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Paleowind directions from the magnetic fabric of loess deposits in the western Chinese Loess Plateau and implications for dust provenance

Published online by Cambridge University Press:  01 April 2021

Xinbo Gao ,
Qingzhen Hao ,
Junyi Ge ,
Long Han ,
Yu Fu ,
Xuechao Wu ,
Chenglong Deng ,
Slobodan B. Marković  and
Zhengtang Guo
Xinbo Gao
Affiliation:
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, No. 19 Beitucheng Western Road, Beijing, 100029, China
Qingzhen Hao*
Affiliation:
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, No. 19 Beitucheng Western Road, Beijing, 100029, China CAS Center for Excellence in Life and Paleoenvironment, Beijing, 100044, China University of Chinese Academy of Sciences, No.19(A) Yuquan Road, Beijing, 100049, China
Junyi Ge
Affiliation:
CAS Center for Excellence in Life and Paleoenvironment, Beijing, 100044, China University of Chinese Academy of Sciences, No.19(A) Yuquan Road, Beijing, 100049, China Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, P.O. Box 643, Beijing, 100044, China
Long Han
Affiliation:
School of Environmental Science and Engineering, Southern University of Science and Technology, 1088 Xueyuan Road, Shenzhen, 518055, China
Yu Fu
Affiliation:
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, No. 19 Beitucheng Western Road, Beijing, 100029, China University of Chinese Academy of Sciences, No.19(A) Yuquan Road, Beijing, 100049, China
Xuechao Wu
Affiliation:
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, No. 19 Beitucheng Western Road, Beijing, 100029, China University of Chinese Academy of Sciences, No.19(A) Yuquan Road, Beijing, 100049, China
Chenglong Deng
Affiliation:
University of Chinese Academy of Sciences, No.19(A) Yuquan Road, Beijing, 100049, China State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, No. 19 Beitucheng Western Road, Beijing, 100029, China
Slobodan B. Marković
Affiliation:
Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, Novi Sad, 21000, Serbia Serbian Academy of Sciences and Arts, Knez Mihajlova 35, Belgrade, 11000, Serbia
Zhengtang Guo
Affiliation:
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, No. 19 Beitucheng Western Road, Beijing, 100029, China CAS Center for Excellence in Life and Paleoenvironment, Beijing, 100044, China University of Chinese Academy of Sciences, No.19(A) Yuquan Road, Beijing, 100049, China
*
Corresponding author: Qingzhen Hao, Email: haoqz@mail.iggcas.ac.cn
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Abstract

The aeolian loess-paleosol sequences in the Chinese Loess Plateau (CLP) are an excellent archive of variations in atmospheric circulation in the geological past. However, there is no consensus regarding the roles of the East Asian winter monsoon and westerly winds in transporting the dust responsible for loess deposition during glacial and interstadial periods. We conducted detailed measurements of the anisotropy of magnetic susceptibility (AMS) on two parallel loess profiles covering the most recent 130 ka in the western CLP to determine paleowind directions. Results show that the magnetic lineations of the loess and paleosol units in both sections are significantly clustered along the northwest to southeast direction. These observations demonstrate that the prevailing wind system responsible for dust transport in the western CLP was the northwesterly winter monsoon, rather than the westerly winds. The AMS-derived dust-bearing wind direction was relatively stable during the last glacial and interglacial cycle in the western CLP, consistent with sedimentary and AMS evidence from the eastern CLP. Accordingly, it is reasonable to conclude that large areas of deserts and Gobi deserts areas located in the upwind direction were the dominant sources for the aeolian deposits of the Loess Plateau.

