Mass extinctions are frequently followed by short-term reductions in body sizes of survivor lineages, a pattern known as the ‘Lilliput effect’ (Urbanek, 1993; Harries, Kauffman & Hansen, 1996). However, in the absence of adequate phylogenetic and life history data, the mechanisms of size reductions can be unclear and likely differ across environments, taxonomic groups, and extinction events (Twitchett, 2007; Harries & Knorr, 2009). Lilliput patterns have been documented widely in marine invertebrate groups following the end-Permian extinction (Payne, 2005; Twitchett, 2007; Luo et al., 2008; Mutter & Neuman, 2009; Metcalfe, Twitchett & Price-Lloyd, 2011; Song, Tong & Chen, 2011; Rego et al., 2012), and anecdotally in tetrapods of the Triassic Lystrosaurus Assemblage Zone in the Karoo Basin of South Africa (ca. 252.3 Ma), but growth dynamics underlying these patterns are not fully understood. Therocephalians represent an exemplary clade of nonmammalian therapsids that thrived from the Middle Permian to Middle Triassic, and survived the end-Permian extinction as important components of Triassic survivor and recovery faunas in the Karoo Basin (Botha & Smith, 2006). In addition to the dicynodont Lystrosaurus, at least three genera of therocephalians in two major groups have observed stratigraphic occurrences that span the extinction boundary in the Karoo: the baurioid Tetracynodon, and the akidnognathids Promoschorhynchus and Moschorhinus (Smith & Botha, 2005; Botha & Smith, 2006; Huttenlocker, Sidor & Smith, 2011). Other Triassic taxa (e.g., Olivierosuchus, Regisaurus) have long ghost lineages extending into the Permian, indicating that they too survived the extinction but lack a Permian record within the depositional basin (Huttenlocker, 2009; Huttenlocker, Sidor & Smith, 2011). Although therocephalians are generally exceeded in abundance by dicynodont therapsids in the Karoo Basin, their diversity, extensive stratigraphic range, and success during the end-Permian extinction make them an ideal group to study evolutionary patterns during the Permian-Triassic transition.
Previous morphological studies of therocephalians have emphasized their functional anatomy, including jaw mechanics and locomotory specializations (e.g., Kemp, 1972a; Kemp, 1972b; Kemp, 1978; Kemp, 1986; Fourie & Rubidge, 2007; Fourie & Rubidge, 2009). Recent collaborative work on therocephalians has emphasized integration of their fine structure and internal anatomy to resolve paleobiological questions, including tooth replacement patterns, braincase structure, and growth and histomorphologic structure (Abdala, Rubidge & van den Heever, 2008; Sigurdsen et al., 2012; Huttenlocker & Botha-Brink, 2013). Detailed investigations of histmorphology are particularly useful, permitting assessments of growth patterns and variation within or among closely related therapsid species (e.g., Botha & Angielczyk, 2007; Huttenlocker & Botha-Brink, 2013). Moreover, as growth patterns are associated with organismal fitness, recent investigations into bone microstructure have inquired into whether certain growth strategies conferred success on some groups during the end-Permian mass extinction (e.g., rapid growth in the dicynodont Lystrosaurus and its relatives; Botha-Brink & Angielczyk, 2010).
Bone microstructure in therapsids
Bone histology has offered insights into the lifestyles and growth patterns of many of the major subclades of nonmammalian therapsids. Recent examples include investigations of feeding and locomotion, habitat use, and especially growth dynamics (e.g., Ray, Chinsamy & Bandyopadhyay, 2005; Jasinoski, Rayfield & Chinsamy, 2010; Chinsamy-Turan, 2012). Earlier surveys of bone histology emphasized differences between basal (pelycosaurian-grade) synapsid and therapsid tissue composition, matrix organization, and degree of vasculature of the limb bones (Enlow & Brown, 1957; Enlow, 1969; Ricqlès, 1969; Ricqlès, 1974a; Ricqlès, 1974b; Ricqlès, 1976). Particularly, fibrolamellar tissue complexes (vascularized bone tissues that incorporate primary osteons within a woven-fibered matrix) were found to be near ubiquitous among limb elements of sampled therapsids, suggesting that this tissue complex appeared early during therapsid evolution prior to the origination of mammals bearing this tissue-type (Ricqlès, 1969; Ricqlès, 1974a; Ricqlès, 1974b; Ray, Botha & Chinsamy, 2004; Chinsamy & Hurum, 2006; Ray, Bandyopadhyay & Bhawal, 2009). Indeed, fibrolamellar bone has been reported in basal therapsids (e.g., Biarmosuchus: Ricqlès, 1974b), as well as in some immature pelycosaurian-grade synapsids (e.g., Sphenacodon and Dimetrodon juveniles) and in fast-growing portions of the skeleton (e.g., the elongated neural spines of Dimetrodon and crossbars on the neural spines of Edaphosaurus) (Huttenlocker, Rega & Sumida, 2010; Huttenlocker, Mazierski & Reisz, 2011; Huttenlocker & Rega, 2012; Shelton et al., 2013). However, there is great histovariability in the organization of fibrolamellar bone even within major subclades of therapsids. Fibrolamellar bone may be formed by varying degrees of woven- and parallel-fibered interstitial matrix and incorporates a variety of vascular motifs, and may be zonal (punctuated by cyclic growth marks) or azonal. Ray, Botha & Chinsamy (2004) reported the presence of zonal fibrolamellar bone in many Permian and Middle Triassic taxa, but suggested that sustained (non-cyclic) growth patterns might have arisen occasionally in a number of phylogenetically disparate taxa that do not encompass the immediate ancestors of mammals (gorgonopsian Aelurognathus; eucynodont Cynognathus; and some bidentalian dicynodonts). The abundance of dicynodont fossils in Permian and Triassic rocks and recent advances in their systematic relationships have permitted more detailed comparisons of growth patterns in this diverse subclade (Chinsamy & Rubidge, 1993; Botha, 2003; Ray & Chinsamy, 2004; Ray, Chinsamy & Bandyopadhyay, 2005; Botha & Angielczyk, 2007; Ray, Bandyopadhyay & Bhawal, 2009; Botha-Brink & Angielczyk, 2010; Green, Schweitzer & Lamm, 2010; Nasterlack, Canoville & Chinsamy-Turan, 2012; Ray, Botha-Brink & Chinsamy-Turan, 2012). Phylogenetic comparative surveys have revealed patterns of increasing tissue vascularity during the evolutionary history of bidentalian dicynodonts (especially in Triassic forms like Lystrosaurus), and determinate growth patterns with peripheral rest lines and systematic cortical remodeling in large kannemeyeriiforms (Botha-Brink & Angielczyk, 2010; Green, Schweitzer & Lamm, 2010; Ray, Botha-Brink & Chinsamy-Turan, 2012).
