Recent 8 ka Mud Records of the East Asian Winter Monsoon from the Inner Shelf of the East China Sea
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摘要: 尝试从陆架上寻找全新世高分辨率的东亚季风替代性指标和记录.通过对位于东海内陆架闽浙沿岸泥中部的PC-6孔进行AMS14C年龄测试和粒度分析, 综合沉积构造、沉积层序与海平面变化讨论该孔的沉积环境, 其下、中、上段分别对应于前滨、近滨和与现今环境基本一致的浅海沉积环境.因上段的沉积作用主要受控于东海冬季沿岸流, 通过粒级-标准偏差分析, 提取了相对应的粒度组分或粒度子体, 该组分的平均粒径被用来作为研究东亚冬季风演化的替代性指标.分析表明, 由此方法建立的PC-6孔上段粒径时间序列, 较完整地反映了近8ka来东亚古季风的演化.东亚冬季风的变化呈现出3个各具特点的阶段7.6~5.1kaB.P.为中等强度的高频率波动; 5.1~1.7kaB.P.以多期、较频繁的强盛活动为特点; 1.7~0kaB.P.为稳定而较弱的时期.由PC-6孔指示的东亚冬季风活动的强盛期, 均在不同区域和材料的记录中找到了相对应降温的证据, 说明气候变化的区域性以至全球性联系.Abstract: High resolution proxy and record of the Holocene East Asian monsoon is presented based on AMS 14 C dating and grain-size analysis from Core PC-6, located in the middle of the Yangtze River-derived mud off the Zhejiang-Fujian coasts on the inner shelf of the East China Sea (ECS). The sedimentary environments of its upper, middle and lower sections are foreshore, nearshore and shallow sea, similar to the present. The sedimentation of the upper section is controlled by the ECS Winter Coast Current, and corresponding grain-size subpopulation is identified by using grain-size vs. standard deviation. The mean grain-size of the subpopulation is used as a proxy of the East Asian winter monsoon (EAWM), and a recent 8 ka grain-size time series is established to study the evolution of the EAWM. The series showing 3 characteristic sections of the EAWM: moderate and high fluctuation frequency during 7.6-5.1 kaB.P.; much strengthened during 5.1-1.7 kaB.P.; and relatively stable and weakened during 1.7-0 kaB.P.. Periods of the strengthened winter monsoon indicated by PC-6 are all corroborated by other proxies in various areas, which show that regional and even global relationships of climate change exist.
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Key words:
- the East China Sea /
- mud /
- East Asian winter monsoon /
- coastal current /
- grain size /
- Holocene
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图 1 东海海流(a) 与内陆架泥质沉积物分布(b) 概图
a.重绘自秦蕴珊等(1987)、胡敦欣和杨作升(2001)和Su (2001); b.重绘自秦蕴珊等(1987)
Fig. 1. Surface currents (a) and distribution of muddy sediments on the inner shelf (b) of the East China Sea
图 3 PC-6孔粒度序列与其他地区氧同位素序列对比
Fig. 3. Comparison between grain-size time series of PC-6 and various δ18O records
图 4 PC-6孔(a) 和DD2孔(b) 粒度序列的对比
Fig. 4. Comparison between grain-size time series of PC-6 (a) and DD2 (b)
表 1 PC-6孔AMS14C年代数据与样品分辨率
Table 1. AMS14C dating age of Core PC-6 and sample resolution
表 2 PC-6孔2~7.6 kaB.P.的冬季风强盛期与其他代用指标的对比
Table 2. Comparison between periods of the strengthened winter monsoon indicated by PC-6 and other proxies
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An, Z. S., Liu, T. S., Lu, Y., et al., 1990. The long-term pale-omonsoon variation recorded by the loess aleosol sequence in central China. Quaternary International, 7-8: 91-95. doi: 10.1016/1040-6182(90)90042-3 An, Z. S., Kukla, G., Porter, S. C., et al., 1991. Magnetic susceptibility evidence of monsoon variation on the Lo- ess Plateau of central China during the last 130 000 years. Quaternary Research, 36: 29-36. doi: 10.1016/0033-5894(91)90015-W An, Z. S., Porter, S. C., Wu, X. H., et al., 1993. The Holocene optimum in the