Long bone histology of the most derived Sauropoda, the Titanosauria suggests that titanosaurian long bone histology differs from the uniform bone histology of basal Sauropoda. Here we describe the long bone histology of the titanosaur Ampelosaurus atacis and compare it to that of basal neosauropods and other titanosaurs to clarify if a special titanosaur bone histology exists.
Ampelosaurus retains the laminar vascular organization of basal Sauropoda, but throughout most of cortical growth, the scaffolding of the fibrolamellar bone, which usually is laid down as matrix of woven bone, is laid down as parallel-fibered or lamellar bone matrix instead. The remodeling process by secondary osteons is very extensive and overruns the periosteal bone deposition before skeletal maturity is reached. Thus, no EFS is identifiable. Compared to the atypical bone histology of Ampelosaurus, the large titanosaur Alamosaurus shows typical laminar fibrolamellar bone. The titanosaurs Phuwiangosaurus, Lirainosaurus, and Magyarosaurus, although differing in certain features, all show this same low amount or absence of woven bone from the scaffolding of the fibrolamellar bone, indicating a clear reduction in growth rate resulting in a higher bone tissue organization. To describe the peculiar primary cortical bone tissue of Phuwiangosaurus, Ampelosaurus, Lirainosaurus, and Magyarosaurus, we here introduce a new term, “modified laminar bone” (MLB).
Importantly, MLB is as yet not known from extant animals. At least in Lirainosaurus and Magyarosaurus the reduction of growth rate indicated by MLB is coupled with a drastic body size reduction and maybe also a reduction in metabolic rate, interpreted as a result of dwarfing on the European islands during the Late Cretaceous. Phuwiangosaurus and Ampelosaurus both show a similar reduction in growth rate but not in body size, possibly indicating also a reduced metabolic rate. The large titanosaur Alamosaurus, on the other hand, retained the plesiomorphic bone histology of basal neosauropods.
Citation: Klein N, Sander PM, Stein K, Le Loeuff J, Carballido JL, Buffetaut E (2012) Modified Laminar Bone in Ampelosaurus atacis and Other Titanosaurs (Sauropoda): Implications for Life History and Physiology. PLoS ONE 7(5): e36907. doi:10.1371/journal.pone.0036907
Editor: Andrew A. Farke, Raymond M. Alf Museum of Paleontology, United States of America
Received: January 27, 2012; Accepted: April 9, 2012; Published: May 16, 2012
Copyright: © 2012 Klein 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.
Funding: The study was funded by the DFG (Deutsche Forschungsgemeinschaft/FOR 533: Biology of the Sauropod Dinosaurs: The Evolution of Gigantism). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Long Bone Histology of Sauropoda
The histology of fossil tetrapod bones has proven to be a rich source of paleobiological and evolutionary information –, particularly for groups that have no living relatives or in which the living relatives occupy a fundamentally different ecological niche. This is particularly true for sauropod dinosaurs, the largest land-living animals ever , , for which a large amount of histological data have become available in recent years , , . Sauropod long bone histology so far has been viewed as rather uniform , , allowing broad comparisons between taxa . However, bone histology has been less forthcoming in providing characters for phylogenetic analysis, because phylogeny is not the controlling factor in bone histogenesis , .
The most morphologically derived sauropods, the Titanosauria, remain poorly sampled (Fig. 1) because of the relative incompleteness of their remains and the difficulties in their taxonomical assignment. This contrasts with their great diversity and dominance in Cretaceous faunas, particularly on the southern continents . Recently, evidence has accumulated – that titanosaurian long bone histology may be different from that of the more basal neosauropods, i.e., diplodocoid and basal macronarian sauropods of the Jurassic. While some of these differences may be attributed to evolutionary size changes related to island habitats (Magyarosaurus ; Lirainosaurus ), the case is less clear-cut in the limited number of other taxa (Phuwiangosaurus ) that have been studied. Contrary to those smaller sized forms, the large titanosaur Alamosaurus shows a more typical bone tissue type comparable to that of the Jurassic sauropods . It is in this context that our contribution focuses on a growth series of the derived titanosaur Ampelosaurus atacis Le Loeuff, 1995  from the Late Campanian-Early Maastrichtian of southern France .
For the reconstruction of body size evolution, we used femur length as a proxy for body size and optimized it on the only phylogeny that includes all the taxa discussed in this study . Europasaurus was inserted into this phylogeny as a basal macronarian . Magyarosaurus, Lirainosaurus, and Europasaurus show autapomorphic size decrease, i.e., dwarfing. Phuwiangosaurus also has a slightly reduced body size compared to the stem line, while Ampelosaurus shows a slight phylogenetic size increase. Character optimization analysis was performed in TNT .
The differences between basal neosauropods and some titanosaurs are related to the scaffolding of the fibrolamellar bone deposited in the long bones of those sauropods. The typical fibrolamellar bone of basal Neosauropoda is a 3D structure which shows a sequential deposition of different bone types to form a complex tissue. In a first step, a scaffolding of woven (or fibrous) bone matrix is deposited fast around a large vascular canal, and only later is the vascular canal filled in centripetally by lamellar bone. This infill is then called a primary osteon. Fibrolamellar bone is highly vascularized, and its vascular system is dominated by circumferential vascular canals wherefore the tissue is also called laminar fibrolamellar bone, or laminar bone for short.
By describing the long bone (humerus and femur) histology of Ampelosaurus atacis in detail and reviewing the known histology of other titanosaurs (Fig. 1), we would like to address the following questions: Is there such a thing as special titanosaurian bone histology, as proposed by Company ? Can all the peculiarities of titanosaurian bone histology be explained by evolutionary body size reduction? What is the role of island dwarfing in shaping titanosaur bone histology? What are the implications of titanosaurian bone histology for life history, physiology, and evolution of the group? As always, a comparative histological approach is necessary, comparing not only different taxa of titanosaurian and non-titanosaurian sauropods (Fig. 1) but also the same histologic ontogenetic stages (HOS of Klein and Sander ). At this point we would like to emphasize again the importance of sampling homologous points in the long bones of the different sauropod taxa , ,  without which comparisons become difficult, if not impossible.
Previous Work on Sauropod Bone Histology
Bone histology of Diplodocoidea and basal Macronaria.
Because primary bone tissues and patterns of remodeling by secondary osteons are very similar in all studied Diplodocoidea and basal Macronaria , , , , , , , Klein and Sander  erected histological ontogenetic stages (HOS) for these taxa and correlated them with biological ontogenetic stages (BOS) . The HOS were defined on the basis of changes in the principally laminar fibrolamellar bone tissue. These changes mainly concern the type of primary bone tissue (i.e., the amount of woven bone matrix, parallel-fibered bone matrix, and lamellar bone matrix in the fibrolamellar complex), organization of the vascular system, the degree of vascularization, the presence and degree of development of primary osteons, the presence of growth marks, and the appearance of an external fundamental system (EFS). A further important characteristic is the occurrence and density of secondary osteons . Thus, each HOS for Diplodocoidea and basal Macronaria is defined by a certain bone tissue type, the absence or presence of growth marks and an EFS, and by the degree of remodeling by secondary osteons .
Bone histology of humeri and femora of basal Macronaria is similar to that of most other basal Neosauropoda (mainly Diplodocoidea). They share a thick cortex which consists of large amounts of laminar fibrolamellar bone tissue. Later in ontogeny, the fibrolamellar bone tissue changes to lamellar zonal bone tissue, called an external fundamental system, convergent on the conditions in mammals (EFS; sensu Cormack ). The EFS is thought to indicate a growth plateau which indicates that maximum body size and skeletal maturity is reached in an individual. No kind of growth marks appear in those taxa before type E bone tissue is deposited (HOS 9 or 10; ), and growth marks usually remain rare until late ontogenetic stages, when a distinct slow down in growth rate occurs. Vascularization, and therefore growth rate, decreases gradually from young to fully grown individuals. Dense remodeling of the primary cortex by secondary osteons is characteristic of Diplodocoidea and basal Macronaria. Remodeling by secondary osteons starts in young adults (type D bone tissue, HOS 8) and continuously progresses to very old individuals, in which the entire cortex is made of dense secondary osteons ( = Haversian bone).
