Aquatic Species Dominate Organic Matter in Qinghai Lake during the Holocene: Evidence from Eolian Deposits around the Lake
文献类型：期刊论文
| 作者 | Zeng, Fangming1 ; Liu, Xiangjun1; Li, Xiangzhong2; E, Chongyi3
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| 刊名 | JOURNAL OF EARTH SCIENCE
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| 出版日期 | 2017-06-01 |
| 卷号 | 28期号:3页码:484-491 |
| 关键词 | Qinghai Lake Total Organic Carbon (Toc) Organic Carbon Isotope (Delta C-13(Org)) Qinghai Tibetan Plateau |
| 文献子类 | Article |
| 英文摘要 | Total organic carbon (TOC) in lake sediments and its stable carbon isotope (delta C-13(org)) are widely applied to investigate paleoenvironmental changes even though their implications are complicated and multi -explanatory. Organic geochemistry studies of lake sediments from Qinghai Lake have been investigated, but some interpretations are controversial. In this study, TOC of one Holocene eolian section and delta C-13(org) of three eolian sections were studied around Qinghai Lake. Results indicate that the TOC content in eolian deposits was low during the Early Holocene, and gradually increased to high values during the Middle and Late Holocene. The variation in TOC content of eolian deposits is different from that in the lacustrine sequence from Qinghai Lake during the Holocene. The delta C-13(org) values in the eolian sections were relatively stable, with oscillation amplitudes of similar to 4 parts per thousand (ranging from -25.8 parts per thousand to -22.1 parts per thousand), in contrast to similar to 10 parts per thousand variations in delta C-13(org) values (varying from -30 parts per thousand to -20 parts per thousand) in lacustrine sediments. Through comparison of TOC and delta C-13(org) values between eolian deposits and lacustrine sediments, we can confirm indications that the organic matter in Qinghai Lake sediments during the Holocene was primarily a contribution of the aquatic species in the lake. This is significant for understanding the origin of organic matter in lake sediments on the northeastern Qinghai -Tibetan Plateau and for paleoenvironmental inferences using such proxies. |
| WOS关键词 | CHINESE LOESS PLATEAU ; TIBETAN PLATEAU ; LEVEL VARIATIONS ; LUMINESCENCE ; BASIN ; CHRONOLOGY ; EVOLUTION ; SEQUENCES ; SEDIMENTS ; ISOTOPES |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000402694100007 |
| 源URL | [http://ir.isl.ac.cn/handle/363002/6215]  |
| 专题 | 青海盐湖研究所_青海盐湖研究所知识仓储 青海盐湖研究所_盐湖地质与环境实验室 |
| 作者单位 | 1.Chinese Acad Sci, Qinghai Inst Salt Lakes, Key Lab Comprehens & Highly Efficient Utilizat Sa, Xining 810008, Peoples R China 2.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China 3.Qinghai Normal Univ, Key Lab Phys Geog & Environm Proc Qinghai Prov, Xining 810008, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zeng, Fangming,Liu, Xiangjun,Li, Xiangzhong,et al. Aquatic Species Dominate Organic Matter in Qinghai Lake during the Holocene: Evidence from Eolian Deposits around the Lake[J]. JOURNAL OF EARTH SCIENCE,2017,28(3):484-491. |
| APA | Zeng, Fangming,Liu, Xiangjun,Li, Xiangzhong,&E, Chongyi.(2017).Aquatic Species Dominate Organic Matter in Qinghai Lake during the Holocene: Evidence from Eolian Deposits around the Lake.JOURNAL OF EARTH SCIENCE,28(3),484-491. |
| MLA | Zeng, Fangming,et al."Aquatic Species Dominate Organic Matter in Qinghai Lake during the Holocene: Evidence from Eolian Deposits around the Lake".JOURNAL OF EARTH SCIENCE 28.3(2017):484-491. |
入库方式： OAI收割
来源：青海盐湖研究所
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