[1] 黄镇国,张伟强. 中国红土期气候期构造期的耦合[J]. 地理学报,2000,55（2）：200-208.

Huang Zhenguo, Zhang Weiqiang. Coupling relationship between the red earth evolution, climate change and tectonic movement in China[J]. Acta Geographica Sinica, 2000, 55(2): 200-208.
[2] 邓黄月,郑祥民,杨立辉,等. 长江中下游地区第四纪红土磁学特征及其环境意义[J]. 沉积学报,2015,33（2）：285-298.

Deng Huangyue, Zheng Xiangmin, Yang Lihui, et al. Magnetic properties of Quaternary red earth profile in Yangtze River valley and its paleo-environmental implications[J]. Acta Sedimentologica Sinica, 2015, 33(2): 285-298.
[3] 吴开钦,李凤全,王天阳,等. 浙江金华红土网纹成因的磁学证据[J]. 沉积学报,2023,41（3）：706-719.

Wu Kaiqin, Li Fengquan, Wang Tianyang, et al. Magnetic characteristics evident in the formation of the reticulate structure of red paleosol in Jinhua, Zhejiang[J]. Acta Sedimentologica Sinica,2023,41(3):706-719.
[4] 杨浩,赵其国,李小平,等. 安徽宣城风成沉积—红土系列剖面ESR年代学研究[J]. 土壤学报,1996,33（3）：293-300.

Yang Hao, Zhao Qiguo, Li Xiaoping, et al. ESR dating of eolian sediment and red earth series from Xuancheng profile in Anhui province[J]. Acta Pedologica Sinica, 1996, 33(3): 293-300.
[5] 邓黄月,高悦,郑祥民,等. 我国南方红土岩石磁学特征及其磁化率增强机制[J]. 海洋地质与第四纪地质,2015,35（4）：163-175.

Deng Huangyue, Gao Yue, Zheng Xiangmin, et al. Rock-magnetic characteristics of the red soils in southern China and the magnetism for enhancing magnetic susceptibility[J]. Marine Geology & Quaternary Geology, 2015, 35(4): 163-175.
[6] 刘彩彩,邓成龙. 南方红土的磁性矿物组成及其区域性差异[J]. 第四纪研究,2012,32（4）：626-634.

Liu Caicai, Deng Chenglong. Magnetic mineralogy of the red soil sequences in southern China and its variety[J]. Quaternary Sciences, 2012, 32(4): 626-634.
[7] Hu X F, Wei J, Xu L F, et al. Magnetic susceptibility of the Quaternary red clay in subtropical China and its paleoenvironmental implications[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2009, 279(3/4): 216-232.
[8] Liu C C, Deng C L, Liu Q S. Mineral magnetic studies of the vermiculated red soils in southeast China and their paleoclimatic significance[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2012, 329-330: 173-183.
[9] 朱丽东,周尚哲,李凤全,等. 庐山JL红土剖面的色度气候意义[J]. 热带地理,2007,27（3）：193-197,202.

Zhu Lidong, Zhou Shangzhe, Li Fengquan, et al. Climatic implication of the chroma of JL red earth section in the Lushan Mountain[J]. Tropical Geography, 2007, 27(3): 193-197, 202.
[10] 朱丽东,刘名瑜,谷喜吉,等. 金衢盆地网纹红土色度及其环境意义[J]. 海洋地质与第四纪地质,2014,34（3）：133-141.

Zhu Lidong, Liu Mingyu, Gu Xiji, et al. Envionmental implication of the color index of the plinthitic red earth in Jinhua-Quzhou Basin[J]. Marine Geology & Quaternary Geology, 2014, 34(3): 133-141.
[11] 张智,凌超豪,贾玉连,等. 多重理化指标揭示的中国南方更新世网纹红土网纹化机制[J]. 地层学杂志,2020,44（1）：95-103.

