首页> 外文OA文献 >Figure 3: The ensemble of 216 species distribution models of Nymania capensis projected onto (A) present and (B) Last Glacial Maximum (CCSM) simulated and downscaled climate, as well as the changes in climatically suitable (C) area, and (D) patch cohesion index, within each basin.

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Figure 3: The ensemble of 216 species distribution models of Nymania capensis projected onto (A) present and (B) Last Glacial Maximum (CCSM) simulated and downscaled climate, as well as the changes in climatically suitable (C) area, and (D) patch cohesion index, within each basin.

机译：图3：投影到（a）的Nymania capensis的216种分布模型的集合和（b）最后冰川最大值（CCSM）模拟和缩小的气候，以及气候合适（c）区域的变化，以及（d ）在每个盆内内的斑块凝聚率指数。

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Figure 3: The ensemble of 216 species distribution models of Nymania capensis projected onto (A) present and (B) Last Glacial Maximum (CCSM) simulated and downscaled climate, as well as the changes in climatically suitable (C) area, and (D) patch cohesion index, within each basin.

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