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Hydroclimatic changes in south-central China during the 4.2 ka event and their potential impacts on the development of Neolithic culture

Published online by Cambridge University Press:  12 May 2022

Tianli Wang ,
Dong Li ,
Xing Cheng ,
Jianghu Lan ,
R. Lawrence Edwards ,
Hai Cheng ,
Xingxing Liu ,
Gang Xue ,
Hai Xu  and
Le Ma
...Show all authors
Tianli Wang
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China University of Chinese Academy of Sciences, Beijing 100049, China Institute of Global Environment Change, Xi'an Jiaotong University, Xi'an 710054, China
Dong Li
Affiliation:
Library of Chang'an University, Xi'an 710064, China
Xing Cheng
Affiliation:
Shaanxi Experimental Center of Geological Survey, Shaanxi Institute of Geological Survey, Xi'an 710054, China
Jianghu Lan
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
R. Lawrence Edwards
Affiliation:
Department of Earth and Environmental Sciences, University of Minnesota, Minneapolis, Minnesota 55455, USA School of Geography, Nanjing Normal University, Nanjing 210097, China
Hai Cheng
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China Institute of Global Environment Change, Xi'an Jiaotong University, Xi'an 710054, China
Xingxing Liu
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
Gang Xue
Affiliation:
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China
Hai Xu
Affiliation:
Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China
Le Ma
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
Jingjie Zang
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
Yaqin Wang
Affiliation:
Xi'an Institute for Innovative Earth Environment Research, Xi'an 710061, China
Yongli Gao
Affiliation:
Department of Geological Sciences, University of Texas at San Antonio, San Antonio, Texas 78249, USA
Ashish Sinha
Affiliation:
Department of Earth Science, California State University, Carson, California 90747, USA
Liangcheng Tan*
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China Institute of Global Environment Change, Xi'an Jiaotong University, Xi'an 710054, China
*
*Corresponding author at: State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China. E-mail address: [email protected] (L. Tan).
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Abstract

The 4.2 ka event is widely presumed to be a globally widespread aridity event and has been linked to several episodes of societal changes across the globe. Whether this climate event impacted the cultural development in south-central China remains uncertain due to a lack of regional paleorainfall records. We present here stalagmite stable carbon isotope and trace element–based reconstruction of hydroclimatic conditions from south-central China. Our data reveal a sub–millennial scale (~5.6 to 4.3 ka) drying trend in the region followed by a gradual transition to wetter conditions during the 4.2 ka event (4.3–3.9 ka). Together with the existing archaeological evidence, our data suggest that the drier climate before 4.3 ka may have promoted the Shijiahe culture, while the pluvial conditions during the 4.2 ka event may have adversely affected its settlements in low-lying areas. While military conflicts with the Wangwan III culture may have accelerated the collapse of Shijiahe culture, we suggest that the joint effects of climate and the region's topography also played important causal roles in its demise.

Keywords

SpeleothemPrecipitationMiddle Yangtze RiverShijiahe cultureLate Holocene4.2 ka event
Type
Research Article
Information
Quaternary Research , Volume 109 , September 2022 , pp. 39 - 52
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Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2022

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Footnotes

†

Joint first authors: T. Wang and D. Li.

