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Mid-Holocene coastal hydrology and salinity changes in the east Taihu area of the lower Yangtze wetlands, China

Published online by Cambridge University Press:  20 January 2017

Yongqiang Zong ,
James B. Innes ,
Zhanghua Wang  and
Zhongyuan Chen
Yongqiang Zong*
Affiliation:
Department of Earth Sciences, The University of Hong Kong, Hong Kong, Hong Kong Special Administration Region, China
James B. Innes
Affiliation:
Geography Department, Durham University, Durham, UK
Zhanghua Wang
Affiliation:
State key laboratory for Estuarine and Coastal Research, East China Normal University, Shanghai, China
Zhongyuan Chen
Affiliation:
State key laboratory for Estuarine and Coastal Research, East China Normal University, Shanghai, China
*
⁎Corresponding author. E-mail address:yqzong@hkucc.hku.hk (Y. Zong).
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Abstract

During the mid-Holocene the eastern Taihu area, on China's Yangtze delta plain, was populated by advanced late Neolithic cultures supported by intensive domesticated rice cultivation. This agricultural system collapsed around 4200 cal yr BP, with severe population decline, the end of the Liangzhu culture, and about half a millennium of very low-scale human activity in the area before the re-establishment of agricultural production. Microfossil analyses from six sedimentary sequences, supported by AMS 14C dating, has allowed reconstruction of mid-Holocene hydrological conditions and salinity changes which would have had a major influence on agricultural viability and cultural history in the coastal wetlands. These data, allied to existing stratigraphic and sea-level records, show that chenier ridges that developed after ca. 7000 cal yr BP in the east of the area sheltered it from marine inundation and although still connected to the sea through tidal creeks, low-salinity conditions persisted throughout the Neolithic period. There is no evidence that marine flooding caused the collapse of Liangzhu culture. Marine influence was stable and evolved slowly. Social and cultural causes may also have been important, but if environmental change triggered the collapse of Neolithic agricultural society here, other natural forces must be sought to explain this event.

Keywords

Mid-HoloceneCoastal environmentSea levelTaihu LakeNeolithic culturesDiatoms
Type
Research Article
Information
Quaternary Research , Volume 76 , Issue 1 , July 2011 , pp. 69 - 82
Copyright
University of Washington

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References

An, Z.S., Porter, S.C., Kutzbach, J.E., Wu, X.H., Wang, S.M., Liu, X.D., Li, X.Q., and Zhou, W.J. Asynchronous Holocene optimum of the East Asian monsoon. Quaternary Science Reviews 19, (2000). 743–762.Google Scholar
An, C.-B., Feng, Z., and Tang, L. Environmental change and cultural responses between 8000 and 4000 cal. yr BP in the western Loess Plateau, northwest China. Journal of Quaternary Science 19, (2004). 529–535.CrossRefGoogle Scholar
An, C.-B., Tang, L., Barton, L., and Chen, F.-H. Climate change and cultural response around 4000 cal yr BP in the western part of Chinese Loess Plateau. Quaternary Research 63, (2005). 347–352.Google Scholar
Anderson, A., Gagan, M., and Shulmeister, J. Mid-Holocene cultural dynamics and climatic change in the Western Pacific. Anderson, D.G., Maasch, K.A., and Sandweiss, D.H. Climate Change and Cultural Dynamics: A Global Perspective on Mid-Holocene Transitions. (2007). Academic Press, London. 265–296.Google Scholar