The diversity of growth patterns in other nonmammalian therapsid groups, as well as their phylogenetic and temporal distributions, is incompletely known. A body of literature on nonmammalian cynodont histology has accrued in recent years (e.g., Ricqlès, 1969; Botha & Chinsamy, 2000; Botha & Chinsamy, 2004; Botha & Chinsamy, 2005; Ray, Botha & Chinsamy, 2004; Chinsamy & Abdala, 2008; Botha-Brink, Abdala & Chinsamy, 2012), but sampling has been more limited in other theriodonts, such as the gorgonopsians and therocephalians (Ray, Botha & Chinsamy, 2004; Chinsamy-Turan & Ray, 2012; Huttenlocker & Botha-Brink, 2013). Ricqlès (1969) suggested differential rates of growth between a basal therocephalian from the Middle Permian of South Africa and the Late Permian whaitsiid ‘Notosollasia’ (= Theriognathus). Given the comparatively more vascularized cortical bone in the radius of the whaitsiid (1969: plate IV), Ricqlès suggested that therocephalians might have exhibited accelerated growth rates later in their evolutionary history, paralleling the aforementioned temporal pattern of increasing growth rates in some dicynodonts. More recently, Ray, Botha & Chinsamy (2004) and Chinsamy-Turan & Ray (2012) analyzed additional material from an indeterminate scylacosaurid (erroneously identified as ‘Pristerognathus’), in addition to other therapsid material, and argued for similar ‘flexible’ growth patterns in gorgonopsians, basal therocephalians, and most early cynodonts. The authors suggested that more rigorous taxonomic sampling would better substantiate parallel trends toward a loss in developmental plasticity and acceleration of growth rates as in dicynodonts. Inadequate sampling of eutherocephalians before and after the end-Permian mass extinction limits our understanding of evolutionary patterns in therapsid histomorphology and skeletal growth during this important geologic transition.
Although eutherocephalians have not been sampled histologically for such comparisons, recent revisions to Permo-Triassic boundary-crossing taxa have necessitated cursory descriptions of eutherocephalian histology for its ontogenetic and paleobiological implications (e.g., Tetracynodon: Sigurdsen et al., 2012; Moschorhinus: Huttenlocker & Botha-Brink, 2013). During the course of this work, we developed a database of histological data and images with the goal of addressing features of life history evolution in Permian and Triassic eutheriodonts (therocephalians and cynodonts), particularly in the context of the end-Permian extinction. Here, we present a reappraisal of limb bone microstructure in Permian and Triassic therocephalians based on new histologic sampling, and offer a hypothesis of the evolution of their growth patterns. We suggest that therocephalians provide a robust study system for investigating the evolution of growth strategies during the Permian-Triassic transition, and a useful point of comparison and contrast to other groups that lived during this time (e.g., dicynodonts, cynodonts).
Materials and Methods
Specimen selection and histological processing
Specimens were selected based on completeness and availability for histological processing, but a broad sample of the major representatives of South African therocephalians was desired in order to recognize long-term patterns (if present) or clade specific histomorphology. Specimens that were semi-articulated and included diagnostic cranial material were preferred for accuracy of taxonomic identifications. Some specimens were not diagnosable to genus, but were resolved to their respective higher taxon as in the case of five indeterminate scylacosaurids described here. Scylacosaurids are generally difficult to identify unless a complete and accurate antecanine tooth count can be made, and some authors have suggested that the diversity of scylacosaurids is over-split because variations in tooth count may be ontogenetically variable (e.g., Abdala, Rubidge & van den Heever, 2008). The sample therefore included 80 limb elements from 33 individuals in 11 genera: Lycosuchus, Glanosuchus, Moschorhinus, Olivierosuchus, Hofmeyria, Mirotenthes, Theriognathus, Ictidosuchoides, Tetracynodon, Scaloposaurus, and Microgomphodon (Fig. 1), plus additional scylacosaurid material not diagnosed to genus. Thin-sections were prepared using standard histological techniques modified from Chinsamy & Raath (1992) and Wilson (1994). Limb bone midshafts were sampled cross-sectionally and imaged using Nikon Eclipse 50i and LV100 POL petrographic microscopes with a digital image capture system. Histomorphometric variables (discussed below) were measured using NIS-Elements and NIH ImageJ v. 1.42q software (Rasband, 1997–2012). Moschorhinus histomorphology was excluded from present description as it has been discussed elsewhere (Huttenlocker & Botha-Brink, 2013), but data from Moschorhinus were included in the quantitative analyses (Table 1).
