of the East China Sea[J]. Acta Oceanologica Sinica, 2011, 33(03):85-93.]
[45] 许靖华. 太阳、气候、饥荒与民族大迁移[J]. 中国科学(D辑), 1998(4):366-384.[XU Jinghua. Sun, weather, famine and national migration[J]. Science in China(Series D), 1998(4):366-384.] [46] 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(中国地质大学学报), 2005, 30(05 ):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 Journal of China University of Geosciences, 2005, 30(5):573-581.]
-
期刊类型引用(1)
1. 孔凡彪,徐树建,贾广菊. 沉积物中硬质粘土层的研究进展. 山东国土资源. 2018(03): 1-7+14 . 百度学术
其他类型引用(1)
计量
- 文章访问数: 2030
- HTML全文浏览量: 275
- PDF下载量: 12
- 被引次数: 2