Anderson, D.G., Maasch, K.A., Sandweiss, D.H., and Mayewski, P.A. Climate and culture change: exploring Holocene transitions. Anderson, D.G., Maasch, K.A., and Sandweiss, D.H. Climate Change and Cultural Dynamics: A Global Perspective on Mid-Holocene Transition. (2007). Academic Press, London. 1–23.Google Scholar
Atahan, P., Grice, K., and Dodson, J. Agriculture and environmental change at Qingpu, Yangtze delta region, China: a biomarker, stable isotope and palynological approach. The Holocene 17, (2007). 507–515.CrossRefGoogle Scholar
Atahan, P., Itzstein-Davey, F., Taylor, D., Dodson, J., Qin, J., Zheng, H., and Brooks, A. Holocene-aged sedimentary records of environmental changes and early agriculture in the lower Yangtze, China. Quaternary Science Reviews 27, (2008). 556–570.Google Scholar
Bird, M.I., Fifield, L.K., Teh, T.S., Chang, C.H., Shirlaw, N., and Lambeck, K. An inflection in the rate of early mid-Holocene eustatic sea-level rise: a new sea-level curve from Singapore. Estuarine Coastal and Shelf Science 71, (2007). 523–536.CrossRefGoogle Scholar
Cao, Z., Ding, J., Hu, Z., Knicker, H., Kogel-Knabner, I., Yang, L., Yin, R., Lin, X., and Dong, Y. Ancient paddy soils from the Neolithic age in China's Yangtze River Delta. Naturwissenschaften 93, (2006). 232–236.Google Scholar
Chang, W.Y.B. Large lakes of China. Journal of Great Lakes Research 13, (1987). 235–249.Google Scholar
Chang, S., Yan, Q., and Guo, X. Characteristics and development of cheniers, southern part of Yangtze delta plain. Yan, Q., and Xu, S. Recent Yangtze Delta Deposits, Shanghai. (1987). East China Normal University Press, Shanghai. 37–48. (in Chinese) Google Scholar
Chang, W.Y.B., Xu, X., Yang, J., and Liu, J. Evolution in Taihu Lake ecosystem as evidence of changes in sediment profiles. Journal of Lake Sciences 6, (1994). 217–226.CrossRefGoogle Scholar
Chen, X. Changjiang (Yangtze) River delta, China. Journal of Coastal Research 14, (1998). 838–858.Google Scholar
Chen, Z., and Stanley, D.J. Sea-level rise on eastern China's Yangtze delta. Journal of Coastal Research 14, (1998). 360–366.Google Scholar
Chen, X., and Zong, Y. Coastal erosion along the Changjiang deltaic shoreline, China: history and prospective. Estuarine Coastal and Shelf Science 46, (1998). 733–742.Google Scholar
Chen, J., Liu, C., Zhang, C., and Walker, H.J. Geomorphological development and sedimentation in Qiantang estuary and Hangzhou Bay. Journal of Coastal Research 6, (1990). 559–572.Google Scholar
Chen, Z., Wang, Z., Schneiderman, J., Tao, J., and Cai, Y. Holocene climate fluctuations in the Yangtze delta of eastern China and the Neolithic response. The Holocene 15, (2005). 917–926.Google Scholar
Chen, Z., Zong, Y., Wang, Z., Wang, H., and Chen, J. Migration patterns of Neolithic settlements on the abandoned Yellow and Yangtze deltas of China. Quaternary Research 70, (2008). 301–314.Google Scholar
Chen, W., Wang, W.-M., and Dai, X.-R. Holocene vegetation history with implications of human impact in the Lake Chaohu area, Anhui Province, East China. Vegetation History and Archaeobotany 18, (2009). 137–146.CrossRefGoogle Scholar
CPAM (Committee for Preservation of Artifact Management) of Shanghai Fuchuanshan: report on excavations of the Neolithic site. (2000). Wenwu Press, Beijing. (in Chinese) Google Scholar
