Progress and outlooks on magnetostratigraphy of Chinese loess

CHEN Tianran; XIAO Guoqiao; LIN Xinru; PAN Qing

doi:10.16562/j.cnki.0256-1492.2024013001

Marine Geology & Quaternary Geology > 2024 > 44(2): 1-15. > DOI: 10.16562/j.cnki.0256-1492.2024013001

CHEN Tianran，XIAO Guoqiao，LIN Xinru，et al. Progress and outlooks on magnetostratigraphy of Chinese loess[J]. Marine Geology & Quaternary Geology，2024，44(2)：1-15. DOI: 10.16562/j.cnki.0256-1492.2024013001

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Progress and outlooks on magnetostratigraphy of Chinese loess

1.
Hubei Key Laboratory of Critical Zone Evolution, School of Geography and Information Engineering, China University of Geosciences, Wuhan 430078, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
3.
Planetary Environmental and Astrobiological Research Laboratory, School of Atmospheric Sciences, Sun Yat-Sen University, Zhuhai 519000, China

More Information

Received Date: January 29, 2024
Revised Date: March 06, 2024
Accepted Date: March 06, 2024
Available Online: April 15, 2024

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Abstract

Abstract

The Chinese loess is one of the most important terrestrial records of the Quaternary climate changes. Magnetostratigraphy is one of the primary methods for establishing the chronological framework of the Quaternary loess. The measured positions of the Brunhes/Matuyama, Jaramillo, Olduvai, and Matuyama/Gauss polarity reversal boundaries in Chinese loess were summarized and compared against corresponding marine records. It was found that the positions of each polarity reversal boundary are inconsistent among different loess sections, and the difference spanned more than one loess-paleosol cycle. This discrepancy cannot be attributed to the lock-in effect, regional climate, sedimentation rate or different loess stratigraphic divisions. This may indicate that the polarity reversal boundaries recorded by loess deposits had probably experienced significant remagnetization, leading to a large discrepancy between loess geochronometer in magnetostratigraphy at orbital scale and marine oxygen isotope records by different researchers. In the future, studies shall focus more on the relative paleointensity (RPI) of loess to confirm the true position of each polarity reversal boundary and ultimately resolve the discrepancy in the comparison scheme between Chinese loess data and deep-sea sediment record.
- Chinese loess,
- Quaternary,
- magnetostratigraphy,
- remagnetization,
- relative paleointensity

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References (113)

