Subsequently, we divided the entire period into four distinct intervals and applied the Wilcoxon test to compare derivatives among the four taxa across these intervals: (i) before the PGM (~140 ka), when global temperatures exhibited a declining trend (200 to 140 ka); (ii) from the PGM to the LIG (140 to 120 ka), characterized by an increasing trend in global temperatures; (iii) from the LIG to the LGM (120 to 19 ka), marked by a decline in global temperatures; and (iv) after the LGM (19 to 10 ka), when global temperatures exhibited an increasing trend.
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Global spatiotemporal patterns of demographic fluctuations in terrestrial vertebrates during the Late Pleistocene.
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