So tell me what you would like to know about the article.
Since nobody has given me a clue so far, I'll post the "highlights"
and the "Summary and Conclusions." The latter is LONG!
Highlights
► The origin of Cetacea (whales) represents a key macroevolutionary transition within Mammalia. ► We assess the distribution of support among molecular datasets for Artiodactyla relationships. ► Three supermatrices of molecular and fossil data yield a composite phylogenetic hypothesis. ► We infer a phylogenetic blueprint that outlines the stepwise evolution of modern whales.
3.4. Summary and conclusions
The current analysis represents a first attempt at combining genomic and paleontological data to derive a wide-ranging phylogenetic hypothesis for Cetacea (Fig. 7) and a unified reconstruction of the many evolutionary novelties that characterize this group (Fig. 2). Crown cetaceans such as Physeter macrocephalus and Balaenoptera musculus (Fig. 1) are highly derived outliers relative to the majority of extant mammalian species, most of which are furry, four-limbed, terrestrial, and miniscule in comparison (Fig. 4). The phenotypic divide between extant cetaceans and even their closest living relatives (Figs. 1C and 5) indicates that extinction has erased much of the historical evidence of whale evolution. Luckily, recent fossil finds have contributed to a rapidly growing inventory of extinct taxa that fill in wide anatomical gaps (Fig. 3). To make sense of this diversity, however, the fossil record of whales must be organized phylogenetically to distinguish primitive from derived states and to reconstruct long sequences of anatomical transformation. Many paleontologists have attacked this problem through phylogenetic analysis of morphological characters, the only systematic evidence that can be garnered from whale fossils (e.g., Geisler and Sanders, 2003, Theodor and Foss, 2005, Thewissen et al., 2007, Fitzgerald, 2010, Marx, 2010), but the results often have been incongruent with trees based on large matrices of molecular data (e.g., Gatesy, 1998, McGowen et al., 2009, Steeman et al., 2009; Zhou et al., 2011a, Zhou et al., 2012).
The past two decades have seen the emergence and pre-eminence of genomic data in systematics (Delsuc et al., 2005), perhaps due to the sheer quantity of available data, the simplicity of nucleotide characters, as well as the tractability of molecular evolution models utilized in phylogenetic analysis, but a sole reliance on DNA sequences has limitations as a general approach to reconstructing the history of Life. Molecular systematic hypotheses that place cetaceans in the context of extant mammalian diversity (Fig. 4, Fig. 5) represent ‘phylogenetic skeletons’ that are woefully incomplete in terms of documenting key anatomical transitions, and ironically must be fleshed out by the addition of fossilized bones. DNA sequences cannot be recovered from most extinct taxa, making genetic data relatively impotent with regard to the placement of fossils. Furthermore, despite the huge weight of character evidence provided by genomic information, morphological data can overturn phylogenetic hypotheses based on large compilations of molecular data. Although likely to be rare in the age of comparative genomics, this possibility was demonstrated here; the addition of only 115 phenotypic characters overturned a topology for Mysticeti supported by analysis of >30,000 molecular characters (Fig. 6).
Our research group and collaborators have therefore committed the past decade to merging morphology and molecules in combined supermatrix studies of Cetacea to reconcile paleontological and genomic evidence (Gatesy and O’Leary, 2001, O’Leary et al., 2004, Deméré et al., 2005, Deméré et al., 2008, Geisler and Uhen, 2005, Geisler et al., 2007, Geisler et al., 2011, O’Leary and Gatesy, 2008, Geisler and Theodor, 2009, Spaulding et al., 2009). In this more inclusive approach to systematics, phenotypic characters coded from extant taxa provide the critical link of homologies that connect phenotypic characters from fossils to molecular data from extant taxa. We have examined whale phylogeny at several hierarchical scales. Here, results from these supermatrix studies were merged to yield a single composite phylogenetic tree that encompasses the early derivation of whales as well as the subsequent diversification of crown group cetaceans (Fig. 7). The overall topology represents a phylogenetic blueprint for modern cetaceans, a hypothesis that summarizes the approximate age and relative sequence of changes that have occurred in the evolutionary construction of extant whales over the Cenozoic (Fig. 8, Fig. 9; Table 1). Due to the inclusion of genomic data, our hypothesis disagrees with trees based on morphology alone in the deep nesting of Cetacea within Artiodactyla as well as contrasting relationships within both Odontoceti and Mysticeti. The rearrangement of extant lineages, in turn, forces a reinterpretation of anatomical homologs and alters the placement of extinct taxa in the tree.
