Postglacial sequence stratigraphy and sedimentary environment evolution of the Yangtze River subaqueous delta

doi:10.7605/gdlxb.2017.03.042

JOPC ›› 2017, Vol. 19 ›› Issue (3): 541-556. doi: 10.7605/gdlxb.2017.03.042

• SEQUENCE STRATIGRAPHY AND PALAEOGEOGRAPHY • Previous Articles Next Articles

Postglacial sequence stratigraphy and sedimentary environment evolution of the Yangtze River subaqueous delta

Su Jianfeng^{1, 2}, Fan Daidu^{1, 3}, Leng Wei¹, Chen Lingling¹, Yin Ping⁴

1 State Key Laboratory of Marine Geology,Tongji University,Shanghai 200092;
2 State Key Laboratory of Estuarine and Coastal Research,East China Normal University,Shanghai 200062;
3 School of Geoscience,Yangtze University,Wuhan 430100,Hubei;
4 Qingdao Institute of Marine Geology,Qingdao 266071,Shandong

Received:2016-06-24 Revised:2016-09-27 Online:2017-06-01 Published:2017-06-01
Contact: Fan Daidu,born in 1972,is a professor of sedimentology at Tongji University. E-mail: ddfan@tongji.edu.cn.
About author:Su Jianfeng,born in 1989,is a master candidate of marine geology at Tongji University. E-mail: 385715061@qq.com.About the corresponding author Fan Daidu,born in 1972,is a professor of sedimentology at Tongji University. E-mail: ddfan@tongji.edu.cn.
Supported by:
[Co-funded by the National Natural Science Foundation of China(No.41476031),Ph.D.Programs Foundation of Ministry of Education of China(No.20130072130003),Research Fund for Marine Geological Protection(No.GZH201100203),International Cooperation Project of the State Oceanic Administration(No.GASI-GEOGE-02)and State Key Laboratory of Estuarine and Coastal Research Opening Project,East China Normal University(No.SKLEC-KF201506)]

冰后期以来长江水下三角洲层序地层特征及沉积环境演化^*

苏建锋^{1, 2}, 范代读^{1, 3}, 冷伟¹, 陈玲玲¹, 印萍⁴

1 同济大学海洋地质国家重点实验室,上海 200092;
2 华东师范大学河口海岸国家重点实验室,上海 200062;
3 长江大学地球科学学院,湖北武汉 430100;
4 青岛海洋地质研究所,山东青岛 266071

通讯作者: 范代读,男,1972年生,教授,博士生导师,从事海洋沉积学研究。E-mail: ddfan@tongji.edu.cn。
作者简介:苏建锋,男,1989年生,硕士研究生,海洋地质学专业。E-mail: 385715061@qq.com。
基金资助:
*国家自然科学基金项目(编号:41476031)、教育部博士点基金项目(编号:20130072130003)、海洋地质保障专项项目(编号:GZH201100203)、国家海洋局国际合作项目(编号:GASI-GEOGE-02)和华东师范大学河口海岸国家重点实验室开放课题(编号:SKLEC-KF201506)联合资助

