As gigantic herbivores, sauropod dinosaurs were among the most important members of Mesozoic communities. Understanding their ecology is fundamental to developing a complete picture of Jurassic and Cretaceous food webs. One group of sauropods in particular, Diplodocoidea, has long been a source of debate with regard to what and how they ate. Because of their long lineage duration (Late Jurassic-Late Cretaceous) and cosmopolitan distribution, diplodocoids formed important parts of multiple ecosystems. Additionally, fortuitous preservation of a large proportion of cranial elements makes them an ideal clade in which to examine feeding behavior.
Hypotheses of various browsing behaviors (selective and nonselective browsing at ground-height, mid-height, or in the upper canopy) were examined using snout shape (square vs. round) and dental microwear. The square snouts, large proportion of pits, and fine subparallel scratches in Apatosaurus, Diplodocus, Nigersaurus, and Rebbachisaurus suggest ground-height nonselective browsing; the narrow snouts of Dicraeosaurus, Suuwassea, and Tornieria and the coarse scratches and gouges on the teeth of Dicraeosaurus suggest mid-height selective browsing in those taxa. Comparison with outgroups (Camarasaurus and Brachiosaurus) reinforces the inferences of ground- and mid-height browsing and the existence of both non-selective and selective browsing behaviors in diplodocoids.
These results reaffirm previous work suggesting the presence of diverse feeding strategies in sauropods and provide solid evidence for two different feeding behaviors in Diplodocoidea. These feeding behaviors can subsequently be tied to paleoecology, such that non-selective, ground-height behaviors are restricted to open, savanna-type environments. Selective browsing behaviors are known from multiple sauropod clades and were practiced in multiple environments.
Citation: Whitlock JA (2011) Inferences of Diplodocoid (Sauropoda: Dinosauria) Feeding Behavior from Snout Shape and Microwear Analyses. PLoS ONE 6(4): e18304. https://doi.org/10.1371/journal.pone.0018304
Editor: Andrew Allen Farke, Raymond M. Alf Museum of Paleontology, United States of America
Received: October 27, 2010; Accepted: February 24, 2011; Published: April 6, 2011
Copyright: © 2011 John A. Whitlock. 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: Funding was provided by the Scott Turner Fund (University of Michigan), the Jurassic Foundation (http://jurassicfoundation.org/), and the Geological Society of America (8689-07; http://geosociety.org/). 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.
Herbivory evolved multiple times within Archosauria, the group uniting crocodiles and birds and containing a variety of fossil forms such as dinosaurs, aetosaurs, phytosaurs, rauisuchians, and pterosaurs. Among living archosaurs, however, herbivory is restricted to birds and potentially turtles, which have been recovered as the sister clade to crown-group Archosauria –. Jaw morphology in these living representatives is highly derived (e.g., secondary loss of teeth) and provides a poor analog for the vast majority of extinct, herbivorous archosaurs. Without a direct behavioral analog, progress in understanding the behavior of herbivorous archosaurs has not reached the level of sophistication seen in studies of extinct mammals, whose craniodental anatomy is readily interpreted using modern analogues and dental wear features. As a result, studies of Mesozoic ecology are often hampered by an incomplete understanding of herbivore behavior—an issue that carries great weight due to the relative abundance of herbivores in any ecosystem. As a major link between primary productivity and secondary and tertiary consumers, herbivores represent the base of the animal food pyramid and therefore influence the flow of energy through an ecosystem.
Of particular importance to the understanding of Mesozoic ecology are sauropod dinosaurs, which were the dominant megaherbivores during most of the Jurassic and Cretaceous, a span of approximately 135 million years. Sauropods were typically quite large, with the largest reaching over 30 m in total body length . Although estimates of metabolic rates and food requirements vary –, it is clear that these organisms required a large amount of browse daily. There is also evidence of herding behavior , increasing the local impact of sauropods on a community—higher population density results in greater stress on plant communities as more animals utilize the available resources. Disregarding all other impacts, these animals must have had major effects on communities in terms of bulk mass consumed daily.
Although sauropods lack the obvious adaptations for herbivory (e.g., beaks and cheeks) present in the other major clade of herbivorous dinosaurs, Ornithischia , ongoing work suggests that sauropods were equally specialized for the task. Histological study of thin-sectioned teeth reveals that sauropod dinosaurs had the fastest known tooth replacement rates among vertebrates—some sauropods replaced their teeth every 30 days . Even the slowest replacing teeth in neosauropods (∼62 days; ) were replaced at a rate similar to the fastest replacement rate seen in non-sauropod dinosaurs . Given the remarkable degree of wear seen on shed teeth—perhaps 25–40% crown height lost, based on estimated Nigersaurus crown heights —the implication is that sauropod teeth experienced extreme wear throughout their short life span. As the plant materials a sauropod would have encountered are not particularly abrasive in comparison to modern floras , it is likely that a combination of feeding behavior and sheer volume of plant material ingested is responsible for high wear. Debate continues, however, on how and what sauropods, particularly diplodocoid sauropods, were eating. In this contribution, I examine the diet and behavior of diplodocid sauropods, using data from analyses of snout shape and dental wear (both micro- and macrowear features).
Diplodocoid diets: previous studies
Within Sauropoda, no clade has received as much attention with regard to diet as Diplodocoidea , –. This is due in large part to their unusual skulls, which feature elongate, horse-like faces ending in a squared snout and a comparably short arcade of tiny, narrow-crowned teeth . Because this morphology has typically been regarded as poorly suited for biting or slicing through vegetation, many other hypotheses of feeding behavior have been put forth, including eating plants from riverbeds , scraping algae from rocks, stripping leaves from branches by using the teeth as a sort of ‘comb’ or ‘rake’ , , , and at least partial reliance on carnivory, either on bivalves (Sternfeld in ) or fish . Other workers have suggested that diplodocoid sauropods fed in a manner similar to modern large-bodied herbivores: ground-level browsing , , , . This latter hypothesis has the benefit of being directly observable in modern animals and thus requires no invocation of novel behaviors. Testing this hypothesis is consequently more straightforward and can be accomplished using methods proven effective in studies of both mammals and dinosaurs.
The reconstruction of diet in fossil taxa has a long methodological history, and in sauropods dates back to the 19th century . Two morphological features in particular, snout shape and tooth wear, have proven informative in mammals. Here, I discuss methods historically used to examine those features, and their relevance to the reconstruction of diets in diplodocoid sauropods.
The shape of the premaxilla, constituting the entirety of the anterior-most extremity of the skull, or ‘snout’, in most mammals, has long been suggested to be related to dietary preference or selectivity in herbivorous mammals –. Boué  provided the first quantitative measurement of snout shape in ungulates, the Arcade Index (AI). The AI measured the shape of the incisive arcade in the dentary in ruminants and was calculated by dividing the breadth of the arcade by its anteroposterior depth. An AI of over 1.0 (a square jaw) was found to be associated with grazers, whereas scores below 1.0 (pointed jaws) were found most commonly in browsers, although this measurement is primarily a measure of breadth and does not fully capture snout shape.
Janis and Erhardt  found that although both palatal breadth and snout breadth scale with body size, palatal breadth was more strongly correlated with dietary selectivity (e.g., grazing vs. browsing behavior) in ungulates. The narrowest snout breadths occurred in animals browsing in upper story vegetation . Gordon and Illius  expanded on these observations, noting that incisor arcade structure is also correlated with selectivity. Broader arcades are maladaptive for selective browsing behavior, as this morphology is more likely to result in the unintentional ingestion of unpalatable, undigestible, or dangerous woody parts of browse plants (e.g., thorns). Narrow arcades, conversely, are maladaptive for grazing (a non-selective feeding behavior) because the small breadth of the arcade results in reduced intake efficiency when consuming sward-like growth forms such as grasses. Gordon and Illius  also noted that grazers, in addition to having broader snouts, also have sublinear arcades with a more transversely oriented anterior tooth row. So-called ‘intermediate’ feeders, which may utilize both selective and non-selective behaviors, have snout shapes more similar to those of browsers than grazers. Gordon and Illius  concluded that snout shapes have evolved to maximize food intake within a particular nutritional quality constraint. There also appears to be a size component to behavioral and morphological differentiation: larger animals were found to be less selective than smaller taxa, although at body sizes below about 100 kg, morphological differentiation between snouts seems to be minor .
Solounias et al.  and Solounias and Moelleken  demonstrated that a similar relationship between snout shape and diet also occurred in extinct ungulates. These two studies used a method originally applied to hominids . Snout shape was quantified along a profile defined using the midline and the intersection of the snout with a line drawn at 26° from the midline, originating at the anterior-most point of the premaxillary symphysis. These profiles were then digitized and analyzed using spline-fit functions. Upon examining both reconstructed fossil premaxillae and those of extant ruminants, Solounias et al.  and Solounias and Moelleken  found that snout shape correlates well with selectivity in extant species. Solounias et al.  also confirmed their inferences from snout shape using dental microwear data (see below).
Dompierre and Churcher  modified the method used by Solounias et al.  and Solounias and Moelleken  for their study of diet in extinct camelids. The original method, which relied on the curvature of snout profiles, necessitated scaling each profile to an equivalent size; the Premaxillary Shape Index (PSI) of Dompierre and Churcher  used area ratios and so removed the size component. PSI scores were found to correlate with diet in extant herbivores, such that the highest PSI scores were present in grazers and lower scores were present in selective browsers . Dompierre and Churcher  concluded that PSI scores are potentially indicative of diet in extinct animals as well.
The relationship between snout shape and dietary habit has also been inferred outside of ungulate mammals. Christiansen  examined the relationship between muzzle breadth and body mass in sauropodomorph dinosaurs and found that breadth and mass were correlated, although there was no discussion of snout shape in relation to overall breadth. Additionally, snout breadth was measured at the premaxilla-maxilla suture, which occurs in markedly different places relative to the anterior-most point of the snout in macronarian and diplodocoid sauropods  and may have over-estimated snout breadth in narrow-snouted taxa as a result. Carrano et al.  examined the relationship between a suite of morphological characters (including snout breadth) and dietary preference in hadrosaur dinosaurs. The two subclades within Hadrosauridae, Lambeosaurinae and Hadrosaurinae, were found to be differentiated by relative snout breadth and limb proportions, similar to the pattern seen in ungulates. Carrano et al.  used this to infer an open-habitat, non-selective feeding behavior for the broad-snouted hadrosaurines and a closed-habitat, selective-feeding behavior for the narrow-snouted lambeosaurines. One hadrosaurine, Prosaurolophus, has a relative snout breadth within the range seen in the selectively browsing lambeosaurines ; this may suggest that there is not a perfect correlation between phylogeny and behavior. Similar, though less quantitative, inferences have also been made for ceratopsians  and thyreophorans , .
Although sauropods were typically much larger than both large ungulates and large hadrosaurs, absolute skull size does not differ greatly between the two dinosaurian clades. Cranial volume estimates in sauropods range from ca. 0.05 m3 in Dicraeosaurus  to 0.2 m3 in Brachiosaurus , compared to to ca. 0.3 m3 in the hadrosaur Edmontosaurus . As a result, snout breadths are roughly constrained within a similar morphospace (although some sauropod taxa greatly exceed the range of breadths seen in hadrosaurs, e.g., Nigersaurus ). Sauropod snouts also display a range of variation in shape, from narrow-snouted taxa like Camarasaurus to broader snouted taxa like Diplodocus, that is reminiscent of the pattern observed in modern ungulates (Fig. 1). It is reasonable to hypothesize that the snout morphologies noted in sauropods would have impacted selectivity and intake rate in much the same way that they do in extant ungulates, although in the absence of direct behavioral observations, additional evidence may needed. One source of such evidence is dental wear.
Above: A) Plateosaurus, B) Camarasaurus, and C) Diplodocus snouts. Below: Outlines of snouts from a mammalian browser D), an intermediate feeder E), and a grazer F). Sauropod snouts modified from ; mammal snout outlines modified from .
Dental microwear is the study of damage done to teeth by contact with other surfaces, in particular the interactions between a tooth and food, grit, and opposing teeth. Studies of microwear typically include the quantification of features falling into one of the following three categories (Fig. 2; ):
- scratches: features that are at least 4 times longer than wide
- pits: deep, subcircular features
- gouges: oblate features with irregular margins
A) Scratches, features at least 4× longer than wide. B) Gouges, large features with irregular margins. C) Pits, subcircular features, typically small. D) A tooth of Nigersaurus, illustrating the paired wear facets, labial (ewf) and lingual (lwf), seen on rebbachisaurid teeth. The labial facet is seen in most diplodocoid dentitions. Scale in A = 0.5 mm; B, C to scale with A. Scale in D = 1 cm. D is modified from .
Such features preserve information about the last few meals an organism ate and are one of the few direct lines of evidence we have for interpreting the diets of extinct organisms, particularly when those organisms have no extant descendants for comparison. Although caution must be used when interpreting diets of extinct organisms, broad dietary categories are often assignable. By providing direct evidence of what organisms ate, microwear features can also indicate overlap in resource exploitation and behavior.
The majority of microwear studies to date involve the reconstruction of diets in extinct and extant mammals , –, based primarily on wear features recovered from molars and premolars. Increasingly, however, studies focusing on the dental microwear of non-mammalian organisms have begun to appear, including cynodonts , crurotarsans , dinosaurs , , , , , –, and fish , . Of these, only the analyses of microwear in stickleback fish ,  were able to control diet experimentally using the organism itself; the rest relied upon comparisons with studies of mammalian microwear.
This reliance is a potential concern, due to broad differences in shape and function between the majority of teeth in question and the molariform teeth examined in the mammalian studies. Molars are used for oral processing of food in mammals, using a combination of puncturing, slicing, and crushing to break down foodstuffs. Non-mammalian animals typically have no oral processing (with the notable inferred exceptions of marginocephalian and ornithopod dinosaurs) and use their teeth solely for food-acquisition behaviors involving puncturing or slicing. Incisiform teeth, therefore, may prove a more useful analogue to archosaur teeth than molariform teeth.
The majority of incisor microwear studies have been done on primates, although isolated studies of non-primate incisor microwear exist –. There is evidence for a correlation between incisor wear and diet in primates – although some  suggest that incisor microwear is useful only for determining finer-scale dietary preference, once a broader category (e.g., frugivory) has been determined by other means.
Although the degree to which the manual manipulation of foodstuff by primates alters the character of wear is uncertain, some behaviors, such as leaf stripping, are strong candidates to broadly correspond with potential food acquisition behaviors in other organisms. Importantly, leaf stripping is known to leave characteristic microwear patterns on incisors in Gorilla . There is also evidence that browse height impacts incisor microwear in predictable ways, with a greater proportion of large features appearing on the teeth of upper canopy feeders than on those of ground-level feeders as a result of the lower concentration of grit relative to phytoliths in food obtained at those greater heights , , . In the Mesozoic, it is probable that phytoliths occurred in both understory plants (i.e., ferns; ) and upper-story conifers . Studies of modern plants, however, suggest that ferns accumulate substantially less silica (primarily taken up as phytoliths) than other gymnosperms, such as conifers ; extrapolated to the Mesozoic, this suggests that an organism feeding on the ground cover would encounter a higher grit-to-phytolith ratio, as suggested above. Some understory plants (particularly Equisetum) are presumed to have been major silica accumulators, however , .
