[1] Retallack G J. Soils and global change in the carbon cycle over geological time[M]//Holland H D, Turekian K K. Treatise on geochemistry. Amsterdam: Elsevier Science, 2003: 581-605.
[2] Li X H, Xu W L, Liu W H, et al. Climatic and environmental indications of carbon and oxygen isotopes from the Lower Cretaceous calcrete and lacustrine carbonates in Southeast and Northwest China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 385:171-189. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=2772fb8867f4ddacdbd6040559f67162
[3] 刘东生.黄土与环境[M].北京:科学出版社, 1985.

Liu Tungsheng. Loess and the environment[M]. Beijing:Science Press, 1985.
[4]

An Z S. Late Cenozoic climate change in Asia:Loess, monsoon and monsoon-arid environment evolution[M]. Dordrecht:Springer, 2014.
[5] 胡泉旭, 王先彦, 孟先强, 等.青藏高原东北部黄土次生碳酸盐氧同位素的古气候意义[J].地球科学, 2018, 43(11):4128-4137. http://d.old.wanfangdata.com.cn/Periodical/dqkx201811028

Hu Quanxu, Wang Xianyan, Meng Xianqiang, et al. Paleoclimatic implications of oxygen isotope from Authigenic carbonates in loess deposit of northeastern Tibetan Plateau[J]. Earth Science, 2018, 43(11):4128-4137. http://d.old.wanfangdata.com.cn/Periodical/dqkx201811028
[6] 侯战方, 张军, 宋春晖, 等.青藏高原天水盆地中新世沉积物碳氧同位素对古气候演化的指示[J].海洋地质与第四纪地质, 2011, 31(3):69-78. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201103009

Hou Zhanfang, Zhang Jun, Song Chunhui, et al. The oxygen and carbon isotopic records of Miocene sediments in the Tianshui Basin of the northestern Tibetan Plateau and their paleoclimatic implications[J]. Marine Geology & Quaternary Geology, 2011, 31(3):69-78. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201103009
[7] 李林, 周锡强, 黄永建, 等.色度学方法的深时研究:以藏南贡扎剖面白垩系赛诺曼/土仑阶为例[J].地学前缘, 2009, 16(5):153-159. doi:  10.3321/j.issn:1005-2321.2009.05.015

Li Lin, Zhou Xiqiang, Huang Yongjian, et al. The deep-time research by chromatometry:An example from the Cenomanian to Turonian Stages of the Cretaceous, Gongza section, Southern Tibet[J]. Earth Science Frontiers, 2009, 16(5):153-159. doi:  10.3321/j.issn:1005-2321.2009.05.015
[8] 陈杰, 杨太保, 曾彪, 等.中国帕米尔地区黄土上部色度变化特征及古气候意义[J].沉积学报, 2018, 36(2):333-342. http://www.cjxb.ac.cn/CN/abstract/abstract3869.shtml

Chen Jie, Yang Taibao, Zeng Biao, et al. Chroma characteristics and its paleoclimatic significance in Pamir Loess Section, China[J]. Acta Sedimentologica Sinica, 2018, 36(2):333-342. http://www.cjxb.ac.cn/CN/abstract/abstract3869.shtml
[9] 丁敏, 庞奖励, 黄春长, 等.全新世黄土-古土壤序列色度特征及气候意义:以关中平原西部梁村剖面为例[J].陕西师范大学学报(自然科学版), 2010, 38(5):92-97. http://d.old.wanfangdata.com.cn/Periodical/sxsfdxxb201005022

Ding Min, Pang Jiangli, Huang Chunchang, et al. Chroma characteristics and its climatic significance in Holocene loess-paleosol sequence:A case study of the Holocene Liangcun profile in the western Guanzhong Basin[J]. Journal of Shaanxi Normal University(Natural Science Edition), 2010, 38(5):92-97. http://d.old.wanfangdata.com.cn/Periodical/sxsfdxxb201005022
[10] 高鹏坤, 庞奖励, 黄春长, 等.陕南丹凤茶房村黄土-古土壤剖面色度参数特征[J].沉积学报, 2015, 33(3):537-542. http://www.cjxb.ac.cn/CN/abstract/abstract3537.shtml

Gao Pengkun, Pang Jiangli, Huang Chunchang, et al. Chroma characteristics and its significances of the Chafangcun loesspaleosol profile in Southeast Shaanxi, China[J]. Acta Sedimentologica Sinica, 2015, 33(3):537-542. http://www.cjxb.ac.cn/CN/abstract/abstract3537.shtml
[11]