References

[1]	An Z S. The history and variability of the East Asian paleomonsoon climate[J]. Quaternary Science Reviews, 2000, 19(1-5):171-187. doi: 10.1016/S0277-3791(99)00060-8
[2]	An Z S. Late Cenozoic Climate Change in Asia: Loess, Monsoon and Monsoon-Arid Environment Evolution[M]. Dordrecht: Springer, 2014: 1-582.
[3]	Guo Z T, Biscaye P, Wei L Y, et al. Summer monsoon variations over the last 1.2 Ma from the weathering of loess-soil sequences in China[J]. Geophysical Research Letters, 2000, 27(12):1751-1754. doi: 10.1029/1999GL008419
[4]	Hao Q Z, Wang L, Oldfield F, et al. Delayed build-up of Arctic ice sheets during 400, 000-year minima in insolation variability[J]. Nature, 2012, 490(7420):393-396. doi: 10.1038/nature11493
[5]	Liu T, Ding Z L. Chinese loess and the paleomonsoon[J]. Annual Review of Earth and Planetary Sciences, 1998, 26:111-145. doi: 10.1146/annurev.earth.26.1.111
[6]	Cohen K M, Gibbard P L. Global chronostratigraphical correlation table for the last 2.7 million years, version 2019 QI-500[J]. Quaternary International, 2019, 500:20-31. doi: 10.1016/j.quaint.2019.03.009
[7]	Gradstein F M, Ogg J G, Schmitz M D, et al. Geologic Time Scale 2020[M]. Amsterdam: Elsevier, 2020: 1-1357.
[8]	Heller F, Tung-sheng L. Magnetostratigraphical dating of loess deposits in China[J]. Nature, 1982, 300(5891):431-433. doi: 10.1038/300431a0
[9]	Heller F, Tungsheng L. Magnetism of Chinese loess deposits[J]. Geophysical Journal International, 1984, 77(1):125-141. doi: 10.1111/j.1365-246X.1984.tb01928.x
[10]	Kukla G, Heller F, Ming L X, et al. Pleistocene climates in China dated by magnetic susceptibility[J]. Geology, 1988, 16(9):811-814. doi: 10.1130/0091-7613(1988)016<0811:PCICDB>2.3.CO;2
[11]	Hovan S A, Rea D K, Pisias N G, et al. A direct link between the China loess and marine δ¹⁸O records: aeolian flux to the north Pacific[J]. Nature, 1989, 340(6231):296-298. doi: 10.1038/340296a0
[12]	Ding Z, Yu Z, Rutter N W, et al. Towards an orbital time scale for Chinese loess deposits[J]. Quaternary Science Reviews, 1994, 13(1):39-70. doi: 10.1016/0277-3791(94)90124-4
[13]	Lu H U, Liu X D, Zhang F Q, et al. Astronomical calibration of loess-paleosol deposits at Luochuan, central Chinese Loess Plateau[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1999, 154(3):237-246. doi: 10.1016/S0031-0182(99)00113-3
[14]	Heslop D, Langereis C G, Dekkers M J. A new astronomical timescale for the loess deposits of Northern China[J]. Earth and Planetary Science Letters, 2000, 184(1):125-139. doi: 10.1016/S0012-821X(00)00324-1
[15]	Ding Z L, Derbyshire E, Yang S L, et al. Stacked 2.6-Ma grain size record from the Chinese loess based on five sections and correlation with the deep-sea δ¹⁸O record[J]. Paleoceanography, 2002, 17(3):1033.
[16]	Sun Y B, Clemens S C, An Z S, et al. Astronomical timescale and palaeoclimatic implication of stacked 3.6-Myr monsoon records from the Chinese Loess Plateau[J]. Quaternary Science Reviews, 2006, 25(1-2):33-48. doi: 10.1016/j.quascirev.2005.07.005
[17]	Zhu Z Y, Dennell R, Huang W W, et al. Hominin occupation of the Chinese Loess Plateau since about 2.1 million years ago[J]. Nature, 2018, 559(7715):608-612. doi: 10.1038/s41586-018-0299-4
[18]	Ao H, Rohling E J, Stringer C, et al. Two-stage mid-Brunhes climate transition and mid-Pleistocene human diversification[J]. Earth-Science Reviews, 2020, 210:103354. doi: 10.1016/j.earscirev.2020.103354
[19]	Beck J W, Zhou W J, Li C, et al. A 550, 000-year record of East Asian monsoon rainfall from ¹⁰Be in loess[J]. Science, 2018, 360(6391):877-881. doi: 10.1126/science.aam5825
[20]	Han Y M, An Z S, Marlon J R, et al. Asian inland wildfires driven by glacial-interglacial climate change[J]. Proceedings of the National Academy of Sciences of the United States of America, 2020, 117(10):5184-5189.
