Abstract
The magnetic susceptibility (MS) of Chinese loess showing a general proportional relationship to pedogenic grade has been widely recognized and used for reconstruction of paleoclimate by Quaternary scientists. The in-situ pedogenic enhancement of ferrimagnetic content is normally believed to be the main reason for the increase of susceptibility in soil units. However, this pattern of high magnetic susceptibility in palaeosols, and low values in loess, are not replicated in some loess deposits. Siberian loess deposits display a completely opposite susceptibility behavior: high values in loess and low values in palaeosols. This inverse relationship has been explained by the idea that magnetic susceptibility is reflecting the magnitude of an aeolian ferrimagnetic component of consistent mineralogy, the grain size of which is related to average wind velocity. Our magnetic study of Siberian samples in this paper suggests that there are notable differences in magnetic properties between Siberian loess and developed palaeosols, not only in magnetic grain-size and concentration but also in magnetic mineralogy. This evidence is difficult to explain fully through variation in wind strength alone, but implies that the low magnetic susceptibility values in the Siberian paleosol units are a reflection, at least in part, of the alteration of the ferrimagnetic content by post-depositional processes. The Loess Plateau is a very arid area where potential evaporation is always higher than precipitation; pedogenesis occurs under dry oxidising conditions. The Siberian Kurtak region is located on the edge of the tundra where it is always wet and saturation during interglacials will lead to a reducing pedogenic environment. Ferrimagnetic minerals under this condition will be destroyed, resulting in lower magnetic susceptibility. Therefore, great care should be taken when using susceptibility values for paleoclimatic reconstruction.
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References
Heller F, Liu T S. Magnetostratigraphical dating of loess deposits in China. Nature, 1982, 300: 431–433
Hovan S A, Rea D K, Pisias NG, et al. A direct link between the loess and marine 18O records: eolian flux to the north Pacific. Nature, 1989, 340: 296–298
Petit J R, Mounier L, Jouzel J, et al. Paleoclimatological and chronological implications of the Vostok core dust record. Nature, 1990, 343: 56–58
Heller F, Chen C D, Beer J, et al. Quantitative estimates of pedogenic ferromagnetic mineral formation in Chinese loess and palaeoclimatic implications. Earth Planet Sci Lett, 1993, 114: 385–390
Maher B A, Thompson R, Zhou L P. Spatial and temporal reconstructions of changes in the Asian palaeomonsoon—A new mineral magnetic approach. Earth Planet Sci Lett, 1990, 125: 461–471
Liu X M, Rolph T, Bloemendal J, et al. Quantitative estimates of paleoprecipitation at Xifeng in the loess plateau of China. Palaeogeogr Palaeoclimatol Palaeoecol, 1995, 113: 243–248
Han J M, Lü H Y, Wu N Q, et al. Magnetic susceptibility of modern soils in China and climate conditions. Stud Geophys Geodetica, 1996, 40: 262–275
Hao Q Z, Guo Z T. Spatial variations of magnetic susceptibility of Chinese loess for the last 600 ka: Implications for monsoon evolution. J Geophy Res, 2005, 110: B12101
Evans M E, Heller F. Magnetism of loess palaeosol sequences: recent developments. Earth-Science Rev, 2001, 54: 129–144
Kukla J G, An Z S. Loess stratigraphy in central China. Palaeogeogr Palaeoclimatol Palaeoecol, 1989, 72: 203–225
Heller F, Liu T S. Magnetism of Chinese loess deposits. Geophys J R astr Soc, 1984, 77: 125–141
Zhou L P, Oldfield F, Wintle A G, et al. Partly pedogenic origin of magnetic variations in Chinese loess. Nature, 1990, 346: 737–739
Liu X M., Liu T S., Heller F. Xu T C, Frequency-dependent susceptibility of loess and Quaternary paleoclimate. Quat Sci, 1990, 1: 41–50
Liu X M, Shaw J, Liu T S, et al. Magnetic mineralogy of Chinese loess and its significance. Geophys J Inter, 1992, 108: 301–308
Maher B A, Thompson R. Paleoclimatic significance of the mineral magnetic record of the Chinese loess and paleosols. Quat Res, 1992, 37: 155–170