Bone histology of Europasaurus as described by Sander et al. .
Europasaurus holgeri is a dwarfed, basal macronarian from Kimmeridgian (Upper Jurassic) marine sediments of the Lower Saxony Basin in northern Germany . Its long bone histology resembles that of large basal neosauropods and consists of laminar fibrolamellar bone with an EFS deposited in the outermost cortex of fully grown individuals. Remodeling by secondary osteons increases during ontogeny and is comparable to the pattern seen in basal Neosauropoda. Europasaurus differs from other basal neosauropods in having growth marks in the form of lines of arrested growth (LAGs) throughout its entire cortex, even in ontogenetically young individuals . However, except for the occurrence of these LAGs and the therefore cyclical interruption of growth, the HOS defined for neosauropods are well applicable for Europasaurus. The authors hypothesized that the regular occurrence of growth marks in Europasaurus indicates that bone apposition rate was lower when compared to other basal Neosauropoda. Additionally, growth mark count suggests that the period of active growth was shortened. This implies that Europasaurus, which has a body length of only 6 m, reached its diminutive body size by a reduction in growth rate and a shortening of ontogeny . The reduction in growth rate is indicated by the regular occurrence of lines of arrested growth, which are lacking in all large-bodied sauropods , , whereas the shortening of ontogeny is documented by comparing growth mark counts.
Bone histology of Alamosaurus as described by Woodward and Lehman .
Bone histology of Alamosaurus sanjuanensis from the Upper Cretaceous Javelina and Black Peaks formations in Big Bend National Park, Texas, was extensively studied from different bones of the skeleton by Woodward and Lehman . Woodward and Lehman  described laminar fibrolamellar bone tissue for a humerus of 59% maximum length; in a humerus of 78% maximum length, most of the compact bone is composed of secondary osteons, but remains of primary bone show parallel-fibered bone tissue, and a femur of 81% maximum length is completely remodeled by secondary osteons. Woodward and Lehman  determined the bone tissue type for each bone and HOS following the definition of Klein and Sander . Woodward and Lehman  did not find an EFS in any of their Alamosaurus samples, but they mentioned the possibility of not having sampled fully grown individuals. They found extensive remodeling by secondary osteons in Alamosaurus starting with HOS 7 , which is earlier in ontogeny than in Diplodocoidea where at HOS 7 secondary remodeling starts only scattered . Finally, Woodward and Lehman stated that Alamosaurus bone histology largely resembles that of Apatosaurus as described by Curry .
Bone histology of Phuwiangosaurus as described by Klein et al. .
Humeri and femora of the medium-sized basal titanosaur Phuwiangosaurus sirindhornae from the Lower Cretaceous of Thailand were sampled by core drilling at the standardized sampling location . In general, the bone tissue is continuously growing laminar fibrolamellar bone, typical for other sauropods. The samples of Phuwiangosaurus can be largely assigned to the HOS of Klein and Sander , , although bone histology of Phuwiangosaurus differs in some respects from the original definition of the HOS. For example, type D bone tissue and type E bone tissue have a much higher amount of parallel-fibered and lamellar bone matrix in the fibrolamellar complex when compared to more basal neosauropods. Furthermore, type G bone tissue is not developed, which means that none of the bones is completely or nearly completely remodeled by secondary osteons. Large femora consisting of type E or F bone tissue do not show strong remodeling by secondary osteons which is contrary to the condition in humeri. Growth marks may occur in the outer cortex of both, humeri and femora, but none of the samples shows an EFS. No complete shaft cross sections are known from Phuwiangosaurus bones, but based on the observation of deep drill cores reaching the inner cortex of the opposite side of the shaft, the medullary region is filled by secondary trabeculae.
Klein et al.  concluded that Phuwiangosaurus had a lower growth rate than diplodocoids and basal macronarians. Despite covering a great size range, the Phuwiangosaurus sample may not include very large and old ( = fully grown) individuals, because a fully remodeled cortex and an EFS are missing. Differences in the degree of remodeling between humeri and femora may be explained by biomechanical factors such as strains and forces during limb growth and locomotion, or they could indicate lower apposition rates of the cortical bone in the humerus compared with the femur because of the smaller midshaft diameter of the humerus.
Bone histology of Lirainosaurus as described by Company .
Lirainosaurus astibiae from the Upper Cretaceous of northern Spain is a small (8–10 m) titanosaur related to the Eutitanosauria  and possibly also to the South American Saltasaurinae . The histological study of eleven long bones revealed that Lirainosaurus grew with laminar fibrolamellar bone tissue, which was irregularly interrupted by growth marks . Intense secondary remodeling started early in ontogeny and tended to replace the entire primary bone tissue . Lirainosaurus has a thin bone wall in the femur, with a laterally thicker cortex when compared to the anterior and posterior bone sides . The narrow medullary cavity is almost filled with secondary cancellous tissue and is surrounded by a medullary region containing trabeculae . Mainly on the basis of remodeling by secondary osteons, “young adult individuals”, which equal HOS 11 of Klein and Sander , and “adult individuals” were distinguished. According to Company , no EFS was developed in the outer cortex of Lirainosaurus long bones. Company  concluded that Lirainosaurus attained its smaller size compared to typical sauropods by reducing the rate of primary periosteal apposition and by developing an extensive secondary remodeling well before adult size was reached. He explained the bone histological characteristics of Lirainosaurus as peramorphosis by pre-displacement and sees a reversal of the accelerated pattern of bone deposition normally typical for the sauropod lineage . Company  follows other authors and finds the small body size of Lirainosaurus best explained by insular dwarfing.
Bone histology of Magyarosaurus as described by Stein et al. .
Magyarosaurus dacus is a dwarfed titanosaur from Maastrichtian terrestrial sediments of Romania. The long bone histology of Magyarosaurus is unique among sauropods, because even the smallest individuals of 45% maximum size show nearly complete replacement of the primary cortex by secondary osteons. The well-defined medullary cavity is small and surrounded by cancellous bone. The cortex is thick. The primary organization of the bone tissue is laminar fibrolamellar bone, which mainly consists of parallel-fibered and lamellar bone matrix and has only a minimal amount of woven bone matrix. Magyarosaurus did not have an EFS developed in any sampled individual. Due to the extensive remodeling and the high amount of slow-growing bone matrix in the fibrolamellar complex, the HOS was not strictly applicable. Also, Stein et al.  erected an additional histological ontogenetic stage (HOS 14) to obtain a higher ontogenetic resolution. In two samples of Magyarosaurus, lines of arrested growth are visible (humerus V13492, humerus R 1195), although they are vague and cannot be traced along the complete circumference of the section. Stein et al.  concluded that the intense remodeling of the Magyarosaurus cortex suggests an extremely reduced growth rate compared to basal neosauropods. Stein et al.  interpreted the bone histology and diminutive body size of Magyarosaurus as a result of insular dwarfism.
Materials and Methods
Growth series of humeri and femora assigned to the Late Cretaceous (Late Campanian – Early Maastrichtian) titanosaur Ampelosaurus atacis were sampled. New finds of Ampelosaurus revealed that the maximum known femur length (FL) (ca. 1100 mm, MDE field no. C3-02-172) as well as the largest femur sampled in our study are much larger than the FL cited for Ampelosaurus in the literature (802 mm ). This also necessitated a revision (Fig. 1) of the phylogenetic optimization of body size of titanosaurs by Stein et al. . The current size optimization shows that Ampelosaurus slightly increased in size compared to the ancestral condition. However, the largest humerus sampled is from a distinctly smaller individual than the largest femur known.