CPAM (Committee for Preservation of Artifact Management) of Shanghai Maqiao: report on the excavations between 1993 and 1997. (2002). Shanghai Fine Arts Publisher, Shanghai. (in Chinese) Google Scholar
Crawford, G.W., and Shen, C. The origins of rice agriculture: recent progress in East Asia. Antiquity 72, (1998). 858–866.Google Scholar
Fuller, D.Q., and Qin, L. Water management and labour in the origins and dispersal of Asian rice. World Archaeology 41, (2009). 88–111.Google Scholar
Fuller, D.Q., Qin, L., Zheng, Y., Zhao, Z., Chen, X., Hosoya, L.-A., and Sun, G.-P. The domestication process and domestication rate in rice: spikelet bases from the lower Yangtze. Science 323, (2009). 1607–1610.Google Scholar
Gao, H., Zhu, C., and Xu, W. Environmental change and cultural response around 4200 cal.yr BP in the Yishu River Basin, Shandong. Journal of Geographical Sciences 17, (2007). 285–292.CrossRefGoogle Scholar
Grimm, E.C. TILIA Software. (1993). Illinois State Museum, Chicago.Google Scholar
He, Y., Theakstone, W.H., Zhang, Z.L., Zhang, D.A., Yao, T.D., Chen, T., Shen, Y.P., and Pang, H.X. Asynchronous Holocene climatic change across China. Quaternary Research 61, (2004). 52–63.Google Scholar
Hong, X. Low temperature climates and sea-level changes during the Holocene. Yang, Z.G., and Lin, H.M. Quaternary Processes and Events in China Offshore and Onshore Areas. (1989). China Ocean Press, Beijing. 111–116. (in Chinese) Google Scholar
Hong, X. Origin and evolution of the Taihu Lake. Marine Geology and Quaternary Geology 11, (1991). 87–99. (in Chinese) Google Scholar
Hori, K., Saito, Y., Zhao, Q.H., and Wang, P.X. Architecture and evolution of the tide-dominated Changjiang (Yangtze) River delta, China. Sedimentary Geology 146, (2002). 249–264.Google Scholar
Huang, F., and Zhang, M. Pollen and phytolith evidence for rice cultivation during the Neolithic at Longqiuzhuang, eastern Jianghuai, China. Vegetation History and Archaeobotany 9, (2000). 161–168.CrossRefGoogle Scholar
Huang, R., Zhu, C., Guan, Y., and Zheng, C. Impact of Holocene environmental change on temporal-spatial distribution of Neolithic sites in Huaihe River Basin, Anhui Province. Journal of Geographical Sciences 16, (2006). 199–208.Google Scholar
Huang, C.C., Pang, J., Zha, X., Zhou, Y., Su, H., and Li, Y. Extraordinary floods of 4100–4000 a BP recorded at the Late Neolithic ruins in the Jinghe River Gorges, middle reach of the Yellow River, China. Palaeogeography, Palaeoclimatology, Palaeoecology 289, (2010). 1–9.CrossRefGoogle Scholar
Innes, J.B., Zong, Y., Chen, Z., Chen, C., Wang, Z., and Wang, H. Environmental history, palaeoecology and human activity at the early Neolithic forager/cultivator site at Kuahuqiao, Hangzhou, eastern China. Quaternary Science Reviews 28, (2009). 2277–2294.Google Scholar
Itzstein-Davey, F., Atahan, P., Dodson, J.R., Taylor, D., and Zheng, H. Environmental and cultural changes during the terminal Neolithic: Qingpu, Yangtze delta, eastern China. The Holocene 17, (2007). 875–887.CrossRefGoogle Scholar
Jiang, M., and Liu, Z. The Quaternary marine transgression in the northwest of Taihu Lake plain. Jiangsu. Geology 25, (2001). 78–81. (in Chinese) Google Scholar
Jiang, L., and Liu, L. New evidence for the origins of sedentism and rice domestication in the Lower Yangzi River, China. Antiquity 80, (2006). 355–361.Google Scholar