Keywords

Anisotropy of magnetic susceptibility (AMS)LoessPaleowind directionEast Asian winter monsoonChinese Loess Plateau
Type
Thematic Set: Eurasian Climate and Environment
Information
Quaternary Research , Volume 103 , September 2021 , pp. 74 - 87
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Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2021

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References

REFERENCES

Antoine, P., Goval, E., Jamet, G., Coutard, S., Moine, O., Hérisson, D., Auguste, P., et al. , 2014. The Upper Pleistocene loess sequences of Havrincourt (Pas-de-Calais, France): stratigraphy, paleoenvironments, geochronology and human occupations. Quaternaire 25, 321–368. [in French with English abstract]Google Scholar
Arimoto, R., 2001. Eolian dust and climate: relationships to sources, tropospheric chemistry, transport and deposition. Earth-Science Reviews 54, 29–42.CrossRefGoogle Scholar
Banerjee, S.K., Hunt, C.P., Liu, X.M., 1993. Separation of local signals from the regional paleomonsoon record of the Chinese Loess Plateau: a rock-magnetic approach. Geophysical Research Letters 20, 843–846.CrossRefGoogle Scholar
Bird, A., Millar, I., Rodenburg, T., Stevens, T., Rittner, M., Vermeesch, P., Lu, H., 2020. A constant Chinese Loess Plateau dust source since the late Miocene. Quaternary Science Reviews 227, 106042. https://doi.org/10.1016/j.quascirev.2019.106042.CrossRefGoogle Scholar
Boyd, P.W., Watson, A.J., Law, C.S., Abraham, E.R., Trull, T., Murdoch, R., Bakker, D.C.E., et al. , 2000. A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization. Nature 407, 695–702.CrossRefGoogle ScholarPubMed
Bradák, B., Újvári, G., Seto, Y., Hyodo, M., Végh, T., 2018. A conceptual magnetic fabric development model for the Paks loess in Hungary. Aeolian Research 30, 20–31.CrossRefGoogle Scholar
Bullard, J.E., Baddock, M., Bradwell, T., Crusius, J., Darlington, E., Gaiero, D., Gassó, , et al. , 2016. High-latitude dust in the Earth system. Reviews of Geophysics 54, 447–485.CrossRefGoogle Scholar
Che, X., Li, G., 2013. Binary sources of loess on the Chinese Loess Plateau revealed by U–Pb ages of zircon. Quaternary Research 80, 545–551.CrossRefGoogle Scholar
Constable, C., Tauxe, L., 1990. The bootstrap for magnetic susceptibility tensors. Journal of Geophysical Research: Solid Earth 95, 8383–8395.CrossRefGoogle Scholar
Deng, C., Vidic, N.J., Verosub, K.L., Singer, M.J., Liu, Q., Shaw, J., Zhu, R., 2005. Mineral magnetic variation of the Jiaodao Chinese loess/paleosol sequence and its bearing on long-term climatic variability. Journal of Geophysical Research: Solid Earth 110. https://doi.org/10.1029/2004JB003451.CrossRefGoogle Scholar
Deng, C., Zhu, R., Verosub, K.L., Singer, M.J., Yuan, B., 2000. Paleoclimatic significance of the temperature-dependent susceptibility of Holocene loess along a NW–SE transect in the Chinese loess plateau. Geophysical Research Letters 27, 3715–3718.CrossRefGoogle Scholar
Ding, Z.L., Derbyshire, E., Yang, S.L., Yu, Z.W., Xiong, S.F., Liu, T.S., 2002. Stacked 2.6-Ma grain size record from the Chinese loess based on five sections and correlation with the deep-sea δ18O record. Paleoceanography and Paleoclimatology 17, 5-1–5-21.Google Scholar
Ding, Z., Sun, J., Rutter, N.W., Rokosh, D., Liu, T., 1999. Changes in sand content of loess deposits along a North–South transect of the Chinese Loess Plateau and the implications for desert variations. Quaternary Research 52, 56–62.CrossRefGoogle Scholar
Ellwood, B.B., 1984. Bioturbation: minimal effects on the magnetic fabric of some natural and experimental sediments. Earth and Planetary Science Letters 67, 367–376.CrossRefGoogle Scholar
