- Research article
- Open Access
Evolutionary implications of the divergent long bone histologies of Nothosaurus and Pistosaurus(Sauropterygia, Triassic)
BMC Evolutionary Biology volume 13, Article number: 123 (2013)
Eosauropterygians consist of two major clades, the Nothosauroidea of the Tethysian Middle Triassic (e.g., Nothosaurus) and the Pistosauroidea. The Pistosauroidea include rare Triassic forms (Pistosauridae) and the Plesiosauria of the Jurassic and Cretaceous. Long bones of Nothosaurus and Pistosaurus from the Muschelkalk (Middle Triassic) of Germany and France and a femur of the Lower Jurassic Plesiosaurus dolichodeirus were studied histologically and microanatomically to understand the evolution of locomotory adaptations, patterns of growth and life history in these two lineages.
We found that the cortex of adult Nothosaurus long bones consists of lamellar zonal bone. Large Upper Muschelkalk humeri of large-bodied Nothosaurus mirabilis and N. giganteus differ from the small Lower Muschelkalk (Nothosaurus marchicus/N. winterswijkensis) humeri by a striking microanatomical specialization for aquatic tetrapods: the medullary cavity is much enlarged and the cortex is reduced to a few millimeters in thickness. Unexpectedly, the humeri of Pistosaurus consist of continuously deposited, radially vascularized fibrolamellar bone tissue like in the Plesiosaurus sample. Plesiosaurus shows intense Haversian remodeling, which has never been described in Triassic sauropterygians.
The generally lamellar zonal bone tissue of nothosaur long bones indicates a low growth rate and suggests a low basal metabolic rate. The large triangular cross section of large-bodied Nothosaurus from the Upper Muschelkalk with their large medullary region evolved to withstand high bending loads. Nothosaurus humerus morphology and microanatomy indicates the evolution of paraxial front limb propulsion in the Middle Triassic, well before its convergent evolution in the Plesiosauria in the latest Triassic. Fibrolamellar bone tissue, as found in Pistosaurus and Plesiosaurus, suggests a high growth rate and basal metabolic rate. The presence of fibrolamellar bone tissue in Pistosaurus suggests that these features had already evolved in the Pistosauroidea by the Middle Triassic, well before the plesiosaurs radiated. Together with a relatively large body size, a high basal metabolic rate probably was the key to the invasion of the Pistosauroidea of the pelagic habitat in the Middle Triassic and the success of the Plesiosauria in the Jurassic and Cretaceous.
Sauropterygian phylogeny and evolution of aquatic locomotion
Since the beginning of the 19th century, the Mesozoic marine reptile clade Sauropterygia has been subject to intensive morphological studies [e.g., [1, 2]]. Sauropterygia are divided into the Placodontia and the Eosauropterygia which, in turn, classically consist of the Eusauropterygia and the Pachypleurosauria [3–5] (see also Figure 1). Eusauropterygia are divided into the plesiosaur lineage (Pistosauroidea) and the nothosaur lineage (Nothosauroidea). However, in a recent analysis by Holmes et al. , Eosauropterygia remained unresolved in a polytomy, and Eusauropterygia turned out to be paraphyletic (Figure 1A). The Pistosauroidea include the plesiosaurs.
The non-plesiosaurian sauropterygians, commonly referred to as “stem-group sauropterygians”, are known from various localities in Europe [e.g., [7–10]], China [e.g., [6, 11]], USA [e.g., ], Tunisia , and Israel . In the fossil record, they appear for the first time in the latest Early Triassic and disappear in the latest Triassic . The Plesiosauria, also termed “crown-group sauropterygians”, first occur in the earliest Jurassic (or possibly latest Triassic) of Europe , but they spread rapidly around the world during the later Jurassic and Cretaceous to become the most diverse group of marine reptiles .
One of the most familiar stem-group sauropterygians is Nothosaurus, several species of which inhabited the Muschelkalk Sea of the Germanic Basin from early Anisian to early Carnian times (for about 15 Ma). Finds come from the Lower Muschelkalk to the Lower Keuper beds of France, Germany, Poland, The Netherlands, and Switzerland . Unfortunately, phylogenetic relationships within the genus Nothosaurus remain largely unresolved (see most recent phylogenetic analysis , Figure 1C).
Important stem-group sauropterygians of the plesiosaur lineage are Cymatosaurus and Pistosaurus from the Muschelkalk beds. While Cymatosaurus (total length <1.5 m) appears to be restricted to the Lower Muschelkalk , Pistosaurus is only found in beds recording maximum flooding of the Germanic Basin in the Upper Muschelkalk . Pistosaurus and other Pistosauridae such as Augustasaurus from the Anisian of Nevada [12, 18] and Yunguisaurus from the Carnian of China  share a seemingly pelagic lifestyle, consistent with their Northern Hemisphere and presumably cosmopolitan distribution. Pistosauridae are substantially larger (2–3 m total lengh) than the more basal Pistosauroidea such as Cymatosaurus and Corosaurus[19–21] but are of the same size as the basal Plesiosauria .
The diverse humerus morphologies of Sauropterygia (Figure 2 A-E) partially reflect adaptations to an increasingly pelagic habitat and also different modes of locomotion, which fundamentally changed from basal Pistosauroidea to Plesiosauria [17, 22–26]. While the former mainly employed lateral undulation for propulsion, the latter reduced the tail and uniquely evolved two morphologically nearly identical pairs of flippers, which were employed in a paraxial swimming mode [see  for review].
Locomotion in Nothosauroidea clearly differed from either the more basal sauropterygians such as pachypleurosaurs and the basal pistosauroids or plesiosaurs. By reconstructing musculature and based on morphological observations of the pectoral girdle, Carroll and Gaskill , Watson , and v. Huene  hypothesized that Nothosauroidea independently evolved paraxial locomotion, where the front limbs were employed in a “rowing flight”, combining lift- and drag-based elements of propulsion, like recent sea lions , while the hind limbs were used for maneuvering.
Tetrapod long bone histology and secondary aquatic adaptation
Pachyostosis, osteosclerosis, pachyosteosclerosis, and the retention and subsequent calcification of cartilage at distance from the epiphyses are all mechanisms through which secondarily aquatic tetrapods increase their specific density to counteract the positive buoyancy caused by the lungs [28–30]. Pachyostosis, osteosclerosis, and pachyosteosclerosis, subsumed under the term bone mass increase (BMI, ), are different ways of increasing bone mass. Pachyostosis is the hyperplasy of bone deposition, leading to a swollen appearance of the bone, and osteosclerosis is the increase in inner bone compactness by an inhibition of cortical resorption and/or excessive deposition of secondary bone [29, 30]; pachyosteosclerosis is the combination of pachyostosis and osteosclerosis [29, 30]. An increase in body density seems to be typical for vertebrates living in a lagoonal or shallow water habitat, either marine or freshwater , like Sirenia  and pachypleurosaurs [e.g., [4, 22, 33].
BMI appears to be the initial step in secondary adaptation to an aquatic environment [29, 34]. Further aquatic adaptation results in the reduction in body density through an osteoporotic-like state of the skeleton (sensu [20, 34]) because a decrease in body density allows faster acceleration and increased maneuverability [30, 34]. An osteoporotic-like state is found in pelagic animals like some modern whales (e.g., [28, 30, 34, 35]), ichthyosaurs (e.g., [30, 34, 36, 37]) and some adult plesiosaurs [30, 34, 38, 39]. While the terminology suggests that the decrease in bone density is brought about by increased cortical resorption activity [30, 34], an alternative pathway to bone density reduction would be a strong increase in vascularization, leading to the periosteal bone being primarily cancellous. In either case, decrease in bone density is the terminal state in histological adaptation to a secondarily aquatic mode of life. This histological adaptation does not appear to have been modified further in any secondarily aquatic tetrapod, and there is no known case of a high-performance, pelagic swimmer reinvading shallow-water habitats.
Biological and histological ontogenetic stages
For non-mammalian fossil tetrapods, bone histology is the most reliable means of ascertaining their ontogenetic stage . The general approach is to correlate specifics of histology that change with ontogeny to life history events. In large samples covering closely related taxa, such specifics of histology and their ontogenic change can be formalized as histologic ontogenetic stages .
Life history events that are potentially reflected in bone histology are hatching or birth, sexual maturity, attainment of full size, and senescence . Biological ontogenetic stages are preceded or succeded by these events. Thus, an embryo or fetus exists before hatching or birth; a hatchling or neonate lives after birth; a juvenile lives well past hatching or birth but is not yet approaching sexual maturity; a subadult is approaching sexual maturity, which is recorded in histology by a distinctive slow-down in growth; an adult is sexually mature but not necessarily fully grown; and a senescent individual lives on after having attained final size, attainment of final size being indicated histologically by an external fundamental system (EFS).
In particular, the definition of “adult” has historically led to confusion because of the derived mammalian and avian condition in which sexual maturity coincides with full size (most mammals) or even postdates attainment of full size (birds) . However, the plesiomorphic condition for reptiles (seen in all extant non-avian reptiles) is that sexual maturity is attained well before full size , and it is most parsimonious to assume this applied to sauropterygians as well. Thus, the marked decrease in growth rate observable in medium-sized individuals is here interpreted as indicative of sexual maturity (see also [43, 44]).
History of research on sauropterygian histology and microanatomy
Already in the late 19th and early 20th century, the bone histology of sauropterygians was described and illustrated [45–50], sometimes in great detail but with a limited understanding of its meaning. In the modern studies by Enlow and Brown  and particularly Ricqlès [36, 52], the histology of various reptile taxa, including eosauropterygians, was reviewed, and questions about the function of different bone tissue types and their implications for the thermal regime and for phylogenies of extinct species were raised. Sander [33, 53] investigated longevity and life history of the pachypleurosaur Neusticosaurus by applying skeletochronology. Ricqlès , Ricqlès and Buffrénil , and Houssaye  discussed various microanatomical adaptations of secondarily aquatic tetrapods to the marine environment connected to different habitats and locomotory styles (including Eosauropterygia). Several recent studies illustrate aspects of plesiosaur bone histology [38, 55–58], but only that of Wiffen et al.  offers sufficent data to be of use in a broader comparative context. Bone histology of Pistosauridae has not previously been studied.
