Translator Disclaimer
1 June 2014 Bone Microstructure and Relative Age of the Holotype Specimen of the Diplodocoid Sauropod DinosaurSuuwassea emilieae
Author Affiliations +

We present the first study of bone microstructure in Suuwassea emilieae, a diplodocoid sauropod from the Morrison Formation. Although the holotype of Suuwassea was recently identified as a subadult, bone histology demonstrates that this individual had reached sexual maturity at approximately 75–80% of maximum adult size. The smaller size of the holotype of Suuwassea relative to contemporary sauropods is due to ontogeny rather than a true reflection of adult size. A fully adult individual would have likely been similar in size to a fully adult specimen of Apatosaurus. Suuwassea has a number of plesiomorphic characters that might have been explained by its supposed early ontogenetic status, and would then have called the validity of the taxon into question. However, our demonstration that it was an adult confirms that these features represent retention of plesiomorphic character states or evolutionary reversals in a derived animal. Additionally, the specimen shows extensive cortical drift and secondary osteon formation related to skeletal loading, which is often obscured by complete remodeling of Haversian systems in sauropod taxa. There are substantial differences in the microstructure across the bone, which could make histologic samples not based upon complete cross sections problematic. Suuwassea is one of four currently recognized dicraeosaurid taxa, and this study contributes potential taxonomic characters in sauropod bone microstructure.


Suuwassea emilieae Harris and Dodson, 2004 is a diplodocoid sauropod from the Upper Jurassic Morrison Formation of Montana. The holotype (ANS 21122), a partial skeleton that includes numerous cranial, axial, and appendicular elements, is currently the only known specimen (Harris and Dodson 2004). In phylogenetic analyses, Suuwassea originally created a trichotomous clade Flagellicaudata, as the sister taxon to diplodocids and dicraeosaurids (Harris and Dodson 2004). However, a newly described dentary added three dicraeosaurid characters to Suuwassea, so strengthening its placement as a basal dicraeosaurid (Salgado et al. 2006; Whitlock and Harris 2010; Whitlock 2011). This made Suuwassea the first dicraeosaurid found on the Laurasian continent, extending the geographic range for dicraeosaurids substantially (Whitlock and Harris 2010). Even though there is only one specimen, Suuwassea has been extensively studied (Harris and Dodson 2004; Harris 2006ac, 2007; Whitlock and Harris 2010).

The holotype specimen of Suuwassea was originally characterized by its small size and was estimated to be approximately two-thirds the size of the fully adult contemporary Morrison sauropods, Apatosaurus and Diplodocus (Harris 2006b, c). The complete humerus of Suuwassea (ANS 21122) measures 752 mm in length and the complete tibia (based on the fibula) is 839 mm. Apatosaurus (CMNH 3018) has a humerus measuring 1150 mm and a tibia of 1115 mm (Gilmore 1936). Diplodocus (CMNH 94) has a tibia 1006 mm long (Hatcher 1901). Therefore, based on the tibia, ANS 21122 is actually 83% the size of Diplodocus and 75% the size of Apatosaurus rather than a mere 66%. However, it should be noted that differing allometry of the tibia between these taxa could cause discrepancies in determining absolute size using simple ratios. Further, Suuwassea retains a number of plesiomorphic characters (amphiplatyan distal caudals, post-parietal foramen, elongate pedal phalanges with a small, uncompressed ungual). These and other characters distinguish it from contemporary sauropod taxa (Harris 2006ac; 2007). Plesiomorphies are often found in juvenile specimens, which make it advisable to name new taxa based only on adult individuals (Rozhdestvensky 1965; Gould 1966; Sereno 2010).

Woodruff and Fowler (2012) suggested that Suuwassea was a subadult specimen of another Morrison sauropod because its phylogenetic position was difficult to discern owing to plesiomorphic characters and that it appeared to be small in body size. The subadult status of ANS 21122 was inferred on the basis of neurocentral fusion and some fusion in the skull and braincase (Harris 2006c). All of the cervical neural arches are fused with the synostoses completely obliterated, the dorsal neural arches are fused with the synostoses visible, and the caudal neural arches are unfused (Harris 2006b).

Although synostosis (fusion) is often used to infer ontogenetic status (Brochu 1996), the most precise method for determining relative age is bone histology. Recent years have seen an explosion of studies of bone histology in Sauropodomorpha (see SOM: table S1, Supplementary Online Material at; Chinsamy 1995; Curry 1999; Sander 1999, 2000; Sander and Tückmantel 2003; Klein and Sander 2008; Woodward and Lehman 2009; Stein et al. 2010; Sander et al. 2011). Not only does this large body of work reinforce the validity of characters distinguishing histologic ontogenetic stages (Klein and Sander 2008) in sauropods, but it also provides a basis for meaningful comparisons among the bone microstructures of groups within Sauropodomorpha. To better understand the ontogenetic stage and phylogenetic position of Suuwassea, we sectioned the tibia to examine the internal microstructure of the bone.

