1 Jian Z M, Wang P X, Saito Y et al. Holocene variability of the Kuroshio Current in the Okinawa Trough, Northwestern Pacific Ocean. Earth and Planetary Science Letters, 2000, 184 (1):305~319
[2]
2 窦衍光, 杨守业, 唐 珉等. 冲绳海槽中部28ka以来陆源物质输入和古环境演化的生源组分记录. 第四纪研究, 2011, 31 (2):236~243 Dou Yanguang, Yang Shouye, Tang Min et al. Using biogenic components to decipher the terrigenous input and paleoenvironmental changes over the last 28ka in the Middle Okinawa Trough. Quaternary Sciences, 2011, 31 (2):236~243
[3]
3 杨永亮, 刘振夏, 沈承德等. 末次冰期及全新世冲绳海槽东部 Z14-6孔的 10 Be记录. 第四纪研究, 2012, 32 (3):417~422 Yang Yongliang, Liu Zhenxia, Shen Chengde et al.10 Be isotope records in sediment core Z14-6 from the Eastern Okinawa Trough during the Last Deglaciation and Holocene. Quaternary Sciences, 2012, 32 (3):417~422
[4]
4 郑旭峰, 李安春, 万世明等. 冲绳海槽中全新世的浊流沉积及其控制因素. 第四纪研究, 2014, 34 (3):579~589 Zheng Xufeng, Li Anchun, Wan Shiming et al. The turbidity events in Okinawa Trough during Middle Holocene and its potential dominating mechanisms. Quaternary Sciences, 2014, 34 (3):579~589
[5]
5 苍树溪, 阎 军. 西太平洋特定海域古海洋学. 青岛: 青岛海洋大学出版社, 1992. 1~172 Cang Shuxi, Yan Jun. Paleoceanography of Special Areas in Western Pacific Ocean. Qingdao:Qingdao Ocean University Press, 1992. 1~172
[6]
6 Li T, Liu Z, Hall M A et al. Heinrich event imprints in the Okinawa Trough:Evidence from oxygen isotope and planktonic foraminifera. Palaeogeography, Palaeoclimatology, Palaeoecology, 2001, 176 (1):133~146
[7]
7 Li Baohua, Jian Zhimin, Wang Pinxian. Pulleniatina obliquiloculata as a paleoceanographic indicator in the Southern Okinawa Trough during the last 20
[8]
00 0 years. Marine Micropaleontology, 1997, 32 (1):59~69
[9]
8 Dadson S J, Hovius N, Chen H et al. Links between erosion, runoff variability and seismicity in the Taiwan orogen. Nature, 2003, 426 (6967):648~651
[10]
9 Jeng W L, Lin S, Kao S J. Distribution of terrigenous lipids in marine sediments off northeastern Taiwan. Deep Sea Research Part Ⅱ: Topical Studies in Oceanography, 2003, 50 (6):1179~1201
[11]
10 Liu K K, Peng T H, Shaw P T et al. Circulation and biogeochemical processes in the East China Sea and the vicinity of Taiwan: An overview and a brief synthesis. Deep Sea Research Part Ⅱ: Topical Studies in Oceanography, 2003, 50 (6):1055~1064
[12]
11 Yu K F, Zhao J X, Collerson K D et al. Storm cycles in the last millennium recorded in Yongshu reef, southern South China Sea. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004, 210 (1):89~100
[13]
12 Walsh K J, Ryan B F. Tropical cyclone intensity increase near Australia as a result of climate change. Journal of Climate, 2000, 13 (16):3029~3036
[14]
13 Knutson T R, McBride J L, Chan J et al. Tropical cyclones and climate change. Nature Geoscience, 2010, 3 (3):157~163
[15]
14 Emanuel K. Increasing destructiveness of tropical cyclones over the past 30 years. Nature, 2005, 436 (7051):686~688
[16]
15 Ho C H, Baik J J, Kim J H et al. Interdecadal changes in summertime typhoon tracks. Journal of Climate, 2004, 17 (9):1767~1776
[17]
17 Kao S J, Liu K K. Estimating the suspended sediment load by using the historical hydrometric record from the Lanyang-Hsi watershed. Terrestrial, Atmospheric and Oceanic Sciences, 2001, 12 (2):401~414
[18]
18 Chan J C L. Tropical cyclone activity over the western North Pacific associated with El Ni?o and La Ni?a events. Journal of Climate, 2000, 13 (16):2960~2972
[19]
19 Elsner J B, Liu K B. Examining the ENSO-typhoon hypothesis. Climate Research, 2003, 25 (1):43~54
[20]