References

REFERENCES

Berkelhammer, M., Sinha, A., Stott, L., Cheng, H., Pausata, F.S.R., Yoshimura, K., 2012. An abrupt shift in the Indian monsoon 4000 years ago. Geophysical Monograph Series 198, 75–88.Google Scholar
Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P., deMenocal, P., Priore, P., Cullen, H., Hajdas, I., Bonani, G., 1997. A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science 278, 1257–1266.CrossRefGoogle Scholar
Bradley, R.S., Bakke, J., 2019. Is there evidence for a 4.2 ka BP event in the northern North Atlantic region? Climate of the Past 15, 1665–1676.CrossRefGoogle Scholar
Breitenbach, S.F.M., Rehfeld, K., Goswami, B., Baldini, J.U.L., Ridley, H.E., Kennett, D.J., Prufer, K.M., et al. , 2012. Constructing proxy records from age models (COPRA). Climate of the Past 8, 1765–1779.CrossRefGoogle Scholar
Broecker, W.S., 1994. Massive iceberg discharges as triggers for global climate change. Nature 372, 421–424.CrossRefGoogle Scholar
Cai, Y., Cheng, X., Ma, L., Mao, R., Breitenbach, S.F.M., Zhang, H., Xue, G., Cheng, H., Edwards, R.L., An, Z., 2021. Holocene variability of East Asian summer monsoon as viewed from the speleothem δ18O records in central China. Earth and Planetary Science Letters 558, 116758.CrossRefGoogle Scholar
Carolin, S.A., Walker, R.T., Day, C.C., Ersek, V., Sloan, R.A., Dee, M.W., Talebian, M., Henderson, G.M., 2019. Precise timing of abrupt increase in dust activity in the Middle East coincident with 4.2 ka social change. Proceeding of the National Academy of Science USA 116, 67–72.CrossRefGoogle ScholarPubMed
Chen, F., Xu, Q., Chen, J., Birks, H.J.B., Liu, J., Zhang, S., Jin, L., et al. , 2015. East Asian summer monsoon precipitation variability since the last deglaciation. Scientific Reports 5, 11186.CrossRefGoogle ScholarPubMed
Cheng, H., Edwards, R.L., Shen, C., Polyak, V.J., Asmerom, Y., Woodhead, J., Hellstrom, J., et al. , 2013. Improvements in 230Th dating, 230Th and 234U half-life values, and U-Th isotopic measurements by multi-collector inductively coupled plasma mass spectrometry. Earth and Planetary Science Letters 371–372, 82–91.CrossRefGoogle Scholar
Cheng, H., Edwards, R.L., Sinha, A., Spötl, C., Yi, L., Chen, S., Kelly, M., et al. , 2016a. The Asian monsoon over the past 640,000 years and ice age terminations. Nature 534, 640–646.CrossRefGoogle Scholar
Cheng, H., Spötl, C., Breitenbach, S.F.M., Sinha, A., Wassenburg, J.A., Jochum, K.P., Scholz, D., et al. , 2016b. Climate variations of Central Asia on orbital to millennial timescales. Scientific Reports 6, 36975.CrossRefGoogle Scholar
Cheng, H., Zhang, H., Zhao, J., Li, H., Ning, Y., Kathayat, G., 2019. Chinese stalagmite paleoclimate researches: a review and perspective. Science China-Earth Sciences 62, 1489–1513.CrossRefGoogle Scholar
Cosford, J., Qing, H., Eglington, B., Mattey, D., Yuan, D., Zhang, M., Cheng, H., 2008. East Asian monsoon variability since the mid-Holocene recorded in a high-resolution, absolute-dated aragonite speleothem from eastern China. Earth and Planetary Science Letters 275, 296–307.CrossRefGoogle Scholar
Cosford, J., Qing, H., Mattey, D., Eglington, B., Zhang, M., 2009. Climatic and local effects on stalagmite δ13C values at Lianhua Cave, China. Palaeogeography Palaeoclimatology Palaeoecology 280, 235–244.CrossRefGoogle Scholar