Institutional abbreviations.—AMNH, American Museum of Natural History, New York, USA; ANS, Academy of Natural Sciences of Drexel University, Philadelphia, Pennsylvania, USA; BYU, Brigham Young University, Provo, Utah, USA; CMNH, Carnegie Museum of Natural History, Pittsburgh, Pennsylvania, USA; DMNH, Denver Museum of Natural History, Denver, Colorado, USA; GCP, Grupo Cultural Paleontológico de Elche, Elche, Spain; HMN, Humboldt Museum für Naturkunde, Berlin, Germany; ISIR, Palaeontological Collection, Geology Museum, Indian Statistical Institute, Calcutta, India; IVPP, Institute of Vertebrate Paleontology and Paleoanthropology, Beijing, China; MACN,N, Argentine Museum of Natural Sciences “Bernardino Rivadavia”, Buenos Aires, Argentina; MLP, Museo de la Plata, La Plata, Argentina; MNN, Musée National du Niger, Niamey, Republic of Niger; MUCPv, Geology and Paleontology Museum of the National University of Comahue, Neuquén, Argentina; NMNH, National Museum of Natural History, Washington, DC, USA; SMNS, Staatliches Museum für Naturkunde, Struttgart, Germany; T, Chongqing Natural History Museum, Chongqing, China; UNPSJB,PV, Universidad Nacional de la Patagonia “San Juan Bosco”, Paleovertebrados, Comodoro Rivadavia, Argentina; YPM, Yale Peabody Museum, New Haven, Connecticut, USA; ZDM, Zigong Dinosaur Museum, Zigong, China; ZPAL, Institute of Paleobiology, Polish Academy of Sciences, Warsaw, Poland.

Other abbreviations.—BOS, biological ontogenetic stage; HOS, histologic ontogenetic stages; LAG, line of arrested growth.

Material and methods

We took our histologic section from the mid-diaphysis of the right tibia. As there is presently only one specimen of Suuwassea, destructive sampling had to be kept to a minimum. The tibia was chosen because the bone was originally broken at midshaft, allowing for minimal destruction and information loss. It is 535 mm in preserved length and the section was taken 30 mm from the distal preserved end (Fig. 1). ANS 21122 also preserves a complete fibula and humerus, but the data from the tibia were sufficient to make sectioning these bones unnecessary. In other studies of Sauropodomorpha (Sander 2000; Klein and Sander 2008; Sander et al. 2011), humeri and femora are preferentially used over tibiae. However, other authors argue that the tibia is the ideal bone to section (Horner and Padian 2004).

The terminology for ontogenetic stages (juvenile, subadult, adult) has not been standardized. Often sexual maturity is used as the transition between subadult and adult. This is often defined in fossil taxa by the inflection point in a taxon growth curve (Erickson et al. 2001; Erickson 2005). However, Lee and Werning (2008) suggest that the inflection point may not demonstrate the onset on sexual maturity in dinosaurs based on data from extant animals. Other authors define adulthood by the attainment of maximum body size (Scannella and Horner 2010). The distinction between juveniles and subadults is even less clear. As ANS 21122 is a single specimen and its ontogenetic stage cannot be related to a growth curve, we use the biologic ontogenetic stage correlated with its HOS as defined by Klein and Sander (2008), which defines growth stage via the supposed inflection point along a growth curve. This technique was developed in order to determine the biologic ontogenetic stage of a sauropod based on bone histology. The term senescent adult is used here for animals that had reached maximum body size.

The large size of the cross section (total circumference, 370 mm) meant the entire bone could not fit on a single thin section slide. The transverse cut section was subdivided into five portions, which were mounted on five 50 mm × 75 mm glass slides. Overall data loss during histologic preparation was minimal. There was some loss of trabecular bone from the center of the cross-section following uneven grinding of one of the slides during preparation. However, the trabecular bone does not preserve ontogenetically diagnostic features (Francillon-Vieillot et al. 1990), so this data loss is negligible. Methods for thin sectioning follow Chinsamy and Raath (1992), and the terminology follows Francillon-Vieillot et al. (1990).

Fig. 1.

The right tibia of the holotype (ANS 21122) of the diplodocoid sauropod Suuwassea emilieae Harris and Dodson, 2004, Morrison Formation, Late Jurassic. For ease of sectioning, the tibia was dismantled at a natural break and then sectioned 3 cm from the preserved distal end (red line) to ensure a complete cross section. The proximal end of the distal segment was then re-attached to the proximal segment.



The bone microstructure is very well preserved and clearly shows histologic patterns and structures (Fig. 2A). The hollow cavities (trabecular bone and interior of osteons) are filled with calcite. The bone material itself is preserved as fluorapatite. There is cortical drift leading to a disproportionate amount of compact bone on the caudolateral side where the thickness is 1.5–2 times greater than on the medial, cranial, or caudal sides (30–40 mm on the lateral side compared with 15–20 mm on the other aspects of the bone). The compacta are thinnest caudally.

The bone is fibrolamellar with a high density of well-developed primary osteons throughout the entire compact bone wall, indicating a high degree of vascularization (Fig. 3A). The primary osteons have a parallel arrangement throughout the cavity. This arrangement is evident even in the inner cortex where the primary osteons are partially overprinted by secondary osteons. There are five total growth cycles preserved with alternating highly vascularized zones and poorly vascularized annuli (Fig. 2B). The cycles are most completely visible in the caudolateral region of the bone (Fig. 3A). Other regions only preserve three clear cycles of alternating vascularization. Fibrolamellar and lamellar zonal bone are gradational and are not dichotomous (Francillon-Viellot et al. 1990), so these cycles indicate differences in growth rate.