Bone tissue typology: definitions and selection of growth proxies
Bone tissue texture exhibits marked variation in therocephalians and other therapsids, varying from highly organized and lamellar to disorganized and woven. Only a few recent studies have integrated qualitative and quantitative assessments of tissue texture and vascular proxies of growth in Permo-Triassic therapsids (Botha & Chinsamy, 2000; Botha & Chinsamy, 2004; Botha & Chinsamy, 2005; Ray & Chinsamy, 2004; Ray, Botha & Chinsamy, 2004; Ray, Chinsamy & Bandyopadhyay, 2005; Ray, Bandyopadhyay & Appana, 2010; Botha-Brink & Angielczyk, 2010; Huttenlocker & Botha-Brink, 2013). Generally, cellular bone forms as osteoblasts become incorporated into the extracelluar (or interstitial) matrix (ECM) forming quiescent osteocytes. The overall bone apposition rate affects the texture of the mineralized ECM, with collagen fibers and crystallites bearing a more lamellar organization under slower growth and a nonlamellar (woven-fibered) texture under faster growth. Parallel-fibered bone, an intermediate tissue-type, can be identified by its ‘streaky’ appearance under polarized light, with the predominant fiber orientation being parallel to the surface of the bone and forming a woven-basket texture in most cases. In cases in which birefringent properties have been disrupted by diagenetic processes, it is possible to approximate the relative organization of mineralized fibers with reference to the organization of the lacunocanalicular network within the ECM (Stein & Prondvai, 2013). In contrast to parallel-fibered bone, woven-fibered bone includes large, globular osteocyte lacunae that are usually densely packed within the mineralized ECM. Nonlamellar tissues (parallel- and woven-fibered) may also frequently incorporate large vascular canals that later become infilled with one or two concentric lamellae forming primary osteons (diagnosed by their ‘Maltese cross’ pattern of birefringence under polarized light). These osteons house passageways for blood vessels and nerves while also contributing to the structural integrity of the bone by providing added bone mass and helping to blunt microcracks (Currey, 2002). The result is a fibrolamellar bone complex (herein ‘FLB’), in which a disorganized, fibrous or nonlamellar interstitial matrix incorporates an anastomosing network of centripetally lamellated primary osteons. Currey (1987) and Currey (2002) defined FLB broadly as a tissue complex formed by parallel- (or woven-) fibered bone with primary osteons (2002: p. 18). By contrast, Ricqlès (1974a) originally restricted the term ‘fibrolamellar’ to tissues formed largely by woven-fibered bone with primary osteons, excluding parallel-fibered bone from this category. Herein, we follow the traditional usage of Ricqlès, but temper this strict definition by noting that parallel- and woven-fibered bone form a continuum that is often ill-defined (and may be present simultaneously in many therapsid bony tissues, even within the same section). Bone cortices formed primarily by lamellar tissue, which forms at relatively slower apposition rates (∼1 µm/day or less) (de Margerie, Cubo & Castanet, 2002; Lee et al., 2013), do not typically incorporate primary osteons, instead bearing simple vascular canals or being avascular. In lamellar bone, the lacunocanalicular network is ordered, the osteocyte lacunae being small and more lenticular in appearance with the long axis oriented parallel to the surface of the bone. Both tissue complexes can be zonal (periodically interrupted by growth marks) or azonal. Growth marks in zonal bone may be present in the form of lines of arrested growth or ‘LAGs’ (denoted by an opaque cement line, traceable around the entire cortex, and indicative of a temporary cessation of growth) or annuli (thin bands of dense, annular tissue, usually parallel-fibered or lamellar, deposited during periods of slowed growth).
For quantitative histomorphometric analysis, two vascular proxies of skeletal growth were selected: cortical vascularity and mean primary osteon diameter. These proxies were selected in order to evaluate the extent to which histological correlatives of growth varied across phylogeny, and whether their evolution was tied to body size or other biological factors. Vascular proxies have offered useful indicators of skeletal growth in extant and extinct tetrapods (Castanet et al., 2000; de Margerie, Cubo & Castanet, 2002; de Margerie et al., 2004; Buffrénil, Houssaye & Böhme, 2007; Cubo et al., 2012), and their utility here allows comparisons with other histological studies of therapsids in which similar measures were used (e.g., Botha-Brink & Angielczyk, 2010; Huttenlocker & Botha-Brink, 2013). Notably, ontogenetic variation in growth may introduce a lesser degree of cortical vascularity in adult bones that exhibited decreasing apposition rates prior to death and burial, and may therefore introduce variation in a single cross-section where this transition is recorded. Nonmammalian therapsids, however, are well suited to relative growth rate estimation based on tissue texture and vascularity, due to their generally thick bone walls (preserving the early record of primary growth) and limited secondary remodeling (Botha-Brink & Angielczyk, 2010). Measurement of cortical vascularity (%CV, the relative area of the cortex that is occupied by porous, vascular spaces) follows Lee et al. (2013). Measurements were restricted to the inner two-thirds to three-quarters of the cortex where the bone formed at high, sustained growth rates (Cubo et al., 2012), and were averaged from ten quadrants sampled circularly around each midshaft cross-section. The subsampled quadrants excluded areas of secondary reconstruction and outer regions of simple canals. We also estimated mean primary osteon diameter (POD) by measuring in microns the transverse (or minimum) widths of 15 primary osteons visible in the subsampled regions and averaging them across all regions within a given midshaft cross-section.
To examine potential effects of size and robusticity on measured histomorphometric variables, we also estimated two proxies of overall bone robusticity: (1) K (the proportional diameter of the medullary region relative to the total diameter of the cross-section; Currey & Alexander, 1985) and (2) relative bone wall thickness or ‘RBT’ (the percentage of the average cross-sectional thickness of the bone wall relative to the total diameter of the cross-section; Chinsamy, 1993). These variables play a frequent role in histological studies of fossil tetrapod bone, as bone robusticity may correspond to habitat preferences or mechanical loading (Wall, 1983; Currey & Alexander, 1985; Currey, 2002; Laurin, Girondot & Loth, 2004; Germain & Laurin, 2005; Kriloff et al., 2008). However, their relationships to size, growth, and vascularity have been underexplored in a comparative framework. These measurements, as well as cross-sectional area at midshaft, were attained using NIH ImageJ, and were tested for correlations with vascular growth proxies using Pearson’s product-moment correlation tests. Histomorphometric data are recorded in Table 1.
Pearson’s product-moment correlation tests
We performed a series of correlation tests in order to evaluate the extent to which variations in vascular growth proxies were dependent upon size and robusticity, which bear a strong influence on many aspects of organismal biology (Peters, 1983; Calder, 1984; Stearns, 1992). For instance, small-bodied therocephalians might have achieved their increasingly diminutive sizes by having a slower growing, less vascularized skeleton compared to their larger-bodied predecessors. In this scenario, one would expect a correlation between smaller size and slower growth, and between larger size and faster growth across subclades. A similar correlation in which small-bodied species generally exhibit slower growth rates than larger-bodied groups has been identified in extant vertebrates (Case, 1978), and suggested by histologic data in fossil non-avian dinosaurs (Erickson et al., 2004; Lee, 2007). On the other hand, smaller sizes may have been achieved by shortening the duration of the growth period, in which case no generalized correlations between size and vascular proxies of skeletal growth are necessary. To address these hypotheses, histomorphometric data (%CV, POD, RBT) and midshaft cross-sectional area were recorded for each sectioned limb bone. The data were organized into propodial, epipodial, and pooled subsets to control for the effects of increased variance from pooling limb bones of different types (although the effects appeared to be minimal as all tests ultimately yielded similar results). For each data partition, Pearson’s product-moment correlation tests were performed between histomorphometric variables (%CV, POD, RBT) and the natural log of midshaft cross-sectional area. Vascular growth proxies were also tested for correlations with bone robusticity independent of size, and with each other to assess whether %CV and POD provided comparable estimates of vascularization.