deMenocal, P.B., 2001. Cultural responses to climate change during the late Holocene. Science 292, 667–673.CrossRefGoogle ScholarPubMed
Dong, G., Li, T., Zhang, S., Ren, L., Li, R., Li, G., Xiao, Y., Wang, Z., Chen, F., 2021. Precipitation in surrounding mountains instead of lowlands facilitated the prosperity of ancient civilizations in the eastern Qaidam Basin of the Tibetan Plateau. Catena 203, 105318.CrossRefGoogle Scholar
Dong, J., Wang, Y., Cheng, H., Hardt, B., Edwards, R. L., Kong, X., Wu, J., et al. , 2010. A high-resolution stalagmite record of the Holocene East Asian monsoon Mt Shennongjia, central China. The Holocene 20, 257–264.CrossRefGoogle Scholar
Dorale, J.A., Liu, Z., 2009. Limitations of Hendy Test criteria in judging the paleoclimatic suitability of speleothems and the need for replication. Journal of Cave and Karst Studies 71, 73–80.Google Scholar
Dykoski, C.A., Edwards, R.L., Cheng, H., Yuan, D., Cai, Y., Zhang, M., Lin, Y., Qing, J., An, Z., Revenaugh, J., 2005. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China. Earth and Planetary Science Letters 233, 71–86.CrossRefGoogle Scholar
Edwards, R.L., Chen, J.H., Wasserburg, G.J., 1987. 238U-234U-230Th-232Th systematics and the precise measurement of time over the past 500,000 years. Earth and Planetary Science Letters 81, 175–192.CrossRefGoogle Scholar
Fairchild, I.J., Borsato, A., Tooth, A.F., Frisia, S., Hawkesworth, C.J., Huang, Y., McDermott, F., Spiro, B., 2000. Controls on trace element (Sr-Mg) compositions of carbonate cave waters: implications for speleothem climatic records. Chemical Geology 166, 255–269.CrossRefGoogle Scholar
Fairchild, I.J., Treble, P.C., 2009. Trace elements in speleothems as recorders of environmental change. Quaternary Science Reviews 28, 449–468.CrossRefGoogle Scholar
Fleitmann, D., Burns, S.J., Mudelsee, M., Neff, U., Kramers, J., Mangini, A., Matter, A., 2003. Holocene forcing of the Indian monsoon recorded in a stalagmite from southern Oman. Science 300, 1737–1739.CrossRefGoogle Scholar
Fohlmeister, J., Scholz, D., Kromer, B., Mangini, A., 2011. Modelling carbon isotopes of carbonates in cave drip water. Geochimica et Cosmochimica Acta 75, 5219–5228.CrossRefGoogle Scholar
Genty, D., Baker, A., Massault, M., Proctor, C., Gilmour, M., Pons-Branchu, E., Hamelin, B., 2001. Dead carbon in stalagmites: carbonate bedrock paleodissolution vs. ageing of soil organic matter. Implications for 13C variations in speleothems. Geochimica et Cosmochimica Acta 65, 3443–3457.Google Scholar
Genty, D., Blamart, D., Ouahdi, R., Gilmour, M., Baker, A., Jouzel, J., Van-Exter, S., 2003. Precise dating of Dansgaard-Oeschger climate oscillations in western Europe from stalagmite data. Nature 421, 833–837.CrossRefGoogle ScholarPubMed
Han, J., 2016. A comparison of civilized course between the central plain and Jianghan area. [In Chinese with English abstract.] Jianghan Archaeology 6, 39–44Google Scholar
Han, J., 2020a. Neolithic wars and the course of the early Chinese civilization. [In Chinese with English abstract.] Social Science Front: Military and Political History 10, 99–107.Google Scholar
Han, J., 2020b. Violent cultural changes in Longshan period and tribal warfare in Chinese legendary era. [In Chinese with English abstract.] Social Sciences 1, 152–163.Google Scholar
Han, J., Yang, X., 1997. A study of the Wangwan III culture. [In Chinese with English abstract.] Acta Archaeolofica Sinica 1, 1–22.Google Scholar