While femur length is generally a good proxy for body size in sauropods , , the measurement is difficult to obtain in the sometimes poorly preserved Ampelosaurus material. This also applies to the humeri sampled here. In addition, the correlation between femoral or humeral length and circumference is not very strong (Fig. 2, regression line: R2 = 0.7579 for femora, R2 = 0.3365 for humeri) compared to other sauropods . This is mainly because humeri and femora of Ampelosaurus, each of a similar bone length, can differ in circumference at midshaft by around 100 mm (Table 1, Fig. 2), possibly documenting a gracile and a more robust morphotype . Therefore, we use minimal midshaft circumference as a proxy for body size here, well aware that this is a relatively poor predictor of length in both femora and humeri but a good proxy for body mass. Sampled humeri ranged in midshaft circumference from 130 mm to 320 mm, whereas the size range of femora was smaller, with 235 mm to 480 mm (Table 1). Although we chose to use shaft circumference as a proxy for body size, we recognize that femur and humerus lengths calculated from circumference may have to be used in future comparative work instead of circumferences.
A) Femora. B) Humeri. The plot suggests that there are two morphotypes, because humeri and femora of a similar length form two groups in terms of circumference. A gracile and a more robust type is thus suggested by differences around 100 mm in circumference at midshaft. This graph also includes bones which were not sampled.
Sampled bones are stored in the Musée des Dinosaures, Espéraza, France (labelled as MDE; note: C3 is the code for the locality of Bellevue) or in the local museum of Cruzy, France (labelled as Cru). Bones from the MDE originate from the Bellevue locality in the Upper Aude Valley. The excavation site is located near the small village of Campagne-sur-Aude, which is 3 km southwest of Espéraza. The Bellevue locality has mainly produced disarticulated bones  although a partially articulated titanosaur skeleton is under study. Recent studies have questioned the occurrence of only one titanosaur taxon from this locality . However, the bone bed character of the locality, the preservation of bones, and the uniform morphology of sauropod/titanosaur long bones limits exact taxonomical assignment of isolated humeri and femora.
The bones labelled “Cru” originate from three localities: Cruzy, Montouliers, and Massecaps, all located north of Narbonne and not in the Aude Valley. Stratigraphical age and sediments are similar to the titanosaur locality in the Aude Valley, possibly representing the same historical environment . Therefore, those bones have been preliminarily assigned to Ampelosaurus atacis (Buffetaut pers. obs.). However, ongoing morphological studies indictae that the material from Massecaps (Cru-1723, Cru-4) did not belong to A. atacis but to a new titanosaur (Buffetaut and Le Loeuff pers. obs.). This might be also the case for the other material labelled as “Cru”. However, long bone histology of those samples did not differ from that of A. atacis and can therefore be included in the current study.
The sample location was always in the midshaft region, to gather the most complete record of the appositional growth phase and for comparability with samples from other studies. The standard sampling location for humeri is the posterior bone side of the midshaft, and for femora it is the anterior bone side of the midshaft , , . However, due to preservation of Ampelosaurus bones it was sometimes necessary to sample the opposite side of the shaft. As described in the “Results” section, bone tissue varies between the anterior and posterior bone side of humeri and femora in Ampelosaurus. Humeri show posteriorly an older bone tissue and therefore a later histological ontogenetic stage and a higher degree of remodeling by secondary osteons than anteriorly (see Table S1). In femora, the reverse is true. While to be expected, the difference between the anterior and the posterior side of the bone has not been described in any detail in other sauropod long bones previously. For comparing the Ampelosaurus samples with those from other sauropods, we use only the histology at the standardized location, even when the entire cross section is available.
Four humeri of Alamosaurus sanjuanensis from the Upper Cretaceous Javelina Formation in Big Bend National Park, Texas, housed in the TMM were sampled by core drilling (Table 2; Fig. 3) according to the methods described by Sander  and Stein and Sander . The humeri represent a small growth series and were sampled to supplement the data set of Woodward and Lehman .
The bones tissues in this growth series of the large titanosaur Alamosaurus are identical to those of large diplodocoid and basal macronarian sauropods. The plane of sectioning is perpendicular to bone long axis, and the direction of bone apposition is towards the top of the images. A) Typical laminar fibrolamellar bone tissue of a young individual (HOS 4; TMM 45600-1; 460 mm long, 31% max. size) in normal light. Note the absence of LAGs but the subtle modulations in vascularization (arrows). B) Same view in polarized light. Note the dominance of the scaffolding of woven bone in the fibrolamellar complex. C) Typical laminar fibrolamellar bone tissue of a young adult individual (HOS 7; TMM 43600-2; 915 mm long, 61% max. size). Note the strictly circumferential arrangement of the vascular canals. D) Same view in polarized light. Note the primary osteons in the scaffolding of woven bone. E) Incipient EFS in the outermost cortex and scattered secondary osteons in laminar fibrolamellar bone of a fully grown individual (HOS 12; TMM uncat.; 1350 mm long, 90% max. size). F) Same view in polarized light. Note the highly birefringent parallel-fibered bone of the EFS and the woven to parallel-fibered scaffolding of the fibrolamellar bone in the deeper cortex, between the secondary osteons. The high amount of parallel-fibered bone in the scaffolding of the fibrolamellar bone is typical in late ontogenetic stages in diplodocoid and basal macronarian dinosaurs  as well as for Alamosaurus but occurs already in early ontogenetic stages in Ampelosaurus.
Sampling was by core drilling, extraction of bone fragments, and cross sectioning at midshaft. The coring method used here has been described in detail before , , . The cores and bone pieces were embedded in epoxy resin and cut perpendicular to the long axis of the bone, which is also perpendicular to the growth direction. Half of the sample was processed into a standard petrographic thin section and the other half into a polished section. Thin sections were examined by standard light microscopic techniques (normal transmitted light, polarized light) with a Leica DMLP compound microscope (1.6x to 40x objective lenses). Terminology follows Francillon-Vieillot et al.  and Klein and Sander .
Long Bone Histology of Ampelosaurus Atacis
The primary bone tissue of all sampled Ampelosaurus bones shows principally the typical laminar organization and a 3D structure (scaffolding) of bone deposition similar to the fibrolamellar bone of Diplodocoidea and basal Macronaria (as described before and by, e.g., , , , , , , , ). However, in one aspect, the primary cortical bone tissue of Ampelosaurus atacis differs largely from that of more basal neosauropod dinosaurs (Fig. 4, 5), because already at an early ontogenetic stage the scaffolding of the fibrolamellar bone is partially laid down as parallel-fibred and lamellar bone matrix instead of woven bone matrix (Table S1, Fig. 4, 5). In adult but still growing individuals, no woven bone matrix was deposited at all in the primary cortex (Fig. 4, 5).
A) Modified laminar bone at the anterior bone side of humerus C3-270 (cam 170 mm). The vascular canals are wide open, and primary osteons had not yet developed. The scaffolding of the fibrolamellar bone consists largely of parallel-fibered and lamellar bone matrix. This bone tissue represents HOS 7. B) Modified laminar bone at the posterior bone side of humerus C3-270 (cam 170 mm). The vascular canals are still distinctly open. Laminar organization is greater when compared to the anterior bone side. Primary osteons had partially developed. The scaffolding of the fibrolamellar bone consists of parallel-fibered and lamellar bone matrix. This bone tissue represents HOS 9. C) Modified laminar bone at the anterior bone side of humerus C3-1506 (cam 195 mm, humerus length is 620 mm). Primary bone tissue is visible in the upper third of the cortex, whereas the inner part is remodeled by secondary osteons. The scaffolding of the fibrolamellar bone consists of parallel-fibered and lamellar bone matrix. Primary osteons are nearly filled in. This bone tissue represents HOS 11. D) Modified laminar bone of humerus Cru-1723 (cam 250 mm). The scaffolding of the fibrolamellar bone consists largely of lamellar bone matrix. The vascular density in this sample is still moderate with still open primary osteons. Most of the cortex is completely remodeled by secondary osteons. The outer cortex shows dense secondary osteons. This bone tissue represents HOS 12. E) The posterior bone side of humerus C3-602 (cam 250 mm) is completely remodeled by secondary osteons representing HOS 13. F) The anterior bone side of humerus C3-1189 (cam 310 mm) is completely remodeled by secondary osteons representing HOS 13.