The most recent studies dealing extensively with stem-group sauropterygian long bone histology are that by Klein  and Hugi et al. . Klein  surveyed histological diversity of Lower Muschelkalk (Anisian) taxa. Among these, Nothosaurus species differ histologically from pachypleurosaurs (Anarosaurus) and cf. Cymatosaurus. Hugi et al.  focussed on Southern Alpine pachypleurosaurs of the genera Serpianosaurus and Neusticosaurus and found that all show lamellar zonal bone tissue (LZB) with high compactness values.
In this study, we histologically sampled an array of Nothosaurus species from the Lower Muschelkalk and from the Upper Muschelkalk to the Lower Keuper beds, Pistosaurus longaevus from the Upper Muschelkalk beds, and Plesiosaurus dolichodeirus from the Lower Jurassic of Lyme Regis, England . We found a remarkable diversity in histologies among the different Nothosaurus species, Pistosaurus, and Plesiosaurus, reflecting different biomechanical and physiological specializations. We interpret these results in terms of the evolution of locomotory styles and aquatic adaptation.
Material and methods
The material examined in this study is mainly from the Middle Triassic Upper Muschelkalk beds and the Grenzbonebed horizon (Lower Keuper) and is thus of Ladinian age (242–235 million years ago, ). Geographically it hails from various localities in southern Germany and France (Additional file 1). The Upper Muschelkalk/Grenzbonebed sample comprises complete or partial long bones, which pertain to Nothosaurus giganteus, N. mirabilis, and Pistosaurus longaevus. Nothosaurus mirabilis and N. giganteus material had been identified to species level in the collections it came from. Since there is little to no association between the name-bearing cranial material of the species of Nothosaurus and postcranial parts of the skeleton, these identifications are based on the dimensions of the bones (Additional file 1). We also sampled two small humeri and one femur that could not be assigned to species to test whether these pertain to juveniles of the larger species or to adults of a species of smaller body size such as N. juvenilis, N. edingerae, or N. jagisteus, all of which are from the Upper Muschelkalk or the Lower Keuper beds. For phylogenetic and stratigraphic comparison (Table 1), a Nothosaurus humerus from the Lower Muschelkalk of Förderstedt, south of Magdeburg, Saxony-Anhalt, Germany, was sampled. It belongs to morphotype II of Bickelmann and Sander  and can thus be assigned to Nothosaurus marchicus/N. winterswijkensis. Pistosaurus longaevus material (Figure 2, Table 1) was assigned to genus and species by morphological and histological comparison with Pistosaurus material in the collections of SMNS, and by comparison to the description of Pistosaurus by Sues . The plesiosaur specimen (Figure 2, Table 1) is a Plesiosaurus dolichodeirus femur in the SIPB collections from the Lower Jurassic of Lyme Regis, U.K., which is either Hettangian or Pliensbachian in age .
Based on principles of long bone growth , the middle region of the shaft at its narrowest part is the best region to sample long bones, because it yields the longest growth record and it corresponds approximately to the neutral zone of growth [64, 65]. Skeletochronology, i.e., study of growth marks in bone, does not only provide information on the age of an individual but also on other aspects of its life history, e.g., sexual maturity, bone growth rates, and reproduction cycles [60, 64–69]. The terminology used to describe bone histology follows Francillon-Vieillot et al. .
Both, thin sections (Figure 3, 4, 5) and polished sections (Figure 6A-D) were produced to observe eosauropterygian bone microanatomy and histology, generally by removing a thin slice of bone with a rock saw. Before sampling the bones, their proximal and distal width and length, the shaft width and length, the total or preserved length, and shaft circumference were recorded (Additional file 1). Molds of the shaft regions were produced for all complete bones, so they could be restored after sampling by filling in the gaps with plaster. The samples were processed by standard petrographic techniques into thin sections. Thin sections were studied with a Leica DM EP® compound microscope in normal transmitted and polarized light. Photomicrographs of thin sections were taken with a Leica DFC420® digital camera mounted on the compound microscope and processed with Imagic Imageaccess®.
Additionally, serial polished sections of a N. mirabilis humerus (SIPB R 54/2) and femur (SIPB R 54/1) were produced. Their preparation and terminology is based on the work of Sander [43, 70, 71]. Polished sections were studied with incident light using a Wild M5A® binocular and overview images were produced by scanning them with a desktop scanner at 1200 dpi.
Because of the great range of the size of the medullary region observed in eosauropterygians, we devised a medullary index (MI, Table 1) to quantify medullary region size. Note that only the sections in the middle of the shaft were used, where the medullary region is the smallest. MI was calculated as the percentage of the dorsoventral diameter of the bone taken up by the dorsoventral diameter of the medullary region. MI was calculated from measurements taken from overview photographs of the thin sections. All other terminology used to describe bone microanatomy and histology follows Francillon-Vieillot et al. .
At the suprageneric level, the bone microanatomy and histology of the sampled sauropterygian taxa is described in the order of the phylogenetic hypothesis of Rieppel  and Liu et al.  (Figure 1B). Specimens of the different Nothosaurus species are described in order of decreasing stratigraphic age and increasing body size, since Nothosaurus intrarelationships are insufficiently resolved  (Figure 1C) to serve as an ordering criterion. The results are summarized in Table 1 and Additional file 1 which also includes detailed information about the samples.
Nothosaurus marchicus/Nothosaurus winterswijkensisHumerus MfN R 174–2
MfN R 174–2 is a left humerus fragment of 44 mm length, lacking the distal end. The MI of this humerus is 42.5%, which indicates that the cortex is relatively thick (Figure 3A). The cortex consists of radially and longitudinally vascularized lamellar zonal bone tissue (RLLZB) and primary osteons are developed. The cortical bone shows seven growth cycles (Table 1). Beyond the third LAG, the bone tissue becomes markedly more organized. The amount of lamellar bone matrix increases, the vascularization decreases and growth marks show a closer spacing towards the bone surface.
The medullary region is separated from the cortex by a thin, highly birefringent layer of lamellar bone, which in some regions has subsequently been resorbed. Large amounts of calcified cartilage are preserved in the partially open medullary region. The calcified cartilage was slightly resorbed in parts and also partly encased by endosteal lamellar bone, forming trabeculae (Figure 7A, Figure 8G).
Nothosaurus mirabilishumerus SIPB R 54/2
SIPB R 54/2 is a complete right humerus with the total length of 200 mm (Figure 6D), though part of the shaft was restored. We prepared a thin section of the mid-diaphysis in cross section, a longitudinal section of the proximal epiphysis in an anteroposterior plane, and nine serial cross sections to study microanatomical and histological variation along the bone.
Microanatomy and histology of the mid-diaphysis
The MI of the humerus is 64%, indicating a rather thin cortex (Figure 3B), with the relatively thickest part situated posteroventrally. The cortex is composed of RLLZB. Some radial canals surrounded by “funnel structures” are scattered throughout the cortex (Figure 8A). Funnel structures is a descriptive term we use for parallel-fibered or lamellar bone surrounding vascular canals which appears sunken towards the center of the bone (see also ). Funnel structures result from the vascular canals exiting the bone in a pit. During apposition of the bone matrix, the pit grows outwards and results in a funnel shape. In parts, especially dorsally, radial vascular canals are more abundant than longitudinal canals. The primary osteons are immature to mature.
Ten growth cycles indicated by LAGs can be counted, but resorption has destroyed an unknown number of inner cycles (Table 1). The LAGs are spaced more closely beyond the sixth LAG.
The medullary region is lined with a thick layer of endosteal bone, especially on its dorsal and ventral sides. It is especially dorsally and posterodorsally filled with secondary cancellous bone, while it is mostly free anteriorly and ventrally. The secondary cancellous bone within the medullary region was formed by at least three resorption-reconstruction cycles recognizable by cross-cutting relationships (Figure 8B), but it also contains small fragments of primary cortex in the periphery. No calcified cartilage is preserved in the trabecular bone of the medullary region.
Microanatomy and histology of the proximal epiphysis
In the proximal epiphysis (Figure 6D, F), the medullary region extends almost up to the proximal articular bone surface, and it is surrounded by rare, randomly deposited, mostly endosteo-endochodral spongiosa with little calcified cartilage, which has been modified by resorption and redeposition of lamellar bone. Below the articular surface, the spongiosa merges with a thin layer of very small and fine trabeculae consisting of calcified cartilage (Figure 9A). This spongiosa seems to be capped by a very thin layer of mostly lamellar bone, which was covered by the articular cartilage in the living animal. Large vascular canals perforate the proximal end of the humerus (Figure 6F) and formerly connected the articular cartilage with the medullary region [c.f. [37, 72]].
Microanatomy and histology observed in serial polished sections
The polished sections (Figure 6E, sections 1–9) reveal changes in microanatomy from the mid-diaphysis (section 1) to the proximal head of the humerus (sections 2 to 5) and then from the mid-diaphysis to the distal articular head (sections 6 to 9). Consistent with principles of long bone growth, the cortex greatly decreases in thickness both proximally and distally, while the medullary region expands. The secondary cancellous bone of the medullary region is most dense in the mid-shaft region with little cancellous bone in the metaphyses and a slight increase in the epiphyses.
Three Nothosaurus mirabilis femora were sampled: SIPB R 54/1 is a complete femur (165 mm in total length), but parts of the shaft were restored (Figure 6A). SIPB R 50/1 is a 120 mm long fragment of a left femur, consisting of the proximal head and a large part of the shaft. SIPB R 50/2 (120 mm long) is the distal head and part of the shaft of a right femur. SIPB R 50/2 is markedly larger than the two other specimens (Additional file 1). We prepared thin sections of the mid-diaphysis in cross section of all three specimens, a longitudinal section of the proximal epiphysis of SIPB R 54/1 in a dorsoventral plane, and eight serial cross sections of SIPB R 54/1 to study microanatomical and histological variation along the bone.