[21]	Sun Y B, McManus J F, Clemens S C, et al. Persistent orbital influence on millennial climate variability through the Pleistocene[J]. Nature Geoscience, 2021, 14(11):812-818. doi: 10.1038/s41561-021-00794-1
[22]	Sun Y B, Clemens S C, Morrill C, et al. Influence of Atlantic meridional overturning circulation on the East Asian winter monsoon[J]. Nature Geoscience, 2012, 5(1):46-49. doi: 10.1038/ngeo1326
[23]	Lu H X, Liu W G, Yang H, et al. 800-kyr land temperature variations modulated by vegetation changes on Chinese Loess Plateau[J]. Nature Communications, 2019, 10(1):1958. doi: 10.1038/s41467-019-09978-1
[24]	Zhou L P, Shackleton N J. Misleading positions of geomagnetic reversal boundaries in Eurasian loess and implications for correlation between continental and marine sedimentary sequences[J]. Earth and Planetary Science Letters, 1999, 168(1-2):117-130. doi: 10.1016/S0012-821X(99)00052-7
[25]	Liu Q S, Roberts A P, Rohling E J, et al. Post-depositional remanent magnetization lock-in and the location of the Matuyama-Brunhes geomagnetic reversal boundary in marine and Chinese loess sequences[J]. Earth and Planetary Science Letters, 2008, 275(1-2):102-110. doi: 10.1016/j.jpgl.2008.08.004
[26]	Zhou W J, Beck J W, Kong X H, et al. Timing of the Brunhes-Matuyama magnetic polarity reversal in Chinese loess using ¹⁰Be[J]. Geology, 2014, 42(6):467-470. doi: 10.1130/G35443.1
[27]	Liu Q S, Jin C S, Hu P X, et al. Magnetostratigraphy of Chinese loess-paleosol sequences[J]. Earth-Science Reviews, 2015, 150:139-167. doi: 10.1016/j.earscirev.2015.07.009
[28]	Jin C S, Liu Q S, Xu D K, et al. A new correlation between Chinese loess and deep-sea δ¹⁸O records since the middle Pleistocene[J]. Earth and Planetary Science Letters, 2019, 506:441-454. doi: 10.1016/j.jpgl.2018.11.022
[29]	强小科, 徐新文, 陈艇, 等. 黄土高原黄土序列松山-布容地磁极性倒转界线空间分布特征与影响因素探讨[J]. 第四纪研究, 2016, 36(5):1125-1138 doi: 10.11928/j.issn.1001-7410.2016.05.09 QIANG Xiaoke, XU Xinwen, CHEN Ting, et al. Spatial characteristics and influencing factors of Matuyama-Brunhes polarity reversal boundary (MBB) in eolian sequences from the Chinese Loess Plateau[J]. Quaternary Sciences, 2016, 36(5):1125-1138.] doi: 10.11928/j.issn.1001-7410.2016.05.09
[30]	刘维明, 张立原, 孙继敏. 高分辨率洛川剖面黄土磁性地层学[J]. 地球物理学报, 2010, 53(4):888-894 doi: 10.3969/j.issn.0001-5733.2010.04.013 LIU Weiming, ZHANG Liyuan, SUN Jimin. High resolution magnetostratigraphy of the Luochuan loess-paleosol sequence in the central Chinese Loess Plateau[J]. Chinese Journal of Geophysics, 2010, 53(4):888-894.] doi: 10.3969/j.issn.0001-5733.2010.04.013
[31]	Pan Q, Xiao G Q, Zhao Q Y, et al. The Jaramillo subchron in Chinese loess-paleosol sequences[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2021, 572:110423. doi: 10.1016/j.palaeo.2021.110423
[32]	Channell J E T, Xuan C, Hodell D A. Stacking paleointensity and oxygen isotope data for the last 1.5 Myr (PISO-1500)[J]. Earth and Planetary Science Letters, 2009, 283(1-4):14-23. doi: 10.1016/j.jpgl.2009.03.012
[33]	Lisiecki L E, Raymo M E. A Pliocene‐Pleistocene stack of 57 globally distributed benthic δ¹⁸O records[J]. Paleoceanography, 2005, 20(1):PA1003.
[34]	Wang X S, Løvlie R, Chen Y, et al. The Matuyama-Brunhes polarity reversal in four Chinese loess records: high-fidelity recording of geomagnetic field behavior or a less than reliable chronostratigraphic marker?[J]. Quaternary Science Reviews, 2014, 101:61-76. doi: 10.1016/j.quascirev.2014.07.005
[35]	Xiao G Q, Pan Q, Zhao Q Y, et al. Early Pleistocene integration of the Yellow River II: evidence from the Plio-Pleistocene sedimentary record of the Fenwei Basin[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2021, 577:110550. doi: 10.1016/j.palaeo.2021.110550
