Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene
详细信息 查看全文
- 作者：ShengFa Liu (1) (2) (3)
XueFa Shi (2)
YanGuang Liu (2)
ShuQing Qiao (2)
Gang Yang (2)
XiSheng Fang (2)
YongHua Wu (2)
ChaoXin Li (2)
XiaoYan Li (2)
AiMei Zhu (2)
JingJing Gao (2) - 关键词：Holocene ; inner shelf of the East China Sea ; mud areas ; grain size ; clay mineral ; elemental analysis ; East Asia winter monsoon
- 刊名：Chinese Science Bulletin
- 出版年：2010
- 出版时间：July 2010
- 年：2010
- 卷：55
- 期：21
- 页码：2306-2314
- 全文大小：801KB
- 参考文献：1. Liu J P, Xu K H, Li A C, et al. Flux and fate of Yangtze River sediment delivered to the East China Sea. Geomorphology, 2007, 85: 208-24 CrossRef
2. Xiao S B, Li A C, Jiang F Q, et al. Geochemical characteristics of recent 2 ka mud on the inner shelf of the East China Sea (in Chinese). Acta Sedimentol Sin, 2005, 23: 268-74
3. Xiao S B, Li A C, Liu W G, et al. Geochemical characteristics of mud on the inner shelf of the East China Sea (in Chinese). Prog Nat Sci, 2009, 19: 185-91
4. Xiao S B, Li A C, Chen M H, et al. Recent 8 ka mud records of the East Asian Winter Monsoon from the inner shelf of the East China Sea (in Chinese). Earth Sci-J Chi Univ Geosci, 2005, 30: 573-81
5. Xiao S B, Li A C, Liu J P, et al. Coherence between solar activity and the East China Asian winter monsoon variability in the past 8000 years from Yangtze River-derived mud in the East China Sea. Palaeogeogr Palaeoclimatol Palaeoecol, 2006, 237: 293-04 CrossRef
6. Zhang X D, Xu S M, Zhai S K, et al. The Inversion of Climate Information from the Sediment of Inner Shelf of East China Sea using End-Member Model (in Chinese). Mar Geol Quat Geol, 2006, 26: 25-2
7. Wei G J, Li X H, Chen Y W, et al. High-resolution records of transitive metals of sediments from Core NS93-5 and their paleoceanography implications (in Chinese). Geochimica, 2001, 30: 450-58
8. Liu Z F, Colin A, Trentesaux D, et al. Clay mineral records of East Asian monsoon evolution during late Quaternary in the southern South China Sea. Sci China Ser D-Earth Sci, 2005, 48: 84-2 CrossRef
9. Qin Y S, Zhao Y Y, Chen L R, et a1. Geology of the East China Sea (in Chinese). Beijing: Science Press, 1987. 1-86
10. Hu D X, Yang Z S. Margin flux in the East China Sea (in Chinese). Beijing: Ocean Press, 2001. 3-3
11. Su J L. A review of circulation dynamics of the coastal oceans near China (in Chinese). Acta Oceanonl Sin, 2001, 23: 1-6
12. Yoneda M, Uno H, Shibata Y, et al. Radiocarbon marine reservoir ages in the western Pacific estimated by pre-bomb molluscan shells. Nucl Instrum Meth Phys Res B, 2007, 259: 432-37 CrossRef
13. Guo Z G, Yang Z S, Zhang D Q, et al. Seasonal distribution of suspended matter in the northern East China Sea and barrier effect of current circulation on its transport (in Chinese). Acta Oceanol Sin, 2002, 24: 71-0
14. Yang Z S, Guo Z G, Wang Z X, et al. Suspended sediments on the Yellow and East China Sea shelf and macro-pattern of their being transported to the eastern deeper sea (in Chinese). Acta Oceanol Sin, 1992, 14: 81-0
15. Sun X G, Fang M, Huang W. Spatial and temporal variations in suspended particulate matter transport on the Yellow and East China Sea shelf (in Chinese). Oceanol Etlimnol Sin, 2000, 31: 581-87
16. Jin Y H. The characteristics of estuarine in China (in Chinese). Donghai Mar Sci, 1988, 6: 1-1
