Figure 2.

Bayesian phylogeny in kākāpō for full mitogenomes (16,588 bp). Timing of events was estimated assuming a substitution rate of 1–3 × 10⁻⁸ site⁻¹ year⁻¹ [39]. The x-axis is in calendar years before present and nodes with posterior probability larger than 0.7 are depicted. Maps show the extent of ice during (white) and after the last glacial maximum (LGM) (after [49]).