Secondary osteons have varying degrees of density and distribution in different regions of the bone (Fig. 2B). The medial, caudolateral, and cranial regions have the highest density of secondary osteons, whereas other regions have sparse secondary osteons confined to the deeper cortex close to the trabecular bone. The lowest density is in the caudal region where secondary osteons do not extend more than 1.5 mm from the edge of the trabecular bone. The medial region has the highest density of secondary osteons, which extend 10 mm from the edge of the trabecular bone. This region also has overprinting of the first generation of secondary osteons by a second generation (Fig. 3B). Additionally, there are clusters of multiple generations of secondary osteons in the outer cortex surrounded by primary osteons (Fig. 3C).

A single line of arrested growth (LAG) is preserved at the outer edge of the fourth annulus along the entire circumference of the bone, although it is discontinuous in some areas (Figs. 2B, 3D). It is most evident on the medial and lateral sides. The cortical drift is also evident by the position of this LAG approximately 1.5 mm from the periosteal surface of the bone on all sides except for the caudolateral side where it is 4.5 mm from the surface (Fig. 2B). Additionally, the lateral region of the bone also preserves two closely spaced LAGs in the outermost cortex (Fig. 3E). These are not traceable along the entire margin of the bone. The fact that the cortex is significantly thicker with a higher density of primary osteons in the lateral region suggests faster bone appositional rates specific to this region. The LAGs in the outermost cortex indicate growth cessation in this region. These closely spaced LAGs should not, however, be considered an external fundamental system, because primary osteons are seen in the outermost cortex in all other regions of the bone, indicating the individual was still growing rapidly at the time of its death (Fig. 3F).

Fig. 2.

The right tibia of the holotype (ANS 21122) of the diplodocoid sauropod Suuwassea emilieae Harris and Dodson, 2004, Morrison Formation, Late Jurassic. The full cross section under cross-polarized light. Cortical drift and changes in compact bone thickness in different sections of the bone is evident. Arrows indicate areas with the highest densities of secondary osteons. The yellow line demonstrates locations where the LAG (line of arrested growth) following the fourth annulus can be traced along the circumference of the bone. White brackets show the five highly vascularized zones in the lateral region of the bone. Between the brackets are poorly vascularized annuli. The lettered boxes correspond to the locations of the images in Fig. 3.


In order to make meaningful comparisons between Suuwassea and other sauropods, it is first necessary to understand the relative size of ANS 21122 in comparison with other sauropods. As only one specimen of Suuwassea is known, it is not possible to estimate adult weight and construct a growth curve as has been done in other studies using techniques such as developmental mass extrapolation (Erickson and Tumanova 2000; Erickson et al. 2001; Lehman and Woodward 2008). However, it is possible to make length estimates of unknown limb elements (radius, ulna, femur) from known elements (humerus, tibia) to compare ANS 21122 to similarly sized individuals (SOM: table S2). ANS 21122 has a humerus length, LH, of 752 mm and a tibia length, LT, of 839 mm (based on the fibula). Regression over a dataset of 16 sauropods with known humerus and radius lengths, LR, produces the equation:

with an R2 value of 0.936 suggesting an excellent correlation between humerus and radius length (Fig. 4A). Similar equations can be found for the ulna, Lu, (n = 15; R2 = 0.938) using the humerus (Fig. 4B), and for the femur, Lp (n = 18; R2 = 0.939) using the tibia (Fig. 4C).


These equations allow estimation of missing elements in ANS 21122 (radius = 505 mm, ulna = 507 mm, femur = 1359 mm), and comparison with similarly sized sauropod elements of different taxa that have been examined histologically.


Many different methods have been proposed for approximating individual age in fossil taxa. Often this determination is based on the number of growth lines present and a retrocalculated number of resorbed juvenile growth rings based on width between successive annuli (Amprino 1947; Sander and Tückmantel 2003). However, sauropods pose the problem of both fast growth with few growth stops before adulthood, and extensive secondary remodeling throughout the cortex obscuring potential growth lines after adulthood (Stein et al. 2010). Because of these complications, growth lines were not found in sauropods until 1981 (Reid 1981; Ricqlès 1981). Therefore, sauropods require careful consideration to interpret specimen age, as even presumably old individuals often do not preserve growth lines (Ricqlès 1980). Klein and Sander (2008) proposed such a system, which served to standardize the determination of relative age in sauropods based on the ontogenetic succession of tissue types as revealed by bone histology.

Fig. 3.

Histologic structures visible in the tibia of the holotype (ANS 21122) of the diplodocoid sauropod Suuwassea emilieae Harris and Dodson, 2004, Morrison Formation, Late Jurassic, photographed under plane-polarized light. A. Successive growth cycles in the caudolateral region of the bone. Brackets indicate successive highly and poorly vascularized zones. Highly vascularized zone with dense primary osteons (right), followed by a poorly vascularized annulus (middle). The leftmost region shows the subsequent zone characterized by higher vascularization (outermost cortex to left). B. The high density of secondary osteons (outlined in green) in the medial inner cortex, showing overprinting by a second generation (green arrow). Additionally, primary osteons are visible between secondary osteons showing that the bone is not completely remodeled (blue arrow). C. A cluster of secondary osteons in the outer cortex of the craniomedial region. This cluster is surrounded by primary osteons. D. Outer cortex of the caudolateral region, showing the LAG (line of arrested growth) (arrow) associated with the fourth annulus. E. Two LAGs in the outermost cortex of the lateral region. F. Primary osteons in the outermost cortex of the craniolateral region leading up to the periosteal surface of the bone.