A) Modified laminar bone at the anterior side of femur C3-1182 (cam is 255 mm, femur length is 695 mm). The scaffolding of the fibrolamellar bone consists largely of parallel-fibered bone matrix. The vascular canals are still open. Primary osteons had partially developed. Dense remodeling occurs up to the middle cortex, and there are scattered secondary osteons in the outer cortex. This bone tissue represents HOS 11. B) Modified laminar bone on the anterior side of femur C3-203 (cam 270 mm, femur length is 780 mm). The scaffolding of the fibrolamellar bone consists largely of lamellar bone matrix. The vascular canals are still open, and primary osteons had partially developed. Dense remodeling occurs up to the outer cortex. This bone tissue represents HOS 12. C) Modified laminar bone on the anterior side of femur C3-527 (cam 280 mm, femur length is 680 mm). The primary cortex is completely remodeled by secondary osteons. This bone tissue represents HOS 13. D) Modified laminar bone on the anterior bone side of femur C3-261 (cam 288 mm, femur length is 840 mm). The vascular canals are nearly filled in. Primary osteons had only poorly developed. The scaffolding of the fibrolamellar bone consists largely of parallel-fibered bone matrix. This bone tissue represents HOS 12. E) Modified laminar bone on the anterior side of femur C3-1239 (cam 350 mm). The vascular canals are still open. Primary osteons are well developed. The scaffolding of the fibrolamellar bone consists of parallel-fibered and lamellar bone matrix. This bone tissue represents HOS 11. F) Modified laminar bone on the anterior side of femur C3-78 (cam 465 mm). The vascular canals are still open. Primary osteons are well developed. The scaffolding of the fibrolamellar bone consists laregly of lamellar bone matrix. Secondary osteons are only scattered throughout the cortex. This bone tissue represents HOS 11.
Osteocytes are in most places numerous, although often flattened. In many samples the outermost cortex is partially or completely absent due to poor preservation. On the basis of the cross sections, the posterior bone side of the humeri always shows “older” bone tissue (i.e., a higher HOS) than the anterior side (Fig. 6). Thus, the primary cortex is more organized, less vascularized, and more remodeled when compared with the bone tissue at the anterior bone side (Table S1; Fig. 6). The opposite situation seems to be true for femora, although our study includes only one informative femur cross section.
Vascular organization and vascular density.
The vascular density is generally higher in early histological ontogenetic stages (Fig. 4, 5) and decreases progressively with increasing ontogenetic age, as was described before for other sauropods . However, vascular density remains relatively high with still open vascular canals in the outer cortex even when the fibrolamellar bone has a primarily lamellar bone scaffolding. On the basis of the cross sections, the posterior bone side of the humeri always show a lower vascular density when compared with the anterior bone side (Table S1; Fig. 4, 5), as noted above. In femora, the anterior bone side shows a lower vascular density. The organization of vascular canals is laminar in most samples, but some show a less laminar organization and a higher amount of longitudinal vascular canals (Table S1). In one humerus cross section (MDE C3-270), the vascular canals are diagenetically widened. In some samples of a similar HOS, primary osteons are well developed, but only poorly developed in others (Table S1). This means that no distinct centripetal infilling of the vascular canal by lamellar bone matrix is visible. This infilling is then hard to distinguish from the initially laid down framework of lamellar matrix.
Growth marks and EFS.
In none of our samples are growth marks of any kind or an EFS developed (Table S1) despite sufficient preservation of the outer bone surface. However, since we did not sample the largest individuals assigned to Ampelosaurus (Le Loeuff pers. obs.), we cannot exclude the possibility that these preserve an EFS. In addition, an EFS may have been present in some of the bones in our sample but may have been obliterated by remodeling (see below).
Remodeling by secondary osteons.
Remodeling by secondary osteons is common in the current sample, with only three exceptions. Secondary osteons are not developed in MDE C3-977 and MDE C3-270, which, on the basis of their primary bone tissue, represent early HOS (Fig. 4A, B; Table 3, Table S1). The femur sample Cru-3, which is assigned to HOS 11 (Table 3), shows only a few scattered secondary osteons throughout the entire cortex and cross section. All other Ampelosaurus samples show dense secondary osteons in the inner and middle cortex with scattered ones in the outer cortex, or they are already completely or nearly completely remodeled by secondary osteons (Table S1). In the humeri, the process of remodeling by secondary osteons is faster on the posterior bone side than on the anterior bone side (Fig. 6); in femora it is the other way around (Table S1). In one sample (Cru-4), the secondary osteons have an untypical, elongated diamond-shaped form, although the sampling plane is the same in all samples. This suggests that these secondary osteons are not oriented strictly longitudinally but at some angle to the bone long axis, which is atypical for Neosauropoda.
A free medullary cavity does not exist in Ampelosaurus, but the medullary region consists completely of secondary cancellous bone (Fig. 6). The medullary region is relatively large in all samples (Table S1). In the triangular to oval humeral cross section of MDE C3-270 and MDE C3-238, the medullary region is more or less centered, and the primary cortex is consistently thin all around the cross section, except for the medial bone side where the primary cortex is thicker. In the oval cross section of humerus MDE C3-977, the medullary region is smaller and displaced towards the posteromedial bone side. The primary cortex is very thick along the anterolateral bone sides (more than three times when compared to the other bone sides). In both samples, the secondary trabeculae of the medullary region are partially replaced in the center by a postmortem modification in form of a hole that was filled with fine sediment during fossilization. These holes apparently were caused by some bone-mining organism such as arthropods. The round to oval cross sections of femora Cru-3 and Cru-6 show a relatively smaller medullary region when compared to the humerus cross sections (Table S1). Both medullary regions originally contained secondary trabeculae but are now partially replaced by several small roundish holes filled with sediment during fossilization. In Cru-3, the medullary region is displaced posteriorly and somewhat laterally, leaving the anterior and medial bone side with the thickest primary cortex. In Cru-6, the medullary region is centered, and the primary cortex is of more or less even thickness around the cross section.
Ontogenetic Variation and Taxonomical Implications
On the basis of morphology and size, the sampled humeri represent one ontogenetic series (Table 1, Table S1). However, the two smallest humeri sampled (MDE C3-977, MDE C3-270; Table 1, Table S1) show clear differences in bone tissue and HOS. Humeri MDE C3-977 and MDE C3-270 show a low but certain amount of woven bone matrix in the scaffolding of the fibrolamellar complex, both are well laminar organized, and they lack any growth marks (Fig. 4A, B). They show no secondary osteons in their cortex.
Based on the maximum femur length for Ampelosaurus of around 1100 mm, the femur sample includes half-sized individuals (min. sampled femur length is 630 mm; Table 1, Table S1). However, the histology of femora does not show a large range of HOS (Table 3, Table S1) but can be divided into two groups: some larger femora are not yet completely remodeled, but other smaller femora are (Fig. 5, 7, Table 3, Table S1). This disparity must not represent different taxa but could instead also indicate sexual dimorphism or developmental plasticity .
Circumference at midshaft (mm) versus histological ontogenetic stage (HOS) from the posterior and the anterior bone side. Note that the posterior side in the humerus is a later stage than the anterior one (the standard sampling location) and that the anterior side of femur is older than the posterior side (the standard sampling location). Red arrows connect the anterior and posterior side of the same bone (from old to young). The rectangles mark the samples form A. atacis from Bellevue locality. The triangles mark the samples from titanosaurs north of Narbonne (Cru).
Modified Histological Ontogenetic Stages (HOS) for Ampelosaurus
Differences in bone histology of A. atacis compared to basal neosauropods limit the application of the HOS of Klein and Sander , necessitating modifications to accommodate Ampelosaurus. Accordingly, we redefine bone tissue types C to F of Klein and Sander  for Ampelosaurus (Table 3, Fig. 7) to improve comparability with the HOS of more basal Diplodocoidea and basal Macronaria.