[36]	Zheng H B, Huang X T, Ji J L, et al. Ultra-high rates of loess sedimentation at Zhengzhou since Stage 7: implication for the Yellow River erosion of the Sanmen Gorge[J]. Geomorphology, 2007, 85(3-4):131-142. doi: 10.1016/j.geomorph.2006.03.014
[37]	Wang D J, Wang Y C, Han J T, et al. Geomagnetic anomalies recorded in L9 of the Songjiadian loess section in southeastern Chinese Loess Plateau[J]. Chinese Science Bulletin, 2010, 55(6):520-529. doi: 10.1007/s11434-009-0565-9
[38]	Wang X S, Løvlie R, Yang Z Y, et al. Remagnetization of Quaternary eolian deposits: a case study from SE Chinese Loess Plateau[J]. Geochemistry, Geophysics, Geosystems, 2005, 6(6):Q06H18.
[39]	Pan Y X, Zhu R X, Liu Q S, et al. Geomagnetic episodes of the last 1.2 Myr recorded in Chinese loess[J]. Geophysical Research Letters, 2002, 29(8):1282.
[40]	Yang T S, Hyodo M, Yang Z Y, et al. Multiple rapid polarity swings during the Matuyama-Brunhes transition from two high-resolution loess-paleosol records[J]. Journal of Geophysical Research:Solid Earth, 2010, 115(B5):B05101.
[41]	Meng X Q, Liu L W, Wang X T, et al. Mineralogical evidence of reduced East Asian summer monsoon rainfall on the Chinese loess plateau during the early Pleistocene interglacials[J]. Earth and Planetary Science Letters, 2018, 486:61-69. doi: 10.1016/j.jpgl.2017.12.048
[42]	Song Y G, Fang X M, Li J J, et al. The Late Cenozoic uplift of the Liupan Shan, China[J]. Science in China Series D:Earth Sciences, 2001, 44(1):176-184.
[43]	Ding Z L, Sun J M, Liu D S. Stepwise advance of the Mu Us Desert since late Pliocene: evidence from a red clay-loess record[J]. Chinese Science Bulletin, 1999, 44(13):1211-1214. doi: 10.1007/BF02885968
[44]	Niu Y N, Fan Y X, Qiao Y S, et al. Chronostratigraphy of a loess-paleosol sequence in the western Chinese Loess Plateau based on ESR dating and magnetostratigraphy[J]. Quaternary International, 2022, 637:1-11. doi: 10.1016/j.quaint.2022.08.005
[45]	Zhang J, Li J J, Guo B H, et al. Magnetostratigraphic age and monsoonal evolution recorded by the thickest Quaternary loess deposit of the Lanzhou region, western Chinese Loess Plateau[J]. Quaternary Science Reviews, 2016, 139:17-29. doi: 10.1016/j.quascirev.2016.02.025
[46]	Sun Y B, Yin Q Z, Crucifix M, et al. Diverse manifestations of the mid-Pleistocene climate transition[J]. Nature Communications, 2019, 10(1):352. doi: 10.1038/s41467-018-08257-9
[47]	杨东, 方小敏, 董光荣, 等. 1.8 Ma BP以来陇西断岘黄土剖面沉积特征及其反映的腾格里沙漠演化[J]. 中国沙漠, 2006, 26(1):6-13 doi: 10.3321/j.issn:1000-694X.2006.01.002 YANG Dong, FANG Xiaomin, DONG Guangrong, et al. Loess deposit characteristic in Duanxian section of Longxi Basin and its reflected evolution of Tengger Desert at north of China since last 1.8 Ma[J]. Journal of Desert Research, 2006, 26(1):6-13.] doi: 10.3321/j.issn:1000-694X.2006.01.002
[48]	An Z S, Kutzbach J E, Prell W L, et al. Evolution of Asian monsoons and phased uplift of the Himalaya–Tibetan plateau since Late Miocene times[J]. Nature, 2001, 411(6833):62-66. doi: 10.1038/35075035
[49]	Spassov S, Heller F, Evans M E, et al. A lock-in model for the complex Matuyama-Brunhes boundary record of the loess/palaeosol sequence at Lingtai (Central Chinese Loess Plateau)[J]. Geophysical Journal International, 2003, 155(2):350-366. doi: 10.1046/j.1365-246X.2003.02026.x
[50]	Sun Y B, Qiang X K, Liu Q S, et al. Timing and lock-in effect of the Laschamp geomagnetic excursion in Chinese Loess[J]. Geochemistry, Geophysics, Geosystems, 2013, 14(11):4952-4961. doi: 10.1002/2013GC004828
[51]	Zhu R X, Pan Y X, Guo B, et al. A recording phase lag between ocean and continent climate changes: constrained by the Matuyama/Brunhes polarity boundary[J]. Chinese Science Bulletin, 1998, 43(19):1593-1599. doi: 10.1007/BF02883400
[52]	Jin C S, Liu Q S. Reliability of the natural remanent magnetization recorded in Chinese loess[J]. Journal of Geophysical Research:Solid Earth, 2010, 115(B4):B04103.
