中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Freshwater radiocarbon reservoir age in the lower Yellow River floodplain during the late Holocene

文献类型:期刊论文

作者Cheng, Peng2; Yu, Shi-Yong1; Chen, Xue-Xiang3; Chen, Shiyue1; Hou, Zhanfang4
刊名HOLOCENE
出版日期2018
卷号28期号:1页码:119-126
关键词Flooding Sediments Lake Sediments Late Holocene Lower Yellow River Radiocarbon Reservoir Effect
DOI10.1177/0959683617715699
文献子类Article
英文摘要The radiocarbon concentration of the dissolved inorganic carbon (DIC) pool of most freshwater bodies such as lakes and rivers tends to be depleted with respect to that of the contemporaneous atmosphere, resulting in an apparent radiocarbon age of inorganic carbon therein known as freshwater reservoir effect. This phenomenon of radiocarbon age offset is usually site specific and varies over time. By radiocarbon dating pairs of twigs and gastropod shells preserved in an ancient lake, as well as gastropod shells in pre-bomb flooding sediments of known age, we are able to determine the freshwater radiocarbon reservoir effect in the lower Yellow River floodplain during the late Holocene. The regional freshwater radiocarbon reservoir age ranges from 1081 to 233 years with an average of 575 +/- 317 years, slightly older than that obtained from Lake Dongping by radiocarbon dating of live submerged aquatic plants. Our results show that the freshwater radiocarbon reservoir age is much older than its marine counterpart of the Yellow Sea and Bohai Bay. A source inversion using dual carbon isotopes (i.e. C-14 and C-13) and a linear mixing model revealed that the DIC in the surface water bodies was mainly from shallow groundwater and the Yellow River. Our results have broad relevance to the geological and archaeological chronologies based on the radiocarbon method for this area.
WOS关键词NORTH CHINA PLAIN ; ORGANIC-CARBON ; C-14 DATA ; VARIABILITY ; SEA ; CIVILIZATION ; OCEAN ; CALIBRATION ; ATMOSPHERE ; INITIATION
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000419836400009
源URL[http://ir.ieecas.cn/handle/361006/5182]  
专题地球环境研究所_加速器质谱中心
作者单位1.Jiangsu Normal Univ, Sch Geog Geomat & Planning, Xuzhou 221116, Jiangsu, Peoples R China
2.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Beijing, Peoples R China
3.Shandong Univ, Dept Archaeol, Jinan, Shandong, Peoples R China
4.Liaocheng Univ, Sch Environm & Planning, Liaocheng, Peoples R China
推荐引用方式
GB/T 7714
Cheng, Peng,Yu, Shi-Yong,Chen, Xue-Xiang,et al. Freshwater radiocarbon reservoir age in the lower Yellow River floodplain during the late Holocene[J]. HOLOCENE,2018,28(1):119-126.
APA Cheng, Peng,Yu, Shi-Yong,Chen, Xue-Xiang,Chen, Shiyue,&Hou, Zhanfang.(2018).Freshwater radiocarbon reservoir age in the lower Yellow River floodplain during the late Holocene.HOLOCENE,28(1),119-126.
MLA Cheng, Peng,et al."Freshwater radiocarbon reservoir age in the lower Yellow River floodplain during the late Holocene".HOLOCENE 28.1(2018):119-126.

入库方式: OAI收割

来源:地球环境研究所

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