Chlachula J, Evans M E, Rutter N W. A magnetic investigation of a late Quaternary loess/palaeosol record in Siberia. Geophys J Int, 1998, 132: 128–132
Chlachula J. The Siberian loess record and its significance for reconstruction of Pleistocene climate change in north-central Asia. Quat Sci Rev, 2003, 22: 1879–1906
Matasova G, Petrovsky E, Jordanova N, et al. Magnetic study of Late Pleistocene loess/palaeosol sections from Siberia: palaeoenvironmental implications. Geophys J Int, 2001, 147: 367–380
Zhu R X, Kazansky A, Matasova G, et al. Rock-magnetic investigation of Siberia loess and its implication. Chin Sci Bull, 2000, 45: 2192–2198
Zhu R X, Matasova G, Kazansky A, et al. Rock magnetic record of the last glacial-interglacial cycle from the Kurtak loess section, southern Siberia. Geophys J Int, 2003, 152: 335–343
Begét J, Hawkins D. Influence of orbital parameters on Pleistocene loess deposition in central Alaska. Nature, 1989, 337: 151–153
Begét J, Stone D, Hawkins D. Paleoclimate forcing of magnetic susceptibility variations in Alaskan loess. Geology, 1990, 18: 40–43
Liu X M, Hesse P, Rolph T, et al. Properties of magnetic mineralogy of Alaskan loess: evidence for pedogenesis. Quat Int, 1999, 62: 92–102
Liu X M, Hesse P, Begét J, et al. Pedogenic destruction of ferrimagnetics in Alaskan loess deposits. Australian J Soil Res, 2001, 39: 99–115
Liu X M, Hesse P, Rolph T. Origin of maghaemite in Chinese loess deposits: aeolian or pedogenic? Phys Earth Planet Int, 1999, 112: 191–201
Rowan C J, Roberts A P. Magnetite dissolution, diachronous greigite formation, and secondary magnetization from pyrite oxidation: Unravelling complex magnetizations in Neogene marine sediments from New Zealand. Earth Planet Sci Lett, 2006, 241: 119–137
Emiroglu S, Rey D, Peterson N. Magnetic properties of sediment in the Ria de Arousa (Spain): dissolution of iron oxides and formation of iron sulphides. Physics Chem Earth, 2004, 29: 947–959
Hu S, Appel E, Hoffmann V, et al. Gyromagnetic remanence acquired by greigite (Fe3S4) during static three-axis alternating field demagnetization. Geophys J Int, 1998, 152: 831–842
Geiss C E, Banerjee S K. A multi-parameter rock magnetic record of the last glacial-interglacial paleoclimate from south-central Illinois, USA. Earth Planet Sci Lett, 1997, 152: 203–216
Bina M, Daly L. Mineralogical change and self-reversed magnetizations in pyrrhotite resulting from partial oxidation; geophysical implications. Phys Earth Planet Int, 1994, 85: 83–99
Zhu R X, Shi C D, Suchy V, et al. The magnetic properties of Czech loess and its paleoclimatic significances. Sci China Ser D-Earth Sci, 2001, 31(2): 146–154.
Shi C D, Zhu R X, Suchy V, et al. Identification and origins of sulfides in Czech loess. Geophysical Res Lett, 2001, 28(20): 3903–3906
Lagroix F, Banerjee S K. Paleowind directions from the magnetic fabric of loess pro¢les in central Alaska. Earth Planet Sci Lett, 2002, 195: 99–112
Yang S L, Ding Z L. Winter-spring precipitation as the principal control on predominance of C3 plants in Central Asia over the past 1.77 Ma: Evidence from δ 13C of loess organic matter in Tajikistan. Palaeogeogr Palaeoclimatol Palaeoecol, 2003, 235: 330–339
Vlag P. The magnetic signal in loess-sequences in Alaska. The Institute for Rock Magnetism Quarterly. 1998, 8: 1–7
Rosenbaum J G, Reynolds R L, Muhs D R, et al. Geochemical constraint on the interpretation of magnetic property variations in loess/paleosol sequences from central Alaska. EOS, Transactions, AGU Fall Meeting, 1997, 78: F170–F171
Sun J M, Liu T S. Multiple origins and interpretations of the magnetic susceptibility signal in Chinese wind-blown sediments. Earth Planet Sci Lett, 2000, 180: 287–296
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Supported by the National Natural Science Foundation of China (Grant Nos. 40421101 and 40772109) and Macquarie University, Australia
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Liu, X., Liu, T., Paul, H. et al. Two pedogenic models for paleoclimatic records of magnetic susceptibility from Chinese and Siberian loess. Sci. China Ser. D-Earth Sci. 51, 284–293 (2008). https://doi.org/10.1007/s11430-007-0145-2
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DOI: https://doi.org/10.1007/s11430-007-0145-2