middle and east China and the variation of East Asian summer monsoon. Chinese Science Bulletin, 38 (14): 1302-1305 (in Chinese). doi: 10.1360/csb1993-38-14-1302 Baroni, C., Orom, B. G., 1996. The Alpine"Iceman" and Holocene climate change. Quaternary Research, 46 (1): 78-83. doi: 10.1006/qres.1996.0046 Bond, G., Showers, W., Cheseby, M., et al., 1997. A pervasive millennial-scale cycle in north Atlantic Holocene and glacial climates. Science, 278: 1257-1266. doi: 10.1126/science.278.5341.1257 Cai, Y. J., Peng, Z. C., An, Z. S., et al., 2001. The oxygen isotope record of the Holocene talagmite in the Qixing cave of Guizhou Province and its significance of mon- soon climatic variation. Chinese Science Bulletin, 46 (16): 1398-1401 (in Chinese). doi: 10.1007/BF03183398 Ding, Y.H., 1996. Study on the test of the South China Sea monsoon and the East China monsoon. The leading edge and prospect of modern atmospheric science, China Meteorological Press, Beijing, 43-46. Ding, Z. L., Liu, T. S., Rutter, N. W., et al., 1995. Ice-volume forcing of East Asian winter monsoon variation in the past 800 000 years. Quaternary Research, 44: 149-158. doi: 10.1006/qres.1995.1059 Dorale, J. A., Gonzalez, L. A., Reagan, M. K., et al., 1992. A high-resolution record of Holocene climate change in speleothem calcite from Cold Water Cave, Northeast Iowa. Science, 258: 1626-1630. doi: 10.1126/science.258.5088.1626 Gasse, F., Arnold, M., Fontes, J. C., et al., 1991. A 13 000- year climate record from western Tibet. Nature, 353: 742-745. doi: 10.1038/353742a0 Guo, Z. G., Yang, Z. S., Lei, K., et al., 1999. Seasonal variation of the sedimentary dynamic processes for the mud area in the northern East China Sea. Journal of Ocean University of Qingdao, 29 (3): 507-513 (in Chinese with English abstract). Hong, Y. T., Jiang, H. B., Liu, T. S., et al., 2000. Response of climate to solar forcing recorded in a 6 000-year δ18O time series of Chinese peat cellulose. The Holocene, 10 (1): 1-7. doi: 10.1191/095968300669856361 Hong, Y. T., Jiang, H. B., Tao, F. X., et al., 1997. The oxy- gen isotope record of turf in Jinchuan during the last 5 ka. Science in China (Series D), 27 (6): 525-530 (in Chinese with English abstract). Hori, K., Saito, Y., Zhao, Q., et al., 2002. Evolution of the coastal depositional systems of the Changjiang(Yangtze) River in response to late Pleistocene-Holocene sea-level changes. Journal of Sedimentary Research, 72 (6): 884-897. doi: 10.1306/052002720884 Hou, Y. J., Zhu, Y. Z., 2000. Important climatic events showed by history records from middle and lower reach plain of the Yellow River during 5 -2.7 ka and their environmental significance. Marine Geologyand Quaternary Geology, 20 (4): 23-29 (in Chinese with English abstract). Hu, D. X., Yang, Z. S., 2001. The key process of ocean flux in the East China Sea. Ocean Press, Beijing, 3-13 (in Chinese). Jian, Z., Wang, P., Saito, Y., et al., 2000. Holocene variability of the Kuroshio current trough, northwestern Pacific ocean. Earth and Planetary Science Letters, 184 (1): 305-319. doi: 10.1016/S0012-821X(00)00321-6 Jin, G. Y., Liu, D. S., 2001. Mid-Holocene cooling climatic events and the variation of ancient civilization in the north of North China. Chinese Science Bulletin, 