The interplay of evolution and development has been at the heart of evolutionary theory for more than a century1.
Heterochrony—change in the timing or rate of developmental events—has
been implicated in the evolution of major vertebrate lineages such as
mammals2, including humans1. Birds are the most speciose land vertebrates, with more than 10,000 living species3
representing a bewildering array of ecologies. Their anatomy is
radically different from that of other vertebrates. The unique bird
skull houses two highly specialized systems: the sophisticated visual
and neuromuscular coordination system4, 5
allows flight coordination and exploitation of diverse visual
landscapes, and the astonishing variations of the beak enable a wide
range of avian lifestyles. Here we use a geometric morphometric approach
integrating developmental, neontological and palaeontological data to
show that the heterochronic process of paedomorphosis, by which
descendants resemble the juveniles of their ancestors, is responsible
for several major evolutionary transitions in the origin of birds. We
analysed the variability of a series of landmarks on all known theropod
dinosaur skull ontogenies as well as outgroups and birds. The first
dimension of variability captured ontogeny, indicating a conserved
ontogenetic trajectory. The second dimension accounted for phylogenetic
change towards more bird-like dinosaurs. Basally branching
eumaniraptorans and avialans clustered with embryos of other archosaurs,
indicating paedomorphosis. Our results reveal at least four
paedomorphic episodes in the history of birds combined with localized
peramorphosis (development beyond the adult state of ancestors) in the
beak. Paedomorphic enlargement of the eyes and associated brain regions
parallels the enlargement of the nasal cavity and olfactory brain in
mammals6.
This study can be a model for investigations of heterochrony in
evolutionary transitions, illuminating the origin of adaptive features
and inspiring studies of developmental mechanisms.
Birds are living theropod dinosaurs and are one branch of
Archosauria (‘ruling reptiles’), the other major branch of which
consists of extant crocodylians and their stem lineage (Fig. 1a)7.
Archosaurs diversified into several body plans on their divergence from
the lizard/snake (lepidosaur) lineage in the Palaeozoic, including many
adapted to macropredation7. Skulls of crocodylians (Fig. 1b) and early dinosaurs such as Coelophysis (Fig. 1c)
undergo considerable ontogenetic change, the juveniles displaying the
typical juvenile amniote features of relatively short facial
(antorbital) regions and large brains and eyes. In contrast, basally
branching members of the dinosaur clade Eumaniraptora, which includes Archaeopteryx and modern birds, seem to change little from juvenile to adult. The Eichstätt and Berlin specimens of Archaeopteryx (Fig. 1d)
are nearly identical cranially despite the fact that the former is half
the size of the latter and is ontogenetically the youngest of the known
specimens8, 9. Extant birds show a similar dearth of change10.
Birds (here referring to the extant radiation) and their close
relatives thus seem to be paedomorphic, retaining a morphology as adults
that resembles that of the juveniles or embryos of most other
archosaurs. This paedomorphosis is most evident in their relatively
enormous eyes and enlarged brains, especially those regions correlated
with visual function4, 11, 12, 13.
Given these qualitative indications that bird skulls are
paedomorphic, we tested this hypothesis with a principal-component
analysis (PCA) of shape variation sampled broadly across theropods,
using original photographs and computed tomography (CT) scans when
possible, and novel or published reconstructions when this was not
possible (Supplementary Information).
To incorporate ontogeny into the analysis, we included all published
juvenile–adult pairs or series of non-avian theropods, as well as
selected modern birds and Alligator. Note that some of the
juvenile–adult pairs—compsognathids and therizinosaurs, part of the
tyrannosaur series—use different but closely related taxa. The stem
archosaur Euparkeria was also included7.
Forty-five landmarks (Supplementary Fig. 1)
provided a comprehensive coverage of the lateral view of the cranium,
the only view represented in some of the most important specimens, which
are two-dimensionally crushed. New data including an undescribed
perinate of the oviraptorid Citipati and CT scans of birds and crocodylians were employed.
The
first two principal components (PCs) of the PCA explained 42.75% and
13.82% of the variation in the sample, respectively; all others
explained less than 10% (Fig. 2). The first of these two principal axes (PC1) largely accounted for ontogenetic change, revealing a conserved pattern of transformation across archosaurs (Supplementary Fig. 2 and Supplementary Information. Note, however, novel ontogenetic transformation related to gigantism in advanced tyrannosaurs; Supplementary Information and Supplementary Fig. 8). The second axis captured transformations between primitive archosaurs and the coelurosaurian theropods. PC1,
in the direction of ontogenetic growth, describes the extension of the
face, the relative diminution of orbit and neurocranium, and a
constriction in the lower temporal fenestra (Fig. 2 and Supplementary Movie). PC2,
towards coelurosaurian theropods, describes dorsoventral narrowing of
the face, alterations in orbital and premaxillary shape, neurocranial
enlargement, and the characteristic posteroventral rotation of the
braincase seen during evolution towards birds14 (Fig. 2 and Supplementary Movie).
