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Science China Earth Sciences

, Volume 53, Issue 5, pp 633–641 | Cite as

Precise dating of abrupt shifts in the Asian Monsoon during the last deglaciation based on stalagmite data from Yamen Cave, Guizhou Province, China

  • Yan Yang
  • DaoXian Yuan
  • Hai Cheng
  • MeiLiang Zhang
  • JiaMing Qin
  • YuShi Lin
  • XiaoYan Zhu
  • R. Lawrence Edwards
Research Paper

Abstract

Based on 33 U/Th dates and 1020 oxygen isotopic data from stalagmite Y1 from Yamen Cave, Guizhou Province, China, a record of the Asian Summer Monsoon (ASM) was established. The record covers the last deglaciation and the early Holocene (from 16.2 to 7.3 ka BP) with an average oxygen isotope resolution of 9 years. The main millennial-scale deglacial events first identified in Greenland (Greenland Interstadial Events: GIS 1e through GIS 1a) and later in China are clearly present in the Y1 record. By analogy to earlier work, we refer to these as Chinese Interstadials (CIS): CIS A.1e to CIS A.1a. The onset of these events in Y1 δ 18O records are nominally dated at: 14750±50, 14100±60, 13870±80, 13370±80, and 12990±80 a BP. The end of CIS A.1a or the beginning of the Younger Dryas (YD) event is nominally at 12850±50 a BP and the end of the YD dates to 11500±40 a BP. The δ 18O values shift by close to 3‰ during the transition into the Bølling-Allerød (BA, the onset of CIS A.1e) and at the end of the YD. Comparisons of Y1 to previously published early Holocene records show no significant phase differences. Thus, the East Asia Monsoon and the Indian Monsoon do not appear to have been out of phase during this interval. The Y1 record confirms earlier work that suggested that solar insolation and North Atlantic climate both affect the Asian Monsoon.

Keywords

stalagmite Asian Monsoon the last deglaciation Holocene U-series dating Yamen Cave 