Independent contrast methods were carried out to control for the effects of phylogenetic non-independence of putative correlations (Felsenstein, 1985; Garland, Bennett & Rezende, 2005). For example, one might find low tissue vascularity in Triassic baurioids due to their generally small sizes, or due to their close relatedness (and, by extension, their inherited phenotypic similarities). We carried out additional correlation tests on an augmented data set using the PDAP:PDTREE module (Midford, Garland & Maddison, 2011) in Mesquite version 2.0 (Maddison & Maddison, 2007). This required a tree and branch lengths (adapted from Huttenlocker, 2013; Huttenlocker, 2014) pruned to the 11 histologically sampled taxa. First, tip data for each of the 11 taxa were recorded in a NEXUS file, including average %CV, POD, RBT and the natural log of midshaft area of the propodials and epipodials separately (limb bones were not pooled for independent contrasts). Second, ancestral character states (estimated using squared-change parsimony) were checked for the assumption of Brownian motion evolution that governs independent contrasts (Felsenstein, 1985; Díaz-Uriarte & Garland, 1996). This was performed by running assumption-testing operations in PDAP that evaluate the relationship between the absolute values of independent contrasts and their corresponding standard deviations. Non-significant relationships were determined for each of the data partitions, indicating that a Brownian motion model adequately fit the tip data. Finally, the same sets of regressions were performed on independent contrasts as in the untransformed data (size, robusticity, and vascular growth proxies).
Results 1: qualitative histomorphology
Due to space limitations, the present description is accompanied by a more detailed account in the Supplemental Data file. In general, limb bone cortices in studied therocephalians were thick and formed primarily by FLB with varying degrees of vascularization, depending on size and phylogenetic position. For example, large basal therocephalians from the Middle Permian exhibited subplexiform FLB in the propodial elements with a comparatively high degree of vascularization (%CV ∼13–16%; POD ∼75–168 µm). By contrast, some smaller-bodied taxa in both the Permian and Triassic tended to incorporate more parallel-fibered bone or showed evidence of increased parallel-fibered and lamellar bone deposition with less vasculature toward the outer cortex, indicative of growth attenuation and attainment of somatic maturity (de Margerie, Cubo & Castanet, 2002). This pattern is marked in Mirotenthes, which preserves an external fundamental system (‘EFS’) in some elements (an outer collar of avascular, generally acellular, lamellar bone indicative of virtual cessation of circumferential growth in adult individuals; Cormack (1987); Huttenlocker, Woodward & Hall (2013)). Systematic cortical remodeling by Haversian bone formation was rare and only a few sparse secondary osteons were identified in some Permian scylacosaurian taxa [e.g., an indeterminate scylacosaurid and Moschorhinus, contrary to reports of extensive skeletal remodeling by Chinsamy-Turan & Ray (2012): p. 203)]. As in dicynodonts and other therapsids in which histology is well known, most basal therocephalians and eutherocephalians exhibited remarkably thick bone walls (∼20–35% RBT in forelimb elements of lycosuchids, scylacosaurids, and akidnognathids; ∼40% in forelimbs of hofmeyriids). This condition, however, was lost in baurioids, which were instead characterized by a much thinner cortical bone wall (<25% in the forelimb and propodials) and more slender limb bones.
Permian basal therocephalians and eutherocephalians (Figs. 2A–2C, 2F, 2G; 3A, 3B) generally showed multiple growth zones as well, demarcated by cyclic growth marks indicative of periodic pauses in growth as in other Permian therapsids (Ray, Botha & Chinsamy, 2004; Ray, Botha-Brink & Chinsamy-Turan, 2012; Botha-Brink & Angielczyk, 2010; Botha-Brink, Abdala & Chinsamy, 2012). Although Triassic therocephalians (Figs. 2D, 2E; 3C–3F) showed a variety of vascular motifs and tissue-types (e.g., richly vascularized and disorganized bone tissues in akidnognathids; less vascularized parallel-fibered bone tissue in baurioids), fewer growth marks were recorded in all Triassic species. Small Triassic baurioids in particular showed thinner bone walls with few growth marks, less vascularized limb bone cortices, and smaller, more sparsely distributed primary osteons on average.
Result 2: quantitative histometrics
Pearson’s correlation and phylogeny-independent contrasts
Results of raw and phylogeny-corrected correlation tests are presented in Table 2. Correlation tests on raw data found that vascular growth proxies were strongly positively correlated with size [i.e., the natural log of midshaft cross-sectional area, underscoring greater overall tissue vascularity in large bones from larger taxa (e.g., Lycosuchus, scylacosaurids, Moschorhinus)] (Fig. 4; Table 2). Both %CV and POD also exhibited a strong positive correlation with each other, indicating that %CV and POD represent equivalent proxies for understanding relationships between bone tissue vascularization and growth across the therocephalian clade. Whereas the selected vascular growth proxies shared a consistent positive relationship with size for all data partitions, putative associations between robusticity and size were less clear. Correlation tests on raw size data and RBT were non-significant. Likewise, correlation tests on raw vascular growth proxies and RBT either yielded non-significant p-values or, in the case of the propodial-only data partition, had low correlation coefficients with only a weakly positive association. This result is likely due to the fact that even some small-bodied taxa exhibited unexpectedly thick bone walls, as in the case of the hofmeyriids Hofmeyria and Mirotenthes. Bone wall thickness correlates poorly with size and growth proxies, suggesting that bone robusticity is not necessarily tied directly to growth (perhaps being constrained by ecology, habitat, or mechanical regimen in different groups of therocephalians).
|All therocephalians, raw data|
|ln midshaft area vs. RBT||0.309||0.109||−0.186||0.267||−0.126||0.301|
|ln midshaft area vs. %CV||0.744||<0.001||0.714||<0.001||0.746||<0.001|
|ln midshaft area vs. POD||0.853||<0.001||0.847||<0.001||0.850||<0.001|
|RBT vs. %CV||0.452||0.012||0.034||0.839||0.149||0.217|
|RBT vs. POD||0.360||0.050||0.111||0.512||0.143||0.237|
|%CV vs. POD||0.760||<0.001||0.802||<0.001||0.796||<0.001|
|All therocephalians, independent contrasts|
|ln midshaft area vs. RBT||−0.466||0.174||−0.476||0.232||–||–|
|ln midshaft area vs. %CV||0.765||0.006||0.807||0.015||–||–|
|ln midshaft area vs. POD||0.656||0.028||0.859||0.006||–||–|
|RBT vs. %CV||−0.077||0.831||−0.224||0.592||–||–|
|RBT vs. POD||−0.472||0.168||−0.010||0.979||–||–|
|%CV vs. POD||0.639||0.034||0.877||0.004||–||–|
Results of phylogeny-corrected correlations further indicated a strong relationship between size and some histometrics (but not with limb bone robusticity) (Table 2). Evolutionary decreases in cross-sectional area of limb bones were generally associated with decreases in average %CV and POD. Eutherocephalians and particularly baurioids demonstrated a noteworthy pattern in which reconstructed ancestor-descendant size reductions of Late Permian and Triassic lineages were associated with decreases in the average level of tissue vascularization. Patterns in limb bone robusticity were less clear. As in the analyses of the raw data, phylogeny-corrected correlations between RBT and size or growth proxies were non-significant.
