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Optical dating of sediments from manas lake in northwestern china: Paleoenvironmental and neotectonic implications

Autorzy
Identyfikatory
Warianty tytułu
Konferencja
Conference Proceedings of the 4th Asia Pacific Luminescence and Electron Spin Resonance Dating Conference Nov 23rd-25th, 2015, Adelaide, Australia
Języki publikacji
EN
Abstrakty
EN
Manas Lake is a closed lake basin in northern Xinjiang Province of China, with its current lake bed at 244 m a.s.l. Sediments from the lake area provide valuable information about the paleoenvironmental changes in the Westerlies-dominated arid region. To obtain a chronological constraint on the past changes, optically stimulated luminescence dating was conducted on sediments from the lake beaches. The results show that lacustrine episodes dated at ~80–73 ka ago were recorded in northwestern side of the lake at 270 m a.s.l., while paleoshoreline to near-shore environments during ~80–90 ka ago were recorded in the opposite side of the lake at 262 m a.s.l. The ~80 ka old sedimentary layers are overlain by paleoshoreline sediments formed within the last ~1 ka, separated by a large age gap. From this study and the results from previous studies, it is concluded that breaks in sedimentary records are common in the lake area at elevation > 260 m a.s.l. When comparing sedimentary environments at different times from different sites in this study and previous studies, it is suggested that a small amount of uplift of the northwestern side of Manas Lake relative to the southeastern side may have occurred in the last 80 ka.
Wydawca
Czasopismo
Rocznik
Strony
175--187
Opis fizyczny
Bibliogr. 29 poz., rys.
Twórcy
autor
  • Department of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong, China
autor
  • Department of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong, China
Bibliografia
  • 1. Adamiec G and Aitken MJ, 1998. Dose-rate conversion factors: update. Ancient TL 16: 37–50.
  • 2. Aitken MJ, 1998. An Introduction to Luminescence Dating. Oxford University Press, London: 267pp.
  • 3. Arnold LJ and Roberts RG, 2009. Stochastic modelling of multi-grain equivalent dose (De) distributions: implications for OSL dating of sediment mixtures. Quaternary Geochronology 4: 204–230.
  • 4. Banerjee J, Murray AS, Bøtter-Jensen L and Lang A, 2001. Equivalent dose estimation using a single aliquot of polymineral fine grains. Radiation Measurements 33: 73–94.
  • 5. Cheng WM, Zhou CH and Li JX, 2001. Evolution of Manas Lake landscape in Xinjiang and its eco-environmental effect.Quaternary Sciences 21: 560–565 (in Chinese with English abstract).
  • 6. Fan A, Li SH and Chen YG, 2012. Late pleistocene evolution of Lake Manas in western China with constraints of OSL ages of lacustrine sediments. Quaternary Geochronology 10: 143–149.
  • 7. Fain J, Soumana S, Montret M, Miallier D, Pilleyre T and Sanzelle S, 1999. Luminescence and ESR dating Beta-dose attenuation for various grain shapes calculated by a Monte-Carlo method. Quaternary Science Reviews 18: 231–234.
  • 8. Fu X, Li SH, Li B and Fu BH, 2017. A fluvial terrace record of late Quaternary folding rate of the Anjihai anticline in the northern piedmont of Tian Shan, China. Geomorphology 278: 91–104.
  • 9. Galbraith RF and Roberts RG, 2012. Statistical aspects of equivalent dose and error calculation and display in OSL dating: an overview and some recommendations. Quaternary Geochronology 11: 1–27.
  • 10. Galbraith RF, Roberts RG, Laslett GM, Yoshida H and Olley JM, 1999. Optical dating of single and multiple grains of quartz from Jinmium rock shelter, northern Australia, part 1, experimental design and statistical models. Archaeometry 41: 339–364.
  • 11. Gong ZJ, Li SH and Li B, 2014. The evolution of a terrace sequence along Manas River in the northern foreland basin of Tian Shan, China, as inferred from optical dating. Geomorphology213: 201–212.