Taxonomic and functional groups separate along the axes (Fig. 2 and Supplementary Fig. 5). Early archosaurs cluster away from the more advanced theropods along PC2. Giant theropods group together (Supplementary Fig. 6),
a result consistent with those of a recent morphometric analysis of
theropod skulls that excluded avialans and ontogenies, and used 24
landmarks15. Basally branching eumaniraptorans and avialans cluster, as do crown-clade birds. The early ornithurine Yixianornis
spans the gap between these clusters, as might be expected
phylogenetically. The morphologically disparate oviraptorosaurs occupy a
unique region of the morphospace, separated from the other groups by
their position along PC2. An analysis without oviraptors yielded the same major clusters as the inclusive analysis (Supplementary Information and Supplementary Fig. 9).
Evidence
for heterochrony is clear. Whereas adults of taxa distantly related to
birds (non-eumaniraptorans) cluster together, basally branching bird
relatives (eumaniraptorans) cluster with the embryos and youngest
juveniles of other non-avian archosaurs (Figs 2 and 3), with the more crownward avialan Confuciusornis nearly identical to embryos and particularly close to the perinate enantiornithine (Figs 3d and 4).
The cluster of eumaniraptorans and non-avian embryos is widely
separated from the adult cluster. Only a few specimens, all juvenile,
intervene (Supplementary Fig. 6 and Supplementary Information). Groupings are confirmed by minimum-spanning-tree analysis (Supplementary Information and Supplementary Fig. 4). The clustering of adult early bird relatives with the youngest individuals of more basal archosaurs (Figs 2–4) supports the hypothesis of paedomorphosis. Moreover, at least four heterochronic transformations are evident (I–IV in Figs 1 and 5; see also Supplementary Information),
although additional sampling along the avian stem might reveal more
transitions: I, paedomorphosis between other theropods and
Eumaniraptora; II, paedomorphosis between Eumaniraptora and Confuciusornis;
III, general paedomorphosis plus localized peramorphosis (growth beyond
the state in adult ancestors) in the premaxillary beak, between Confuciusornis and Yixianornis; and IV, paedomorphosis between Yixianornis and Aves. Before transformationI, a phylogenetic sequence moves largely along PC2, before taking an abrupt 90° turn to move in the reverse-ontogenetic direction along PC1 (Fig. 5).
Extant birds are truly extreme, falling farther in that direction than
late embryos and perinates of more conservative archosaurs (Fig. 3f, g).
The paedomorphic trend holds even after size and phylogeny are statistically accounted for (Supplementary Information and Supplementary Figs 3–5). Compsognathus
is tiny, yet as a non-eumaniraptoran it falls within the ancestral
adult cluster; small size alone does not result in paedomorphic
morphology. Struthio and Dromaius are large but group with
other birds. Transformations II–IV occurred among animals that were
roughly the same size. Transformation I, however, was accompanied by a
marked reduction in size.
A regression of shape change on centroid size as a proxy for ontogenetic time (Fig. 6 and Supplementary Information)
demonstrates that birds and their close relatives (eumaniraptorans)
have shorter ontogenetic trajectories along the PC axes (see also Supplementary Table 1 and the similarity of ontogenetic trajectories indicated by Supplementary Tables 3 and 4)
than all other included archosaurs. These short trajectories are
consistent with histological data that suggest that sexual and somatic
maturation times were truncated during each heterochronic transformation
(Supplementary Fig. 10 and Supplementary Table 2)16. As expected, compsognathids show an ancestral magnitude of shape change (along the y axis) despite their small adult size, whereas Struthio
shows a bird-like magnitude despite its giant size. The aggregate of
evidence suggests paedomorphosis by progenesis, early somatic maturation
resulting in a truncated ontogeny17. Paedomorphosis by truncation is also supported by the position of secondarily larger-bodied eumaniraptorans—Byronosaurus, Zanabazar and Velociraptor—in the PCA. These animals were derived from much smaller, possibly volant, ancestors18.
They have (secondarily) long ontogenetic trajectories and their adults
cluster with advanced maniraptorans that diverged from the bird lineage
before transformationI.
Strong support for a progenetic paedomorphic origin of the bird
skull seemingly contradicts early work suggesting that simple
paedomorphosis in the form of having “retained a juvenile shape” was not
involved in the origin of the bird skeleton16.
