Vascularization in Ornamented Osteoderms: Physiological Implications in Ectothermy and Amphibious Lifestyle in the Crocodylomorphs?

Vascularization in the core of crocodylian osteoderms, and in their superficial pits has been hypothesized to be a key feature involved in physiological thermoregulation and/or acidosis buffering during anoxia (apnea). However, up to now, there have been no quantitative data showing that the inner, or superficial, blood supply of the osteoderms is greater than that occurring in neighboring dermal tissues. We provide such data: our results clearly indicate that the vascular networks in both the osteoderms and the pits forming their superficial ornamentation are denser than in the overlying dermis. These results support previous physiological assumptions and indicate that vascularization in pseudosuchian (crocodylians and close relatives) ornamented osteoderms could be part of a broad eco-physiological adaptation towards ectothermy and aquatic ambush predation acquired by the crocodylomorphs during their post-Triassic evolution. Moreover, regressions demonstrate that the number of enclosed vessels is correlated with the sectional area of the cavities housing them (superficial pits and inner cavities). These regressions can be used to infer the degree of vascularization on dry and fossilized osteoderms and thus document the evolution of the putative function of the osteoderms in the Pseudosuchia. Anat Rec, 2017. © 2017 Wiley Periodicals, Inc. Anat Rec, 301:175-183, 2018. © 2017 Wiley Periodicals, Inc.

Does skull morphology constrain bone ornamentation? A morphometric analysis in the Crocodylia.

Previous quantitative assessments of the crocodylians' dermal bone ornamentation (this ornamentation consists of pits and ridges) has shown that bone sculpture results in a gain in area that differs between anatomical regions: it tends to be higher on the skull table than on the snout. Therefore, a comparative phylogenetic analysis within 17 adult crocodylian specimens representative of the morphological diversity of the 24 extant species has been performed, in order to test if the gain in area due to ornamentation depends on the skull morphology, i.e. shape and size. Quantitative assessment of skull size and shape through geometric morphometrics, and of skull ornamentation through surface analyses, produced a dataset that was analyzed using phylogenetic least-squares regression. The analyses reveal that none of the variables that quantify ornamentation, be they on the snout or the skull table, is correlated with the size of the specimens. Conversely, there is more disparity in the relationships between skull conformations (longirostrine vs. brevirostrine) and ornamentation. Indeed, both parameters GApit (i.e. pit depth and shape) and OArelat (i.e. relative area of the pit set) are negatively correlated with snout elongation, whereas none of the values quantifying ornamentation on the skull table is correlated with skull conformation. It can be concluded that bone sculpture on the snout is influenced by different developmental constrains than on the skull table and is sensible to differences in the local growth 'context' (allometric processes) prevailing in distinct skull parts. Whatever the functional role of bone ornamentation on the skull, if any, it seems to be restricted to some anatomical regions at least for the longirostrine forms that tend to lose ornamentation on the snout.

Testing gradual and speciational models of evolution in extant taxa: the example of ratites.

Ever since Eldredge and Gould proposed their model of punctuated equilibria, evolutionary biologists have debated how often this model is the best description of nature and how important it is compared to the more gradual models of evolution expected from natural selection and the neo-Darwinian paradigm. Recently, Cubo proposed a method to test whether morphological data in extant ratites are more compatible with a gradual or with a speciational model (close to the punctuated equilibrium model). As shown by our simulations, a new method to test the mode of evolution of characters (involving regression of standardized contrasts on their expected standard deviation) is easier to implement and more powerful than the previously proposed method, but the Mesquite module comet (aimed at investigating evolutionary models using comparative data) performs better still. Uncertainties in branch length estimates are probably the largest source of potential error. Cubo hypothesized that heterochronic mechanisms may underlie morphological changes in bone shape during the evolution of ratites. He predicted that the outcome of these changes may be consistent with a speciational model of character evolution because heterochronic changes can be instantaneous in terms of geological time. Analysis of a more extensive data set confirms his prediction despite branch length uncertainties: evolution in ratites has been mostly speciational for shape-related characters. However, it has been mostly gradual for size-related ones.

Phylogenetic signal in bone microstructure of sauropsids.

