Palaeoenvironmental implications of a Holocene sequence of lacustrine-peat sediments from the desert-loess transitional zone in Northern China
文献类型:期刊论文
作者 | Jia, Feifei1; Lu, Ruijie2,3,4; Liu, Xiaokang2,3,4,5; Zhao, Chao6; Lv, Zhiqiang2,3,4; Gao, Shangyu2,3,4 |
刊名 | JOURNAL OF ASIAN EARTH SCIENCES
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出版日期 | 2018-05-01 |
卷号 | 156页码:167-173 |
关键词 | Desert-loess transitional zone Holocene Lacustrine sediments Environmental evolution |
ISSN号 | 1367-9120 |
DOI | 10.1016/j.jseaes.2018.01.030 |
通讯作者 | Lu, Ruijie(ruijielu@bnu.edu.cn) |
英文摘要 | A high-resolution lacustrine-peat record from the desert-loess transitional zone in Northern China was obtained to reconstruct Holocene environmental change in the region. AMS C-14 dates are used to provide a chronology. The results indicate that the site was a desert environment before 12.2 cal kyr BP, and was then occupied by a paleolake which started to shrink, with a wetland occurring from 6.2 to 3.0 cal kyr BP. Subsequently, the site became a seasonally water-filled depression. Based on the lithology and measurements of grain size and total organic carbon content, the climate changed from arid to humid at 12.2 cal kyr BP, and became more humid after 8.3 cal kyr BP. From 6.2 to 3.0 cal kyr BP, precipitation decreased but the climate remained at an optimum. After 3.0 cal kyr BP, the climate was dry overall but with several humid intervals. A comparison of paleoclimatic records from lacustrine and aeolian deposits from the region reveals a discrepancy about the nature of the early Holocene climate, and we conclude that this is because lacustrine sediments responded more sensitively to precipitation than aeolian deposits when the temperature was low. The environmental evolution of the region was synchronous with changes in the Asian summer monsoon (ASM), but temperature also played a key role in the early Holocene. |
WOS关键词 | MU US DESERT ; MULTI-PROXY ANALYSES ; ASIAN MONSOON ; ENVIRONMENTAL-CHANGES ; MONGOLIAN PLATEAU ; CLIMATIC CHANGES ; NORTHWEST CHINA ; TIBETAN PLATEAU ; INNER-MONGOLIA ; POLLEN RECORD |
资助项目 | National Natural Science Foundation of China[41330748] ; National Natural Science Foundation of China[41571184] ; National Natural Science Foundation of China[41071128] ; National Natural Science Foundation of China[41601190] |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000428829700012 |
出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
资助机构 | National Natural Science Foundation of China |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/57294] ![]() |
专题 | 中国科学院地理科学与资源研究所 |
通讯作者 | Lu, Ruijie |
作者单位 | 1.Liaoning Normal Univ, Sch Urban & Environm Sci, Dalian 116029, Peoples R China 2.Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China 3.Beijing Normal Univ, MOE Engn Ctr Desertificat & Blownsand Control, Beijing 100875, Peoples R China 4.Beijing Normal Univ, Fac Geog Sci, Beijing 100875, Peoples R China 5.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, State Key Lab Resources & Environm Informat Syst, Beijing 100101, Peoples R China 6.Univ Chinese Acad Sci, Beijing 100049, Peoples R China |
推荐引用方式 GB/T 7714 | Jia, Feifei,Lu, Ruijie,Liu, Xiaokang,et al. Palaeoenvironmental implications of a Holocene sequence of lacustrine-peat sediments from the desert-loess transitional zone in Northern China[J]. JOURNAL OF ASIAN EARTH SCIENCES,2018,156:167-173. |
APA | Jia, Feifei,Lu, Ruijie,Liu, Xiaokang,Zhao, Chao,Lv, Zhiqiang,&Gao, Shangyu.(2018).Palaeoenvironmental implications of a Holocene sequence of lacustrine-peat sediments from the desert-loess transitional zone in Northern China.JOURNAL OF ASIAN EARTH SCIENCES,156,167-173. |
MLA | Jia, Feifei,et al."Palaeoenvironmental implications of a Holocene sequence of lacustrine-peat sediments from the desert-loess transitional zone in Northern China".JOURNAL OF ASIAN EARTH SCIENCES 156(2018):167-173. |
入库方式: OAI收割
来源:地理科学与资源研究所
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