General histological patterns
Size, robusticity, and vascular growth proxies
Biologically meaningful associations are detectable in therocephalian histology, as in some other therapsid groups. For example, vascular growth proxies were strongly positively correlated with size as larger-bodied species typically exhibited greater overall tissue vascularity (e.g., Lycosuchus, scylacosaurids, Moschorhinus). Previous tests incorporating a large histologic sample of dicynodonts and other therapsids found similar correlations between raw vascular growth proxies and size (estimated from skull lengths), although tests on a subset of dicynodonts were only marginally significant and non-significant when independent contrasts were evaluated (Botha-Brink & Angielczyk, 2010). The new data agree with these earlier results by large measure. However, the present analysis found a strongly positive correlation between size and both vascular growth proxies (%CV and POD) even when corrected for phylogeny. Prior analyses implementing phylogeny-independent contrasts on dicynodonts were unable to identify similar patterns, despite a significant correlation between the raw data (Botha-Brink & Angielczyk, 2010). Improved statistical results in this study are a likely consequence of sampling bones of particular types separately (rather than averaging vascularity across all bones) and using cross-sectional measurements from sampled bones as a size proxy (rather than representative skull lengths from specimens that were not sampled histologically). Tests on raw cortical thickness (RBT) in dicynodonts also showed no clear association with size or degree of vascularization as in the present study, even though a positive association with size was discovered when corrected for phylogeny. No correlation was observed between bone robusticity (RBT) and size or degree of vascularization in therocephalians (raw or phylogeny-corrected), suggesting that size and rate of growth may have had limited influence over bone robusticity as compared to other aspects of organismal biology such as mechanical regime (e.g., locomotor behavior, stance or gait; Currey & Alexander, 1985) and ecology or habitat preference (e.g., burrowing, semi-aquatic/aquatic; Wall, 1983; Laurin, Girondot & Loth, 2004; Germain & Laurin, 2005). Similarly, data on the genus Moschorhinus indicated that overall bone compactness was related to the thickness of the bone wall, but was largely independent of growth and degree of vascularity (Huttenlocker & Botha-Brink, 2013).
Previous interpretations of growth patterns in early therocephalians were based on limited information from incomplete specimens (Ricqlès, 1969; Ray, Botha & Chinsamy, 2004; Chinsamy-Turan & Ray, 2012). Additional specimens described here suggest that at least some large-bodied predators from the Middle Permian, including Lycosuchus and some scylacosaurids, exhibited subplexiform FLB in propodial elements. Some of the larger-bodied predators in the sample also showed the highest degree of cortical vascularization. This is remarkable, as subplexiform FLB is one of the most rapidly deposited tissue-types in archosaurian and mammalian limb bones, and similarly vascularized bone in birds and mammals forms periosteally at a rate generally greater than 15 µm/day (Castanet et al., 2000; de Margerie, Cubo & Castanet, 2002; Cubo et al., 2012). It is noteworthy that the subplexiform tissue complex, present in Lycosuchus and scylacosaurids, represents the prototype upon which earlier workers first described FLB [see Stein & Prondvai (2013) for a review]. This subplexiform condition is conspicuously lacking in the whaitsiid Theriognathus(Fig. 5) and some later eutherocephalians. Consequently, the evolutionary scenario suggested by Ricqlès (1969) and critically re-examined by Chinsamy-Turan & Ray (2012) should be revised: basal therocephalians exhibited highly vascularized FLB and grew relatively rapidly over many growing seasons but with frequent interuptions, in contrast to some later eutherocephalians (with the exception of the akidnognathid Moschorhinus, which maintained relatively fast growth).
Moreover, elevated vascularity and rapid growth may be a characteristic of larger bodied taxa, an interpretation that is supported by observations in other large predatory theriodonts such as the cynodont Cynognathus and some large gorgonopsians (Botha-Brink, Abdala & Chinsamy, 2012; Chinsamy-Turan & Ray, 2012). Importantly, evolutionary decreases in body size during the Permian (Huttenlocker, 2013; Huttenlocker, 2014) were associated with decreases in overall degree of skeletal vascularization. Both hofmeyriids and Theriognathus (in spite of the latter’s substantial size) showed modest cortical vascularity and smaller mean primary osteon diameters than in basal lycosuchids, scylacosaurids or akidnognathids, but the baurioids (which are deeply nested in the tree and generally smaller-bodied) had the least vascularized bone tissues (Fig. 6). These clade-level patterns suggest that reductions in body size of some Late Permian eutherocephalians were coupled with decreased rates of skeletal apposition leading up to the end-Permian extinction, particularly in the baurioid lineage.
