中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The Jaramillo subchron in Chinese loess-paleosol sequences

文献类型:期刊论文

作者Pan, Qing1; Xiao, Guoqiao1,2,3; Zhao, Qingyu2; Chen, Ruisheng1; Ao, Hong3; Shen, Yanfei1; Cheng, Junyao1; Zhu, Zongmin2
刊名PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
出版日期2021-06-15
卷号572页码:19
ISSN号0031-0182
关键词Chinese Loess Plateau Magnetostratigraphy Rock magnetism Relative paleointensity Remagnetization Matuyama-Brunhes boundary
DOI10.1016/j.palaeo.2021.110423
通讯作者Xiao, Guoqiao(xgqiaocug@gmail.com)
英文摘要The Chinese loess is one of the most important terrestrial records of the Quaternary climate changes. However, the positional discrepancy of geomagnetic polarity boundaries, such as Matuyama-Brunhes boundary (MBB), between Chinese loess and marine sediments remains controversial, hampering to establish an accurate chronological framework for the Chinese loess and its correlation with marine oxygen isotope records. The Jaramillo subchron within the Matuyama Chron is an important paleomagnetic age constraint for Quaternary magnetostratigraphic dating. Here, we present a high-resolution magnetostratigraphic, rock magnetism, and relative paleointensity (RPI) study of the stratigraphic interval between paleosols S9 and S18 in two parallel loess sections from the southeastern Chinese Loess Plateau, with an aim to explore the positions of the upper and lower boundaries of the Jaramillo in the Chinese loess. The results show that significant uncertainty and variability (more than one loess-paleosol cycle) for the positions of the measured upper and lower Jaramillo boundaries among different loess sections cannot be explained by the discrepancy of loess stratigraphy, sedimentation rate or regional climate. The measured upper and lower Jaramillo boundaries in the loess can be above or below their true positions, which cannot be explained by the lock-in effect. As the measured boundaries in the loess are mostly within the intervals of low-intensity geomagnetic field, we propose that the loess deposits may have acquired unstable primary remanent magnetization during the intervals of geomagnetic reversals or excursions with low-intensity geomagnetic field, and these deposits could be easily overprinted (remagnetizated) by the ensuing high-intensity field. This hypothesis is able to explain the phenomena that the measured MBB in the Eurasian loess is downward shifted by tens centimeters to several meters relative to the true boundary, and it can also explain the anomalistic polarity zones recorded in some loess sections.
WOS关键词BRUNHES GEOMAGNETIC REVERSAL ; LOCK-IN ; LOESS/PALAEOSOL SEQUENCE ; MAGNETIC-SUSCEPTIBILITY ; ASTRONOMICAL TIMESCALE ; POLARITY REVERSAL ; QUATERNARY LOESS ; MATUYAMA CHRON ; LATE MIOCENE ; MARINE
资助项目National Science Foundation of China[41830319] ; National Science Foundation of China[41888101] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB26000000]
WOS研究方向Physical Geography ; Geology ; Paleontology
语种英语
出版者ELSEVIER
WOS记录号WOS:000648525800020
资助机构National Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences
源URL[http://ir.ieecas.cn/handle/361006/16678]  
专题地球环境研究所_古环境研究室
通讯作者Xiao, Guoqiao
作者单位1.China Univ Geosci, Sch Geog & Informat Engn, Hubei Key Lab Crit Zone Evolut, Wuhan 430074, Peoples R China
2.China Univ Geosci, Sch Earth Sci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China
3.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China
推荐引用方式
GB/T 7714
Pan, Qing,Xiao, Guoqiao,Zhao, Qingyu,et al. The Jaramillo subchron in Chinese loess-paleosol sequences[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2021,572:19.
APA Pan, Qing.,Xiao, Guoqiao.,Zhao, Qingyu.,Chen, Ruisheng.,Ao, Hong.,...&Zhu, Zongmin.(2021).The Jaramillo subchron in Chinese loess-paleosol sequences.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,572,19.
MLA Pan, Qing,et al."The Jaramillo subchron in Chinese loess-paleosol sequences".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 572(2021):19.

入库方式: OAI收割

来源:地球环境研究所

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