Jianghan plain, the locale of China’s Great Flood four thousand years ago

Abstract The Yellow River Plain (YRP), being regarded as the cradle of Chinese civilization, is traditionally thought to be the locale of the Great Flood, a hazardous flood (or floods) tamed by Yu who started China’s first “dynasty”, Xia, in ~ 2000 BC. However, by integrating published archaeologica...

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Main Authors: Li-Xin Guo, Meng-Long Hsieh, Olga Gorodetskaya, Zi-Hao Fan, Shih-Ying Chiu
Format: Article
Language:English
Published: Springer 2023-09-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access:https://doi.org/10.1007/s44195-023-00044-4
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author Li-Xin Guo
Meng-Long Hsieh
Olga Gorodetskaya
Zi-Hao Fan
Shih-Ying Chiu
author_facet Li-Xin Guo
Meng-Long Hsieh
Olga Gorodetskaya
Zi-Hao Fan
Shih-Ying Chiu
author_sort Li-Xin Guo
collection DOAJ
description Abstract The Yellow River Plain (YRP), being regarded as the cradle of Chinese civilization, is traditionally thought to be the locale of the Great Flood, a hazardous flood (or floods) tamed by Yu who started China’s first “dynasty”, Xia, in ~ 2000 BC. However, by integrating published archaeological data, we propose that the Great Flood in fact impacted the Jianghan Plain (JHP) along the middle course of the Yangtze River. The arguments include: (1) around the era of the Great Flood, the most civilized and populated society in East Asia, named the Jianghan society, was located around the JHP (at that time, the habitation on the YRP remained limited); (2) the Jianghan society lived on river resources (shipping and rice growing) and was thus subject to flood risks (but not for the people inhabiting the YRP); (3) the people in the Jianghan society were experienced in dredging moats/ditches for shipping and irrigation; (4) unlike the floods on the YRP that were characterized by dynamic sedimentation and channel avulsion, those on the JHP typically occurred with slow-moving water manageable to ancient people; (5) the JHP has been associated with lake/wetland systems serving as detention basins during floods. Here, the recorded method for controlling the Great Flood, dredging channels to divert flood water to a “sea”, was feasible. Known speleothem paleo-rainfall data from multiple sites show that the climate of the JHP had been wet since the middle Holocene (earlier than the era of the Great Flood) and significantly turned dry after ~ 1850 BC (~ 150 years later than the Great Flood). Thus, the uniqueness of the Great Flood was likely to reflect an increase in land use on the JHP with the expansion of the Jianghan society, and the success in taming this flood was mainly due to the efforts of the society, not by luck.
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spelling doaj.art-002d4e46d3604a138e961df7b53aad962023-11-26T13:33:18ZengSpringerTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802023-09-0134112610.1007/s44195-023-00044-4Jianghan plain, the locale of China’s Great Flood four thousand years agoLi-Xin Guo0Meng-Long Hsieh1Olga Gorodetskaya2Zi-Hao Fan3Shih-Ying Chiu4Department of Anthropology, Sun Yat-Sen UniversityDepartment of Earth and Environmental Sciences, National Chung Cheng UniversityInstitute of Global Humanities, Nanjing UniversityInstitute of Archaeology, Chinese Academy of HistoryDepartment and Institute of History, National Chung Cheng UniversityAbstract The Yellow River Plain (YRP), being regarded as the cradle of Chinese civilization, is traditionally thought to be the locale of the Great Flood, a hazardous flood (or floods) tamed by Yu who started China’s first “dynasty”, Xia, in ~ 2000 BC. However, by integrating published archaeological data, we propose that the Great Flood in fact impacted the Jianghan Plain (JHP) along the middle course of the Yangtze River. The arguments include: (1) around the era of the Great Flood, the most civilized and populated society in East Asia, named the Jianghan society, was located around the JHP (at that time, the habitation on the YRP remained limited); (2) the Jianghan society lived on river resources (shipping and rice growing) and was thus subject to flood risks (but not for the people inhabiting the YRP); (3) the people in the Jianghan society were experienced in dredging moats/ditches for shipping and irrigation; (4) unlike the floods on the YRP that were characterized by dynamic sedimentation and channel avulsion, those on the JHP typically occurred with slow-moving water manageable to ancient people; (5) the JHP has been associated with lake/wetland systems serving as detention basins during floods. Here, the recorded method for controlling the Great Flood, dredging channels to divert flood water to a “sea”, was feasible. Known speleothem paleo-rainfall data from multiple sites show that the climate of the JHP had been wet since the middle Holocene (earlier than the era of the Great Flood) and significantly turned dry after ~ 1850 BC (~ 150 years later than the Great Flood). Thus, the uniqueness of the Great Flood was likely to reflect an increase in land use on the JHP with the expansion of the Jianghan society, and the success in taming this flood was mainly due to the efforts of the society, not by luck.https://doi.org/10.1007/s44195-023-00044-4China’s Great FloodYellow RiverYangtze RiverArchaeologySpeleothem paleo-rainfall record
spellingShingle Li-Xin Guo
Meng-Long Hsieh
Olga Gorodetskaya
Zi-Hao Fan
Shih-Ying Chiu
Jianghan plain, the locale of China’s Great Flood four thousand years ago
Terrestrial, Atmospheric and Oceanic Sciences
China’s Great Flood
Yellow River
Yangtze River
Archaeology
Speleothem paleo-rainfall record
title Jianghan plain, the locale of China’s Great Flood four thousand years ago
title_full Jianghan plain, the locale of China’s Great Flood four thousand years ago
title_fullStr Jianghan plain, the locale of China’s Great Flood four thousand years ago
title_full_unstemmed Jianghan plain, the locale of China’s Great Flood four thousand years ago
title_short Jianghan plain, the locale of China’s Great Flood four thousand years ago
title_sort jianghan plain the locale of china s great flood four thousand years ago
topic China’s Great Flood
Yellow River
Yangtze River
Archaeology
Speleothem paleo-rainfall record
url https://doi.org/10.1007/s44195-023-00044-4
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