He, N., 2006. The discussion on the Xiaojiawuji culture and its related issues. [In Chinese.] Archaeology of the Three Dynasties (Two), 98–145Google Scholar
Hu, C., Henderson, G.M., Huang, J., Xie, S., Sun, Y., Johnson, K.R., 2008. Quantification of Holocene Asian monsoon rainfall from spatially separated cave records. Earth and Planetary Science Letters 266, 221–232.CrossRefGoogle Scholar
Huang, C., Pang, J., Zha, X., Su, H., Jia, Y., 2011. Extraordinary floods related to the climatic event at 4200 a BP on the Qishuihe River, middle reaches of the Yellow River, China. Quaternary Science Reviews 30, 460–468.CrossRefGoogle Scholar
Huang, C., Pang, J., Zha, X., Zhou, Y., Su, H., Li, Y., 2010. 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, 1–9.CrossRefGoogle Scholar
Huang, C., Pang, J., Zha, X., Zhou, Y., Su, H., Zhang, Y., Wang, H., Gu, H., 2012. Holocene palaeoflood events recorded by slackwater deposits along the lower Jinghe River valley, middle Yellow River basin, China. Journal of Quaternary Science 27, 485–493.CrossRefGoogle Scholar
Huang, X., Lin, D., Wang, J., Chang, S., 2013. Temporal and spatial NPP variation in the karst region in South China under the background of climate change. [In Chinese with English abstract.] Scientia Silvae Sinicae 49, 10–16.Google Scholar
Huang, Y.M., Fairchild, I.J., Borsato, A., Frisia, S., Cassidy, N.J., McDermott, F., Hawkesworth, C.J., 2001. Seasonal variations in Sr, Mg and P in modern speleothems (Grotta di Ernesto, Italy). Chemical Geology 175, 429–448.CrossRefGoogle Scholar
Jia, T., Ma, C., Zhu, C., Guo, T., Xu, J., Guan, H., Zeng, M., Huang, M., Zhang, Q., 2017. Depositional evidence of palaeofloods during 4.0-3.6 ka BP at the Jinsha site, Chengdu Plain, China. Quaternary International 440, 78–89.CrossRefGoogle Scholar
Kato, M., Fukusawa, H., Yasuda, Y., 2003. Varved lacustrine sediments of Lake Tougou-ike, western Japan, with reference to Holocene sea-level changes in Japan. Quaternary International 105, 33–37.CrossRefGoogle Scholar
Li, B., Zhu, C., Wu, L., Li, F., Sun, W., Wang, X., Liu, H., Meng, H., Wu, D., 2013. Relationship between environmental change and human activities in the period of the Shijiahe culture, Tanjialing site, Jianghan Plain, China. Quaternary International 308–309, 45–52.CrossRefGoogle Scholar
Li, D., Tan, L., Cai, Y., Jiang, X., Ma, L., Cheng, H., Edwards, R.L., Zhang, H., Gao, Y., An, Z., 2019a. Is Chinese stalagmite δ18O solely controlled by the Indian summer monsoon? Climate Dynamic 53, 2969–2983.CrossRefGoogle Scholar
Li, D., Tan, L., Guo, F., Cai, Y., Sun, Y., Xue, G., Cheng, X., et al. , 2019b. Application of Avaatech X-ray fluorescence core-scanning in Sr/Ca analysis of speleothems. Science China-Earth Sciences 62, 964–973.CrossRefGoogle Scholar
Li, H., Cheng, H., Sinha, A., Kathayat, G., Spötl, C., André, A.A., Meunier, A., et al. , 2018. Hydro-climatic variability in the southwestern Indian Ocean between 6000 and 3000 years ago. Climate of the Past 14, 1881–1891.CrossRefGoogle Scholar
Liu, F., Feng, Z., 2012. A dramatic climatic transition at ~4000 cal. yr BP and its cultural responses in Chinese cultural domains. The Holocene 22, 1181–1197.CrossRefGoogle Scholar
Liu, J., 2021. Preliminary exploration of prehistoric water control civilization in China. [In Chinese with English abstract.] Cultural Relics in Southern China 6, 5–11.Google Scholar