46 (20): 1725-1730 (in Chinese). doi: 10.1360/csb2001-46-20-1725 Li, C., Chen, Q., Zhang, J., et al., 2000. Stratigraphy and paleoenvironmental changes in the Yangtze Delta during the Late Quaternary. Journal of Asian Earth Sciences, 18 (4): 453-469. doi: 10.1016/S1367-9120(99)00078-4 Liu, J. P., Milliman, J. D., Gao, S., et al., 2004. Holocene development of the Yellow River's subaqueous delta, North Yellow Sea. Marine Geology, 209: 45-67. doi: 10.1016/j.margeo.2004.06.009 Liu, J.P., Xu, K.H., Li, A.C., et al., 2005. Flux and fate of Yangtze River sediment delivered to the East China Sea. Geomorphology(in press). Qin, Y. S., Zhao, Y. Y., Chen, L. R., et al., 1987. Geology in. Science Press, Beijing, 7 (in Chinese). Shen, J., Liu, X. Q., Matsumoto, R., et al., 2004. High-resolution climate change indicated by multi-proxies in sediment of Qinghai Lake since the late glaciation. Science in China (Series D), 34 (6): 582-589 (in Chinese with English abstract). Shi, Y. F., Kong, Z. C., Wang, S. M., et al., 1992. The climate pulse and significant events during the Holocene optimum. Science in China (Series B), 22 (12): 1300-1308 (in Chinese). Sirocko, F., Sarnthein, P., Erlenkeuser, H., 1993. Centuryscale events in monsoonal climate over the past 24 000 years. Nature, 364: 322-324. doi: 10.1038/364322a0 Stuiver, M., Burr, G. S., Hughen, K. A., et al., 1998. INTCAL98 radiocarbon age calibration, 24 000 -0 cal a B.P. . Radiocarbon, 40 (3): 1041-1083. doi: 10.1017/S0033822200019123 Stuiver, M., Grootes, P. M., Braziunas, T. F., 1995. The GISP2 δ18O climate record of the past 16 500 years and the role of the sun, ocean and volcanoes. Quaternary Research, 44: 341-354. doi: 10.1006/qres.1995.1079 Su, J. L., 2001. A review of circulation dynamics of the coastal oceans near China. Acta Oceanonlogica Sinica, 23 (4): 1-16. Sun, B. M., Li, C. Y., 1997. The harass of the East Asian air groove and its relation to the tropic convection activity. Chinese Science Bulletin, 42 (5): 500-504 (in Chinese). doi: 10.1360/csb1997-42-5-500 Sun, X. G., Fang, M., Huang, W., 2000. Spatial and tempo- ral variations in suspended particulate matter transport on the Yellow and East China Sea shelf. Oceanologia et Limnologia Sinica, 31 (6): 581-587 (in Chinese with English abstract). Tan, J. M., Yuan, D. X., Cheng, H., et al., 2004. The rapid change climatic events during the Younger Dryas and the early and middle Holocene: Oxygen isotope record of talagmite in Maolan of Guizhou Province. Science in China (Series D), 34 (1): 39-74 (in Chinese with English abstract). Van, G. B., Buurman, J., Waterbolk, H. T., 1996. Archaeological and palaeoecological indications of an abrupt climate change in the Netherlands, and evidence for climatological teleconnections around 2 650 aB.P. . Journal of Quaternary Science, 11 (6): 451-460. doi: 10.1002/(SICI)1099-1417(199611/12)11:6<451::AID-JQS275>3.0.CO;2-9 Wang, L., Sarnthein, M., 1999. Holocene variations in Asian monsoon moisture: A bidecadal sediment record from the South China Sea. Geophysical Research Letters, 26 (18): 2889-2892. doi: 10.1029/1999GL900443 Weiss, H., Courty, M. A., Wetterstrom, W., et al., 1993. The genies and collapse of third-millennium north Mesopotamian civilization. Science, 261: 