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Patterns of diversification and timing of evolution within Neoaves, which includes almost 95% of all bird species, are virtually unknown. On the other hand, molecular data consistently indicate a Cretaceous origin of many neoavian lineages and the fossil record seems to support an Early Tertiary diversification. Here, we present the first well-resolved molecular phylogeny for Neoaves, together with divergence time estimates calibrated with a large number of stratigraphically and phylogenetically well-documented fossils. Our study defines several well-supported clades within Neoaves. The calibration results suggest that Neoaves, after an initial split from Galloanseres in Mid-Cretaceous, diversified around or soon after the K/T boundary. Our results thus do not contradict palaeontological data and show that there is no solid molecular evidence for an extensive pre-Tertiary radiation of Neoaves.
Birds are used as model organisms in many fields of biology, and the lack of a thorough understanding of their systematics has often compromised interpretations of experiments and observations. The DNA–DNA hybridization studies of Sibley & Ahlquist (1990) have repeatedly been criticized for methodological reasons (Harshman 1994; Cracraft et al. 2004), and the few cladistic analyses of Neoaves with dense taxon sampling show poor resolution of the deep divergences (Livezey & Zusi 2001; Cracraft et al. 2004; Fain & Houde 2004). DNA sequence data have begun to clarify interfamily relationships for a handful of higher level groups such as some aquatic birds (van Tuinen et al. 2001), ‘higher land birds’ (Johansson et al. 2001; Mayr et al. 2003), shorebirds (Ericson et al. 2003; Paton et al. 2003) and passerines (Barker et al. 2004). Recent analyses of morphological and molecular data support a sister group relationship between Galloanseres (land- and waterfowl) and all other neognathous birds, the Neoaves (Livezey & Zusi 2001; Mayr & Clarke 2003; Cracraft et al. 2004; Fain & Houde 2004). However, there are no hypotheses concerning the most basal neoavian divergences, except for the proposed division of the group into Metaves and Coronaves based on an analysis of β-fibrinogen sequence data (Fain & Houde 2004).
Molecular clock analyses have suggested that the earliest diversification of Neoaves had already occurred in the Cretaceous (Hedges et al. 1996; Cooper & Penny 1997; Cracraft 2001; van Tuinen & Hedges 2001). However, there are few neoavian fossils from the Cretaceous (Hope 2002; Feduccia 2003) and instead the palaeontological record suggests that only a few neoavian lineages existed at the end of the Cretaceous, 65Myr ago (Feduccia 2003). The considerable diversity of stem group representatives of modern neoavian taxa, which is evident in the Early Eocene 50Myr ago (Mayr 2005), would thus result from a rapid diversification of taxa, which filled the many vacant ecological niches after the K/T boundary (Feduccia 2003). There is an apparent conflict between earlier molecular datings and the palaeontological record—but is this conflict real? The molecular dating methods must be correctly calibrated to yield reliable data, and this has not previously been done in studies including Neoaves. Since all Cretaceous fossils of neornithine birds are very fragmentary (Hope 2002) and their identification is often uncertain (Hope 2002), most calibrations have so far used a calculated age for the split between galliforms and anseriforms (90Myr ago) which is in turn based on the diapsid/synapsid split age at 310Myr ago (Hedges et al. 1996). However, Graur & Martin (2004) have argued convincingly that this estimate is not reliable, and nor are any of the calibration points that are based on it. Here, we employ an alternative strategy and use multiple fossils of more recent neoavian groups as internal calibration points in order to test the different diversification models suggested by Penny & Phillips (2004).
Traditional classification recognizes 145 families in Neoaves (Morony et al. 1975). We obtained genomic DNA from blood or tissue samples of 87 neoavian species representing 75 families. Charadriiformes (shorebirds and allies, 19 families in total) and Passeriformes (passerines, 57 families in total), which have been shown to be monophyletic (Ericson et al. 2002, 2003; Paton et al. 2003; Barker et al. 2004), are represented by four and two families, respectively. At least one genus was sampled from the remaining neoavian families. Two palaeognaths (Rhea and Apteryx), one megapode and one screamer, were used as outgroups following the well-established hypothesis that Palaeognathae are the sister taxon of Neognathae, and that Galloanseres, in turn, are the sisters of Neoaves (Groth & Barrowclough 1999). The sample information and GenBank accession numbers are given in the electronic supplementary material.