In spite of the fact that the potential usefulness of bone histology in systematics has been discussed for over one and a half centuries, the presence of a phylogenetic signal in the variation of histological characters has rarely been assessed. A quantitative assessment of phylogenetic signal in bone histological characters could provide a justification for performing optimizations of these traits onto independently generated phylogenetic trees (as has been done in recent years). Here we present an investigation on the quantification of the phylogenetic signal in the following bone histological, microanatomical, and morphological traits in a sample of femora of 35 species of sauropsids: vascular density, vascular orientation, index of Haversian remodeling, cortical thickness, and cross-sectional area (bone size). For this purpose, we use two methods, regressions on distance matrices tested for significance using permutations (a Mantel test) and random tree length distribution. Within sauropsids, these bone microstructural traits have an optimal systematic value in archosaurs. In this taxon, a Mantel test shows that the phylogeny explains 81.8% of the variation of bone size and 86.2% of the variation of cortical thickness. In contrast, a Mantel test suggests that the phylogenetic signal in histological traits is weak: although the phylogeny explains 18.7% of the variation of vascular density in archosaurs, the phylogenetic signal is not significant either for vascular orientation or for the index of Haversian remodeling. However, Mantel tests seem to underestimate the proportion of variance of the dependent character explained by the phylogeny, as suggested by a PVR (phylogenetic eigenvector) analysis. We also deal with some complementary questions. First, we evaluate the functional dependence of bone vascular density on bone size by using phylogenetically independent contrasts. Second, we perform a variation partitioning analysis and show that the phylogenetic signal in bone vascular density is not a by-product of phylogentic signal in bone size. Finally, we analyze the evolution of cortical thickness in diapsids by using an optimization by squared change parsimony and discuss the functional significance of this character in terms of decreased buoyancy in crocodiles and mass saving in birds. These results are placed in the framework of the constructional morphology model, according to which the variation of a character in a clade has a historical (phylogenetic) component, a functional (adaptive) component, and a structural (architectural) component.

Relationship between bone growth rate and the thickness of calcified cartilage in the long bones of the Galloanserae (Aves).

The histological features of mineralized tissues can be preserved for hundreds of millions of years, and are therefore important potential sources of information for reconstructing the life history traits of extinct species. Bone growth rates and the duration of the growth period have recently been estimated in fossil archosaurs from periosteal ossification (a mechanism responsible for bone diametral growth). Similarly, data on endochondral ossification (the mechanism responsible for bone longitudinal growth) may also yield information on growth duration and rate among extinct vertebrates, as long as potentially informative structures are preserved. However, in order to carry out palaeobiological estimations of growth rate and/or the duration of growth, it is first necessary to quantify in extant species the relationship between these life history traits and the histological features of endochondral ossification that are potentially preserved in the fossil record. Here we analyse the ontogenetic variation of both bone longitudinal growth rate and the thickness of the calcified cartilage in the femora of two Galloanserae (Aves) and find a significant positive relationship between these variables in both species. We discuss possible factors underlying interspecific differences in this relationship, and conclude that it could be applied with caution to draw palaeobiological inferences.

Assessing a relationship between bone microstructure and growth rate: a fluorescent labelling study in the king penguin chick (Aptenodytes patagonicus).

Microstructure-function relationships remain poorly understood in primary bone tissues. The relationship between bone growth rate and bone tissue type, although documented in some species by previous works, remains somewhat unclear and controversial. We assessed this relationship in a species with extreme adaptations, the king penguin (Aptenodytes patagonicus). These birds have a peculiar growth, interrupted 3 months after hatching by the austral winter. Before this interruption, chicks undergo extremely rapid statural and ponderal growth. We recorded experimentally (by means of fluorescent labelling) the growth rate of bone tissue in four long bones (humerus, radius, femur and tibiotarsus) of four king penguin chicks during their fastest phase of growth (3-5 weeks after hatching) and identified the associated bone tissue types ('laminar', 'longitudinal', 'reticular' or 'radial' fibro-lamellar bone tissue). We found the highest bone tissue growth rate known to date, up to 171 microm day(-1) (mean 55 microm day(-1)). There was a highly significant relationship between bone tissue type and growth rate (P<10(-6)). Highest rates were obtained with the radial microarchitecture of fibro-lamellar bone, where cavities in the woven network are aligned radially. This result supports the heuristic value of a relationship between growth rate and bone primary microstructure. However, we also found that growth rates of bone tissue types vary according to the long bone considered (P<10(-5)) (e.g. growth rates were 38% lower in the radius than in the other long bones), a result that puts some restriction on the applicability of absolute growth rate values (e.g. to fossil species). The biomechanical disadvantages of accelerated bone growth are discussed in relation to the locomotor behaviour of the chicks during their first month of life.