Growth and the end-permian extinction
The end-Permian extinction was associated with evidence of temporary body size reductions, restricted primarily to faunas of the earliest Triassic (Induan) (although size reductions in some therapsids may reflect larger-scale patterns of body size evolution tracing back to the Permian; Huttenlocker, 2013; Huttenlocker, 2014). Such size shifts have been documented previously based on invertebrate burrows, foraminifera, brachiopods, gastropods, bivalves, conodonts, and fish (Twitchett & Barras, 2004; Payne, 2005; Twitchett, 2007; Luo et al., 2008; Mutter & Neuman, 2009; Metcalfe, Twitchett & Price-Lloyd, 2011; Song, Tong & Chen, 2011; Rego et al., 2012). Nevertheless, questions remain regarding the evolution of growth patterns and their underlying influence on size shifts (Twitchett, 2007; Harries & Knorr, 2009). For example, organisms may have experienced slower overall growth rates in response to more limited resources or environmental degradation during the Permian-Triassic transition. Growth mark analyses on marine brachiopod shells (i.e., ‘Lingula’) have indicated slow growth rates with frequent interruptions to growth in earliest Triassic shells (Metcalfe, Twitchett & Price-Lloyd, 2011). The authors attributed their results to suboptimal environmental conditions, including episodes of benthic hypoxia, hypercapnia, ocean acidification, and/or disruptions to primary productivity. Such environmental factors would place strong physiological limits on shell formation. However, identifications of lingulid specimens were tenuous given conservatism in external morphology of the group, and growth marks were only studied in shells from Triassic survival and recovery faunas without being compared to Permian specimens. Alternatively, surviving lineages could have exhibited heterochronic shifts shortening time to maturity (e.g., progenesis) and thus rapid, sustained growth over a brief growth period. Progenesis is a classic example of an r-selection strategy in perturbed or unstable environments (Gould, 1977) and has been identified as a potential mechanism of some Lilliput patterns (Harries, Kauffman & Hansen, 1996). Finally, if shifts in body size distributions were influenced primarily by differential extinction of large- versus small-bodied forms, then there may have been no resulting changes in growth patterns at all (that is to say, changes in growth dynamics are not necessary to explain post-extinction body size distributions).
Growth patterns in Permo-Triassic therapsids compared
New data on growth patterns in nonmammalian therapsids, as well as other Permo-Triassic tetrapods, offer the potential to further evaluate patterns of selectivity during mass extinctions (Botha-Brink & Angielczyk, 2010; Botha-Brink & Smith, 2012). Bone histology has been studied in numerous genera of Permian and Triassic dicynodont therapsids (Chinsamy & Rubidge, 1993; Ray, Botha & Chinsamy, 2004; Ray, Bandyopadhyay & Bhawal, 2009; Ray, Botha-Brink & Chinsamy-Turan, 2012) and recent progress in dicynodont paleobiology has permitted evolutionary investigations of their growth patterns (Botha-Brink & Angielczyk, 2010). Increased rates of skeletal growth originated relatively early, either within or prior to the divergence of bidentalian dicynodonts (e.g., Dicynodon, Lystrosaurus) by the early-Late Permian. Medium-to-large Late Permian dicynodonts continued to show patterns of increased cortical vascularity, especially within the Permo-Triassic boundary-crossing genus Lystrosaurus, which demonstrated some of the highest levels of tissue vascularity (∼20%). Triassic specimens of Lystrosaurus showed relatively higher vascularity and fewer growth marks. In the therocephalian Moschorhinus, the only large therapsid predator to cross the Permian-Triassic boundary, within-lineage size reduction was associated with the maintenance of rapid but attenuating growth over a short period (Huttenlocker & Botha-Brink, 2013). This pattern suggests that Moschorhinus may have been under selection for reaching its adult size relatively more quickly than in other Permian therocephalians. Notably, Moschorhinus exhibited comparably high levels of tissue vascularity as Lystrosaurus during the Triassic (∼20–25%).
Whereas anecdotal evidence in Lystrosaurus and Moschorhinus is suggestive of within-lineage heterochronic shifts, clade-level patterns introduce a more complex explanation for observed body size reductions in therocephalians. In particular, body size reductions occurred early during the evolution of eutherocephalians and were associated with a lesser degree of cortical vascularity in medium-to-small-bodied Permian and Triassic forms (e.g., hofmeyriids and especially baurioids). The two major subclades of therocephalians that persisted into the earliest Triassic, Akidnognathidae and Baurioidea, revealed distinctly different growth patterns from each other as interpreted through their tissue texture and degree of vascularity. Their histology suggests a bimodality of life history strategies in earliest Triassic therocephalians: small-to-medium akidnognathids with well-vascularized (fast-growing) bone and smaller-bodied baurioids with less vascularized (slower-growing) bone. However, both groups shared a reduced number of growth marks compared to their Permian relatives in addition to their generally smaller sizes. This nuance is not evident from the quantitative analysis based on vascular proxies of growth rate alone, but is evident from growth mark counts in surveyed specimens. Permian theriodonts that have been sampled histologically, including some gorgonopsians, the cynodont Procynosuchus, basal therocephalians, Permian (but not Triassic) specimens of Moschorhinus, hofmeyriids, and Theriognathus, typically showed evidence of prolonged, multi-year growth often to larger body sizes, a pattern that is not represented in earliest Triassic therapsids sampled to date (Botha-Brink & Angielczyk, 2010; Botha-Brink, Abdala & Chinsamy, 2012).
The present discussion of associations between micro- and macrostructure provides a more functional and wholistic context for the evolution of histological features in Permian and Triassic therocephalians. However, it is important to note that the patterns discussed here have not been evaluated quantitatively and therefore merit future investigation. Recent large-scale phylogenetic studies in other therapsids have addressed how life history and functional morphology might have contributed to the success of some groups during the Late Permian and Triassic (e.g., bidentalian dicynodonts). For example, the degree of development of the secondary palate has been linked anecdotally to new environmental conditions with the onset of the Early Triassic, particularly a dramatic decline in atmospheric pO2 from the Late Permian and continuing through the Middle and Late Triassic (Retallack, 2003). However, a rigorous collections-based study found no difference between secondary palate length in Permian and Triassic dicynodonts when corrected for size and phylogeny (Angielczyk & Walsh, 2008). Similarly, a bony secondary palate can be found in a number of therocephalian subgroups, both in the Permian and Triassic, and Triassic therocephalian faunas consisted of species both with (e.g., baurioids) and without (e.g., akidnognathids) a secondary palate (Fig. 7). No clear association with global hypoxia and respiratory efficiency can be made based on this character, and, as a result, other factors may have been more important in maintaining and shaping the evolution of the secondary palate (e.g., feeding mechanics; Thomason & Russell, 1986).