Du X B, Xie X N, Lu Y C, et al. Distribution of continental red paleosols and their forming mechanisms in the Late Cretaceous Yaojia Formation of the Songliao Basin, NE China[J]. Cretaceous Research, 2011, 32(2):244-257. doi:  10.1016/j.cretres.2010.12.010
[12]

Huang C M, Retallack G J, Wang C S, et al. Paleoatmospheric pCO2 fluctuations across the Cretaceous-Tertiary boundary recorded from paleosol carbonates in NE China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 385:95-105. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=9a1c61b9449faf40ed20ad30c7980bfa
[13]

Gao Y, Ibarra D E, Wang C S, et al. Mid-latitude terrestrial climate of East Asia linked to global climate in the Late Cretaceous[J]. Geology, 2015, 43(4):287-290. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=76eb37d83453e62873609e61b906d417
[14] 曹珂.胶莱盆地晚白垩世辛格庄组钙质结核的碳、氧同位素特征[J].矿物岩石, 2014, 34(2):85-90. http://d.old.wanfangdata.com.cn/Periodical/kwys201402013

Cao Ke. Carbon and oxygen isotopic compositions of carbon nodule in the Xingezhuang Formation of Late Cretaceous, Jiaozhou-Laiyang Basin[J]. Journal of Mineralogy and Petrology, 2014, 34(2):85-90. http://d.old.wanfangdata.com.cn/Periodical/kwys201402013
[15]

Zhang L M, Wang C S, Cao K, et al. High elevation of Jiaolai Basin during the Late Cretaceous:Implication for the coastal mountains along the East Asian margin[J]. Earth and Planetary Science Letters, 2016, 456:112-123. http://cn.bing.com/academic/profile?id=5b2ba092cb14de23806712892c9315fe&encoded=0&v=paper_preview&mkt=zh-cn
[16]

Huang C M, Retallack G J, Wang C S. Early Cretaceous atmospheric pCO2 levels recorded from pedogenic carbonates in China[J]. Cretaceous Research, 2012, 33(1):42-49. doi:  10.1016/j.cretres.2011.08.001
[17]

Li J, Wen X Y, Huang C M. Lower Cretaceous paleosols and paleoclimate in Sichuan Basin, China[J]. Cretaceous Research, 2016, 62:154-171. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=b601a9f38e4f082d04c3c3d839d5c681
[18] 李祥辉, 陈斯盾, 曹珂, 等.浙闽地区白垩纪中期古土壤类型与古气候[J].地学前缘, 2009, 16(5):63-70. doi:  10.3321/j.issn:1005-2321.2009.05.006

Li Xianghui, Chen Sidun, Cao Ke, et al. Paleosols of the mid-Cretaceous:A report from Zhejiang and Fujian, SE China[J]. Earth Science Frontiers, 2009, 16(5):63-70. doi:  10.3321/j.issn:1005-2321.2009.05.006
[19] 刘秀铭, 吕镔, 毛学刚, 等.风积地层中铁矿物随环境变化及其启示[J].第四纪研究, 2014, 34(3):443-457. doi:  10.3969/j.issn.1001-7410.2014.03.01

Liu Xiu-ming, Lü Bin, Mao Xuegang, et al. Iron minerals of aeolian deposits vary with environment and its significances[J]. Quaternary Sciences, 2014, 34(3):443-457. doi:  10.3969/j.issn.1001-7410.2014.03.01
[20] 温昌辉.江西石城盆地白垩纪红色地层中成壤特征及古环境分析[D].福州: 福建师范大学, 2016.

Wen Changhui. The Cretaceous stratum: Pedogenesis recognition and paleoenvironmental analysis, in Shicheng Basin, Jiangxi province[D]. Fuzhou: Fujian Normal University, 2016.
[21] 江西省地质矿产局.江西省岩石地层[M].武汉:中国地质大学出版社, 2008.

Bureau of Geology and Mineral Resources Jiangxi Provincial. Lithostratigraphy in Jiangxi province[M]. Wuhan:China University of Geosciences Press, 2008.
[22]

Chen L Q, Guo F S, Steel R J, et al. Petrography and geochemistry of the Late Cretaceous redbeds in the Gan-Hang Belt, southeast China:Implications for provenance, source weathering, and tectonic setting[J]. International Geology Review, 2016, 58(10):1196-1214. doi:  10.1080/00206814.2016.1141378
[23]

Chen L Q, Steel R J, Guo F S, et al. Alluvial fan facies of the Yongchong Basin:Implications for tectonic and paleoclimatic changes during Late Cretaceous in SE China[J]. Journal of Asian Earth Sciences, 2017, 134:37-54.
[24] 陈留勤, 刘鑫, 李鹏程.古土壤:沉积环境和古气候变化的灵敏指针[J].沉积学报, 2018, 36(3):510-520. http://www.cjxb.ac.cn/CN/abstract/abstract3883.shtml