The importance of morphological characters, particularly fossil data, is evident in a summary topology that tracks the evolutionary lineage that terminates at Balaenoptera musculus (Fig. 10). Based on molecular data alone, it is impossible to discern the relative order of the many important evolutionary modifications (Fig. 2) that have culminated in this remarkable species. The ancestral lineage that connects the basal node of Artiodactyla to the extant blue whale traverses 30 branch points in our composite tree, but only 9 of the 30 side branches include lineages that extend to the living biota (Fig. 7). Numerous extinct side branches permit reconstruction of a more fine-grained sequence of evolutionary change (Gauthier et al., 1988, Donoghue et al., 1989). Our summary of the available evidence (Fig. 7, Fig. 8, Fig. 9, Fig. 10; Table 1) implies that a double-trochelated astragalus, the fibro-elastic penis, and a multi-chambered stomach evolved deep in the history of Cetacea over 60 million years ago (branches A–B), and that these changes were followed by the derivation of several “aquatic” specializations (sparse hair, loss of sebaceous glands, ability to nurse and birth underwater) in the common ancestor of Cetacea and Hippopotamidae (branch C) (Fig. 8). Over the next ∼20 million years, the involucrum (branch D), simplification of the dentition (branch E), a robust tail (branch E), an enlarged mandibular foramen (branch F), the transition to saltwater (branches F–G), shortened neck vertebrae (branch H), separation of the pelvis from the vertebral column (branch L), posterior migration of the external nares (branch L), vestigial hindlimbs (branches K–M), reduction of elbow flexion (branch O), and many additional specializations evolved sequentially on the stem lineage to crown Cetacea (Table 1). From ∼35–28 million years ago, the key anatomical traits that characterize filter-feeding whales were derived in succession on the stem to crown Mysticeti (Fig. 9): a broad rostrum (branch a), an unsutured mandibular symphysis (branches b–c), palatal nutrient foramina and by inference baleen (branch c), loss of mineralized teeth (branch d), and bowed mandibles (branch e). Features that are unique to the engulfment feeding apparatus of balaenopterids (pleated throat pouch, reduced tongue, fibrous temporomandibular joint) and unprecedented body size evolved later, within crown group Mysticeti (branches g and h; Fig. 9). Balaenoptera musculus displays a mosaic of features acquired at various time depths over the past ∼60 million years of artiodactyl evolution; our composite tree summarizes the age and phylogenetic generality of the various traits that characterize this highly derived species (Fig. 10).
Our hypothesis should be considered a starting point toward a more comprehensive phylogenetic analysis of whale origins and diversification. We see several obvious ways that improvements can be achieved. First, taxonomic sampling can be expanded. Several recent supermatrix studies have included nearly all extant species of Cetacea, but these efforts focused on molecular data (McGowen et al., 2009, Steeman et al., 2009; Slater et al., 2010). DNA sequences have been published for over 90 extant species, but effective integration of these data with the fossil record of Cetacea will require coding morphological characters from many more extant taxa to provide an overlap of systematic information. In terms of fossils, the sampling of extinct taxa in our composite tree focused on filling gaps on the stem lineages of Odontoceti, Mysticeti, Cetacea, Ruminantia, Suina, and Camelidae (Fig. 7). However, >700 wholly extinct artiodactyl genera have been described (McKenna and Bell, 1997, O’Leary et al., 2004). Many additional extinct taxa should be coded to yield a more detailed evolutionary reconstruction. Second, it would be preferable to compile a single supermatrix with a broadly applicable set of phenotypic characters that characterizes variation across both deep and shallow divergences within Artiodactyla. The present supertree of three supermatrix topologies (Fig. 7) is based on several assumptions of monophyly that would not be required if the same phenotypic characters were coded for all relevant taxa. This is a challenging task, but a recent effort to compile a morphological matrix across all mammalian orders demonstrates that several thousand phenotypic characters from diverse taxa can be scored with the aid of modern web-based tools (O’Leary and Kaufman, 2007) and cooperation among taxonomic specialists (Novacek et al., 2008). Third, genomic resources now permit a mapping of critical molecular changes that correlate with the unique specializations and degenerative features of whales. Recent studies of DNA sequences from Cetacea have documented convergent changes in the auditory genes of echolocating cetaceans and bats (Li et al., 2010, Liu et al., 2010, Davies et al., 2012), as well as adaptive evolution of brain development genes (McGowen et al., 2011, McGowen et al., 2012, Xu et al., 2012) and Hox loci involved in forelimb development (Wang et al., 2009). Other work has characterized patterns of pseudogenization in Cetacea that parallel evolutionary losses at the phenotypic/behavioral level, including mutational decay of genes related to color vision (Levenson and Dizon, 2003), enamel formation (Deméré et al., 2008, Meredith et al., 2009, Meredith et al., 2011b), olfaction (Kishida et al., 2007, McGowen et al., 2008, Hayden et al., 2010), taste (Jiang et al., 2012), and vomeronasal chemoreception (Yu et al., 2010). Further efforts that tie particular anatomical transformations to underlying molecular change will contribute to the emerging macroevolutionary synthesis.
[beautiful Fig. 10 with long caption omitted]
As phylogenetics proceeds into the twenty-first century, a focus has been rightly placed on genome-scale datasets because of the nearly limitless supply of discrete systematic characters (Delsuc et al., 2005). Regardless, many neontologists recently have come to the realization that, moving forward, paleontological data will be essential for phylogenetic analysis, divergence dating, estimation of diversification and extinction rates, biogeography, and the mapping of particular phenotypic traits (Wiens, 2009, Losos, 2011, Pyron, 2011, Slater et al., 2012). These revelations are not really new (Gauthier et al., 1988, Donoghue et al., 1989, Novacek, 1992, Novacek and Wheeler, 1992, Smith and Littlewood, 1994, Smith, 1998), but instead indicate that even with the development of ‘sophisticated’ likelihood models, genomic data can advance the field only so far. We predict a blossoming relationship between paleontology and genomics in the coming years, with the hope that a more complete phylogenetic reconstruction of Life, including its many extinct lineages, will be achieved.