Microanatomy and histology of the mid-diaphysis
The average MI of the femora is 46%, indicating a rather thick cortex (Figure 4B-C). The RLLZB of the cortex is well developed in all three femora. In SIPB R 54/1 and SIPB R 50/1, the inner cortex is more highly vascularized than the outer cortex. Primary osteons are developed to an intermediate degree. In the mid to outer region of the cortex, funnel structures are visible. Eight to nine growth cycles can be observed (Table 1) as well as several subcycles. The spatial arrangement of the LAGs is rather even, so there is no notable slowdown of growth, except possibly in SIPB R 54/1.
The open medullary region of SIPB R 50/1 is completely lined with a thin layer of two generations of endosteal lamellar bone (Figure 8C), despite the resorption cavities in the innermost cortex. In contrast, only about a third of the circumference of the medullary cavity of SIPB R 54/1 is lined with endosteal lamellar bone, the remainder having been destroyed by resorption. In SIPB R 50/2, the boundary between cortex and medullary region shows fresh resorption surfaces but no endosteal bone. A small, circular, open medullary cavity resides in the center of its medullary region. In the medullary region, secondary cancellous bone of endosteal origin is sparse to subordinate in both SIPB R 50/1 and SIPB R 54/1. In contrast, secondary cancellous bone, resulting from at least two resorption-reconstruction cycles, is prominent in SIPB R 50/2. SIPB R 50/1 and SIPB R 54/1 reveal a tendency towards osteosclerosis while the larger SIPB R 50/2 does not (Table 1).
Microanatomy and histology of the proximal epiphysis of SIPB R 54/1
The medullary region is positioned relatively anteroventrally in the proximal femoral head of N. mirabilis femur SIPB R 54/1 (Figure 6A, C), and it is surrounded by primary endochondral spongiosa. Towards the proximal articular surface, the spongiosa contains an increasing amount of calcified cartilage (compare with Omphalosaurus) (Figure 9B, C). A thin layer of calcified cartilage, visible as very small and fine trabeculae, caps the proximal end of the epiphysis.
Microanatomy and histology of serial polished sections of SIPB R 54/1
The eight serial polished sections of the N. mirabilis femur SIPB R 54/1 (Figure 6A, B) reveal variation in cortex thickness and development of trabecular bone from the midshaft region towards the proximal and distal ends. The cortex of the mid-diaphyseal section (section 1, Figure 4B) is relatively thick, and only very sparse secondary cancellous bone is observable. The cortical bone in section 2 (Figure 6B) is similarly thick, but the cross section is larger, so the medullary region appears larger, too. Sparse secondary cancellous bone is present. Bone drift, probably due to formation and shifting of the trochanters, can be seen in section 3. Towards the proximal epiphysis, cortex thickness decreases, but the amount of secondary cancellous bone increases due to remodeling resulting from bone drift. In the most proximal section (section 4, Figure 6B), the cortical bone is thin, but secondary cancellous bone and the medullary region increase greatly. The same pattern is repeated towards the distal epiphysis of the femur.
Four Nothosaurus giganteus humeri (Additional file 1) were sampled: SIPB R 45, SIPB R 53, SIPB R 40, and MHI 1903. The first two were studied from cross sections of the mid-shaft region, but SIPB R 40 was sampled in the proximal region of the shaft. MHI 1903 was studied from two consecutive partial cross sections of the proximal metaphysis and epiphysis.
Microanatomy and histology of the mid-diaphysis
The cortex of SIPB R 45, SIPB R 53, and SIPB R 40 is thin and composed of RLLZB (Figure 3C, D). Based on SIPB R 45 and SIPB R 53, the average MI of the N. giganteus humeri is 68% (Table 1). The MI of SIPB R 40 could not be reliably measured because of the proximal location of the section. The cortical bone of SIPB R 45 is more highly vascularized than that of SIPB R 40, which is in turn more highly vascularized than that of SIPB R 53. Primary osteons in SIPB R 40 are immature but mature in SIPB R 53, and funnel structures can be observed throughout the whole cortex, as in the N. mirabilis humerus (Figure 8A). The cortical bone generally becomes more highly organized towards the bone surface (Figure 7C). Both SIPB R 53 and SIPB R 45 show an external fundamental system (EFS) (Figure 7C, D, Table 1).
The medullary regions are open, although sometimes sparse secondary trabeculae of at least two resorption-reconstruction cycles was deposited randomly within the medullary cavity (Figure 3C, D). No calcified cartilage is preserved in the trabecular bone. The medullary region of SIPB R 45 is partly lined by a very thin layer of endosteal lamellar bone. In contrast, SIPB R 40 shows a thick, but discontinuous layer of circumferential endosteal bone only in some places, and SIPB R 53 shows none.
Microanatomy and histology of metaphysis and epiphysis
The proximal head and the metaphysis of humerus MHI 1903 was cut into two consecutive cross sections. Section 1 (Figure 3E) is positioned more proximal than section 2. The cortex is thin in both sections and consists of LZB. In section 1, highly vascularized zones alternate with less vascularized, thinner and more highly organized annuli, in each of which a LAG is found. The LAGs are relatively evenly spaced, indicating cyclical growth at a rather constant rate (Figure 7E). Vascular canals have sometimes a reticular orientation but more often a longitudinal one. This is similar to section 2, but its vascular canals are smaller and mainly oriented longitudinally and seldom reticular.
Towards the anterior side of section 1, the LZB grades into primary coarse cancellous bone which also shows the growth cycles that are seen in the LZB (Figure 7F). Resorption cavities are observable, especially anteriorly in the deeper cortex.
Nothosaurus giganteusfemur IPB R 49
SIPB R 49 is a complete right femur. At a total length of 230 mm, it is the largest femur sampled (Additional file 1). The MI is 76% which indicates a similarly thin cortex as described for the humeri of the same species (Figure 4A). The cortex, which consists of RLLZB, is thickest on the dorsal side, and it is poorly vascularized. The outer cortex shows mainly mature longitudinal primary osteons. LAGs are relatively evenly spaced, indicating rather constant growth rates. Seven growth cycles can be counted (Table 1), some of which show subcycles.
The medullary region contains much secondary cancellous bone with a very small open medullary cavity in the center. The bone trabeculae were formed by at least two resorption-reconstruction cycles (Figure 8B). No calcified cartilage is preserved in the trabecular bone of the medullary region.
Small Nothosaurussp. indet. humerus MHI 1906
MHI 1906 is the distal half of a small left nothosaur humerus (Additional file 1). The MI of the specimen is 35%, but because most of the original bone surface was not preserved, the MI originally must have been lower (Figure 3F). The cortical bone can be differentiated into two regions. Up to the first growth mark, the bone tissue probably consists of embryonic bone. In polarized light, this tissue stays opaque and can be identified as woven-fibered bone. We interpret the first growth mark as the neonatal line, recording hatching or birth (compare with [65, 68, 73]). Note that we do not know whether nothosaurs were oviparous or viviparous, with their sistergroup, the pachypleurosaurs, having been life-bearing . Beyond the neonatal line, the cortex is made up of RLLZB (Figure 8D). The primary osteons are very immature. Bone tissue organization increases towards the bone surface, and three growth cycles are observable (Table 1). The medullary region is only partially open and surrounded by a thin lining of endosteal bone, which is only preserved on the ventral side. Posteriorly and dorsally, it had been resorbed, and endosteal bone was deposited instead. Within the medullary region, a small amount of calcified cartilage is preserved, which was slightly resorbed in parts and partially lined with secondary endosteal bone of two generations (Figure 8D, and compare to Figure 8G). This humerus thus fits the definition of osteosclerosis (Table 1). Its histology suggests that the humerus pertains to a juvenile of a larger species.
Small Nothosaurussp. indet. humerus MHI 633
MHI 633 is the distal half of a small left nothosaur humerus (Additional file 1). The MI of this specimen is very low at 27%, so the cortical bone is thick (Figure 3G). The cortex consists of incipient fibrolamellar bone tissue (FLB), unlike all the other sampled Nothosaurus long bones. The first growth mark, in the inner region of the cortex, probably is the neonatal line. The probably embryonic bone consists of woven-fibered bone tissue (Figure 8E). Beyond the neonatal line, there is a woven-fibered bone matrix surrounding immature primary osteons (Figure 8E), hence the notion of “incipient FLB”. Three growth cycles could be counted (Table 1). There is no outward increase in bone tissue organization. Based on Amprino’s Rule (e.g., [75, 76]), this bone grew at a relatively high and rather constant rate. The cortex is well vascularized with radial canals, much more so than in the other Nothosaurus long bones. Cell lacunae in the incipient FLB are rounded and plump and show no preferred orientation. The radial vascular canals pierce the bone surface, creating a pitted surface.
The cortex is set off abruptly and irregularly from an open medullary cavity (compare to , plate 1, Figure 3). The inner margin of the cortex lacks any evidence of resorption, and there is no endosteal bone lining the medullary region. The thin cementing line between medullary region and cortex, as seen in MHI 1906 and MfN R 174–2, cannot be observed. No calcified cartilage is preserved. This microanatomy and histology is unique among the sampled Nothosaurus long bones and is most consistent with an early juvenile stage of the specimen, before perimedullary resorption and calcification of cartilage set in. The open medullary cavity may have been filled with uncalcified cartilage that was completely removed during decay and fossilization.
Because humerus MHI 633 experienced no perimedullary resorption activity, it would seem to follow the pathway to osteosclerosis [29, 30, 34]. However, we refrain from applying this term to the specimen because of its very immature nature and the strong vascularization. Without quantification of bone compactness and porosity (which is beyond the scope of this study), it is uncertain whether MHI 633 does indeed shows bone mass increase relative to the terrestrial condition or whether the strong vascularization compensates for the apparent gain in bone mass caused by the absence of perimedullary resorption activity.