[53]	Løvlie R, Wang R H, Wang X S. In situ remagnetization experiments of loess on the Chinese Loess Plateau: evidence for localized post-depositional remanent magnetization[J]. Geochemistry, Geophysics, Geosystems, 2011, 12(12):Q12015.
[54]	Channell J E T, Hodell D A, Curtis J H. Relative paleointensity (RPI) and oxygen isotope stratigraphy at IODP Site U1308: North Atlantic RPI stack for 1.2-2.2 Ma (NARPI-2200) and age of the Olduvai Subchron[J]. Quaternary Science Reviews, 2016, 131:1-19. doi: 10.1016/j.quascirev.2015.10.011
[55]	Channell J E T, Singer B S, Jicha B R. Timing of Quaternary geomagnetic reversals and excursions in volcanic and sedimentary archives[J]. Quaternary Science Reviews, 2020, 228:106114. doi: 10.1016/j.quascirev.2019.106114
[56]	Valet J P, Bassinot F, Simon Q, et al. Constraining the age of the last geomagnetic reversal from geochemical and magnetic analyses of Atlantic, Indian, and Pacific Ocean sediments[J]. Earth and Planetary Science Letters, 2019, 506:323-331. doi: 10.1016/j.jpgl.2018.11.012
[57]	Valet J P, Meynadier L, Guyodo Y. Geomagnetic dipole strength and reversal rate over the past two million years[J]. Nature, 2005, 435(7043):802-805. doi: 10.1038/nature03674
[58]	Guyodo Y, Valet J P. Global changes in intensity of the Earth's magnetic field during the past 800 kyr[J]. Nature, 1999, 399(6733):249-252. doi: 10.1038/20420
[59]	Izett G A, Obradovich J D. ⁴⁰Ar/³⁹Ar age constraints for the Jaramillo Normal Subchron and the Matuyama‐Brunhes geomagnetic boundary[J]. Journal of Geophysical Research:Solid Earth, 1994, 99(B2):2925-2934. doi: 10.1029/93JB03085
[60]	Singer B S, Hoffman K A, Chauvin A, et al. Dating transitionally magnetized lavas of the late Matuyama Chron: toward a new ⁴⁰Ar/³⁹Ar timescale of reversals and events[J]. Journal of Geophysical Research:Solid Earth, 1999, 104(B1):679-693. doi: 10.1029/1998JB900016
[61]	赵志中, 吴锡浩, 蒋复初, 等. 三门峡地区黄土与古季风[J]. 地质力学学报, 2000, 6(4):19-26,66 doi: 10.3969/j.issn.1006-6616.2000.04.003 ZHAO Zhizhong, WU Xihao, JIANG Fuchu, et al. The loess stratigraphy in Sanmenxia area[J]. Journal of Geomechanics, 2000, 6(4):19-26,66.] doi: 10.3969/j.issn.1006-6616.2000.04.003
[62]	Rutter N, Ding Z L, Evans M E, et al. Magnetostratigraphy of the Baoji loess-paleosol section in the north-central China Loess Plateau[J]. Quaternary International, 1990, 7-8:97-102. doi: 10.1016/1040-6182(90)90043-4
[63]	Ding Z L, Sun J M, Yang S L, et al. Preliminary magnetostratigraphy of a thick eolian red clay-loess sequence at Lingtai, the Chinese Loess Plateau[J]. Geophysical Research Letters, 1998, 25(8):1225-1228. doi: 10.1029/98GL00836
[64]	Sun D H, Shaw J, An Z S, et al. Magnetostratigraphy and paleoclimatic interpretation of a continuous 7.2 Ma Late Cenozoic eolian sediments from the Chinese Loess Plateau[J]. Geophysical Research Letters, 1998, 25(1):85-88. doi: 10.1029/97GL03353
[65]	Li T, Liu F, Abels H A, et al. Continued obliquity pacing of East Asian summer precipitation after the mid-Pleistocene transition[J]. Earth and Planetary Science Letters, 2017, 457:181-190. doi: 10.1016/j.jpgl.2016.09.045
[66]	Guo B, Zhu R X, Florindo F, et al. A short, reverse polarity interval within the Jaramillo subchron: evidence from the Jingbian section, northern Chinese Loess Plateau[J]. Journal of Geophysical Research:Solid Earth, 2002, 107(B6):2124.
[67]	Jin C S, Liu Q S. Remagnetization mechanism and a new age model for L9 in Chinese loess[J]. Physics of the Earth and Planetary Interiors, 2011, 187(3-4):261-275. doi: 10.1016/j.pepi.2011.03.010
[68]	朱日祥, 岳乐平, 白立新. 中国第四纪古地磁学研究进展[J]. 第四纪研究, 1995, 15(2):162-173 doi: 10.3321/j.issn:1001-7410.1995.02.009 ZHU Rixiang, YUE Leping, BAI Lixin. Progress of quaternary paleomagnetism in China[J]. Quaternary Sciences, 1995, 15(2):162-173.] doi: 10.3321/j.issn:1001-7410.1995.02.009