20 Lander M A. An exploratory analysis of the relationship between tropical storm formation in the western North Pacific and ENSO. Monthly Weather Review, 1994, 122 (4):636~651
[21]
21 Hendey N I. An Introductory Account of the Smaller Algae of British Coastal Waters. Part Ⅴ:Bacillariophyceae(Diatom). London:Her Majesty''s Stationery Office, 1964. 317
[22]
22 Hasle G R, Syvertsen E E. Marine diatoms. In:Tomas C R ed. Identifying Marine Phytoplankton. San Diego:Academic Press, 1997. 5~385
[23]
23 Chen C, Ruo R, Paid S et al. Exchange of water masses between the East China Sea and the Kuroshio off northeastern Taiwan. Continental Shelf Research, 1995, 15 (1):19~39
[24]
24 Chen C T A. The Three Gorges Dam:Reducing the upwelling and thus productivity in the East China Sea. Geophysical Research Letters, 2000, 27 (3):381~383
[25]
25 Tang T, Hsueh Y, Yang Y et al. Continental slope flow northeast of Taiwan. Journal of Physical Oceanography, 1999, 29 (6):1353~1362
[26]
26 Huh C A, Su C C, Wang C H et al. Sedimentation in the Southern Okinawa Trough——Rates, turbidites and a sediment budget. Marine Geology, 2006, 231 (1~4):129~139
[27]
27 Tang T, Tai J, Yang Y. The flow pattern north of Taiwan and the migration of the Kuroshio. Continental Shelf Research, 2000, 20 (4):349~371
[28]
28 Chen H F, Wen S Y, Song S R et al. Strengthening of paleo-typhoon and autumn rainfall in Taiwan corresponding to the Southern Oscillation at Late Holocene. Journal of Quaternary Science, 2012, 27 (9):964~972
[29]
29 H?kansson H. The recent diatom succession of Lake Havg?rdssj?n, South Sweden. In:Mann D G ed. Proceedings of the Seventh International Diatom Symposium. Koenigstein:Otto Koeltz Science Publishers, 1984. 411~429
[30]
30 Ramsey C B. Deposition models for chronological records. Quaternary Science Reviews, 2008, 27 (1):42~60
[31]
31 Reimer P J, Baillie M G, Bard E et al. IntCal09 and Marine09 radiocarbon age calibration curves, 0~50
[32]
00 0 years cal BP. Radiocarbon, 2009, 51 (4):1111~1150
[33]
32 Li D, Knudsen M F, Jiang H et al. A diatom-based reconstruction of summer sea-surface salinity in the Southern Okinawa Trough, East China Sea, over the last millennium. Journal of Quaternary Science, 2012, 27 (8):771~779
[34]
33 Tomas C R. Identifying Marine Phytoplankton. London:Academic Press, 1997. 6~206
[35]
68 Matsuura T, Yumoto M, Iizuka S et al. Typhoon and ENSO simulation using a high-resolution coupled GCM. Geophysical Research Letters, 1999, 26 (12):1755~1758
[36]
69 Chan J C. Tropical cyclone activity in the Northwest Pacific in relation to the El Ni?o/Southern Oscillation phenomenon. Monthly Weather Review, 1985, 113 (4):599~606
[37]
70 Elsner J B, Liu K. Examining the ENSO-typhoon hypothesis. Climate Research, 2003, 25 (1):43~54
[38]
71 Donnelly J P, Woodruff J D. Intense hurricane activity over the past 5
[39]
00 0 years controlled by El Ni?o and the West African monsoon. Nature, 2007, 447 (7143):465~468
[40]
72 Woodruff J D, Donnelly J P, Emanuel K et al. Assessing sedimentary records of paleohurricane activity using modeled hurricane climatology. Geochemistry, Geophysics, Geosystems, 2008, 9 (9):1~12
[41]
16 侯统昭, 李锦育. 台风灾害之水文因子之探讨——以台北市为例. 亚热带水土保持, 2009, 21 (4):1~9 Hou Tongzhao, Li Jinyu. Study on the hydrological factor in the typhoon hazard of Taipei City. Subtropical Soil and Water Conservation, 2009, 21 (4):1~9
[42]
34 Jousé A P, Kozlova O, Muhina V. Distribution of diatoms in the surface layer of sediment from the Pacific Ocean. In:Funnell B M, Riedel W R Eds. Micropaleontology of Oceans. Cambridge:Cambridge University Press, 1971. 263~269
