中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Process of rice domestication in relation to Holocene environmental changes in the Ningshao Plain, lower Yangtze

文献类型:期刊论文

作者Shao, Konglan2,3; Zhang, Jianping2,5; Lu, Houyuan2,3,5; Gu, Zhaoyan2,3; Xu, Bing2,3; Zheng, Hongbo1; Sun, Guoping4; Huan, Xiujia2; He, Keyang2; Zou, Yafei1
刊名GEOMORPHOLOGY
出版日期2021-05-15
卷号381页码:11
关键词Phytoliths Diatoms Rice domestication Environmental change Neolithic Ningshao Plain
ISSN号0169-555X
DOI10.1016/j.geomorph.2021.107650
英文摘要Understanding the process of domestication and its relationship with environmental changes is fundamental to rice domestication research. The lower Yangtze region in China, with varied coastal environments and a flourishing Neolithic culture, was one of the major rice domestication centers in Asia. Here we present the results of 348 phytolith and 87 diatom samples from a 43.88-m-long core HMD1401 in the Ningshao Plain, southern part of the lower Yangtze. The results show that the study site was in a marine condition during the interval of -10,000?7000 cal. yr BP. Marine regressed after -7000 cal. yr BP, with occasional influences by sea water and flood. Rice was being domesticated in the Ningshao Plain at -9600 cal. yr BP, and rice domestication experienced a protracted process that lasted for over 3500 years. The influence of marine condition might contribute to the prolonging of rice domestication. Relatively stable terrestrial condition and intensive human activities promoted rice domestication in the Ningshao Plain. The results provide an improved understanding of the interrelations between early rice domestication and Holocene environmental changes in East Asia. Understanding the process of domestication and its relationship with environmental changes is fundamental to rice domestication research. The lower Yangtze region in China, with varied coastal environments and a flourishing Neolithic culture, was one of the major rice domestication centers in Asia. Here we present the results of 348 phytolith and 87 diatom samples from a 43.88-m-long core HMD1401 in the Ningshao Plain, southern part of the lower Yangtze. The results show that the study site was in a marine condition during the interval of-10,000?7000 cal. yr BP. Marine regressed after-7000 cal. yr BP, with occasional influences by sea water and flood. Rice was being domesticated in the Ningshao Plain at-9600 cal. yr BP, and rice domestication experienced a protracted process that lasted for over 3500 years. The influence of marine condition might contribute to the prolonging of rice domestication. Relatively stable terrestrial condition and intensive human activities promoted rice domestication in the Ningshao Plain. The results provide an improved understanding of the interrelations between early rice domestication and Holocene environmental changes in East Asia. ? 2021 Elsevier B.V. All rights reserved.
资助项目National Natural Science Foundation of China (NSFC)[41672176] ; Strategic Priority Research Program of Chinese Academy of Sciences[XDB26000000] ; National Key R&D Program of China[2020YFC1521605] ; Youth Innovation Promotion Association of the Chinese Academy of Sciences
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000634863200004
出版者ELSEVIER
资助机构National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; National Natural Science Foundation of China (NSFC) ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; Youth Innovation Promotion Association of the Chinese Academy of Sciences ; Youth Innovation Promotion Association of the Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/101073]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Shao, Konglan; Zhang, Jianping
作者单位1.Yunnan Univ, Yunnan Key Lab Earth Syst Sci, Kunming 650500, Yunnan, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Zhejiang Prov Inst Cultural Rel & Archaeol, Hangzhou 310014, Peoples R China
5.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Shao, Konglan,Zhang, Jianping,Lu, Houyuan,et al. Process of rice domestication in relation to Holocene environmental changes in the Ningshao Plain, lower Yangtze[J]. GEOMORPHOLOGY,2021,381:11.
APA Shao, Konglan.,Zhang, Jianping.,Lu, Houyuan.,Gu, Zhaoyan.,Xu, Bing.,...&Wu, Naiqin.(2021).Process of rice domestication in relation to Holocene environmental changes in the Ningshao Plain, lower Yangtze.GEOMORPHOLOGY,381,11.
MLA Shao, Konglan,et al."Process of rice domestication in relation to Holocene environmental changes in the Ningshao Plain, lower Yangtze".GEOMORPHOLOGY 381(2021):11.

入库方式: OAI收割

来源:地质与地球物理研究所

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