Zhang Zhi, Ling Chaohao, Jia Yulian, et al. Multi-physico chemical evidences for formation of Pleistocene reticulated soil and its environmental implication in South China[J]. Journal of Stratigraphy, 2020, 44(1): 95-103.
[12] Hu X F, Du Y, Guan C L, et al. Color variations of the Quaternary red clay in southern China and its paleoclimatic implications[J]. Sedimentary Geology, 2014, 303: 15-25.
[13] 朱丽东,周尚哲,李凤全,等. 南方更新世红土氧化物地球化学特征[J]. 地球化学,2007,36（3）：295-302.

Zhu Lidong, Zhou Shangzhe, Li Fengquan, et al. Geochemical behavior of major elements of Pleistocene red earth in South China[J]. Geochimica, 2007, 36(3): 295-302.
[14] 许良峰,魏骥,姜伟. 皖南网纹红土的剖面风化特征及其古气候意义[J]. 土壤通报,2010,41（1）：7-12.

Xu Liangfeng, Wei Ji, Jiang Wei. The weathering characteristics of the reticulate red clay in southern Anhui province and its paleo-environmental significance[J]. Chinese Journal of Soil Science, 2010, 41(1): 7-12.
[15] Hong H L, Gu Y S, Yin K, et al. Red soils with white net-like veins and their climate significance in South China[J]. Geoderma, 2010, 160(2): 197-207.
[16] Hong H L, Gu Y S, Li R B, et al. Clay mineralogy and geochemistry and their palaeoclimatic interpretation of the Pleistocene deposits in the Xuancheng section, southern China[J]. Journal of Quaternary Science, 2010, 25(5): 662-674.
[17] Hong H L, Li Z H, Yang M Z, et al. Kaolin in the net-like horizon of laterite in Hubei, South China[J]. Clay Minerals, 2009, 44(1): 51-66.
[18] 徐传奇,廖富强,贾玉连,等. 中国南方网纹红土元素地球化学特征及其对网纹化过程的指示意义[J]. 古地理学报,2016,18（5）：865-878.

Xu Chuanqi, Liao Fuqiang, Jia Yulian, et al. Element geochemical characteristics of the reticulate red clay in southern China and its significance for the formation proccess of reticulated mottles[J]. Journal of Palaeogeography, 2016, 18(5): 865-878.
[19] 朱景郊. 网纹红土的成因及其研究意义[J]. 地理研究,1988,7（4）：12-20.

Zhu Jingjiao. Genesis and research significance of the plinthitic horizon[J]. Geographical Research, 1988, 7(4): 12-20.
[20] 熊尚发,丁仲礼,刘东生. 南方红土网纹：古森林植物根系的土壤学证据[J]. 科学通报,2000,45（12）：1317-1321.

Xiong Shangfa, Ding Zhongli, Liu Tungsheng. The worm-shaped veins in the red earth of South China: Pedological evidence for root traces of past forest[J]. Chinese Science Bulletin, 2000, 45(12): 1317-1321.
[21] 王春林. 湖南第四系蠕虫状网纹红土的成因及其对新构造运动研究的意义[J]. 湖南师范大学（自然科学学报）,1986,9（1）：100-106.

Wang Chunlin. On the origin of Quaternary worm-likenet-veined red (laterite) soil in Hunan province and its significantin neotectonic studies[J]. Journal of Natural Science of Hunan Normal University, 1986, 9(1): 100-106.
[22] 朱丽东. 中亚热带加积型红土及其所记录的第四纪环境变化探讨[D]. 兰州：兰州大学,2007.

Zhu Lidong. Aggradation red earth sediments in mid-subtropics of China and their recorded environmental changes during Quaternary[D]. Lanzhou: Lanzhou University, 2007.
[23] 张硕. 宣城向阳剖面网纹红土微区地球化学特征及网纹成因研究[D]. 芜湖：安徽师范大学,2020.

Zhang Shuo. The study of micro-area geochemical characteristics and genesis of reticulated red clay in Xiangyang Xuancheng profile[D]. Wuhu: Anhui Normal University, 2020.
[24] 刘海丽. 宣城官塘村红土剖面的网纹成因浅析[D]. 南京：南京大学,2012.