Liu, Z., Qu, Y., 2019. Vegetation change and its response to climate change based on SPOT-VGT in Hunan Province of southern China. [In Chinese with English abstract.] Journal of Beijing Forestry University 41, 80–87.Google Scholar
Maher, B.A., Thompson, R., 2012. Oxygen isotopes from Chinese caves: records not of monsoon rainfall but of circulation regime. Journal of Quaternary Science 27, 615–624.CrossRefGoogle Scholar
Ma, M., Dong, G., Chen, F., Meng, X., Wang, Z., Elston, R., Li, G., 2014. Process of paleofloods in Guanting basin, Qinghai Province, China and possible relation to monsoon strength during the mid-Holocene. Quaternary International 321, 88–96.CrossRefGoogle Scholar
Mayewski, P.A., Meeker, L.D., Twickler, M.S., Whitlow, S., Yang, Q., Lyons, W.B., Prentice, M., 1997. Major features and forcing of high-latitude northern hemisphere atmospheric circulation using a 110,000-year-long glaciochemical series. Journal of Geophysical Research Oceans 102, 26345–26366.CrossRefGoogle Scholar
McDermott, F., 2004. Palaeo-climate reconstruction from stable isotope variations in speleothems: a review. Quaternary Science Reviews 23, 901–918.CrossRefGoogle Scholar
Meng, H., 1997. Prehistoric Culture Structure in the Middle Reaches of the Yangtze River. [In Chinese.] Yangtze Literature and Art Press, Wuhan.Google Scholar
Meng, Y., 2011. The northward spread of Qujialing culture. [In Chinese with English abstract.] Huaxia Archaeology 3, 51–63.Google Scholar
Mudelsee, M., 2009. Break function regression: a tool for quantifying trend changes in climate time series. European Physical Journal-Special Topics 174, 49–63.CrossRefGoogle Scholar
Nagashima, K., Tada, R., Toyoda, S., 2013. Westerly jet-East Asian summer monsoon connection during the Holocene. Geochemistry Geophysics Geosystems 14, 5041–5053.CrossRefGoogle Scholar
Novello, V.F., Cruz, F.W., McGlue, M.M., Wong, C.I., Ward, B.M., Vuille, M., Santos, R.A., et al. , 2019. Vegetation and environmental changes in tropical South America from the last glacial to the Holocene documented by multiple cave sediment proxies. Earth and Planetary Science Letters 524, 115717.CrossRefGoogle Scholar
Ön, Z.B., Greaves, A.M., Akcer-Ön, S., Özeren, M.S., 2021. A Bayesian test for the 4.2 ka BP abrupt climatic change event in southeast Europe and southwest Asia using structural time series analysis of paleoclimate data. Climatic Change 165, 7.CrossRefGoogle Scholar
Railsback, L.B., Liang, F., Brook, G.A., Voarintsoa, N.R.G., Sletten, H.R., Marais, E., Hardt, B., Cheng, H., Edwards, R.L., 2018. The timing, two-pulsed nature, and variable climatic expression of the 4.2 ka event: a review and new high-resolution stalagmite data from Namibia. Quaternary Science Reviews 186, 78–90.CrossRefGoogle Scholar
Ronay, E.R., Breitenbach, S.F.M., Oster, J.L., 2019. Sensitivity of speleothem records in the Indian Summer Monsoon region to dry season infiltration. Scientific Reports 9, 5091.CrossRefGoogle ScholarPubMed
Shen, H., Yu, L., Zhang, H., Zhao, M., Lai, Z., 2015. OSL and radiocarbon dating of flood deposits and its paleoclimatic and archaeological implications in the Yihe River Basin, East China. Quaternary Geochronology 30, 398–404.CrossRefGoogle Scholar
Sinha, A., Kathayat, G., Weiss, H., Li, H., Cheng, H., Reuter, J., Schneider, A.W., et al. , 2019. Role of climate in the rise and fall of the Neo-Assyrian Empire. Science Advances 5, eaax6656.CrossRefGoogle ScholarPubMed