The aligned dataset consists of 5007bp obtained from five gene regions: c-myc (exon 3), RAG-1, myoglobin (intron 2), β-fibrinogen (intron 7) and ornithine decarboxylase (introns 6 and 7, along with the intercepting exon 7). For laboratory procedures, alignments, selection of models for nucleotide substitutions, parsimony analysis and Bayesian analyses of individual gene regions, see electronic supplementary material.
Divergence times were estimated using two rate-smoothing methods, penalized likelihood (PL; Sanderson 2002) and PATHd8 (Britton et al. 2006). PL combines a model that overfits the data with a penalty for fast-rate changes between mother and daughter lineages. PATHd8 smoothes substitution rates between sister groups, instead of mother–daughter lineages, by sequentially taking averages over path lengths from an internode to all its descending terminals. Both PL and PATHd8 need one fixed calibration point. For this purpose, we used a 47.5-Myr-old stem group representative of hummingbirds. We also constrained the root of the tree (the stem species of extant birds) to a maximum age of 100Myr. An additional set of 21 stratigraphically and phylogenetically well-studied fossils were used as minimum age constraints. All the fossils used for calibrations (see electronic supplementary material) are stem group representatives of extant higher level taxa and provide a minimum age for the divergence of the total group (stem and crown group) from its sister taxon.
Our Bayesian analysis of the dataset resulted in a well-resolved and strongly supported topology defining several clades within Neoaves (figure 1). The obtained tree topologies, one from the combined data, one without β-fibrinogen and one based on β-fibrinogen only, are similar in many respects, providing further evidence for a strong phylogenetic signal in the analysed data (see electronic supplementary material).
The combined data support a basal dichotomy into Metaves and Coronaves as proposed by Fain & Houde (2004). However, monophyly of Metaves (doves, sandgrouse, mesites, flamingos, grebes, kagu, sunbittern, hoatzin, tropicbirds, swifts, treeswifts, hummingbirds and nightbirds) is retained only if the β-fibrinogen data are included. Moreover, our Bayesian analysis of the β-fibrinogen data alone did not provide a strong support for Metaves even though this group was originally defined in an analysis based on this gene (Fain & Houde 2004). We obtained strong support for Metaves only after the inclusion of all genes, which shows that all or some other genes also contain a phylogenetic signal for Metaves, albeit this signal seems to be weak. Our data also strongly support the recently suggested flamingo–grebe clade (van Tuinen et al. 2001; Cracraft et al. 2004; Mayr 2004).
All trees support a clade including nightbirds (the traditional ‘caprimulgiforms’ but not owls) and apodiform birds (swifts and hummingbirds; figure 1, node 1). Our results confirm a sister group relationship between the owlet-nightjars and Apodiformes (Mayr 2002; Cracraft et al. 2004), and for the first time, suggest monophyly of a clade that includes all the taxa traditionally placed in ‘Caprimulgiformes’ and Apodiformes. The obtained topology suggests that the diurnal Apodiformes evolved within a radiation of nocturnal birds, indicating a nocturnal ancestor of Apodiformes.
Strongly supported is a previously unrecognized major clade (Johansson et al. 2001; Mayr et al. 2003), which includes diurnal birds of prey, seriemas, parrots and the ‘higher landbird assemblage’ (figure 1, node 2). For the majority of families, traditionally included in the orders Coraciiformes and Piciformes (figure 1, node 3), the same internal relationships have been recovered as in other recent molecular analyses (Johansson et al. 2001; Johansson & Ericson 2003; Mayr et al. 2003).
