Remanence acquisition efficiency in biogenic and detrital magnetite and   recording of geomagnetic paleointensity

doi:10.1002/2016GC006753

CORC > 北京大学 > 地球与空间科学学院

	Remanence acquisition efficiency in biogenic and detrital magnetite and recording of geomagnetic paleointensity
	Chen, Liang ; Heslop, David ; Roberts, Andrew P. ; Chang, Liao ; Zhao, Xiang ; McGregor, Helen V. ; Marino, Gianluca ; Rodriguez-Sanz, Laura ; Rohling, Eelco J. ; Paelike, Heiko
刊名	GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
	2017
关键词	EQUATORIAL PACIFIC RELATIVE PALEOINTENSITY MAGNETOTACTIC BACTERIA MAGNETOSOME CHAINS VERWEY TRANSITION MARINE CARBONATES LOESS SEQUENCES SOUTH ATLANTIC MATUYAMA CHRON SEDIMENTS
DOI	10.1002/2016GC006753
英文摘要	Relative paleointensity (RPI) variations of Earth's magnetic field are widely used to understand geomagnetic field behavior and to develop age models for sedimentary sequences. RPI estimation is based on a series of assumptions. One key assumption that is rarely considered is that all magnetic particles in the sediment acquired a magnetization in an identical manner. In this paper, we test this assumption for sediments from the eastern equatorial Pacific Ocean that record well-documented global RPI variations over the last similar to 780 kyr. The magnetization is carried by two stable single domain magnetic components, which we identify as magnetite magnetofossils and titanomagnetite nanoparticle inclusions within larger silicate particles. By analyzing signals carried by the two components separately, we determine for the first time that magnetic nanoparticle inclusions can cause their host particles to record reliable but inefficient sedimentary paleomagnetic signals. The magnetization carried by biogenic magnetite is acquired more efficiently than that carried by the nanoparticle inclusions. Variations in the concentration of both components are modulated climatically so that they record nearly identical RPI signals. In many sediment types, there is no correlation between the concentrations of different magnetic components so that variable remanence acquisition efficiency will complicate RPI recording. Our work demonstrates that detailed assessment of paleomagnetic recording by each constituent magnetic component needs to become a routine part of sedimentary RPI analysis.; China Scholarship Council; Australian Research Council (ARC) [DP120103952, DP140104544, LE120100218]; ARC Future Fellowship [FT140100286]; ARC Australian Laureate Fellowship [FL120100050]; European Research Council [617462]; NSF [OCE-1558679]; SCI(E); ARTICLE; 4; 1435-1450; 18
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/474150]
专题	地球与空间科学学院
推荐引用方式 GB/T 7714	Chen, Liang,Heslop, David,Roberts, Andrew P.,et al. Remanence acquisition efficiency in biogenic and detrital magnetite and recording of geomagnetic paleointensity[J]. GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,2017.
APA	Chen, Liang.,Heslop, David.,Roberts, Andrew P..,Chang, Liao.,Zhao, Xiang.,...&Paelike, Heiko.(2017).Remanence acquisition efficiency in biogenic and detrital magnetite and recording of geomagnetic paleointensity.GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS.
MLA	Chen, Liang,et al."Remanence acquisition efficiency in biogenic and detrital magnetite and recording of geomagnetic paleointensity".GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS (2017).