Chen Liuqin, Liu Xin, Li Pengcheng. Paleosols:Sensitive indicators of depositional environments and paleoclimate[J]. Acta Sedimentologica Sinica, 2018, 36(3):510-520. http://www.cjxb.ac.cn/CN/abstract/abstract3883.shtml
[25] 王凤之, 陈留勤, 郭福生, 等.江西信江盆地晚白垩世塘边组成壤碳酸盐岩碳、氧同位素特征[J].岩石矿物学杂志, 2018, 37(1):143-151. doi:  10.3969/j.issn.1000-6524.2018.01.012

Wang Fengzhi, Chen Liuqin, Guo Fusheng, et al. Carbon and oxygen isotopic compositions of pedogenic carbonates from the Late Cretaceous Tangbian Formation in the Xinjiang Basin, Jiangxi province[J]. Acta Petrologica et Mineralogica, 2018, 37(1):143-151. doi:  10.3969/j.issn.1000-6524.2018.01.012
[26] 刘细元, 衷存堤, 张永忠, 等.江西省晚白垩世周田组的再划分[J].地质调查与研究, 2004, 27(4):217-222. doi:  10.3969/j.issn.1672-4135.2004.04.002

Liu Xiyuan, Zhong Cundi, Zhang Yongzhong, et al. Redefinition of the Late Cretaceous Zhoutian Formation, Jiangxi province[J]. Geological Survey and Research, 2004, 27(4):217-222. doi:  10.3969/j.issn.1672-4135.2004.04.002
[27] 肖光荣, 姚琪, 范爱春.江西省晚白垩世层序地层研究[J].资源调查与环境, 2013, 34(3):141-149. doi:  10.3969/j.issn.1671-4814.2013.03.001

Xiao Guangrong, Yao Qi, Fan Aichun. Research on sequence stratigraphy of Late Cretaceous in Jiangxi province[J]. Resources Survey & Environment, 2013, 34(3):141-149. doi:  10.3969/j.issn.1671-4814.2013.03.001
[28] 邓家瑞, 张志平.赣杭构造带及其地质意义[J].铀矿地质, 1989, 5(1):15-21. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201503009

Deng Jiarui, Zhang Zhiping. Gan-Hang tectonic belt and its geologic significance[J]. Uranium Geology, 1989, 5(1):15-21. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201503009
[29] 余心起, 舒良树, 颜铁增, 等.赣杭构造带红层盆地原型及其沉积作用[J].沉积学报, 2005, 23(1):12-20. doi:  10.3969/j.issn.1000-0550.2005.01.002

Yu Xinqi, Shu Liangshu, Yan Tiezeng, et al. Prototype and sedimentation of red basins along the Ganhang tectonic belt[J]. Acta Sedimentologica Sinica, 2005, 23(1):12-20. doi:  10.3969/j.issn.1000-0550.2005.01.002
[30] 余达淦, 叶发旺, 王勇.江西广丰早白垩世中晚期盆地火山-侵入杂岩活动序列确认及地质意义[J].大地构造与成矿学, 2001, 25(3):271-276. doi:  10.3969/j.issn.1001-1552.2001.03.008

Yu Dagan, Ye Fawang, Wang Yong. Active succession establishment for volcanic-intrusive complex in Middle-Late Lower Cretaceous in Guangfeng, Jiangxi and its geological implication[J]. Geotectonic et Metallogenia, 2001, 25(3):271-276. doi:  10.3969/j.issn.1001-1552.2001.03.008
[31] 姜勇彪, 郭福生, 刘林清, 等.广丰盆地白垩纪红层及其地貌景观发育研究[J].资源调查与环境, 2009, 30(4):235-242. doi:  10.3969/j.issn.1671-4814.2009.04.001

Jiang Yongbiao, Guo Fusheng, Liu Linqing, et al. A study on Cretaceous red beds and their geomorphologic landscapes in Guangfeng Basin[J]. Resources Survey & Environment, 2009, 30(4):235-242. doi:  10.3969/j.issn.1671-4814.2009.04.001
[32] 衷存堤, 徐平, 肖晓林, 等.对江西晚白垩世赣州群茅店组的重新厘定[J].中国地质, 2002, 29(3):271-274. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi200203006