The only study to examine both molar and incisor microwear in an ungulate (Equus quagga, a grazer; ), found that patterns of molar microwear and incisor microwear were not similar, such that pits, rather than scratches, were the dominant feature on the incisors. This is potentially explained either as a function of exogenous grit, as the incisors would have been the first teeth to contact a foodstuff and would therefore encounter more of the grit, or as a function of selective use of incisors in feeding on more robust foodstuffs (e.g., woody plants) .
As noted above, several studies have discussed microwear features in sauropod dinosaurs, most commonly in diplodocoid sauropods , , , . Although the features recovered from diplodocoid teeth (Diplodocus in , , ; Nigersaurus in ) are typically similar, primarily fine scratches, the interpretation of the behavior that caused these features differs, from high browsing (e.g., feeding on upper canopy vegetation) ,  to branch stripping  to ground-level browsing . The uncertainty over the functional significance of these wear features is likely exacerbated by two factors: first, sauropod microwear has previously been examined in the absence of other data, unlike what has been done for modern and extinct mammals; and second, sauropod diversity has been sampled only narrowly, and so there has been little relevant comparative data.
The influence of jaw motion on microwear features in sauropod dinosaurs is also worthy of discussion. The tooth row in diplodocoids is restricted anteriorly, resulting in a dentition that is primarily oriented transversely . Because of this orientation, it is most probable that diplodocoid sauropods utilized a shearing bite with a primarily orthal motion, making their dentitions coarsely analogous to the incisors of many primates , , but not necessarily ungulates . Although previous work , ,  has suggested the possibility of propaliny in the bite stroke of diplodocids, the lack of marginal dentition in diplodocoids would mean that much of the fore-aft motion would be wasted during the slicing phase of the bite, as the transversely-oriented tooth row would only occlude for a fraction of the stroke before being taken out of alignment. Additionally, when propaliny has been proposed for other dinosaurs , , , it has been demonstrated as a means to prolong the occlusion and increase oral processing efficiency . Sauropods, however, lack the fleshy cheek that enables oral processing in ornithischian herbivores , and the teeth were likely used purely for food acquisition rather than processing. It is most parsimonious to assume, therefore, that the functional component of the bite—where tooth met food—was orthal in nature. This does not mean that there could have been no palinal motion during the stroke; fore-aft movement of the lower jaw may have been used to accomplish occlusion of the upper and lower tooth rows prior to the final bite phase (as also happens in some mammals , ) or to widen the gape , . It does suggest, however, that there was little to no retractive component of the bite stroke during a microwear-producing phase (i.e., where tooth-food contact occurred). Although the articulation in many diplodocoids is known only from the quadrate and not the lower jaw, most diplodocoid jaw joints are presumed to be similar , suggesting that any in-group variation in wear features perceived is most likely the result of diet and not jaw motion.
It is also important to note that much of the work on mammalian microwear surrounds the grazer-browser continuum, which necessarily cannot apply to Jurassic and Early Cretaceous dinosaurs due to the lack of grasses at that time . Therefore, many of the assumptions about the relationship between microwear patterns and ground-height feeding behavior, such as the dominance of scratches over pits seen in grazers , must be re-examined. As seen elsewhere (fig. 8A in ), browsers and grazers separate along the scratch count axis, but browsers (including low, medium, and high browsers) separate primarily along the pit count axis (figs. 8A–D in ). It is probable, then, that the ratio of pits-to-scratches is more likely to be informative of diet in browsers such as sauropods.
Caution should be exercised when drawing parallels between microwear on mammalian teeth (including incisors) and that found on sauropod teeth. The chewing motion of an ungulate, with its transverse power stroke, is highly derived and without parallel in Sauropoda. Certain aspects of foodstuffs, particularly their toughness and grit content, however, can be expected to influence microwear features with reasonable consistency across taxa. Although the relationship between incisor microwear and diet is uncertain, inferences can still be drawn about the character of foodstuffs ingested. In particular, feature size and texture are expected to correspond with browse height and certain intrinsic plant properties, such as woody vs. herbaceous stems.
To develop a testable hypothesis for diplodocoid feeding behavior, evidence from snout shape and microwear will be compared, not just with data from modern herbivores, but also with each other. In this way, an approximation of the “total evidence” approach will be brought to bear on this question.
Materials and Methods
Morphological data, in this case snout shape and microwear features, can be used to distinguish between several combinations of browse height (ground-height, mid-height, and upper canopy) and browse strategy (selective and nonselective) in diplodocoid sauropods. Here, ground-level feeding is defined as feeding on vegetation within 1 m of ground height, mid-height feeding is defined as feeding between ground height and 10 m, and upper canopy feeding is feeding at all heights above 10 m. Ten meters is chosen as the upper limit for mid-height browsing based on estimated maximum head height of diplodocoids in quadrupedal stance, using combined neck and forelimb height . The following is summarized in Table 1.
Evidence for browse height
Browse height was examined primarily through the examination of dental microwear features. The primary influence of browse height on microwear is through the creation of pits as a consequence of ingested grit. Grit, exogenous mineral particles, are suspended and transported in the air through aeolian processes and through the actions of animals (e.g., walking). These particles then fall out of suspension and are deposited on the ground or on plants. A proportionally larger amount of grit is deposited on plant surfaces at lower heights than those that greater heights , . Taxa that browse at lower heights therefore typically ingest more extraneous grit, and their teeth may have a higher proportion of pits in their microwear features, as is seen in ground-height browsing ungulates ; this trend may be particularly exaggerated in the incisors of those animals . Recent work also suggests that grit and dust does not have an additive effect on scratch counts in mammals , so we might expect to see the effect of increasing grit solely in the proportion of compressional features such as pits. Ground-height browsing sauropods will therefore be expected to have the highest proportion of pits in their microwear features, followed by mid-height and upper canopy browsers.
The incisors of ground-height feeding primates also display a slightly different character than those of taxa browsing at greater heights. Mean scratch breadth is lower in taxa browsing at or near ground height, as a function of mean particle size and the ratio of soil particles to phytoliths , . Because the teeth of sauropod dinosaurs are assumed to be functionally analogous to the incisors of mammalian herbivores (see above), it is expected that the scratch breadth in ground-height browsing sauropods will also be smaller than in those that browse at different heights. Although a diet heavy on plants with substantial silica accumulation (e.g., modern Equisetum; ) may skew scratch breadth towards the broad end of the spectrum, such plants were rarely a dominant component of relevant ecosystems (see Environmental Signal, below), and silica accumulation in other ground-height forage is assumed to be lower than that of mid- and upper-canopy browse . Additionally, the impact of woody browse (likely a component of selective browser diets) may overwhelm the signal from phytolith components, resulting in still broader scratches in selective browsers. Nonetheless, the potential impact of diet on scratch breadth will need to be accounted for where appropriate.
Evidence for browsing strategy
Browsing strategy (selective vs. nonselective) was examined using both microwear and snout shape indices. Snout shapes in selective browsers were predicted to be narrower than those of nonselective browsers, as in herbivorous mammals. Two microwear features can indicate browse type: scratch orientation consistency and feature size. Consistency of scratch orientation has been related to food texture, such that softer (e.g., herbaceous) foods result in more unimodally distributed scratch orientations, whereas low consistency of orientation (i.e., cross-scratches) is related to eating harder or more brittle foods , . Cross-scratching of this type has been seen on the shearing facets of cat carnassials, where it has been hypothesized to be the result of the multiple bite actions observed in those animals when attempting to bite through tough materials , ; movement of incompletely sheared foodstuffs across the facet during this process would create cross-scratching on a shearing facet , . Note that this does not require complex jaw movements, as the cheek teeth in cats are in precise occlusion , . Harder foods encountered by a sauropod would likely have included thick stems, indicating woody browse that is selectively browsed upon. Larger features (i.e., gouges, coarse scratches) also indicate selective browsing, either as a result of woody stems (coarse scratches) or large particles such as seeds or spores (gouges).
Quantifying snout shape
Six genera of diplodocoid sauropod dinosaur (Apatosaurus, Dicraeosaurus, Diplodocus, Nigersaurus, Suuwassea and Tornieria) preserve enough of the skull to reconstruct the snout shape. The skulls of these six genera were reconstructed in dorsal view based on examination of the original materials (Table S1). These reconstructions are prone to some error, and the amount of material available necessarily influences their accuracy; Diplodocus, for example, is known from multiple articulated skulls, whereas Dicraeosaurus is known only from disarticulated braincases and fragmentary dermal elements. Nonetheless, these were produced with as much rigor as possible, and so should vary in ways consistent with their variation in life.
These reconstructions (Fig. 3) were measured using two squareness indices: the upper arcade index (uAI) and the premaxillary-maxillary index (PMI). A third method, measuring the divergence angle of the premaxillae, enables the direct measurement of squareness from fossils, as it does not require a reconstruction to remove deformation. These indices were then compared among taxa, first to test the null hypothesis that there is no difference in snout squareness among diplodocoids, and second to test the hypothesis that any variation in snout shape is correlated with phylogeny, not diet. The non-diplodocoid neosauropods Brachiosaurus and Camarasaurus were also examined, as taxa widely recognized as relatively selective browsers and as outgroups to the diplodocoids. To further elucidate trends in snout shape, the basal eusauropods Jobaria (based on ), Mamenchisaurus (based on ; this shape is extrapolated from a dentary), Patagosaurus (extrapolated from the dentary MPEF-PV 1670), and Shunosaurus (extrapolated from the dentary ZG65430) were also examined, as was the basal sauropodomorph Plateosaurus (based on ). In the absence of microwear or other contextual data for these latter organisms, interpretation of their feeding behavior is limited.
Reconstructions of Nigersaurus and Diplodocus modified from  and , respectively. All other reconstructions based on material listed in Table S1. Skulls scaled to equivalent anteroposterior lengths.
The uAI is a modification of the AI introduced by Boué . Although the original metric measured the ratio of the depth and breadth in the lower dental arcade, the uAI utilizes the upper jaw instead, because upper jaws are more commonly preserved in diplodocoid dinosaurs. In order to retain 1.0 as the dividing score between square and round jaws, the uAI measures only the right or left half of the snout (Fig. 4), although Boué's metric included both right and left jaws in its width measurement. In both metrics, the measured variable is the width of the dental arcade (in the uAI, the half-width) divided by the anteroposterior depth.
Snout depicted based on Diplodocus in Figure 3, anterior towards top of page. From left to right: the upper arcade index (uAI) measures snout breadth by taking the ratio of arcade width to arcade depth (higher numbers indicate squarer snouts); the premaxilla-maxilla index (PMI) is determined by taking the ratio of an area covered by the snout within a predetermined triangle to the area of that triangle (higher numbers indicate squarer snouts); the premaxillary divergence angle (PMDA) determines squareness by measuring the divergence of the anterior margin of the premaxilla from perfectly square (higher numbers indicate greater divergence from square and therefore roundness). The angle of the hypotenuse of the triangle used to calculate PMI (26°; 64° internal angle) is based on the angle used in the PMI's parent metric, the PSI .
The PMI is also a modification of an older metric; in this case it is a modification of the premaxillary shape index (PSI) . Because the sauropod snout includes both the premaxilla and the maxilla, the PSI is only slightly modified as the premaxillary-maxillary index (PMI). This index is otherwise calculated in much the same way as the PSI (Fig. 4). First, a line is drawn perpendicular to the sagittal midline of the skull and tangent to the anterior-most point on the skull. A second line is drawn parallel to the midline tangent to the broadest point of the snout. A third line is then drawn at 26° from the long axis of the skull connecting the first two lines, forming a right triangle; 26° is used to be consistent both with the PSI and with work predating the PSI. The area of the skull within that triangle is calculated (using the measure tool in Adobe Photoshop CS4) and compared to the area of the triangle as a whole to compute the PMI. In cases where the snout narrows behind its broadest part (e.g., Nigersaurus, certain hadrosaurs), the shape posterior to the broadest point is disregarded, and the snout is considered to have continued in a straight line to the point of intersection with the hypotenuse. Although this may inflate the PMI score slightly, it more accurately reflects the effective shape of the snout.
Premaxilla Divergence Angle.
Due to the often fragmentary or deformed nature of fossil material, the prior two metrics rely on reconstructions of skulls; measurements based on deformed materials would necessarily represent an unrealistic shape. Although every effort was made to accurately reconstruct morphology, this has resulted in a small sample size. One method to measure squareness directly from fossil material (reducing potential error inherent in reconstruction) and increase sample size involves comparing the angles of divergence on the anterior margin of the premaxilla (PMDA). This is measured here by orienting the specimen in strict dorsal or ventral view and measuring the angle formed between the anterolateral and anteromedial corners of the premaxilla and a line drawn perpendicular to symphysis (Fig. 4).
Forty-seven teeth belonging to seven genera were examined for microwear features (Table S2); of these, only 12 were subsequently deemed suitable for analysis (Table 4). Damaged or heavily weathered teeth were deemed unsuitable and not examined, following . The suitable teeth were molded using a high-resolution polyvinylsiloxane dental molding material (Coltene Whaledent President microSystem 6012). Casts were made in water-clear epoxy and examined at 70× using transmitted light microscopy, following . Images were taken using a Spot CCD camera (Spot Insight 11.2 Color Mosaic, Diagnostic Instruments) at the highest resolution available (36 bits/pixel, 300 dpi), mounted on a Nikon SMZ 1500 microscope. Image analysis was performed in Microware 4.02 . Where possible, wear was examined from multiple sites on the same tooth and averaged. Features measured were scratch number, scratch orientation, pit number, and pit size. Patterns of microwear were examined against patterns characteristic of feeding behavior in modern mammals (see below). Following recent criticisms of purely quantitative analyses of microwear , analysis of microwear features is based solely on qualitative comparisons (e.g., average size, shape) and feature-to-feature ratios; raw counts and counts per unit area are provided but not analyzed.
Although sauropod remains are abundant globally, skulls are a rare component of sauropod fossil assemblages . Even Diplodocoidea, the clade most completely represented by cranial material, contains only six genera with tooth-bearing elements associated with them (see above). Isolated, shed teeth are common finds, but are not identifiable to a useful degree, and can only be assigned to large clades (e.g., Diplodocoidea). In some instances, particularly involving Morrison Formation sauropods, isolated dentigerous elements are also not identifiable to the genus level, due to the paucity of non-basicranial autapomorphies in the clade. Even among those teeth that are both worn and assignable to a particular taxon, preserved wear features are rare, resulting in the relatively small sample size seen here.
The distributions of three variables were examined statistically: snout shape (for browsing strategy), scratch breadth (for browse height), and pit/gouge size (for both height and strategy). For two-sample comparisons, non-parametric Mann-Whitney U tests were performed; sample sizes for snout shape were too small to meet normality criteria, and both scratch breadth and pit/gouge size failed a normality test (Shapiro-Wilk) for all samples. The Kruskal-Wallis test (an extension of the Mann-Whitney U) was used for instances where multiple comparisons were desirable. For significant results of Kruskal-Wallis tests, pairwise comparisons (following the method of ) with an adjusted P-value were used to determine which samples were distinguishable from each other.
