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. 2013 May 20;110(23):9374–9379. doi: 10.1073/pnas.1220228110

Fig. 3.

Fig. 3.

Range of climate dissimilarity and model predictions for the Late Pleistocene (21–11 kyBP) (A–E) and Holocene (10–0 kyBP) (F–J). Light gray indicates the unsampled datasets, red indicates the climate-subsampled spatial datasets, and blue indicates the climate-subsampled temporal datasets. (A and F) Euclidean climate dissimilarity for the spatial datasets. (D and I) Euclidean climate dissimilarity for the temporal datasets. (B and G) Space-for-time OLS regression between observed temporal turnover and temporal turnover predicted by the spatial model. (E and J) Time-for-time OLS regression between observed temporal turnover and temporal turnover predicted by the temporal model. (C and H) Model-to-model RMA regression between temporal turnover predicted by the temporal model and by the spatial model for the climate-subsampled dataset (dark gray) and the unsampled dataset. Regression statistics for analyses based on the climate-subsampled datasets are indicated for each scatter plot. Abbreviations are as in Fig. 1.