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The evolution of cropping structure in prehistoric Xizang.
Wang, Yanren; Yang, Qi; Yang, Jishuai; Sharma, Shalini; Huang, Yunzhe; He, Wei; Tsring, Tinley; Hu, Shihua; Chen, Songtao; Sun, Qingli; You, Ting; Gu, Zhengquan; Tsho, Yang; Wangdue, Shargan; Chen, Zujun; Gao, Yu; Yang, Xiaoyan; Chen, Fahu.
Afiliação
  • Wang Y; Group of Alpine Paleoecology and Human Adaptation (ALPHA), State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; National Centre for Archaeology, Beijing 100013, China.
  • Yang Q; Group of Alpine Paleoecology and Human Adaptation (ALPHA), State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; University of Chinese Academy of Sciences, Beijing 100086, C
  • Yang J; Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China; Key Scientific Research Base of Bioarchaeology in Cold and Arid Regions (Lanzhou University & Gansu Provincial Institute of Cul
  • Sharma S; Group of Alpine Paleoecology and Human Adaptation (ALPHA), State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China.
  • Huang Y; Group of Alpine Paleoecology and Human Adaptation (ALPHA), State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; University of Chinese Academy of Sciences, Beijing 100086, C
  • He W; Tibetan Institute for the Preservation of Cultural Relics, Lhasa 850001 China.
  • Tsring T; Tibetan Institute for the Preservation of Cultural Relics, Lhasa 850001 China. Electronic address: chilie@126.com.
  • Hu S; Group of Alpine Paleoecology and Human Adaptation (ALPHA), State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; University of Chinese Academy of Sciences, Beijing 100086, C
  • Chen S; Group of Alpine Paleoecology and Human Adaptation (ALPHA), State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; National Centre for Archaeology, Beijing 100013, China.
  • Sun Q; Group of Alpine Paleoecology and Human Adaptation (ALPHA), State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; Zhejiang Provincial Institute of Cultural Relics and Archaeo
  • You T; Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China; Key Scientific Research Base of Bioarchaeology in Cold and Arid Regions (Lanzhou University & Gansu Provincial Institute of Cul
  • Gu Z; Group of Alpine Paleoecology and Human Adaptation (ALPHA), State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China.
  • Tsho Y; Tibetan Institute for the Preservation of Cultural Relics, Lhasa 850001 China.
  • Wangdue S; Tibetan Institute for the Preservation of Cultural Relics, Lhasa 850001 China.
  • Chen Z; Tibetan Institute for the Preservation of Cultural Relics, Lhasa 850001 China.
  • Gao Y; Group of Alpine Paleoecology and Human Adaptation (ALPHA), State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China. Electronic address: yugao@itpcas.ac.cn.
  • Yang X; Group of Alpine Paleoecology and Human Adaptation (ALPHA), State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; Key Laboratory of Western China's Environmental Systems (Min
  • Chen F; Group of Alpine Paleoecology and Human Adaptation (ALPHA), State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; Key Laboratory of Western China's Environmental Systems (Min
Sci Bull (Beijing) ; 2024 Jun 24.
Article em En | MEDLINE | ID: mdl-39030104
ABSTRACT
The origin and spread of agriculture facilitated a decline in human mobility and eventually led to a predominantly sedentary lifestyle globally, including on the Tibetan Plateau. Previous studies have proposed an evolution of prehistoric agriculture, from millet-based to barley-based farming. However, details regarding the process are vague. Here, we present diachronic changes in cropping structure from Xizang on the basis of a quantitative analysis of archaeobotanical remains from 12 sites located in southeastern Xizang. The advent of agriculture in Xizang began in the southeastern region around 4800 cal a BP and resulted in a quick spread of millet agriculture from the Hengduan Mountains to the Yarlung Zangbo River region. Subsequently, the introduction of barley and wheat in Xizang led to the transformation of millet-based farming into mixed farming after 3600 cal a BP. Eventually, around 3000 cal a BP, barley and wheat dominated across the entire Xizang with declining occurrences of millet. It took more than 600 years for barley and wheat to dominate in the Tibetan cropping system, which may reflect the time required for these exotic species to adapt physiologically to their new niche. In addition to the diachronic changes in crop farming, the ratio of barley to wheat and foxtail millet to broomcorn millet also varied at different elevations possibly due to local environmental variations and the crops' physiological requirements.
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Texto completo: 1 Base de dados: MEDLINE Idioma: En Ano de publicação: 2024 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Idioma: En Ano de publicação: 2024 Tipo de documento: Article