Abstract

Abstract: Sequence stratigraphic research of the Yangtze River subaqueous delta is conducive to a comprehensive understanding of the Yangtze River delta stratigraphic characteristics and sedimentary environment evolution model. Detailed analyses of grain-size compositions,sedimentary facies and elemental ratios(Cl/Ti、Zr/Rb)of cores from Boreholes YD0901 and YD0903 located at the Yangtze paleo-incised valley establish the postglacial period high-resolution stratigraphic framework of the Yangtze River subaqueous delta.The postglacial facies associations in the Yangtze River delta(YRD)are vertically stacked from fluvial facies at the bottom,through tidal-river facies,estuarine facies,and shallow-marine facies,to deltaic facies at the top. Since the Last Glacial period sea-level began to decline,and the incised valley of ancient Yangtze River developed. Stiff clay on the interfluve of the incised valley constitutes the Ⅰ-type sequence boundary. After then the sea-level began to rise,the regression and transgression reached its maximum in 15 cal ka BP and 8.0 cal ka BP respectively,and the time of maximum transgression at subaqueous delta slightly lagged behind the plain area which is about 7.5 cal ka BP. According to these three sequence boundaries,the strata were divided into lowstand system tracts(LST),transgressive system tracts(TST)and highstand system tracts(HST). Based on AMS¹⁴C dating results,post-LGM (Last Glacial Maximum)transgression reached the coring area roughly in 14.8 cal ka BP. The rate of shoreline retreatment was up to 71.9,km/ka,resulting from rapid sea-level rise by the MWP(Meltwater Pulse)-1A event in 14.8~13cal ka BP. In the early regression period,the deposition rate of the boreholes was low. It increased significantly since 2 cal ka BP.

Key words: Yangtze River subaqueous delta, Last Glacial Maximum, AMS14C dating, sedimentary facies, sequence stratigraphy

摘要： 长江水下三角洲层序地层学研究有助于全面了解长江三角洲地层特征和沉积环境演化模式。通过对长江水下三角洲下切河谷区YD0901和YD0903孔岩心的详细沉积物粒度、特征元素比值(Cl/Ti和Zr/Rb)、沉积相对比分析,恢复了冰后期以来长江水下三角洲层序地层格架。研究区冰后期以来自下而上依次出现河流相、潮汐河流相、河口湾相、浅海相和三角洲相的沉积相序。末次冰期海平面下降,古长江形成下切河谷,古河间地发育硬黏土层,构成五级Ⅰ型层序界面。之后海平面回升,分别于15 cal ka BP和8.0 cal ka BP形成最大海退和最大海侵界面,水下三角洲区域最大海侵发生时间略滞后于平原区,约为7.5 cal ka BP。据此3个层序界面将冰后期地层划分为低位体系域、海侵体系域和高位体系域。钻孔岩心记录揭示了14.8 cal ka BP海侵到达研究区;14.8~13 cal ka BP期间,受MWP-1A冰融水事件影响海平面快速上升,海岸线向陆推进速率可达71.9,km/ka;海退期间各钻孔沉积速率较低,直至2 cal ka BP开始,沉积速率明显增加。

关键词: 长江水下三角洲, 末次冰盛期, AMS14C测年, 沉积相, 层序地层

CLC Number:

P736.21

Su Jianfeng, Fan Daidu, Leng Wei, Chen Lingling, Yin Ping. Postglacial sequence stratigraphy and sedimentary environment evolution of the Yangtze River subaqueous delta[J]. JOPC, 2017, 19(3): 541-556.

苏建锋, 范代读, 冷伟, 陈玲玲, 印萍. 冰后期以来长江水下三角洲层序地层特征及沉积环境演化^*[J]. 古地理学报, 2017, 19(3): 541-556.