Small Nothosaurussp. indet. femur SMNS 84856
SMNS 84856 is an incomplete right femur (Additional file 1). The MI of the specimen is 28%, indicating a thick cortex (Figure 4D) which is composed of RLLZB. Primary osteons are developed to an intermediate degree, and funnel structures are present (Figure 8A). In the outer periphery of the cross section, ten growth cycles can be counted (Table 1). The spacing of the LAGs (Figure 8F) becomes narrower towards the outer bone surface, and the organization of the bone tissue increases (Table 1). The medullary region is almost completely filled with secondary endosteal bone of two generations. SMNS 84856 thus exhibits osteosclerosis (Table 1).
One complete (SIPB R 46) and one incomplete humerus (SMNS 84825) of Pistosaurus were sampled, with the former representing a smaller individual than the latter (Additional file 1). The MI is extremely low at around 6% (Figure 5A-B), indicating a very small medullary region. The very thick cortex is composed of a woven bone matrix with radial vascular canals that are filled in by centripetal deposition of lamellar bone (Figure 10A-G). These structures thus represent primary osteons, and the tissue is FLB. The FLB is cyclically interrupted by growth marks. While the cortical bone of Pistosaurus is quite comparable to that of dinosaurs and large mammals [e.g., [41, 64]], it differs in that the primary osteons are mainly radially oriented. Pistosaurus humeri are markedly higher vascularized than nothosaur long bones. Primary osteons of SIPB R 46 (Figure 10A, C) are rather immature in comparison to SMNS 84825 (Figure 10B, D). Secondary osteons are absent in Pistosaurus humeri.
Because of the very small medullary region, it is clear that the first growth mark (Figure 10C, D) must represent the neonatal line in both specimens. The embryonic bone is moderately vascularized woven-fibered bone. In both specimens, growth marks consisting of an annulus with an indistinct LAG are spaced closer together with increasing body size, and finally, in the outermost periphery of the cortex, thick avascular parallel-fibered annuli alternate with zones of FLB with longitudinal and very short radial vascular canals (Figure 10A, B). This indicates that diaphyseal growth slowed down in the fourth to fifth growth cycle. Five growth cycles (Table 1) were counted in the small specimen and seven in the larger specimen.
The medullary region is open and lined by endosteal lamellar bone in SMNS 84825, but in SIPB R 46 it is filled and contains very sparse remnants of calcified cartilage incorporated into endosteal bone. The very small medullary cavity of the Pistosaurus humeri obviously results from a suppressed perimedullary resorption activity, which is one of the conditions leading to osteosclerosis. However, as in the case of MHI 633, and based on the same arguments, we refrain from employing the term osteosclerosis in the case of Pistosaurus. This is because the decrease in resorption activity may have been compensated for by the increase in vascularity in the FLB of the cortex.
Pistosaurus longaevusfemur SIPB R 74
SIPB R 74 is an incomplete Pistosaurus femur (Additional file 1). At 66%, the MI of the femur is much higher than that of the humeri of Pistosaurus (Figure 5C). The femoral cortex is mostly made up of poorly vascularized RLLZB (Figure 11A, B) instead of the FLB of the humeri. Only in the deep regions of the femoral cortex, sparse woven-fibered bone matrix can be observed. Superficially, the cortical bone shows mainly funnel structures. In the deeper region, mature longitudinally oriented primary osteons are found. Eight growth cycles (Table 1) and several subcycles can be observed. The LAGs in the LZB part of the cortex are relatively evenly spaced. The increase in bone tissue organization, from FLB to LZB, records a slowdown in growth. In the center of the medullary region, there is a small medullary cavity surrounded by secondary cancellous bone of at least two generations of endosteal lamellar bone and of interstitial primary cortex.
One side of the cross section (we do not know which, because we are unable to orient the Pistosaurus femora in dorsoventral direction, see above), records a peculiar growth spurt in the outer cortex (Figure 11A, B). Radially vascularized FLB is partially filled in with lamellar bone matrix. The deposit shows four subcycles. Each of them ends in a thin layer of lamellar bone. Laterally in the section, the first three subcycles merge into the seventh growth cycle and the fourth subcycle and the eighth growth cycle converge. In the eighth growth cycle, the individual had died.
Similar observations of radially vascularized FLB in the outer cortex and recording local growth spurts have also been reported by Erickson and Tumanova  and Klein and Sander  for Psittacosaurus and Plateosaurus, respectively. In the Pistosaurus femur, this bone tissue is deposited onto LZB, whereas in Psittacosaurus and Plateosaurus, it is deposited onto FLB with laminar vascularization. Growth of radially vascularized FLB is associated with a rapid change of morphology, possibly due to a fast ontogenetic relocation of muscle insertion areas [71, 78]. The presence of some Sharpey’s fibers in radially vascularized FLB bone of the Pistosaurus femur is consistent with the muscle insertion hypothesis.
Plesiosaurus dolichodeirusfemur IPB R 90
IPB R 90 is a plesiosaur femur 150 mm long (Additional file 1). The MI is about 35% (Figure 5D). However, the cross section appears relatively spongy (typical for secondarily marine tetrapods (compare with, e.g., [38, 64]), and the transition from the medullary region to the cortex is very gradual (Figure 5D). Unlike in all previously discussed specimens, the cortex is subject to intensive Haversian remodeling, with only limited areas of primary cortex remaining. These are located beneath the bone surface and interstitially between the secondary osteons. The primary cortex consists of well vascularized FLB. The primary osteons show a preferred radial orientation, but are not strictly radial (Figure 11C). In this way they differ from the radial vascularization in Pistosaurus and Nothosaurus. The primary osteons are unusual and differ from those of Pistosaurus and typical FLB in that the centripetal infill of the vascular canals does not only consist of lamellar bone but also of parallel-fibered bone (Figure 11D). The outer periphery of the cortex shows closely spaced growth marks forming an EFS (Figure 11C).
Locally, there are at least three generations of secondary osteons as indicated by cross-cutting relationships. The cementing lines that separate the osteons from the primary cortical bone and from each other are undulating and irregular (Figure 11C, D). Although most secondary osteons are oriented longitudinally, resorption activity leading to the first generation of secondary osteons appears to have been controlled by the radial fabric of the primary bone. This leads to an arrangement of the secondary osteons in radial rows (Figure 11D). Towards the anterior and posterior side, secondary osteons appear elliptical, indicating an oblique orientation. Their longer axes point towards the medullary region and towards either the anterior or the posterior side. This leads to the overall impression that the cortex is rather radially vascularized. In the medullary region, there is secondary cancellous bone produced by intensive remodeling. The Plesiosaurus femur appears to be osteoporotic in some regions of the cortex but not in all. Osteoporosis is not as prevalent as shown by e.g., Wiffen et al.  and Buffrénil and Mazin  for other plesiosaurs but the more remodeled the cortex is, the more vascularized it becomes.
Quantitative comparison of medullary region size in Eosauropterygia
As noted, long bones of Nothosaurus, Pistosaurus, and Plesiosaurus show great variation in relative size of their medullary region. In particular, two Upper Muschelkalk nothosaur species of large body size, N. giganteus and N. mirabilis, greatly decrease cortical thickness by increasing medullary space especially in their humeri. Three clusters of relative medullary region size can be differentiated based on MI (Figure 12A). The first represents the humeri of Pistosaurus with their extremly low MI (less than 10%). The second group consists of the long bones of Nothosaurus sp. indet., the two smaller femora of N. mirabilis (SIPB R 50/1 and SIPB R 54/1), the N. marchicus/N. winterswijkensis humerus, and the Lower Jurassic Plesiosaurus dolichodeirus femur, all of which have intermediate MIs ranging from approximately 25% and 45% (Figure 12A). The third group comprises all long bones of N. giganteus, the humerus and the large femur of N. mirabilis (SIPB R 50/2), and the femur of Pistosaurus, which have very high MIs ranging from 58% to 77% (Figure 12A). A plot of MI against minimal shaft circumference (MSC), as a proxy of body size (Figure 12A), shows a week trend of increasing MI with increasing MSC.
Biomechanical implications of Nothosaurusmicroanantomy
Our histological study of Nothosaurus long bones shows that biomechanical adaptations evolved within the genus during the Middle Triassic and that the changes are correlated with increasing body size . The plesiomorphic state is seen in N. marchicus/N. winterswijkensis (MfN R 174–2) from the Anisian (Lower Muschelkalk) as well as the small femora (SIPB R 54/1 and SIPB R 50/1) of N. mirabilis and the humerus and femur of Nothosaurus sp. indet. (MHI 1906 and SMNS 84856) from the Upper Muschelkalk (Ladinian). These bones show lamellar zonal bone tissue with mainly longitudinal vascular canals and differing degrees of cortical thickening (Figure 12) and bone mass increase (i.e., limited endosteal resorption, incomplete endochondral ossification resulting in calcified cartilage, or dense secondary tissue in the medullary region) (Table 1). Character polarity is known from work on pachypleurosaur bone histology [53, 59, 60].
The derived state is represented by the humeri of large-bodied Upper Muschelkalk species of Ladinian age, namely Nothosaurus giganteus and N. mirabilis and the femur of N. giganteus. These share a very thin cortex and an unusually large medullary cavity (MI approx. 60 to 80%, Figure 12) with few trabeculae, resulting in greatly decreased skeletal density. This suggests that Nothosaurus evolution saw a shift in lifestyle and habitat. While the small-bodied basal nothosaur species from the Lower Muschelkalk adapated to shallow water by an increase in bone mass, the large-bodied and derived species from the Upper Muschelkalk moved into the open marine environment and became more active swimmers, for which bone mass decrease was adaptive. The small-bodied species from the Upper Muschelkalk retained the ancestral condition of living in shallow water. Among the large-bodied Upper Muschelkalk species these evolutionary changes seem to have been recapitulated in their ontogeny (see below).
The histological specialization of achieving low skeletal density by extreme resorption of the cortex, described here for the two large-bodied Upper Muschelkalk Nothosaurus species, is unique among secondarily aquatic tetrapods and has not been described before. While low density of skeletal elements evolved convergently several times in secondarily aquatic tetrapods and represents the terminal adaptation to the aquatic environment [e.g., 28, 29, 30, 34], in all the other instances bone mass decrease evolved by the transformation of compact bone to cancellous as seen in, e.g., extant whales  and ichthyosaurs . However, their cortex consists of FLB instead of LZB. Since there is no recent analog for the large-bodied Nothosaurus microanatomy, it is unclear what kind of soft tissue filled their large medullary cavity. A likely candidate is fatty yellow bone marrow which would have decreased the density of these bones compared to a fill of red bone marrow in the juveniles.
