Misleading positions of geomagnetic reversal boundaries in Eurasian loess and implications for correlation between continental and marine sedimentary sequences
Zhou, LP; Shackleton, NJ
刊名EARTH AND PLANETARY SCIENCE LETTERS
1999-04-30
卷号168期号:1-2页码:117-130
关键词Brunhes epoch Matuyama epoch Gauss epoch loess deep-sea sedimentation reversals microtektites palaeomagnetism Quaternary geochronology
ISSN号0012-821X
文献子类Article
英文摘要The Matuyama-Brunhes boundary (MBB) where the Earth's magnetic field changed to its present orientation is one of the most frequently used time markers in continental Quaternary stratigraphy. Although magnetic signals have been successfully recovered from loess deposits and an apparently coherent magnetostratigraphy seems to be in place, a close examination of the published loess records from northern mid-latitudes reveals significant uncertainty and variability for the position of the MBB. In Asia and part of Central Europe, the MBB has been found in loess, a glacial deposit. This is in contrast to the well-established palaeomagnetic records in deep-sea sediments where the MBB is located in the interglacial Oxygen Isotope Stage 19. This discrepancy has caused serious confusion in stratigraphic correlation between loess and marine sequences. Here we examine the causes of the discrepancy between the two sedimentary environments in their records of the MBB. Our approach includes a comparison of the MBB in loess and other continental records, and an evaluation of the stratigraphic significance of the microtektites found around the MBB. Based on the occurrence of the MBB in an interglacial stage in lake and continental margin sequences and the correlative stratigraphic positions of the microtektites in marine sediments and loess, we demonstrate that the measured positions of the MBB in loess are erroneous and misleading, and its true occurrence was during the time of formation of the palaeosol corresponding to Oxygen Isotope Stage 19. The most plausible cause for the apparent offset, i.e. the MBB being found in the underlying loess instead, is that the acquisition of remanent magnetisation in loess occurs at a certain depth substantially below the land surface. The degree of such displacement is dependent on the lithology and structure of the deposits formed prior to the reversal, and the time delay is estimated to be in the order of 10(3)-10(4) years. We show that other geomagnetic boundaries, such as those of Jaramillo and Cobb Mountain, in loess have been similarly displaced though to a varying extent. We suggest that the remanence acquisition in loess is closely related to the post-depositional evolution in the structure of loessic materials which is in part influenced by regional climate conditions. Our conclusions on the displaced remanence acquisition have implications for loess chronology, magnetostratigraphy as well as the geomagnetic interpretation of detailed magnetic signatures from loess. (C) 1999 Elsevier Science B.V. All rights reserved.
WOS关键词CHINESE LOESS ; ASTRONOMICAL CALIBRATION ; REMANENCE ACQUISITION ; MATUYAMA-BRUNHES ; TIME-SCALE ; DEPOSITS ; CLIMATE ; MAGNETISM ; RECORD ; EVENT
WOS研究方向Geochemistry & Geophysics
语种英语
出版者ELSEVIER SCIENCE BV
WOS记录号WOS:000079864900009
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/75324]  
专题中国科学院地质与地球物理研究所
通讯作者Zhou, LP
作者单位1.Univ Cambridge, Dept Earth Sci, Godwin Lab, Cambridge CB2 3SA, England
2.Chinese Acad Sci, Inst Geol, Beijing 100029, Peoples R China
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GB/T 7714
Zhou, LP,Shackleton, NJ. Misleading positions of geomagnetic reversal boundaries in Eurasian loess and implications for correlation between continental and marine sedimentary sequences[J]. EARTH AND PLANETARY SCIENCE LETTERS,1999,168(1-2):117-130.
APA Zhou, LP,&Shackleton, NJ.(1999).Misleading positions of geomagnetic reversal boundaries in Eurasian loess and implications for correlation between continental and marine sedimentary sequences.EARTH AND PLANETARY SCIENCE LETTERS,168(1-2),117-130.
MLA Zhou, LP,et al."Misleading positions of geomagnetic reversal boundaries in Eurasian loess and implications for correlation between continental and marine sedimentary sequences".EARTH AND PLANETARY SCIENCE LETTERS 168.1-2(1999):117-130.
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