Zhong Cundi, Xu Ping, Xiao Xiaolin, et al. Revision of the Late Cretaceous Maodian Formation of the Ganzhou Group in Jiangxi province[J]. Geology in China, 2002, 29(3):271-274. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi200203006
[33] 巫建华, 项媛馨, 钟志菲.江西广丰、玉山盆地橄榄玄粗岩的SHRIMP锆石U-Pb定年和Sr-Nd-Pb-O元素同位素特征[J].岩石矿物学杂志, 2014, 33(4):645-656. doi:  10.3969/j.issn.1000-6524.2014.04.004

Wu Jianhua, Xiang Yuanxin, Zhong Zhifei. SHRIMP zircon U-Pb dating and SrNd-Pb-O isotope characteristics of shoshonite from Guangfeng and Yushan Basins in Jiangxi province[J]. Acta Petrologica et Mineralogica, 2014, 33(4):645-656. doi:  10.3969/j.issn.1000-6524.2014.04.004
[34] 曹珂.中国陆相白垩系地层对比[J].地质论评, 2013, 59(1):24-40. doi:  10.3969/j.issn.0371-5736.2013.01.004

Cao Ke. Cretaceous terrestrial stratigraphic correlation in China[J]. Geological Review, 2013, 59(1):24-40. doi:  10.3969/j.issn.0371-5736.2013.01.004
[35] 周涛, 巫建华, 艾成辉.江西广丰碱性橄榄玄武岩的成因:SHRIMP锆石U-Pb年龄和元素、Sr-Nd-Pb同位素制约[J].东华理工大学学报(自然科学版), 2016, 39(2):108-117. doi:  10.3969/j.issn.1674-3504.2016.02.002

Zhou Tao, Wu Jianhua, Ai Chenghui. Petrogenesis of alkali olivine basalt from Guangfeng Basins in Jiangxi province:SHRIMP zircon U-Pb Dating and element、Sr-Nd-Pb isotope constraints[J]. Journal of East China University of Technology, 2016, 39(2):108-117. doi:  10.3969/j.issn.1674-3504.2016.02.002
[36] 杨胜利, 方小敏, 李吉均, 等.表土颜色和气候定性至半定量关系研究[J].中国科学(D辑):地球科学, 2001, 31(增刊1):175-181.

Yang Shengli, Fang Xiaomin, Li Jijun, et al. Transformation functions of soil color and climate[J]. Science China (Seri. D):Earth Sciences, 2001, 31(Suppl. 1):175-181.
[37] 何柳, 孙有斌, 安芷生.中国黄土颜色变化的控制因素和古气候意义[J].地球化学, 2010, 39(5):447-455. http://d.old.wanfangdata.com.cn/Periodical/dqhx201005005

He Liu, Sun Youbin, An Zhisheng. Changing color of Chinese loess:Controlling factors and paleocliamtic significances[J]. Geochimica, 2010, 39(5):447-455. http://d.old.wanfangdata.com.cn/Periodical/dqhx201005005
[38] 石培宏, 杨太保, 田庆春, 等.靖远黄土-古土壤色度变化特征分析及古气候意义[J].兰州大学学报(自然科学版), 2012, 48(2):15-23. doi:  10.3969/j.issn.0455-2059.2012.02.004

Shi Peihong, Yang Taibao, Tian Qingchun, et al. Chroma chracteristics in the loess-paleosol at Jingyuan section and its signification to paleocliamete[J]. Journal of Lanzhou University(Natural Sciences), 2012, 48(2):15-23. doi:  10.3969/j.issn.0455-2059.2012.02.004
[39] 赵景波.风化淋滤带地质新理论-CaCO3淀积深度理论[J].沉积学报, 2000, 18(1):29-35. doi:  10.3969/j.issn.1000-0550.2000.01.006

Zhao Jingbo. A new geological theory about eluvial zone-theory illuvial on depth of CaCO3[J]. Acta Sedimentologica Sinica, 2000, 18(1):29-35. doi:  10.3969/j.issn.1000-0550.2000.01.006
[40]

Sun Y B, He L, Liang L J, et al. Changing color of Chinese loess:Geochemical constraint and paleoclimatic significance[J]. Journal of Asian Earth Sciences, 2011, 40(6):1131-1138. doi:  10.1016/j.jseaes.2010.08.006
[41]

Torrent J, Barrón V, Liu Q S. Magnetic enhancement is linked to and precedes hematite formation in aerobic soil[J]. Geophysical Research Letters, 2006, 33(2):L02401. doi:  10.1029-2005GL024818/
[42]

Deaton B C, Balsam W L. Visible spectroscopy:A rapid method for determining hematite and goethite concentration in geological materials[J]. Journal of Sedimentary Research, 1991, 61(4):628-632. doi:  10.1306/D4267794-2B26-11D7-8648000102C1865D
[43]

Ji J F, Balsam W, Chen J. Mineralogic and climatic interpretations of the Luochuan loess section(China)based on diffuse reflectance spectrophotometry[J]. Quaternary Research, 2001, 56(1):23-30.
[44] 何同.黄土高原晚中新世-上新世红粘土碳酸盐地球化学研究[D].南京: 南京大学, 2012.

