Diets, eco-environments and seasonal variations recorded in the oxygen and carbon isotopic compositions of mammal tooth enamel from the Shunshanji site, Sihong County, Jiangsu Province, China

被引:9
作者
Tian XiaoSi [1 ,2 ]
Zhu Cheng [3 ]
Shui Tao [1 ]
Huang YunPing [4 ]
机构
[1] Nanjing Univ, Dept Hist, Nanjing 210093, Jiangsu, Peoples R China
[2] Chizhou Coll, Chizhou 247100, Peoples R China
[3] Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing 210093, Jiangsu, Peoples R China
[4] Peking Univ, Fac Archaeol & Museol, Beijing 100871, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 2013年 / 58卷 / 31期
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
Shunshanji site; enamel; stable carbon isotope; stable oxygen isotope; palaeodiets; eco-environment; seasonal variations; PLEISTOCENE MAMMALS; STABLE CARBON; PHOSPHATE; ECOLOGY; HABITAT; HORSES; AGE;
D O I
10.1007/s11434-013-5894-z
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The carbon and oxygen isotopic compositions of the tooth enamel of mammals, including deer, wild pigs, buffaloes and domesticated pigs from the Shunshanji site, Sihong County, Jiangsu Province, China, were analyzed to reconstruct the mammals' ecoenvironments and diets, and to evaluate seasonal variations in the study area. Carbon isotopic compositions of buck samples revealed that the deer ate completely C-3 plants and the environments they inhabited were relatively open and that wild pigs ate primarily C-3 plants. Oxygen isotopic compositions indicated that the body sources of these two mammals were different, i.e. the deer and pigs lived in different niches within a relatively similar ecosystem. Modern domesticated pigs were isotopically more positive than the ancient wild pigs in carbon delta C-13 values, suggesting the former ingested more C-3 plants relative to the latter. Although the delta O-18 data showed modern domesticated and ancient pigs had similar oxygen isotope compositions, their water sources were different. The carbon and oxygen isotopic patterns of premolar microsamples of ancient and modern buffaloes indicated that the plants ingested by the ancient buffalo varied with seasonal shifts, but plants ingested by the modern buffalo were relatively constant. The eco-environment of the modern buffalo was more open, warmer and drier than eco-environment of the ancient buffalo, which may be the result of the deforestation and other human activities. Ancient and modern seasonal changes were clearly recorded in the isotopic patterns and the seasonal variation amplitudes of the ancient and modern eco-environments were similar.
引用
收藏
页码:3788 / 3795
页数:8
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