17. Sun D H, Bloemendal J, Rea D K, et al. Grain-size distribution function of polymodal sediments in hydraulic and aeolian environments, and numerical partitioning of the sedimentary components. Sediment Geol, 2002, 152: 263-77 CrossRef
18. Prins M A, Postma G, Cleveringa J, et al. Controls on terrigenous sediment supply to the Arabian Sea during the late Quaternary: The Indus Fan. Mar Geol, 2000, 169: 327-49 CrossRef
19. Prins M A, Bouwer L M, Beets C J, et al. Ocean circulation and iceberg discharge in the glacial North Atlantic: Inferences from unmixing of sediment size distributions. J Geol, 2002, 30: 555-58 CrossRef
20. Prins M A, Vriend M, Nugteren G, et al. Late Quaternary Aeolian dust input variability on the Chinese Loess Plateau: inferences from unmixing of loess grain-size records. Quat Sci Rev, 2007, 26: 230-42 CrossRef
21. Stuut J B W, Prins M A, Ralph R S, et al. A 300-kyr record of aridity and wind strength in southwestern Africa: Inferences from grain-size distributions of sediments on Walvis Ridge, SE Atlantic. Mar Geol, 2002, 180: 221-33 CrossRef
22. Sun Y B, Gao S, Li J. Primary analysis on the sensitive grain size of terrigenous sediment to environments in marginal sea (in Chinese). Chinese Sci Bull, 2003, 48: 83-6
23. Boulay S, Colin C, Trentesaux A, et al. Mineralogy and sedimentology of Pleistocene sediments on the South China Sea (ODP Site 1144). In: Prell W L, Wang P, Blum P, et al., eds. Proc ODP, Sci Res, 2003, 184: 1-1
24. Xiang R, Yang Z S, Satio Y, et al. East Asia Winter Monsoon changes inferred from environmentally sensitive grain-size component records during the last 2300 years in mud area southwest off Cheju Island, ECS. Sci China, Ser D-Earth Sci, 2006, 49: 604-14 CrossRef
25. Xiao S B, Li A C, Jiang F Q, et al. Recent 2000-year geological records of mud in the inner shelf of the East China Sea and their climatic implications. Chinese Sci Bull, 2005, 50: 466-71
26. Yan W, Gu S C, Chen L Z, et al. Characteristics of major elements of sediments in core 97-37 from Southern South China Sea and potential implications to paleoenvironment (in Chinese). J Tropical Oceanogr, 2002, 21: 75-3
27. Zhao H Q, Han X B, Chen R H, et al. Characteristics of main elements and their palaeoenvironment significance of Core 191 in the northern South China Sea (in Chinese). Acta Oceanol Sin, 2008, 30: 85-3
28. Liu S F, Shi X F, Liu Y G, et al. Geochemical characteristics and geological significance of major elements in surface sediments form the inner continental shelf mud area of the East China Sea (in Chinese). Adv Marine Sci, 2010, 28: 80-6
29. Honda M, Shimizu H. Geochemical mineralogical and sedimentological studies on the Taklimakan Desert sands. Sedimentology, 1998, 45: 1125-143 CrossRef
30. Nesbitt H W, Yong G M. Early proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature, 1982, 299: 715-17 CrossRef
31. Petschick R, Kuhn G Gingele F. Clay mineral distribution in surface sediments of the South Atlantic: Sources, transport, and relation to oceanography. Mar Geol, 1996, 130: 203-29 CrossRef
32. Liu Z, Trentesaux A, Clemens S C, et al. Clay mineral assemblages in the northern South China Sea: Implications for East Asian monsoon evolution over the past 2 million years. Mar Geol, 2003, 201: 133-46 CrossRef