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References

  1. 1.
    Alley R B, Marotzke J, Nordhaus W D, et al. Abrupt climate change. Science, 2003, 299: 2005–2010CrossRefGoogle Scholar
  2. 2.
    Broecker W S. Does the trigger for abrupt climate change reside in the ocean or in the atmosphere? Science, 2003, 300: 1519–1522CrossRefGoogle Scholar
  3. 3.
    Cheng H. Global climate change research: Controversy or action? (in Chinese) Chin Sci Bull, 2004, 49: 1339–1344Google Scholar
  4. 4.
    An Z S. The history and variability of the East Asian paleomonsoon climate. Quat Sci Rev, 2000, 19: 171–187CrossRefGoogle Scholar
  5. 5.
    Yuan D X, Liu Z H, Jiang Z C, et al. The Carbon Cycle and Karst Geological Environment (in Chinese). Beijing: Science Press, 2003. 95–177Google Scholar
  6. 6.
    Martinson D G, Pisias N J, Hays J D. Age dating and the orbital theory of ice ages: Development of a high-resolution 0 to 30,0000-year chronostratigraphy. Quat Res, 1987, 27: 1–29CrossRefGoogle Scholar
  7. 7.
    Lehman S J, Keigwin L D. Sudden changes in North Atlantic circulation during the last deglaciation. Nature, 1992, 356: 757–762CrossRefGoogle Scholar
  8. 8.
    Wang P X, Bian Y H, Li B H, et al. The Younger Dryas in the West Pacific marginal seas. Sci China Ser D-Earth Sci, 1996, 39: 452–460Google Scholar
  9. 9.
    Bond G, Showers W, Cheseby M, et al. A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science, 1997, 278: 1257–1266CrossRefGoogle Scholar
  10. 10.
    Haug G H, Hughen K A, Sigman D M, et al. Southward migration of the Intertropical Convergence Zone through the Holocene. Science, 2001, 293: 1304–1308CrossRefGoogle Scholar
  11. 11.
    Stott L D, Poulsen C, Lund S, et al. Super ENSO and global climate oscillations at millennial time scales. Science, 2002, 297: 222–226CrossRefGoogle Scholar
  12. 12.
    Stocker T F, Johnsen S J. A minimum thermodynamic model for the bipolar seesaw. Paleoceanography, 2003, 18: 1087–1095CrossRefGoogle Scholar
  13. 13.
    Gupta A K, Anderson D M, Overpeck J T. Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean. Nature, 2003, 421: 354–356CrossRefGoogle Scholar
  14. 14.
    Broecker W S. Musings about the connection between thermohaline circulation and climate. Am Geophys Union Monograph, 2007, 173: 265–278Google Scholar
  15. 15.
    Lamy F, Kaiser J, Arz H W, et al. Modulation of the bipolar seesaw in the Southeast Pacific during Termination 1. Earth Planet Sci Lett, 2007, 259: 400–413CrossRefGoogle Scholar
  16. 16.
    Anderson R F, Ali S, Bradtmiller L I, et al. Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2. Science, 2009, 323: 1443–1448CrossRefGoogle Scholar
  17. 17.
    Barker S, Diz P, Vautravers M J, et al. Interhemispheric Atlantic seesaw response dring the last deglaciation. Nature, 2009, 457: 1097–1103CrossRefGoogle Scholar
  18. 18.
    Wang P X. Global monsoon in a geological perspective. Chin Sci Bull, 2009, 54: 1113–1136CrossRefGoogle Scholar
  19. 19.
    Dansgaard W, White J W C, Johnsen S J. The abrupt termination of the Younger Dryas climate event. Nature, 1989, 339: 532–534CrossRefGoogle Scholar
  20. 20.
    Stuiver M, Grootes P M, Braziunas T F. The GISP2 δ 18O climate record of the past 16,500 years and the role of the sun, ocean, and volcanoes. Quat Res, 1995, 44: 341–354CrossRefGoogle Scholar
  21. 21.
    Taylor K C, Mayewski P A, Alley R B, et al. The Holocene-Younger Dryas Transition recorded at Summit, Greenland. Science, 1997, 278: 825–827CrossRefGoogle Scholar
  22. 22.
    Meese D A, Gow A J, Alley R B. et al. The Greenland Ice Sheet Project 2 depth-age scale: Methods and results. J Geophys Res, 1997, 102: 26411–26423CrossRefGoogle Scholar
  23. 23.
    Greenland Ice Sheet Project 2 (GISP2). The Greenland Summit Ice Cores, National Snow and Ice Data Center, University of Colorado at Boulder, and the World Data Center-A for Paleoclimatology. National Geophysical Data Center, Boulder Colorado, 1997Google Scholar
  24. 24.
    Petit J R, Jouzel J, Raynaud D, et al. Climate and Atmospheric history of the past 420,000 years from the Vostok ice core, Antarctic. Nature, 1999, 399: 429–436CrossRefGoogle Scholar
  25. 25.
    Yao T D. Abrupt climatic changes on the Tibetan Plateau during the Last Ice Age—Comparative study of the Guliya ice core with the Greenland GRIP ice core. Sci China Ser D-Earth Sci, 1999, 42: 358–368Google Scholar