Fig. 4.

Allometric graphs of sauropodomorph appendicular elements. Gray lines delineate 95% confidence interval. A. Plot of sauropod humerus length versus radius length. R2 = 0.936. B. Plot of sauropod humerus length versus ulna length. R2 = 0.938. C. Plot of sauropod femur length versus tibia length. R2 = 0.939.


The HOS technique includes 13 separate stages, later expanded to 14 stages to accommodate Magyarosaurus (Stein et al. 2010), which document the transition from embryo to senescent adult (Klein and Sander 2008). These stages assess age based upon a combination of histologic structures: development of primary osteons, development and degree of vascularity, relative amount of different types of fibrolamellar bone, development and density of secondary osteons, and occurrence of LAGs (Klein et al. 2009). It is crucial to assess ontogenetic stage based upon all of these factors rather than a subset of them, as each structure can show some individual variation. Sander et al. (2011) outline the characters distinguishing each HOS and the biological ontogenetic stage (BOS) correlated with the HOS. BOS is a hypothetical relative age correlate to different histologic structures whereby sexual maturity is recognized by a decrease in growth rate on a growth curve rather than attainment of full adult size (Klein and Sander 2008).

ANS 21122 is transitional between type D and type E bone (as defined by Klein and Sander 2008) with well-formed primary osteons, high vascularization, and somewhat dense secondary osteons in certain areas of the bone, as well as the presence of LAGs. These structures give ANS 21122 a HOS of 8–9, which are correlated to a BOS ranging from sexually mature to Adult stage I (of three possible adult stages). The LAGs suggest an older HOS (9–10), but the lack of secondary osteons in many parts of the bone and the high vascularity suggest a somewhat younger animal. Therefore, although ANS 21122 is not a senescent adult, it is certainly older than subadult and has reached sexual maturity.

Recently, Woodruff and Fowler (2012) suggested that Suuwassea was an immature version of a different Morrison sauropod taxon based on its modest amount of neural spine bifurcation, which they interpreted as an ontogenetically variable character. However, on the basis of the present analysis, ANS 21122 is a young adult (based on HOS). After sexual maturity, characters are not simply early ontogenetic stages of characters seen in senescent adults of other taxa, but are taxonomically viable (Gould 1966). This implies that the modest neural spine bifurcation in ANS 21122 at a relatively late ontogenetic stage is a taxonomic character separating it from other diplodocoids (Harris 2006b), but a detailed analysis comparing the HOS of diplodocoids with degree of neural spine bifurcation has yet to be performed.

Woodruff and Fowler (2012) base their assessment of Suuwassea on a sample set of 18 sauropod individuals, with only four preserving a relatively complete vertebral series. Neural spine bifurcation varies through the vertebral column interand intraspecifically, which may account for some of the variation interpreted by Woodruff and Fowler (2012) as ontogenetic (Wedel and Taylor 2013). This would only be evident from a larger sample set of complete individuals. Additionally, other characters in Suuwassea, such as the postparietal foramen (Harris 2006a) are not seen in juvenile specimens of other Morrison taxa (Whitlock et al. 2010) and must be accounted for in order to justify synonymization. The postparietal foramen is seen in large, presumably adult individuals of dicraeosaurid taxa such as Dicraeosaurus and Amargasaurus (Salgado and Calvo 1992), but not in any other known Morrison sauropod taxa. Though a potentially intriguing idea (Woodruff and Fowler 2012), degree of neural spine bifurcation cannot be used as a reliable method for inferring ontogeny until a complementary histologic analysis is performed confirming ontogenetic stages in examined specimens using a larger sample set of individuals with complete vertebral columns.

Some sauropodomorphs exhibit developmental plasticity such that body size and animal age are poorly correlated. This is especially apparent in the basal sauropodomorph Plateosaurus (Sander and Klein 2005; Klein and Sander 2007). Some derived taxa such as the macronarian Camarasaurus and titanosaur Phuwiangosaurus also exhibit a modest amount of developmental plasticity, though much less than Plateosaurus (Klein and Sander 2008). This could also be the case in the basal sauropod Shunosaurus, which does not have any secondary osteons even at a large size (Ye et al. 2007). Non-avian theropods and birds also commonly show variable degrees of developmental plasticity (Starck and Chinsamy 2002). Therefore, it could be that Suuwassea was also developmentally plastic. However, other flagellicaudatans (Apatosaurus, Diplodocus, Barosaurus, Dicraeosaurus) and Brachiosaurus show strong correlation between histologic stage and body size (Klein and Sander 2008), as do other basal sauropodomorphs such as Massospondylus (Chinsamy 1995). There is variation in the sizes of different species of Apatosaurus (Upchurch et al. 2004), but this is likely interspecific variation rather than developmental plasticity. Since related taxa are generally not developmentally plastic, it is reasonable to assume Suuwassea also was not.