Jiao, T. Environment and culture change in Neolithic Southeast China. Antiquity 80, (2006). 615–621.Google Scholar
Jin, D., Cheng, X., Lin, Z., and Liu, X. Marine Diatoms in China. (1982). China Ocean Press, Beijing. (in Chinese).Google Scholar
Jing, Y., Flad, R., and Luo, Y. Meat-acquisition patterns in the Neolithic Yangzi river valley, China. Antiquity 82, (2008). 351–366.CrossRefGoogle Scholar
Lee, G.-A., Crawford, G.W., Liu, L., and Chen, X. Plants and people from the Early Neolithic to Shang periods in North China. Proceedings of the National Academy of Sciences 104, (2007). 1087–1092.Google Scholar
Li, C., Chen, Q., Zhang, J., Yang, S., and Fan, D. Stratigraphy and palaeoenvironmental changes in the Yangtze delta during the Late Quaternary. Journal of Asian Earth Sciences 18, (2000). 453–469.Google Scholar
Li, L., Zhu, C., Lin, L., Zhao, Q., Shi, G., Zheng, C., and Fan, C. Evidence for marine transgression between 7500–5400 BC at the Luotuodun site in Yixing, Jiangsu Province. Journal of Geographical Sciences 19, (2009). 671–680.CrossRefGoogle Scholar
Li, M., Mo, D., Mao, L., Sun, G., and Zhou, K. Palaeosalinity in the Tianluoshan site and the correlation between the Hemudu culture and its environmental background. Journal of Geographical Sciences 20, (2010). 441–454.Google Scholar
Li, Y., Wu, J., Hou, S., Shi, C., Mo, D., Liu, B., and Zhou, L. Palaeoecological records of environmental change and cultural development from the Liangzhu and Qujialing archaeological sites in the middle and lower reaches of the Yangtze River. Quaternary International 227, (2010). 29–37.CrossRefGoogle Scholar
Liu, L. The Chinese Neolithic—Trajectories to Early States. (2004). Cambridge University Press, Cambridge.Google Scholar
Liu, C., and Walker, H.J. Sedimentary characteristics of cheniers and the formation of the Chenier Plains of east China. Journal of Coastal Research 5, (1989). 353–368.Google Scholar
Liu, K., Sun, S., and Jiang, X. Environmental change in the Yangtze River delta since 12,000 years B.P. Quaternary Research 38, (1992). 32–45.Google Scholar
Liu, L., Lee, G.A., Jiang, L., and Zhang, J. Evidence for the early beginning (c. 9000 cal. BP) of rice domestication in China: a response. The Holocene 17, (2007). 1059–1068.CrossRefGoogle Scholar
Liu, X., Hunt, H.V., and Jones, M.K. River valleys and foothills: changing archaeological perceptions of North China's earliest farms. Antiquity 83, (2009). 82–95.Google Scholar
Lu, T.L.-D. Mid-Holocene climate and cultural dynamics in eastern Central China. Anderson, D.G., Maasch, K.A., and Sandweiss, D.H. Climate Change and Cultural Dynamics: A Global Perspective on Mid-Holocene Transitions. (2007). Academic Press, London. 297–329.Google Scholar
Lu, H., Liu, Z., Wu, N., Berné, S., Saito, Y., Liu, B., and Wang, L. Rice domestication and climatic change: phytolith evidence from East China. Boreas 31, (2002). 378–385.Google Scholar
Lutaenko, K.A., Zhuschikhovskaya, I.S., Mikishin, Y.A., and Popov, A.N. Mid-Holocene climate changes and cultural dynamics in the basin of the Sea of Japan and adjacent areas. Anderson, D.G., Maasch, K.A., and Sandweiss, D.H. Climate Change and Cultural Dynamics: A Global Perspective on Mid-Holocene Transitions. (2007). Academic Press, London. 331–406.Google Scholar
Moore, P.D., Webb, J.A., and Collinson, M.E. Pollen Analysis. (1991). Blackwell Scientific Publications, Oxford.Google Scholar