AMNH, American Museum of Natural History, New York, New York, USA; ANSP, Academy of Natural Sciences, Philadelphia, Pennsylvania, USA; CM, Carnegie Museum of Natural History, Pittsburgh, Pennsylvania, USA; CMC, Cincinnati Museum Center, Cincinnati, Ohio, USA; CMN, Canadian Museum of Nature, Ottawa, Ontario, Canada; CPC, Colección Paleontológica de
Coahuila, Saltillo, Coahuila, Mexico; MB.R., Humboldt Museum für Naturkunde, Berlin, Germany; MNN, Museé National du Niger, Niamey, Niger; MPEF, Museo Paleontológico Egidio Feruglio, Trelew, Chubut, Argentina; MOR, Museum of the Rockies, Bozeman, Montana, USA; PU, Museum of Natural History, Princeton University, Princeton, New Jersey, USA; ROM, Royal Ontario Museum, Toronto, Ontario, Canada; RTMP, Royal Tyrell Museum of Palaeontology, Drumheller, Alberta, Canada; USNM, United States National Museum, Washington, D.C., USA; UUVP, University of Utah, Salt Lake City, Utah, USA; YPM, Yale Peabody Museum, New Haven, Connecticut, USA; ZG, Zigong Dinosaur Museum, Zigong, Sichuan, People's Republic of China.
Four taxa (Apatosaurus, Dicraeosaurus, Diplodocus, and Nigersaurus) preserve enough of the maxilla that the uAI can be calculated. This metric could not be determined for Suuwassea and Tornieria; the only known maxillae of those taxa are distally incomplete and the position of the posterior-most tooth cannot be accurately determined. Nigersaurus had the highest uAI score and therefore the squarest snout (4.0), followed by Apatosaurus (1.5) and Diplodocus (1.2). Dicraeosaurus has the lowest uAI score (0.6). The non-diplodocoid sauropods Brachiosaurus and Camarasaurus have uAI scores similar to those of Dicraeosaurus (0.6 and 0.4, respectively).
As above, Nigersaurus had the highest PMI value (95%). Apatosaurus (84%) and Diplodocus (84%) had the next highest PMI, followed by Dicraeosaurus (74%) and Suuwassea (74%). Tornieria (71%) had the lowest PMI score of the ingroup taxa. Diplodocoids had higher PMI scores (and therefore squarer snouts) than all outgroup taxa (Brachiosaurus = 68%; Camarasaurus = 63%). Snouts of the basal eusaruopods Jobaria (55%), Mamenchisaurus (58%), and Shunosaurus (58%) were rounder than those of all examined neosauropods, although Patagosaurus (65%) has a snout shape intermediate between Brachiosaurus and Camarasaurus. The basal sauropodomorph Plateosaurus (44%) was roundest of all.
Premaxillary Divergence Angle.
The initial sample included 16 premaxillae. Of those 16, 12 were deemed complete enough to measure (Table 3). In the incomplete premaxillae, the thin ‘lateral plate’  that extends ventrally from the labial margin of the premaxilla and forms the ventral-most portion of the element was missing or heavily damaged, preventing accurate assessment of the PMDA from those elements.
The diplodocoids again appear to have segregated into two groups, with Dicraeosaurus (24°), Suuwassea (25°), and Tornieria (25°) having high divergence angles compared to Apatosaurus (6°), Diplodocus (7°), and Nigersaurus (4°). The snout of Nigersaurus is again the squarest; those of Suuwassea and Tornieria are the roundest. The difference between Nigersaurus and Apatosaurus is less marked (2°) than with previous metrics. The PMDA of Brachiosaurus (35°, 30°; average = 33°) and Camarasaurus (27°, 45.4°, 46.5°; average = 40°) are higher than for any diplodocoid. The variation observed in Camarasaurus is potentially the result of ontogeny; the element that provided the 27° PMDA measurement (UUVP 3999) is much larger and presumably came from an adult, whereas CM 11338 is a subadult individual.
Although 47 teeth were examined for microwear features, only 11 (23%) were found to have features that record diet. Of these, only seven teeth belonging to five taxa (Brachiosaurus, Camarasaurus, Dicraeosaurus, Diplodocus, and Nigersaurus) appeared to preserve an accurate sample of wear. Figure 5 illustrates representative wear features for these five taxa. The remaining four teeth preserve microwear that cannot be directly attributed to diet, either due to taphonomic alteration (Apatosaurus), location (not on the wear facet itself; Diplodocus USNM 2673, Nigersaurus G100), or because the preserved features are so few in number (Rebbachisaurus).These final four teeth and their microwear features are described below and compared qualitatively. Full results are presented in Table 4; raw data (including individual feature dimensions) are available in Table S3.
A, Diplodocus. B, E, Dicraeosaurus. C, Nigersaurus. D, Apatosaurus. F. c.f. Rebbachisaurus. A, C, D, and F dominated by small pits and fine scratches, interpreted as indications of ground-height, non-selective browsing; B and E are dominated by large gouges and coarse scratches, interpreted as indications of mid-height, selective browsing. A–F to scale; scale bar in A, E = 0.5 mm.
The probable Apatosaurus skull CMC VP 7180 contains multiple teeth in-situ, although the majority of these teeth were broken apically. Wear features were only recovered from one tooth, the first tooth in the left dentary. Although this tooth was heavily abraded post-mortem, as indicated by a ‘sugary’ texture , many small, subcircular features can be seen dotting the surface of the dentine. No scratches are recorded in the dentin, and no features were recovered from the enamel of any tooth.
Two teeth (MB.R. 2204 and 2197), tentatively assigned to D. hansemanni, preserve some microwear features. Features are recovered from both dentine and enamel surfaces of MB.R. 2204. On both surfaces, pits and gouges outnumber scratches, and large irregular features (gouges) are more common than the smaller, subcircular pits. On both surfaces, scratches lack a preferred orientation and cross-scratches are common. Features on the dentine are finer than those on the enamel surface.
The second tooth, MB.R. 2197, does not preserve a large amount of microwear, although some features are present on the labial enamel edge. Here, two exceptionally large gouges are preserved. No scratches or smaller pits were observed, and it is probable (although not certain) that these gouges are not the result of tooth-food or tooth-tooth contact.
Three teeth from two specimens (CM 11161 and USNM 2673) preserve microwear features on the enamel.
Microwear features were recovered from small areas of the labial enamel margin of the facet on the second right premaxillary tooth and the first left premaxillary tooth of CM 11161. Identification of features was hampered here and on other diplodocid specimens by the application of a preservative lacquer, likely around the turn of the century. Attempts to remove this lacquer using alcohol-based solvents were generally unsuccessful.
As also seen in Dicraeosaurus, pits and gouges outnumber scratches on the enamel of teeth from CM 11161. Of the two features, small subcircular pits are substantially more common than large gouges. Scratches are generally subparallel, although cross-scratching does rarely occur, and oriented roughly along the apicobasal axis. Scratches extend over the edge of the facet and onto the lingual surface of the tooth for a short distance.
Seven loose teeth are associated with the Diplodocus longus skull USNM 2673. None of these teeth have wear facets, and based on the size and position of one tooth, some of them may have been unworn replacement teeth. One tooth, however, an incomplete crown recovered separately from the other six loose teeth, does preserve what appear to be wear features on the presumed labial surface some distance from the apex. Based on size comparisons with the intact teeth of USNM 2673, this crown appears to be an upper tooth.
The wear features recovered from this surface differ from those seen on the labial facet in CM 11161 in both size and character. Scratches are substantially longer and broader than those from the facet margin. They are generally sub-parallel with rare-cross scratching, but the orientation is nearly perpendicular to the long axis of the tooth, with only a slight apicobasal component. Pits are also larger than those observed on the facet, although they are proportionally identical to those from CM 11161. Because these features do not come from either a facet or from the apical surface of the crown, they cannot be confirmed as the result of a bite stroke.
Wear features were recovered from two crowns, one each from the the G2 and G100 assemblages.
Wear features were observed on the labial enamel margin of the labial facet on the G2 crown. As in Diplodocus, scratches are elongate and narrow. Scratch orientation is generally apicobasal, without cross-scratching. Small pits are the most common feature on the facet. The proportions of these pits are more oblate than those of Diplodocus and Apatosaurus, but substantially rounder than those observed in the enamel of Dicraeosaurus.
No wear features were recovered from the facet of the crown from G100, perhaps as a result of post-mortem wear. Features were observed on the lingual surface of the enamel basal to the actively worn surface. Of the features observed, the majority were scratches. All features were generally larger than those observed on the facet of G2. Similar to the wear recovered from USNM 2673, scratch orientation is more mesiodistal than apicobasal, although there is still a minor apicobasal component. Cross scratching occurs but is rare. Pit size was also substantially larger than those seen in the G2 tooth. Because these features are located away from surfaces of active wear, it is likely that they were caused by some contact outside of the bite stroke.
A single loose tooth of rebbachisaurid type (MNHN 1512a; see ) is referable to Rebbachisaurus. Wear features were recovered from the enamel near the smaller facet (presumably the labial surface). Scratches were very long and narrow. Cross scratching did occur, although scratches appear to be predominantly mesiodistally oriented. Pits were quite large but generally subcircular.
Two teeth (UUVP 1949, UUVP 3986) preserved a substantial amount of quantifiable microwear features. In both cases, pits outnumber scratches. The pits are large, similar in size to those seen in Dicraeosaurus. Scratch length varies but is generally shorter than that seen in Diplodocus and Nigersaurus. Scratch breadth is broad and most similar to that seen in Dicraeosaurus. Cross scratches are rarer than in Dicraeosaurus but do occur.
Wear features were recovered from a single tooth, MB.R. 2190. Scratches dominate the preserved features. The pits that are preserved are often quite large, larger than but most similar to those preserved in Dicraeosaurus. These largest pits are typical of the wear found at the outermost margin of the facet; basal to the facet, the pits are more typical of the size seen in Diplodocus and Nigersaurus. Scratches are comparatively short, and cross-scratches are common. Scratch breadth is intermediate, occurring between the ranges of Diplodocus and Dicraeosaurus.
The six ingroup taxa examined can be broadly divided into two categories: square and round. Square-snouted diplodocoids include the diplodocids Apatosaurus and Diplodocus and the rebbachisaurid Nigersaurus. Round-snouted diplodocoids include the dicraeosaurids Dicraeosaurus and Suuwassea, and the diplodocid Tornieria. Round-snouted diplodocoids are generally squarer in profile than outgroup taxa such as Brachiosaurus and Camarasaurus, however.
Testing this statistically proves somewhat problematic, however. Grouping the sauropods a priori into three groups—“square” diplodocoids (Apatosaurus, Diplodocus, and Nigersaurus), “round” diplodocoids (Dicraeosaurus, Suuwassea, and Tornieria), and outgroup sauropods (Brachiosaurus and Camarasaurus)—permits examination of any differences in their means, although at such low sample sizes, the power of statistical tests to avoid Type II errors (erroneously failing to reject the null hypothesis) is reduced, and two populations may be construed as falsely similar. A Kruskal-Wallis test rejects the null hypothesis, that all samples have the same median, for both PMI (H = 6.402, d.f. = 2, P = 0.041) and PMDA scores (H = 13.176, d.f. = 2, P = 0.001). Pairwise comparisons found that, for both metrics, only the square population could be distinguished from the outgroup (P = 0.038). All other pairwise comparisons (round vs. outgroup, P = 0.773; square vs. round, P = 0.387) were found to be indistinguishable. The small sample size hampers the power of statistical tests to separate these groups, however.
This pattern of snout shapes is reminiscent of the pattern seen in modern ungulates. In light of that comparison, the broad-snoutedness seen in Apatosaurus, Diplodocus, and Nigersaurus is interpreted as an adaptation to ground-level, non-selective browsing in at least some diplodocoid sauropods. The narrower, rounded snouts of Dicraeosaurus, Suuwassea, and Tornieria are interpreted as evidence for greater subsistence on mid-height, selective browse, although the intermediacy of these shapes between the squarest diplodocoids and the roundest outgroups may indicate at least partial reliance on non-selective browsing in these taxa.
The snout shapes of macronarian sauropods like Brachiosaurus and Camarasaurus are consistently rounder than those of diplodocoid sauropods. If this difference is reflective of a different feeding behavior, it may be due to the difference in browse height. Brachiosaurus and Camarasaurus were both probably mid- to upper-canopy browsers, based on studies of neck posture , , ,  (but see ) and limb proportions , , . Diplodocids and dicraeosaurids, however, were likely browsing near or at ground level , , . Differences in available vegetation at such lower heights (herbaceous plants at low heights, woody browse at mid- and upper heights), potentially resulting in the occasional non-selective exploitation of browse, may have influenced the relative breadth of the snout in Dicraeosaurus, Suuwassea, and Tornieria. Alternatively, there may be a phylogenetic component to the difference in snout shapes between selectively browsing diplodocoids and macronarians—if broad snouts are plesiomorphic for Diplodocoidea, there may be some constraint on the degree of roundness attained.
Examination of sauropod taxa outside the neosauropod radiation (Jobaria, Mamenchisaurus, Patagosaurus, and Shunosaurus) suggests that neosauropods as a whole display increased snout squareness over more basal taxa (U = 1, P = 0.01), although taxa like Patagosaurus appear to have achieved macronarian-type snout broadness early in eusauropod evolution. Eusauropods, in turn, are squarer than basal sauropodomorphs like Plateosaurus. This general trend towards increasingly square snouts may be related to an increased reliance on bulk herbivory ,  and is possibly also related to the observed trend towards larger tooth crowns in sauropod and eusauropod dinosaurs . The variation seen in basal eusauropods may be related to feeding behavior, but more research (particularly the acquisition of microwear data) is required to fully evaluate this hypothesis.
Comparisons with hadrosaurids.
As discussed previously (see Reconstructing Diets, above), Carrano et al.  noted a general dichotomy of form between hadrosaurine and lambeosaurine hadrosaurs—hadrosaurines had broad snouts, lambeosaurines had narrow snouts—and related this difference to a division in dietary habit, such that the hadrosaurines (H) were interpreted as non-selective browsers and the lambeosaurines (L) were selective browsers. As large bodied dinosaurian herbivores, hadrosaurids are a potentially useful comparison for sauropods, particularly with regard to snout shape. PMI scores were determined for Anatotitan copei (H; ; this may be referrable to Edmontosaurus, however ), Edmontosaurus regalis (H; ), Maiasaura peeblesorum (H; ), Prosaurolophus maximus (H; ), Saurolophus osborni (H; ), Corythosaurus sp. (L; CMN 34825), Hypacrosaurus altispinus (L; ROM 702), Lambeosaurus sp. (L; ROM 758) and Velafrons coahuilensis (L; ). Although the premaxilla would have been covered in a keratinous beak in vivo, it is not unreasonable to assume the shape in life closely mirrored that of the bony supporting elements beneath. Although CMN 34825 and ROM 758 most likely represent juveniles, no study has yet noted shape change associated with the snout through ontogeny in ornithopods – or other dinosaurs, excluding only Diplodocus . Furthermore, examination of an embryonic specimen of Hypacrosaurus (RTMP 87.79.334, ) results in an identical PMI to that of the adult (ROM 702), suggesting that snout shape was conserved in these taxa. Snout shape (PMI) scores and material used for reconstructions are given in Table S4.