33. Colin C, Turpin L, Bertaux J, et al. Erosional history of the Himalayan and Burman ranges during the last two glacial-interglacial cycles. Earth Planet Sci Lett, 1999, 171: 647-60 CrossRef
34. Tang S, Shao L, Zhao Q H. Characteristics of clay mineral in South China Sea since Oligocene and its significance (in Chinese). Acta Sedimentol Sin, 2004, 22: 337-41
35. Zhu F G. Clay minerals of the East China Sea shelf area in the recent Epoch stratum (in Chinese). Donghai Mar Sci, 1985, 3: 32-0
36. Lan X H, Ma D X, Xu M G, et al. Clay minerals in the late Quaternary sediments of the Zhujiang estuary and their facies significance (in Chinese). J Oceanogr Taiwan Strait, 1988, 7: 127-34
37. He L B, Liu Q Y. Chemical characteristics of clay minerals in the sediments from the Yellow River and the Changjiang River. Chinese Sci Bull, 1997, 42: 488-92 CrossRef
38. Lan X H. Clay minerals as an index of paleoclimate (in Chinese). Geol Sci Tech Inf, 1990, 9: 31-5
39. Cheng J, Tang D X, Zhang X J, et al. Research on the Holocene climate in the source area of the Yellow river by clay minerals (in Chinese). Geoscience, 2003, 17: 47-0
40. Wu Y Y, Chen Z Y, Wang Z H. Distribution of clay minerals in the Yangtze Delta Plain and its Paleoenvironmental implication (in Chinese). J East China Norm Univ Nat Sci, 2005, 2005: 92-8
41. Stuiver M, Grootes P M, Braziunas T F. The GISP2 δ18O climate record of the past 16500 years and the role of the sun, ocean and volcanoes. Quat Res, 1995, 44: 341-54 CrossRef
42. Shi Y F, Kong Z C, Wang S M, et al. The climate fluctuation and important events during the Holocene Megathermal in China. Sci China Ser B, 1994, 37: 353-65
43. Beget J E. Radiocarbon-dated evidence of worldwide early Holocene climate change. Geology, 1983, 11: 389-93 CrossRef
44. 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: 854-57 CrossRef
45. Bond G, Showers W, Cheseby M, et al. A pervasive millennial-scale cycle in north Atlantic Holocene and glacial climates. Science, 1997, 278: 1257-266 CrossRef
46. Sepp? H, Blrks H J B, Glesecke T, et al. Spatial structure of the 8200 cal yr BP event in Northern Europe. Clim Past Dis, 2007, 3: 165-95 CrossRef
47. Hong Y T, Hong B, Lin Q H, et al. Correlation between Indian Ocean summer monsoon and North Atlantic climate during the Holocene. Earth Planet Sci Lett, 2003, 211: 371-80 CrossRef
48. Yang H R. Quaternary Geology (in Chinese). Beijing: Higher Education Press, 1987. 1-28
49. Gasse F, Arnold M, Fontes J C, et al. A 13000 year climate record from western Tibet. Nature, 1991, 353: 742-45 CrossRef
50. Cai Y J, Peng Z C, An Z S, et al. The δ18O variation of a stalagmite from Qixing Cave, Guizhou Province and indicated climate change during the Holocene. Chinese Sci Bull, 2001, 46: 1904-908 CrossRef
51. Xu H, Hong Y T, Lin Q H, et al. Temperature variations in the past 6000 years inferred from δ18O of peat cellulose from Hongyuan, China. Chinese Sci Bull, 2002, 47: 1578-584 CrossRef
52. Sirocko F, Sarnthein P, Erlenkeuser H. Century scale events in monsoonal climate over the past 24000 years. Nature, 1993, 364: 322-24 CrossRef
53. Hong Y T, Jiang H B, Tao F X, et al. Temperature variations in the past 5000 years inferred from δ18O of peat cellulose from Jinchuan, China. Sci China Ser D-Earth Sci, 1997, 27: 520-24
