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Magnetic stratigraphy of the Danube loess: A composite Titel-Stari Slankamen loess section over the last one million years in Vojvodina, Serbia

文献类型：期刊论文

作者Song, Yang1,2; Guo, Zhengtang1,3,4; Markovic, Slobodan5,6; Hambach, Ulrich6,7,8; Deng, Chenglong3,9; Chang, Lin1,10; Wu, Jianyu1; Hao, Qingzhen1,3
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2018-04-15
卷号155页码:68-80
关键词Magnetostratigraphy Serbian loess Danube loess Chinese loess Intercontinental correlations
ISSN号1367-9120
DOI10.1016/j.jseaes.2017.11.012
文献子类Article
英文摘要In Europe, the most complete loess-paleosol sequences over the past million years are preserved in the Serbian part of the Danube River drainage basin. The similarity in stratigraphy and climatic cycles between the Serbian and the Chinese loess sequences suggests that the loess deposits in these two regions could play an important role in the study of intercontinental climatic correlations and linkage. However, previous magnetostratigraphic studies of the Serbian loess, mainly conducted using the alternating field (AF) demagnetization approach, show significant differences with the Chinese loess, especially the stratigraphic positioning of the Matuyama-Brunhes boundary (MBB). Here, we conduct a detailed magnetostratigraphic investigation of a composite Titel-Stari Slankamen loess section in the Vojvodina (northern Serbia), using thermal and hybrid demagnetization methods, aiming to establish new chronological constraints for the Danube Basin loess. Based on the analyses of the mineral magnetic properties, anisotropy of magnetic susceptibility, progressive thermal and hybrid demagnetization, the MBB was determined within S8, broadly consistent with the MBB position seen in the Chinese loess. Present evidence supports the hypothesis that the overall normal polarity in the upper part of L9, with a thickness of 2.1 m, was possibly caused by a combination of the remagnetization of remanence-carrying coarse grained magnetite during the Brunhes normal chron and bioturbation during the forming of the overlying paleosol S8. Thus, our magnetostratigraphic results provide solid chronological evidence for the coherence of pedostratigraphy and climatostratigraphy for the loess deposits in the Danube Basin and China. The synchronous occurrence of the strongest developed paleosol S5 (corresponding to MISs 15-13) and the least weathered thick loess unit L9 (corresponding to MISs 24-22) in the two regions confirms that extreme climatic events during these two intervals are possibly common features of the climate in the Northern Hemisphere at those times.
WOS关键词VIATOVO NE BULGARIA ; CHINESE LOESS ; PALEOSOL SEQUENCES ; MATUYAMA-BRUNHES ; CENTRAL-EUROPE ; LOESS/PALAEOSOL SEQUENCE ; PALEOCLIMATIC RECORD ; PLEISTOCENE LOESS ; CLIMATIC CYCLES ; NORTHERN SERBIA
WOS研究方向Geology
语种英语
WOS记录号WOS:000428006300007
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Natural Science Foundation of China(41430531 ; National Natural Science Foundation of China(41430531 ; National Natural Science Foundation of China(41430531 ; National Natural Science Foundation of China(41430531 ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; Serbian Ministry of Education and Science(176020) ; Serbian Ministry of Education and Science(176020) ; Serbian Ministry of Education and Science(176020) ; Serbian Ministry of Education and Science(176020) ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; CAS ; CAS ; CAS ; CAS ; 41690114 ; 41690114 ; 41690114 ; 41690114 ; 41625010) ; 41625010) ; 41625010) ; 41625010) ; National Natural Science Foundation of China(41430531 ; National Natural Science Foundation of China(41430531 ; National Natural Science Foundation of China(41430531 ; National Natural Science Foundation of China(41430531 ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; Serbian Ministry of Education and Science(176020) ; Serbian Ministry of Education and Science(176020) ; Serbian Ministry of Education and Science(176020) ; Serbian Ministry of Education and Science(176020) ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; CAS ; CAS ; CAS ; CAS ; 41690114 ; 41690114 ; 41690114 ; 41690114 ; 41625010) ; 41625010) ; 41625010) ; 41625010) ; National Natural Science Foundation of China(41430531 ; National Natural Science Foundation of China(41430531 ; National Natural Science Foundation of China(41430531 ; National Natural Science Foundation of China(41430531 ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; Serbian Ministry of Education and Science(176020) ; Serbian Ministry of Education and Science(176020) ; Serbian Ministry of Education and Science(176020) ; Serbian Ministry of Education and Science(176020) ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; CAS ; CAS ; CAS ; CAS ; 41690114 ; 41690114 ; 41690114 ; 41690114 ; 41625010) ; 41625010) ; 41625010) ; 41625010) ; National Natural Science Foundation of China(41430531 ; National Natural Science Foundation of China(41430531 ; National Natural Science Foundation of China(41430531 ; National Natural Science Foundation of China(41430531 ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; International Partnership Program of Chinese Academy of Sciences(131C11KYSB20160061) ; Serbian Ministry of Education and Science(176020) ; Serbian Ministry of Education and Science(176020) ; Serbian Ministry of Education and Science(176020) ; Serbian Ministry of Education and Science(176020) ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; grant "Development of novel methods for better understanding of loess formation and reconstruction of the Pleistocene climate and environmental dynamics" of Inter-Governmental Chinese Serbian bilateral program ; CAS ; CAS ; CAS ; CAS ; 41690114 ; 41690114 ; 41690114 ; 41690114 ; 41625010) ; 41625010) ; 41625010) ; 41625010)
源URL[http://ir.iggcas.ac.cn/handle/132A11/83056]  
专题中国科学院地质与地球物理研究所
通讯作者Guo, Zhengtang
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Res Ctr Ecoenvironm Sci, State Key Lab Urban & Reg Ecol, Beijing 100085, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
5.Univ Novi Sad, Fac Sci, Phys Geog, Trg Dositeja Obradov 3, Novi Sad 21000, Serbia
6.Univ Novi Sad, Fac Sci, Lab Palaeoenvironm Reconstruct, Trg Dositeja Obradov 3, Novi Sad 21000, Serbia
7.Univ Bayreuth, BayCEER, D-95440 Bayreuth, Germany
8.Univ Bayreuth, Chair Geomorphol, D-95440 Bayreuth, Germany
9.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
10.Tsinghua Univ, Dept Phys, Beijing 100084, Peoples R China
推荐引用方式
GB/T 7714		 Song, Yang,Guo, Zhengtang,Markovic, Slobodan,et al. Magnetic stratigraphy of the Danube loess: A composite Titel-Stari Slankamen loess section over the last one million years in Vojvodina, Serbia[J]. JOURNAL OF ASIAN EARTH SCIENCES,2018,155:68-80.
APA Song, Yang.,Guo, Zhengtang.,Markovic, Slobodan.,Hambach, Ulrich.,Deng, Chenglong.,...&Hao, Qingzhen.(2018).Magnetic stratigraphy of the Danube loess: A composite Titel-Stari Slankamen loess section over the last one million years in Vojvodina, Serbia.JOURNAL OF ASIAN EARTH SCIENCES,155,68-80.
MLA Song, Yang,et al."Magnetic stratigraphy of the Danube loess: A composite Titel-Stari Slankamen loess section over the last one million years in Vojvodina, Serbia".JOURNAL OF ASIAN EARTH SCIENCES 155(2018):68-80.

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来源：地质与地球物理研究所

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