Abstract
We present a 50-year pollen record at near-annual resolution from Gahai Lake in the Qaidam Basin on the northeastern Tibetan Plateau. Chronology of a 22-cm short core was established by 210Pb and 137Cs analysis. The pollen results at 0.5 cm intervals show large changes in Artemisia/Chenopodiaceae (A/C) ratios from < 0.2 to 0.95 in the last 50 years. High (low) A/C ratios represent increase (decrease) in steppe pollen production, which correspond to high (low) relative humidity observed at nearby Delingha weather station. On the basis of good correspondence with instrumental records and carbonate content from Gahai Lake, we conclude that A/C ratio is sensitive to moisture change and can be a very useful index in reconstructing paleoclimate of arid regions. Comparison with pollen and snow accumulation data from Dunde ice core suggests that effective moisture at low and high elevations shows the opposite relationship when mountain precipitation was extremely high, possibly due to topography-induced uplifting and subsiding air dynamics.
Original language | English (US) |
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Pages (from-to) | 107-114 |
Number of pages | 8 |
Journal | Global and Planetary Change |
Volume | 62 |
Issue number | 1-2 |
DOIs | |
State | Published - May 2008 |
Bibliographical note
Funding Information:We thank J.J. Chen and C. Zhao for field assistance, and P. Wilkinson and E. Slavicek for 210 Pb and 137 Cs dating analysis, and three anonymous reviewers and the editor for useful comments and suggestions. This project was supported by the National Natural Science Foundation of China (Grants #40528001, 40421101 and 40771212), and US NSF (EAR #0518774 and #0519255). During the final preparation of the manuscript, the senior author was a Visiting Research Scientist in the Department of Earth and Environmental Sciences at Lehigh University, supported by the US NSF.
Keywords
- A/C ratio
- Gahai Lake
- Qaidam Basin
- climate data
- effective moisture
- fossil pollen