State Administration of Cultural Heritage of China, 2002. Cultural Relics Atlas of China. Part 1, Hubei Province. [In Chinese.] Map Press of Xi'an, Xi'an, China.Google Scholar
Staubwasser, M., Sirocko, F., Grootes, P.M., Segl, M., 2003. Climate change at the 4.2 ka BP termination of the Indus valley civilization and Holocene south Asian monsoon variability. Geophysical Research Letters 30, 1425.CrossRefGoogle Scholar
Sun, Q., Liu, Y., Wünnemann, B., Peng, Y., Jiang, X., Deng, L., Chen, J., Li, M., Chen, Z., 2019. Climate as a factor for Neolithic cultural collapses approximately 4000 years BP in China. Earth-Science Reviews 197, 102915.CrossRefGoogle Scholar
Tan, L., Cai, Y., Cheng, H., Edwards, R.L., Gao, Y., Xu, H., Zhang, H., An, Z., 2018a. Centennial- to decadal-scale monsoon precipitation variations in the upper Hanjiang River region, China over the past 6650 years. Earth and Planetary Science Letters 482, 580–590.CrossRefGoogle Scholar
Tan, L., Dong, G., An, Z., Edwards, R.L., Li, H., Li, D., Spengler, R., et al. , 2021. Megadrought and cultural exchange along the proto-silk road. Science Bulletin 66, 603–611.CrossRefGoogle Scholar
Tan, L., Liu, W., Wang, T., Cheng, P., Zang, J., Wang, X., Ma, L., et al. , 2020b. A multiple-proxy stalagmite record reveals historical deforestation in central Shandong, northern China. Science China-Earth Sciences 63, 1622–1632.CrossRefGoogle Scholar
Tan, L., Li, Y., Wang, X., Cai, Y., Lin, F., Cheng, H., Ma, L., Sinha, A., Edwards, R.L., 2020a. Holocene monsoon change and abrupt events on the western Chinese Loess Plateau as revealed by accurately dated stalagmites. Geophysical Research Letters 46, e2020GL090273.Google Scholar
Tan, L., Shen, C., Cai, Y., Cheng, H., Edwards, R.L., 2018b. Great flood in the middle-lower Yellow River reaches at 4000 a BP inferred from accurately-dated stalagmite records. Science Bulletin 63, 206–208.CrossRefGoogle Scholar
Tan, L., Shen, C., Cai, Y., Lo, L., Cheng, H., An, Z., 2014. Trace-element variations in an annually layered stalagmite as recorders of climatic changes and anthropogenic pollution in Central China. Quaternary Research 81, 181–188.CrossRefGoogle Scholar
Treble, P., Shelley, J.M.G., Chappell, J., 2003. Comparison of high resolution sub-annual records of trace elements in a modern (1911-1992) speleothem with instrumental climate data from southwest Australia. Earth and Planetary Science Letters 216, 141–153.CrossRefGoogle Scholar
Wang, C., Bendle, J.A., Zhang, H., Yang, Y., Liu, D., Huang, J., Cui, J., Xie, S., 2018. Holocene temperature and hydrological changes reconstructed by bacterial 3-hydroxy fatty acids in a stalagmite from central China. Quaternary Science Reviews 192, 97–105.CrossRefGoogle Scholar
Wang, H., 2013. Viewing the decline of Sanmiao culture from the archaeological remains in the heartland of Shijiahe culture. [In Chinese.] Jintian: Historical Philosophy 300, 120–121Google Scholar
Wang, J., 2007. On Post-Shijihe culture: terminology. Jianghan Archaeology 102, 60–72.Google Scholar
Wang, W., 2013. The Karst Features Research and Potential Calculation on Carbon Sink in the Basin of Dalongdong Underground in the Hunan Province. [In Chinese with English abstract.] Master's thesis, Guangxi Teachers Education University, Guilin Guangxi Province, China.Google Scholar