[69]	Rolph T C. The Matuyama-Jaramillo R-N transition recorded in a loess section near Lanzhou, P. R. China[J]. Journal of Geomagnetism and Geoelectricity, 1993, 45(4):301-318. doi: 10.5636/jgg.45.301
[70]	Yang S L, Ding Z L. Drastic climatic shift at ~ 2.8 Ma as recorded in eolian deposits of China and its implications for redefining the Pliocene-Pleistocene boundary[J]. Quaternary International, 2010, 219(1-2):37-44. doi: 10.1016/j.quaint.2009.10.029
[71]	刘平, 张崧, 韩家懋, 等. 甘肃龙担早第四纪黄土堆积古地磁年代研究[J]. 第四纪研究, 2008, 28(5):796-805 doi: 10.3321/j.issn:1001-7410.2008.05.002 LIU Ping, ZHANG Song, HAN Jiamao, et al. Paleomagnetic chronology of Quaternary stratigraphy of the Longdan section in Gansu Province of China[J]. Quaternary Sciences, 2008, 28(5):796-805.] doi: 10.3321/j.issn:1001-7410.2008.05.002
[72]	Yang T S, Hyodo M, Yang Z Y, et al. Latest Olduvai short-lived reversal episodes recorded in Chinese loess[J]. Journal of Geophysical Research:Solid Earth, 2008, 113(B5):B05103.
[73]	Spassov S, Hus J, Heller F, et al. The termination of the Olduvai Subchron at Lingtai, Chinese Loess Plateau: geomagnetic field behavior or complex remanence acquisition?[M]//Petrovský E, Ivers D, Harinarayana T, et al. The Earth's Magnetic Interior. Dordrecht: Springer, 2011: 235-245.
[74]	Cande S C, Kent D V. Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic[J]. Journal of Geophysical Research:Solid Earth, 1995, 100(B4):6093-6095. doi: 10.1029/94JB03098
[75]	Deino A L, Kingston J D, Glen J M, et al. Precessional forcing of lacustrine sedimentation in the late Cenozoic Chemeron Basin, Central Kenya Rift, and calibration of the Gauss/Matuyama boundary[J]. Earth and Planetary Science Letters, 2006, 247(1-2):41-60. doi: 10.1016/j.jpgl.2006.04.009
[76]	Ohno M, Hayashi T, Komatsu F, et al. A detailed paleomagnetic record between 2.1 and 2.75 Ma at IODP Site U1314 in the North Atlantic: geomagnetic excursions and the Gauss-Matuyama transition[J]. Geochemistry, Geophysics, Geosystems, 2012, 13(5):Q12Z39.
[77]	Liu X M, Liu T, Xu T C, et al. The Chinese loess in Xifeng, I. The primary study on magnetostratigraphy of a loess profile in Xifeng area, Gansu province[J]. Geophysical Journal International, 1988, 92(2):345-348. doi: 10.1111/j.1365-246X.1988.tb01146.x
[78]	孙建中, 赵景波, 孙秀英, 等. 黄土, 还要更老些[J]. 海洋地质与第四纪地质, 1987, 7(1):105-112 SUN Jianzhong, ZHAO Jingbo, SUN Xiuying, et al. Loess is even older[J]. Marine Geology & Quaternary Geology, 1987, 7(1):105-112.]
[79]	Ding Z L, Derbyshire E, Yang S L, et al. Stepwise expansion of desert environment across northern China in the past 3.5 Ma and implications for monsoon evolution[J]. Earth and Planetary Science Letters, 2005, 237(1-2):45-55. doi: 10.1016/j.jpgl.2005.06.036
[80]	朱日祥, 郭斌, 丁仲礼, 等. Gauss-Matuyama极性转换期间地球磁场方向和强度变化特征[J]. 地球物理学报, 2000, 43(5):621-634 doi: 10.3321/j.issn:0001-5733.2000.05.006 ZHU Rixiang, GUO Bin, DING Zhongli, et al. Gauss-Matuyama polarity transition obtained from a loess section at Weinan, North-Central China[J]. Chinese Journal of Geophysics, 2000, 43(5):621-634.] doi: 10.3321/j.issn:0001-5733.2000.05.006
[81]	Ding Z L, Rutter N W, Liu T. The onset of extensive loess deposition around the G/M boundary in China and its palaeoclimatic implications[J]. Quaternary International, 1997, 40:53-60. doi: 10.1016/S1040-6182(96)00061-4
[82]	Zhou W J, Kong X H, Du Y J, et al. ¹⁰Be indicator for the Matuyama‐Gauss magnetic polarity reversal from Chinese Loess[J]. Geophysical Research Letters, 2023, 50(8):e2022GL102486. doi: 10.1029/2022GL102486
[83]	Yang T S, Hyodo M, Yang Z Y, et al. High-frequency polarity swings during the Gauss-Matuyama reversal from Baoji loess sediment[J]. Science China Earth Sciences, 2014, 57(8):1929-1943. doi: 10.1007/s11430-014-4825-4
