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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 4 | Copyright
Clim. Past, 9, 1863-1877, 2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Review article 09 Aug 2013

Review article | 09 Aug 2013

Late Cenozoic continuous aridification in the western Qaidam Basin: evidence from sporopollen records

Y. F. Miao1, X. M. Fang2, F. L. Wu2, M. T. Cai2, C. H. Song3, Q. Q. Meng3, and L. Xu4 Y. F. Miao et al.
  • 1Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Lanzhou, 730000, China
  • 2Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100085, China
  • 3School of Earth Science, Lanzhou University, Lanzhou, 730000, China
  • 4Qinghai Petroleum Sub-corporation of Petro China Company Limited, Dunhuang, 736202, China

Abstract. Cenozoic climate changes in inner Asia provide a basis for understanding linkages between global cooling, the Tibetan Plateau uplift, and possibly the development of the East Asian monsoon. Based on a compilation of palynological results from the western Qaidam Basin, this study reconstructed a 15-million-year (Ma) record of changing vegetation and paleoclimates spanning the middle Miocene to present (comprising two series: ~ 18–5 Ma and ~ 3.1–0 Ma, respectively). The thermophilic percentages were highest between 18 and 14 Ma, and decreased after 14 Ma, closely corresponding to the Middle Miocene Climatic Optimum (MMCO) between 18 and 14 Ma and the following global climatic cooling between 14 and 5 Ma. At the same time, decreases in the xerophytic and coniferous taxa percentages, and the increasing logarithmic ratio of non-arboreal pollen to arboreal pollen (ln (NAP/AP)), reveal the continuous aridification across both the basin and surrounding mountains. Between ~ 3.1 and 0 Ma, the percentages of the thermophilic, xerophytic and coniferous pollen as well as the ln (NAP/AP) imply further cooling and drying in this region since 3.1 Ma. We argue that these vegetation and climate patterns during the late Cenozoic western Qaidam Basin are primarily a result of the global cooling, with the Tibetan Plateau uplift and East Asian summer monsoon having contributions of lesser importance.

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