Bone morphology and microanatomy are fundamentally influenced by mechanical factors. According to Wolff’s law, bone will be resorbed if loading decreases . Thus, if bone density and the amount of bone tissue remain constant but the diaphyseal diameter increases, the bone wall becomes thinner and at the same time the bone will become adapted to resist higher torsional loads (e.g., ). The large, triangular cross section of Nothosaurus humeri (not seen in any other sauropterygians) and the shape of the bone wall provided a mechanically strong construction despite the thinness of the cortex. This peculiar bone microanatomical specialization would have been able to withstand high mechanical loads despite low skeletal mass.
This suggests that the forelimb played an important role in the locomotion of N. giganteus and N. mirabilis, a view that is also supported by the complex morphology of the nothosaur humerus [22, 62] and nothosaur muscle reconstructions [25, 26]. We hypothesize that this adaptation to high bending loads indicates either underwater flight, as employed by sea turtles  and penguins [83, 84], or the so-called “rowing flight” employed by sea lions . In addition, the generally lower density of skeletal elements in the two large-bodied Upper Muschelkalk Nothosaurus species suggests that these nothosaurs were able to swim faster and more energy-efficient than the smaller Nothosaurus species.
The distinct differences in bone microanatomy and histology of long bone shafts between large-bodied Nothosaurus and similar-sized Plesiosauria indicate that lightening of the skeleton evolved convergently in the two lineages. The pressing question though is, why lightening of the skeleton in Nothosaurus evolved along such a different pathway compared to all the other secondarily aquatic and pelagic tetrapod clades i.e., some adult Plesiosauria, Ichthyosauria, Mosasauridae, some Chelonioidea, and Cetacea. These groups all convergently evolved the same solution, highly cancellous bone and a reduction of the cortex, but at different times in geologic history . Possibly, the evolutionary pathway to completely cancellous bone is linked to a high basal metabolic rate and endothermy, which obviously preceeded the aquatic adaptation in cetaceans, but may have evolved concurrently in ichthyosaurs, plesiosaurs and possibly in mosasaurs . Today’s Chelonioidea with the exception of Dermochelys seem to pose an exception to this hypothesis because they are ectothermic but have spongy long bone shafts. Bone microstructure in Dermochelys is consistent with our hypothesis because of its increased basal metabolic rate, which is three times that of a typical reptile [86, 87].
Ontogenetic implications of Nothosaurushistology and microanatomy
Assigning individuals to biological ontogenetic stages
The questions arise whether the observed microanatomical and histological differences between individuals and taxa may be due to different ontogenetic stages and whether these differences can be used to determine the biological ontogenetic stage of eosauropterygian specimens. We suggest that counting growth marks (Table 1) and describing and interpreting bone tissue types (Table 1) do indeed permit identifying the individuals as juvenile, subadult, adult, and fully grown.
Although we do not know what the growth curves of either Nothosaurus, Pistosaurus, or Plesiosaurus look like, it seems to be reasonable to presume that they followed the general plesiomorphic reptilian pattern of growth, including the timing of sexual maturity (see discussion in the Background section). With the onset of sexual maturity, resource allocation shifts from gaining size to reproduction, which in turn is reflected by the closer spacing of growth marks [40, 42]. Accordingly, we identified individuals with very few LAGs and highly vascularized bone tissue as juveniles. Individuals with several regularly spaced LAGs, decrease in vascularization, and increase in bone tissue organization were interpreted as subadults, approaching sexual maturity. Individuals that record a sudden decrease in growth rate, e.g., by a sudden decrease in LAG spacing, were interpreted as adults (though not fully grown). Finally, individuals that show a cessation of growth (EFS) were termed fully grown. There were no obviously senescent individuals in this study.
The qualitative and quantitative record of growth in Nothosaurus long bones
The two small humeri MHI 633 and MHI 1906 come from juvenile individuals because only two LAGs (neonatal line + one LAG) are present. Since the two specimens are both of roughly the same size, but also of roughly the same stratigraphic age and coeval with the larger-bodied Nothosaurus species, we hypothesized that the earlier juvenile (MHI 633) belongs to the very large N. giganteus and the later juvenile (MHI 1906) belongs to the large N. mirabilis. According to the criteria introduced above, the femora SIPB R 49, SIPB R 50/1, and SIPB R 50/2 had not reached sexual maturity yet and are therefore identified as subadults. The humeri MfN R 174–2 (from the Lower Muschelkalk), SIPB R 40, and SIPB R 54/2, the femur SMNS 84856 and possibly also the femur SIPB R 54/1 record a slowdown in growth rate, suggesting sexual maturity [53, 65, 68]. Hence, the specimens were assigned to the “adult” category. Notably, SMNS 84856 is the smallest femur in the sample but on the basis of its bone histology also one of the most mature. The humeri SIPB R 45 and SIPB R 53 are interpreted as fully-grown specimens because bone growth has almost ceased as recorded by the deposition of an EFS.
The highest number of LAGs (10) was counted in SIPB R 54/2 and SMNS 84856. However, because the former shows perimedullary resorption and neither of them shows an EFS, we estimate a time frame of 15 to 20 years for the larger nothosaur species (N. mirabilis, N. giganteus, Nothosaurus sp. indet.) before growth stopped, taking several resorbed growth marks and several growth marks yet to be deposited into account.
The juvenile Nothosaurus humeri and their evolutionary implications
The hypothesis that MHI 633 and MHI 1906 are juveniles of two species of Nothosaurus that differ in adult size, i.e., N. mirabilis and N. giganteus, has implications for body size evolution in Nothosaurus via heterochrony. The cortex of the juvenile N. mirabilis (MHI 1906) is composed of LZB and that of the juvenile N. giganteus (MHI 633) of FLB. Thus MHI 633 grew faster than MHI 1906 in the same amount of time, because general bone apposition rate is higher for FLB than for LZB. The large body size of N. giganteus evolved due to an acceleration of growth during early ontogeny (MHI 633, FLB), allowing N. giganteus to attain a larger body size than basal nothosaurs from the Lower Muschelkalk, but in the same time. After the juvenile stage, N. giganteus growth slowed down and LZB was laid down.
The relatively large body size of N. mirabilis may also have been reached by acceleration. Compared to a more basal Lower Muschelkalk Nothosaurus species such as N. marchicus/N. winterswijkensis, N. mirabilis may have grown faster in its first few years, laying down the highly vascularized LZB with a high amount of parallel-fibered bone matrix seen in MHI 1906.
The juvenile N. mirabilis and N. giganteus specimens have a comparably thick cortex (MI 25-35%) while the large humeri assigned to these two species have a thin cortex (MI of 58% and 77%). This suggests that there was an ontogenetic shift in lifestyle and habitat in these two species. While the juveniles may have lived closer to shore and were bottom-dwelling, the adults shifted to a more pelagic lifestyle in the water column. Such a shift has previously been suggested by Wiffen et al.  for plesiosaurs from the Upper Cretaceous of New Zealand and by Katsura  for champsosaurs from the Late Cretaceous of Montana, USA.
Ontogenetic implications of Pistosaurus and Plesiosaurushistology
Histology suggests that no juvenile individuals of these two taxa were sampled. In the Pistosaurus femur SIPB R 74, the eight growth marks are spaced evenly, and no sudden decrease of vascularization can be recognized. However, there is an outward change in bone tissue from FLB to LZB, so the individual was subadult or adult, but not fully grown. The uncertainty stems from the fact that the specimen is not part of a growth series. The humeri SMNS 84825 and SIPB R 46 must have belonged to adult individuals because they had reached sexual maturity as suggested by the slow-down in growth in the fourth to fifth cycle. In terms of age at death, the Pistosaurus samples suggest similar ages as those recorded by the Nothosaurus mirabilis samples.
The EFS in the femur of Plesiosaurus indicates that the individual was fully grown. At least ten growth cycles can be counted, including those of the EFS, but most of the earlier growth mark record was destroyed by intense cortical remodeling.
As in Nothosaurus, the humerus of Pistosaurus shows a more derived histology (FLB over LZB) than the femur. However, the humerus exhibits reduced perimedullary resorption activity while the femur reveals a rather similar MI to the larger of the two N. mirabilis femora (SIPB R 50/2). These differences suggest that humerus and femur also differed in their function. It also underscores the notion that postcranial skeletal adaptations to a secondarily aquatic lifestyle first happened in the forelimb of stem-group sauropterygians, particularly in the humeri, and were linked to the evolution of different modes of locomotion [22–26] and/or sexual dimorphism and different morphotypes [33, 59, 62, 74, 89].
Fibrolamellar bone in Pistosaurusand the evolution of the Plesiosauria
The most surprising result of this study was the fundamental differences between the microanatomy and histology of Pistosaurus long bones, particularly the humerus, and those of Nothosaurus (as already briefly announced by ). The highly vascularized and nearly continuously deposited FLB of the Pistosaurus humerus suggests high growth rates. FLB also suggests endothermy (e.g., [36, 52, 77, 90, 91]) because fast growth requires a high basal metabolic rate. This implies that the high basal metabolic rate of plesiosaurs  arose in the last common ancestor of Plesiosauria and Pistosauridae, although an earlier origin among basal Pistosauroidea is possible .
We also found abundant FLB in Plesiosaurus dolichodeirus. Unlike in Pistosaurus, the primary cortex of Plesiosaurus was subject to extensive Haversian remodeling. A bone tissue consisting of woven-fibered bone but apparently lacking primary osteons was described in plesiosaurs from the Upper Cretaceous . These specimens also show intense Haversian remodeling. Thus, our Plesiosaurus sample moves the record of fast growing woven-fibered bone tissue (as a component of FLB) in the plesiosaur lineage back to at least the Lower Jurassic. Our Pistosaurus samples show that this tissue had already evolved in sauropterygians by the Middle Triassic, at least 30 million years before the plesiosaur radiation. In fact, some Lower Muschelkalk (Anisian) sauropterygian long bones that may belong to the basal pistosauroid Cymatosaurus or a closely related taxon also show some FLB, albeit in a zonal pattern alternating with LZB .