Morrill, C., Overpeck, J.T., and Cole, J.E. A synthesis of abrupt changes in the Asian summer monsoon since the last deglaciation. The Holocene 13, (2003). 465–476.Google Scholar
Palmer, A.J.M., and Abbott, W.H. Diatoms as indicators of sea-level change. van de Plassche, O. Sea-Level Research: a Manual for the Collection and Evaluation of Data. (1986). GeoBooks, Norwich. 457–488.Google Scholar
Peiser, B.J. Comparative analysis of late Holocene environmental and social upheaval: evidence for a disaster around 4000 BP. Peiser, B.J., Palmer, T., and Bailey, M. Natural Catastrophes during Bronze Age Civilisations. BAR International Series 728, (1998). 117–139. Oxford Google Scholar
Perry, C.A., and Hsu, K.J. Geophysical, archaeological and historical evidence support a solar-output model for climate change. Proceedings of the National Academy of Sciences 97, (2000). 12433–12438.CrossRefGoogle ScholarPubMed
Qin, J., Wu, G., Zheng, H., and Zhou, Q. The palynology of the First Hard Clay layer (late Pleistocene) from the Yangtze delta, China. Review of Palaeobotany and Palynology 149, (2008). 63–72.Google Scholar
Qin, J., Taylor, D., Atahan, P., Zhang, X., Wu, G., Dodson, J., Zheng, H., and Itzstein-Davey, F. Neolithic agriculture, freshwater resources and rapid environmental change on the lower Yangtze, China. Quaternary Research 75, (2010). 55–65.Google Scholar
Qu, W., Xue, B., Dickman, M.D., Wang, S., Fan, C., Wu, R., Zhang, P., Chen, J., and Wu, Y. A 14 000 year record of palaeoenvironmental change in the western basin of China's third largest lake, Lake Taihu. Hydrobiologia 432, (2000). 113–120.Google Scholar
Ren, G. Changes in forest cover in China during the Holocene. Vegetation History and Archaeobotany 16, (2007). 119–126.Google Scholar
Shanghai Museum, The Tangcunmiao Neolithic settlement, Songjiang, Shanghai. Kaogu 7, (1985). 584–594. (in Chinese) Google Scholar
Shanghai Museum, Report on the excavation of Siqian Neolithic settlement, Qingpu, Shanghai. Kaogu 10, (2002). 13–30. (in Chinese) Google Scholar
Shanghai Museum, Report on the 1988 and 1990 excavations of Tinglin Neolithic settlement, Jinshan, Shanghai. Kaogu 10, (2002). 49–63. (in Chinese) Google Scholar
Shanghai Museum, Report on the 2001–2005 excavations of Guangfulin Neolithic settlement, Songjiang, Shanghai. Kaogu 8, (2008). 675–693. (in Chinese) Google Scholar
Shi, Y., Kong, Z., Wang, S., Tang, L., Wang, F., Yao, T., Zhao, X., Zhang, P., and Shi, S. Mid-Holocene climates and environments in China. Global and Planetary Change 7, (1993). 219–233.Google Scholar
Shu, J., Wang, W., and Chen, W. Holocene vegetation and environmental changes in the NW Taihu plain, east China. Acta Micropalaeontologica Sinica 24, (2007). 210–221. (in Chinese) Google Scholar
Shu, J., Wang, W., Jiang, L., and Takahara, H. Early Neolithic vegetation history, fire regime and human activity at Kuahuqiao, lower Yangtze River, east China: new and improved insight. Quaternary International 227, (2010). 10–21.Google Scholar
Song, J. Reviews on the Archaeology of Shanghai. Kaogu 10, (2002). 867–872. (in Chinese) Google Scholar
Stanley, D.J., and Chen, Z. Neolithic settlement distributions as a function of sea level controlled topography in the Yangtze delta, China. Geology 24, (1996). 1083–1086.Google Scholar
Stanley, D.J., and Chen, Z. Radiocarbon dates in China's Holocene Yangtze delta: record of sediment storage and reworking, not timing of deposition. Journal of Coastal Research 16, (2000). 1126–1132.Google Scholar