Wang, Y., Cheng, H., Edwards, R.L., He, Y., Kong, X., An, Z., Wu, J., Kelly, M.J., Dykoski, C.A., Li, X., 2005. The Holocene Asian monsoon: links to solar changes and North Atlantic climate. Science 308, 854–857.CrossRefGoogle ScholarPubMed
Wassenburg, J.A., Scholz, D., Jochum, K.P., Cheng, H., Oster, J., Immenhauser, A., Richter, D.K., et al. , 2016. Determination of aragonite trace element distribution coefficients from speleothem calcite–aragonite transitions. Geochimica et Cosmochimica Acta 190, 347–367.CrossRefGoogle Scholar
Watanabe, T.K., Watanabe, T., Yamazaki, A., Pfeiffer, M., 2019. Oman corals suggest that a stronger winter shamal season caused the Akkadian Empire (Mesopotamia) collapse. Geology 47, 1141–1145.CrossRefGoogle Scholar
Weiss, H., Bradley, R.S., 2001. What drives societal collapse? Science 291, 609–610.CrossRefGoogle ScholarPubMed
Weiss, H., Courty, M.A., Wetterstrom, W., Guichard, F., Senior, L., Meadow, R., Curnow, A., 1993. The genesis and collapse of third millennium North Mesopotamian civilization. Science 261, 995–1004.CrossRefGoogle ScholarPubMed
Wu, L., Zhu, C., Ma, C., Li, F., Meng, H., Liu, H., Li, L., Wang, X., Sun, W., Song, Y., 2017. Mid-Holocene palaeoflood events recorded at the Zhongqiao Neolithic cultural site in the Jianghan Plain, middle Yangtze River Valley, China. Quaternary Science Reviews 173, 145–160.CrossRefGoogle Scholar
Wu, W., Liu, T., 2004. Possible role of the “Holocene Event 3” on the collapse of Neolithic cultures around the Central Plain of China. Quaternary International 117, 153–166.Google Scholar
Xiao, J., Zhang, S., Fan, J., Wen, R., Zhai, D., Tian, Z., Jiang, D., 2018. The 4.2 ka event: multi-proxy records from a closed lake in the northern margin of the East Asian summer monsoon. Climate of the Past 14, 1417–1425.CrossRefGoogle Scholar
Xie, S., Evershed, R.P., Huang, X., Zhu, Z., Pancost, R.D., Meyers, P.A., Gong, L., et al. , 2013. Concordant monsoon-driven postglacial hydrological changes in peat and stalagmite records and their impacts on prehistoric cultures in central China. Geology 41, 827–830.CrossRefGoogle Scholar
Xue, G., Cai, Y., Lu, Y., Ma, L., Cheng, X., Liu, C., Yan, H., et al. , 2021. Speleothem-based hydroclimate reconstructions during the penultimate deglaciation in Northern China. Paleoceanography and Paleoclimatology 36, e2020PA004072.CrossRefGoogle Scholar
Yang, X., Scuderi, L.A., Wang, X., Scuderi, L.J., Zhang, D., Li, H., Forman, S., et al. , 2015. Groundwater sapping as the cause of irreversible desertification of Hunshandake Sandy Lands, Inner Mongolia, northern China. Proceeding of the National Academy of Science USA 112, 702–706.CrossRefGoogle ScholarPubMed
Yasuda, Y., Fujiki, T., Nasu, H., Kato, M., Morita, Y., Mori, Y., Kanehara, M., et al. , 2004. 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, 149–158.CrossRefGoogle Scholar
Yuan, D., Cheng, H., Edwards, R.L., Dykoski, C.A., Kelly, M.J., Zhang, M., Qing, J., et al. , 2004. Timing, duration, and transitions of the last interglacial Asian monsoon. Science 304, 575–578.CrossRefGoogle ScholarPubMed
Yu, S., Zhu, C., Song, J., Qu, W., 2000. Role of climate in the rise and fall of Neolithic cultures on the Yangtze Delta. Boreas 29, 157–165.CrossRefGoogle Scholar