Gao, X., Hao, Q., Oldfield, F., Bloemendal, J., Deng, C., Wang, L., Song, Y., et al. , 2019. New high-temperature dependence of magnetic susceptibility-based climofunction for quantifying paleoprecipitation from Chinese loess. Geochemistry, Geophysics, Geosystems 20, 4273–4291.CrossRefGoogle Scholar
Ge, J., Guo, Z., Zhao, D., Zhang, Y., Wang, T., Yi, L., Deng, C., 2014. Spatial variations in paleowind direction during the last glacial period in north China reconstructed from variations in the anisotropy of magnetic susceptibility of loess deposits. Tectonophysics 629, 353–361.CrossRefGoogle Scholar
Gong, H., Xie, W., Wang, J., Zhang, R., Zhang, Y., Yang, L., 2017. Zircon U-Pb ages of quaternary loess-paleosol sequences from the Luochuan section: implication for sediment provenance. Acta Geologica Sinica 91, 357–358. [English edition]CrossRefGoogle Scholar
Gong, H., Zhang, R., Yue, L., Zhang, Y., Li, J., 2015. Magnetic fabric from Red clay sediments in the Chinese Loess Plateau. Scientific Reports 5, 9706. https://doi.org/10.1038/srep09706.CrossRefGoogle ScholarPubMed
Goudie, A.S., Middleton, N.J., 2006. Desert Dust in the Global System. Springer-Verlag, Berlin. 288 pp.Google Scholar
Graham, J.W., 1954. Magnetic anisotropy, an unexploited petrofabric element. Geological Society of America Bulletin 65, 1257–1258.Google Scholar
Guo, J., Lou, M., Miao, Y., Wang, Y., Zeng, Z., Liu, H., He, J., et al. , 2017. Trans-Pacific transport of dust aerosols from East Asia: insights gained from multiple observations and modeling. Environmental Pollution 230, 1030–1039.CrossRefGoogle ScholarPubMed
Guo, Z.T., Ruddiman, W.F., Hao, Q.Z., Wu, H.B., Qiao, Y.S., Zhu, R.X., Peng, S.Z., Wei, J.J., Yuan, B.Y., Liu, T.S., 2002. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China. Nature 416, 159–163.CrossRefGoogle ScholarPubMed
Guo, Z.T., Sun, B., Zhang, Z.S., Peng, S.Z., Xiao, G.Q., Ge, J.Y., Hao, Q.Z., et al. , 2008. A major reorganization of Asian climate by the early Miocene. Climate of the Past 4, 153–174.CrossRefGoogle Scholar
Hadley, G., 1735. VI. Concerning the cause of the general trade-winds. Philosophical Transactions of the Royal Society of London 39, 58–62.Google Scholar
Hao, Q., Guo, Z., 2007. Magnetostratigraphy of an early-middle Miocene loess-soil sequence in the western Loess Plateau of China. Geophysical Research Letters 34. https://doi.org/10.1029/2007GL031162.CrossRefGoogle Scholar
Hao, Q., Wang, L., Oldfield, F., Peng, S., Qin, L., Song, Y., Xu, B., Qiao, Y., Bloemendal, J., Guo, Z., 2012. Delayed build-up of Arctic ice sheets during 400,000-year minima in insolation variability. Nature 490, 393–396.CrossRefGoogle ScholarPubMed
Harrison, R.J., Feinberg, J.M., 2008. FORCinel: an improved algorithm for calculating first-order reversal curve distributions using locally weighted regression smoothing. Geochemistry, Geophysics, Geosystems 9. https://doi.org/10.1029/2008GC001987.CrossRefGoogle Scholar
Hrouda, F., 1982. Magnetic anisotropy of rocks and its application in geology and geophysics. Geophysical Surveys 5, 37–82.CrossRefGoogle Scholar
Huang, X.G., Sun, J.M., 2005. Study of the magnetic fabrics in Chinese loess-paleosols since the last interglacial: implication of the paleowind direction. Quaternary Sciences 25, 516–522. [in Chinese with English abstract]Google Scholar
Hus, J.J., 2003. The magnetic fabric of some loess/palaeosol deposits. Physics and Chemistry of the Earth, Parts A/B/C 28, 689–699.CrossRefGoogle Scholar
Ising, G., 1943. On the magnetic properties of varved clay: line of investigation: Measurements on a varve series from Viby in southern Sweden, Volume 1. Arkiv för Matematik, Astronomi och Fysik 29A, 37 p.Google Scholar
