Clay mineralogy of the Stari Slankamen (Serbia) loess-paleosol sequence during the last glacial cycle d Implications for dust provenance and interglacial climate
文献类型：期刊论文
| 作者 | Fu, Yu1,2; Hao, Qingzhen1,2,3; Peng, Shuzhen4; Markovic, Slobodan B.5; Gao, Xinbo1; Han, Long1; Wu, Xuechao1; Namier, Namier1,2; Zhang, Wei4; Gavrilov, Milivoj B.5 |
| 刊名 | QUATERNARY SCIENCE REVIEWS
 |
| 出版日期 | 2021-07-01 |
| 卷号 | 263页码:14 |
| 关键词 | Loess Europe Carpathian Basin Clay mineralogy Last glacial cycle Provenance |
| ISSN号 | 0277-3791 |
| DOI | 10.1016/j.quascirev.2021.106990 |
| 英文摘要 | ABS T R A C T Clay minerals in loess-paleosol sequences carr y important information on dust source and the paleo-environments of the areas of loess distribution. The loess-paleosol sequences in the Serbian part of the Carpathian Basin are among the most complete Quaternary terrestrial sedimenta r y sequences in Europe. However, relatively little is known about the origin and temporal variations of clay minerals in these deposits and their paleoclimatic implications. Here we present the results of high-resolution XRD clay mineral analysis of the Stari Slankamen loess-paleosol sequence through the last glacial cycle. The roughly constant composition of the clay minerals within the loess unit and most of the paleosol sug-gests that the clay minerals are of detrital origin and that pedogenic transformation has only occurred in the lower part of paleosol S1, which corresponds to the climatic optimum of Marine Isotope Stage (MIS) 5e. This provides a basis for addressing several important issues regarding the Carpathian Basin loess, including its provenance, glacial dust activity, and the interglacial climate. The smectite-rich character-istic of the glacial loess provides a diagnostic indicator for confirming local sources for the Carpathian Basin loess deposits, and that these sources made little contribution to the dust deposited in Greenland during the last glacial. The first application of illite crystallinity and the chlorite ratio to the Carpathian Basin loess-paleosol sequence suggests that they are more sensitive indicators than the clay mineral proxies previously used in European loess studies. The enhanced precipitation during MIS 5e indicated by the new proxies and the transformation of clay mineral potentially provide new insights into un-derstanding the regional climatic response to future global warming. (c) 2021 Elsevier Ltd. All rights reserved. |
| WOS关键词 | SURFACE TEMPERATURE VARIABILITY ; PLEISTOCENE LOESS ; NORTHERN SERBIA ; PALEOCLIMATIC SIGNIFICANCE ; VOJVODINA REGION ; CENTRAL-EUROPE ; STORM-TRACKS ; GRAIN-SIZE ; ICE CORE ; SEA |
| 资助项目 | Natural Science Foundation of China (NSFC)[41888101] ; National Key Research and Development Program[2017YFE0112800] ; NSFC[41625010] ; NSFC[41690114] ; NSFC[41877442] ; Strategic Priority Research Program of Chinese Academy of Sciences[XDB26000000] ; First Program of the Chinese-Serbian Developing Projects |
| WOS研究方向 | Physical Geography ; Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000664741500001 |
| 出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
| 资助机构 | Natural Science Foundation of China (NSFC) ; Natural Science Foundation of China (NSFC) ; Natural Science Foundation of China (NSFC) ; Natural Science Foundation of China (NSFC) ; National Key Research and Development Program ; National Key Research and Development Program ; National Key Research and Development Program ; National Key Research and Development Program ; NSFC ; NSFC ; NSFC ; NSFC ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; First Program of the Chinese-Serbian Developing Projects ; First Program of the Chinese-Serbian Developing Projects ; First Program of the Chinese-Serbian Developing Projects ; First Program of the Chinese-Serbian Developing Projects ; Natural Science Foundation of China (NSFC) ; Natural Science Foundation of China (NSFC) ; Natural Science Foundation of China (NSFC) ; Natural Science Foundation of China (NSFC) ; National Key Research and Development Program ; National Key Research and Development Program ; National Key Research and Development Program ; National Key Research and Development Program ; NSFC ; NSFC ; NSFC ; NSFC ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; First Program of the Chinese-Serbian Developing Projects ; First Program of the Chinese-Serbian Developing Projects ; First Program of the Chinese-Serbian Developing Projects ; First Program of the Chinese-Serbian Developing Projects ; Natural Science Foundation of China (NSFC) ; Natural Science Foundation of China (NSFC) ; Natural Science Foundation of China (NSFC) ; Natural Science Foundation of China (NSFC) ; National Key Research and Development Program ; National Key Research and Development Program ; National Key Research and Development Program ; National Key Research and Development Program ; NSFC ; NSFC ; NSFC ; NSFC ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; First Program of the Chinese-Serbian Developing Projects ; First Program of the Chinese-Serbian Developing Projects ; First Program of the Chinese-Serbian Developing Projects ; First Program of the Chinese-Serbian Developing Projects ; Natural Science Foundation of China (NSFC) ; Natural Science Foundation of China (NSFC) ; Natural Science Foundation of China (NSFC) ; Natural Science Foundation of China (NSFC) ; National Key Research and Development Program ; National Key Research and Development Program ; National Key Research and Development Program ; National Key Research and Development Program ; NSFC ; NSFC ; NSFC ; NSFC ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; First Program of the Chinese-Serbian Developing Projects ; First Program of the Chinese-Serbian Developing Projects ; First Program of the Chinese-Serbian Developing Projects ; First Program of the Chinese-Serbian Developing Projects |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/101968]  |
| 专题 | 地质与地球物理研究所_中国科学院新生代地质与环境重点实验室 |
| 通讯作者 | Hao, Qingzhen; Peng, Shuzhen |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China 4.Taishan Univ, Key Lab Tourism & Resources Environm Univ Shandon, Tai An 271021, Shandong, Peoples R China 5.Univ Novi Sad, Fac Sci, Dept Phys Geog, Trg Dositeja Obradovica 3, Novi Sad 21000, Serbia |
| 推荐引用方式 GB/T 7714 | Fu, Yu,Hao, Qingzhen,Peng, Shuzhen,et al. Clay mineralogy of the Stari Slankamen (Serbia) loess-paleosol sequence during the last glacial cycle d Implications for dust provenance and interglacial climate[J]. QUATERNARY SCIENCE REVIEWS,2021,263:14. |
| APA | Fu, Yu.,Hao, Qingzhen.,Peng, Shuzhen.,Markovic, Slobodan B..,Gao, Xinbo.,...&Guo, Zhengtang.(2021).Clay mineralogy of the Stari Slankamen (Serbia) loess-paleosol sequence during the last glacial cycle d Implications for dust provenance and interglacial climate.QUATERNARY SCIENCE REVIEWS,263,14. |
| MLA | Fu, Yu,et al."Clay mineralogy of the Stari Slankamen (Serbia) loess-paleosol sequence during the last glacial cycle d Implications for dust provenance and interglacial climate".QUATERNARY SCIENCE REVIEWS 263(2021):14. |
入库方式： OAI收割
来源：地质与地球物理研究所
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