To understand the origin of FLB and high growth rates in Eosauropterygia, their sistergroup, the Placodontia needs to be considered. As for plesiosaurs, placodont bone histology remains little studied, although there is evidence that placodonts also had fast-growing bone tissue [59, 92]. Thus, at least intermittent deposition of FLB is present in at least three different lineages of early Sauropterygia (Placodontia, Pistosauroidea and in the pachypleurosaur Anarosaurus heterodontus) . Our observation of uninterrupted FLB in a juvenile of a large-bodied nothosaur, presumably N. giganteus, indicates that all sauropterygians were able to lay down this bone tissue at least during early stages of their life history, but only in the Pistosauria, sustained deposition of FLB appears to have evolved.
Until recently, Pistosaurus was the only representative of the Pistosauridae, and its occurrence was restricted to rare finds from the Upper Muschelkalk beds (Middle Triassic). However, finds from the Middle Triassic of Nevada (Augustasaurus; [12, 18]) and of China  indicate that the Pistosauridae had already spread over the entire northern hemisphere by the Middle Triassic. This suggests the ability of pelagic dispersal, which may have included a certain cold-water tolerance [19, 59]. Nothosauroidea, in contrast, remained restricted to the warm waters of the Tethys and surrounding epicontinental seas throughout their evolutionary history and went extinct at the end of the Middle Triassic.
Recently, Klein  hypothesized that it was the evolution of a high basal metabolic rate in the most basal Pistosauria such as Cymatosaurus and Anarosaurus that permitted the plesiosaur lineage to achieve a pelagic lifestyle already during the Middle Triassic and to survive into the Jurassic. However, here we refine this hypothesis by noting that another prerequisite for a pelagic lifestyle is a substantial increase in body size from the generally small (<1 m total length) basal pistosauroids to the larger Pistosauria (> 2 m total length). This is based on the observation that all pelagic marine mammals of today are in the size range of Pistosauridae and Plesiosauria and that there are no open-ocean marine mammals the size of Cymatosaurus, let alone Anarosaurus. The ability to grow quickly as recorded by FLB may have been the prerequsite to large body size.
Together, large body size, high growth rates and presumably high basal metabolic rates having been present in Pistosauridae suggest that at least some Plesiosauria also possessed these features, which is indeed the case . We hypothesize that these features were the key to the evolutionary success of the Plesiosauria to become the most successful and long-lived radiation of marine reptiles [15, see also 59]. Large body size, high growth rates and presumably high basal metabolic rates must have facilitated the pelagic lifestyle of adult plesiosaurs (the juveniles apparently having inhabited coastal waters ) and rapid spread of plesiosaurs around the globe since the Early Jurassic.
This hypothesis raises the issue of the lack of a Triassic record of the Plesiosauria because Plesiosauria are separated from Pistosauridae by a 30 million years ghost lineage . There are two possible, not mutually exclusive, explanations: Triassic Plesiosauria may have inhabited the Southern Hemisphere and only spread to the Northern Hemisphere in the Jurassic, or the remains of Triassic Plesiosauria have not been discovered yet because of the paucity of Late Triassic marine reptile faunas. The latter view is supported by the extremely long duration of the Norian stage of about 25 million years, which only recently has been recognized (e.g., ). This makes it by far the longest stage of the entire Phanerozoic, but considerably fewer marine reptile Lagerstätten are known from the Norian than from the much shorter Middle Triassic stages.
Support for our hypothesis is also found in the paleobiogeography of Pistosauroidea. Corosaurus from the early Middle Triassic of Wyoming, USA [19–21] is a basal pistosauroid. Its presence on the western shelf of North America indicates that Pistosauroidea were already able to disperse across the Northern Hemisphere at this early time, unlike all other sauropterygian clades which remained restricted to the Tethys. If basal pistosauroids were already characterized by a high basal metabolic rate, this would indicate a general evolutionary pattern in the secondary adaptation to the marine environment where changes in physiology predate morphological adaptations to a pelagic lifestyle.
Our results support the hypothesis of Motani  and Bernard et al.  that a high basal metabolic rate and at least incipient endothermy is the prerequisite for the spread of a secondarily aquatic lineage across the globe. This applied even during the Mesozoic with its generally higher sea surface temperatures. Lineages that were not able to evolve a constant high basal metabolic rate remained restricted to the warm shallow seas, the Nothosauroidea studied by us being a case in point. The pattern of extinction at the end of the Middle Triassic, with Nothosauroidea disappearing from the fossil record, but Placodontia and Pistosauria surviving, may also be explained by the differences in thermophysiology as revealed by bone histology. Lineages with high basal metabolic rates may have been less affected by global sea level and temperature changes because of their ability to inhabit cooler waters and the open ocean.
We studied the long bone microanatomy and histology of the stem-group sauropterygians Nothosaurus spp. and Pistosaurus longaevus from the Muschelkalk (Middle Triassic) and of the Early Jurassic plesiosaur Plesiosaurus dolichodeirus. Nothosaurus long bones generally consist of RLLZB. However, at least one juvenile nothosaur individual grew with continuously deposited FLB (MHI 633). The Lower Muschelkalk N. marchicus/N. winterswijkensis humerus, a small Upper Muschelkalk Nothosaurus sp. indet. humerus, and Nothosaurus femora all show a thick cortex (MI around 30%) of LZB, consistent with previous studies .
Humeri of adult Upper Muschelkalk N. giganteus and N. mirabilis show an exceptional histological pattern: a very thin cortex (MI around 70%) and a much enlarged medullary region (Figure 3). The thin bone walls combined with the increased diameter of the triangular diaphyseal cross section were well suited to resist bending loads. This suggests that in the two large-bodied Nothosaurus species the forelimbs played an important role in locomotion. Nothosauroidea may have evolved towards an increasingly pelagic lifestyle convergently to Pistosauria, not owing to a higher basal metabolic rate, but due to their newly achieved biomechnical adaptations, involving a lightening of the skeleton and some kind of limb-based propulsion.
In contrast to Nothosaurus, the Pistosaurus humeri show a cortex entirely formed by FLB with mainly radial vascular canals and have a very small marrow cavity. Pistosaurus histology thus reflects high growth rates but gives no indication that the forelimb was important in propulsion, unlike in the later plesiosaurs. The femur of Plesiosaurus dolichodeirus from the Lower Jurassic of Lyme Regis, UK, also consists of FLB. However, unlike any of the Triassic sauropterygians, it was intensively remodeled (compare with ).
FLB, and by extension high growth rates and high basal metabolic rates, had already evolved among stem-group Sauropterygia by Ladinian times in the Pistosauria or even earlier . The invasion of the pelagic realm by the Pistosauroidea already in the Middle Triassic correlates with a substantial increase in body size, presumably facilitated by the increased metabolic rate that had evolved in earlier Pistosauroidea and was retained in the later Pistosauria (Pistosauridae and Plesiosauria). A high basal metabolic rate may have been a prerequisite for the pelagic life style of Pistosauridae and Plesiosauria by keeping the body warm in cold waters, providing endurance and making a sufficiently large body size possible.
Steinmann-Institut für Geologie, Mineralogie und Paläontologie, Universität Bonn, Germany
Museum für Naturkunde – Leibniz-Institut für Evolutions- und Biodiversitätsforschung an der Humboldt-Universität zu Berlin, Berlin, Germany
Muschelkalkmuseum Hagdorn, Ingelfingen, Germany
Staatliches Museum für Naturkunde Stuttgart, Stuttgart, Germany.
Benson RBJ, Evans M, Druckenmiller PS: High diversity, low disparity and small body size in plesiosaurs (Reptilia, Sauropterygia) from the Triassic-Jurassic boundary. PLoS One. 2012, 7: 1-15.
Meyer H, der Vorwelt Zur Fauna: Die Saurier des Muschelkalkes mit Rücksicht auf die Saurier aus buntem Sandstein und Keuper. 1847-1855, Frankfurt am Main: Heinrich Keller
Rieppel O: Osteology of Simosaurus gaillardoti, and the phylogenetic interrelationships of stem-group Sauropterygia. Field Geol, N S. 1994, 28: 1-85.
Rieppel O: Sauropterygia I. In Encyclopedia of Paleoherpethology. Edited by: Kuhn PWO. 2000, München: Verlag Dr. Friedrich Pfeil, 1-134.
Liu J, Rieppel O, Jiang D-Y, Aitchison JC, Motani R, Zhang Q-Y, Zhou C-Y, Sun Y-Y: A new pachypleurosaur (Reptilia: Sauropterygia) from the lower Middle Triassic of southwestern China and the phylogenetic relationships of Chinese pachypleurosaurs. J Vert Paleont. 2011, 31: 292-302. 10.1080/02724634.2011.550363.
Holmes R, Cheng Y-N, Wu X-C: New information on the skull of Keichosaurus hui (Reptilia: Sauropterygia) with comments on sauropterygian interrelationships. J Vert Paleont. 2008, 28: 76-84. 10.1671/0272-4634(2008)28[76:NIOTSO]2.0.CO;2.
von Huene FR: Pistosaurus, a Middle Triassic plesiosaur. Am J Sci. 1948, 246: 46-52. 10.2475/ajs.246.1.46.
Sues HD: Postcranial skeleton of Pistosaurus and interrelationships of the Sauropterygia (Diapsida). Zool J Lin Soc London. 1987, 90: 109-131. 10.1111/j.1096-3642.1987.tb01351.x.
Benton MJ, Spencer PS: Fossil Reptiles of Great Britain. Geological Conservation Review Series. 1995, London: Chapman & Hall, 1-386. 10
Albers PCH, Rieppel O: A new species of the sauropterygian genus Nothosaurus from the Lower Muschelkalk of Winterswijk, the Netherlands. J Paleont. 2003, 77: 738-744. 10.1666/0022-3360(2003)077<0738:ANSOTS>2.0.CO;2.