  • 12. Gong ZJ, Li SH and Li B, 2015. Late Quaternary faulting on the Manas and Hutubi reverse faults in the northern foreland basin of Tian Shan, China. Earth and Planetary Science Letters424: 212–225.
  • 13. Herzschuh U, 2006. Palaeo-moisture evolution in monsoonal Central Asia during the last 50,000 years. Quaternary Science Reviews25: 163–178.
  • 14. Li SH, Sun JM and Zhao H, 2002. Optical dating of dune sands in the northeastern deserts of China. Palaeogeography, Palaeoclimatology, Palaeoecology181: 419–429.
  • 15. Li SH and Fan AC, 2011. OSL chronology of sand deposits and climate change of last 18 ka in Gurbantunggut Desert, northwest China. Journal of Quaternary Science26(8): 813–818, .Mu G, Bao A and Hao J, 2001. Geotectonic environment of the tail-end-lakes evolution, Xinjiang, China. Arid Land Geography24(3): 193–200 (in Chinese with English abstract).
  • 16. Murray AS and Wintle AG, 2000. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements32: 57–73.
  • 17. Prescott JR and Hutton JT, 1994. Cosmic-ray contribution to dose rates for luminescence and ESR dating: large depths and long-term time variations. Radiation Measurements23: 497–500.
  • 18. Rhodes TE, Gasse F, Lin RF, Fontes JC, Wei KQ, Bertrand P, Gibert E, Melieres F, Tucholka P, Wang ZX and Cheng ZY, 1996. A late Pleistocene-Holocene lacustrine record from Lake Manas, Zunggar (northern Xinjiang, western China).Palaeogeography, Palaeoclimatology, Palaeoecology120: 105–121.
  • 19. Shi XM, Li YL and Yang JC, 2008. Climatic and tectonic analysis of Manas Lake changes. Scientia Geographica Sinica 28(2): 266–271 (in Chinese with English abstract).
  • 20. Wang DJ, 1991. Formation and evolution of Manas Lake, Xinjiang, Remote Sensing of Environment China 6: 247–252 (in Chinese with English abstract).
  • 21. Wang R, 2014. Optical dating of young lacustrine sediment from Lake Manas in Northwestern China. MPhil thesis, University of Hong Kong: 118pp.
  • 22. Wang RL, Scarpitta SC, Zhang SC and Zheng MP, 2002. Later Pleistocene/Holocene climate conditions of Qinghai-Xizang plateau (Tibet) based on carbon and oxygen stable isotopes of Zabuye Lake sediments. Earth and Planetary Science Letters 203: 461–477.
  • 23. Wang XM, Dong ZB, Yan P, Zhang JW and Qian GQ, 2005. Wind energy environments and dunefield activity in the Chinese deserts. Geomorphology65: 33–48.
  • 24. Wintle AG and Murray AS, 2006. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. Radiation Measurements41: 369–391 .
  • 25. Yang B and Shi Y, 2003. Warm-humid climate in northwest China during the period of 40~30 ka B.P.: geological records and origin. Quaternary Sciences23(1): 60–68 (in Chinese with English abstract).
  • 26. Yao YH and Li HG, 2010. Tectonic geomorphological characteristics for evolution of the Manas Lake. Journal of Arid Land2(3): 167–173.
  • 27. Yao YH, Wang XQ, Zhou CH, Xu M, Zhang BP and Li HG, 2007. Changes of Manas Lake in the past 50 years in Xinjiang province. Advances in Water Science 18: 17–23 (in Chinese with English abstract).
  • 28. Zhang L and Li Y, 2004. On the changes of Manas Lake in the past 300 years. Collections of Essays on Chinese Historical Geography 19(4): 127–142 (in Chinese).
  • 29. Zhou TR, 1963. Relationship between Quaternary terrestrial deposit types and development of geomorphology and climates in Xinjiang. Acta Geographica Sinica 29(2): 109–125 (in Chinese).
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-f0d5d017-b114-4eaa-989a-de0d2b6f0f34
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