Controlled nucleation and growth of thin hydroxyapatite layers on titanium implants by using induction heating technique.

This paper reports the results obtained by the development of a new wet method of hydroxyapatite (HA) thin layer deposition. The method is based on the localized precipitation of HA on metallic substrates activated by induction heating. The technique developed has been shown to allow for the complete coating of substrates with micrometric thin films of HA within a low processing time. The method has been successfully applied to coat Ti plaques and Ti-6A1-4V cylinders.

Heterochronic detection through a function for the ontogenetic variation of bone shape.

Heterochrony, evolutionary modifications in the rates and/or the timing of development, is widely recognized as an important agent of evolutionary change. In this paper, we are concerned with the detection of this evolutionary mechanism through the analysis of long bone growth. For this, we provide a function sigma (t) for the ontogenetic variation of bone shape by taking the ratio of two Gompertz curves explaining, respectively, the relative contribution to long bone growth of (a) endochondral ossification and (b) periosteal ossification. The significance of the fitting of this function to empirical data was tested in Anas platyrhynchos (Anseriformes). In this function sigma (t), the time t(m) at which periosteal growth rate first equalizes endochondral growth rate was taken as the timing parameter to be compared between taxa. On the other hand, the maximum rate of ontogenetic change in bone shape (maximum slope, beta) from hatching to t(m) was taken as the rate parameter to be compared. Comparisons of these parameters between the plesiomorphic condition and the derived character state would provide evidence for hypomorphosis (earlier occurrence of t(m)), hyper-morphosis (delayed occurrence of t(m)), deceleration (smaller beta) or acceleration (higher beta). Regarding the phylogenetic context, the ancestral condition for the character of interest should be estimated to polarize the direction of the heterochronic change. We have quantified the influence of the phylogenetic history on the variation of adult bone shape in a sample of 13 species of Anseriformes and 17 species from other neornithine orders of birds by using permutational phylogenetic regressions. Phylogenetic effects are significant, and this fact allows the optimization of bone shape onto a phylogenetic tree of Anseriformes to estimate the ancestral condition for Anas platyrhynchos.

Heterochronic patterns in primate evolution: evidence from endochondral ossification.

Heterochrony (evolutionary modifications in developmental timing and/or rates) is widely recognized as an important agent of morphological change. The adaptive significance of heterochronic changes might lie either in the advantages of the derived morphologies (organ size and shape) or the derived growth parameters themselves (rate and duration of growth). We have tested these hypotheses by comparing the growth rate, the duration of growth and the relative length of the adult tibia in Primates in a phylogenetic context. We report an evolutionary decrease in growth rates (paedochronocline) and an increase in the duration of growth (perachronocline), lying in the cline from the last common ancestor of Primates, passing through the last common ancestor of Haplorhini, that of Catarrhini, to the last common ancestor of the Hominidae. However, the variation in the relative length of the adult tibia does not show any phylogenetic pattern. The derived growth parameters in themselves (slower rate, longer duration) would be of adaptive significance and they would have been selected because a prolonged learning period prior to maturity conferred advantage. The proximate (developmental) causation of differences in bone growth rate were also investigated and it was found that cell production rate in the growth plates rather than the chondrocyte size, underlies the variation in bone growth rate.

Avian long bones, flight and bipedalism.

Morphological, geometrical, chemical and mechanical characteristics of avian long bones are reviewed. Important differences exist between long bones of birds and mammals. Differences are also present in appendicular bones of birds, either between wing bones and leg bones or proximal (stylopodial) long bones and distal (zeugopodial) long bones. Special emphasis is put on pneumatization, in terms of both phylogenetic origin and geometrical and mechanical characteristics linked to it. Cortical thickness, bending strength and flexural Young's modulus were significantly lower in pneumatized bones than in marrow-filled bones. Possible adaptive reasons for the differences shown are discussed.

Periosteal bone growth rates in extant ratites (ostriche and emu). Implications for assessing growth in dinosaurs.