Similar studies addressing the possible effects of hypoxia on cortical tissue vascularity have found few differences between Permian and Triassic therapsids, instead demonstrating that highly vascularized tissues with enlarged canals evolved early in bidentalian dicynodonts (Botha-Brink & Angielczyk, 2010). In therocephalians, variation in the degree of vascularization of limb cortices is best explained by size variation observed across clades (Fig. 7). Most smaller-bodied groups exhibited less vascularized limb bone cortices, a character that evolved relatively early in the evolutionary history of eutherocephalians and held over in some small Triassic taxa. The smallest Triassic forms, derived bauroids, typically had lighter, more gracile skeletons with an open medullary cavity, thinner bone walls, and few to no growth marks. In addition to longer, more slender limb bones, they also had an elongate hind foot with a calcaneal tuber on the heel, maxillary bridge forming a bony secondary palate (discussed above), increasingly specialized multi-cusped teeth, and often lacked a parietal foramen (or reduced the pineal body altogether as in Tetracynodon; Sigurdsen et al., 2012). The selective value of maintaining a parietal eye for temperature regulation and modulating melatonin production may have been diminished in some small, nocturnal or crepuscular baurioid therocephalians, or in short-lived animals less dependent on seasonal cues in photoperiodicity (Roth, Roth & Hotton, 1986). The latter scenario is consistent with the lack of cyclic bone deposition and paucity of growth marks in small Triassic baurioids (although one genus, Scaloposaurus, is distinguished from other small Triassic baurioids in its retention of the parietal foramen and pineal body).
A survey of histological patterns in therocephalians found that limb bone cortices composed of thick deposits of FLB with cyclic growth marks were widespread in early therocephalians, but evolutionary decreases in adult body sizes of some clades were associated with reductions in cortical vascularity and skeletal growth leading up to the end-Permian mass extinction. In Permo-Triassic therocephalians, a pattern of multi-year growth to large body size that was common in the Permian was selected against in the earliest Triassic. This conclusion is supported by (1) ecological removal of large-bodied taxa having prolonged, multi-year growth patterns; (2) cladistically inferred survival of small-bodied taxa with modest skeletal apposition rates, but truncated growth durations (i.e., baurioids); and (3) within-lineage shifts in growth patterns observed in boundary-crossing genera in the Karoo (i.e., Lystrosaurus and Moschorhinus). A synergistic combination of local within-lineage effects and differential extinction patterns strongly influenced Triassic Lilliput faunas, weakening the hypothesized role of rapid adaptive evolution of new small-bodied forms. Similar within-lineage size decreases and size selective extinctions contributed strongly to Lilliput patterns in marine gastropods, foraminifera, and brachiopods, although all three mechanisms have been invoked to explain Early Triassic foraminifera size distributions globally (Payne, 2005; Metcalfe, Twitchett & Price-Lloyd, 2011; Song, Tong & Chen, 2011; Rego et al., 2012). Contrary to the present results, growth mark analyses on lingulid brachiopods are suggestive of different physical factors influencing skeletal growth in marine benthos (due to slowed, but prolonged shell secretion over many years) (Metcalfe, Twitchett & Price-Lloyd, 2011). More skeletochronologic and phylogenetic data are needed, however, to understand the generality of these patterns among Permo-Triassic Lilliput taxa in marine and terrestrial realms.
Although some effects on size and growth are observable in Triassic therocephalians (and perhaps therapsids more generally), it is important to note that much of the diversity observed in the earliest Triassic Lystrosaurus Assemblage Zone of the Karoo originated during the Late Permian, and that variation in body sizes and growth patterns during the Late Permian was supplanted by increased bimodality in the Early Triassic Lystrosaurus AZ: small-to-medium, fast-growing akidnognathids and the still smaller, slower-growing baurioids. Small size and short growth duration were dominant life history strategies of Early Triassic therocephalians in the Karoo, and reductions in size were typically associated with lesser tissue vascularity and growth rates across but not within taxa. Furthermore, although these strategies were apparently common in the post-extinction environment, their success was temporary. Low rates of origination in therocephalians during this time, coupled with small sizes and reduced niche occupation may have afforded the opportunity for more marginalized groups to diversify (e.g., cynodonts and archosauromorphs). Future applications of phylogenetic comparative methods to studies of body size and growth during the Permo-Triassic will enhance our understanding of interplay between macroevolution and extinctions, and will identify areas of phylogeny that correspond to shifts in trait evolution that conferred success on lineages.
Bone histology in Lycosuchus vanderrieti from the Middle Permian Tapinocephalus Assemblage Zone
(A) SAM-PK-9084, radius midshaft, cortical fibrolamellar bone viewed at high magnification (crossed-nicols with wave plate). (B) Same as (A) viewed under normal polarized light without wave plate. (C) SAM-PK-9084, ulna midshaft, cortex showing growth marks and well-vascularized fibrolamellar bone viewed at low magnification (non-polarized light). Note the thick bone wall and inner coarse cancellous structure. (D) SAM-PK-K9012, femur midshaft, dorsal cortex showing subplexiform fibrolamellar bone viewed under non-polarized light. (E) SAM-PK-K9012, femur midshaft, posterior region of cortex showing three bands of parallel-fibered bone (blue bands denoted by arrows) representing possible growth marks, viewed at low magnification (crossed-nicols with wave plate). Arrows denote growth marks. Abbreviations: po, primary osteon.
Bone histology in Scylacosauridae from the Middle Permian Tapinocephalus Assemblage Zone
(A) Glanosuchus macrops, BP/1/6228, ulna midshaft, cortical fibrolamellar bone viewed at low magnification (crossed-nicols with wave plate). (B) Scylacosauridae indet., SAM-PK-5018, fibula midshaft close-up of secondary osteon in deep cortex (crossed-nicols with wave plate). (C) Scylacosauridae indet., CGS R300, humerus midshaft cortex viewed at low magnification showing growth marks (crossed-nicols with wave plate). (D) Scylacosauridae indet., BP/1/5576, ulna midshaft cortex viewed at low magnification showing growth marks (crossed-nicols with wave plate). (E) Scylacosauridae indet., BP/1/5587, ulna midshaft cortex viewed at low magnification showing growth marks (crossed-nicols with wave plate). Arrows denote growth marks. Abbreviations: cl, cement line; Hc, Haversian canal; po, primary osteon.
Bone histology in the akidnognathid Olivierosuchus parringtoni from the Triassic Lystrosaurus Assemblage Zone
(A) NMQR 3605, cross-sectional profile of humerus midshaft viewed at low magnification (crossed-nicols with wave plate). Note the occluded medullary region and relatively thick cortical bone wall. (B) NMQR 3605, humerus midshaft, cortical fibrolamellar bone showing large primary osteons preceding a thin zone of parallel-fibered bone near a LAG (crossed-nicols with wave plate). (C) NMQR 3605, humerus midshaft, cortex showing thick zone of reticular fibrolamellar bone followed by parallel-fibered bone and a LAG (crossed-nicols with wave plate). (D) Triassic Moschorhinus (SAM-PK-K118) humerus midshaft shown at same scale as (C) for comparison (crossed-nicols with wave plate). Note the densely packed reticular and radial primary osteons and globular osteocyte lacunae. (E) SAM-PK-K10617, femur midshaft, cortical fibrolamellar bone viewed at low magnification (crossed-nicols with wave plate). (F) SAM-PK-K10617, femur midshaft, close-up of primary osteons and interstitial bone matrix (normal polarized light at maximum extinction). Arrows denote growth marks. Abbreviations: pfb, parallel-fibered bone; po, primary osteon.