Stanley, D.J., and Warne, A.G. Worldwide initiation of Holocene marine deltas by deceleration of sea-level rise. Science 265, (1994). 228–231.Google Scholar
Stanley, D.J., Chen, Z., and Song, J. Inundation, sea-level rise and transition from Neolithic to Bronze Age culture, Yangtze delta, China. Geoarchaeology 14, (1999). 15–26.3.0.CO;2-N>CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., and Braziunas, T.F. High-resolution radiocarbon age calibration for terrestrial and marine samples. Radiocarbon 40, (1998). 215–230.Google Scholar
Sun, S.C., and Huang, Y.P. The Taihu Lake. (1993). China Ocean Press, Beijing. 271 pp. (in Chinese) Google Scholar
Sun, S.C., Wu, Y.F., and Dong, B.F. Evolution and modern sediment of the Taihu Lake. Science in China, Series B 12, (1987). 78–86.Google Scholar
Tan, L.C., An, Z.S., Cai, Y.J., and Long, H. Hydrological representation of the 4.2 ka BP event in China and its global linkages. Geological Review 54, (2008). 94–104.Google Scholar
Tao, J., Chen, M., and Xu, S. A Holocene environmental record from the southern Yangtze River delta, eastern China. Palaeogeography, Palaeoclimatology, Palaeoecology 230, (2006). 204–229.Google Scholar
van der Werff, A. and Huls, H., (1958–1966). Diatomeeënflora van Nederland, 8 parts. published privately by van der Werff, A., Westziijde, 13a, De Hoef (U), The Netherlands.Google Scholar
van Geel, B. Application of fungal and algal remains and other microfossils in palynological analyses. Berglund, B.E. Handbook of Palaeoecology and Palynology. (1986). John Wiley and Sons, Chichester. 497–505.Google Scholar
van Geel, B. Non-pollen palynomorphs. Smol, J.P., Birks, H.J.B., and Last, W.M. Tracking Environmental Change using Lake Sediments, Volume 3: Terrestrial, Algal and Siliceous Indicators. (2001). Kluwer, Dordrecht. 99–119.Google Scholar
van Geel, B., and Aptroot, A. Fossil ascomycetes in Quaternary deposits. Nova Hedwigia 82, (2006). 313–329.Google Scholar
Vos, P.C., and de Wolf, H. Diatoms as a tool for reconstructing sedimentary environments in coastal wetlands: methodological aspects. Hydrobiologia 269, 270 (1993). 285–296.Google Scholar
Wang, J., and Liu, J. Amino acids and stable carbon isotope distributions in Taihu Lake, China, over the last 15,000 years, and their paleoecological implications. Quaternary Research 53, (2000). 223–228.Google Scholar
Wang, P., and Murray, J.W. The use of foraminifera as indicators of tidal effects in estuarine deposits. Marine Geology 51, (1983). 239–250.Google Scholar
Wang, F., Chien, N., Zhang, Y., and Yang, H. Pollen Flora of China. second ed. (1995). Science Press, Beijing (in Chinese).Google Scholar
Wang, J., Chen, X., Zhu, X., Liu, J., and Chang, W.Y.B. Taihu Lake, lower Yangtze drainage basin: evolution, sedimentation rate and the sea level. Geomorphology 41, (2001). 183–193.Google Scholar
Wang, Y., Cheng, H., Edwards, R.L., He, Y., Kong, X., An, Z., Wu, J., Kelly, M., Dykoski, C., and Li, X. The Holocene Asian monsoon: links to solar changes and North Atlantic climate. Science 308, (2005). 854–857.Google Scholar
Wang, Z.H., Chen, Z.Y., and Tao, J. Clay mineral analysis of sediments in the Changjiang delta plain and its application to the Late Quaternary variations of sea level and sediment provenance. Journal of Coastal Research 22, (2006). 683–691.Google Scholar
