Sedimentary Components Responsibilities on the Holocene
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Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s10553-024-01665-2.pdf
Reference33 articles.
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2. Frenzel, P., Wrozyna, C., Xie, M., et al. Palaeo-water depth estimation for a 600-year record from Nam Co (Tibet) using an ostracod-based transfer function. Quaternary International, 2010, 218, 157-165.
3. Zhao, Y., Yu, Z.C., Zhao, W.W. Holocene vegetation and climate histories in the eastern Tibetan Plateau: controls by insolation-driven temperature or monsoon-derived precipitation changes? Quaternary Science Reviews, 2011, 30, 1173-1184.
4. Su, Y.L., Gao, X., Liu QingSong, et al. Mechanism of variations in environmental magnetic proxies of lake sediments from Nam Co, Tibet during the Holocene. Chinese Science Bulletin, 2013, 58(13), 1568-1578.
5. O’Brien, S.R., Mayewski, P.A., Meeker, L.D. et al. Complexity of Holocene climate as reconstructed from a Greenland icecore. Science, 1995, 270(5244), 1962-1964.
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