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References

[1] 陈报章,李从先,业治铮. 1991. 长江三角洲北翼全新统底界和“硬黏土层”的讨论. 海洋地质与第四纪地质,11(2): 37-46. [Chen B Z,Li C X,Ye Z Z. 1991. Holocene bottom boundary and‘hard clay band' in the northern flank of the Changjiang River Delta. Marine Geology & Quaternary Geology,11(2): 37-46]
[2] 范代读,李从先,陈美发,王德杰,丁平兴. 2001. 长江三角洲泥质潮坪沉积间断的定量分析. 海洋地质与第四纪地质,21(4): 1-6. [Fan D D,Li C X,Chen M F,Wang D J,Ding P X. 2011. Quantitative analyses on diastems of the mudflat deposit in the Yangtze River Delta. Marine Geology & Quaternary Geology,21(4): 1-6]
[3] 黄慧珍,唐保根,杨文达. 1996. 长江三角洲沉积地质学. 北京: 地质出版社,59-80. [Huang H Z,Tang B G,Yang W D. 1996. Sedimentary Geology of the Changjiang River Delta. Beijing: Geological Publishing House,59-80.]
[4] 冷伟,范代读. 2014. 联用筛析法与激光法进行粒度接序分析的界点选择. 沉积学报,32(3): 478-484. [Leng W,Fan D D. 2014. Selecting nodal size for the application of combined using sieving and laser methods in grain-size analysis. Acta Sedimentologica Sinica,32(3): 478-484]
[5] 李保华,王强,李从先. 2010. 长江三角洲亚三角洲地层结构对比. 古地理学报,12(6): 685-698. [Li B H,Wang Q,Li C X. 2010. Correlation of stratigraphic architecture of sub-deltas of Changjiang River Delta. Journal of Palaeogeography(Chinese Edition),12(6): 685-698]
[6] 李从先,陈庆强,范代读,张家强,杨守业. 1999. 末次盛冰期以来长江三角洲地区沉积相和古地理. 古地理学报,1(4): 12-25. [Li C X,Chen Q Q,Fan D D,Zhang J Q,Yang S Y. 1999. Palaeogeography and palaeoenvironment in Changjiang Delta since Last Glaciation. Journal of Palaeogeography(Chinese Edition),1(4): 12-25]
[7] 李从先,郭蓄民,许世远,王靖泰,李萍. 1979. 全新世长江三角洲地区砂体的特征和分布. 海洋学报,1(2): 252-268. [Li C X,Guo X M,Xu S Y,Wang J T,Li P. 1979. The characteristics and distribution of Holocene sand bodies in Changjiang River Delta area. Acta Oceanologia Sinica,1(2): 252-268]
[8] 李从先,汪品先. 1998. 长江晚第四纪河口地层学研究. 北京: 科学出版社,114-153. [Li C X,Wang P X. 1998. Late Quaternary Stratigraphy of the Yangtze Delta. Beijing: Science Press,114-153.]
[9] 李从先,张桂甲. 1996. 晚第四纪长江三角洲高分辨率层序地层学的初步研究. 海洋地质与第四纪地质,16(3): 13-24. [Li C X,Zhang G J. 1996. A primary study on high-resolution sequence stratigraphy of late Quaternary in the Yangtze River Delta area. Marine Geology & Quaternary Geology,16(3): 13-24]
[10] 尚帅,范代读,王强,张梦莹. 2013. MIS3以来浙江温瑞平原YQ0902孔古环境与古气候变化记录. 古地理学报,15(4): 551-564. [Shang S,Fan D D,Wang Q,Zhang M Y. 2013. Records of palaeoenvironment and palaeoclimate changes since the MIS3 in Borehole YQ0902 at Wenrui Plain,Zhejiang Province. Journal of Palaeogeography(Chinese Edition),15(4): 551-564]
[11] 施雅风,孔昭宸,王苏民,唐领余,王富葆,姚檀栋,赵希涛,张丕远,施少华. 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. [Shi Y F,Kong Z C,Wang S M,Tang L Y,Wang F B,Yao T D,Zhao X T,Zhang P Y,Shi S H. 1992. The climate fluctuation and important events of Holocene Megathermal in China. Science in China(Series B),22(12): 1300-1308]
[12] 唐保根,昝一平. 1986. 长江水下三角洲浅孔岩心的地层划分. 海洋地质与第四纪地质,6(2): 41-52. [Tang B G,Zan Y P. 1986. Stratigraphic division of cores from shallow holes in Changjiang River subaqueous delta. Marine Geology & Quaternary Geology,6(2): 41-52]