The first quantitative experimental data on growth dynamics of the primary cortical bone of young ratites demonstrate the following. 1) From hatching to 2 months of age, cortical thickness remains constant, thereby expressing equilibrium between periosteal bone deposition and an endosteal bone resorption. 2) Radial growth rates of the diaphyseal bone cortex are high (10-40 microns.day-1 on average--maximum 80 microns.day-1) in the hindlimb (femur, tibiotarsus and tarsometatarsus). Wing bones are smaller and later developed. They have lower rates of radial osteogenesis (2-14 microns.day-1). 3) High growth rates are linked to densely vascularized primary bone belonging to the reticular or laminar tissue types. Growth rates fall when bone vascular density decreases. These results emphasize the importance of examining a large number of skeletal elements in order to build a precise knowledge of the general relationship between bone growth rate and bone tissue type. They also stress the potential of bone growth rate quantification among extinct tetrapods, including non-avian dinosaurs.

Process heterochronies in endochondral ossification.

Heterochrony, evolutionary changes in developmental rates and timing, is a key concept in the construction of a synthesis of development and evolution. Heterochronic changes in vertebrate evolution have traditionally been identified through plesiomorphic-apomorphic comparisons of bone growth. This methodological framework assumes that observed heterochronies are the outcome of dissociations of developmental processes in time. Recent findings of non-heterochronic developmental changes underlying morphological heterochrony invalidate this assumption. In this paper, a function for bone growth (at the organ level) has been mathematically deduced from the underlying developmental mechanisms. The temporal domain of the model spans from the time at maximum growth rate, after the formation of growth plates, to the time at atrophy of the proliferating stratum of cells. Three organizational levels were considered: (a) cell kinetics of endochondral ossification, (b) variation of bone growth rates and (c) variation of accumulated bone growth with increasing age. This quantitative model provides an excellent tool to deal with the problem of the developmental basis of morphological change. I have modelled potential evolutionary changes on the system at different levels of biological organization. This new framework involves an epistemological shift in heterochronic analysis from a pattern-oriented inductive way to a process-oriented deductive way. The analysis of the relationships between the evolutionary alterations of endochondral ossification and the morphological expression of these changes reveals that observed pattern heterochronies can be the outcome of different process heterochronies. Moreover, I discuss at length the heteroposic hypothesis, that evolutionary changes in the tight regulation of the amount of protein synthesized by a cell population during development would underlie acceleration or deceleration in cases of evolutionary changes in the initial number of proliferating cells at growth plates. Future research on the genetic basis of process heterochronies and heteroposies will complete our understanding of these evolutionary phenomena.

Mechanical properties and chemical composition of avian long bones.

We have studied the mechanical behaviour of avian long bones as whole structures, by calculating mechanical parameters such as maximum load, stiffness, bending strength and flexural Young's modulus; bones were always tested in three-point bending. Furthermore composition in several chemical elements and amino acids related to collagen content was also analysed. Correlations were established between body mass, mechanical parameters and chemical contents. Both bending strength and Young's modulus were negatively correlated to body mass. Significant correlations were found between nitrogen content and both strength and Young's modulus, with negative slopes in both cases. Magnesium and phosphorus appear to be the most important inorganic elements to the understanding of the mechanical behaviour of avian long bones.

Biomechanical significance of cross-sectional geometry of avian long bones.

Cortical area, maximum second moment of area and polar moment were calculated for the long bones of 39 species of birds. Regressions of all these parameters to body mass were established. At the same time, the orientations of the maximum second moment of area were statistically tested. The parameters calculated on humerus and ulna scaled according to the predictions derived from the geometric similarity hypothesis, while those calculated for the long bones of the leg showed higher exponents, very close to the predictions of the elastic similarity hypothesis. Confidence intervals calculated for radius parameters appeared to agree with both predictions. Only the for tarsometarsus was it impossible to establish a global orientation pattern for the maximum second moment of area. In the other cases, the orientation was: sagittal in the radius, posteromedial-anterolateral in the proximal long bones (humerus and femur) and posterolateral-anteromedial in the distal long bones (ulna and tibiotarsus). The implications of the present findings are discussed in terms of the possible correlations between the orientation patterns produced in the cross-sectional geometry of avian long bones and the load carried.