Type A and type B bone tissues are not known for Ampelosaurus. Assuming that humeri MDE C3-977 and MDE C3-270 are juveniles of Ampelosaurus, the definition of type C bone tissue is largely the same in Ampelosaurus as in other sauropods , except for a low amount of woven bone matrix in the scaffolding of the fibrolamellar complex. Instead parallel-fibered matrix and lamellar bone matrix builds most of the scaffolding here. Type D bone tissue of Ampelosaurus differs in nearly all aspects from that of Diplodocoidea and basal Macronaria. The scaffolding of the fibrolamellar complex is solely built of parallel-fibered matrix and lamellar bone matrix, resulting in much more highly organized primary bone tissue. There are no growth marks in type D bone tissue of Ampelosaurus, and secondary osteons are absent throughout the primary cortex (Fig. 4A, B). Type E bone tissue of Ampelosaurus is characterized by a moderate vascular density. The scaffolding of the fibrolamellar complex shows nearly exclusively lamellar bone matrix. However, the primary cortex still does not show any growth marks or secondary osteons. Type F bone tissue type of Ampelosaurus shows a generally lower vascular density (when compared to type E bone tissue type), but in some samples there is still a moderate vascular density (Fig. 4C). Primary osteons are still immature, and the framework of the fibrolamellar complex consists exclusively of lamellar bone matrix. In type F bone tissue of Diplodocoidea and basal Macronaria, a change in bone tissue type from the fibrolamellar complex to lamellar zonal bone tissue is initiated, ultimately forming an EFS (sensu Cormarck ). Neither an EFS nor any other growth marks occur in any bone tissues of specimens of Ampelosaurus. Remodeling by secondary osteons does not occur before type F bone tissue in Ampelosaurus. In Diplodocoidea and basal Macronaria, remodeling already starts in type D bone tissue, but the remodeling is not very dense before some type E bone tissue is deposited. Whereas in Diplodocoidea and basal Macronaria secondary osteons are initially scattered and become more and more dense during ontogeny, secondary osteons appear very suddenly in Ampelosaurus and from dense Haversian bone from their first appearance onwards. All Ampelosaurus samples show this sudden dense remodeling except for two femur samples (Cru-3; MDE C3-638). In these samples, remodeling is more moderate, with scattered or dense secondary osteons only rarely reaching the middle of cortex. Type G bone tissue in Ampelosaurus means a cortex completely remodeled by secondary osteons, as in basal Neosauropoda.
Long Bone Histology of Alamosaurus Sanjuanensis
Alamosaurus sanjuanensis shows the laminar fibrolamellar bone tissue typical for basal neosauropods and macronarians with a scaffolding of woven bone matrix. Its cortical histology shows the ontogenetically different bone tissue types which meet the definition of the HOS as described by Klein and Sander  (Fig. 3A). The primary bone tissue of Alamosaurus has a much woven bone matrix in early ontogenetic stages. In late ontogenetic stages the amount of parallel-fibered and lamellar matrix increases successively in the scaffolding of the fibrolamellar bone of Alamosaurus. Humerus TMM uncataloged (1350 mm) has in its outermost cortex two LAGs deposited accompanied by a change from fibrolamellar bone to avascular lamellar bone tissue, which may represent an incipient EFS (Fig. 3B).
Implications of Histology for Life History and Growth Pattern
The peculiar histology of the Ampelosaurus primary cortical bone and the modifications of the HOS as described here raises the question what we can deduce about patterns of growth and life history in this taxon. Ampelosaurus seems to have grown in a way similar to more basal sauropods (although more slowly, as evidenced by the already very highly organized bone tissue before sexual maturity is reached). After this point in ontogeny, bone microstructure of Ampelosaurus differs greatly from that of more basal Sauropoda. Bone tissue types D to E, representing this phase in ontogeny, are characterized by a much higher organization of primary bone and therefore presumably a lower apposition rate. However, this highly organized primary bone is inconsistent with the absence of growth marks and the relatively extensive vascularization, indicating that growth continued slowly but uninterrupted. Although Diplodocoidea and basal Macronaria also show an increase in bone tissue organization ( = decrease in growth rate) around the presumed onset of sexual maturity, it is much more gradual and this phase seems to have lasted longer than in Ampelosaurus. The process of remodeling by secondary osteons, which in other sauropods started around sexual maturity , is clearly delayed in Ampelosaurus. The period of growth after sexual maturity seems to be shortened in Ampelosaurus and is dominated by remodeling instead of fast appositional growth.
A very interesting and not yet understood fact is that most of the Ampelosaurus samples are dominated by type G bone tissue but do not represent the largest known individuals (Le Loeuff pers. obs.). Thus, these bones presumably do not represent fully grown (i.e., skeletally mature) individuals, which is also consistent with the lack of an EFS. This is quite different from the condition in Diplodocoidea and basal Macronaria, in which type G bone tissue only occurs after an EFS was deposited and only in the largest specimens.
Ampelosaurus Histology Compared with other Titanosaurs
The observation that the cortical bone histology of Ampelosaurus is distinct from that of more basal, non-titanosaurian sauropods raises the question of how Ampelosaurus histology compares to that of other titanosaurs (as reviewed in the introductory section of this study) and how features of long bone histology relate to body size.
The largest titanosaur for which comprehensive histological information is available is Alamosaurus sanjuanensis (Fig. 1). In bone dimension and mass this animal rivaled large diplodocoids and large basal macronarians . Alamosaurus also shows a similar long bone histology to the non-titanosaurian sauropods (, this study), and the HOS erected for basal neosauropods are perfectly applicable to Alamosaurus long bones (Fig. 3, Table 2).
In early ontogenetic stages, the long bones of the basal titanosaur Phuwiangosaurus sirindhornae (Fig. 1) show a normal amount of woven bone matrix in the fibrolamellar complex. However, the scaffolding of long bone tissue of adult (sexually mature) Phuwiangosaurus is dominated by parallel-fibered bone matrix and is characterized by the absence of woven bone matrix, similar to Ampelosaurus. Contrary to Ampelosaurus, Phuwiangosaurus has developed growth marks in the outer cortex. The lack of an EFS in Phuwiangosaurus is most probably a sampling artifact, because no fully grown individuals were sampled, and probably does not represent a true histological character of this taxon. An additional argument that the EFS simply was not sampled is the fact of less remodeling in Phuwiangosaurus than in other taxa. In its humeri, Phuwiangosaurus shows a similar remodeling pattern as basal neosauropods starting with scattered secondary osteons. Phuwiangosaurus femora show only little remodeling at all, even in late HOS. Phylogenetic body size optimizations suggest Phuwiangosaurus has somewhat reduced its body size (Fig. 1) compared to the stem line ancestor, and long bone histology suggests that this body size reduction evolved via a reduction in growth rate.
In the case of Lirainosaurus astibiae, phylogenetic optimization of body size (Fig. 1) indicates that this taxon is part of a clade of small-bodied titanosaurs. Lirainosaurus and Ampelosaurus share a high amount of parallel-fibered and lamellar bone matrix, but unlike Ampelosaurus, Lirainosaurus still has woven bone matrix included in the fibrolamellar complex . The two taxa also share strong remodeling by secondary osteons. Company  stated that remodeling was initiated early in the ontogeny of Lirainosaurus, whereas we observed that remodeling in Ampelosaurus does not start before HOS 9/10 (Table S1), a stage which is interpreted as already representing adult (sexual mature) individuals. Although Lirainosaurus and Ampelosaurus share the absence of an EFS, they differ in the presence of growth marks in the primary cortex of Lirainosaurus. Lirainosaurus also has a clearly defined medullary cavity which is not the case in Ampelosaurus.
The island dwarf Magyarosaurus dacus experienced a dramatic evolutionary body size reduction (Fig. 1). However, among the taxa compared here, Magyarosaurus and Ampelosaurus are most similar. Both share dense and extensive cortical remodeling by secondary osteons which leads to a complete remodeling of the primary cortex long before skeletal maturity is reached. This intensive remodeling right up to the outer bone surface seems to be the reason for the absence of an EFS in both taxa. Ampelosaurus and Magyarosaurus differ in the timing of the onset of that remodeling process, which seems to start in Magyarosaurus much earlier in ontogeny  than in Ampelosaurus (see above). However, one could argue that the extensive remodeling by secondary osteons observed in Ampelosaurus was carried to extremes in Magyarosaurus. Differences between Magyarosaurus and Ampelosaurus concern the primary bone tissue organization. In Magyarosaurus the framework consists mainly of parallel-fibered bone matrix, but in Ampelosaurus it consists of lamellar bone matrix. Thus, the degree of bone crystallite organization is higher in Ampelosaurus than in Magyarosaurus (in which it is already higher than in non-titanosaurian sauropods).