[13] 同济大学海洋地质系三角洲科研组. 1978. 全新世长江三角洲的形成和发育. 科学通报,23(5): 310-313. [The Marine Geology Department in Tongji University. 1978. The formation and growth of Yangtze Delta in Holocene Epoch. Chinese Science Bulletin,23(5): 310-313.]
[14] 王敏杰,郑洪波,谢昕,范代读,杨守业,赵泉鸿. 2010. 长江流域600年来古洪水: 水下三角洲沉积与历史记录对比. 科学通报,55(34): 3320-3327. [Wang M J,Zheng H B,Xie X,Fan D D,Yang S Y,Zhao Q H. 2010. A 600-year flood history in the Yangtze River drainage: Comparison between a subaqueous delta and historical records. Chinese Science Bulletin,55(34): 3320-3327]
[15] 王绍武. 2011. 全新世气候变化. 北京: 气象出版社,112-114. [Wang S W. 2011. The Holocene Climate Change. Beijing: China Meteorological Press,112-114]
[16] 王张华,Jingpu Paul Liu,赵宝成. 2007. 全新世长江泥沙堆积的时空分布及通量估算. 古地理学报,9(4): 419-429. [Wang Z H,Liu J P,Zhao B C. 2007. Spatial and temporal distribution of Changjiang sediments and estimation of sediment budget during the Holocene. Journal of Palaeogeography(Chinese Edition),9(4): 419-429]
[17] 魏乃颐,杨献忠,于俊杰,蒋仁,赵玲,张宗言,马雪,劳金秀. 2010. 长江三角洲顶部冰后期地层的沉积特征. 资源调查与环境,31(2): 79-86. [Wei N Y,Yang X Z,Yu J J,Jiang R,Zhao L,Zhang Z Y,Ma X,Lao J X. 2010. Seidmentary features of postglacial strata at the top of Changjiang River Delta. Resources Survey and Environment,31(2): 79-86]
[18] 吴标云,李从先. 1987. 长江三角洲第四纪地质. 北京: 海洋出版社,1-166. [Wu B Y,Li C X. 1987. Quaternary Geology of the Changjiang Delta. Beijing: Ocean Press,1-166.]
[19] 于俊杰,胡飞,杨祝良,张宗言,蒋仁,柯学,劳金秀. 2014. 江苏南通市四甲镇全新世以来有孔虫动物群的发现及其地质意义. 地质通报,33(10): 1609-1620. [Yu J J,Hu F,Yang Z L,Zhang Z Y,Jiang R,Ke X,Lao J X. 2014. Identification of Holocene foraminifera assemblages in Sijia Town of Nantong City,Jiangsu Province,and its geological significance. Geological Bulletin of China,33(10): 1609-1620]
[20] 张瑞虎,谢建磊,刘韬,赵宝成. 2011. 长江口水下三角洲沉积物记录的古环境演化. 海洋地质与第四纪地质,31(2),1-10. [Zhang R H,Xie J L,Liu T,Zhao B C. 2011. Palaeoenvironmental evolution of Subaqueous Yangtze Delta inferred from sedimentary records. Marine Geology & Quaternary Geology,31(2): 1-10]
[21] 张志忠,邹亮,杨振京,韩月,翟滨. 2015. 东海北部海域 DZS1钻孔孢粉记录与古环境研究. 海洋通报,34(5): 499-507. [Zhang Z Z,Zou L,Yang Z J,Han Y,Zhai B. 2015. Study of the spore-pollen record and palaeo-environment from borehole DZS1 in the northern sea area of East China Sea. Marine Science Bulletin,34(5): 499-507]
[22] 赵宝成. 2013. 长江三角洲前缘晚第四纪层序特征及冰后期海平面波动沉积响应. 上海国土资源,34(2): 50-54. [Zhao B C. 2013. Late Quaternary sequence stratigraphy of the Yangtze River Delta-front area with special reference to the response of the sedimentary environment to postglacial sea-level change. Shanghai Land and Resources,34(2): 50-54]
[23] 朱玉荣. 1999. 古长江河口湾充填潮流作用机制的初步探讨. 海洋学报,21(3): 73-82. [Zhu Y R. 1999. Preliminary study on the role of tidal currents in the filling of the paleo-Changjiang River estuary. Acta Oceanologica Sinica,21(3): 73-82]
[24] 竹淑贞,陈业裕,吕全荣,奚建国,孙永福. 1983. 上海地区全新世地层与古地理. 科学通报,28(5): 296-299. [Zhu S Z,Chen Y Y,Lü Q R,Xi J G,Sun Y F. 1983. The Holocene strata and pelaeogeography in Shanghai area. Chinese Science Bulletin,28(5): 296-299]
[25] 邹亮,张志忠,韩月. 2015. 长江口外海区DZS2孔第四纪磁性地层. 海洋地质与第四纪地质,35(2): 43-52. [Zou L,Zhang Z Z,Han Y. 2015. Magnetostratigraphy of core DZS2 off the Yangtze River estuary. Marine Geology & Quaternary Geology,35(2): 43-52]