Liu Haili. Formation of vermiculated mottles in the laterite at Guantangcun of Xuancheng[D]. Najing: Najing University, 2012.
[25] 张姗姗. 基于监督分类的中国南方网纹红土色彩与形态研究[D]. 金华：浙江师范大学,2015.

Zhang Shanshan. Researches on plinthitic red earth colors and forms of southern China based on supervised classification[D]. Jinhua: Zhejiang Normal University, 2015.
[26] McLennan S M. Weathering and global denudation[J]. The Journal of Geology, 1993, 101(2): 295-303.
[27] 胡雪峰,朱煜,沈铭能. 南方网纹红土多元成因的粒度证据[J]. 科学通报,2005,50（9）：918-925.

Hu Xuefeng, Zhu Yu, Sheng Mingneng. Grain-size evidence for multiple origins of the reticulate red clay in southern China[J]. Chinese Science Bulletin, 2005, 50(9): 918-925.
[28] 朱丽东,叶玮,周尚哲,等. 中亚热带第四纪红粘土的粒度特征[J]. 地理科学,2006,26（5）：586-591.

Zhu Lidong, Ye Wei, Zhou Shangzhe, et al. Grain-size features of red earth in mid-subtropics[J]. Scientia Geographica Sinica, 2006, 26(5): 586-591.
[29] 叶玮,朱丽东,李凤全,等. 中国中亚热带网纹红土的地球化学特征与沉积环境[J]. 土壤学报,2008,45（3）：385-391.

Ye Wei, Zhu Lidong, Li Fengquan, et al. Sedimentary environment of vermicular red earth in mid-subtropical China[J]. Acta Pedologica Sinica, 2008, 45(3): 385-391.
[30] 刘东生. 黄土与环境[M]. 北京：科学出版社,1985.

Liu Tungsheng. Loess and environment[M]. Beijing: Science Press, 1985.
[31] 张晓,朱丽东,李凤全,等. 0.44Ma以来南方风尘加积型红土物源分析：重矿物和碎屑锆石年代学证据[J]. 沉积学报,2022,40（2）：494-507.

Zhang Xiao, Zhu Lidong, Li Fengquan, et al. Provenance analysis of eolian red earth aggradation in southern China since 0.44 Ma: Heavy minerals and detrital zircon geochronology[J]. Acta Sedimentologica Sinica, 2022, 40(2): 494-507.
[32] 黄颖,朱丽东,张晓,等. 庐山北麓JL红土剖面粉砂粒级元素地球化学特征及其物源意义[J]. 第四纪研究,2019,39（5）：1092-1102.

Huang Ying, Zhu Lidong, Zhang Xiao, et al. Geochemical characteristics and their provenance implications of the silt fraction from JL red erath section in Lushan region, Jiujiang, South China[J]. Quaternary Sciences, 2019, 39(5): 1092-1102.
[33] 凌超豪,张智,贾玉连,等. 元素地球化学揭示的长江中游鄱阳湖地区中更新世以来粉尘堆积的物源特征及其环境意义[J]. 第四纪研究,2019,39（5）：1103-1115.

Ling Chaohao, Zhang Zhi, Jia Yulian, et al. Geochemical evidence for provenance of aeolian depostion from poyang lake region in the middle reaches of Yangtze River since the Middle Pleistocene and its environmental significance[J]. Quaternary Sciences, 2019, 39(5): 1103-1115.
[34] 黄翡,熊尚发. 江西九江第四纪红土中的植物硅酸体及孢粉[J]. 微体古生物学报,2001,18（2）：203-210.

Huang Fei, Xiong Shangfa. Phytolith and pollen records of Quaternary red earth in Jiujiang city, Jiangxi province[J]. Acta Micropalaeontologica Sinica, 2001, 18(2): 203-210.
[35] Taylor S R, McLennan S M. The continental crust: Its composition and evolution[M]. Oxford : Blackwell, 1985.
[36] Nesbitt H W Young G M. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites[J]. Nature, 1982, 299(5885): 715-717.
[37] Pendleton R L, Jenny H. Factors of soil formation: A system of quantitative pedology[J]. Geographical Review, 1945, 35(2): 336.
[38] 袁国栋,龚子同. 第四纪红土的土壤发生及其古地理意义[J]. 土壤学报,1990,27（1）：54-62.