Modified Laminar Fibrolamellar Bone
The generally accepted definition of fibrolamellar compact bone  calls for a scaffolding of woven bone matrix filled in by primary osteons. The fibrolamellar complex in the long bones of Phuwiangosaurus, Ampelosaurus, Lirainosaurus, and Magyarosaurus differs from this definition and is also contrary to the condition in non-titanosaurian sauropods and in Alamosaurus. While all of these titanosaurs show the typical laminar vascular organization of sauropod primary cortical bone, the scaffolding in the fibrolamellar complex is laid down as parallel-fibered or lamellar bone instead of woven bone, at least in later ontogenetic stages. It should be noted that high amounts of parallel-fibered and lamellar bone matrix in the scaffolding should not be confused with particularly well developed primary osteons that would have developed only after the deposition of the scaffolding. Neither do we think it is likely that the primary cortical bone of Ampelosaurus is the result of a complete reduction of the scaffolding leading to bone formation by primary osteons only. If this were the case, we should not observe any parallel-fibered matrix at all because osteonal deposition is exclusively lamellar. The question thus arises if the primary cortical tissue of Phuwiangosaurus, Ampelosaurus, Lirainosaurus, and Magyarosaurus still should be called fibrolamellar bone.
To describe this peculiar primary cortical bone tissue of Phuwiangosaurus, Ampelosaurus, Lirainosaurus, and Magyarosaurus, we here introduce a new term, “modified laminar bone” (MLB). Based on accepted sauropod phylogenies (e.g., , see also Fig. 1), MLB is clearly a derived bone tissue type. Its structure also indicates that it must have evolved from the laminar fibrolamellar bone tissue typical for non-titanosaurian sauropods and Alamosaurus (e.g., , , , , , ) by simply laying down the scaffolding as parallel- fibered or lamellar bone matrix instead of woven bone matrix.
Differences between titanosaur bone tissue and that of more basal sauropods were already discussed by Company , who raised the question whether titanosaurs have “special titanosaur histology”. However, he also included the large titanosaur Alamosaurus in the “special titanosaur histology”, a hypothesis that clearly contradicts our own and previously published observations . Thus MLB is currently only known from medium-sized and small titanosaurs. As usual for describing bone histological features, the main terminological problem is that the transition from laminar fibrolamellar complex with a scaffolding of woven bone matrix to MLB with a scaffolding largely without woven bone matrix is gradual and a quantitive definition cannot be given at the moment.
Application of Amprino’s rule  and general principles of biological and physiological organization suggests that MLB had significantly lower apposition rate than regular laminar bone. The initially deposited framework, with a high amount of parallel-fibered or even lamellar bone matrix in MLB could not have been deposited as fast as with woven bone matrix. This also suggests that the overall growth rate of titanosaurs showing MLB was significantly lower than that of neosauropods having grown with normal fibrolamellar bone. A test for this hypothesis is offered by the extinct insular bovid Myotragus balearicus  which grew much more slowly than similar-sized mainland bovids, as evidenced by growth mark counts. Myotragus also shows a complete loss of woven bone matrix from its cortex. However, illustrations and descriptions of its cortical histology are insufficient for determining whether it retained the laminar organization seen in mainland bovids , and whether its tissue thus is MLB.
Growth Marks in Titanosaurs
Growth marks being generally rare in sauropods or appearing only late in ontogeny, if at all , is contrary to the condition in early sauropodomorphs (e.g., Plateosaurus and Massospondylus) and the sister group to Sauropodomorpha, Theropoda , . The absence of growth marks throughout most of sauropod ontogeny is problematic because it hampers the construction of growth curves and estimates of absolute bone apposition rates , . On the other hand, the lack of growth marks is suggestive of fast and uninterrupted growth in sauropods, which supports the hypothesis that they achieved large body size through the heterochronic process of acceleration .
The deposition of growth marks in the outer cortex of adult Phuwiangosaurus and in the middle to outer cortex of adult Lirainosaurus long bones starts in young adult individuals and therefore conforms to the typical pattern in sauropods. However, the more regular occurrence and higher number of growth marks in Lirainosaurus when compared to non-titanosaurian sauropods  suggests that this titanosaur, in addition to its reduced growth rate (achieved by a higher organized bone tissue), slowed growth by regular cessations in growth. Conversely, one could argue that growth in Lirainosaurus was slow enough so that growth marks were deposited.
Magyarosaurus shows LAGs only in two samples, and Ampelosaurus does not show any growth marks in any bone sample. This is rather inconsistent with the apparently reduced growth rate and high level of bone organization seen in both taxa, features which are often associated with the deposition of growth marks. The most likely explanations for the lack of growth marks in Magyarosaurus and Ampelosaurus are: (1) the process of remodeling by secondary osteons was so fast that the primary cortex was already remodeled before any growth marks could have been deposited and (2) existing growth marks were obliterated by remodeling shortly after they were deposited. In both cases it is clear that the remodeling process in Ampelosaurus and Magyarosaurus is much faster than in Phuwiangosaurus and Lirainosaurus or any other sauropod.
The Lack of an EFS in Titanosaurs
Based on the observations of extant mammals by Cormack , skeletal maturity of an individual was reached in sauropods when an EFS developed. Lirainosaurus, Magyarosaurus, and Ampelosaurus do not show an EFS. Company  had discussed several hypotheses explaining the lack of an EFS in Lirainosaurus such as: an indeterminate growth strategy, remodeling by secondary osteons, or the sampled individuals were still actively growing (despite strong remodeling). However, he finally concluded that none of these hypotheses fit and that the lack of an EFS is a real histological feature of Lirainosaurus and possibly other titanosaurs as well . Stein et al.  also offered various explanations for the lack of an EFS in Magyarosaurus: the EFS was already obliterated by secondary osteons, an EFS was generally not deposited, or the outer surface of the bones was incompletely preserved.
The absence of an EFS in Ampelosaurus is best explained with arguments similar to those above. The fact that the largest femora and humeri of Ampelosaurus are around 20% larger than the largest bones of Ampelosaurus sampled here may explain the lack of an EFS in this taxon as an an artifact of incomplete sampling. However, even in smaller bones of Ampelosaurus, remodeling by secondary osteons is so fast and intense that the entire primary bone tissue is already remodeled (Table S1), although these bones do not come from fully grown individuals. Thus, an EFS in Ampelosaurus could simply have been obliterated by the fast remodeling process (as suggested for Magyarosaurus by Stein et al. ). This would mean that the deposition of primary bone is closely followed by the remodeling process and, therefore, primary bone tissue is no longer visible. This hypothesis is supported by the observation that in humeri, the anterior bone side always shows a “younger” bone tissue than the posterior bone side and the other way around in femora (see above and SI). Thus, several samples still have remains of primary cortex without an EFS developed at one bone side whereas the other bone side is already completely remodeled (Table S1).
Patterns of Remodeling by Secondary Osteons
Remodeling of primary bone tissue by secondary osteons, culminating in dense Haversian bone, is widespread in large-bodied Dinosauria and Mammalia , . However, the meaning of this cortical remodeling process is not well understood. Several, not mutually exclusive, hypotheses explain the occurrence of secondary osteons: healing of fatigue microcracks, removal of dead tissue, remobilization of bone mineral, and simply a time-dependant process (see Currey  and Sander et al.  for a good review). A commonly cited hypothesis, that Haversian remodeling strengthens the bone, seems unlikely because Haversian bone is less strong than primary bone, at least under a bending load .
Klein et al.  hypothesized that the co-occurrence of intense remodeling and high amounts of parallel-fibered bone in Phuwiangosaurus may indicate that remodeling in sauropods progresses outwards at a constant rate independent of the apposition rate of the primary tissue. If apposition rate is comparatively low, as in the MLB of the titanosaurs studied here, remodeling will affect relatively more of the primary bone than in faster growing non-titanosaurian sauropods and Alamosaurus. Similarly, in Ampelosaurus and Magyarosaurus, the apposition front depositing primary bone tissue obviously was overrun by the process of remodeling. Additionally, in Ampelosaurus, the remodeling process must have been extremely fast, because it started only late in ontogeny but reached the bone surface quickly.