Bone histology in the hofmeyriid Hofmeyria atavus
(A) BP/1/4404, cortex of humerus midshaft viewed at low magnification (crossed-nicols with wave plate). (B) BP/1/4404, cross-sectional profile of radius midshaft viewed at low magnification (crossed-nicols with wave plate). (C) Same as (B) close-up of cortex showing growth marks and lamellar bone in outer cortex (crossed-nicols with wave plate). (D) Same as (B) close-up of cortex showing longitudinal primary osteons and outer lamellar bone (crossed-nicols with wave plate). (E) BP/1/4404, ulna midshaft cross-section viewed at low magnification (crossed-nicols with wave plate). (F) BP/1/4404, ulna midshaft cortex viewed at high magnification, showing sharp transition to lamellar bone in outer cortex (crossed-nicols with wave plate). Brackets denote outer zone of lamellar bone with simple canals, indicating marked decrease in bone apposition. Abbreviations: pfb, parallel-fibered bone; po, primary osteon.
Bone histology in the hofmeyriid Mirotenthes digitipes
(A) SAM-PK-K6511, humerus midshaft cross-section viewed at low magnification (crossed-nicols with wave plate). (B) SAM-PK-K6511, radius midshaft cortex (crossed-nicols with wave plate). (C) SAM-PK-K6511, ulna midshaft cortex (crossed-nicols with wave plate). (D) SAM-PK-K6511, femur midshaft cortex showing extensive parallel-fibered and lamellar bone (normal polarized light at maximum extinction). (E) SAM-PK-K6511, tibia midshaft cross-section viewed at low magnification (non-polarized light). (F) SAM-PK-K6511, fibula midshaft cross-section viewed at low magnification (non-polarized light). Bracket indicates avascular outer zone. Abbreviations: pfb, parallel-fibered bone; po, primary osteon.
Bone histology in the whaitsiid Theriognathus microps
(A) NMQR 3375, femur midshaft cross-section viewed at low magnification (non-polarized light). (B) NMQR 3375, femur midshaft cortical bone viewed at medium magnification showing growth marks (arrows) (non-polarized light). (C) same as ‘B,’ viewed at high magnification with wave plate, showing close-up of outer zone of well-vascularized fibrolamellar bone (bracket). (D) BP/1/719, femur midshaft cortex (crossed-nicols with wave plate). Arrows denote growth marks. Abbreviations: flb, fibrolamellar bone; rc, radial canals.
Bone histology in the baurioid Ictidosuchoides longiceps
(A) SAM-PK-K8659, humerus midshaft cross-section viewed at low magnification (normal polarized light). (B) SAM-PK-K8659, radius midshaft cortex and inner cancellous bony scaffold (crossed-nicols with wave plate). (C) SAM-PK-K8659, tibia midshaft cortex and inner cancellous bony scaffold (crossed-nicols with wave plate). (D) SAM-PK-K8659, femur midshaft showing inner cancellous bone and outer bone compacta with a woven-fibered matrix (crossed-nicols with wave plate). (E) SAM-PK-K10423, femur distal shaft cortex (crossed-nicols with wave plate). (F) SAM-PK-K10423, fibula proximal shaft cortex (crossed-nicols with wave plate). (G) BP/1/75, humerus midshaft cortex (crossed-nicols with wave plate). (H) BP/1/4092, midshaft cross-section of large humerus viewed at low magnification (crossed-nicols with wave plate). (I) BP/1/4092, radius close-up showing growth mark (annulus) in outer cortex (non-polarized light). Arrows denote growth marks. Abbreviations: nc, nutrient canal; pfb, parallel-fibered bone; spc, subplexiform canals; wb, woven-fibered bone.
Bone histology in the baurioid Tetracynodon darti
(A) NMQR 3745, humerus midshaft cross-sectional profile viewed at low magnification (non-polarized light). (B) UCMP 78396, humerus midshaft cortex (normal polarized light at maximum extinction). Bracket denotes outer zone of parallel-fibered and lamellar bone. (C) UCMP 78396, humerus midshaft cortex showing outer line of arrested growth (demarcated by cement line at arrow) (non-polarized light). (D) UCMP 78395, radius midshaft cortex and perimedullary region viewed at low magnification (crossed-nicols with wave plate). (E) UCMP 78396, femur midshaft cortex and perimedullary region showing woven- and parallel-fibered bone (crossed-nicols with wave plate). (F) UCMP 78396, femur midshaft cortex close-up (normal polarized light at maximum extinction). (G) UCMP 78396, fibula midshaft cortical bone packed with longitudinal primary osteons (non-polarized light). Arrows denote growth marks. Abbreviations: elb, endosteal lamellar bone; pfb, parallel-fibered bone; po, primary osteon; Sf, Sharpey’s fibers; wb, woven-fibered bone.
Bone histology in the baurioid Scaloposaurus constrictus
(A) Humerus midshaft cross-section showing fibrolamellar bone deposition followed by a thin collar of lamellar bone in the subperiosteal region (normal polarized light at maximum extinction). (B) Humerus midshaft cortex close-up showing longitudinal primary osteons and a large nutrient canal within a woven-fibered bone matrix (crossed-nicols with wave plate). Abbreviations: lb, lamellar bone; nc, nutrient canal; po, primary osteon.
Bone histology in the baurioid Microgomphodon oligocynus
(A) NMQR 3605, humerus midshaft cross-section viewed at low magnification (crossed-nicols with wave plate). Note local histovariation in the arrangements of vascular canals. (B) NMQR 3605, femur midshaft cross-sectional profile viewed at low magnification (crossed-nicols with wave plate). (C) Close-up of ‘B’ showing abundant reticular canals in cortex and lack of growth marks. (D) NMQR 3605, tibia midshaft cross-sectional profile viewed at low magnification (crossed-nicols with wave plate). (E) NMQR 3605, fibula midshaft cortex (crossed-nicols with wave plate). Abbreviations: cc, circular canal; rc, reticular canal; po, primary osteon; Sf, Sharpey’s fibers.