54. Liu X Q, Wang Y B, Shen J, et al. Evolution of Chaka salt lake during the last 16000 years and its response to climatic change (in Chinese). Acta Geol Sin, 2007, 81: 843-49
55. Ge Q S, Wang S B, Zheng J Y. Reconstruction on the series of temperature over the past 3000 years in China (in Chinese). Prog Nat Sci, 2006, 16: 689-96
56. Ge Q S, Fang X Q, Zheng J Y. Warm-cold change in millenarian cycle derived from natural proxy data in China during the past 3000 years (in Chinese). Adv Earth Sci, 2002, 17: 96-03
57. Zhu K Z. A preliminary study on the climate fluctuations during the last 5000 years in China. Sci China Ser A, 1973, 16: 226-56
58. Wang S W, Ye J L, Gong D Y. Climate in China during the Little Ice Age (in Chinese). Quat Sci, 1998, 18: 54-4
59. Yao T D, Xie Z C, Wu X L, et al. Climatic record during the Little Ice Age in Dunde ice cap. Sci China Ser B, 1990, 33: 760-67
60. Shi Y F, Yao T D, Yang B. Decadal climatic variations recorded in Guliya ice core and comparison with the historical documentary data from East China during the last 2000 years. Sci China Ser D-Earth Sci, 1999, 42(Supp): 91-00 CrossRef
61. Liu C P, Yao T D, Thompson L G, et al. Microparticle concentration within the Dunde ice core and its relation to dust storm and climate since the Little Ice Age (in Chinese). J Glaciol Geocryol, 1999, 21: 9-4
62. Hong Y T, Liu D S, Jiang H B, et al. Evidence for solar forcing of climate variation from oxygen isotope of peat cellulose. Sci China Ser D-Earth Sci, 2000, 43: 217-24 CrossRef
63. Jin Z D, Wang S M, Shen J, et al. Carbonate versus silicate Sr isotope in lake sediments and its response to Little Ice Age. Chinese Sci Bull, 2003, 48: 95-00
64. Zhang P Y, Ge Q S, Zhang S H. The modes and abrupt changes of climate in China during recent 2000 years (in Chinese). Quat Sci, 1997, 17: 12-0 - 作者单位：ShengFa Liu (1) (2) (3)
XueFa Shi (2)
YanGuang Liu (2)
ShuQing Qiao (2)
Gang Yang (2)
XiSheng Fang (2)
YongHua Wu (2)
ChaoXin Li (2)
XiaoYan Li (2)
AiMei Zhu (2)
JingJing Gao (2)
1. Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China
2. Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China
3. Graduate University of Chinese Academy of Sciences, Beijing, 100049, China - ISSN：1861-9541
文摘
AMS14C dating and analysis of grain size, major elements and clay minerals were applied to Core MZ01 from the mud area on the inner shelf of the East China Sea. Based on the environmentally sensitive grain size, clay mineral and major element assemblages, the history of the East Asia winter monsoon since the mid-Holocene could be reconstructed. These three proxies, mean grain size (>9.71 μm), chemical index of alteration (CIA) and ratio of smectite to kaolinite in particular, show similar fluctuation patterns. Furthermore, 10 extreme values corresponding to the contemporary cooling events could be recognized since the mid-Holocene; these extreme values are likely to have been caused by the strengthening of the East Asia winter monsoon. The cooling events correlated well with the results of the δ18O curves of the Dunde ice core and GISP2, which therefore revealed a regional response to global climate change. Four stages of the East Asia winter monsoon were identified, i.e. 8300-300 a BP, strong and unstable; 6300-800 a BP, strong but stable; 3800-400 a BP, weak and unstable; after 1400 a BP, weak but stable.