  26. 26.
    Johnsen S, Dahl-Jensen D, Gundestrup N S, et al. Oxygen isotope and palaeotemperature records from six Greenland ice-core stations: Camp century, Dye-3, GRIP, GISP2, Renland and NorthGRIP. J Quat Sci, 2001, 16: 299–307CrossRefGoogle Scholar
  27. 27.
    North Greenland Ice Core Project (NGRIP) Members. High-resolution record of Northern hemisphere climate extending into the last interglacial period. Nature, 2004, 431: 147–151CrossRefGoogle Scholar
  28. 28.
    Lowe J J, Rasmussen S O, Björck J, et al. Synchronisation of palaeoenvironmental events in the North Atlantic region during the Last Termination: A revised protocol recommended by the INTIMATE group. Quat Sci Rev, 2008, 27: 6–17CrossRefGoogle Scholar
  29. 29.
    Ding Z L, Liu T S, Rutter N W, et al. Ice-volume forcing of East Asian winter monsoon variation the past 800,000 years. Quat Res, 1995, 44: 149–159CrossRefGoogle Scholar
  30. 30.
    Zhou W J, Head M J, An Z S, et al. Terrestrial evidence for a spatial structure of tropical-polar interconnections during the Younger Dryas episode. Earth Planet Sci Lett, 2001, 191: 231–239CrossRefGoogle Scholar
  31. 31.
    Bjorck S, Kromer B, Johnsen S, et al. Synchronized terrestrialatmospheric deglacial records from around the North Atlantic, Science, 1996, 274: 1155–1160CrossRefGoogle Scholar
  32. 32.
    Liu X Q, Shen J, Wang S M, et al. A 16000-year pollen record of Qinghai Lake and its paleoclimate and paleoenvironment. Chin Sci Bull, 2002, 47: 1931–1936CrossRefGoogle Scholar
  33. 33.
    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: 371–380CrossRefGoogle Scholar
  34. 34.
    Hong Y T, Hong B, Lin Q H, et al. Inverse phase oscillations between the East Asian and Indian ocean summer monsoons during the last 12000 years and paleo-E1 Niño. Earth Planet Sci Lett, 2005, 231: 331–346CrossRefGoogle Scholar
  35. 35.
    He Y, Theakstone W H, Zhang Z L, et al. Asynchronous Holocene climatic change across China. Quat Res, 2004, 61: 52–63CrossRefGoogle Scholar
  36. 36.
    Garcin Y, Vincens A, Williamson D, et al. Abrupt resumption of the African monsoon at the Younger Dryas-Holocene climatic transition. Quat Sci Rev, 2007, 26: 690–704CrossRefGoogle Scholar
  37. 37.
    Chen F H, Yu Z C, Yang M L, et al. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history. Quat Sci Rev, 2008, 27: 351–364CrossRefGoogle Scholar
  38. 38.
    Schaub M, Buntgen U, Kaiser K F, et al. Lateglacial environmental variability from Swiss tree rings. Quat Sci Rev, 2008, 27: 29–41CrossRefGoogle Scholar
  39. 39.
    Wang Y J, Cheng H, Edwards R L, et al. A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu Cave, China. Science, 2001, 294: 2345–2348CrossRefGoogle Scholar
  40. 40.
    Fleitmann D, Burns S J, Mudelsee M, et al. Holocene forcing of the Indian Monsoon recorded in a stalagmite from Southern Oman. Science, 2003, 300: 1737–1739CrossRefGoogle Scholar
  41. 41.
    Fleitmann D, Burns S J, Mangini A, et al. Holocene ITCZ and Indian monsoon dynamics recorded in stalagmites from Oman and Yemen (Socotra). Quat Sci Rev, 2007, 26: 170–188CrossRefGoogle Scholar
  42. 42.
    Neff U, Burns S J, Mangini A, et al. Strong coherence between solar variability and the monsoon in Oman between 9 and 6 ka ago. Nature, 2001, 411: 290–293CrossRefGoogle Scholar
  43. 43.
    Sinha A, Cannariato K G, Stott L D, et al. Variability of Southwest Indian summer monsoon precipitation during the Bølling-Allerød. Geology, 2005, 33: 813.816 Google Scholar
  44. 44.
    Yuan D X, Cheng H, Edwards R L, et al. Timing, duration, and transitions of the last interglacial Asian monsoon. Science, 2004, 304: 575–578CrossRefGoogle Scholar
  45. 45.
    Qin J M, Yuan D X, Cheng H, et al. The Y. D. and climate abrupt events in the early and middle Holocene: Stalagmite oxygen isotope record from Maolan, Guizhou, China. Sci China Ser D-Earth Sci, 2005, 48: 530–537CrossRefGoogle Scholar
  46. 46.
    Zhang M L, Cheng H, Lin Y S, et al. High resolution paleo-climatic environment records from a stalagmite of Dongge Cave since 15000 a in Libo, Guizhou Province, China (in Chinese). Geochimica, 2004, 33: 65–74Google Scholar
  47. 47.
    Dykoski C A, Edwards R L, Cheng H, et al. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China. Earth Planet Sci Lett, 2005, 233: 71–86CrossRefGoogle Scholar