[26] Allen G P,Posamentier H W. 1993. Sequence stratigraphy and facies model of an incised valley fill: The Gironde estuary,France. Journal of Sedimentary Research,63(3): 378-391.
[27] Bard E,Hamelin B,Arnold M,Montaggioni L,Cabioch G,Faure G. 1996. Deglacial sea-level record from Tahiti corals and the timing of global meltwater discharge. Nature,382(6588): 241-244.
[28] Bard E,Hamelin B,Delanghe-Sabatier D. 2010. Deglacial meltwater pulse 1B and Younger Dryas sea levels revisited with boreholes at Tahiti. Science,327(5970): 1235-1237.
[29] Bird M I,Austin W E,Wurster C M,Fifield L K,Mojtahid M,Sargeant C. 2010. Punctuated eustatic sea-level rise in the early mid-Holocene. Geology,38(9): 803-806.
[30] Bond G,Showers W,Cheseby M,Lotti R,Almasi P,Priore P,Bonani G. 1997. A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science,278(5341): 1257-1266.
[31] Catuneanu O,Galloway W E,Kendall C G S C,Miall A D,Posamentie H W,Strasser A,Tucker M E. 2011. Sequence stratigraphy: Methodology and nomenclature. Newsletters on Stratigraphy,44(3): 173-245.
[32] Chen Z Y,Song B P,Wang Z H,Cai Y L. 2000. Late Quaternary evolution of the sub-aqueous Yangtze Delta,China: Sedimentation,stratigraphy,palynology,and deformation. Marine Geology,162(2): 423-441.
[33] Chen Z Y,Wang Z H,Schneiderman J,Tao J,Cai Y L. 2005. Holocene climate fluctuations in the Yangtze delta of eastern China and the Neolithic response. The Holocene,15(6): 915-924.
[34] Fan D D,Shang S,Cai G F,Tu J B. 2015. Distinction and grain-size characteristics of intertidal heterolithic deposits in the middle Qiantang Estuary(East China Sea). Geo-Marine Letters,35(3): 161-174.
[35] Feng Z B,Liu B H,Zhao Y X,Li X S,Jiang L,Si S K. 2016. Spatial and temporal variations and controlling factors of sediment accumulation in the Yangtze River estuary and its adjacent sea area in the Holocene,especially in the Early Holocene. Continental Shelf Research,125(7): 1-17.
[36] Hanebuth T,Stattegger K,Grootes P M. 2000. Rapid flooding of the Sunda Shelf: A late-glacial sea-level record. Science,288(5468): 1033-1035.
[37] Hori K,Saito Y,Zhao Q H,Cheng X R,Wang P X,Sato Y,Li C X. 2001. Sedimentary facies and Holocene progradation rates of the Changjiang(Yangtze)delta,China. Geomorphology,41(2): 233-248.
[38] Hori K,Saito Y,Zhao Q H,Wang P X. 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.
[39] Innes J B,Zong Y Q,Wang Z H,Chen Z Y. 2014. Climatic and palaeoecological changes during the mid-to Late Holocene transition in eastern China: High-resolution pollen and non-pollen palynomorph analysis at Pingwang,Yangtze coastal lowlands. Quaternary Science Reviews,99(9): 164-175.
[40] Li C X,Chen Q Q,Zhang J Q,Yang S Y,Fan D D. 2000. Stratigraphy and paleoenvironmental changes in the Yangtze Delta during the Late Quaternary. Journal of Asian Earth Sciences,18(4): 453-469.
[41] Li C X,Wang P X,Sun H P,Zhang J Q,Fan D D,Deng B. 2002. Late Quaternary incised-valley fill of the Yangtze delta(China): Its stratigraphic framework and evolution. Sedimentary Geology,152(1): 133-158.