Zeng, M., Ma, C., Zhu, C., Song, Y., Zhu, T., He, K., Chen, J., Huang, M., Jia, T., Guo, T., 2016. Influence of climate change on the evolution of ancient culture from 4500 to 3700 cal. yr BP in the Chengdu Plain, upper reaches of the Yangtze River, China. Catena 147, 742–754.CrossRefGoogle Scholar
Zhang, H., Brahim, Y.A., Li, H., Zhao, J., Kathayat, G., Tian, Y., Baker, J., et al. , 2019. The Asian summer monsoon: teleconnections and forcing mechanisms—a review from Chinese speleothem δ18O records. Quaternary 2, 26.CrossRefGoogle Scholar
Zhang, H., Cheng, H., Cai, Y., Spötl, C., Kathayat, G., Sinha, A., Edwards, R.L., Tan, L., 2018. Hydroclimatic variations in southeastern China during the 4.2 ka event reflected by stalagmite records. Climate of the Past 14, 1805–1817.CrossRefGoogle Scholar
Zhang, H., Cheng, H., Sinha, A., Spötl, C., Cai, Y., Liu, B., Kathayat, G., et al. , 2021. Collapse of the Liangzhu and other cultures in the lower Yangtze region in response to climate change. Science Advances 7, eabi9275.CrossRefGoogle ScholarPubMed
Zhang, H., Yu, K., Zhao, J., Feng, Y., Lin, Y., Zhou, W., Liu, G., 2013. East Asian Summer Monsoon variations in the past 12.5ka: high-resolution δ18O record from a precisely dated aragonite stalagmite in central China. Journal of Asian Earth Sciences 73, 162–175.Google Scholar
Zhang, J., Xia, Z., 2011. Deposition evidences of the 4 ka BP flood events in central China plains. [In Chinese with English abstract.] Acta Geographica Sinica 66, 685–697.Google Scholar
Zhang, Q., Zhu, C., Liu, C.L., Jiang, T., 2005. Environmental change and its impacts on human settlement in the Yangtze Delta, P.R. China. Catena 60, 267–277.CrossRefGoogle Scholar
Zhang, X., 1996. The origin and development of prehistoric rice-farming in the middle reaches of the Yangtze River. [In Chinese.] Agricultural History of China 15, 18–22.Google Scholar
Zhang, Y., Huang, C.C., Pang, J., Zha, X., Zhou, Y., Gu, H., 2013. Holocene paleofloods related to climatic events in the upper reaches of the Hanjiang River valley, middle Yangtze River basin, China. Geomorphology 195, 1–12.CrossRefGoogle Scholar
Zhang, Y., Huang, C.C., Pang, J., Zha, X., Zhou, Y., Wang, X., 2015. Holocene palaeoflood events recorded by slackwater deposits along the middle Beiluohe River valley, middle Yellow River basin, China. Boreas 44, 127–138.CrossRefGoogle Scholar
Zhao, J., Tan, L., Yang, Y., Pérez-Mejías, C., Brahim, Y.A., Lan, J., Wang, J., Li, H., Wang, T., Zhang, H., Cheng, H., 2021. New insights towards an integrated understanding of NE Asian monsoon during mid to late Holocene. Quaternary Science Reviews 254, 106793.CrossRefGoogle Scholar
Zhong, X., 2019. A review of the research on the Post-Shijiahe culture. [In Chinese with English abstract.] Journal of Archaeology and Museology 4, 24–33Google Scholar
Zhou, F., 1994. Historical evolution of Yunmeng marsh and Jingjiang delta. [In Chinese with English abstract.] Journal of Lake Sciences 6, 22–32.Google Scholar
Zhu, C., Zhong, Y., Zheng, C., Ma, C., Li, L., 2007. Relationship of Archaeological sites distribution and environment from the Paleolithic Age to the Warring States time in Hubei Province. [In Chinese with English abstract.] Acta Geographica Sinica 62, 227–242.Google Scholar
Zhu, Z., Feinberg, J.M., Xie, S., Bourne, M.D., Huang, C., Hu, C., Cheng, H., 2017. Holocene ENSO-related cyclic storms recorded by magnetic minerals in speleothems of central China. Proceeding of the National Academy of Science USA 114, 852–857.CrossRefGoogle ScholarPubMed