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Post-Pliocene establishment of the present monsoonal climate in SW China: evidence from the late Pliocene Longmen megaflora

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Academic year: 2020

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Figure

Fig. 1.36 (Xu et al., 2004; Kou et al., 2006); (3) Liantie, Eryuan (Kou etal., 2006); (4) Yangyi, Baoshan (Kou et al., 2006); (5) Tuantian,Tengchong (Xie et al., 2012); (6) Yuanmou (Yao et al., 2012); (7)Longchuan (Zhao et al., 2004); (8) L¨uhe, Chuxiong (
Table 1. Percentages of 31 leaf characters in the Longmen flora.
Fig. 2. Position of the Longmen flora in the physiognomic space of the calibrated CLAMP dataset – PhysgAsia1.627
Fig. 3. Comparisons on climatic parameters among the late Miocene, the late Pliocene and the present day in Yunnan
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