955. Winkler, M.G., Wang, P. K., 1993. The Late Quaternary vegetation and climate of China. In: Wright, H.E., Jr. et al., eds., Global climates since the last glacial maximum. University of Minnesota Press, Minnesota, 221-264. Wu, X.H., An, Z.S., Wang, S.M., et al., 1994. The temporal and spatial variation of East Asian summer monsoon in Holocene optimum in China. Quaternary Sciences, (1): 24-37(in Chinese with English abstract). Xiao, S. B., Li, A. C., Jiang, F. Q., et al., 2005. Recent 2 000-year geological records of mud in the inner shelf of the East China Sea and their climatic implications. Chinese Science Bulletin, 50 (1): 1-6. Xiao, S. B., Li, A. C., 2005. Grain-size populations with environmentally sensitive sediment component in the inter shelf of the East China Sea. Acta Sedimentologica Sinica, 23 (1): 122-129 (in Chinese with English abstract). Xu, H., Hong, Y. T., Lin, Q. H., et al., 2002. The temperature change during the last 6 ka indicated by oxygen isotope record in turf fibrin of Hongyuan. Chinese Science Bulletin, 47 (15): 1181-1186 (in Chinese). doi: 10.1360/csb2002-47-15-1181 Xu, J.H., 1998. Sun, climate, famine and the large-scale national migration. Science in China(Series D), 28(4): 367-384(in Chinese with English abstract). 安芷生, Porter, S. C., 吴锡浩, 等, 1993. 中国中、东部全新世气候适宜期与东亚夏季风变迁. 科学通报, 38 (14): 1302-1305. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199314013.htm 蔡演军, 彭子成, 安芷生, 等, 2001. 贵州七星洞全新世石笋的氧同位素记录及其指示的季风气候变化. 科学通报, 46 (16): 1398-1401. doi: 10.3321/j.issn:0023-074X.2001.16.020 郭志刚, 杨作升, 雷坤, 等, 1999. 东海陆架北部泥质区沉积动力过程的季节性变化. 青岛海洋大学学报, 29 (3): 507-513. https://www.cnki.com.cn/Article/CJFDTOTAL-QDHY903.019.htm 洪业汤, 姜洪波, 陶发祥, 等, 1997. 近5ka温度的金川泥炭δ18O记录. 中国科学(D辑), 27 (6): 525-530. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199706008.htm 侯甬坚, 祝一志, 2000. 历史记录提取的近5-2.7ka黄河中下游平原重要气候事件及其环境意义. 海洋地质与第四纪地质, 20 (4): 23-29. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200004005.htm 胡敦欣, 杨作升, 2001. 东海海洋通量关键过程. 北京: 海洋出版社, 3-13. 靳桂云, 刘东生, 2001. 华北北部中全新世降温气候事件与古文化变迁. 科学通报, 46 (20): 1725-1730. doi: 10.3321/j.issn:0023-074X.2001.20.014 秦蕴珊, 赵一阳, 陈丽蓉, 等, 1987. 东海地质. 北京: 科学出版社, 7. 沈吉, 刘兴起, Matsumoto, R., 等, 2004. 晚冰期以来青海湖沉积物多指标高分辨率的古气候演化. 中国科学(D辑), 34 (6): 582-589. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200406010.htm 施雅风, 孔昭宸, 王苏民, 等, 1992. 中国全新世大暖期的气候波动与重要事件. 中国科学(B辑), 22 (12): 1300-1308. https://www.cnki.com.cn/Article/CJFDTOTAL-JBXK199212010.htm 孙柏民, 李崇银, 1997. 冬季东亚大槽的扰动与热带对流活动的关系. 科学通报, 42 (5): 500-504. doi: 10.3321/j.issn:0023-074X.1997.05.015 孙效功, 方明, 黄伟, 2000. 黄东海陆架区悬浮体输运的时空变化规律. 海洋与湖沼, 31 (6): 581-587. doi: 10.3321/j.issn:0029-814X.2000.06.001 覃嘉铭, 袁道先, 程海, 等, 2004. 新仙女木及全新世早中期气候突变事件: 贵州茂兰石笋氧同位素记录. 中国科学(D辑), 34 (1): 39-74. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200401007.htm 吴锡浩, 安芷生, 王苏民, 等, 1994. 中国全新世气候适宜期东亚夏季风时空变迁. 第四纪研究, (1): 24-37. 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. 沉积学报, 23 (1): 122-129. doi: 10.3969/j.issn.1000-0550.2005.01.016 徐海, 洪业汤, 林庆华, 等, 2002. 红原泥炭纤维素氧同位素指示的距今6ka温度变化. 科学通报, 47 (15): 1181-1186. doi: 10.3321/j.issn:0023-074X.2002.15.014 许靖华, 1998. 太阳、气候、饥荒与民族大迁移. 中国科学(D辑), 28 (4): 367-384. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199804012.htm -
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