Jelinek, V., 1981. Characterization of the magnetic fabric of rocks. Tectonophysics 79, T63–T67.CrossRefGoogle Scholar
Kapp, P., Pelletier, J.D., Rohrmann, A., Heermance, R., Russell, J., Ding, L., 2011. Wind erosion in the Qaidam basin, central Asia: implications for tectonics, paleoclimate, and the source of the Loess Plateau. GSA Today 21, 4–10.Google Scholar
Kinne, S., Pueschel, R., 2001. Aerosol radiative forcing for Asian continental outflow. Atmospheric Environment 35, 5019–5028.CrossRefGoogle Scholar
Lagroix, F., Banerjee, S.K., 2002. Paleowind directions from the magnetic fabric of loess profiles in central Alaska. Earth and Planetary Science Letters 195, 99–112.CrossRefGoogle Scholar
Lagroix, F., Banerjee, S.K., 2004a. Cryptic post-depositional reworking in aeolian sediments revealed by the anisotropy of magnetic susceptibility. Earth and Planetary Science Letters 224, 453–459.CrossRefGoogle Scholar
Lagroix, F., Banerjee, S.K., 2004b. The regional and temporal significance of primary aeolian magnetic fabrics preserved in Alaskan loess. Earth and Planetary Science Letters 225, 379–395.CrossRefGoogle Scholar
Licht, A., Pullen, A., Kapp, P., Abell, J., Giesler, N., 2016. Eolian cannibalism: reworked loess and fluvial sediment as the main sources of the Chinese Loess Plateau. Geological Society of America Bulletin 128, 944–956.CrossRefGoogle Scholar
Li, L., Chen, J., Chen, Y., Hedding, D.W., Li, T., Li, L., Liu, X., et al. , 2018. Uranium isotopic constraints on the provenance of dust on the Chinese Loess Plateau. Geology 46, 747–750.CrossRefGoogle Scholar
Lisiecki, L.E., Raymo, M.E., 2005. A Pliocene–Pleistocene stack of 57 globally distributed benthic δ18O records. Paleoceanography 20. https://doi.org/10.1029/2004PA001071.Google Scholar
Liu, Q., Deng, C., Yu, Y., Torrent, J., Jackson, M.J., Banerjee, S.K., Zhu, R., 2005. Temperature dependence of magnetic susceptibility in an argon environment: implications for pedogenesis of Chinese loess/palaeosols. Geophysical Journal International 161, 102–112.CrossRefGoogle Scholar
Liu, T., 1985. Loess and the Environment. China Ocean Press, Beijing. [in Chinese]Google Scholar
Liu, T.S., 1966. Composition and Texture of Loess. Science Press, Beijing. [in Chinese]Google Scholar
Liu, W., Sun, J., 2012. High-resolution anisotropy of magnetic susceptibility record in the central Chinese Loess Plateau and its paleoenvironment implications. Science China Earth Sciences 55, 488–494.CrossRefGoogle Scholar
Lowrie, W., 1989. Magnetic analysis of rock fabric. In: James, D.E. (Ed.), Encyclopedia of Earth Sciences Series: Encyclopedia of Solid Earth Geophysics, Springer, Boston. pp. 698–706.Google Scholar
Lu, H., Sun, D., 2000. Pathways of dust input to the Chinese Loess Plateau during the last glacial and interglacial periods. Catena 40, 251–261.CrossRefGoogle Scholar
Lu, H., Wang, X., Li, L., 2010. Aeolian sediment evidence that global cooling has driven late Cenozoic stepwise aridification in central Asia. Geological Society of London Special Publications 342, 29–44.Google Scholar
Maher, B.A., Thompson, R., 1991. Mineral magnetic record of the Chinese loess and paleosols. Geology 19, 3–6.2.3.CO;2>CrossRefGoogle Scholar
Manabe, S., 1969. Climate and the ocean circulation I: the atmospheric circulation and the hydrology of the Earth's surface. Monthly Weather Review 97, 739 –774.2.3.CO;2>CrossRefGoogle Scholar
Martin, J.H., Coale, K.H., Johnson, K.S., Fitzwater, S.E., Gordon, R.M., Tanner, S.J., Hunter, C.N., et al. , 1994. Testing the iron hypothesis in ecosystems of the equatorial Pacific Ocean. Nature 371, 123–129.CrossRefGoogle Scholar
