[1] An Zhisheng, Port S C, Wu Xihao, 1993. The variation of East Asian summer monsoon in Holocene optimum in middle and eastern China. Chinese Science Bulletin, 38(14): 1302–1305. (in Chinese)
[2] Bi Fuzhi, Yuan Youshen, 1987. A preliminary study on the periods of coastal elevation and subsidence along the southeast coast of China in the past 5000 years or more. Science in China (Series B), (4): 429–440. (in Chinese)
[3] Bird E, 2005. Eolianite. In: Maurice L Schwartz. Encyclopedia of Coastal Science 5. Berlin: Springer-Verlag, 426–428.
[4] Blay C T, Longman M W, 2001. Stratigraphy and sedimentology of Pleistocene and Holocene carbonates, Kaua’I, Hawai’I, USA. In: Abegg F E, Harris P, Loop D B. Moden and Ancient Carbonate Eolianites: Sedimentology, Sequence Stratigraphy, and Diagenesis. SEPM Special Publication No.71, 93–115.
[5] Brooke B, 2001. The distribution of carbonate eolianite. Earth-Science Reviews, 55(1): 135–164. Cao Jiaxin 1983. Quaternary Geology. Beijing: The Commercial Press. (in Chinese)
[6] Curran H A, White B, 2001. Ichnology of Holocene carbonate eolianites of the Bahamas. In: Abegg F E, Harris P, Loop D B. Modern and Ancient Carbonate Eolianites: Sedimentology, Sequence Stratigraphy, and Diagenesis. SEPM Special Publication No.71. 47–56.
[7] Fairbridge R W, Johnson, D L, 1978. Eolianite. In: Fairbridge R W, Bourgeios J. The Encyclopedia of Sedimentology. Stroudsburg, Pennsylvania: Dowden, Hutchinson and Ross, 279–293.
[8] Gardner R A M, 1983. Aeolianite. In: Goudie A S, Kenneth P. Chemical Sediments and Geomorphology. London: Academic Press, 265–300.
[9] Hafsten U, 1970. A sub-division of the Late Pleistocene period on a synchronous basis, intended for global and universal usage. Paleogeography, Paleoclimatology, Paleoecology, 7(4): 279–296.
[10] Hong Yetang, Hong Bing, Lin Qinghua et al., 2003. Subtropical high activity of Western Pacific Ocean during the last 5000 years recorded in isotope time series of beat bog. Quaternary Sciences, 23(5): 485–492. (in Chinese)
[11] Huang Zhengguo, Li Pingri, Zhang Zhongying et al., 1982. Zhujiang Delta. Beijing: China Ocean Press, 150–163. (in Chinese)
[12] Kindler P, Davaud E, 2001. Recognizing eolianites in thin section. Review and case study: The lower Cretaceous chambotte formation, Saleve Chain, Southeastern France. In: Abegg F E, Harris P, Loop D B. Modern and anWANG Wei et al.: Coastal dune rock development and Holocene climate changes in South China 479 cient carbonate eolianites: Sedimentology, sequence stratigraphy, and diagenesis. SEPM Special Publication No.71: 141–150.
[13] Li Pingri, 1991. Analysis of Holocene eolian bio-fragment sand-stones on South China coasts and their formation conditions. Acta Oceanologica Sinica, 13(2): 221–229. (in Chinese)
[14] Li Pingri, Qiao Pengnian, Zheng Honghan et al., 1991. The Environment Evolution of the Zhujiang Delta in the last 10000 years. Beijing: China Ocean Press, 1–155. (in Chinese)
[15] Liu Yixuan, Zhu Yuanzhi, Zhuo Jialun, 1987. Discovery of Holocene eolian-deluvium dune rock at Shantou Guangao: Discussion on types of Holocene calci-cemented clasolite along the coast of Southeast China. Tropical Oceanology, 6(4): 1–9. (in Chinese)
[16] Nilsson T, 1983. The Pleistocene: Geology and Life in the Quaternary Ice Age. Stuttart, Germany: Ferdinand Enke Verlag, 526–532.
[17] Pye K, Tsoar H, 1990. Aeolian Sand and Sand Dunes. London: Uniwin Hyman, 274-284. Scoffin T P, Stoddart D R, 1983. Beach rock and intertidal cements. In: Goudie A S, Kenneth P. Chemical Sediments and Geomorphology. London: Academic Press, 401–425.