In concordance with other recent analyses (Sibley & Ahlquist 1990; Cracraft et al. 2004; Fain & Houde 2004), our data recover a clade (figure 1, node 4) that includes the secretarybird and accipitrid diurnal birds of prey (osprey, hawks and allies) to the exclusion of falcons. This grouping is recovered in separate analyses of four of the five investigated genes. The New World vultures clearly have their affinity with other raptors and not with storks (contra, e.g. Sibley & Ahlquist 1990).
Another well-supported clade includes birds with various aquatic or semi-aquatic adaptations (figure 1, node 5), as well as, in unresolved basal positions, the terrestrial turacos, bustards and cuckoos. The well-supported groupings within this clade are the ‘core-gruiforms’ (i.e. cranes, limpkin, rails, finfoots and trumpeters; figure 1, node 6), procellariiforms (albatrosses, storm-petrels, diving petrels, petrels and shearwaters; figure 1, node 7) and a group consisting of the anhingas, cormorants, gannets and frigatebirds (figure 1, node 8). As suggested previously, pelicans group not only with shoebill and hamerkop (Cottam 1957; Livezey & Zusi 2001; van Tuinen et al. 2001; Cracraft et al. 2004), but also with herons and ibises. Penguins, loons and storks also belong to this clade. The results confirm that the traditional Pelecaniformes and Ciconiiformes are not monophyletic. The shorebirds (figure 1, node 9) are in an unresolved position relative to the two major clades of terrestrial/arboreal and aquatic/semi-aquatic groups, respectively.
The PATHd8 analysis suggests that although the earliest diversification of Neoaves took place in the Late Cretaceous, the majority of higher level phylogenetic splits in Neoaves occurs after the K/T boundary (figure 2). The pattern of divergence obtained from PATHd8 and PL is similar with both the methods. However, PL adds an average ‘ghost range’ of 21Myr to all the fossil records, and hence provides systematically older ages. We therefore consider the PATHd8 result to be the more reliable one (a comparison between the PATHd8 and the PL chronograms, and age estimates for major bird groups, are placed in the electronic supplementary material). The differences between the results of the PATHd8 and PL analyses leave open the question of how many stem lineages of neoavian birds existed before the K/T boundary. While the PATHd8 analysis suggests that there were only a few (model 2 of Penny & Phillips 2004), the PL analysis (see electronic supplementary material; Figure 9) indicates that there may have been more lineages of which some may have already obtained the ecological adaptation of their crown group representatives (model 4 of Penny & Phillips 2004). The present reconstruction of the phylogeny and divergence times of Neoaves accounts for both molecular and palaeontological data. It disagrees with the claim that molecular data indicate a deep Cretaceous diversification of neoavian birds (cf. Hedges et al. 1996; van Tuinen & Hedges 2001; corresponding to model 5 of Penny & Phillips 2004).
For help in the laboratory we thank Krzysia Nowak and Lukasz Pasko at the University of Wroclaw, and Martin Irestedt and Elisabeth Ko¨ster at the Swedish Museum of Natural History. We are grateful to the following institutions and people for granting access to blood and tissue samples: Australian Museum, Sydney; Academy of Natural Sciences, Philadelphia; Field Museum, Chicago; Louisiana Museum of Natural Science, Baton Rouge; Museum Victoria, Melbourne; National Museum of Natural History, Windhoek; Swedish Museum of Natural History, Stockholm; Percy Fitzpatrick Institute of African Ornithology, Cape Town; Senckenberg Museum, Frankfurt; Burke Museum of Natural History and Culture, Seattle; Zoological Museum, University of Copenhagen; Susie Dunham and Christophe Lambert. This work has been funded by the Swedish Research Council (grant no. 621-2004-2913 to P.E.) and Poland's Committee for Scientific Research (KBN) (grant no. 3 PO4C 069 25 to A.E). We also acknowledge the support of a SYNTHESYS grant to G.M. (SE-TAF-646) made available by the European Community - Research Infrastructure Action under the FP6 Structuring the European Research Area Program.