Matasova, G., Petrovský, E., Jordanova, N., Zykina, V., Kapička, A., 2001. Magnetic study of Late Pleistocene loess/palaeosol sections from Siberia: palaeoenvironmental implications. Geophysical Journal International 147, 367–380.CrossRefGoogle Scholar
Mathé, P.E., Rochette, P., Colin, F., 1997. The origin of magnetic susceptibility and its anisotropy in some weathered profiles. Physics and Chemistry of the Earth 22, 183–187.CrossRefGoogle Scholar
Muxworthy, A.R., Dunlop, D.J., 2002. First-order reversal curve (FORC) diagrams for pseudo-single-domain magnetites at high temperature. Earth and Planetary Science Letters 203, 369–382.CrossRefGoogle Scholar
Nawrocki, J., Gozhik, P., Łanczont, M., Pańczyk, M., Komar, M., Bogucki, A., Williams, I., Czupyt, , Z., 2018. Palaeowind directions and sources of detrital material archived in the Roxolany loess section (southern Ukraine). Palaeogeography, Palaeoclimatology, Palaeoecology 496, 121–135.CrossRefGoogle Scholar
Nawrocki, J., Polechońska, O., Boguckij, A., Łanczont, M., 2006. Palaeowind directions recorded in the youngest loess in Poland and western Ukraine as derived from anisotropy of magnetic susceptibility measurements. Boreas 35, 266−271.CrossRefGoogle Scholar
Nie, J., Pullen, A., Garzione, C.N., Peng, W., Wang, Z., 2018. Pre-Quaternary decoupling between Asian aridification and high dust accumulation rates. Science Advances 4. https://doi.org/10.1126/sciadv.aao6977.CrossRefGoogle ScholarPubMed
Nie, J., Ren, X., Saylor, J.E., Su, Q., Horton, B.K., Bush, M.A., Chen, W., Pfaff, K., 2019 (2020). Magnetic polarity stratigraphy, provenance, and paleoclimate analysis of Cenozoic strata in the Qaidam Basin, NE Tibetan Plateau. Geological Society of America Bulletin 132, 310–320.CrossRefGoogle Scholar
Nie, J., Stevens, T., Rittner, M., Stockli, D., Garzanti, E., Limonta, M., Bird, A., et al. , 2015. Loess plateau storage of Northeastern Tibetan Plateau-derived Yellow River sediment. Nature Communications 6, 8511. https://doi.org/10.1038/ncomms9511.CrossRefGoogle ScholarPubMed
Owens, W.H., Bamford, D., 1976. A discussion on natural strain and geological structure—magnetic, seismic, and other anisotropic properties of rock fabrics. Philosophical Transactions of the Royal Society of London Series A: Mathematical and Physical Sciences 283, 55–68.Google Scholar
Özdemir, Ö., Dunlop, D.J., Moskowitz, B.M., 1993. The effect of oxidation on the Verwey transition in magnetite. Geophysical Research Letters 20, 1671–1674.CrossRefGoogle Scholar
Peng, S., Ge, J., Li, C., Liu, Z., Qi, L., Tan, Y., Cheng, Y., Deng, C., Qiao, Y., 2015. Pronounced changes in atmospheric circulation and dust source area during the mid-Pleistocene as indicated by the Caotan loess-soil sequence in North China. Quaternary International 372, 97–107.CrossRefGoogle Scholar
Pike, C.R., Roberts, A.P., Dekkers, M.J., Verosub, K.L., 2001. An investigation of multi-domain hysteresis mechanisms using FORC diagrams. Physics of the Earth and Planetary Interiors 126, 11–25.CrossRefGoogle Scholar
Pullen, A., Kapp, P., McCallister, A.T., Chang, H., Gehrels, G.E., Garzione, C.N., Heermance, R.V., Ding, L., 2011. Qaidam Basin and northern Tibetan Plateau as dust sources for the Chinese Loess Plateau and paleoclimatic implications. Geology 39, 1031–1034.CrossRefGoogle Scholar
Pye, K., Tsoar, H., 1987. The mechanics and geological implications of dust transport and deposition in deserts with particular reference to loess formation and dune sand diagenesis in the northern Negev, Israel. Geological Society of London Special Publications 35, 139–156.CrossRefGoogle Scholar