Broad-snouted diplodocids group within the range of PMI scores seen in hadrosaurines; in both clades, scores cluster around 80–85% (Fig. 6; only those taxa examined by Carrano et al.  are plotted). The exceedingly square snout of Nigersaurus (95%) is nearly matched by that of Anatotitan (93%). Lambeosaurines, particularly Hypacrosaurus (76%) and Lambeosaurus (74%), typically have rounder snouts than hadrosaurines, although there is some overlap (e.g., Corythosaurus, 80%). There is also overlap in the range of scores between the upper end of the round-snouted diplodocoid range (Dicraeosaurus, 74%) and lower end of the lambeosaurine range (Lambeosaurus, 74%), although the PMI of Tornieria (71%) is lower than in any hadrosaurid examined. The lambeosaurine Velafrons, which was not included by Carrano et al.  and was not plotted in Figure 6, has a PMI score (85%) more similar to those of square-snouted diplodocids and hadrosaurines, which suggests the potential for non-selective browsing in Lambeosaurinae.
The vertical axis separates taxa into sauropods (top), hadrosaurines (middle) and lambeosaurines (bottom). Squares represent taxa considered to have been non-selective browsers, circles represent taxa considered to have been selective browsers. Blue tones indicate the range of square snouts and yellow tones indicate the range of round snouts; green tone indicates overlap; dark blue/dark yellow represent the limits of hadrosaurian snout shape diversity. Overlap in snout shape occurs between behavioral guilds in hadrosaurs, but not in sauropods, although sample size is limited for sauropods. Sauropod snout shapes are also more disparate than snout shapes in hadrosaurids. Inferences of hadrosaur diet based on . Abbreviations: An, Anatotitan; Ap, Apatosaurus; Br, Brachiosaurus; Ca Camarasaurus; Co, Corythosaurus; Dic, Dicraeosaurus; Dip, Diplodocus; Ed, Edmontosaurus, Hy, Hypacrosaurus; La, Lambeosaurus; Ni, Nigersaurus; Pr, Prosaurolophus; Sa, Saurolophus; Su, Suuwassea; To, Tornieria.
A Mann-Whitney U test comparing the PMI scores recorded for combined diplodocoid and hadrosaurid “square” (Apatosaurus, Diplodocus, Nigersaurus, and the hadrosaurines) and “round” (Dicraeosaurus, Suuwassea, Tornieria, and the lambeosaurines) groups demonstrates that the two groups can be distinguished (U = 1, P = 0.002). The overall similarity between snout shape in putatively nonselective and selective browsers in both diplodocoids and hadrosaurids suggests that a) PMI is a valid measure of an ecomorphological variable and b) hypotheses of non-selective and selective browsing based on snout shape in diplodocoid sauropods are well-founded.
Although the relationship between wear on molar and incisiform teeth is uncertain, the pattern of variation in wear features between round-snouted (Dicraeosaurus) and square-snouted (Apatosaurus, Diplodocus, Nigersaurus) diplodocoids is quite similar to that expressed in the molariform teeth of mammals. Dicraeosaurus featured larger, coarser features in general, with less orientational consistency than in the square-snouted taxa. These features can be tentatively interpreted as evidence for variation in both browse height and type (e.g., woody vs. herbaceous, high vs. low concentrations of phytoliths/sclerenchyma, selective vs. non-selective).
Dicraeosaurus, Diplodocus, and Nigersaurus all had a large proportion of pits in their microwear features. Nigersaurus had the highest proportion of pits to scratches (2∶1), followed by Dicraeosaurus (1.3∶1) and Diplodocus (1.1∶1); the lowest proportion occurred in the putatively higher-browsing taxon Brachiosaurus (0.7∶1), although the mid-height browser Camarasaurus had a ratio similar to that of Diplodocus and Dicraeosaurus (1.2∶1). The ratio of pits to scratches in Diplodocus may be artificially low; only 96 total features were recovered from two teeth (compared to 414 in Nigersaurus and 403 in Dicraeosaurus). The proportion of those features varies between teeth, such that the first left premaxillary tooth has a pit∶scratch ratio of 0.7∶1, while the second right premaxillary tooth has a ratio of 1.4∶1. Regardless, it is clear that Nigersaurus has a higher proportion of pits to scratches than Dicraeosaurus, which suggests that Nigersaurus ate at a lower browse height (i.e., at ground level). The same is potentially true for Diplodocus, even allowing for the potentially misleading results from the left premaxillary tooth. The similarity in pits-to-scratches ratios in Diplodocus, Camarasaurus and Dicraeosaurus may indicate some overlap in browse height (and indeed, the two categories do overlap as defined here; Table 1), although the distinctly larger features present in Camarasaurus and Dicraeosaurus (see below) suggest that the subcircular features in each taxon had different root causes, most likely different browse types.
Square-snouted diplodocoids Diplodocus and Nigersaurus are characterized by an abundance of fine (breadth <3.5 µm), subparallel scratches; round-snouted taxa such as Camarasaurus and Dicraeosaurus are dominated by coarse (breadth >3.75 µm) scratches, including a large proportion of cross-scratches. Following a significant Kruskal-Wallace result (H = 179.34, d.f. = 4, P = 0.000), pairwise comparisons found that the pairs Diplodocus and Nigersaurus, Diplodocus and Brachiosaurus, and Brachiosaurus and Camarasaurus were indistinguishable from each other (Table 5). This suggests that Diplodocus and Nigersaurus were both primarily browsing on similar foods, although Diplodocus may also have incorporated a small component of hard foods in its diet; such a diet may explain the observed similarity to Brachiosaurus. A diet heavy on silica-accumulating plants may also have caused this; one such plant, Equisetum, is known from the Morrison Formation, and has previously been suggested to form a component of the diet of Diplodocus . Dicraeosaurus, which differed significantly in scratch breadth with all other study taxa, was potentially also a mixed feeder.
The greater orientational consistency in Diplodocus and Nigersaurus suggests that these animals were biting through softer stems, consistent with a hypothesis of browsing on herbaceous plants, such as low-growing ferns. Conversely, the low consistency of scratches in Dicraeosaurus is indicative of harder, more brittle foods, possibly including the shearing of woody stems. The significantly coarser scratches and larger pits/gouges observed Dicraeosaurus also suggest a diet including coarser plants and a large proportion of larger particles than those ingested by Diplodocus and Nigersaurus, and probably Apatosaurus and Rebbachisaurus as well. The larger particles in question may have been hard objects such as seeds; an abundance of such high-quality foodstuffs in the diet indicates selective browsing behavior . Brachiosaurus and Camarasaurus have relatively high orientational consistencies despite the common occurrence of cross-scratches. In those taxa, the higher than expected orientational consistency is likely a function of an interlocking dentition and precise occlusion, two features not seen in diplodocoids.
Pit/gouge size was also found to differ significantly between several of the taxa (H = 229.386, df = 2, P = 0.000). Pairwise comparisons found significant differences in pit/gouge area between Diplodocus and all others and Nigersaurus and all others, but not between Brachiosaurus, Camarasaurus, and Dicraeosaurus (Table 6). Pit/gouge size appears to be able to distinguish between selective and non-selective (or less selective) browsers, although Diplodocus and Nigersaurus, both potentially non-selective browsers as predicted by snout shape, had statistically distinguishable pit/gouge size distributions as well. Average pit size in the two taxa is quite similar (34.6 µm2 in Nigersaurus, 22.7 µm2 in Diplodocus), however, and the next most-similar is substantially larger (Camarasaurus, at 88.4 µm2), suggesting that the perceived difference between pit/gouge size in Diplodocus and Nigersaurus may not be functionally significant.
In addition to their significantly larger size, the features recovered from Camarasaurus, Dicraeosaurus and Brachiosaurus are notably more oblate and gouge-like than the subcircular features recovered from the other taxa. Although the meaning of this shape difference is uncertain, it may be related to physical differences in the particles causing the wear, or to the orientation of the force compressing the particle into the tooth (e.g., meeting the enamel edge obliquely vs. orthogonally). In either case, the shape difference suggests some significant difference in diet or behavior between Dicraeosaurus and the square-snouted diplodocoids, as has been previously suggested .
Comparison with previous results
Fiorillo , , Calvo , and Upchurch and Barrett  previously examined wear features on the teeth of Diplodocus. All studies agree on the dominance of fine, subparallel scratches oriented generally along the labiolingual axis. Neither Fiorillo ,  nor Calvo  recovered pits or gouges. Upchurch and Barrett  did recover large pits, although these were considered larger than those normally produced by grit or phytoliths. These features appear to have been recovered from the dentine of a heavily worn tooth, however , where larger features may be expected. The lack of pits led Fiorillo ,  and Calvo  to suggest an upper-canopy browsing behavior for Diplodocus, which is counter to much of the evidence for ground-level browsing presented more recently , , , . High browsing was also inferred as a possible feeding mechanism for Diplodocus by Upchurch and Barrett , based on macrowear features.
The absence of pits/gouges in most previous studies is somewhat perplexing, given their relative abundance in all teeth examined in this study. Further confusion comes from the overlap in sample between a number of studies: this study, the study of Upchurch and Barrett , and the studies of Fiorillo ,  all examine the same specimen of Diplodocus (CM 11161), but obtain a spectrum of results ranging from a majority of pits (this study), to some pits , to no pits , . As a result, it is unlikely that such biological factors as seasonality are responsible for the differences, at least in those samples that directly overlap. The different patterns of features may be a result of methodology, given the reliance of previous studies on SEM images (at extremely high magnification) as opposed to the use of low-magnification microscopy here. It may also be the result of sample size, as all studies (including the current study) examined relatively few teeth per taxon compared to studies of mammals. The ubiquity of pits in all teeth examined here, their similarity in form among broad-snouted taxa, and their difference in form in the round-snouted Dicraeosaurus, however, all reinforce the validity of the interpretation presented here.
Sereno et al.  examined microwear features on the teeth of Nigersaurus. The results of that study are essentially identical to those presented here, although this study identified a significantly larger number of small pits. Both Sereno et al.  and this work infer a diet based on ground-level browsing of herbaceous plant materials based on the consistent labiolingual orientation of fine scratches on the labial surface of the enamel and a high pit/scratch ratio.
Leaf stripping behavior?
Ryan  suggested that some features of incisor microwear in Gorilla, Pan, and Papio were indicative of leaf-stripping behavior: polished surfaces and a preponderance of subparallel, fine scratches on the apical surface of the incisors. However, the proportion of features (scratches and pits) in the microwear assemblages reported here for sauropods differ from wear produced by leaf-stripping. In all but one sample (left premaxillary tooth 1 of Diplodocus) from the occlusal surface of sauropod teeth, pits outnumber scratches significantly, whereas scratches substantially outnumber pits in each of the samples reported by Ryan . This latter result was suggested to have been a consequence of repeated drawing of plant materials over the enamel surface. In leaf stripping behavior, grit causes striations rather than compressional features (i.e., pits) as seen in wear caused by a bite. Because of the high proportion of pits in the sauropod microwear sampled, leaf stripping behavior is considered to be less plausible than ground-level browsing behavior, although it is noted that leaf stripping and ground-level browsing do leave superficially similar traces on incisiform teeth.
Non-facet microwear features
Features recorded from the non-occlusal surfaces of presumptive ground-level browsing taxa such as Diplodocus and Nigersaurus differ from the features recorded from facets in both taxa. Specifically, larger features are recovered, and those features (particularly scratches) are in a different orientation relative to the tooth, nearly orthogonal to the long axis of the tooth rather than subparallel to it. Because these features are located outside the occlusal surface, it is highly unlikely that they represent wear formed during the bite stroke. The implication, therefore, is that the wear was caused by nearby vegetation, which in turn suggests a dense (perhaps sward-like) growth form for the food resource in question. The orientation of the wear at nearly 90° to the occlusal features may have been the result of vegetation scraping against the labial margin of the upper dentition as the head and neck are moved laterally to obtain the next bite; this would fit with the interpretation of some authors ,  of the long neck as a means to increase the feeding envelope without moving the body. These features may also be have resulted from incidental contact in leaf-stripping behavior, although as noted above that behavior is considered to be less likely. In either case, root causes of such features are poorly constrained and non-facet microwear is unlikely to serve as evidence for feeding behavior at this point in time. Such features were not recorded from the selectively browsing Dicraeosaurus.
Feeding Behavior: Summary
Snout shape and microwear indices suggest the presence of both a ground-level, nonselective browsing behavior and a mid-height (above 1 m), selective browsing behavior in diplodocoid sauropods. Here, feeding behavior is examined in relation to body size, phylogeny, and paleoecology, to determine the influence of each on behavior in diplodocoid sauropods.
Body size and feeding behavior.
Among flagellicaudatans (the group containing Diplodocidae and Dicraeosauridae), selectively browsing taxa had smaller skulls, and were smaller overall, than non-selective browsers , –. The rebbachisaurid Nigersaurus, however, was the most specialized non-selective browser sampled and was of similar size to Dicraeosaurus and Tornieria. Although this rules out the hypothesis that feeding behavior was entirely size-dependent, it does not necessarily mean that there is no relationship between size and behavior. It is possible that above 10–12 meters in body length, selective browsing behavior became untenable as a feeding mode (although this restriction does not appear to apply to upper-canopy feeders like Brachiosaurus and Camarasaurus); non-selective browsing behavior was clearly effective even at small (by sauropod standards) body sizes. Other dinosaurs hypothesized to have been ground- and mid-height selective browsers, such as ceratopsians , heterodontosaurs , lambeosaurines , and stegosaurs  also tended to be small in comparison to sauropods, and even the largest rarely exceeded 12 m in body length , –. It is possible that above this size, handling and forage time for selective browsing exceeded some metabolic threshold when an animal is limited to lower-canopy browse. Selective vs. nonselective browsing strategies do generally scale with body size in mammals , although the degree to which this analogy would be expected to hold for dinosaurs is uncertain. The relationship in mammals is based primarily on increased retention time as a function of increased body (and gut) size in large mammals  and relatively increased metabolic requirements in smaller mammals ; sauropods and other herbivorous dinosaurs often far surpassed the body sizes of even very large mammals , however, and estimates of metabolic rate in dinosaurs are still fraught with uncertainty –. However, the relationship between body size and the relative rarity of high-quality forage in most ecosystems and its associated foraging cost is also documented in mammals , , , providing some evidence for an upper size limit on selective browsing in sauropods. Although macronarian sauropods successfully grew large while selectively browsing in the upper canopy, they also had exclusive dominion over those heights as no other clade of dinosaurian herbivore was able to access those resources .
