Ili Basin, China 80KYr Loess Magnetic Data Song, Y.G.; Shi, Z.T.; Fang, X.M.; Nie, J.S.; Ishikawa, N.; Qiang, X.K.; Wang, X.L. Song, Y.G. Shi, Z.T. Fang, X.M. Nie, J.S. Ishikawa, N. Qiang, X.K. Wang, X.L. Monsoon millennial resolution earth science/paleoclimate/loess (mass magnetic susceptibility,loess,null,cubic meter per kilogram,null,loess,null,null,N,Chaona; High frequency mass magnetic susceptibility; units 10E-7 m3 kg-2) earth science/paleoclimate/loess (mass magnetic susceptibility,loess,null,cubic meter per kilogram,null,loess,null,null,N,Chaona; Absolute frequency mass magnetic susceptibility; units 10E-7 m3 kg-3) earth science/paleoclimate/loess (age,null,null,calendar kiloyear before present,null,loess,null,null,N,Chaona) earth science/paleoclimate/loess (mass magnetic susceptibility,loess,null,percent,null,loess,null,null,N,Zhaosu; percent frequency dependent mass magnetic susceptibility) earth science/paleoclimate/loess (mass magnetic susceptibility,loess,null,cubic meter per kilogram,null,loess,null,null,N,Zhaosu; Absolute frequency mass magnetic susceptibility; units 10E-7 m3 kg-3) earth science/paleoclimate/loess (depth,null,null,meter,null,loess,null,null,N,Chaona) earth science/paleoclimate/loess (mass magnetic susceptibility,loess,null,cubic meter per kilogram,null,loess,null,null,N,Zhaosu; High frequency mass magnetic susceptibility; units 10E-7 m3 kg-2) earth science/paleoclimate/loess (anhysteretic remanent magnetization,loess,null,cubic meter per kilogram,null,loess,null,null,N,Chaona; normalized ARM with units 10^-6) earth science/paleoclimate/loess (mass magnetic susceptibility,loess,null,cubic meter per kilogram,null,loess,null,null,N,Chaona; Low frequency mass magnetic susceptibility; units 10E-7 m3 kg-1) earth science/paleoclimate/loess (age,null,null,calendar kiloyear before present,null,loess,null,null,N,Zhaosu) earth science/paleoclimate/loess (anhysteretic remanent magnetization,loess,null,cubic meter per kilogram,null,loess,null,null,N,Zhaosu; normalized ARM with units 10^-6) earth science/paleoclimate/loess (depth,null,null,meter,null,loess,null,null,N,Zhaosu) earth science/paleoclimate/loess (mass magnetic susceptibility,loess,null,cubic meter per kilogram,null,loess,null,null,N,Zhaosu; Low frequency mass magnetic susceptibility; units 10E-7 m3 kg-1) earth science/paleoclimate/loess (mass magnetic susceptibility,loess,null,percent,null,loess,null,null,N,Chaona; percent frequency dependent mass magnetic susceptibility) earth science/paleoclimate/loess (Chaona section>LATITUDE 35.1>LONGITUDE 107.2) Over the past two decades, magnetoclimatological studies of loess-paleosol sequences in the Chinese Loess Plateau (CLP) have made outstanding achievements, which greatly promote the understanding of East Asian paleomonsoon evolution, inland aridification of Asia, and past global climate changes. Loess magnetic properties of the CLP have been well studied. In contrast, loess magnetic properties from outside the CLP in China have not been fully understood. We have little knowledge about the magnetic properties of loess in the Ili Basin, an intermontane depression of the Tianshan (or Tien Shan) Mountains. Here, we present the results of rock magnetic measurements of the Ili loess including mass magnetic susceptibility (?) and anhysteretic remanent magnetization (ARM), high/low temperature dependence of susceptibility (TDS) and hysteresis, as well as X-ray diffraction (XRD) for mineral analysis. Based on the comparison with loess-paleosol sequences in the CLP (hereafter referred to as the Chinese loess), we discuss the possible magnetic susceptibility enhancement mechanism of the Ili loess. The results show that 1) the total magnetic mineral concentration of the Ili loess is far lower than that of the Chinese loess, though they have similar magnetic mineral compositions. The ferrimagnetic minerals in the Ili loess are magnetite and maghemite, and the antiferromagnetic mineral is hematite; XRD analysis also identifies the presence of ilmenite. The ratio of maghemite is lower in the Ili loess than in the Chinese loess, but the ratios of magnetite and hematite are higher in the Ili loess than in the Chinese loess. 2) The granularity of magnetic minerals in the Ili loess, dominated by pseudo-single domain (PSD) and multi-domain (MD) grains, is generally much coarser than that of the Chinese loess. Ultrafine pedogenically-produced magnetic grains have a very limited contribution to the susceptibility enhancement. Rather, PSD and MD particles of magnetite and maghemite are the main contributors to the enhancement of susceptibility in the Ili loess. 3) The susceptibility enhancement mechanism for the Ili loess is complicated and superimposes both a wind velocity/vigor model (Alaskan or Siberian model) and the in situ ultrafine grain pedogenic model; the former might play an important role in the Ili loess. 4) Magnetic susceptibility enhancements of the Ili loess are related not only to the eolian input of the source area, but also to the local climate, landform, and geological background. Therefore, great care should be taken when reconstructing paleoclimate using magnetic susceptibility data from the Ili loess. STUDY NOTES: Magnetic susceptibility data of two loess-paleosol sequences since the last interglaciation, from Central Asia and the Chinese Loess Plateau. One section from Zhaosu, Ili Basin, is located in western Zhaosu county near the boundary between China and Kazakhstan. The Zhaosu loess section (ZSP) is 6.9m thick from the top to the upper part the first paleosol (S1), and the bottom consists of fluvial gravel sediments. According to IRSL (infrared stimulated luminescence) dating of this section, the bottom is 80,000 years old. The other loess section is located at the central Chinese Loess Plateau, named Chaona section (CN). The Chaona section is about 10.4m in thickness with a 141ka tuning age. NCDC-Paleoclimatology https://www.ncdc.noaa.gov/data-access/paleoclimatology-data - Bauer Bruce Investigator : Song, Y.G. Investigator : Shi, Z.T. Investigator : Fang, X.M. Investigator : Nie, J.S. Investigator : Ishikawa, N. Investigator : Qiang, X.K. Investigator : Wang, X.L. 2010-10-27 ONLINE Files online, ASCII https://www.ncdc.noaa.gov/paleo/study/9702 https://www1.ncdc.noaa.gov/pub/data/paleo/loess/china/song2010ili.xls https://www1.ncdc.noaa.gov/pub/data/paleo/loess/china/song2010ili.txt https://www1.ncdc.noaa.gov/pub/data/paleo/loess/china/song2010ili.xls https://www1.ncdc.noaa.gov/pub/data/paleo/loess/china/song2010ili.txt English https://www.ncdc.noaa.gov/paleo/study/9702 https://www1.ncdc.noaa.gov/pub/data/paleo/loess/china/song2010ili.xls https://www1.ncdc.noaa.gov/pub/data/paleo/loess/china/song2010ili.txt Song, Y.G., Z.T. Shi, X.M. Fang, J.S. Nie, N. Ishikawa, X.K. Qiang, and X.L. Wang. 2010. Loess magnetic properties in the Ili Basin and their correlation with the Chinese Loess Plateau. China Science: Earth Sciences, Vol. 53(3), pp. 419-431. DOI: 10.1007/s11430-010-0011-5 START YEAR: 141250 cal yr BP * END YEAR: 0 cal yr BP 107.2 35.1 107.2 35.1