The ontogenetic status of the holotype of Suuwassea compares well with similarly sized diplodocoid individuals that had not reached senescence at their time of death. Apatosaurus specimens (CMNH 21715, BYU 681–11940, BYU 6812–4749) with femur lengths of 1218 mm (estimated), 1330 mm, and 1354 mm (estimated) respectively are HOS 8–10 (Klein and Sander 2008). Similarly sized Diplodocus specimens are also within this HOS range (Klein and Sander 2008). Phuwiangosaurus has much older histologic patterns for smaller individuals (∼1000 mm femur = HOS 12) and likely had a maximum body size smaller than these diplodocoids (Klein et al. 2009). In contrast, Alamosaurus has young histologic patterns in large individuals suggesting much larger size than Suuwassea and other diplodocoids (Woodward and Lehman 2009). This is supported by findings of Fowler and Sullivan (2011) who describe a gigantic specimen of Alamosaurus based on a partial femur and two vertebrae. A histologic study of Apatosaurus by Curry (1999) suggested that specimens of equivalent size to Suuwassea were late juveniles rather than subadults or adults. However, in that study, sexual maturity was inferred at the onset of full body size rather than at a slowing of growth rate (Curry 1999). The presence in the Apatosaurus samples of secondary osteons and remodeling make them minimally HOS 7. Given the larger number of sampled sauropods (including more specimens of Apatosaurus) and amount of work done to determine sauropod BOS since Curry's (1999) pioneering study, it is likely these animals were older than originally recognized (implying somewhat slower growth rates than originally inferred).

Considering the close similarity in HOS between ANS 21122 and similarly sized Apatosaurus and Diplodocus specimens, we inferred that a fully adult Suuwassea would likely be approximately the size of a fully adult Apatosaurus or Diplodocus. Though Suuwassea was originally considered a small Morrison sauropod when compared to the largest contemporary Morrison sauropod taxa (Harris and Dodson 2004), the smaller size of the holotype is ontogenetic and does not indicate senescent adult size.

Recent phylogenetic studies have clarified the dicraeo-saurid affinities of Suuwassea (Whitlock 2011). Dicraeosaurus was the only dicraeosaurid prior to this study to be sectioned histologically, based on a sample of six specimens (three femora and three humeri; Sander 2000). In that study, femur length (or equivalent femur length based on humerus length) was fairly small, ranging from 865 mm to 1140 mm. All of these animals were considered subadult to early adult based on histology (Sander 2000). Dicraeosaurus has a pattern in orientation of vascularity alternating between radial canals and longitudinal canals in the outermost cortex as well as large erosional cavities towards the inner cortex. These characters are not observed in ANS 21122, so are probably not dicraeosaurid apomorphies. However, sectioning the two other known dicraeosaurids, Brachytrachelopan and Amargasaurus would be the only method of confirming this, assuming the dicraeosaurid affinities of Suuwassea.

In ontogenetically older sauropods, secondary reconstruction affects the entire bone, obscuring primary histologic structures (Stein et al. 2010). ANS 21122 was still relatively early in its adult development so it provides information on the way in which Haversian systems invade the outer cortex of the bone. It is not only ontogenetic changes that cause secondary osteon formation and overprinting by successive generations, but also skeletal loading (Klein and Sander 2007). Differential loading can also cause cortical bone drift (Ricqlès et al. 2003), evident in ANS 21122. Horner and Padian (2004) suggest the tibia is the ideal bone to section owing to its large size and rapid growth, which delay secondary osteon overprinting. The full cross section in ANS 21122 contains large regions of non-remodeled tissue supporting this assertion. However, cortical drift was extensive and caused a higher degree of secondary remodeling in many areas, obscuring regions of the inner cortex.

ANS 21122 shows overprinting of secondary osteons by a second generation in the innermost cortex (Fig. 3B). This extent of secondary remodeling has previously only been reported in the oldest sauropod individuals (Stein et al. 2010). It is possible this secondary reconstruction is related to a late ontogenetic stage, but in the absence of other factors indicating a higher HOS, it is most parsimonious to consider the reconstruction to be related to skeletal loading in ANS 21122. Overprinting of secondary osteons is still poorly understood and the implications behind their overprinting needs to be further examined.

It is evident that different regions of the tibia had different growth rates. The lateral and medial regions had higher cortical thicknesses than the caudal or cranial regions, indicating relatively more deposition and a faster bone apposition rate medially and laterally. These areas also had a larger number and higher density of secondary osteons than other regions. Further, the lateral region had an additional two LAGs (Fig. 3E), which were not present elsewhere in the bone and reflect different growth rates in the different regions. It is possible that the lateral region, which preserves a larger number of annuli and a high number and density of primary osteons, originally grew faster than other regions of the bone, as suggested by the larger cortical thickness, but then stopped growing earlier than the other regions as indicated by the two outermost LAGs.

