Abstract
Using data from previous research on Quercus sect. Heterobalanus, the coexistence approach to Xixabangma and Namling fossil sets, and altitudinal ranges of vegetation presented by fossil floras, a review and reevaluation have been made of existing theories on the uplift of the Himalayas, especially the palaeoaltitudes of Xixabangma and Namling in Tibet. The Xixabangma fossil set has a palaeoaltitude range of 2500–3500 m, and has risen 2200–3400 m since the Pliocene. The lower and upper assemblages of the Miocene Namling had palaeoaltitudes of 2500–3000 m and 2800–3000 m, respectively. Therefore, Namling has risen at least 1300 m since the Miocene, thereby challenging some existing theories that suggest Namling has been static since the Miocene.
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Supported by the National Natural Science Foundation of China (Grant Nos. 40332021, 30670159) and Wu Zhengyi’s Splendidly Contributing Award of Yunnan Province (Grant No. KIB-WU-2001-01)
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Zhou, Z., Yang, Q. & Xia, K. Fossils of Quercus sect. Heterobalanus can help explain the uplift of the Himalayas. CHINESE SCI BULL 52, 238–247 (2007). https://doi.org/10.1007/s11434-007-0005-7
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DOI: https://doi.org/10.1007/s11434-007-0005-7