[43]
35 蒋 辉. 我国某些常见化石硅藻的环境分析. 植物学报, 1987, 29 (4):440~448 Jiang Hui. Environment analysis of the common fossil diatom from the sediments of the China Seas. Acta Botanica Sinica, 1987, 29 (4):440~448
[44]
36 黄元辉, 黄 玥, 蒋 辉. 南海北部15ka BP以来表层海水温度变化: 来自海洋硅藻的记录. 海洋地质与第四纪地质, 2007, 27 (5):65~75 Huang Yuanhui, Huang Yue, Jiang Hui. Surface water temperature changes in the northern South China Sea over last ca .15
37 蒋 辉. 中国近海表层沉积硅藻. 海洋学报, 1987, 9 (6):735~743 Jiang Hui. Diatoms from surface sediment of the China seas. Acta Oceanologica Sinica, 1987, 9 (6):735~743
[47]
38 冉莉华, 蒋 辉. 南海某些表层沉积硅藻的分布及其古环境意义. 微体古生物学报, 2005, 22 (1):97~106 Ran Lihua, Jiang Hui. Distributions of the surface sediment diatoms from the South China Sea and their palaeoceanographic significance. Acta Micropalaeontologica Sinica, 2005, 22 (1):97~106
40 Jiang H, Zheng Y, Ran L et al. Diatoms from the surface sediments of the South China Sea and their relationships to modern hydrography. Marine Micropaleontology, 2004, 53 (3~4):279~292
[50]
41 金德祥. 台湾海峡硅藻类的特点. 台湾海峡, 1982, 1 (1):80~86 Jin Dexiang. Characteristics of diatom of Taiwan Strait. Journal of Oceanography in Taiwan Strait, 1982, 1 (1):80~86
43 蓝东兆, 方 琦, 廖连招. 冲绳海槽表层沉积硅藻对黑潮流的响应. 台湾海峡, 2002, 21 (1):1~5 Lan Dongzhao, Fang Qi, Liao Lianzhao. Surficial sedimentary diatoms in Okinawa Trough and its response to Kuroshio Current. Journal of Oceanography in Taiwan Strait, 2002, 21 (1):1~5
[53]
44 蓝东兆, 许 江, 陈承惠. 冲绳海槽晚第四纪沉积硅藻及其古海洋学意义. 台湾海峡, 2000, 19 (4):419~425 Lan Dongzhao, Xu Jiang, Chen Chenghui. Late Quaternary sedimentary diatom in Okinawa Trough and its paleoceanographical significance. Journal of Oceanography in Taiwan Strait, 2000, 19 (4):419~425
[54]
45 Krammer K, Lange-Bertalot H. Bacillariophyceae 4. Teil:Achnanthaceae, Kritische Erganzungen zu Navicula(Lineolate)und Gomphonema Gesammliteraturverzeichnis. Stuttgart:Gustav Fischer Verlag, 1991. 252~422
[55]
46 Yang Xiangdong, Wang Sumin, Shen Ji et al. Lacustrine environment responses to human activities in the past 300 years in Longgan Lake catchment, Southeast China. Science in China (Series D), 2002, 45 (8):609~718
[56]
47 胡鸿钧. 中国淡水藻类. 上海: 科学技术出版社, 1980. 5~30 Hu Hongjun. Freshwater Diatoms in China. Shanghai:Technology Press, 1980. 5~30
[57]
48 Chen S H, Wu J T, Yang T N et al. Late Holocene paleoenvironmental changes in subtropical Taiwan inferred from pollen and diatoms in lake sediments. Journal of Paleolimnology, 2009, 41 (2):315~327
[58]
49 Hsu S C, Lin F J, Jeng W L et al. Observed sediment fluxes in the Southwesternmost Okinawa Trough enhanced by episodic events:Flood runoff from Taiwan rivers and large earthquakes. Deep Sea Research Part Ⅰ: Oceanographic Research Papers, 2004, 51 (7):979~997
[59]
50 Li Chuanshun, Jiang Bo, Li Anchun et al. Sedimentation rates and provenance analysis in the Southwestern Okinawa Trough since the Mid-Holocene. Chinese Science Bulletin, 2009, 54 (7):1234~1242
[60]
51 Chen C S, Chen Y L. The rainfall characteristics of Taiwan. Monthly Weather Review, 2003, 131 (7):1323~1341
[61]
52 Milliman J D, Kao S J. Hyperpycnal discharge of fluvial sediment to the ocean:Impact of Super-typhoon Herb (1996) on Taiwanese Rivers. The Journal of Geology, 2005, 113 (5):503~516
[62]
53 况雪源, 刘 健, 王红丽等. 近千年来中国区域降水模拟与重建资料的对比分析. 地球科学进展, 2009, 24 (2):159~171 Kuang Xueyuan, Liu Jian, Wang Hongli et al. Comparison of simulated and reconstructed precipitation in China during the last millennium. Advances in Earth Science, 2009, 24 (2):159~171