This study highlights issues with the coring technique, in which only a cylinder of bone is extracted from the cortex, rather than the entire cortex being sectioned (Sander 1999, 2000; Stein and Sander 2009). The degree of remodeling and vascularization can be very different depending on the section that is cored, as made clear by ANS 21122. Such differences are only visible in complete cross sections (Chinsamy-Turan 2005). The coring technique has been applied widely to humeri and femora to preserve specimen integrity (Klein and Sander 2008). In these bones, differences in regions of the cross section are not as pronounced as in the tibia of ANS 21122. This could be related to the presence of the fibula, which might offset skeletal loading in the tibia, causing variability across the cross section. However, currently there is too small a sample set of sauropod tibia cross sections to confidently make this assertion.

Tornieria was inferred to have had a sexually dimorphic bone microstructure: type A with little secondary osteon remodeling and type B with dense secondary osteon overprinting and LAGs (Sander 2000). In Sander (2000), this material was referred to Barosaurus and was subsequently assigned to Tornieria (Remes 2006). The craniolateral region of ANS 21122 has little remodeling as in Tornieria type A, whereas the caudolateral region has extensive secondary osteon remodeling similar to Tornieria type B. Based on results from this study, it is possible that the bone types merely reflect variation in remodeling across a cross section. In order to verify the validity of the sexual dimorphism hypothesis (Sander 2000), full cross sections of several individuals would be necessary to determine if the degree of remodeling is uniform. Despite the value of limiting the amount of destructive sampling, the coring technique is problematic when comparing bones unless the core is taken in the exact same location on the bone. Therefore, when applying this technique, close adherence to the instructions in Stein and Sander (2009) is paramount. Future studies should focus on understanding how sauropod bones other than the humerus and femur remodel in different regions of a single cross section through ontogeny in order to evaluate the potential limitations of this technique and to better understand sauropod histologic patterns as they relate to ontogeny, phylogeny, and skeletal loading.


A fully-grown adult Suuwassea was larger than previously suggested and was likely similar in size to Apatosaurus and Diplodocus, but did not reach sizes achieved by the largest Morrison sauropods such as Supersaurus. The only known specimen of Suuwassea had reached sexual maturity (HOS 8–9) by the time of death and was likely 75–80% of its full adult size. This study provides the first histologic analysis of Suuwassea and confirms its validity as a separate Morrison taxon, as its plesiomorphic characters are not related to immaturity of the specimen. We also present allometric equations for determining the length of missing elements in sauropod bones based upon a dataset of 15–18 genera. Such equations will allow future histologic comparisons between similarly sized taxa in order to determine relative age and size of sauropod genera in specimens that do not have the same elements preserved. This study adds a new genus to the ever-growing number of sauropod dinosaurs that have been studied histologically and adds the second dicraeosaurid, further expanding the sauropod histologic database.


This paper benefited greatly from reviews by Michael P. Taylor (University of Bristol, UK) and Jerald D. Harris (Dixie State College, St. George, USA), as well as comments by Michael J. Benton (University of Bristol, UK), the academic editor. We are thankful for helpful discussions from Martin P. Sander and Koen Stein (both University of Bonn, Germany), Andrew McDonald and Eric Morschhauser (both University of Pennsylvania, Philadelphia, USA), and D. Cary Woodruff (Montana State University, Bozeman, USA). We are thankful for access to the specimen and permission to perform histologic analysis from Edward B. Daeschler (Academy of Natural Sciences of Drexel University, Philadelphia, USA) and to Jason Poole (Academy of Natural Sciences of Drexel University) for preparing the specimen for us. Finally, we wish to thank Dennis Terry (Temple University, Philadelphia, USA) for access to the microscope used for this study.



R. Amprino 1947. La structure du tissue osseux envisagée comme expression de differences dans la vitesse de l'accroissement. Archives de Biologie 58: 35–330. Google Scholar


C. Brochu 1996. Closure of neurocentral sutures during crocodilian ontogeny: implications for maturity assessment in fossil archosaurs. Journal of Vertebrate Paleontology 16: 49–62. Google Scholar


A. Chinsamy 1995. Bone histology and growth trajectory of the prosauropod dinosaur Massospondylus carinatus Owen. In . W.A.S. Sarjeant (ed.), Vertebrate Fossils and the Evolution of Scientific Concepts, 329–339. Overseas Publishers Association, Amsterdam. Google Scholar


A. Chinsamy and M. Raath 1992. Preparation of fossil bone for histological examination. Palaeontologia Africana 29: 39–44. Google Scholar


A. Chinsamy-Turan 2005. The Microstructure of Dinosaur Bone: Deciphering Biology with Fine-Scale Techniques. 215 pp. Johns Hopkins University Press, Baltimore. Google Scholar


K. Curry 1999. Ontogenetic histology of Apatosauriis (Dinosauria: Sauropoda): new insights on growth rates and longevity. Journal of Vertebrate Paleontology 19: 654–665. Google Scholar


G. Erickson and T. Tumanova 2000. Growth curve of Psittacosaurus mongoliensis Osborn (Ceratopsia: Psittacosauridae) inferred from long bone histology. Zoological Journal of the Linnean Society 130: 551–566. Google Scholar


G. Erickson , K. Curry Rogers , and S. Yerby 2001. Dinosaurian growth patterns and rapid avian growth rates. Nature 412: 429–433. Google Scholar


G. Erickson 2005. Assessing dinosaur growth patterns: a microscopic revolution. Trends in Ecology and Evolution 20: 677–684. Google Scholar