  48. 48.
    Cheng H, Edwards R L, Wang X F, et al. Oxygen isotope records of stalagmites from southern China (in Chinese). Quat Sci, 2005, 25: 157–163Google Scholar
  49. 49.
    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: 854–857CrossRefGoogle Scholar
  50. 50.
    Shao X H, Wang Y J, Cheng H, et al. Long-term trend and abrupt events of the Holocene Asian monsoon inferred from a stalagmite δ 18O record from Shennongjia in Central China. Chin Sci Bull, 2006, 51: 221–228CrossRefGoogle Scholar
  51. 51.
    Liu D B, Wang Y J, Cheng H, et al. A detailed comparison of Asian Monsoon intensity and Greenland temperature during the Allerød and Younger Dryas events. Earth Planet Sci Lett, 2008, 272: 691–697CrossRefGoogle Scholar
  52. 52.
    Hu C Y, Henderson G M, Huang J H, et al. Quantification of Holocene Asian monsoon rainfall from spatially separated cave record. Earth Planet Sci Lett, 2008, 266: 221–232CrossRefGoogle Scholar
  53. 53.
    Cai B G, Edwards R L, Cheng H, et al. A dry episode during the Younger Dryas and centennial-scale weak monsoon events during the early Holocene: A high-resolution stalagmite record from southeast of the Loess Plateau, China. Geophys Res Lett, 2008, 35: L02705CrossRefGoogle Scholar
  54. 54.
    Shakun J D, Burns S J, Fleitmann D, et al. A high-resolution, absolute-dated deglacial speleothem record of Indian Ocean climate from Socotra Island, Yemen. Earth Planet Sci Lett, 2007, 259: 442–456CrossRefGoogle Scholar
  55. 55.
    Wang X F, Auler A S, Edwards R L, et al. Interhemispheric antiphasing of rainfall during the last glacial period. Quat Sci Rev, 2006, 25: 3391–3403CrossRefGoogle Scholar
  56. 56.
    Wang X F, Auler A S, Edwards R L, et al. Millennial-scale precipitation changes in southern Brazil over the past 90,000 years. Geophys Res Lett, 2007, 34: L23701CrossRefGoogle Scholar
  57. 57.
    Wang Y J, Cheng H, Edwards R L, et al. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years. Nature, 2008, 451: 1090–1093CrossRefGoogle Scholar
  58. 58.
    Kelly M J, Edwards R L, Cheng H, et al. High resolution characterization of the Asian monsoon between 146,000 and 99,000 years B.P. from Dongge Cave, China and global correlation of events surrounding Termination II. Paleogeogr Paleoclimatol Paleoecol, 2006, 236: 20–38CrossRefGoogle Scholar
  59. 59.
    Cheng H, Edwards R L, Wang Y J, et al. A penultimate glacial monsoon record from Hulu Cave and two-phase glacial terminations. Geology, 2006, 34: 217–220CrossRefGoogle Scholar
  60. 60.
    Chen S T, Wang Y J, Kong X G, et al. A possible Younger Dryas-type event during Asian monsoonal Termination 3. Sci China Ser D-Earth Sci, 2006, 49: 982–990CrossRefGoogle Scholar
  61. 61.
    Yang Y, Yuan D X, Cheng H. Research on the high precision ICP-MS uranium series 230Th chronology and a case study on stalagmite Y1 in Yamen Cave, Libo County, Guizhou, China (in Chinese). Carsol Sin, 2006, 25: 89–94Google Scholar
  62. 62.
    Shen C C, Edwards R L, Cheng H, et al. Uranium and thorium isotopic and concentration measurements by magnetic sector inductively coupled plasma mass spectrometry. Chem Geol, 2002, 185: 165–178CrossRefGoogle Scholar
  63. 63.
    Cheng H, Edwards R L, Hoff J, et al. The half-lives of uranium-234 and thorium-230. Chem Geol, 2000, 169: 17–33CrossRefGoogle Scholar
  64. 64.
    Yuan D X, Cao J H. Karst Dynamics of the Theory and Practice (in Chinese). Beijing: Science Press, 2008. 1–197Google Scholar
  65. 65.
    Schulza M, Mudelsee M. REDFIT: Estimatingred-noise spectra directly from unevenly spaced paleoclimatic time series. Comput Geosci, 2002, 28: 421–426CrossRefGoogle Scholar

Copyright information

© Science China Press and Springer-Verlag Berlin Heidelberg 2010

Authors and Affiliations

  • Yan Yang
    • 1
    • 2
  • DaoXian Yuan
    • 1
    • 2
  • Hai Cheng
    • 3
  • MeiLiang Zhang
    • 2
  • JiaMing Qin
    • 2
  • YuShi Lin
    • 2
  • XiaoYan Zhu
    • 2
  • R. Lawrence Edwards
    • 3
  1. 1.School of Geographical SciencesSouthwest UniversityChongqingChina
  2. 2.Karst Dynamics Laboratory, Ministry of Land and Resources, Institute of Karst GeologyChinese Academy of Geological SciencesGuilinChina
  3. 3.Department of Geology and GeophysicsUniversity of MinnesotaMinneapolisUSA

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