Within individual diplodocoid clades, feeding behavior was reasonably consistent, although snout shape can be determined for only one rebbachisaurid (Nigersaurus; Fig. 7). However, the diplodocid Tornieria has microwear features and a snout shape most similar to those of the dicraeosaurids Dicraeosaurus and Suuwassea. Because Tornieria is a relatively derived diplodocid , , it appears that the feeding behavior inferred for this taxon is an independent derivation within this lineage, rather than a retained plesiomorphic behavior. This in turn suggests that the behavior was not strictly governed by inheritance, and that some plasticity was possible.
Data suggest that ground-height, non-selective browsing evolved in open, savanna-like environments, whereas selective, mid-height browsing was most common in diplodocoids living in closed environments dominated by mid- and upper-canopy browse. Blue tones indicate data suggestive of ground-height, non-selective browsing; yellow tones indicate data suggestive of mid-height, selective browsing. Inferences for which insufficient data exists are represented in 50% grey tones. Abbreviations: S, savanna type ecosystem; F, forested ecosystem; G, ground-height browser; M, mid-height browser; N, nonselective browser; Sl, selective browser.
The ancestral condition for snout shape in diplodocoids is difficult to determine. Although both diplodocids and rebbachisaurids appear to have square snouts, there is no overwhelming evidence to suggest that this is the original condition for the group as a whole. The ancestral state in Flagellicaudata is equivocal: basal diplodocids have square snouts and basal dicraeosaurids have round snouts. Furthermore, the only rebbachisaurid for which snout shape can be determined (Nigersaurus), is a highly derived taxon that likely does not represent the basal condition for the group. Juvenile Diplodocus have narrow snouts , which may suggest that the square-snouted condition seen in adults is derived from an ancestral round-snoutedness. Outgroup taxa (e.g., macronarians, basal eusauropods) are unequivocally round-snouted, but where, when, and how many times the transition to square-snoutedness occurred in diplodocoidea cannot be said with certainty. If square-snoutedness is taken as the ancestral diplodocoid condition, one origination (at the base of Diplodocoidea) and two reversals (one at the base of Dicraeosauridae, once in Tornieria) are required (three evolutionary steps). If round-snoutedness is basal for sauropods, then at least two originations (once at the base of Diplodocidae and once within Rebbachisauridae) and one reversal (Tornieria) are required (also three steps).
Similar morphological plasticity in other dinosaurian groups (e.g., hadrosaurids) has typically been interpreted in relation to behavior, although often behavior and morphological divergence are correlated with phylogeny , and it can be difficult to tease apart the influences of phylogeny and behavior on morphology. However, as noted above, phylogeny is not a perfect explanation for the diversity of snout shapes seen in diplodocoids. It is likely, then, that this morphological variability was driven in larger part by the browse flora available to these animals.
Herbivory imposes two major constraints on behavior: foraging time and digestive time . Digestive time is a function of the length of the digestive tract and may be loosely interpreted from body size, although soft tissue structures (e.g., the rumen), which are not typically preserved in the fossil record, can substantially impact retention time , . Foraging time, however, can be inferred from skeletal evidence based on models of intake rate. Intake rate has a major influence on feeding behavior in modern herbivores ; which is to say that an organism will attempt to maximize intake rate in a given environment. Broad or square snouts have been demonstrated to maximize intake rate in non-selectively browsing mammals ; a broad snout in selective herbivores decreases intake rate by increasing handling time and minimizing effective bite mass cropped .
Variation in forage quality may also have had some influence on behavior. Two hypotheses in particular, the forage abundance hypothesis (FAH)  and the selective quality hypothesis (SQH) , might be useful in explaining a relationship between ecology and behavior in these sauropods. The FAH suggests that when resources are perceived to be abundant, animals may choose to be more selective; grazing behavior increases when resource levels are low. In this hypothesis, forage abundance is the controlling factor. SQH, conversely, predicts that herbivores are actually less selective when high quality resources are plentiful and homogenously distributed. Under SQH, food quality is the key variable. If the regional ecology can be reconstructed for sauropods, support for one or both of these hypotheses in the feeding behavior may be found.
Although the ecological conditions of Niger during the Aptian-Albian are largely unknown (particularly with regard to flora), the paleoecology of the Late Jurassic Morrison and Tendaguru formations, where the remaining five taxa have been found, is better understood.
The Morrison Formation of North America is dominated by diplodocoid sauropods, in particular the square-snouted diplodocids. Diplodocids (primarily Apatosaurus and Diplodocus) are both the most common sauropod fossils found in these beds and the most widespread, occurring in more localities than any other clade  (n.b., the macronarian Camarasaurus is the most numerous single genus of dinosaur ). Only a single round-snouted diplodocoid taxon (Suuwassea) is known from the Morrison Formation.
Plant fossils from the Morrison include a wide diversity of conifers, ginkophytes, podocarpaceans, ferns, cheirolepidiaceans, and horsetails –. Most recent work suggests that much of the Morrison Formation was an arid to semi-arid savanna-like environment, dominated by ground-height herbaceous browse (e.g., ferns, bryophytes) and low- to mid-height woody shrubs , . Taller browse (primarily conifers; e.g., Pagiophyllum, Podozamites) was restricted to areas near watercourses and isolated pockets, such as that preserved by the Salt Wash member –. It is in these isolated pockets that high-browsing sauropods like Brachiosaurus altithorax are found .
Low browse in the southern Morrison, particularly the ferns and small trees, appears to have been highly nutritious and digestible, on par with extant browse . The abundance of high quality, broadly distributed low browse and the appearance of multiple lineages of non-selectively browsing sauropods fit well with the predictions of the SQH and suggest a relationship between ecology and behavior in the southern Morrison Formation.
The northern end of the Morrison Formation (e.g., Montana) has been recognized for its unusual sauropod fauna, composed of smaller adults and more juveniles than is typical of more southern localities , . Additionally, dicraeosaurids such as Suuwassea and MOR 592 are known exclusively from Montana , . Paleoenvironmental reconstructions of the northern Morrison Formation are also quite different from those of the southern localities. This region was likely to have been a wetter environment than the southern Morrison Formation , , . Morrison Formation sediments found near central Montana are believed to have been deposited in mires, coal swamps and/or peat bogs, and associated riparian environments . Forested habitats have previously been thought to lead to a greater reliance on selective browsing in other dinosaurs  and in modern mammals , . It is probable that the restriction of round-snouted, selectively browsing dicraeosaurids to this type of environment in the Morrison Formation indicates a similar constraint on sauropod dinosaurs. The less homogenous environments of the northern Morrison may have resulted in patches of highly nutritious vegetation, such as Equisetum and the conifer Araucaria ; the increase in selectivity when high-quality resources are restricted matches the predictions of SQH. The relatively high concentration of juvenile diplodocoids in the northern Morrison Formation, with their narrow snouts , is also consistent with this interpretation.
Unlike that of the Morrison, the sauropod fauna of Tendaguru is made up exclusively of round-snouted taxa, including Brachiosaurus, Dicraeosaurus, and Tornieria. The African Brachiosaurus taxon is a much more important component of the fauna compared to its American relative, particularly in the Middle Saurian Beds, where it is the most common sauropod found . The most common fossil sauropod in the Upper Tendaguru is the diplodocid Tornieria, which is rare in the Middle Saurian Beds but common elsewhere . Dicraeosaurus is a minor component of all dinosaur-bearing layers .
The sediments preserved in the Tendaguru Formation encompass both strictly terrestrial uplands and tidal flats/coastal regions, but the latter appear to have been poorly vegetated . In contrast, the uplands seem to have been heavily vegetated by conifer forests, including the very tall araucarians that would have provided a food source for high-browsing sauropods . Also present were evergreen shrubs and small (<25 m) trees in the family Podocarpaceae . Minor components of the flora included cycads and ginkophyte trees. Ferns were exceptionally rare, and only two varieties, either Dicroidium or Pachypteris-type, have been reported from Tendaguru . The uplands of Tendaguru, therefore, were a heterogenous mix of upper-canopy browse dominated by conifers (Cheirolepidiaceae and Araucariaceae) and mid-height woody browse (Podocarpaceae, cycads); comparatively little ground-level bulk forage (ferns) would have been present.
No ground-height, non-selectively browsing sauropod dinosaurs have been recovered from Tendaguru. The sauropods that have been found there are exclusively mid-height (Dicraeosaurus, Tornieria) or upper canopy (Brachiosaurus) feeders, which corresponds well with the recovered vegetation, which is dominated by woody browse. Although cycads and podocarpacean evergreens would have been abundant mid-height browse, they are substantially less nutritious than the ferns, horsetails, and other low browse plants common to the southern Morrison Formation . Here, where high-quality food resources are limited, SQH predicts an increase in selectivity. The lack of evidence for large bodied, non-selective browsers in Tendaguru fits well with this prediction.
Forested habitats that are linked with riparian environments are also associated with round-snouted sauropods in both the Morrison (Brachiosaurus altithorax, Camarasaurus, Suuwassea) and Tendaguru (Brachiosaurus brancai, Dicraeosaurus, Tornieria) Formations. Square-snouted sauropods (Apatosaurus, Diplodocus) are found in the open, savanna-like environment proposed for the southern Morrison Formation, although the round-snouted Camarasaurus is also found in these beds. Evidence suggests that the riparian environments cutting through the savanna-type environments of the Morrison had substantial tree coverage , which could explain the presence of Camarasaurus in those regions. The selective quality hypothesis predicts non-selective browsing when high-quality resources are abundant and broadly distributed and selective browsing when high-quality resources are restricted ; both predictions match the inferences of diplodocoid feeding strategy and floral ecology made for the Morrison and Tendaguru Formations. The general robustness of the relationship between diplodocoid anatomy and paleoecology suggests that square-snoutedness is linked with ground-height, non-selective browsing, and round-snoutedness is associated with mid- to upper-canopy selective browsing (Fig. 7).
Hypotheses of feeding behaviors typical of modern mammalian herbivores (e.g., non-selective and selective browsing) are supported for diplodocoid sauropods using evidence from snout shape and dental microwear. Snout shapes in diplodocoids include both rounded and square snouts, similar to those seen in hadrosaurid dinosaurs. Square snouts have been correlated with non-selective feeding behavior in modern and extinct mammals and in hadrosaurine dinosaurs, whereas round snouts correlate with selective browsing behaviors in those taxa. Dental microwear features indicative of ground-height browsing on herbaceous plants correspond with square snouts in diplodocoid sauropods; microwear features suggestive of mid-height browsing on brittle, potentially woody plants correspond with round snouts.
There is a potential correspondence between body size and feeding behavior in diplodocoids: above 12–15 m body length, diplodocoids are exclusively non-selective, ground-height browsers; small diplodocoids include both selective and non-selective browsers, however. There is probably not a strong phylogenetic signal to morphology and behavior, although most diplodocids (except Tornieria) and rebbachisaurids were ground-height browsers, and dicraeosaurids (and Tornieria) were mid-height-browsers, although potentially restricted to the lower portion of that feeding zone. Feeding behavior corresponds well to environmental associations, such that closed environments dominated by upper-canopy browse lacked the ground-height, nonselective browsers that dominated open environments.
Material examined for cranial reconstructions.
Teeth examined for microwear features. Teeth without position indicated were found isolated.
Complete list of microwear features (including dimensions, area, and type) for all teeth examined.
Jeffrey Wilson, Catherine Badgley, William Fink, and Tomasz Baumiller (UM) provided helpful comments on earlier versions of this paper. Paul Barrett, Andrew Farke, and an anonymous reviewer improved a subsequent draft. Matt Carrano (USNM), Ted Daeschler (ANSP), Nicole Klein (MB), Matt Lamanna (CM), Carl Mehling (AMNH), Paul Sereno (UC), and Phillipe Taquet (MNHN) provided access to specimens. Jeffrey Wilson (UM) provided images of Shunosaurus. Larry Witmer (OU) provided CT data for Corythosaurus, Hypacrosaurus, and Lambeosaurus. Peter Ungar (UA) provided access to the Microware 4.02 software used in this study.
Conceived and designed the experiments: JAW. Performed the experiments: JAW. Analyzed the data: JAW. Contributed reagents/materials/analysis tools: JAW. Wrote the paper: JAW.