Yuan Guodong, Gong Zitong. Soil genesis of Quaternary red earth and its paleogeographic implication[J]. Acta Pedologica Sinica, 1990, 27(1): 54-62.
[39] 熊尚发,刘东生,丁仲礼. 南方红土的剖面风化特征[J]. 山地学报,2000,18（1）：7-12.

Xiong Shangfa, Liu Tungsheng, Ding Zhongli. The weathering sequence of the red earth over southern China[J]. Journal of Mountain Science, 2000, 18(1): 7-12.
[40] 凌超豪,龙进,贾玉连,等. 赣北鄱阳湖地区土塘剖面第四纪红土地球化学特征及古气候意义[J]. 古地理学报,2015,17（5）：699-708.

Ling Chaohao, Long Jin, Jia Yulian, et al. Geochemical characteristics and palaeoclimate significance of the Quaternary laterite of Tutan section in Poyang Lake region, northern Jiangxi province[J]. Journal of Palaeogeography, 2015, 17(5): 699-708.
[41] 李荣彪. 长江中下游网纹红土中氧化铁矿物相及其气候环境意义：以安徽宣城红土剖面为例[D]. 武汉：中国地质大学, 2014.

Li Rongbiao. Iron oxide minerals and their palaeoclimatic significance in laterite profile in the middle to lower reaches of the Yangtze River: A case study in Xuancheng laterite profile[D]. Wuhan: China University of Geosciences, 2014.
[42] 刘彩彩. 南方红土岩石磁学和古地磁学研究[D]. 北京：中国科学院地质与地球物理研究所,2010.

Liu Caicai. Rock magnetism and paleomagnetism of the red soil sequences in southern China[D]. Beijing: Institute of Geology and Geophysics, Chinese Academy of Sciences, 2010.
[43] 卢升高. 亚热带富铁土的磁学性质及其磁性矿物学[J]. 地球物理学报,2000,43（4）：498-504.

Lu Shenggao. Magnetic properties of subtropical ferrisols and its magnetic mineralogical study[J]. Chinese Journal of Geophysics, 2000, 43(4): 498-504.
[44] 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.
[45] Liu C C, Deng C L, Liu Q S, et al. Mineral magnetism to probe into the nature of palaeomagnetic signals of subtropical red soil sequences in southern China[J]. Geophysical Journal International, 2010, 181(3): 1395-1410.
[46] 刘秀铭,夏敦胜,刘东生,等. 中国黄土和阿拉斯加黄土磁化率气候记录的两种模式探讨[J]. 第四纪研究,2007,27（2）：210-220.

Liu Xiuming, Xia Tungsheng, Liu Tungsheng, et al. Discussion on two models of paleoclimatic records of magnetic susceptibility of Alaskan and Chinese loess[J]. Quaternary Sciences, 2007, 27(2): 210-220.
[47] 陈梓炫,吕镔,郑兴芬,等. 基于漫反射光谱和色度的土壤中赤铁矿和针铁矿半定量探讨[J]. 土壤,2020,52（5）：1083-1091.

Chen Zixuan, Bin Lü, Zheng Xingfen, et al. Semi-quantitative study on hematite and goethite in soils based on diffuse reflectance spectrum and chroma[J]. Soils, 2020, 52(5): 1083-1091.
[48] 李徐生,杨达源,鹿化煜. 皖南风尘堆积序列氧化物地球化学特征与古气候记录[J]. 海洋地质与第四纪地质,1999,19（4）：75-82.

Li Xusheng, Yang Dayuan, Lu Huayu. Oxide-geochemistry features and paleoclimatic record of the aeolian-dust depositional sequence in southern Anhui[J]. Marine Geology & Quaternary Geology, 1999, 19(4): 75-82.
[49] 龙进. 庐山WJ剖面第四纪网纹红土特征及其古气候意义初探[D]. 南昌：江西师范大学,2015.