Sato T, Cheng Y-N, Wu X-C, Li C: Osteology of Yunguisaurus (Reptilia; Sauropterygia), a Triassic pistosauroid from China. Paleont Res. 2010, 14: 179-195. 10.2517/1342-8144-14.3.179.
Sander PM, Rieppel OC, Bucher H: A new pistosauroid (Reptilia: Sauropterygia) from the Middle Triassic of Nevada and its implications for the origin of the plesiosaurs. J Vert Paleont. 1997, 17: 526-533. 10.1080/02724634.1997.10010999.
Rieppel O: Sauropterygia from the Muschelkalk of Djebel Rehach, southern Tunisia. N Jb Geol Paläont. 1997, 9: 517-530.
Rieppel O, Mazin J-M, Tchernov E: Speciation along rifting continental margins: a new nothosaur from the Negev (Israel). C R Acad Sci. 1997, 325: 991-997.
Motani R: The evolution of marine reptiles. Evo Edu Outreach. 2009, 2: 224-235. 10.1007/s12052-009-0139-y.
Klein N, Albers PCH: A new species of the sauropsid Nothosaurus from the Lower Muschelkalk of the western Germanic Basin, Winterswijk, The Netherlands. Acta Palaeont Pol. 2009, 54: 589-598. 10.4202/app.2008.0083.
Hagdorn H, Rieppel O: Stratigraphy of marine reptiles in the Triassic of Central Europe. Zb Geol Paläont. 1999, 1: 651-678.
Rieppel O, Sander PM, Storrs GW: The skull of the pistosaur Augustasaurus from the Middle Triassic of northwestern Nevada. J Vert Paleont. 2002, 22: 577-592. 10.1671/0272-4634(2002)022[0577:TSOTPA]2.0.CO;2.
Rieppel O: Phylogeny and paleobiogeography of Triassic Sauropterygia: problems solved and unresolved. Palaeogeogr Palaeoclim Palaeoecol. 1999, 153: 1-15. 10.1016/S0031-0182(99)00067-X.
Rieppel O: Corosaurus alcovensis Case and the phylogenetic interrelationships of Triassic stem-group Sauropterygia. Zool J Lin Soc London. 1998, 124: 1-41. 10.1111/j.1096-3642.1998.tb00568.x.
Storrs GW: Anatomy and relationships of Corosaurus alcovensis (Diapsida, Sauropterygia) and the Triassic Alcova Limestone of Wyoming. Bull Peabody Mus Nat Hist Yale Univ. 1991, 44: 1-155.
Carroll RL, Gaskill P: The nothosaur Pachypleurosaurus and the origin of plesiosaurs. Phil Trans R Soc London B. 1985, 331: 131-393.
Storrs GW: Function and phylogeny in sauropterygian (Diapsida) evolution. Am J Sci. 1993, 293: 63-90. 10.2475/ajs.293.A.63.
Carpenter K, Sanders F, Reed J, Larson P: Plesiosaur swimming as interpreted from skeletal analysis and experimental results. Trans Kansas Acad Sci. 2010, 113: 1-34. 10.1660/062.113.0201.
Watson DMS: The elasmosaurid shoulder-girdle and fore-limb. Proc Zool Soc London. 1924, 24: 885-917.
von Huene FR: Ein beachtenswerter Humerus aus unterstem Muschekalk und seine Bedeutung. N Jb Geol Min Paläont Mh B. 1944, 1944: 223-227.
Feldkamp SD: Foreflipper propulsion in the California sea lion, Zalophus californianus. J Zool. 1987, 212: 43-57. 10.1111/j.1469-7998.1987.tb05113.x.
Gray N-M, Kainec K, Madar S, Tomko L, Wolfe S: Sink or swim? Bone density as a mechanism for buoyancy control in early cetaceans. Anat Rec. 2007, 290: 638-653. 10.1002/ar.20533.
de Buffrénil V, Canoville A, D’Anastasio R, Domning DP: Evolution of sirenian pachyosteosclerosis, a model-case for the study of bone structure in aquatic tetrapods. J Mammal Evol. 2010, 17: 101-120. 10.1007/s10914-010-9130-1.
Houssaye A: Bone histology of aquatic reptiles: what does it tell us about secondary adaptation to an aquatic life?. Biol J Lin Soc. 2013, 108: 3-21. 10.1111/j.1095-8312.2012.02002.x.
Canoville A, Laurin M: Evolution of humeral microanatomy and lifestyle in amniotes, and some comments on paleobiological inferences. Biol J Lin Soc. 2010, 100: 384-406. 10.1111/j.1095-8312.2010.01431.x.
de Buffrénil V, Schoevaert D: Donnés quantitatives et observations histologiques sur la pachyostose du squelette du dugong, Dugong dugon (Müller) (Sirenia, Dugongidae). Can J Zool. 1989, 67: 2107-2119. 10.1139/z89-300.
Sander PM: The pachypleurosaurids (Reptilia: Nothosauria) from the Middle Triassic of Monte San Giorgio, (Switzerland), with the description of a new species. Phil Trans R Soc London B. 1989, 325: 561-670. 10.1098/rstb.1989.0103.
de Ricqlès A, de Buffrénil V: Bone histology, heterochronies and the return of tetrapods to life in water: where are we?. In Secondary Adaptation of Tetrapods to Life in Water. Edited by: Mazin J-M, de Buffrénil V. 2001, München: Verlag Dr. Friedrich Pfeil, 289-310.
Tont SA, Pearcy WG, Arnold JS: Bone structure of some marine vertebrates. Marine Biol. 1977, 39: 191-196. 10.1007/BF00387004.
de Ricqlès A: On bone histology of fossil and living reptiles, with comments on its functional and evolutionary significance. Morphology and Biology of Reptiles, Linnean Society Symposium Series No. 3. Edited by: Bellairs A d’A, Cox CB. 1976, 123-150.
de Buffrénil V, Mazin JM: Caractères structuraux et mode de croissance du fémur d’Omphalosaurus nisseri, ichthyosaurien du Trias moyen de Spitzberg. Ann Paléont. 1987, 73: 195-216.
Wiffen J, de Buffrénil V, de Ricqlès A, Mazin J-M: Ontogenetic evolution of bone structure in Late Cretaceous Plesiosauria from New Zealand. Geobios. 1995, 28: 625-640. 10.1016/S0016-6995(95)80216-9.
Houssaye A: “ Pachyostosis ” in aquatic amniotes: a review. Int Zool. 2009, 4: 325-340. 10.1111/j.1749-4877.2009.00146.x.
Erickson GM: Assessing dinosaur growth patterns: a microscopic revolution. Trends Ecol Evol. 2005, 20: 677-684. 10.1016/j.tree.2005.08.012.
Klein N, Sander PM: Ontogenetic stages in the long bone histology of sauropod dinosaurs. Paleobiol. 2008, 34: 247-263. 10.1666/0094-8373(2008)034[0247:OSITLB]2.0.CO;2.
Erickson GM, Rogers KC, Varricchio DJ, Norell MA, Xu X: Growth patterns in brooding dinosaurs reveals the timing of sexual maturity in non-avian dinosaurs and genesis of the avian condition. Biol Let. 2007, 3: 558-561. 10.1098/rsbl.2007.0254.
Sander PM: Longbone histology of the Tendaguru sauropods: implications for growth and biology. Paleobiol. 2000, 26: 466-488. 10.1666/0094-8373(2000)026<0466:LHOTTS>2.0.CO;2.
Sander PM, Klein N, Stein K, Wings O: Sauropod bone histology and its implications for sauropod biology. Biology of the Sauropod Dinosaurs – Understanding the Life of Giants. Edited by: Klein N, Remes K, Gee CT, Sander PM. 2011, Bloomington, IN: Indiana University Press, 276-302.
Hasse C: Die fossilen Wirbel. Die Histology fossiler Reptilwirbel. Morph Jb. 1878, 4: 480-502.
Kiprijanoff W: Studien über die fossilen Reptilien Russlands. Mém Academie Imp Sci St.-Pétersbourg. 1881, 7: 1-144. 83
Seitz AL: Vergleichende Studien über den mikroskopischen Knochenaufbau fossiler und rezenter Reptilien. Nova Acta Leop. 1907, 87: 230-370.
Gross W: Die Typen des mikroskopischen Knochenbaues bei fossilen Stegocephalen und Reptilien. Z Anat Entw. 1934, 130: 731-64.
Nopcsa F, Heidsieck E: Über eine pachyostotische Rippe aus der Kreide Rügens. Acta Zool. 1934, 15: 431-455. 10.1111/j.1463-6395.1934.tb00661.x.
Zangerl R: Pachypleurosaurus edwardsi, Cornalia, Osteologie, Variations-Breite, Biologie. Abh Schweiz Paläont Ges. 1935, 66: 1-80.
Enlow DH, Brown SO: A comparative histological study of fossil and recent bone tissues. Part II. Texas J Sci. 1957, 9: 186-214.
de Ricqlès A: Recherches paléohistologiques sur les os long des tetrapodes 7: sur la classification, la signification fonctionelle et l’histoire des tissues osseux, des tétrapodes. Ann Paléont. 1978, 64: 85-111.
Sander PM: Skeletochronology in the small Triassic reptile Neusticosaurus. Ann Sci Nat Zool Paris. 1990, 11: 213-217.
de Ricqlès A: Les méchanismes hétérochroniques dans le retour des tétrapodes au milieu aquatiques. Geobios Mém Spéc. 1989, 12: 337-348.
Hampe O: Ein großwüchsiger Pliosauride (Reptilia: Plesiosauria) aus der Unterkreide (oberes Aptium) von Kolumbien. Courier Forschungsinstitut Senckenberg. 1992, 145: 1-32.
Cruickshank ARI, Martill DM, Noe L: A pliosaur (Reptilia, Sauropterygia) exhibiting pachyostosis from the Middle Jurassic of England. J Geol Soc. 1996, 153: 873-9. 10.1144/gsjgs.153.6.0873.