- 1. Zardoya R, Meyer A (1998) Complete mitochondrial genome suggests diapsid affinities of turtles. Proceedings of the National Academy of Sciences 95: 14226–14231.R. ZardoyaA. Meyer1998Complete mitochondrial genome suggests diapsid affinities of turtles.Proceedings of the National Academy of Sciences951422614231
- 2. Kumazawa Y, Nishida M (1999) Complete mitochondrial DNA sequences of the green turtle and blue-tailed mole skink: statistical evidence for archosaurian affinity of turtles. Molecular Biology and Evolution 16: 784–792.Y. KumazawaM. Nishida1999Complete mitochondrial DNA sequences of the green turtle and blue-tailed mole skink: statistical evidence for archosaurian affinity of turtles.Molecular Biology and Evolution16784792
- 3. Iwabe N, Hara Y, Kumazawa Y, Shibamoto K, Saito Y, et al. (2005) Sister group relationship of turtles to the bird-crocodilian clade revealed by nuclear DNA-coded proteins. Molecular Biology and Evolution 22: 810–813.N. IwabeY. HaraY. KumazawaK. ShibamotoY. Saito2005Sister group relationship of turtles to the bird-crocodilian clade revealed by nuclear DNA-coded proteins.Molecular Biology and Evolution22810813
- 4. Lovelace DM, Hartman SA, Wahl WR (2008) Morphology of a specimen of Supersaurus (Dinosauria, Sauropoda) from the Morrison Formation of Wyoming, and a re-evaluation of diplodocid phylogeny. Arquivos do Museu Nacional, Rio de Janeiro 65: 527–544.DM LovelaceSA HartmanWR Wahl2008Morphology of a specimen of Supersaurus (Dinosauria, Sauropoda) from the Morrison Formation of Wyoming, and a re-evaluation of diplodocid phylogeny.Arquivos do Museu Nacional, Rio de Janeiro65527544
- 5. Weaver JC (1983) The improbable endotherm: The energetics of the sauropod dinosaur Brachiosaurus. Paleobiology 9: 173–182.JC Weaver1983The improbable endotherm: The energetics of the sauropod dinosaur Brachiosaurus.Paleobiology9173182
- 6. Curry KA (1999) Ontogenetic histology of Apatosaurus (Dinosauria: Sauropoda): new insights on growth rates and longevity. Journal of Vertebrate Paleontology 19: 654–665.KA Curry1999Ontogenetic histology of Apatosaurus (Dinosauria: Sauropoda): new insights on growth rates and longevity.Journal of Vertebrate Paleontology19654665
- 7. Lehman TM, Woodward HN (2008) Modeling growth rates for sauropod dinosaurs. Paleobiology 34: 264–281.TM LehmanHN Woodward2008Modeling growth rates for sauropod dinosaurs.Paleobiology34264281
- 8. Lockley MG (1991) Tracking dinosaurs. Cambridge: Cambridge University Press. 238 p.MG Lockley1991Tracking dinosaursCambridgeCambridge University Press238
- 9. Chure DJ, Britt BB, Whitlock JA, Wilson JA (2010) First complete sauropod dinosaur skull from the Cretaceous of the Americas and the evolution of sauropod dentition. Naturwissenschaften 97: 379–391.DJ ChureBB BrittJA WhitlockJA Wilson2010First complete sauropod dinosaur skull from the Cretaceous of the Americas and the evolution of sauropod dentition.Naturwissenschaften97379391
- 10. Sereno PC, Wilson JA, Witmer LM, Whitlock JA, Maga A, et al. (2007) Structural extremes in a Cretaceous dinosaur. PLoS ONE 2: e1230.PC SerenoJA WilsonLM WitmerJA WhitlockA. Maga2007Structural extremes in a Cretaceous dinosaur.PLoS ONE2e1230
- 11. Whitlock JA, D'Emic MD, Fisher DC, Smith K, Wilson JA (2010) Trends in sauropod tooth size, shape, and replacement rate. Journal of Vertebrate Paleontology 30: supplement to 3186A.JA WhitlockMD D'EmicDC FisherK. SmithJA Wilson2010Trends in sauropod tooth size, shape, and replacement rate.Journal of Vertebrate Paleontology30supplement to 3186A
- 12. Erickson GM (1996) Incremental lines of von Ebner in dinosaurs and the assessment of tooth replacement rates using growth line counts. Proceedings of the National Academy of Sciences 93: 14623–14627.GM Erickson1996Incremental lines of von Ebner in dinosaurs and the assessment of tooth replacement rates using growth line counts.Proceedings of the National Academy of Sciences931462314627
- 13. Sereno PC, Wilson JA (2005) Structure and evolution of a sauropod tooth battery. In: Curry Rogers KA, Wilson JA, editors. The sauropods: evolution and paleobiology. Berkeley: University of California Press. pp. 157–177.PC SerenoJA Wilson2005Structure and evolution of a sauropod tooth battery.KA Curry RogersJA WilsonThe sauropods: evolution and paleobiologyBerkeleyUniversity of California Press157177
- 14. Hatcher JB (1901) Diplodocus (Marsh): its osteology, taxonomy, and probable habits, with a restoration of the skeleton. Memoirs of the Carnegie Museum 1: 1–63.JB Hatcher1901Diplodocus (Marsh): its osteology, taxonomy, and probable habits, with a restoration of the skeleton.Memoirs of the Carnegie Museum1163
- 15. Holland WJ (1924) The skull of Diplodocus. Memoirs of the Carnegie Museum 9: 379–403.WJ Holland1924The skull of Diplodocus.Memoirs of the Carnegie Museum9379403
- 16. Holland WJ (1906) The osteology of Diplodocus Marsh. Memoirs of the Carnegie Museum 2: 225–264.WJ Holland1906The osteology of Diplodocus Marsh.Memoirs of the Carnegie Museum2225264
- 17. Hay OP (1908) On the habits and the pose of the sauropodous dinosaurs, especially of Diplodocus. The American Naturalist 42: 672–681.OP Hay1908On the habits and the pose of the sauropodous dinosaurs, especially of Diplodocus.The American Naturalist42672681
- 18. Tornier G (1911) Bau und Lebensweise des Diplodokus. Bericht der Senckenbergischen Naturforschenden Gesellschaft 42: 112–114.G. Tornier1911Bau und Lebensweise des Diplodokus.Bericht der Senckenbergischen Naturforschenden Gesellschaft42112114
- 19. Coombs WP (1975) Sauropod habits and habitats. Palaeogeography, Palaeoclimatology, Palaeoecology 17: 1–33.WP Coombs1975Sauropod habits and habitats.Palaeogeography, Palaeoclimatology, Palaeoecology17133
- 20. Bakker RT (1986) The dinosaur heresies. New York: Kensington Press. 481 p.RT Bakker1986The dinosaur heresiesNew YorkKensington Press481
- 21. Dodson P (1990) Sauropod paleoecology. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, First Edition. Berkeley: University of California Press. pp. 402–407.P. Dodson1990Sauropod paleoecology.DB WeishampelP. DodsonH. OsmólskaThe Dinosauria, First EditionBerkeleyUniversity of California Press402407
- 22. Fiorillo AR (1991) Dental microwear on the teeth of Camarasaurus and Diplodocus: implications for sauropod paleoecology. In: Kielan-Jaworowska Z, Heintz N, Nakrem H, editors. Fifth symposium on Mesozoic terrestrial ecosystems and biota. Oslo: Paleontological Museum, University of Oslo. pp. 23–24.AR Fiorillo1991Dental microwear on the teeth of Camarasaurus and Diplodocus: implications for sauropod paleoecology.Z. Kielan-JaworowskaN. HeintzH. NakremFifth symposium on Mesozoic terrestrial ecosystems and biotaOsloPaleontological Museum, University of Oslo2324
- 23. Fiorillo AR (1998) Dental microwear patterns of the sauropod dinosaurs Camarasaurus and Diplodocus: evidence for resource partitioning in the Late Jurassic of North America. Historical Biology 13: 1–16.AR Fiorillo1998Dental microwear patterns of the sauropod dinosaurs Camarasaurus and Diplodocus: evidence for resource partitioning in the Late Jurassic of North America.Historical Biology13116
- 24. Barrett PM, Upchurch P (1994) Feeding mechanisms of Diplodocus. Gaia 10: 195–203.PM BarrettP. Upchurch1994Feeding mechanisms of Diplodocus.Gaia10195203
- 25. Barrett PM, Upchurch P (2005) Sauropodomorph diversity through time: paleoecological and macroevolutionary implications. In: Wilson JA, Curry Rogers KA, editors. The sauropods: evolution and paleobiology. Berkeley: University of California Press. pp. 125–152.PM BarrettP. Upchurch2005Sauropodomorph diversity through time: paleoecological and macroevolutionary implications.JA WilsonKA Curry RogersThe sauropods: evolution and paleobiologyBerkeleyUniversity of California Press125152
- 26. Calvo J (1994) Jaw mechanics in sauropod dinosaurs. Gaia 10: 183–193.J. Calvo1994Jaw mechanics in sauropod dinosaurs.Gaia10183193
- 27. Stevens KA, Parrish JM (1999) Neck posture and feeding habits of two Jurassic sauropod dinosaurs. Science 284: 798–800.KA StevensJM Parrish1999Neck posture and feeding habits of two Jurassic sauropod dinosaurs.Science284798800
- 28. Stevens KA, Parrish JM (2005) Neck posture, dentition, and feeding strategies in Jurassic sauropod dinosaurs. In: Tidwell V, Carpenter K, editors. Thunder-lizards: the sauropodomorph dinosaurs. Bloomington: Indiana University Press. pp. 212–232.KA StevensJM Parrish2005Neck posture, dentition, and feeding strategies in Jurassic sauropod dinosaurs.V. TidwellK. CarpenterThunder-lizards: the sauropodomorph dinosaursBloomingtonIndiana University Press212232
- 29. Christiansen P (2000) Feeding mechanisms of the sauropod dinosaurs Brachiosaurus, Camarasaurus, Diplodocus, and Dicraeosaurus. Historical Biology 14: 137–152.P. Christiansen2000Feeding mechanisms of the sauropod dinosaurs Brachiosaurus, Camarasaurus, Diplodocus, and Dicraeosaurus.Historical Biology14137152
- 30. Upchurch P, Barrett PM (2000) The evolution of sauropod feeding mechanisms. In: Sues H-D, editor. Evolution of herbivory in terrestrial vertebrates: perspectives from the fossil record. Cambridge: Cambridge University Press. pp. 79–122.P. UpchurchPM Barrett2000The evolution of sauropod feeding mechanisms.H-D SuesEvolution of herbivory in terrestrial vertebrates: perspectives from the fossil recordCambridgeCambridge University Press79122
- 31. Barrett PM, Willis KJ (2001) Did dinosaurs invent flowers? Dinosaur-angiosperm coevolution revisited. Biological Reviews of the Cambridge Philosophical Society 76: 411–447.PM BarrettKJ Willis2001Did dinosaurs invent flowers? Dinosaur-angiosperm coevolution revisited.Biological Reviews of the Cambridge Philosophical Society76411447
- 32. Whitlock JA, Wilson JA, Lamanna MC (2010) Description of a nearly complete juvenile skull of Diplodocus (Sauropoda: Diplodocoidea) from the Late Jurassic of North America. Journal of Vertebrate Paleontology 30: 442–457.JA WhitlockJA WilsonMC Lamanna2010Description of a nearly complete juvenile skull of Diplodocus (Sauropoda: Diplodocoidea) from the Late Jurassic of North America.Journal of Vertebrate Paleontology30442457
- 33. Osborn HF (1899) A skeleton of Diplodocus. Memoirs of the American Museum of Natural History 1: 189–214.HF Osborn1899A skeleton of Diplodocus.Memoirs of the American Museum of Natural History1189214
- 34. Wilson JA, Sereno PC (1998) Early evolution and higher-level phylogeny of sauropod dinosaurs. Society of Vertebrate Paleontology Memoir 5: 1–68.JA WilsonPC Sereno1998Early evolution and higher-level phylogeny of sauropod dinosaurs.Society of Vertebrate Paleontology Memoir5168
- 35. Boué C (1970) Morphologie fonctionnelle des dents labiales chez les ruminants. Mammalia 34: 696–711.C. Boué1970Morphologie fonctionnelle des dents labiales chez les ruminants.Mammalia34696711
- 36. Bell RH (1971) A grazing ecosystem in the Serengeti. Scientific American 224: 86–93.RH Bell1971A grazing ecosystem in the Serengeti.Scientific American2248693
- 37. Owen-Smith N (1979) Assessing the foraging efficiency of a large herbivore, the kudu. South African Journal of Wildlife Research 9: 102–110.N. Owen-Smith1979Assessing the foraging efficiency of a large herbivore, the kudu.South African Journal of Wildlife Research9102110
- 38. Bunnell FL, Gillingham MP (1985) Foraging behavior: dynamics of dining out. In: Hudson RJ, White RG, editors. Bioenergetics of wild herbivores. Boca Raton: CRC Press. pp. 53–80.FL BunnellMP Gillingham1985Foraging behavior: dynamics of dining out.RJ HudsonRG WhiteBioenergetics of wild herbivoresBoca RatonCRC Press5380
- 39. Janis CM, D E (1988) Correlation of relative muzzle width and relative incisor width with dietary preference in ungulates. Zoological Journal of the Linnean Society 92: 267–284.CM JanisE. D1988Correlation of relative muzzle width and relative incisor width with dietary preference in ungulates.Zoological Journal of the Linnean Society92267284
- 40. Gordon IJ, Illius AW (1988) Incisor arcade structure and its selection in ruminants. Functional Ecology 2: 15–22.IJ GordonAW Illius1988Incisor arcade structure and its selection in ruminants.Functional Ecology21522
- 41. Solounias N, Teaford M, Walker A (1988) Interpreting the diet of extinct ruminants: the case of a non-browsing giraffid. Paleobiology 14: 287–300.N. SolouniasM. TeafordA. Walker1988Interpreting the diet of extinct ruminants: the case of a non-browsing giraffid.Paleobiology14287300
- 42. Solounias N, Moelleken S (1993) Dietary adaptation of some extinct ruminants determined by premaxillary shape. Journal of Mammology 74: 1059–1071.N. SolouniasS. Moelleken1993Dietary adaptation of some extinct ruminants determined by premaxillary shape.Journal of Mammology7410591071
- 43. Walker A (1984) Extinction in hominid evolution. In: Nitecki MH, editor. Extinctions. Chicago: University of Chicago Press. pp. 119–152.A. Walker1984Extinction in hominid evolution.MH NiteckiExtinctionsChicagoUniversity of Chicago Press119152
- 44. Dompierre H, Churcher CS (1996) Premaxillary shape as an indicator of the diet of seven extinct late Cenozoic new world camels. Journal of Vertebrate Paleontology 16: 141–148.H. DompierreCS Churcher1996Premaxillary shape as an indicator of the diet of seven extinct late Cenozoic new world camels.Journal of Vertebrate Paleontology16141148
- 45. Christiansen P (1999) On the head size of sauropodomorph dinosaurs: implications from ecology and physiology. Historical Biology 13: 269–297.P. Christiansen1999On the head size of sauropodomorph dinosaurs: implications from ecology and physiology.Historical Biology13269297
- 46. Carrano MT, Janis CM, Sepkoski JJ Jr (1999) Hadrosaurs as ungulate parallels: lost lifestyles and deficient data. Acta Palaeontologica Polonica 44: 237–261.MT CarranoCM JanisJJ Sepkoski Jr1999Hadrosaurs as ungulate parallels: lost lifestyles and deficient data.Acta Palaeontologica Polonica44237261
- 47. Dodson P, Forster CA, Sampson SD (2004) Ceratopsidae. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, Second Edition. Berkeley: University of California Press. pp. 494–513.P. DodsonCA ForsterSD Sampson2004Ceratopsidae.DB WeishampelP. DodsonH. OsmólskaThe Dinosauria, Second EditionBerkeleyUniversity of California Press494513
- 48. Barrett PM (2001) Tooth wear and possible jaw action of Scelidosaurus harrisonii Owen and a review of feeding mechanisms in other thyreophoran dinosaurs. In: Carpenter K, editor. The armored dinosaurs. Bloomington: Indiana University Press. pp. 25–52.PM Barrett2001Tooth wear and possible jaw action of Scelidosaurus harrisonii Owen and a review of feeding mechanisms in other thyreophoran dinosaurs.K. CarpenterThe armored dinosaursBloomingtonIndiana University Press2552
- 49. Carpenter K (1982) Skeletal and dermal armor reconstructions of Euoplocephalus tutus (Ornithischia: Ankylosauridae) from the Late Cretaceous Oldman Formation of Alberta. Canadian Journal of Earth Sciences 19: 689–697.K. Carpenter1982Skeletal and dermal armor reconstructions of Euoplocephalus tutus (Ornithischia: Ankylosauridae) from the Late Cretaceous Oldman Formation of Alberta.Canadian Journal of Earth Sciences19689697
- 50. Gunga H-C, Kirsch K, Rittweger J, Röcker L, Clarke A, et al. (1999) Body size and body volume distribution in two sauropods from the Upper Jurassic of Tendaguru (Tanzania). Mitteilungen aus dem Museum für Naturkunde in Berlin Geowissenschaftliche Reihe 2: 91–102.H-C GungaK. KirschJ. RittwegerL. RöckerA. Clarke1999Body size and body volume distribution in two sauropods from the Upper Jurassic of Tendaguru (Tanzania).Mitteilungen aus dem Museum für Naturkunde in Berlin Geowissenschaftliche Reihe291102
- 51. Gunga H-C, Suthau T, Bellmann A, Stoinski S, Friedrich A, et al. (2008) A new body mass estimation of Brachiosaurus brancai Janensch, 1914 mounted and exhibited at the Museum of Natural History (Berlin, Germany). Fossil Record 11: 33–38.H-C GungaT. SuthauA. BellmannS. StoinskiA. Friedrich2008A new body mass estimation of Brachiosaurus brancai Janensch, 1914 mounted and exhibited at the Museum of Natural History (Berlin, Germany).Fossil Record113338
- 52. Bates KT, Manning PL, Hodgetts D, Sellers WI (2009) Estimating mass properties of dinosaurs using laser imaging and 3D computer modelling. PLoS ONE 4(2): e4532.KT BatesPL ManningD. HodgettsWI Sellers2009Estimating mass properties of dinosaurs using laser imaging and 3D computer modelling.PLoS ONE42e4532