[42] Li G X,Li P,Liu Y,Qiao L L,Ma Y Y,Xu J S,Yang Z G. 2014. Sedimentary system response to the global sea level change in the East China Seas since the last glacial maximum. Earth-Science Reviews,139: 390-405.
[43] Liu J,Saito Y,Kong X H,Wang H,Xiang L H,Wen C,Nakashima R. 2010. Sedimentary record of environmental evolution off the Yangtze River estuary,East China Sea,during the last~13,000 years,with special reference to the influence of the Yellow River on the Yangtze River delta during the last 600 years. Quaternary Science Reviews,29(17): 2424-2438.
[44] Liu J P,Milliman J D,Gao S,Cheng P. 2004. Holocene development of the Yellow River's subaqueous delta,North Yellow Sea. Marine Geology,209(1): 45-67.
[45] Reineck H E,Singh I B. 1980. Depositional Sedimentary Environments. Springer Berlin Heidelberg,5-7.
[46] Saito Y. 1998. Sea levels of the last glacial in the East China Sea continental shelf. The Quaternary Research(Daiyonki-Kenkyu),37(3): 235-242.
[47] Song B,Li Z,Saito Y,Okuno J I,Lu A Q,Hua D,Li J,Li Y X,Nakashima R. 2013. Initiation of the Changjiang(Yangtze)delta and its response to the mid-Holocene sea level change. Palaeogeography,Palaeoclimatology,Palaeoecology,388: 81-97.
[48] Southon J,Kashgarian M,Fontugne M,Metivier B,Yim W W. 2002. Marine reservoir corrections for the Indian Ocean and Southeast Asia. Radiocarbon,44(1): 167-180.
[49] Stuiver M,Reimer P J. 1993. Extended 14 C database and revised CALIB radiocarbon calibration program. Radiocarbon,35(1): 215-230.
[50] Tjallingii R,Röhl U,Kölling M,Bickert T. 2007. Influence of the water content on X-ray fluorescence core scanning measurements in soft marine sediments. Geochemistry,Geophysics,Geosystems,8(2): 1074-1086.
[51] Uehara K,Saito Y,Hori K. 2002. Paleotidal regime in the Changjiang(Yangtze)Estuary,the East China Sea,and the Yellow Sea at 6,ka and 10,ka estimated from a numerical model. Marine Geology,183(1): 179-192.
[52] Vail P R. 1991. The stratigraphic signatures of tectonics,eustacy and sedimentology: An overview. Cycles and Events in Stratigraphy,123(1): 617-659.
[53] van Wagoner J C,Mitchum R M,Campion K M,Rahmanian V D. 1990. Siliciclastic sequence stratigraphy in well logs,cores,and outcrops: Concepts for high-resolution correlation of time and facies. American Association of Petroleum Geologists,7: 135-142.
[54] Walker M J C,Berkelhammer M,Björck S,Cwynar L C,Fisher D A,Long A J,Lowe J J,Newnham R M,Rasmussen S O,Weiss H. 2012. Formal subdivision of the holocene series/epoch: A discussion paper by a working group of intimate(integration of ice-core,marine and terrestrial records)and the subcommission on quaternary stratigraphy(international commission on stratigraphy). Journal of Quaternary Science,27(7): 649-659.
[55] Wang X,Shi X F,Wang G Q,Qiao S Q,Wang K S,Yao Z Q,Wang X C. 2015. Late Quaternary sedimentary environmental evolution offshore of the Hangzhou Bay,East China-implications for sea level change and formation of Changjiang alongshore current. Chinese Journal of Oceanology and Limnology,33(3): 748-763.