[84]	杨石岭, 侯圣山, 王旭, 等. 泾川晚第三纪红粘土的磁性地层及其与灵台剖面的对比[J]. 第四纪研究, 2000, 20(5):423-434 doi: 10.3321/j.issn:1001-7410.2000.05.003 YANG Shiling, HOU Shengshan, WANG Xu, et al. Completeness and continuity of the Late Tertiary red clay sequence in Northern China: evidence from the correlation of magnetostratigraphy and pedostratigraphy between Jingchuan and Lingtai[J]. Quaternary Sciences, 2000, 20(5):423-434.] doi: 10.3321/j.issn:1001-7410.2000.05.003
[85]	丁仲礼, 孙继敏, 朱日祥, 等. 黄土高原红粘土成因及上新世北方干旱化问题[J]. 第四纪研究, 1997, 17(2):147-157 doi: 10.3321/j.issn:1001-7410.1997.02.007 DING Zhongli, SUN Jimin, ZHU Rixiang, et al. Eolian origin of the red clay deposits in the Loess Plateau and implications for Pliocene climatic changes[J]. Quaternary Sciences, 1997, 17(2):147-157.] doi: 10.3321/j.issn:1001-7410.1997.02.007
[86]	Zan J B, Fang X M, Zhang W L, et al. A new record of late Pliocene-early Pleistocene aeolian loess-red clay deposits from the western Chinese Loess Plateau and its palaeoenvironmental implications[J]. Quaternary Science Reviews, 2018, 186:17-26. doi: 10.1016/j.quascirev.2018.02.010
[87]	岳乐平. 中国黄土与红色粘土记录的地磁极性界限及地质意义[J]. 地球物理学报, 1995, 38(3):311-320 doi: 10.3321/j.issn:0001-5733.1995.03.006 YUE Leping. Palaeomagnetic polarity boundary were recorded in Chinese loess and red clay, and geological significance[J]. Acta Geophysica Sinica, 1995, 38(3):311-320.] doi: 10.3321/j.issn:0001-5733.1995.03.006
[88]	谢兴俊, 周卫健, 鲜锋, 等. 中国黄土中松山-高斯极性倒转事件记录的空间对比[J]. 中山大学学报:自然科学版, 2014, 53(2):121-130 XIE Xingjun, ZHOU Weijian, XIAN Feng, et al. The spatial discrepancy records of Matuyama-Gauss polarity reversal in Chinese loess[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 2014, 53(2):121-130.]
[89]	Zhao X, Roberts A P. How does Chinese loess become magnetized?[J]. Earth and Planetary Science Letters, 2010, 292(1-2):112-122. doi: 10.1016/j.jpgl.2010.01.026
[90]	Deng C L, Shaw J, Liu Q S, et al. Mineral magnetic variation of the Jingbian loess/paleosol sequence in the northern Loess Plateau of China: implications for Quaternary development of Asian aridification and cooling[J]. Earth and Planetary Science Letters, 2006, 241(1-2):248-259. doi: 10.1016/j.jpgl.2005.10.020
[91]	Tauxe L, Herbert T, Shackleton N J, et al. Astronomical calibration of the Matuyama-Brunhes boundary: consequences for magnetic remanence acquisition in marine carbonates and the Asian loess sequences[J]. Earth and Planetary Science Letters, 1996, 140(1-4):133-146. doi: 10.1016/0012-821X(96)00030-1
[92]	Head M J, Gibbard P L. Early-Middle Pleistocene transitions: linking terrestrial and marine realms[J]. Quaternary International, 2015, 389:7-46. doi: 10.1016/j.quaint.2015.09.042
[93]	Wang X S, Yang Z Y, Løvlie R, et al. A magnetostratigraphic reassessment of correlation between Chinese loess and marine oxygen isotope records over the last 1.1 Ma[J]. Physics of the Earth and Planetary Interiors, 2006, 159(1-2):109-117. doi: 10.1016/j.pepi.2006.07.002
[94]	Sun J M. Long-term fluvial archives in the Fen Wei Graben, central China, and their bearing on the tectonic history of the India-Asia collision system during the Quaternary[J]. Quaternary Science Reviews, 2005, 24(10-11):1279-1286. doi: 10.1016/j.quascirev.2004.08.018
[95]	Liu T, Ding Z L, Rutter N. Comparison of Milankovitch periods between continental loess and deep sea records over the last 2.5 Ma[J]. Quaternary Science Reviews, 1999, 18(10-11):1205-1212. doi: 10.1016/S0277-3791(98)00110-3
[96]	Cai S H, Jin G Y, Tauxe L, et al. Archaeointensity results spanning the past 6 kiloyears from eastern China and implications for extreme behaviors of the geomagnetic field[J]. Proceedings of the National Academy of Sciences of the United States of America, 2017, 114(1):39-44.