- 53. Sereno PC, Beck AL, Dutheil DB, Larssen HCE, Lyon GH, et al. (1999) Cretaceous sauropods from the Sahara and the uneven rate of skeletal evolution among dinosaurs. Science 286: 1342–1347.PC SerenoAL BeckDB DutheilHCE LarssenGH Lyon1999Cretaceous sauropods from the Sahara and the uneven rate of skeletal evolution among dinosaurs.Science28613421347
- 54. Nelson S, Badgley C, Zakem E (2005) Microwear in modern squirrels in relation to diet. Palaeontologia Electronica 8(3), 14A: 1–15.S. NelsonC. BadgleyE. Zakem2005Microwear in modern squirrels in relation to diet.Palaeontologia Electronica8(3), 14A115
- 55. Puech P, Cianfarani F, Albertini H (1986) Dental microwear features as an indicator for plant food in early hominids: a preliminary study of enamel. Human Evolution 1: 507–515.P. PuechF. CianfaraniH. Albertini1986Dental microwear features as an indicator for plant food in early hominids: a preliminary study of enamel.Human Evolution1507515
- 56. Solounias N, Semprebon G (2002) Advances in the reconstruction of ungulate ecomorphology with application to early fossil equids. American Museum Novitates 3366: 1–49.N. SolouniasG. Semprebon2002Advances in the reconstruction of ungulate ecomorphology with application to early fossil equids.American Museum Novitates3366149
- 57. Anyonge W (1996) Microwear on canines and killing behavior in large carnivores: saber function in Smilodon fatalis. Journal of Mammology 77: 1059–1067.W. Anyonge1996Microwear on canines and killing behavior in large carnivores: saber function in Smilodon fatalis.Journal of Mammology7710591067
- 58. Merceron G, Blondel C, de Bonis L, Koufos GD, Viriot L (2005) A new method of dental microwear analysis: application to extant primates and Ouranopithecus macedoniensis (Late Miocene of Greece). Palaios 20: 551–561.G. MerceronC. BlondelL. de BonisGD KoufosL. Viriot2005A new method of dental microwear analysis: application to extant primates and Ouranopithecus macedoniensis (Late Miocene of Greece).Palaios20551561
- 59. Merceron G, Blondel C, Viriot L, Koufos GD, de Bonis L (2007) Dental microwear analysis of bovids from the Vallesian (late Miocene) of Axios Valley in Greece: reconstruction of the habitat of Ouranopithecus macedoniensis (Primates, Hominoidea). Geodiversitas 29: 421–433.G. MerceronC. BlondelL. ViriotGD KoufosL. de Bonis2007Dental microwear analysis of bovids from the Vallesian (late Miocene) of Axios Valley in Greece: reconstruction of the habitat of Ouranopithecus macedoniensis (Primates, Hominoidea).Geodiversitas29421433
- 60. Townsend KEB, Croft DA (2008) Enamel microwear in caviomorph rodents. Journal of Mammology 89: 730–743.KEB TownsendDA Croft2008Enamel microwear in caviomorph rodents.Journal of Mammology89730743
- 61. Goswami A, Flynn JJ, Ranivoharimanana L, Wyss AR (2005) Dental microwear in Triassic amniotes: implications for paleoecology and masticatory mechanics. Journal of Vertebrate Paleontology 25: 320–329.A. GoswamiJJ FlynnL. RanivoharimananaAR Wyss2005Dental microwear in Triassic amniotes: implications for paleoecology and masticatory mechanics.Journal of Vertebrate Paleontology25320329
- 62. Williams VS, Barrett PM, Purnell MA (2009) Quantitative analysis of dental microwear in hadrosaurid dinosaurs, and the implications for hypotheses of jaw mechanics and feeding. Proceedings of the National Academy of Sciences 106: 11194–11199.VS WilliamsPM BarrettMA Purnell2009Quantitative analysis of dental microwear in hadrosaurid dinosaurs, and the implications for hypotheses of jaw mechanics and feeding.Proceedings of the National Academy of Sciences1061119411199
- 63. García RA, Cerda IA (2010) Dentición de titanosaurios (Dinosauria, Sauropoda) del Cretácico Superior de la provincia de Río Negro, Argentina: morfología, inserción y reemplazo. Ameghiniana 47: 45–60.RA GarcíaIA Cerda2010Dentición de titanosaurios (Dinosauria, Sauropoda) del Cretácico Superior de la provincia de Río Negro, Argentina: morfología, inserción y reemplazo.Ameghiniana474560
- 64. Rybczynski N, Vickaryous MK (2001) Evidence of complex jaw movement in the Late Cretaceous ankylosaurid Euoplocephalus tutus (Dinosauria: Thyreophora). In: Carpenter K, editor. The armored dinosaurs. Bloomington: Indiana University Press. pp. 299–317.N. RybczynskiMK Vickaryous2001Evidence of complex jaw movement in the Late Cretaceous ankylosaurid Euoplocephalus tutus (Dinosauria: Thyreophora).K. CarpenterThe armored dinosaursBloomingtonIndiana University Press299317
- 65. Purnell MA, Hart PJB, Baines DC, Bell MA (2006) Quantitative analysis of dental microwear in threespine stickleback: a new approach to analysis of trophic ecology in aquatic vertebrates. Journal of Animal Ecology 75: 967–977.MA PurnellPJB HartDC BainesMA Bell2006Quantitative analysis of dental microwear in threespine stickleback: a new approach to analysis of trophic ecology in aquatic vertebrates.Journal of Animal Ecology75967977
- 66. Purnell MA, Bell MA, Baines DC, Hart PJB, Travis MP (2007) Correlated evolution and dietary change in fossil stickleback. Science 317: 1887.MA PurnellMA BellDC BainesPJB HartMP Travis2007Correlated evolution and dietary change in fossil stickleback.Science3171887
- 67. Young WG, Marty TM (1986) Wear and microwear on the teeth of a moose (Alces alces) population in Manitoba, Canada. Canadian Journal of Zoology 64: 2467–2479.WG YoungTM Marty1986Wear and microwear on the teeth of a moose (Alces alces) population in Manitoba, Canada.Canadian Journal of Zoology6424672479
- 68. Young WG, Stephens M, Juff R (1990) Tooth wear and enamel structure in the mandibular incisors of six species of kangaroo (Marsupialia: Macropodinae). Memoirs of the Queensland Museum 28: 337–347.WG YoungM. StephensR. Juff1990Tooth wear and enamel structure in the mandibular incisors of six species of kangaroo (Marsupialia: Macropodinae).Memoirs of the Queensland Museum28337347
- 69. Domning DP, Beatty BL (2007) Use of tusks in feeding by dugongid sirenians: observations and tests of hypothesis. The Anatomical Record 290: 523–538.DP DomningBL Beatty2007Use of tusks in feeding by dugongid sirenians: observations and tests of hypothesis.The Anatomical Record290523538
- 70. Rivals F, Semprebon GM (2010) What can incisor microwear reveal about the diet of ungulates? Mammalia 74: 401–406.F. RivalsGM Semprebon2010What can incisor microwear reveal about the diet of ungulates?Mammalia74401406
- 71. Ungar PS (1990) Incisor microwear and feeding behavior in Alouatta seniculus and Cebus olivaceus. American Journal of Primatology 20: 43–50.PS Ungar1990Incisor microwear and feeding behavior in Alouatta seniculus and Cebus olivaceus.American Journal of Primatology204350
- 72. Ungar PS (1994) Incisor microwear of Sumatran anthropoid primates. American Journal of Physical Anthropology 94: 339–363.PS Ungar1994Incisor microwear of Sumatran anthropoid primates.American Journal of Physical Anthropology94339363
- 73. Ungar PS, Spencer MA (1999) Incisor microwear, diet, and tooth use in three Amerindian populations. American Journal of Physical Anthropology 109: 387–396.PS UngarMA Spencer1999Incisor microwear, diet, and tooth use in three Amerindian populations.American Journal of Physical Anthropology109387396
- 74. Kelley J (1990) Incisor microwear and diet in three species of Colobus. Folia Primatologica 55: 73–84.J. Kelley1990Incisor microwear and diet in three species of Colobus.Folia Primatologica557384
- 75. Ryan AS (1981) Anterior dental microwear and its relationship to diet and feeding behavior in three African primates (Pan troglodytes troglodytes, Gorilla gorilla gorilla, and Papio hamadryas). Primates 22: 533–550.AS Ryan1981Anterior dental microwear and its relationship to diet and feeding behavior in three African primates (Pan troglodytes troglodytes, Gorilla gorilla gorilla, and Papio hamadryas).Primates22533550
- 76. Walker PL (1976) Wear striations on the incisors of ceropithecid monkeys as an index of diet and habitat preference. American Journal of Physical Anthropology 45: 299–308.PL Walker1976Wear striations on the incisors of ceropithecid monkeys as an index of diet and habitat preference.American Journal of Physical Anthropology45299308
- 77. Ungar PS (1998) Dental allometry, morphology, and wear as evidence for diet in fossil primates. Evolutionary Anthropology 6: 205–217.PS Ungar1998Dental allometry, morphology, and wear as evidence for diet in fossil primates.Evolutionary Anthropology6205217
- 78. Mazumdar J (2011) Phytoliths of pteridophytes. South African Journal of Botany 77: 10–19.J. Mazumdar2011Phytoliths of pteridophytes.South African Journal of Botany771019
- 79. Hodson MJ, White PJ, Mead A, Broadley MR (2005) Phylogenetic variation in the silicon composition of plants. Annals of Botany 96: 1027–1046.MJ HodsonPJ WhiteA. MeadMR Broadley2005Phylogenetic variation in the silicon composition of plants.Annals of Botany9610271046
- 80. Hummel J, Gee CT, Südekum K-H, Sander PM, Nogge G, et al. (2008) In vitro digestibility of fern and gymnosperm foliage: implications for sauropod feeding ecology and diet selection. Proceedings of the Royal Society of London B 275: 1015–1021.J. HummelCT GeeK-H SüdekumPM SanderG. Nogge2008In vitro digestibility of fern and gymnosperm foliage: implications for sauropod feeding ecology and diet selection.Proceedings of the Royal Society of London B27510151021
- 81. Sereno P, Zijin Z, Lin T (2010) A new psittacosaur from Inner Mongolia and the parrot-like structure and function of the psittacosaur skull. Proceedings of the Royal Society B 277: 199–209.P. SerenoZ. ZijinT. Lin2010A new psittacosaur from Inner Mongolia and the parrot-like structure and function of the psittacosaur skull.Proceedings of the Royal Society B277199209
- 82. Norman DB, Weishampel DB (1991) Feeding mechanisms in some small herbivorous dinosaurs: proceses and patterns. In: Rayner JMV, Wooton RJ, editors. Biomechanics and evolution. Cambridge: Cambridge University Press. pp. 161–181.DB NormanDB Weishampel1991Feeding mechanisms in some small herbivorous dinosaurs: proceses and patterns.JMV RaynerRJ WootonBiomechanics and evolutionCambridgeCambridge University Press161181
- 83. Reilly SM, McBrayer LD, White TD (2001) Prey processing in amniotes: biomechanical and behavioral patterns of food reduction. Comparative Biochemistry and Physiology Part A 128: 397–415.SM ReillyLD McBrayerTD White2001Prey processing in amniotes: biomechanical and behavioral patterns of food reduction.Comparative Biochemistry and Physiology Part A128397415
- 84. Sereno PC (1986) Phylogeny of the bird-hipped dinosaurs (Order Ornithischia). National Geographic Research 2: 234–256.PC Sereno1986Phylogeny of the bird-hipped dinosaurs (Order Ornithischia).National Geographic Research2234256
- 85. Thorington RWJ, Darrow K (1996) Jaw muscles of Old World squirrels. Journal of Morphology 230: 145–165.RWJ ThoringtonK. Darrow1996Jaw muscles of Old World squirrels.Journal of Morphology230145165
- 86. Hiiemäe KM, Ardran GM (1968) A cineflourographic study of mandibular movement during feeding in the rat (Rattus norvegicus). Journal of Zoology 154: 139–154.KM HiiemäeGM Ardran1968A cineflourographic study of mandibular movement during feeding in the rat (Rattus norvegicus).Journal of Zoology154139154
- 87. Prasad V, Strömberg CAE, Alimohammadian H, Sahni A (2005) Dinosaur coprolites and the early evolution of grasses and grazers. Science 310: 1177–1180.V. PrasadCAE StrömbergH. AlimohammadianA. Sahni2005Dinosaur coprolites and the early evolution of grasses and grazers.Science31011771180
- 88. Mainland IL (2003) Dental microwear in grazing and browsing Gotland sheep (Ovis aries) and its implications for dietary reconstruction. Journal of Archaelogical Science 30: 1513–1527.IL Mainland2003Dental microwear in grazing and browsing Gotland sheep (Ovis aries) and its implications for dietary reconstruction.Journal of Archaelogical Science3015131527
- 89. Sanson GD, Kerr SA, Gross KA (2007) Do silica phytoliths really wear mammalian teeth? Journal of Archaelogical Science 34: 526–531.GD SansonSA KerrKA Gross2007Do silica phytoliths really wear mammalian teeth?Journal of Archaelogical Science34526531
- 90. DeMiguel D, Fortelius M, Azanza B, Morales J (2008) Ancestral feeding state of ruminants reconsidered: earliest grazing adaptation claims a mixed condition for Cervidae. BMC Evolutionary Biology 13: 1–13.D. DeMiguelM. ForteliusB. AzanzaJ. Morales2008Ancestral feeding state of ruminants reconsidered: earliest grazing adaptation claims a mixed condition for Cervidae.BMC Evolutionary Biology13113
- 91. Hoffman J, Clementz MT (2008) The effects of exogenous grit on the microwear of extant ungulates and the implications for paleodiet interpretations. Journal of Vertebrate Paleontology 28: supplement to 392A.J. HoffmanMT Clementz2008The effects of exogenous grit on the microwear of extant ungulates and the implications for paleodiet interpretations.Journal of Vertebrate Paleontology28supplement to 392A
- 92. Ungar PS (1996) Dental microwear of European Miocene catarrhines: evidence for diets and tooth use. Journal of Human Evolution 31: 335–366.PS Ungar1996Dental microwear of European Miocene catarrhines: evidence for diets and tooth use.Journal of Human Evolution31335366
- 93. Van Valkenburgh B, Teaford MF, Walker A (1990) Molar microwear and diet in large carnivores: inferences concerning diet in the sabretooth cat, Smilodon fatalis. Journal of Zoology 222: 319–340.B. Van ValkenburghMF TeafordA. Walker1990Molar microwear and diet in large carnivores: inferences concerning diet in the sabretooth cat, Smilodon fatalis.Journal of Zoology222319340
- 94. Grine FE (1986) Dental evidence for dietary differences in Australopithecus and Paranthropus. Journal of Human Evolution 15: 783–822.FE Grine1986Dental evidence for dietary differences in Australopithecus and Paranthropus.Journal of Human Evolution15783822
- 95. Hiiemäe KM, Crompton AW (1985) Mastication, food transport, and swallowing. In: Hildebrand M, Bramble DM, Liem KF, Wake DB, editors. Functional vertebrate morphology. Cambridge: Harvard University Press. pp. 262–290.KM HiiemäeAW Crompton1985Mastication, food transport, and swallowing.M. HildebrandDM BrambleKF LiemDB WakeFunctional vertebrate morphologyCambridgeHarvard University Press262290
- 96. Schubert BW, Ungar PS, DeSantis LRG (2010) Carnassial microwear and dietary behaviour in large carnivorans. Journal of Zoology 280: 257–263.BW SchubertPS UngarLRG DeSantis2010Carnassial microwear and dietary behaviour in large carnivorans.Journal of Zoology280257263
- 97. Sereno PC, Beck AL, Dutheil DB, Larsson HCE, Lyon GH, et al. (1999) Cretaceous sauropods from the Sahara and the uneven rate of skeletal evolution among dinosaurs. Science 286: 1342–1347.PC SerenoAL BeckDB DutheilHCE LarssonGH Lyon1999Cretaceous sauropods from the Sahara and the uneven rate of skeletal evolution among dinosaurs.Science28613421347
- 98. Russell DA, Zheng Z (1993) A large mamenchisaurid from the Junggar Basin, Xinjiang, People's Republic of China. Canadian Journal of Earth Sciences 30: 2082–2095.DA RussellZ. Zheng1993A large mamenchisaurid from the Junggar Basin, Xinjiang, People's Republic of China.Canadian Journal of Earth Sciences3020822095
- 99. Teaford MF (1988) A review of dental microwear and diet in modern mammals. Scanning Microscopy 2: 1149–1166.MF Teaford1988A review of dental microwear and diet in modern mammals.Scanning Microscopy211491166
- 100. Ungar PS (2002) Microware 4.02. Fayetteville: The University of Arkansas. PS Ungar2002Microware 4.02FayettevilleThe University of Arkansas
- 101. Mihlbachler M, Beatty BL, Caldera-Siu A, Chan D, Lee R (2010) Exploring the influence of observer bias in dental microwear analysis. Journal of Vertebrate Paleontology 30: supplement to 3134A.M. MihlbachlerBL BeattyA. Caldera-SiuD. ChanR. Lee2010Exploring the influence of observer bias in dental microwear analysis.Journal of Vertebrate Paleontology30supplement to 3134A
- 102. Dunn OJ (1964) Multiple comparisons using rank sums. Technometrics 6: 241–252.OJ Dunn1964Multiple comparisons using rank sums.Technometrics6241252
- 103. Whitlock JAA phylogenetic analysis of the Diplodocoidea (Saurischia: Sauropoda). Zoological Journal of the Linnean Society. JA WhitlockA phylogenetic analysis of the Diplodocoidea (Saurischia: Sauropoda).Zoological Journal of the Linnean SocietyIn press. In press.