Pye, K., Zhou, L.P., 1989. Late Pleistocene and Holocene aeolian dust deposition in north China and the northwest Pacific Ocean. Palaeogeography, Palaeoclimatology, Palaeoecology 73, 11–23.CrossRefGoogle Scholar
Ridgwell, A.J., 2002. Dust in the Earth system: the biogeochemical linking of land, air and sea. Philosophical Transactions of the Royal Society of London Series A: Mathematical, Physical and Engineering Sciences 360, 2905–2924.CrossRefGoogle Scholar
Roberts, A.P., Heslop, D., Zhao, X., Pike, C.R., 2014. Understanding fine magnetic particle systems through use of first-order reversal curve diagrams. Reviews of Geophysics 52, 557–602.CrossRefGoogle Scholar
Roberts, A.P., Pike, C.R., Verosub, K.L., 2000. First-order reversal curve diagrams: a new tool for characterizing the magnetic properties of natural samples. Journal of Geophysical Research: Solid Earth 105, 28461–28475.CrossRefGoogle Scholar
Rochette, P., Fillion, G., Mattéi, J.L., Dekkers, M.J., 1990. Magnetic transition at 30–34 Kelvin in pyrrhotite: insight into a widespread occurrence of this mineral in rocks. Earth and Planetary Science Letters 98, 319–328.CrossRefGoogle Scholar
Rochette, P., Jackson, M., Aubourg, C., 1992. Rock magnetism and the interpretation of anisotropy of magnetic susceptibility. Reviews of Geophysics 30, 209–226.CrossRefGoogle Scholar
Rohrmann, A., Heermance, R., Kapp, P., Cai, F., 2013. Wind as the primary driver of erosion in the Qaidam Basin, China. Earth and Planetary Science Letters 374, 1–10.CrossRefGoogle Scholar
Smirnov, A.V., 2006. Low-temperature magnetic properties of magnetite using first-order reversal curve analysis: implications for the pseudo-single-domain state. Geochemistry, Geophysics, Geosystems 7. https://doi.org/10.1029/2006GC001397.CrossRefGoogle Scholar
Sokolik, I.N., Winker, D.M., Bergametti, G., Gillette, D.A., Carmichael, G., Kaufman, Y.J., Gomes, L., Schuetz, L., Penner, J.E., 2001. Introduction to special section: Outstanding problems in quantifying the radiative impacts of mineral dust. Journal of Geophysical Research: Atmospheres 106, 18015–18027.CrossRefGoogle Scholar
Sun, J., 2002. Provenance of loess material and formation of loess deposits on the Chinese Loess Plateau. Earth and Planetary Science Letters 203, 845–859.CrossRefGoogle Scholar
Sun, J., Huang, X., 2006. Half-precessional cycles recorded in Chinese loess: response to low-latitude insolation forcing during the Last Interglaciation. Quaternary Science Reviews 25, 1065–1072.CrossRefGoogle Scholar
Sun, J.M., Ding, Z.L., Liu, T.S., 1995. Primary application of magnetic susceptibility measurement of loess and paleosols for reconstruction of winter monsoon direction. Chinese Science Bulletin 40, 1976–1978. [in Chinese]Google Scholar
Sun, Y., Clemens, S.C., Morrill, C., Lin, X., Wang, X., An, Z., 2012. Influence of Atlantic meridional overturning circulation on the East Asian winter monsoon. Nature Geoscience 5, 46–49.CrossRefGoogle Scholar
Sun, Y., Yan, Y., Nie, J., Li, G., Shi, Z., Qiang, X., Chang, H., An, Z., 2020. Source-to-sink fluctuations of Asian aeolian deposits since the late Oligocene. Earth-Science Reviews 200. https://doi.org/10.1016/j.earscirev.2019.102963.Google Scholar
Tarling, D., Hrouda, F. (Eds.), 1993. Magnetic Anisotropy of Rocks. Chapman and Hall, London. 218 pp.Google Scholar
Taylor, S.N., Lagroix, F., 2015. Magnetic anisotropy reveals the depositional and postdepositional history of a loess-paleosol sequence at Nussloch (Germany). Journal of Geophysical Research: Solid Earth 120, 2859–2876.Google Scholar
Thistlewood, L., Sun, J., 1991. A palaeomagnetic and mineral magnetic study of the loess sequence at Liujiapo, Xian, China. Journal of Quaternary Science 6, 13–26.Google Scholar