The argument of Company  that “secondary remodeling took place during pauses in periosteal bone deposition, or gradually, as the periosteal growth rate slowed down” was already falsified by the remodeling pattern in Diplodocoidea and basal Macronaria, which clearly show that remodeling takes place independently of periosteal growth , , . Also, Company’s hypothesis that secondary reconstruction “equaled or even exceeded the energy requirements for deposition of primary bone”  is unlikely because resorption and re-deposition takes place very locally and no additional bone tissue is added; only existing tissue is remodeled. Therefore, rather the contrary is likely, and secondary bone seems to require less energy than the deposition of primary bone because no new materials need to be added to the tissue.
A relationship between the degree of secondary osteon development and ontogeny was already pointed out by Sander  and explored more in depth by Klein and Sander  and Sander et al. . Among other histological features, we used the occurrence and density of secondary osteons for the definition of the histological ontogenetic stages for Diplodocoidea and basal Macronaria. However, the sudden onset of remodeling seen in Ampelosaurus has not been observed before in sauropods. A possible explanation involves the hormonal onset of sexual maturity. More explicitly, secondary osteon formation may possibly have been triggered or controlled by hormones which initiate sexual maturity, because bone metabolism in mammals is greatly influenced by hormones . However, this hypothesis fails to explain why the onset of sexual maturity is more sudden in Ampelosaurus than in other sauropods.
Evolutionary Origins of Reduced Growth Rates in Titanosaurs
In order to understand the diversity of histological patterns and growth rate reduction seen in some titanosaurs, a look at the body size of the taxa and possible effects of island dwarfing is needed. Beside the similar size, Alamosaurus (FL = 1610 mm ) and basal neosauropods share a uniform long bone histology and show no indication for reduced growth rates. Patterns divergent from typical sauropod histology are seen in the two small titanosaurs examined or reviewed for this study and in the normal-sized Ampelosaurus and Phuwiangosaurus. Because the rate of deposition of the bone matrix determines the rate of size increase of the bone, the high amount of parallel-fibered and lamellar bone matrix in the early ontogenetic stages of Phuwiangosaurus, Ampelosaurus, Lirainosaurus, and Magyarosaurus implies a low rate of bone deposition and therefore a lower growth rate for these titanosaurs compared to non-titanosaurian sauropods and Alamosaurus.
Together with other histological peculiarities, the reduced growth rate and body size of Magyarosaurus (FL = 540 mm, ) have been interpreted as an adaptation to limited resources on an island (, see also Sander et al.  on Europasaurus). This raises the question whether resources were limited for the other titanosaur species (except Alamosaurus) as well. Both Ampelosaurus (FL = ca. 1100 mm, MDE C3-02-172) and Lirainosaurus (FL = 686 mm, ) inhabited large islands of the Late Cretaceous southwestern European archipelago , , the former the southern French island in the Campanian-Maastrichtian and the latter the Iberian island in the Campanian. While Lirainosaurus may have responded to the resource limitations by a reduction in body size (although body size optimizaton suggests otherwise) and a decrease in growth rate, the larger Ampelosaurus only decreased its growth rate.
An insular habitat limiting resources can be excluded in the case of the relatively large-bodied Phuwiangosaurus (FL = 1250 mm ) that inhabited the Indochina peninsula which remained fully connected to the East Asian land mass throughout the Cretaceous . Thus, while there may well be a distinctive island signal in the decrease in body size and/or growth rate in titanosaurian bone histology (Ampelosaurus, Lirainosaurus, and Magyarosaurus), other adaptive pressures must also have been able to produce reduced growth rates in titanosaurs, notably Phuwiangosaurus. A more complete understanding of this evolutionary phenomenon and the evolution of MLB must await a comprehensive sampling of titanosaur bone histology, especially of the South American species, combined with patterns of body size evolution in titanosaurs .
Based on a detailed histological analysis of the cortical long bone histology of a growth series of the derived titanosaur Ampelosaurus, we review and discuss titanosaurian bone histology. Although taxon sampling is limited (Alamosaurus, Ampelosaurus, Lirainosaurus, Magyarosaurus, Phuwiangosaurus), four out of the five taxa (Alamosaurus being the exception) show a peculiar primary cortical tissue, here termed Modified Laminar Bone (MLB), that evolved from the standard laminar fibrolamellar bone (FLB) of sauropods. During the evolution of MLB, the laminar organization of the vascular network was retained, but only the initial scaffolding of bone deposition in early ontogenetic stages contains a low amount of woven bone matrix (as in typical FLB). During most of ontogeny the scaffolding consists of highly organized parallel-fibered bone matrix grading into lamellar bone matrix instead of woven bone matrix. The gradual infill of the vascular canal by lamellar bone, i.e. the formation of primary osteons, in FLB was retained in MLB. Currently, MLB is unique to the four titanosaur taxa studied here, but it also may have evolved in the extinct island bovid mammal Myotragus. MLB and patterns of remodeling also necessitated the modification of histological ontogenetic stages (HOS) of more basal sauropods for usage in Ampelosaurus.
MLB unequivocally indicates a greatly reduced cortical apposition rate compared to laminar FLB, and thus a greatly reduced growth rate of the titanosaurs that show it. This reduction is difficult to quantify because of the lack of growth marks seen in most titanosaur taxa with MLB. While the drastic growth rate reduction documented by MLB may have evolved as a response to resource limitations on an island, this hypothesis is only satisfactory for the island dwarf Magyarosaurus  and the possible island dwarf Lirainosaurus. Paleogeography suggests that the non-dwarfed Ampelosaurus may also have responded with MLB to resource limitations, but this is not the case in Phuwiangosaurus. Clearly, a better understanding of MLB in titanosaurs must await a more comprehensive taxon sampling.
Histological description of sampled bones of Ampelosaurus atacis from Bellevue locality (MDE C3) and the titanosaurs from north of Narbonne (Cru). The bones are listed by midshaft circumference (see Table 1). Abbreviations: FLB = fibrolamellar bone tissue; ic = inner cortex; lb = lamellar bone matrix; mc = medullary cavity; oc = outer cortex; pfb = parallel-fibered bone matrix; po = primary osteons; wb = woven bone matrix.
We would like to thank our preparatory, Olaf Dülfer (Steinmann Institut, Paleontology, Bonn), for handling the many polished and thin section forming the basis of this study, and Georg Oleschinski for the photographs of the sections (Steinmann Institute, Paleontology, Bonn). KS thanks Wann Langston, Tim Rowe and Ernie Lundelius (Texas Memorial Museum, Austin, Texas) for the warm reception and access and permission to sample Alamosaurus material. We would like to thank an anonymous reviewer, Holly Woodward (Museum of the Rockies, Bozeman, Montana), and the academic editor, Andrew Farke (Raymond M. Alf Museum of Paleontology, Clarement, California), for their helpful comments on the manuscript. This is contribution number 125 of the DFG Research Unit 533, ‘‘Biology of the Sauropod Dinosaurs’’.
Analyzed the data: NK PMS KS. Contributed reagents/materials/analysis tools: JL EB. Wrote the paper: NK PMS. Performed the character optimization for the phylogenetic analysis: JLC. Contributed locality and specimen informations: JL EB.
- 1. Erickson GM (2005) Assessing dinosaur growth patterns: a microscopic revolution. Trends in Ecology and Evolution: 20: 677–684.
- 2. Chinsamy-Turan A (2005) The microstructure of dinosaur bone. Baltimore: Johns Hopkins University Press. 195 p.
- 3. Scheyer TM, Klein N, Sander PM (2010) Developmental palaeontology of Reptilia as revealed by histological studies. Seminars in Cell and Developmental Biology 21: 462–470.
- 4. Sander PM, Klein N, Stein K, Wings O (2011) Sauropod bone histology and implications for sauropod biology. In: Klein N, Remes K, Gee CT, Sander PM, editors. Biology of the sauropod dinosaurs: understanding the life of giants. Bloomington: Indiana University Press. 344p. pp. 276–302.