[18] Shi Yafeng, 1992. The Climate and Environment in the Megathermal. Beijing: Ocean Press, 1–211. (in Chinese)
[19] Wang Jianhua, 1997. Characteristics of dune rocks in the South China coast and their differences from beach rocks. Acta Sedimentologica Sinica, 15(1): 104–110. (in Chinese)
[20] Wang Jianhua, Ye Erkang, 1990. A discussion on some characteristics of Holocene carbonate cemented rocks along the coasts from southeastern Fujian to eastern Guangdong. Guangdong Geology, 5(1): 69–77. (in Chinese)
[21] Wang Shaowu, Gong Daoyi, 2000. Climate in China during the four special periods in Holocene. Progress in Natural Science, 10(4): 325–332. (in Chinese)
[22] Wang Ying, Zhu Dakui, 1987. An approach on the formation causes of coastal sand dunes. Journal of Desert Research, 7(3): 30–40. (in Chinese)
[23] Wen Xiaosheng, Peng Zhicheng, Zhao Huanting, 1994. Advance in study on the Holocene climate evolution in China. Advance in Earth Sciences, 14 (3): 292–298. (in Chinese)
[24] Wright H E Jr, 1976. The dynamic nature of Holocene vegetation, a problem in paleoclimatology, biogeography and stratigraphic nomenclature. Quaternary Research, 6: 581–596.
[25] Wu Zheng, 1985. Sea level changes since the Late Pleistocene in the north of The South China Sea. Tropical Geomorphology, 6 (2): 8–18. (in Chinese)
[26] Wu Zheng, 1995. Research on the Landforms of the Wind-drift Sand on South China Coast. Beijing: Science Press. (in Chinese)
[27] Wu Zheng, Feng Wenke, Liao Bingliang, 1993. Paleogeographic study in the continental shelf of the northern South China Sea during the last stage of the Late Pleistocene. Acta Geographica Sinica, 48(6): 491–496. (in Chinese)
[28] Wu Zheng, Liao Bingliang, Jin Zhimin et al., 1992. The sand surface structure of remnant deposits on the continental shelf in the north of the South China Sea and its environmental significance. Chinese Science Bulletin, 37(20): 1887–1889. (in Chinese)
[29] Wu Zheng, Wang Wei, 1990. The characteristics and the development model of dune rocks on South China coasts. Quaternary Sciences, 4: 334–343. (in Chinese)
[30] Wu Zheng, Wu Kegang, 1987. Sedimentary structure and developing model of coastal dunes along the northeastern coast of Hainan Island, China. Acta Geographica Sinica, 42(2): 129–141. (in Chinese)
[31] Xie Zaituan, Chen Feng, Liu Weikun et al., 1993. Fujian Holocene beach rock and the sea level changes. Taiwan Strait, 2(1): 61–69. (in Chinese)
[32] Xu Hai, 2001. Advance in research on the Holocene climate fluctuations. Geology-Geochemistry, 29(2): 9–16. (in Chinese)
[33] Xu Qihao, Feng Yanji, 1992. Effect of newer and older carbonate 14C dates and possible real ages of dune rocks on Shidao Island, Xisha Archipelago. Scientia Geologica Sinica, (suppl.): 286–294. (in Chinese)
[34] Xu Qihao, Peng Chengguang, Wang Yexin et al., 1987. A preliminary study on the Holocene dune rock in Dahao Peninsula, Guangdong. Tropical Geography, 7(1): 32–42. (in Chinese)
[35] Yang Huairen, 1987. Quaternary Geology. Beijing: Higher Education Press. (in Chinese) Ye Zhizheng, He Qixiang, Zhang Mingshu, 1985. The sedimentary structures and the facies model of the Late Pleistocene eolian biocalcarenites on Shidao Island of Xisha Archipelago. Acta Sedimentologica Sinica, 3(1): 1–15. (in Chinese)
[36] Ye Zhizheng, Zhang Bingshu, Han Ruichun et al., 1984. A new discovery on Shidao Island of Xisha Archipelago: Eolianite (eolian calcarenite) and fossil soils. Marine Geology and Quaternary Geology, 4(1): 1–10. (in Chinese)
[37] Yokohama, 1988. Climate change and ancient civilization before 3500 years. Geographic Translation, (4): 37–44. (in Chinese)
[38] Zhang Jingwen, Li Guiying, Zhao Xitao, 1982. Chronological study on the late Quaternary stratigraphy and neotectonic movement along the coastal area of south Fujian and east Guangdong. Seismology and Geology, 4(3): 27–36. (in Chinese)
[39] Zhang Zhongying, Liu Ruihua, 1987. The Holocene along the coast of Hainan Island. Scientia Geographica Sinica, 7(2): 129–138. (in Chinese)
[40] Zhao Xitao, Sha Qingan, Goldsmith V et al., 1988. Carbonate eolianites in Putian, Fujian (I): Sedimentary structures and paleowinds. Science in China (Series B), (11): 1196–1205. (in Chinese)
[41] Zheng Zhuo, Wang Jianghua, Wang Bing, 2003. High-resolution records of Holocene from the Shuangchi Maar Lake in Hainan Island. Chinese Science Bulletin, 48(3): 282–286. (in Chinese)
[42] Zhu Yuanzhi, Zhong Jinliang. A preliminary study on the dune rock of Shidao Island, Xisha Islands and Hainan Island. Tropical Oceanology, 1984, 3(3): 64–72. (in Chinese)
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