[56] Wang Z,Xu H,Zhan Q,Saito Y,He Z,Xie J,Li X,Dong Y. 2010. Lithological and palynological evidence of late Quaternary depositional environments in the subaqueous Yangtze delta,China. Quaternary Research,73(3): 550-562.
[57] Wang Z H,Zhuang C C,Saito Y,Chen J,Zhan Q,Wang X D. 2012. Early mid-Holocene sea-level change and coastal environmental response on the southern Yangtze delta plain,China: Implications for the rise of Neolithic culture. Quaternary Science Reviews,35(6): 51-62.
[58] Wang Z H,Saito Y,Hori K,Kitamura A,Chen Z Y. 2005. Yangtze offshore,China: Highly laminated sediments from the transition zone between subaqueous delta and the continental shelf. Estuarine,Coastal and Shelf Science,62(1): 161-168.
[59] Wellner R W,Bartek L R. 2003. The effect of sea level,climate,and shelf physiography on the development of incised-valley complexes: A modern example from the East China Sea. Journal of sedimentary research,73(6): 926-940.
[60] Wells J T. 1995. Tide-dominated estuaries and tidal rivers. Developments in Sedimentology,53(6): 179-205.
[61] Woodroffe S A. 2009. Testing models of mid to late Holocene sea-level change,north queensland,Australia. Quaternary Science Reviews,28(23-24): 2474-2488.
[62] Wu L,Zhu C,Zheng C G,Ma C M,Wang X H,Li F,Li B,Li K F. 2014. Impact of Holocene climate change on the prehistoric cultures of Zhejiang region,East China. Journal of Geographical Sciences,24(4): 669-688.
[63] Xu T Y,Wang G Q,Shi X F,Wang X,Yao Z Q,Yang G,Fang X S,Qiao S Q,Liu S F,Wang X C,Zhao Q. 2016. Sequence stratigraphy of the subaqueous Changjiang(Yangtze River)delta since the Last Glacial Maximum. Sedimentary Geology,331(9): 132-147.
[64] Xue C T. 2014. Missing evidence for stepwise postglacial sea level rise and an approach to more precise determination of former sea levels on East China Sea Shelf. Marine Geology,348(2): 52-62.
[65] Yi S,Saito Y,Yang D Y. 2006. Palynological evidence for Holocene environmental change in the Changjiang(Yangtze River)delta,China. Palaeogeography,Palaeoclimatology,Palaeoecology,241(1): 103-117.
[66] Yi S,Saito Y,Zhao Q H,Wang P C. 2003. Vegetation and climate changes in the Changjiang(Yangtze River)Delta,China,during the past 13 000 years inferred from pollen records. Quaternary Science Reviews,22(14): 1501-1519.
[67] Zaitlin B A,Dalrymple R W,Boyd R. 1994. The stratigraphic organization of incised-valley systems associated with relative sea-level change. SEPM Special Publication,51(2): 45-60.

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Postglacial sequence stratigraphy and sedimentary environment evolution of the Yangtze River subaqueous delta

冰后期以来长江水下三角洲层序地层特征及沉积环境演化^*

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Postglacial sequence stratigraphy and sedimentary environment evolution of the Yangtze River subaqueous delta

冰后期以来长江水下三角洲层序地层特征及沉积环境演化*

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冰后期以来长江水下三角洲层序地层特征及沉积环境演化^*