Fostowicz-Frelik L, Gazdzicki A: Anatomy and histology of plesiosaur bones from the Late Cretaceous of Seymour Island, Antarctic Peninsula. Palaeont Pol. 2001, 60: 7-32.
Street HP, O’Keefe FR: Evidence of pachyostosis in the cryptocleidoid plesiosaur Tatenectes laramiensis from the Sundance Formation of Wyoming. J Vert Paleont. 2010, 30: 1279-1282. 10.1080/02724634.2010.483543.
Klein N: Long bone histology of Sauropterygia from the Lower Muschelkalk of the Germanic Basin provides unexpected implications for phylogeny. PLoS One. 2010, 5: 1-25.
Hugi J, Scheyer TM, Sander PM, Klein N, Sánchez-Villagra MR: Long bone microstructure gives new insights into the life history data of pachypleurosaurids from the Middle Triassic of Monte San Giorgio, Switzerland/Italy. Comptes Rendus Palevol. 2011, 10: 413-426. 10.1016/j.crpv.2011.03.009.
Brayard A, Escarguel G, Bucher H, Monnet C, Brühwiler T, Goudemand N, Galfetti T, Guex J: Good genes and good luck: Ammonoid diversity and the end-Permian mass extinction. Science. 2009, 325: 1118-1121. 10.1126/science.1174638.
Bickelmann C, Sander PM: A partial skeleton and isolated humeri of Nothosaurus (Reptilia: Eosauropterygia) from Winterswijk, The Netherlands. J Vert Paleont. 2008, 28: 326-338. 10.1671/0272-4634(2008)28[326:APSAIH]2.0.CO;2.
Currey JD: Bones. Structure and Mechanics. 2000, Princeton University Press: Princeton
Francillon-Vieillot H, de Buffrénil V, Castanet J, Géraudie J, Meunier FJ, Sire JY, Zylberberg L, de Ricqlès A: Microstructure and mineralization of vertebrate skeletal tissues. Skeletal Biomineralization: Patterns, Processes and Evolutionary Trends. Edited by: Carter JG. 1990, New York: Van Norstrand Reinhold, 471-530. 1
Castanet J, Francillon-Vieillot H, Meunier FJ, de Ricqlès A: Bone and individual aging. In Bone. Edited by: Hall BK. 1993, Boca Raton, Florida: CRC Press, 245-283. 7
Padian K: Growth lines. Encyclopedia of Dinosaurs. Edited by: Currie PJ, Padian K. 1997, San Diego, California: Academic Press, 288-291.
Laurin M, Girondot M, Loth M-M: The evolution of long bone microstructure and lifestyle in lissamphibians. Paleobiol. 2004, 30: 589-613. 10.1666/0094-8373(2004)030<0589:TEOLBM>2.0.CO;2.
Chinsamy-Turan A: The Microstructure of Dinosaur Bone. 2005, Baltimore: John Hopkins University Press, 1-195.
Germain D, Laurin M: Microanatomy of the radius and lifestyle in amniotes (Vertebrata, Tetrapoda). Zool Scripta. 2005, 34: 335-350. 10.1111/j.1463-6409.2005.00198.x.
Sander PM, Klein N: Developmental plasticity in the life history of a prosauropod dinosaur. Science. 2005, 310: 1800-1802. 10.1126/science.1120125.
Klein N, Sander PM: Bone histology and growth of the prosauropod dinosaur Plateosaurus engelhardti von Meyer, 1837 from the Norian bonebeds of Trossingen (Germany) and Frick (Switzerland). Spec Pap Palaeont. 2007, 77: 169-206.
Reid REH: How dinosaurs grew. The Complete Dinosaur. Edited by: Farlow JO, Brett-Surman MK. 1997, Bloomington, Indiana: Indiana University Press, 403-413.
Horner JR, Padian K, de Ricqlès A: Comparative osteohistology of some embryonic and perinatal archosaurs: developmental and behavioral implications for dinosaurs. Paleobiol. 2001, 27: 39-58. 10.1666/0094-8373(2001)027<0039:COOSEA>2.0.CO;2.
Cheng Y-N, Wu X-C, Ji Q: Triassic marine reptiles gave birth to live young. Nature. 2004, 432: 383-386. 10.1038/nature03050.
de Ricqlès A, Meunier FJ, Castanet J, Francillon-Vieillot H: Comparative microstructure of bone. In Bone. Edited by: Hall BK. 1991, Boca Raton, Florida: CRC Press, 1-78. 3
Sander PM, Klein N, Buffetaut E, Cuny G, Suteethorn V, le Loeuff J: Adaptive radiation in sauropod dinosaurs: bone histology indicates rapid evolution of giant body size through acceleration. Org Div Evol. 2004, 4: 165-173. 10.1016/j.ode.2003.12.002.
de Ricqlès A, Padian K, Knoll F, Horner JR: On the origin of high growth rates in archosaurs and their ancient relatives: Complementary histological studies on Triassic archosauriforms and the problem of a “phylogenetic signal” in bone histology. Ann Paléont. 2008, 94: 57-76.
Erickson GM, Tumanova TA: Growth curve of Psittacosaurus mongoliensis Osborn (Ceratopsia: Psittacosauridae) inferred from long bone histology. Zool J Lin Soc London. 2000, 130: 551-566. 10.1111/j.1096-3642.2000.tb02201.x.
Krahl A, Sander PM, Klein N: Long bone histology of Middle Triassic Eusauropterygians (Nothosauria and Pistosauria) and its implications for paraxial swimming [Abstract]. J Vert Paleont. 2009, 29: A129-
Preuschoft H, Witzel U: A biomechanical approach to craniofacial shape in primates, using FESA. Ann Anat. 2004, 186: 397-404. 10.1016/S0940-9602(04)80071-2.
Forwood MR: Mechanical effects on the skeleton. Are there clinical implications?. Osteopor Int. 2001, 12: 77-83. 10.1007/s001980170161.
Walker WF: Swimming in sea turtles of the family Cheloniidae. Copeia. 1971, 2: 229-233.
Clark DB, Bemis W: Kinematics of swimming in penguins at the Detroit Zoo. J Zool. 1997, 188: 411-428.
Baudinette RV, Gill P: The energetics of flying and paddling in water: locomotion in penguins and ducks. J Comp Physiol B. 1985, 155: 373-380. 10.1007/BF00687481.
Bernard AI, Lécuyer C, Vincent P, Amiot R, Buffetaut E, Bardet N, Simon L, Prieur A, Fourel F, Martineau F: Regulation of body temperature by some Mesozoic marine reptiles. Science. 2010, 328: 1379-1382. 10.1126/science.1187443.
Paladino FV, Connor MPO, Spotila JR: Metabolism of leatherback turtles, gigantothermy, and thermoregulation of dinosaurs. Nature. 1990, 344: 858-860. 10.1038/344858a0.
Wallace BP, Jones TT: What makes marine turtles go? A review of metabolic rates and their consequences. J Exp Marine Biol Ecol. 2008, 356: 8-24. 10.1016/j.jembe.2007.12.023.
Katsura Y: Ontogenetic change of bone microstructures and its ethological implication in Champsosaurus (Diapsida, Choristodera). Hist Biol. 2010, 22: 380-386. 10.1080/08912961003637066.
Rieppel O: The status of the sauropterygian reptile genera Ceresiosaurus, Lariosaurus, and Silvestrosaurus from the Middle Triassic of Europe. Field Geol NS. 1998, 38: 1-46.
Sander PM, Clauss M: Sauropod gigantism. Science. 2008, 322: 200-201. 10.1126/science.1160904.
Pontzer H, Allen V, Hutchinson JR: Biomechanics of running indicates endothermy in bipedal dinosaurs. PLoS One. 2009, 4: 1-9. 10.1371/journal.pone.0005361.
de Buffrénil V, Mazin JM: Contribution de l’histologie osseuse al’interpretation paleobiologique du genre Placodus Agassiz 1833 (Reptilia Placodontia). Rev Paleobiol. 1992, 11: 397-407.
Romer AS: Osteology of the Reptiles. 1956, Chicago: University of Chicago Press
Fraas E: Die Ichthyosaurier der süddeutschen Trias- und Jura-Ablagerungen. 1891, Tübingen: Laupp
We thank the denizens of the Pop 15/Meck 176 working group for many helpful and inspiring discussions. We thank Hans Hagdorn, founder of the Muschelkalk Museum Ingelfingen, Rainer Schoch, Staatliches Museum für Naturkunde Stuttgart, and Johannes Müller, Museum für Naturkunde, Humboldt-Universität zu Berlin for the loan of fossils, and also for letting us section some of them. We are thankful to Constanze Bickelmann for identification of a morphotype II humerus. Special thanks go to Olaf Dülfer, technician, for instruction and support in preparation of thin sections, polished sections and molds, and to Georg Oleschinski, photographer, both at the Steinmann-Institut für Geologie, Mineralogie und Paläontologie, Universität Bonn, for taking the excellent overview pictures of thin sections. We would like to thank the two reviewers for their comments and discussions which greatly improved the manuscript.
The authors declare that they have no competing interests.
AK, NK, and PMS designed research; AK and PMS performed research; AK, NK, and PMS analyzed data; and AK and PMS wrote the paper. All authors read and approved the final manuscript.
Electronic supplementary material
Additional file 1: The sample of eosauropterygian long bones Information on genus, species, bone type, stratigraphy, locality, and dimensions are given for each sampled specimen. Humeri and femur of Pistosaurus, and the femur of Plesiosaurus dolichodeirus could not confidently be assigned to a body side because of their simplified morphology and insufficient descriptions in the literature. MHI 1906 is incomplete, and the circumference had to be measured 5 mm distally of section plane. Abbreviations: c, circumference; dl, distal length; dw, distal width; ml, measurable length; msl, minimal shaft length; msw, minimal shaft width; pl, proximal length; pw, proximal width; tl, total length; /, absent. (XLS 30 KB)
Authors’ original submitted files for images
Below are the links to the authors’ original submitted files for images.