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Tytuł artykułu

Late Glacial and Holocene vegetation and climate history of an alpine wetland on the Qinghai-Tibetan Plateau

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
This study provides a vegetation and climate history of an alpine wetland in the centre of China’s Qinghai–Tibetan Plateau (QTP) over the last 14.8 ka. High resolution climate proxies include vegetation (pollen), geochemical (Ba, Rb, δ13C) and physical (particle size and magnetic susceptibility) data; optically stimulated luminescence (OSL) and AMS radiocarbon dating were used to reconstruct the environmental changes in the wetland ecosystem. Based on physical and geochemical proxies, the sucession divided into five stratigraphic units encompassing time intervals of 14.76–14.31, 14.31–13.17, 13.17–4.47, 4.47–0.51 and 0.51–0 ka. The average sedimentation rate of all these units was 0.098 mm/a. The study showed that this ecosystem was sensitive to climate change.
Rocznik
Strony
261--–268
Opis fizyczny
Bibliogr. 42 poz., rys., tab., wykr.
Twórcy
autor
  • University of Chinese Academy of Sciences, 19 Yuquan Rd., Beijing 100049, China
autor
  • Northwest Institute of Plateau Biology, Chinese Academy of Sciences, 23 Xinning Rd., Xining 810008, China
autor
  • CAS Key Laboratory of Salt Lake Resources and Chemistry, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, 18 Xinning Rd., Xining 810008, China
  • Northwest Institute of Plateau Biology, Chinese Academy of Sciences, 23 Xinning Rd., Xining 810008, China
autor
  • CAS Key Laboratory of Salt Lake Resources and Chemistry, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, 18 Xinning Rd., Xining 810008, China
autor
  • Northwest Institute of Plateau Biology, Chinese Academy of Sciences, 23 Xinning Rd., Xining 810008, China
autor
  • Northwest Institute of Plateau Biology, Chinese Academy of Sciences, 23 Xinning Rd., Xining 810008, China
Bibliografia
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  • 16. Lai Z.P. (2010) Chronology and the upper dating limit for loess samples from Luochuan section in the Chinese Loess Plateau using quartz OSL SAR protocol. Journal of Asian Earth Sciences, 37: 176-185.
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  • 21. Margielewski W., Kołaczek P., Michczyński A., Obidowicz A., Pazdur A. (2011) Record of the Meso- and Neoholocene palaeoenvironmental changes in the Jesionowa landslide peat bog (Beskid Sądecki Mts., Polish Outer Carpathians). Geochronometria, 38: 138-154.
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  • 24. Murray A.S., Wintle A.G. (2000) Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements, 32: 57-73.
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  • 29. Wang J., Zhu L., Nishimura M., Testsuya M. (2009) Spatial variability and correlation of environmental proxies during the past 18,000 years among multiple cores from Lake Pumoyum Co, Tibet, China. Journal of Paleolimnology, 42: 303-315.
  • 30. Wang M. (2005) A Study on Ecology and Environment Process of Cenozoic Qinghai-Tibet Plateau Hinterland (in Chinese with English abstract). Unpublished Ph.D. dissertation, Chengdu University of Technology.
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  • 32. Wei H.C., Ma H.Z., Zheng Z., Pan A.D., Huang K.Y. (2010) Modern pollen assemblages of surface samples and their relationships to vegetation and climate in the northeastern Qinghai-Tibetan Plateau, China. Review of Palaeobotany and Palynology, 162: 168-182.
  • 33. Wischnewski J., Mischke S., Wang Y., Herzschuh U. (2011) Reconstructing climate variability on the northeastern Tibetan Plateau since the last Lateglacial multi-proxy, dual-site approach comparing terrestrial and aquatic signals. Quaternary Science Re vues, 30: 82-97.
  • 34. Wu Y., Andreas L., Bernd W., Li S., Wang S. (2007) Holocene climate change in the Central Tibetan Plateau inferred by lacustrine sediment geochemical records. Science in China Series D: Earth Sciences, 50: 1548-1555.
  • 35. Yang X., Scuderi L. (2010) Hydrological and climatic changes in deserts of China since the Late Pleistocene. Quaternary Ret search, 73: 1-9.
  • 36. Yang X., Zhu B., Wang X., Lu Y. (2008) Late Quaternary environmental changes and organic carbon density in the Hunshandake Sandy Land, eastern Inner Mongolia, China. Global and Planetary Change, 61: 70-78.
  • 37. Zhao C.H. (2009) Climate Evolution of Holocene in Eastern Aisa and Its Quantitative Analysis (in Chinese with English abstract). Nanjing University.
  • 38. Zhao K. (1999) Marshes and swamps of China: a compilation (in Chinese). Beijing, Science Press of China.
  • 39. Zhao Z., Qiao Y., Wang S., Jiang F. (2008) Geological characteristics and evolution of the eastern Qinghai-Tibetan plateau since the late Cenozoic. Frontiers of Earth Science, 2 (2): 209-216.
  • 40. Zhu L., Zhen X., Wang J., Lü H., Xie M., Kitagawa H., Possnert G. (2009) A ~30,000-year record of envi fonmental changes int ferred from Lake Chen Co, Southern Tibet. Journal of Paleolimnology, 42 (3): 343-358.
  • 41. Zhu L., Peng P., Xie M., Wang J., Frenzel P., Wrozyna C., Schwalb A. (2010) Ostracod-based environmental reconstruction over the last 8,400 years of Nam Co Lake on the Tibetan plateau. Hydrobiologia, 648 (1): 157-174.
  • 42. Zhu L.P., Li Y.F., Li B.Y. (2002) The ostracod assemblages and their environmental significance in the Chen Co area, southern Tibet in recent 1400 years. Journal of Geographical Sciences, 12 (4): 451-459.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-0b9b2ff5-dc97-4d0f-bb99-49b7bd3c3661
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