That work, however, discussed the postcranial skeleton. Birds do show
several peramorphic features in their postcranial skeletons; however,
direct comparison with fossil taxa is difficult because substantially
complete embryonic postcrania are even rarer than skulls. Cranial
evolution is modular with respect to the rest of the body and it is not
unusual to find divergent rates of transformation between crania and
postcrania, for instance in the origins of pterodactyloid pterosaurs19 and the origin of mammals20, 21.
Despite
the overwhelming imprint of paedomorphosis on the evolution of the bird
skull in the collapse of the face and the enlargement of the brain,
peramorphosis also occurs to form the distinctive elongate avian beak
during transformationIII (Figs 3 and 5)17, 22.
In addition, birds do not have embryonic brains. Instead, the neuronal
complexity of their brains is elaborated relative to that of ancestral
archosaurs23.
Whereas the larger relative brain size is a paedomorphic feature, the
elaboration of the neural tissue, in particular the optic regions,
represents a more complex heterometric change14.
The brain emerges in this analysis as a major driver of theropod cranial anatomy (Fig. 5)23, 24.
Cranial transformations driven by optic elaboration during the origin
of birds parallel olfactory elaboration during mammalian origins23. The brain is an early signalling centre during facial development25
and it is possible that the posteroventral rotation of the brain is in
part responsible for the collapse of the facial region in birds. Archaeopteryx-like
elaboration of visually associated brain regions also appears in
Eumaniraptora and may be correlated with some degree of volancy26. Although it has been suggested that reduction in body size, which we show accompanied heterochronic transformationI, was associated with the advent of dinosaurian flight16, our results agree with work suggesting that size reduction preceded powered flight18.
This reduction may, however, have been a necessary precursor to flight
exapted in its service. The origin of flight was a multistep process and
it remains unclear precisely when volancy and powered flight
respectively originated18. Finally, the peramorphic enlargement of the premaxilla to form a long, pointed beak (Fig. 5 and Supplementary Movie) is coupled with progressive loss of manual grasping ability as digits became bound into the wing27. Modern birds are known to perform fine manipulations with the precision tips of their beaks28. It may be that the beak evolved in part as a replacement for the eponymous raptorial hands of maniraptoran dinosaurs.
We
have provided a powerful new example of how heterochronic changes,
paedomorphic and peramorphic, were crucial in the origin and evolution
of birds29.
We further demonstrate that these changes were driven by an extreme
degree of elaboration in vision-associated areas of the brain that
parallels the olfactory elaboration of mammals, and possibly by the
evolution of the face into a precision grasping mechanism as the hands
were co-opted for flight.
Skull images were obtained from published literature.
Original CT scans performed at the University of Texas High-Resolution
X-Ray Scanning Facility (UTCT) and at the Harvard Center for Nanoscale
Systems, photographs and novel reconstructions are detailed in the Supplementary Information.
Scaling and digitization of landmarks used tpsDIG, and PCA was
performed with the software packages TPSRelW, MorphoJ and PAST (see Supplementary Information
for full citations). Size regression was performed and evolutionary
data were obtained using MorphoJ. Full methods are provided in Supplementary Methods.
Department of Organismic and Evolutionary Biology, Harvard University, 16Divinity Avenue, Cambridge, Massachusetts 02138, USA
Bhart-Anjan S. Bhullar,
Fernando Racimo &
Arhat Abzhanov
Unidad de Paleontología, Departamento de Biología, Universidad Autónoma de Madrid, 28049 Cantoblanco (Madrid), Spain
Jesús Marugán-Lobón
Department of Anatomy, New York College of Osteopathic
Medicine of New York Institute of Technology, Old Westbury, New York
11568-8000, USA
Gabe S. Bever
Department of Geological Sciences, Jackson School of Geosciences, The University of Texas at Austin, 1University Station C1100, Austin, Texas 78712, USA
Timothy B. Rowe
Division of Paleontology, American Museum of Natural History,
Central Park West at 79th Street, New York, New York 10024-5192, USA
Mark A. Norell
Contributions
B.-A.S.B. and A.A. designed the study. B.-A.S.B. wrote the paper
and performed CT scans, data entry and analytical work. J.M.-L.
performed analytical work and assisted with writing and figures. F.R.
performed data entry and analytical work. G.B. helped conceive the
project and performed data processing on new CT data. T.B.R. contributed
CT data and assisted in data interpretation and writing the paper.
M.A.N. contributed the major hypotheses to be tested, provided CT data
and assisted in writing the paper. A.A. co-wrote the paper.
Competing financial interests
The authors declare no competing financial interests.
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