Computational estimates of activity periods (normal distributions displayed as ovals29) of selected retroposon subtypes were calculated using the TinT model2529 and plotted on a simplified chronogram30 (black lines) using the experimentally verified retroposon insertion events (numbered blue or red balls, numbers indicate the respective retroposon subtype) of Figure 1 as temporal landmarks. Single capital letters correspond to the branch labels of Figure 1 (A, Aves; B, Neognathae; D, Neoaves; F, incongruent markers; G, 'landbirds'; H, 'landbirds' without mousebirds; I, Eufalconimorphae+seriemas; J, Eufalconimorphae; K, Psittacopasserae; L, Passeriformes). CR1 retroposons are highlighted in blue and LTR retroposons are shown in red. The dashed bracket consists of retroposon markers that were inserted during the neoavian radiation; the grey dashed vertical line indicates the estimated end of the Mesozoic Era at the Cretaceous/Tertiary boundary30. We note that the exceptionally long TinT activity range of the CR1-E_Pass element (no. 4) is most probably an overestimation because of CR1 subfamily misidentification, as only a few diagnostic nucleotides distinguish this retroposon from other CR1 subfamilies.