H. Francillon-Vieillot , V. de Buffrenil , J. Castanet , F. Geraudie , J. Meunier , Y. Sire , L. Zylenberberg , and A. de Ricqlès 1990. Microstructure and mineralization of vertebrate skeletal tissues. In J.E. Carter (ed.), Skeletal Biomineralization: Patterns, Processes, and Evolutionary Trends , 471–530. Van Nostrand Reinhold, New York. Google Scholar


D. Fowler and R. Sullivan 2011. The first giant titanosaurian sauropod from the Upper Cretaceous of North America. Acta Palaeontologica Polonica 56: 685–690. Google Scholar


C. Gilmore 1936. Osteology of Apatosaurus, with special reference to specimens in the Carnegie Museum. Memoirs of the Carnegie Museum 9: 175–308. Google Scholar


S.J. Gould 1966. Allometry and size in ontogeny and phylogeny. Biological Reviews 41: 587–640. Google Scholar


J. Harris 2006a. Cranial osteology of Suwassea emilieae (Sauropoda: Diplodocoidea: Flagellicaudata) from the Upper Jurassic Morrison Formation of Montana, USA. Journal of Vertebrate Paleontology 26: 88–102. Google Scholar


J. Harris 2006b. The axial skeleton of the dinosaur Suuwassea emilieae (Sauropoda: Flagellicaudata) from the Upper Jurassic Morrison Formation of Montana, USA. Palaeontology 49: 1091–1121. Google Scholar


J. Harris 2006c. The significance of Suuwassea emilieae (Dinosauria: Sauropoda) for flagellicaudatan intrarelationships and evolution. Journal of Systematic Palaeontology 4: 185–198. Google Scholar


J. Harris 2007. The appendicular skeleton of Suuwassea emilieae (Sauropoda: Flagellicaudata) from the Upper Jurassic Morrison Formation of Montana (USA). Geobios 40: 501–522. Google Scholar


J. Harris and P. Dodson 2004. Anew diplodocoid sauropod dinosaur from the Upper Jurassic Morrison Formation of Montana, USA. Acta Palaeontologica Polonica 49: 197–210. Google Scholar


J.B. Hatcher 1901. Diplodocus (Marsh): its osteology, taxonomy, and probable habits, with a restoration of the skeleton. Memoirs of the Carnegie Museum 1: 1–63. Google Scholar


J. Horner and K. Padian 2004. Age and growth dynamics of Tyrannosaurus rex. Proceedings of the Royal Society, Series B 271: 1875–1880. Google Scholar


N. Klein and M. Sander 2007. Bone histology and growth of the prosauropod dinosaur Plateosaurus engelhardti Von Meyer, 1837 from the Norian bonebeds of Trossingen (Germany) and Frick (Switzerland). Special Papers in Palaeontology 77: 169–206. Google Scholar


N. Klein and M. Sander 2008. Ontogenetic stages in the long bone histology of sauropod dinosaurs. Paleobiology 34: 247–263. Google Scholar


N. Klein , M. Sander , and V. Suteethorn 2009. Bone histology and its implications for the life history and growth of the Early Cretaceous titanosaur Phuwiangosaurus sirindhornae. In : E. Buffetaut , G. Cuny , J. LeLoeuff , and V. Suteethorn (eds.), Late Palaeozoic and Mesozoic Ecosystems in SE Asia. The Geological Society, London, Special Publications 315: 217–228. Google Scholar


A. Lee and S. Werning 2008. Sexual maturity in growing dinosaurs does not fit reptilian growth models. Proceedings of the National Academy of Sciences, USA 105: 582–587. Google Scholar


T. Lehman and H. Woodward 2008. Modeling growth rates for sauropod dinosaurs. Paleobiology 34: 264–281. Google Scholar


R.E.H. Reid 1981. Lamellar-zonal bone with zones and annuli in the pelvis of a sauropod dinosaur. Nature 292: 49–51. Google Scholar


K. Remes 2006. Revision of the Tendaguru sauropod dinosaur Tornieria africana (Fraas) and its relevance for sauropod paleobiogeography. Journal of Vertebrate Paleontology 26: 651–669. Google Scholar


A. de Ricqlès 1980. Tissue structures of dinosaur bone: functional significance and possible relation to dinosaur physiology. In : D.K. Thomas and E.C. Olsen (eds.), A Cold Look at the Warm Blooded Dinosaurs, 103–139. Westview Press, Boulder, Colorado. Google Scholar


A. de Ricqlès 1981. Cyclical growth in the long limb bones of a sauropod dinosaur. Acta Palaeontologica Polonica 15: 225–232. Google Scholar


A. de Ricqlès , K. Padian , J. Horner , E. Lamm , and N. Myhrvold 2003. Osteohistology of Confuciusornis sanctus (Theropoda: Aves). Journal of Vertebrate Paleontology 28: 373–386. Google Scholar


A. Rozhdestvensky [Roždestvenski, A.] 1965. Growth changes in Asian dinosaurs and some problems of their taxonomy [in Russian]. Paleontologičeskij žurnal 3: 95–109. Google Scholar


L. Salgado and J. Calvo 1992. Cranial osteology of Amargasaurus cazaui Salgado and Bonaparte (Sauropoda, Dicraeosauridae) from the Neocomian of Patagonia. Ameghiniana 29: 337–346. Google Scholar