[97]	Tauxe L. Sedimentary records of relative paleointensity of the geomagnetic field: theory and practice[J]. Reviews of Geophysics, 1993, 31(3):319-354. doi: 10.1029/93RG01771
[98]	Cheng H, Edwards R L, Southon J, et al. Atmospheric ¹⁴C/¹²C changes during the last glacial period from Hulu Cave[J]. Science, 2018, 362(6420):1293-1297. doi: 10.1126/science.aau0747
[99]	Zhou W J, Xian F, Beck J W, et al. Reconstruction of 130-kyr relative geomagnetic intensities from ¹⁰Be in two Chinese loess sections[J]. Radiocarbon, 2010, 52(1):129-147. doi: 10.1017/S0033822200045082
[100]	Xian F, An Z S, Wu Z K, et al. A simple model for reconstructing geomagnetic field intensity with ¹⁰Be production rate and its application in Loess studies[J]. Science in China Series D:Earth Sciences, 2008, 51(6):855-861. doi: 10.1007/s11430-008-0054-z
[101]	Raisbeck G M, Yiou F, Cattani O, et al. ¹⁰Be evidence for the Matuyama-Brunhes geomagnetic reversal in the EPICA Dome C ice core[J]. Nature, 2006, 444(7115):82-84. doi: 10.1038/nature05266
[102]	Baumgartner S, Beer J, Masarik J, et al. Geomagnetic modulation of the ³⁶Cl flux in the GRIP ice core, Greenland[J]. Science, 1998, 279(5355):1330-1332. doi: 10.1126/science.279.5355.1330
[103]	Guyodo Y, Valet J P. Relative variations in geomagnetic intensity from sedimentary records: the past 200, 000 years[J]. Earth and Planetary Science Letters, 1996, 143(1-4):23-36. doi: 10.1016/0012-821X(96)00121-5
[104]	Laj C, Kissel C, Mazaud A, et al. North Atlantic palaeointensity stack since 75ka (NAPIS-75) and the duration of the Laschamp event[J]. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 2000, 358(1768): 1009-1025.
[105]	Stoner J S, Laj C, Channell J E T, et al. South Atlantic and North Atlantic geomagnetic paleointensity stacks (0-80 ka): implications for inter-hemispheric correlation[J]. Quaternary Science Reviews, 2002, 21(10):1141-1151. doi: 10.1016/S0277-3791(01)00136-6
[106]	Yamazaki T, Oda H. A geomagnetic paleointensity stack between 0.8 and 3.0 Ma from equatorial Pacific sediment cores[J]. Geochemistry, Geophysics, Geosystems, 2005, 6(11):Q11H20.
[107]	Pan Y X, Zhu R X, Shaw J, et al. Can relative paleointensities be determined from the normalized magnetization of the wind-blown loess of China?[J]. Journal of Geophysical Research:Solid Earth, 2001, 106(B9):19221-19232. doi: 10.1029/2001JB000360
[108]	Kent D V. Apparent correlation of palaeomagnetic intensity and climatic records in deep-sea sediments[J]. Nature, 1982, 299(5883):538-539. doi: 10.1038/299538a0
[109]	Jin C S, Liu Q S, Larrasoaña J C. A precursor to the Matuyama–Brunhes reversal in Chinese loess and its palaeomagnetic and stratigraphic significance[J]. Geophysical Journal International, 2012, 190(2):829-842. doi: 10.1111/j.1365-246X.2012.05537.x
[110]	Zhu R X, Ding Z L, Wu H N, et al. Details of magnetic polarity transition recorded in Chinese loess[J]. Journal of Geomagnetism and Geoelectricity, 1993, 45(4):289-299. doi: 10.5636/jgg.45.289
[111]	Wu Y, Zhu Z Y, Qiu S F, et al. Magnetic stratigraphy constraints on the Matuyama-Brunhes boundary recorded in a loess section at the southern margin of Chinese Loess Plateau[J]. Geophysical Journal International, 2016, 204(2):1072-1085. doi: 10.1093/gji/ggv502
[112]	Li G H, Xia D S, Appel E, et al. Characteristics of a relative paleointensity record from loess deposits in arid central Asia and chronological implications[J]. Quaternary Geochronology, 2020, 55:101034. doi: 10.1016/j.quageo.2019.101034
[113]	Liu Q S, Banerjee S K, Jackson M J, et al. Inter-profile correlation of the Chinese loess/paleosol sequences during Marine Oxygen Isotope Stage 5 and indications of pedogenesis[J]. Quaternary Science Reviews, 2005, 24(1-2):195-210. doi: 10.1016/j.quascirev.2004.07.021

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Progress and outlooks on magnetostratigraphy of Chinese loess