[63]
54 Liu K B, Shen C, Louie K S. A 1 000-year history of typhoon landfalls in Guangdong, Southern China, reconstructed from Chinese historical documentary records. Annals of the Association of American Geographers, 2001, 91 (3):453~464
[64]
55 朱 芸, 雷国良, 姜修阳等. 晚全新世以来福建仙山泥炭钻孔的正构烷烃记录. 第四纪研究, 2013, 33 (6):1211~1222 Zhu Yun, Lei Guoliang, Jiang Xiuyang et al. Late Holocene origanism records from peat n-alkanes of Xianshan Mountain in Fujian Province, Southeast China. Quaternary Sciences, 2013, 33 (6):1211~1222
[65]
56 Chu G, Liu J, Sun Q et al. The ''Mediaeval Warm Period’ drought recorded in Lake Huguangyan, tropical South China. The Holocene, 2002, 12 (5):511~516
[66]
57 Liu K, Chan J C. Synoptic flow patterns associated with small and large tropical cyclones over the western North Pacific. Monthly Weather Review, 2002, 130 (8):2134~2142
[67]
58 Wang L C, Behling H, Lee T Q et al. Increased precipitation during the Little Ice Age in northern Taiwan inferred from diatoms and geochemistry in a sediment core from a subalpine lake. Journal of Paleolimnology, 2013, 49 (4):619~631
[68]
59 Yan H, Sun L, Oppo D W et al. South China Sea hydrological changes and Pacific Walker Circulation variations over the last millennium. Nature Communications, 2011, 2 (1):293~293
[69]
60 余凤玲, Switzer A D, 郑 卓等. 榕江河口冲积平原的沉积特征及其对灾害气候事件的响应. 第四纪研究, 2013, 33 (6):1171~1182 Yu Fengling, Switzer A D, Zheng Zhuo et al. Sedimentary records as an indicator for palaeotyphoon hazards from the Rongjiang River delta, Chaoshan Plain, Southern China. Quaternary Sciences, 2013, 33 (6):1171~1182
[70]
61 吴江滢, 汪永进, 董进国. 全新世东亚夏季风演化的辽宁暖和洞石笋 δ 18 O记录. 第四纪研究, 2011, 31 (6):990~998 Wu Jiangying, Wang Yongjin, Dong Jinguo. Changes in East Asian summer monsoon during the Holocene recorded by stalagmite δ 18 O records from Liaoning Province. Quaternary Sciences, 2011, 31 (6):990~998
[71]
62 杨文光, 郑洪波, 谢 昕等. 南海北部陆坡沉积记录的全新世早期夏季风极强事件. 第四纪研究, 2008, 28 (3):425~430 Yang Wenguang, Zheng Hongbo, Xie Xin et al. East Asian summer monsoon maximum records in northern South China sea during the Early Holocene. Quaternary Sciences, 2008, 28 (3):425~430
[72]
63 Neff U, Burns S, Mangini A et al. Strong coherence between solar variability and the monsoon in Oman between 9 and 6 kyr ago. Nature, 2001, 411 (6835):290~293
[73]
64 Wang Y J, Cheng H, Edwards R L et al. The Holocene Asian monsoon: Links to solar changes and North Atlantic climate. Science, 2005, 308 (854):854~857
[74]
65 张振球, 刘殿兵, 汪永进等. 中全新世东亚季风年至10年际气候变率: 湖北青天洞5.56~4.84ka B.P. 石笋年层厚度与地球化学证据. 第四纪研究, 2014, 34 (6):1246~1255 Zhang Zhenqiu, Liu Dianbing, Wang Yongjin et al. Annual-to decadal-scale variability of Asian monsoon climates during Mid-Holocene: Evidence from proxies of annual bands and geochemical behaviors of a speleothem from 5.56ka B.P. to 4.84ka B.P. in Qingtian cave, Central China. Quaternary Sciences, 2014, 34 (6):1246~1255
[75]
66 谭亮成, 蔡演军, 安芷生等. 石笋氧同位素和微量元素记录的陕南地区4200~2000a B.P. 高分辨率季风降雨变化. 第四纪研究, 2014, 34 (6):1238~1245 Tan Liangcheng, Cai Yanjun, An Zhisheng et al. High-resolution monsoon precipitation variations in southern Shaanxi, Central China during 4200~2000a B.P. as revealed by speleothem δ 18 O and Sr/Ca records. Quaternary Sciences, 2014, 34 (6):1238~1245
[76]
67 Wan N J, Li H C, Liu Z Q et al. Spatial variations of monsoonal rain in Eastern China:Instrumental, historic and speleothem records. Journal of Asian Earth Sciences, 2011, 40 (6):1139~1150