L. Salgado , I. Carvalho , and A. Garrido 2006. Zapalasaurus bonapartei, a new sauropod dinosaur from La Amarga Formation (Lower Cretaceous), northwestern Patagonia, Neuquén Province, Argentina. Geobios 39: 695–707. Google Scholar


M. Sander 1999. Life history of Tendaguru sauropods as inferred from long bone histology. Fossil Record 2: 103–112. Google Scholar


M. Sander 2000. Longbone histology of the Tendaguru sauropods: implications for growth and biology. Paleobiology 26: 466–488. Google Scholar


M. Sander and N. Klein 2005. Developmental plasticity in the life history of a prosauropod dinosaur. Science 310: 1800–1802. Google Scholar


P. Sander and C. Tückmantel 2003. Bone lamina thickness, bone apposition rates, and age estimates in sauropod humeri and femora. Paläontologische Zeitschrift 77: 161–172. Google Scholar


M. Sander , N Klein , K. Stein , and O. Wings 2011. Sauropod bone histology and its implications for sauropod biology. In : N. Klein , K. Remes , C. Gee , and M. Sander (eds.), Biology of the Sauropod Dinosaurs: Understanding the Life of Giants, 276–302. Indiana University Press, Bloomington. Google Scholar


J. Scannella and J. Horner 2010. Torosaurus Marsh, 1891, is Triceratops Marsh, 1889 (Ceratopsidae: Chasmosaurinae): synonymy through ontogeny. Journal of Vertebrate Paleontology 30: 1157–1168. Google Scholar


P. Sereno 2010. Taxonomy, cranial morphology, and relationships of parrot-beaked dinosaurs (Ceratopsia: Psittacosaurus). In : M. Ryan , B. Chinnery-Allgeier , and D. Eberth (eds.), New Perspectives on Horned Dinosaurs, 21–58. Indiana University Press, Bloomington. Google Scholar


J. Starck and A. Chinsamy 2002. Bone microstructure and developmental plasticity in birds and other dinosaurs. Journal of Morphology 254: 232–246. Google Scholar


K. Stein and M. Sander 2009. Histological core drilling: a less destructive method for studying bone histology. In : M.A. Brown , J.F. Kane , and W.G. Parker (eds.), Methods in Fossil Preparations: Proceedings of the First Annual Fossil Preparation and Collections Symposium, 69–80. Google Scholar


K. Stein , Z. Csiki , K. Curry Rogers , D. Weishampel , R. Redelstorff , J. Carballido , and P.M. Sander 2010. Small body size and extreme cortical bone remodeling indicate phyletic dwarfism in Magyarosaurus dacus (Sauropoda: Titanosauria). Proceedings of the National Academy of Sciences, USA 107: 9258–9263. Google Scholar


P. Upchurch , Y. Tomida , and P. Barrett 2004. A new specimen of Apatosaurus ajax (Sauropoda: Diplodocidae) from the Morrison Formation (Upper Jurassic) of Wyoming, USA. National Science Museum Monographs 26: 1–99. Google Scholar


M.J. Wedel and M.P. Taylor 2013. Neural spine bifurcation in sauropod dinosaurs of the Morrison Formation: ontogenetic and phylogenetic implications. PalArch's Journal of Vertebrate Palaeontology 10: 1–34. Google Scholar


J. Whitlock 2011. A phylogenetic analysis of Diplodocoidea (Saurischia: Sauropoda). Zoological Journal of the Linnean Society 161: 872–915. Google Scholar


J. Whitlock and J. Harris 2010. The dentary of Suuwassea emilieae (Sauropoda: Diplodocoidea). Journal of Vertebrate Paleontology 30: 1637–1641. Google Scholar


J. Whitlock , J. Wilson , and M. Lamanna 2010. Description of a nearly complete juvenile skull of Diplodocus (Sauropoda: Diplodocoidea) from the Late Jurassic of North America. Journal of Vertebrate Paleontology 30: 442–457. Google Scholar


D.C. Woodruff and D. Fowler 2012. Ontogenetic influence on neural spine bifurcation in Diplodocoidea (Dinosauria: Sauropoda): A critical phylogenetic character. Journal of Morphology 273: 754–764. Google Scholar


H. Woodward and T. Lehman 2009. Bone histology and microanatomy of Alamosaurus sanjuanensis (Sauropoda: Titanosauria) from the Maastrichtian of Big Bend National Park, Texas. Journal of Vertebrate Paleontology 29: 807–821. Google Scholar


Y. Ye , G. Peng , and S. Jiang 2007. Preliminary histological study on the long bones of Middle Jurassic Shunosaurus and Omeisaurus from Dashanpu, Zigong, Sichuan. Acta Palaeontologica Sinica 46: 135–144. Google Scholar
© 2014 B.P. Hedrick et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Brandon P. Hedrick, Allison R. Tumarkin-Deratzian, and Peter Dodson "Bone Microstructure and Relative Age of the Holotype Specimen of the Diplodocoid Sauropod DinosaurSuuwassea emilieae," Acta Palaeontologica Polonica 59(2), 295-304, (1 June 2014).
Received: 19 April 2012; Accepted: 9 October 2012; Published: 1 June 2014

Back to Top