- 5. Sander PM, Clauss M (2008) Sauropod gigantism. Science 322: 200–201.
- 6. Klein N, Sander PM (2008) Ontogenetic stages in the long bone histology of sauropod dinosaurs. Paleobiology 34: 247–263.
- 7. Woodward H, Lehman TM (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.
- 8. Cubo J, Legendre P, de Ricqles A, Montes L, de Margerie E, et al. (2008) Phylogenetic, functional, and structural components of variation in bone growth rate of amniotes. Evolution and Development 10: 217–277.
- 9. Montes L, Castanet J, Cubo J (2010) Relationship between bone growth rate and bone tissue organization in amniotes: first test of Amprino’s rule in a phylogenetic context. Animal Biology 60: 25–41.
- 10. Curry-Rogers KA (2005) Titanosauria: a phylogenetic overview. In: Curry-Rogers K, Wilson JA, editors. The sauropods: evolution and paleobiology. Berkeley: University of California Press. p 349. pp. 50–103.
- 11. Klein N, Sander PM, Suteethorn V (2009) Bone histology and its implications for the life history and growth of the Early Cretaceous titanosaur Phuwiangosaurus sirindhornae. Geological Society, Special Publications 315: 217–228.
- 12. Company J (2011) Bone histology of the titanosaur Lirainosaurus astibiae (Dinosauria: Sauropoda) from the Latest Cretaceous of Spain. Naturwissenschaften 98: 67–78.
- 13. Stein K, Csiki Z, Curry-Rogers K, Weishampel DB, Redelstorff R, et al. (2010) Small body size and extreme cortical bone remodeling indicate phyletic dwarfism in Magyarosaurus dacus (Sauropoda: Titanosauria). Proceedings of the National Academy of Sciences of the United States of America 107: 9258–9263.
- 14. Le Loeuff J (1995) Ampelosaurus atacis (nov, gen., nov. sp.), a new titanosaurid (Dinosauria, Sauropoda) from the Upper Cretaceous of the Upper Aude Valley (France). Comptes Rendus de l’Académie des Sciences à Paris Série IIa 321: 693–699.
- 15. Le Loeuff J (2005) Osteology of Ampelosaurus atacis (Titanosauria) from southern France. In: V InTidwell, K Carpenter, editors. editors. Thunder-lizards: the sauropodomorph dinosaurs. Bloomington: Indiana University Press. pp. 115–137.
- 16. Sander PM (2000) Long bone histology of the Tendaguru sauropods: implications for growth and biology. Paleobiology 26: 466–488.
- 17. Sander PM (1999) Life history of the Tendaguru sauropods as inferred from long bone histology. Mitteilungen aus dem Museum für Naturkunde in Berlin, Geowissenschaftliche Reihe 2: 103–112.
- 18. Sander PM, Klein N, Buffetaut E, Cuny G, Suteethorn V, et al. (2004) Adaptive radiation in sauropod dinosaurs: bone histology indicates rapid evolution of giant body size through acceleration. Organisms, Diversity and Evolution 4: 165–173.
- 19. Cormack D (1987) Ham’s histology. New York: Lippincott Williams & Wilkins. 732 p.
- 20. Sander PM, Mateus O, Laven T, Knötschke N (2006) Bone histology indicates insular dwarfism in a new Late Jurassic sauropod dinosaur. Nature 441: 739–741.
- 21. Curry KA (1999) Ontogenetic histology of Apatosaurus (Dinosauria: Sauropoda): new insights on growth rates and longevity. Journal of Vertebrate Paleontology 19: 654–665.
- 22. Company J, Pereda-Suberbiola X, Ruiz-Omeñaca JI (2009) Nuevos restos fósiles del dinosaurio Lirainosaurus (Sauropoda, Titanosauria) en el Cretácico superior (Campaniano-Maastrichtiano) de la Península Ibérica. Ameghiniana 46: 391–405.
- 23. Carrano MT (2006) Body-size evolution in the Dinosauria. In: Carrano MT, Blob RW, Gaudin TJ, Wible JR, editors. Amniote paleobiology: perspectives on the evolution of mammals, birds, and reptiles. Chicago: University of Chicago Press. pp. 225–268.
- 24. Kilbourne BM, Makovicky PJ (2010) Limb bone allometry during postnatal ontogeny in non-avian dinosaurs. Journal of Anatomy 217: 135–152.
- 25. Vila B, Galobart À, Canudo JI, Le Loeuff J, Dinarès-Turell J, et al. (2012) The diversity of sauropod dinosaurs and its first taxonomic succession from latest Cretaceous strata of southwestern Europe: clues to demise and extinction. Palaeogeography, Palaeoclimatology, Palaeoecology: In Press.
- 26. Buffetaut E, Le Loeuff J, Duffaud S, Cavin L, Garcia G, et al. (1999) Un nouveau gisement de vertébrés du Crétacé supérieur à Cruzy (Hérault, Sud de la France). Comptes-Rendus de l’Académie des Sciences de Paris 328: 203–208.
- 27. Stein K, Sander PM (2009) Histological core drilling: a less destructive method for studying bone histology. In: Brown MA, Kane JF, Parker WG, editors. Methods in fossil preparation: proceedings of the first annual Fossil Preparation and Collections Symposium. pp. 69–80.
- 28. Klein N, Sander PM (2007) Bone histology and growth of the prosauropod Plateosaurus engelhardti Meyer, 1837 from the Norian bonebeds of Trossingen (Germany) and Frick (Switzerland). Special Papers in Palaeontology 77: 169–206.
- 29. Francillon-Vieillot H, de Buffrénil V, Castanet J, Géraudie J, Meunier FJ, et al. (1990) Microstructure and mineralization of vertebrate skeletal tissues. In: Carter JG, editor. Skeletal biomineralization: patterns, processes and evolutionary trends. Vol. 1. New York: Van Nostrand Reinhold. pp. 471–530.
- 30. Rimblot-Baly F, Ricqlès A de, Zylberberg L (1995) Analyse paléohistologique d’une série de croissance partielle chez Lapparentosaurus madagascariensis (Jurassique moyen): Essai sur la dynamique de croissance d’un dinosaure sauropode. Annales de Paléontologie (Invert. -Vert.) 81(2): 49–86.
- 31. Sander PM, Klein N (2005) Developmental plasticity in the life history of a prosauropod dinosaur. Science 310: 1800–1802.
- 32. Lehman , TM , Coulson A (2002) A juvenile specimen of the sauropod dinosaur Alamosaurus sanjuanensis from the Upper Cretaceous of Big Bend National Park, Texas. Journal of Paleontology 76: 156–172.
- 33. Wilson JA (2002) Sauropod dinosaur phylogeny: critique and cladistic analysis. Zoological Journal of the Linnean Society of London 136: 217–276.
- 34. Köhler M, Moya-Sola S (2009) Physiological and life history strategies of a fossil large mammal in a resource-limited environment. Proc Natl Acad Sci USA 106: 20354–20358.
- 35. Lehman TM, Woodward HN (2008) Modeling growth rates for sauropod dinosaurs. Paleobiology 34: 264–281.
- 36. Sander PM, Andrássy P (2006) Lines of arrested growth and long bone histology in Pleistocene large mammals from Germany: what do they tell us about dinosaur physiology? Palaeontographica A 277: 143–159.
- 37. Currey JD (2002) Bones: structure and mechanics. Princeton: Princeton University Press. 456 p.
- 38. Smith AG, Smith DG, Funnell BM (1994) Atlas of Mesozoic and Cenozoic coastlines. New York: Cambridge University Press. 99 p.
- 39. Dercourt J, Gaetani M, Vrielynck B, Barrire E, Biju-Duval B, et al. (2000) Peri-Tethys Palaeogeographical Atlas. Paris: Gauthier Villars.
- 40. Metcalfe I (2009) Australia–SE Asia collision: plate tectonics and crustal flow. Geological Society, Special Publications 355: 75–109.
- 41. Goloboff PA, Farris S, Nixon K (2008) TNT, a free program for phylogenetic analysis. Cladistics 24: 774–786.