Tsoar, H., Pye, K., 1987. Dust transport and the question of desert loess formation. Sedimentology 34, 139–153.CrossRefGoogle Scholar
Verosub, K.L., Fine, P., Singer, M.J., TenPas, J., 1993. Pedogenesis and paleoclimate: Interpretation of the magnetic susceptibility record of Chinese loess-paleosol sequences. Geology 21, 1011–1014.2.3.CO;2>CrossRefGoogle Scholar
Wang, B., 2006. The Asian Monsoon. Springer Verlag, Berlin.Google Scholar
Wang, T., Wu, J., Kou, X., Oliver, C., Mou, P., Ge, J., 2010. Ecologically asynchronous agricultural practice erodes sustainability of the Loess Plateau of China. Ecological Applications 20, 1126–1135.Google ScholarPubMed
Wang, W., Zheng, W., Zhang, P., Li, Q., Kirby, E., Yuan, D., Zheng, D., et al. , 2017. Expansion of the Tibetan Plateau during the Neogene. Nature Communications 8, 15887. https://doi.org/10.1038/ncomms15887.CrossRefGoogle ScholarPubMed
Wang, Y., Pan, B., Gao, H., Guan, Q., Chen, Y., Wang, J., 2007. Magnetic fabric-based reconstruction of the paleowind direction from a loess sequence in the northeastern flank of the Qilian mountains. Chinese Journal of Geophysics 50, 1005–1010.CrossRefGoogle Scholar
Wu, H.B., Chen, F.H., Wang, J.M., Cao, J.X., Zhang, Y.T., 1998. A study on the relationship between magnetic anisotropy of modern eolian sediments and wind direction. Chinese Journal of Geophysics 41, 811–817. [in Chinese with English abstract]Google Scholar
Wu, L., Prush, V., Lin, X., Xiao, A., Zhang, L., Chen, N., Yang, R., Chen, H., 2019. Quantifying wind erosion during the late Quaternary in the Qaidam Basin, Central Asia. Geophysical Research Letters 46, 6378–6387.CrossRefGoogle Scholar
Yang, S., Ding, Z., 2008. Advance–retreat history of the East-Asian summer monsoon rainfall belt over northern China during the last two glacial–interglacial cycles. Earth and Planetary Science Letters 274, 499–510.CrossRefGoogle Scholar
Zeeden, C., Hambach, U., Händel, M., 2015. Loess magnetic fabric of the Krems-Wachtberg archaeological site. Quaternary International 372, 188–194.CrossRefGoogle Scholar
Zhang, H., Lu, H., Xu, X., Liu, X., Yang, T., Stevens, T., Bird, A., Xu, Z., Zhang, T., Lei, F., Feng, H., 2016. Quantitative estimation of the contribution of dust sources to Chinese loess using detrital zircon U-Pb age patterns. Journal of Geophysical Research: Earth Surface 121, 2085–2099.Google Scholar
Zhang, R., Kravchinsky, V.A., Zhu, R., Yue, L., 2010. Paleomonsoon route reconstruction along a W–E transect in the Chinese Loess Plateau using the anisotropy of magnetic susceptibility: Summer monsoon model. Earth and Planetary Science Letters 299, 436–446.CrossRefGoogle Scholar
Zhang, X.Y., Gong, S.L., Zhao, T.L., Arimoto, R., Wang, Y.Q., Zhou, Z.J., 2003. Sources of Asian dust and role of climate change versus desertification in Asian dust emission. Geophysical Research Letters 30. https://doi.org/10.1029/2003GL018206.CrossRefGoogle Scholar
Zhao, H., Sun, Y., Qiang, X., 2017. Iron oxide characteristics of mid-Miocene Red Clay deposits on the western Chinese Loess Plateau and their paleoclimatic implications. Palaeogeography, Palaeoclimatology, Palaeoecology 468, 162–172.CrossRefGoogle Scholar
Zhou, L.P., Oldfield, F., Wintle, A.G., Robinson, S.G., Wang, J.T., 1990. Partly pedogenic origin of magnetic variations in Chinese loess. Nature 346, 737–739.CrossRefGoogle Scholar
Zhu, R., Liu, Q., Jackson, M.J., 2004. Paleoenvironmental significance of the magnetic fabrics in Chinese loess-paleosols since the last interglacial (<130 ka). Earth and Planetary Science Letters 221, 55–69.CrossRefGoogle Scholar