He Tong. Geochemistry of carbonates in the Late Miocene-Pliocene red clay deposits on Chinese Loess Plateau[D]. Nanjing: Nanjing University, 2012.
[45] 刘秀铭, 刘东生, Heller F, 等.中国黄土磁化率与第四纪古气候研究[J].地质科学, 1992(增刊1):279-285.

Liu Xiuming, Liu Tungsheng, Heller F, et al. Study on magnetic susceptibility of Loess and Quaternary climate in China[J]. Scientia Geologica Sinica, 1992(Suppl. 1):279-285.
[46] 王文艳.南雄盆地大塘剖面红色地层的磁化率变化机制及其古气候意义[D].福州: 福建师范大学, 2017.

Wang Wenyan. Magnetic susceptibility change mechanism in Datang, Nanxiong Basin and its paleoclimate significances[D]. Fuzhou: Fujian Normal University, 2017.
[47] 张蕊.黄土-红粘土磁学参数记录的晚新生代东亚季风气候演化[D].兰州: 兰州大学, 2017.

Zhang Rui. Late Cenozoic East Asian monsoon climate variations recorded by loess-red clay magnetic parameters on the Chinese Loess Plateau[D]. Lanzhou: Lanzhou University, 2017.
[48] 陈海霞.川西雅安地区白垩纪古环境古气候研究[D].成都: 成都理工大学, 2009.

Chen Haixia. Research of paleoenvironment and paleoclimate of Cretaceous in Ya'an area of western Sichuan Basin[D]. Chengdu: Chengdu University of Technology, 2009.
[49] 王尹, 李祥辉, 周勇, 等.南雄盆地晚白垩世-古新世陆源沉积组份变化的古气候指示[J].沉积学报, 2015, 33(1):116-123. http://www.cjxb.ac.cn/CN/abstract/abstract3496.shtml

Wang Yin, Li Xianghui, Zhou Yong, et al. Paleoclimate indication of terrigenous clastic rock's component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1):116-123. http://www.cjxb.ac.cn/CN/abstract/abstract3496.shtml
[50] 陈留勤.江西永崇盆地晚白垩世沉积演化[M].北京:地质出版社, 2018.

Chen Liuqin. Depositional evolution of the Yongchong Basin during Late Cretaceous in Jiangxi province, SE China[M]. Beijing:Geological Publishing House, 2018.
[51]

Mills H H. Downstream rounding of pebbles:A quantitative review[J]. Journal of Sedimentary Research, 1979, 49(1):295-303. http://cn.bing.com/academic/profile?id=ffd005c6f7831c8b7f4c4cfe8741cf6f&encoded=0&v=paper_preview&mkt=zh-cn
[52]

Nemec W, Postma G. Quaternary alluvial fans in southwestern Crete: Sedimentation processes and geomorphic evolution[M]//Marzo M, Puigdefábregas C. Blackwell: Oxford. Alluvial sedimentation. IAS Special Publication, 1993: 235-276.
[53] 刘鑫, 陈留勤, 李馨敏, 等.江西象山地质公园丹霞地貌成景地层沉积环境分析[J].现代地质, 2018, 32(2):260-269. http://d.old.wanfangdata.com.cn/Periodical/xddz201802005

Liu Xin, Chen Liuqin, Li Xinmin, et al. Depositional environments of the bedrock of Danxia Landform in Xiangshan Geopark of Jiangxi province, SE China[J]. Geoscience, 2018, 32(2):260-269. http://d.old.wanfangdata.com.cn/Periodical/xddz201802005
[54]

Buck B J, Mack G H. Latest Cretaceous(Maastrichtian)aridity indicated by paleosols in the McRae Formation, south-central New Mexico[J]. Cretaceous Research, 1995, 16(5):559-572. doi:  10.1006/cres.1995.1036
[55]

Burgener L, Hyland E, Huntington K W, et al. Revisiting the equable climate problem during the Late Cretaceous greenhouse using paleosol carbonate clumped isotope temperatures from the Campanian of the western Interior Basin, USA[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2019, 516:244-267. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=9ddc2e2a0a52f681bbc84140b928db7d