Supporting Figures and Tables Figure S1. Calculation of disparity for a time point on a hypothetical phylogenetic tree. For a particular time point, corresponding to the date of an interior node, disparity of an ecological trait is calculated for each existing clade (lineage) as the average Euclidian distance among the clade members, in regard to the trait(s) under consideration. In the figure, total disparity at time x, D(tx), is equal to the sum of the disparity values calculated for each of the two clades existing at time x, Dx, one clade with species 1 and 2 and the other with species 3 through 6, divided by the number of clades, C, which here is two. In a disparity through time analysis, values of disparity are determined for the date of each node along the phylogeny. Figure S2. Figure S2. Cumulative inertia explained by successive ordination axes for the Hill-Smith ordination of Eltonian variables and the Multiple Correspondence Analysis of the Grinnellian variables. Figure S3. Distribution of correlation coefficient values for comparisons among the axes of different ordinations. In each case, there seems to be no substantial correlation among the ordinations. a. b. c. Figure S4. Niche diversification on the maximum likelihood tree of phylogenetic relationships among 405 avian species of the western Palearctic. Color swaths represent species scores on the first eigenvector from ordinations of the climatic (red), habitat (blue) and trophic (green) components of the environmental niche. Species scores on each vector have been standardized to range from zero (maximum color intensity) to unity (white), and transformed to approximate a normal distribution. Clustering of color of similar intensity among closely related terminal nodes (species) indicates similar eigenvector scores, and suggests the presence of phylogenetic signal, notably in the trophic niche. Figure S5. Figure S5. Minimum discrimination index (MDI) scores. These box and whisker plots show the difference between curve values of observed node-specific disparity and disparity from Brownian simulations. Observations are MDI scores calculated for the difference between DDT curves for each of 100 trees and the mean of the corresponding Brownian evolution simulations. Bars show first quartiles and square points are outlying values. Table S1. Original variables used in the analyses on niche diversification. With the exception of body mass, all habitat and trophic niche variables were scored as used (1) or not used (0). Climate* Mean temperature Maximum temperature Minimum temperature Temperature coefficient of variation Mean precipitation Maximum precipitation Minimum precipitation Precipitation coefficient of variation Habitat Foraging Wet grassland, fens, tundra Dry grassland Rocky slope Fast lotic Still or slow lotic Near-shore marine Salt marsh Mud or silt flat Sand or gravel beach Reed marsh Conifer forest Deciduous forest Mixed forest Mediterranean or oak Open or low forest Forest edge Shrub, bush, brush Urban Garden High air . Nesting Wet grassland, fens, tundra Dry grassland Banks of sand or mud Near water, lakeshore, island Sand or gravel beach Reed marsh Conifer forest Deciduous forest Mixed forest Mediterranean or oak Open or low forest Shrub, bush, or brush Urban Garden Rock faces, outcrops, structures Nest position (elevated, hole, ground) Trophic . Seed, nuts, grain Frugivory Vegetative parts Invertebrates Fish Small mammals Large mammals Herptiles Vertebrates (unspec.) Small birds Large birds Large bones Carrion Pursuit (air, aquatic) Sally Foliage glean Pounce Graze Pick, peck, stab Dig Overturn objects Probe Water surface Underwater Water (unspecified) Mud Terrestrial ground Table S1. cont. Canopy Shrub Vegetation (unspec.) Air Nocturnal Crepuscular Diurnal Body mass Notes: * Climate variables are based on monthly averages during the six-month period, April through September, which are available from the WorldClim website, http://www.worldclim.org/. These are continuous variables, while all other variables except body weight are scored as Bernoulli variables. See text for scoring criteria. Table S2: Percentage of taxa (genera) represented in Genbank for each region included in the study Gene regions 12S 28S ATP6 ATP8 c-mos c-myc COI COII COIII Cyt b ND1 ND2 ND3 ND4 ND5 ND6 RAG1 RAG2 ZENK % of taxa sampled 63.9 9.6 37.4 27 31.8 34.1 79.6 16.1 21.3 96.7 30.3 82.9 37.9 20.9 31.3 31.3 62.6 17.1 25.1 Table S3: Fossil information and age constraints used in the dating analysis. All the fossils were used as minimum age constraints except *, which was used as a maximum age constraint. Clade Anseriformes Ingroup Apodiformes Upupidae+ Picidae Coraciidae+ Meropidae Pandionidae Sulidae Pteroclidae Rallidae Scolopaciade Strigidae Procellariidae Sulidae Burhinidae Age 66 125* 53 47.5 47.5 37 33 30 33 33 58 23 33 18 Stem/Crown Stem Stem Stem Stem Stem Crown Stem Stem Stem Stem Stem Stem Stem Stem References Clarke et al. (2005) Zhou (2004) Mayr (2003) Mayr (2000) Mayr & Mourer-Chauviré (2000) Harrison & Walker (1976) Mayr (2002) Mourer-Chauviré (1993) Mayr & Smith (2001) Olson (1985) Vickers-Rich & Bohaska (1976) Olson (1985) Mayr (2002) Bickart (1982) References Clarke, J.A., Tambussi, C.P., Noriega, J.I., Erickson, G.M. and Ketcham, R.A. (2005). "Definitive fossil evidence for the extant avian radiation in the Cretaceous." Nature, 433: 305- 308. Zhou. 2004. The origin and early evolution of birds: discoveries, disputes, and perspectives from fossil evidence. Naturwissenschaften 91: 455-471. Mayr, G. 2000. Tiny hoopoe-like birds from the Middle Eocene of Messel (Germany). Auk 117, 968-974. Mayr, G. 2003. Phylogeny of early Tertiary swifts and hummingbirds (Aves: Apodiformes). Auk 120, 145-151. Mayr, G. & Mourer-Chauviré, C. 2000. Rollers (Aves: Coraciiformes s.s.) from the Middle Eocene of Messel (Germany) and the Upper Eocene of the Quercy (France). J. Vert. Paleontol. 20, 533-546. Harrison, C. J. O. & Walker, C. A. 1976. Birds of the British Upper Eocene. Zool. J. Linnean Soc. 59, 323-351. Mayr, G. 2002. A skull of a new pelecaniform bird from the Middle Eocene of Messel, Germany. Acta Palaeontologica Polonica 47, 507-512. Mourer-Chauviré, C. 1993. Les gangas (Aves, Columbiformes, Pteroclidae) du Paléogène et du Miocène inférieur de France. Palaeovertebrata 22, 73-98. Mayr G, Smith R. 2001. Duck, rails, and limicoline waders from the lowermost Oligocene of Belgium. Geobios 34:547–561. Olson SL. 1985. The fossil record of birds. In: Farner D, editor. Avian Biology, London: Academic Press. p 80–238. Vickers-Rich P, Bohaska DJ. 1976. The world’s oldest owl: A new 1944 strigiform from the Paleocene of Southwestern Colorado. 1945 Smithsonian Contrib Paleobiol 27:87–93. Bickart KJ. 1982. A new thickknee, Burhinus, from the Miocene of Nebraska, with comments on the habitat requirements of the Burhinidae (Aves: Charadriiformes). J Vert Paleont 1:273 – 277.