Wang, Z., Xu, H., Zhan, Q., Saito, Y., He, Z., Xie, J., Li, X., and Dong, Y. Lithological and palynological evidence of late Quaternary depositional environments in the subaqueous Yangtze delta, China. Quaternary Research 73, (2010). 550–562.Google Scholar
Wang, Z., Li, M., Zhang, R., Zhuang, C., Liu, Y., Saito, Y., Xie, J., and Zhao, B. Impacts of human activity on the late-Holocene development of the subaqueous Yangtze delta, China, as shown by magnetic properties and sediment accumulation rates. The Holocene 21, (2011). 393–407.Google Scholar
Wu, W.T. Holocene palaeogeography along the Hangzhou Bay as constructed on the basis of Neolithic cultural remains. Acta Geographica Sinica 38, (1983). 113–126. (in Chinese) Google Scholar
Wu, W., and Liu, T. Possible role of the ‘Holocene event 3’ on the collapse of Neolithic cultures around the central plain of China. Quaternary International 117, (2004). 153–166.Google Scholar
Wu, L., Wang, X., Zhou, K., Mo, D., Zhu, C., Gao, C., Zhang, G., Li, L., and Han, W. Transmutation of ancient settlements and environmental changes between 6000 and 2000 a BP in the Chaohu Lake Basin, east China. Journal of Geographical Sciences 20, (2010). 687–700.CrossRefGoogle Scholar
Xu, X., Chang, W.Y.B., and Liu, J. Changes in vegetation and climate in the Taihu Lake during the last 11,000 years. Acta Palaeontologica Sinica 35, (1996). 175–186. (in Chinese) Google Scholar
Yan, Q.S., and Huang, S. Evolution of Holocene sedimentary environment in the Hangzhou-Jiaxing-Huzhou plain. Acta Geographica Sinica 42, (1987). 1–15.Google Scholar
Yan, Q., Xu, S., and Shao, X. Holocene cheniers in the Yangtze delta, China. Marine Geology 90, (1989). 337–343.Google Scholar
Yang, H.R., Xie, Z.R., and Yang, D.Y. Formation and evolution of the Taihu lake and the Holocene sea level. Yang, H.R. Collection of the Quaternary Glaciation and Quaternary Geology. (1987). Publishing House of Geology, Beijing. 49–64. (in Chinese) Google Scholar
Yasuda, Y., Fujiki, T., Nasu, H., Kato, M., Morita, Y., Mori, Y., Kanehara, M., Toyama, S., Yano, A., Okuno, M., He, J., Ishihara, S., Kitagawa, H., Fukusawa, H., and Naruse, T. Environmental archaeology at the Chengtoushan site, Hunan Province, China, and implications for environmental change and the rise and fall of the Yangtze River civilization. Quaternary International 123–125, (2004). 149–158.Google Scholar
Yi, S., Saito, Y., Zhao, Q.H., and Wang, P.X. 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, (2003). 1501–1519.Google Scholar
Yi, S., Saito, Y., and Yang, D. Palynological evidence for Holocene environmental changes in the Changjiang (Yangtze River) delta, China. Palaeogeography, Palaeoclimatology, Palaeoecology 241, (2006). 103–117.CrossRefGoogle Scholar
Yim, W., Huang, W.-S., Fontugne, G., Hale, M.R., Paterne, R.E., Pirazzoli, M., Ridley, P.A., and Thomas, W.N. Postglacial sea-level changes in the northern South China Sea continental shelf: evidence for a post-8200 calendar yr BP meltwater pulse. Quaternary International 145–146, (2006). 55–67.Google Scholar
Yu, S., Zhu, C., Song, H., and Qu, W. Role of climate in the rise and fall of Neolithic cultures on the Yangtze delta. Boreas 29, (2000). 157–165.Google Scholar
Zeng, L., and Shannon, M.C. Salinity effects on seedling growth and yield components of rice. Crop Science 40, (2000). 996–1003.Google Scholar
