Historical records and archaeological remains indicate that the Chinese agricultural economy changed significantly from the Warring States （475-221 BC） to Han Dynasties （206 BC-220 AD）, i.e., from rice-millet base...Historical records and archaeological remains indicate that the Chinese agricultural economy changed significantly from the Warring States （475-221 BC） to Han Dynasties （206 BC-220 AD）, i.e., from rice-millet based agriculture to rice-millet-wheat based agriculture. However, the variation of human diets and the inner relationship between human diets and the agricultural transition during this period remain poorly understood. In this paper, the C and N stable isotopes from human and animal bones at the Shenmingpu site （SMPS）, Xichuan County, Henan Province were analyzed. If some outliers （M34, M36, M102） were excluded, the mean δ13C value （（-16.7±0.8）‰, n=15） of humans in Hart Dynasties was dramatically lower than that in the Warring States （（-12.7±0.8）‰, n=14）, indicating that the cultivation of rice and wheat, especially wheat, had been more widely popularized in Han Dynasties. Meanwhile, the range of 615N values of humans （6.6‰-9.3‰） in Hart Dynasties was narrower than that of the Warring States （6.2‰-10.4‰）, suggesting that the animal protein resources in human foods during Han Dynasties were more concentrated. The transition of human diets and the close relationship with the change of agricultural economy in SMPS were due to more stable society, the carryout of new agricultural policies, and the emergence of new agri- cultural tools in Han Dynasties.展开更多
Earthquake archaeological research was conducted in recent years at four archaeological excavation sites in Shandong,focusing on the identification and analysis of the tectonic deformation phenomena. The non-tectonic ...Earthquake archaeological research was conducted in recent years at four archaeological excavation sites in Shandong,focusing on the identification and analysis of the tectonic deformation phenomena. The non-tectonic deformation phenomena were distinguished at the site of the Shang Dynasty ruins at Daxinzhuang in the Jinan suburbs. In Longshan,sand vein-filled cracks were recognized in the cultural layers of the Chengziya site,Zhangqiu City. Sand veins on the trench wall and sand tubes at the trench bottom were found densely distributed at the Shang and Zhou Dynasty cultural layers,at Qinhuangtai site,Binzhou City. The tectonic and non-tectonic origin cracks were identified on the city wall of the Site of Capital of State Qi,Linzi City. In Rizhao city,parallel distributed sand vein fracture groups were found in the cultural layer of Longshan-Warring States-Han Dynasty at Yaowangcheng site. Typical conjugate shear fractures were identified on the city wall of the ancient city of the State of Xue, Tengzhou City. The above natural deformation phenomena are concentrated in the culture layers of the Spring and AutumnWarring States-Han Dynasties and before, and characterized by seismic sand-soil liquefaction traces,which indicate that these regions might have been in the seismic active episodes in the corresponding periods. The above inference has been confirmed by microscopic data analysis.展开更多
基金supported by grants from CAS Knowledge Innovation Directional Project (Grant No.KZCX2-YW-Q1-04)CAS Strategic Priority Research Program (Grant Nos.XDA05130303, XDA05130501)+2 种基金Chinese Academy of Sciences & Max-Planck Institute Partnership Group Project (Grant No.KACX1-YW-0830)National Science and Technology Ministry (Grant No.2010BAK67B03)Relic Preservation Project of South-to-North Water Diversion
文摘Historical records and archaeological remains indicate that the Chinese agricultural economy changed significantly from the Warring States （475-221 BC） to Han Dynasties （206 BC-220 AD）, i.e., from rice-millet based agriculture to rice-millet-wheat based agriculture. However, the variation of human diets and the inner relationship between human diets and the agricultural transition during this period remain poorly understood. In this paper, the C and N stable isotopes from human and animal bones at the Shenmingpu site （SMPS）, Xichuan County, Henan Province were analyzed. If some outliers （M34, M36, M102） were excluded, the mean δ13C value （（-16.7±0.8）‰, n=15） of humans in Hart Dynasties was dramatically lower than that in the Warring States （（-12.7±0.8）‰, n=14）, indicating that the cultivation of rice and wheat, especially wheat, had been more widely popularized in Han Dynasties. Meanwhile, the range of 615N values of humans （6.6‰-9.3‰） in Hart Dynasties was narrower than that of the Warring States （6.2‰-10.4‰）, suggesting that the animal protein resources in human foods during Han Dynasties were more concentrated. The transition of human diets and the close relationship with the change of agricultural economy in SMPS were due to more stable society, the carryout of new agricultural policies, and the emergence of new agri- cultural tools in Han Dynasties.
基金supported by the Anhui Public Welfare Geological Project(No.2015-g-25)the Special Research Project of CEA(No.TYZ20160101)
文摘Earthquake archaeological research was conducted in recent years at four archaeological excavation sites in Shandong,focusing on the identification and analysis of the tectonic deformation phenomena. The non-tectonic deformation phenomena were distinguished at the site of the Shang Dynasty ruins at Daxinzhuang in the Jinan suburbs. In Longshan,sand vein-filled cracks were recognized in the cultural layers of the Chengziya site,Zhangqiu City. Sand veins on the trench wall and sand tubes at the trench bottom were found densely distributed at the Shang and Zhou Dynasty cultural layers,at Qinhuangtai site,Binzhou City. The tectonic and non-tectonic origin cracks were identified on the city wall of the Site of Capital of State Qi,Linzi City. In Rizhao city,parallel distributed sand vein fracture groups were found in the cultural layer of Longshan-Warring States-Han Dynasty at Yaowangcheng site. Typical conjugate shear fractures were identified on the city wall of the ancient city of the State of Xue, Tengzhou City. The above natural deformation phenomena are concentrated in the culture layers of the Spring and AutumnWarring States-Han Dynasties and before, and characterized by seismic sand-soil liquefaction traces,which indicate that these regions might have been in the seismic active episodes in the corresponding periods. The above inference has been confirmed by microscopic data analysis.