Long Jin. A preliminary study on characteristics of the Quaternary vermicular red clay and its paleoclimate significance from WJ section in Lushan area[D]. Nanchang: Jiangxi Normal University, 2015.
[50] Hu X F, Wei J, Yan D, et al. Regional distribution of the Quaternary red clay with aeolian dust characteristics in subtropical China and its paleoclimatic implications[J]. Geoderma, 2010, 159(3/4): 317-334.
[51] 尹秋珍,郭正堂. 中国南方的网纹红土与东亚季风的异常强盛期[J]. 科学通报,2006,51（2）：186-193.

Yin Qiuzhen, Guo Zhengtang. Mid-Pleistocene vermiculated red soils in southern China as an indication of unusually strengthened East Asian monsoon[J]. Chinese Science Bulletin, 2006, 51(2): 186-193.
[52] 谢树成,易轶,刘育燕,等. 中国南方更新世网纹红土对全球气候变化的响应：分子化石记录[J]. 中国科学（D辑）：地球科学,2003,33（5）：411-417.

Xie Shucheng, Yi Yi, Liu Yuyan, et al. The Pleistocene vermicular red earth in South China signaling the global climatic change: The molecular fossil record[J]. Science China (Seri. D): Earth Sciences, 2003, 33(5): 411-417.
[53] 来红州,莫多闻,李新坡. 洞庭盆地红土地层中网纹的成因探讨[J]. 北京大学学报（自然科学版）,2005,41（2）：240-248.

Lai Hongzhou, Mo Duowen, Li Xinpo. Genesis of reticulate clay in the laterite of the Dongting Basin[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2005, 41(2): 240-248.
[54] 王琳怡,朱丽东,于红梅,等. 加积型红土剖面成壤特征及网纹化成因的土壤微形态证据[J]. 土壤学报,2022,59（5）：1306-1320.

Wang Linyi, Zhu Lidong, Yu Hongmei, et al. Micromorphological evidence on the pedogenic characteristics and reticulated mechanism of aggradation red earth[J]. Acta Pedologica Sinica, 2022,59(5)：1306-1320.
[55] Vepraskas M J. Redoximorphic features for identifying aquic conditions[J]. North Carolina Agricultural Research Service. Technical Bulletin, 1994, 64:301.
[56] 郭海珊. 红色风化壳形成过程中铁的地球化学行为研究：以粤北地区为例[D]. 广州：华南师范大学,2014.

Guo Haishan. The geochemistry behavior of iron in the formation of red weathering crust: Take northern Guangdong as an example[D]. Guangzhou: South China Normal University, 2014.
[57] Chen C M, Barcellos D, Richter D D, et al. Redoximorphic Bt horizons of the Calhoun CZO soils exhibit depth-dependent iron-oxide crystallinity[J]. Journal of Soils and Sediments, 2019, 19(2): 785-797.
[58] 洪祎君. 中国南方网纹红土的形成机制及网纹成熟度研究[D]. 南昌：江西师范大学,2015.

Hong Yijun. Research on the formation mechanism of reticulated red clay and growth of reticulated mottles[D]. Nanchang: Jiangxi Normal University, 2015.
[59] Peterschmitt E, Fritsch E, Rajot J L, et al. Yellowing, bleaching and ferritisation processes in soil mantle of the western Ghaˆts, South India[J]. Geoderma, 1996, 74(3/4): 235-253.
[60] 张中彬,彭新华. 土壤裂隙及其优先流研究进展[J]. 土壤学报,2015,52（3）：477-488.

Zhang Zhongbin, Peng Xinhua. A review of researches on soil cracks and their impacts on preferential flow[J]. Acta Pedologica Sinica, 2015, 52(3): 477-488.
[61] 杨立辉,叶玮,朱丽东,等. 第四纪加积型红土与黄土的风成相似性探讨[J]. 干旱区地理,2008,31（3）：341-347.

Yang Lihui, Ye Wei, Zhu Lidong, et al. Aeolian-genesis comparability of aggraded red earth in South China with loess in North China[J]. Arid Land Geography, 2008, 31(3): 341-347.