Zhang, Y. Causes of Liangzhu culture's disappearance from micropalaeontology. Scientia Geographica Sinica 27, (2007). 376–379.Google Scholar
Zhang, Y., Xi, Y., Zhang, J., Gao, G., Du, N., Sun, X., and Kong, Z. Spore Morphology of Chinese Pteridophytes. (1990). Science Press, Beijing.Google Scholar
Zhang, Q., Liu, C., Zhu, C., and Jiang, T. Environmental change and its impacts on human settlement in the Changjiang river delta in Neolithic age. Chinese Geographical Science 14, (2004). 239–244.Google Scholar
Zhang, Q., Jiang, T., Shi, Y., King, L., Liu, C., and Metzler, M. Palaeo-environmental changes in the Yangtze delta during past 8000 years. Journal of Geographical Sciences 14, (2004). 105–112.Google Scholar
Zhang, Q., Zhu, C., Liu, C.L., and Jiang, T. Environmental change and its impacts on human settlement in the Yangtze delta, P.R. China. Catena 60, (2005). 267–277.Google Scholar
Zhao, X. Development of cheniers in China and their significance to coastal shift. Gardiner, V. International Geomorphology 1986 Part I. (1987). John Wiley and Sons, Chichester. 1251–1268.Google Scholar
Zhao, Y., Yu, Z., Chen, F., Zhang, J., and Yang, B. Vegetation response to Holocene climate change in monsoon-influenced region of China. Earth-Science Reviews 97, (2009). 242–256.Google Scholar
Zheng, Y., Matsui, A., and Fujiwara, H. Phytoliths in rice detected in the Neolithic sites in the valley of the Taihu lake in China. Environmental Archaeology 8, (2003). 177–183.Google Scholar
Zheng, Y., Sun, G., Qin, L., Li, C., Wu, X., and Chen, X. Rice fields and modes of rice cultivation between 5000 and 2500 BC in east China. Journal of Archaeological Science 36, (2009). 2609–2616.Google Scholar
Zhou, W., Yu, X., Jull, A.J.T., Burr, G., Xiao, J.Y., Lu, X., and Xian, F. High-resolution evidence from southern China of an early Holocene optimum and a mid-Holocene dry event during the last 18,000 years. Quaternary Research 62, (2004). 39–48.Google Scholar
Zhu, C., Zheng, C., Ma, C., Yang, X., Gao, X., Wang, H., and Shao, J. On the Holocene sea-level highstand along the Yangtze delta and Ningshao Plain, East China. Chinese Science Bulletin 48, (2003). 2672–2683.Google Scholar
Zong, Y. Mid-Holocene sea-level highstand along the southeast coast of China. Quaternary International 117, (2004). 55–67.Google Scholar
Zong, Y., and Horton, B.J. Diatom zones across intertidal flats and coastal saltmarshes in Britain. Diatom Research 13, (1998). 375–394.Google Scholar
Zong, Y., Lloyd, J.M., Leng, M.J., Yim, W.W.-S., and Huang, G. Reconstruction of Holocene monsoon history from the Pearl River estuary, southern China, using diatoms and carbon isotope ratios. The Holocene 16, (2006). 251–263.Google Scholar
Zong, Y., Chen, Z., Innes, J.B., Chen, C., Wang, Z., and Wang, H. Fire and flood management of coastal swamp enabled first rice paddy cultivation in east China. Nature 449, (2007). 459–463.Google Scholar
Zong, Y., Kemp, A.C., Yu, F., Lloyd, J.M., Huang, G., and Yim, W.W.-S. Diatoms from the Pearl River estuary, China and their suitability as water salinity indicators for coastal environments. Marine Micropaleontology 75, (2010). 38–49.Google Scholar
Zou, H., Gou, J., Li, M., Tang, L., Ding, J., and Yao, Q. Findings of paddies of Majiabang culture at Caoxieshan, Jiangsu Province. Yan, W., and Yasuda, Y. The Origins of Rice Agriculture, Pottery and Cities. (2000). Cultural Relics Publishing House, Beijing. 97–114. (in Chinese) Google Scholar