- 104. Christian A, Dzemski G (2007) Reconstruction of the cervical skeleton posture of Brachiosaurus brancai Janensch, 1914 by an analysis of the intervertebral stress along the neck and a comparison with the results of different approaches. Fossil Record 10: 38–49.A. ChristianG. Dzemski2007Reconstruction of the cervical skeleton posture of Brachiosaurus brancai Janensch, 1914 by an analysis of the intervertebral stress along the neck and a comparison with the results of different approaches.Fossil Record103849
- 105. Christian ASome sauropods raised their necks–evidence for high browsing in Euhelopus zdanskyi. Biology Letters. A. ChristianSome sauropods raised their necks–evidence for high browsing in Euhelopus zdanskyi.Biology LettersIn press. In press.
- 106. Taylor MP, Wedel MJ, Naish D (2009) Head and neck posture in sauropod dinosaurs inferred from extant animals. Acta Palaeontologica Polonica 54: 213–220.MP TaylorMJ WedelD. Naish2009Head and neck posture in sauropod dinosaurs inferred from extant animals.Acta Palaeontologica Polonica54213220
- 107. Noto CR, Grossman A (2010) Broad-scale patterns of Late Jurassic dinosaur paleoecology. PLoS ONE 5(9): e12553.CR NotoA. Grossman2010Broad-scale patterns of Late Jurassic dinosaur paleoecology.PLoS ONE59e12553
- 108. Barrett PM (2000) Prosauropod dinosaurs and iguanas: speculations on the diets of extinct reptiles. In: Sues H-D, editor. Evolution of herbivory in terrestrial vertebrates: perspectives from the fossil record. Cambridge: Cambridge University Press. pp. 42–78.PM Barrett2000Prosauropod dinosaurs and iguanas: speculations on the diets of extinct reptiles.H-D SuesEvolution of herbivory in terrestrial vertebrates: perspectives from the fossil recordCambridgeCambridge University Press4278
- 109. Chapman RE, Brett-Surman MK (1990) Morphometric observations on hadrosaurid ornithopods. In: Carpenter K, Currie PJ, editors. Dinosaur systematics: approaches and perspectives. Cambridge: Cambridge University Press. pp. 163–177.RE ChapmanMK Brett-Surman1990Morphometric observations on hadrosaurid ornithopods.K. CarpenterPJ CurrieDinosaur systematics: approaches and perspectivesCambridgeCambridge University Press163177
- 110. Campione N, Evans DC (2010) Cranial morphology and the diversity of Late Cretaceous edmontosaurs (Ornithischia: Hadrosauridae) from North America. Journal of Vertebrate Paleontology 30: supplement to 369A.N. CampioneDC Evans2010Cranial morphology and the diversity of Late Cretaceous edmontosaurs (Ornithischia: Hadrosauridae) from North America.Journal of Vertebrate Paleontology30supplement to 369A
- 111. Horner JR (1983) Cranial osteology and morphology of the type specimen of Maiasaura peelesorum (Ornithischia: Hadrosauridae), with discussion of its phylogenetic position. Journal of Vertebrate Paleontology 3: 29–38.JR Horner1983Cranial osteology and morphology of the type specimen of Maiasaura peelesorum (Ornithischia: Hadrosauridae), with discussion of its phylogenetic position.Journal of Vertebrate Paleontology32938
- 112. Brown B (1916) A new crested trachodont dinosaur, Prosaurolophus maximus. Bulletin of the American Museum of Natural History 35: 701–708.B. Brown1916A new crested trachodont dinosaur, Prosaurolophus maximus.Bulletin of the American Museum of Natural History35701708
- 113. Brown B (1912) A crested dinosaur from the Edmonton Cretaceous. Bulletin of the American Museum of Natural History 31: 131–136.B. Brown1912A crested dinosaur from the Edmonton Cretaceous.Bulletin of the American Museum of Natural History31131136
- 114. Gates TA, Sampson SD, Delgado De Jesús CR, Zanno LE, Eberth DA, et al. (2007) Velafrons coahuilensis, a new lambeosaurine hadrosaurid (Dinosauria: Ornithopoda) from the Late Campanian Cerro Del Pueblo Formation, Coahuila, Mexico. Journal of Vertebrate Paleontology 27: 917–930.TA GatesSD SampsonCR Delgado De JesúsLE ZannoDA Eberth2007Velafrons coahuilensis, a new lambeosaurine hadrosaurid (Dinosauria: Ornithopoda) from the Late Campanian Cerro Del Pueblo Formation, Coahuila, Mexico.Journal of Vertebrate Paleontology27917930
- 115. Horner JR, Currie PJ (1994) Embryonic and neonatal morphology of a new species of Hypacrosaurus (Ornithischia, Lambeosauridae) from Montana and Alberta. In: Carpenter K, Hirsch KF, Horner JR, editors. Dinosaur eggs and babies. Cambridge: Cambridge University Press. pp. 312–336.JR HornerPJ Currie1994Embryonic and neonatal morphology of a new species of Hypacrosaurus (Ornithischia, Lambeosauridae) from Montana and Alberta.K. CarpenterKF HirschJR HornerDinosaur eggs and babiesCambridgeCambridge University Press312336
- 116. Dodson P (1975) Taxonomic implications of relative growth in lambeosaurine hadrosaurs. Systematic Zoology 24: 37–54.P. Dodson1975Taxonomic implications of relative growth in lambeosaurine hadrosaurs.Systematic Zoology243754
- 117. Evans DC (2010) Cranial anatomy and systematics of Hypacrosaurus altispinus, and a comparative analysis of skull growth in lambeosaurine hadrosaurids (Dinosauria: Ornithischia). Zoological Journal of the Linnean Society 159: 398–434.DC Evans2010Cranial anatomy and systematics of Hypacrosaurus altispinus, and a comparative analysis of skull growth in lambeosaurine hadrosaurids (Dinosauria: Ornithischia).Zoological Journal of the Linnean Society159398434
- 118. Chin K, Kirkland JI (1998) Probable herbivore coprolites from the Upper Jurassic Mygatt-Moore Quarry, western Colorado. Modern Geology 23: 249–275.K. ChinJI Kirkland1998Probable herbivore coprolites from the Upper Jurassic Mygatt-Moore Quarry, western Colorado.Modern Geology23249275
- 119. Janensch WJ (1935–36) Die Schädel der Sauropoden Brachiosaurus, Barosaurus, und Dicraeosaurus. Palaeontographica 2: 147–298.WJ Janensch1935–36Die Schädel der Sauropoden Brachiosaurus, Barosaurus, und Dicraeosaurus.Palaeontographica2147298
- 120. Harris JD, Dodson P (2004) A new diplodocoid sauropod dinosaur from the Upper Jurassic Morrison Formation of Montana, USA. Acta Palaeontologica Polonica 49: 197–210.JD HarrisP. Dodson2004A new diplodocoid sauropod dinosaur from the Upper Jurassic Morrison Formation of Montana, USA.Acta Palaeontologica Polonica49197210
- 121. Remes K (2006) Revision of the Tendaguru sauropod dinosaur Tornieria africana (Fraas) and its relevance for sauropod paleobiogeography. Journal of Vertebrate Paleontology 26: 651–669.K. Remes2006Revision of the Tendaguru sauropod dinosaur Tornieria africana (Fraas) and its relevance for sauropod paleobiogeography.Journal of Vertebrate Paleontology26651669
- 122. Weishampel DB (1984) Interactions between Mesozoic plants and vertebrates: fructifications and seed predation. Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 167: 224–250.DB Weishampel1984Interactions between Mesozoic plants and vertebrates: fructifications and seed predation.Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen167224250
- 123. Norman DB, Sues H-D, Witmer LM, Coria RA (2004) Basal Ornithopoda. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, Second Edition. Berkeley: University of California Press. pp. 393–412.DB NormanH-D SuesLM WitmerRA Coria2004Basal Ornithopoda.DB WeishampelP. DodsonH. OsmólskaThe Dinosauria, Second EditionBerkeleyUniversity of California Press393412
- 124. You H, Dodson P (2004) Basal Ceratopsia. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, Second Edition. Berkeley: University of California Press. pp. 478–493.H. YouP. Dodson2004Basal Ceratopsia.DB WeishampelP. DodsonH. OsmólskaThe Dinosauria, Second EditionBerkeleyUniversity of California Press478493
- 125. Horner JR, Weishampel DB, Forster CA (2004) Hadrosauridae. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, Second Edition. Berkeley: University of California Press. pp. 438–463.JR HornerDB WeishampelCA Forster2004Hadrosauridae.DB WeishampelP. DodsonH. OsmólskaThe Dinosauria, Second EditionBerkeleyUniversity of California Press438463
- 126. Galton PM, Upchurch P (2004) Stegosauria. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, Second Edition. Berkeley: University of California Press. pp. 343–362.PM GaltonP. Upchurch2004Stegosauria.DB WeishampelP. DodsonH. OsmólskaThe Dinosauria, Second EditionBerkeleyUniversity of California Press343362
- 127. Bodmer RE (1990) Ungulate frugivores and the browser-grazer continuum. Oikos 57: 319–325.RE Bodmer1990Ungulate frugivores and the browser-grazer continuum.Oikos57319325
- 128. Gordon IJ, Illius AW (1994) The functional significance of the browser-grazer dichotomy in African ruminants. Oecologia 98: 167–175.IJ GordonAW Illius1994The functional significance of the browser-grazer dichotomy in African ruminants.Oecologia98167175
- 129. Demment MW, Van Soest PJ (1985) A nutritional explanation for body size patterns of ruminant and nonruminant herbivores. American Naturalist 125: 641–672.MW DemmentPJ Van Soest1985A nutritional explanation for body size patterns of ruminant and nonruminant herbivores.American Naturalist125641672
- 130. Sander PM, Clauss M (2008) Sauropod gigantism. Science 322: 200–201.PM SanderM. Clauss2008Sauropod gigantism.Science322200201
- 131. Amiot R, Lecuyer C, Buffetaut E, Escarguel G, Fluteau F, et al. (2006) Oxygen isotopes from biogenic apatites suggest widespread endothermy in Cretaceous dinosaurs. Earth and Planetary Science Letters 246: 41–54.R. AmiotC. LecuyerE. BuffetautG. EscarguelF. Fluteau2006Oxygen isotopes from biogenic apatites suggest widespread endothermy in Cretaceous dinosaurs.Earth and Planetary Science Letters2464154
- 132. Gillooly JF, Allen AP, Charnov EL (2006) Dinosaur fossils predict body temperatures. PLos Biology 4(8): e248.JF GilloolyAP AllenEL Charnov2006Dinosaur fossils predict body temperatures.PLos Biology48e248
- 133. Chinsamy A, Hillenius WJ (2004) Physiology of nonavian dinosaurs. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, Second Edition. Berkeley: University of California Press. pp. 643–659.A. ChinsamyWJ Hillenius2004Physiology of nonavian dinosaurs.DB WeishampelP. DodsonH. OsmólskaThe Dinosauria, Second EditionBerkeleyUniversity of California Press643659
- 134. Padian K, Horner JR (2004) Dinosaur physiology. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, Second Edition. Berkeley: University of California Press. pp. 660–671.K. PadianJR Horner2004Dinosaur physiology.DB WeishampelP. DodsonH. OsmólskaThe Dinosauria, Second EditionBerkeleyUniversity of California Press660671
- 135. Searle KR, Shipley LA (2008) The comparative feeding behaviour of large browsing and grazing herbivores. In: Gordon IJ, Prins HHT, editors. The Ecology of browsing and grazing. Berlin and Heidelberg: Springer Verlag. pp. 117–148.KR SearleLA Shipley2008The comparative feeding behaviour of large browsing and grazing herbivores.IJ GordonHHT PrinsThe Ecology of browsing and grazingBerlin and HeidelbergSpringer Verlag117148
- 136. Owen-Smith RN (1992) Megaherbivores: the influence of very large body size on ecology. Cambridge: Cambridge University Press. 388 p.RN Owen-Smith1992Megaherbivores: the influence of very large body size on ecologyCambridgeCambridge University Press388
- 137. Fastovsky DE, Smith JB (2004) Dinosaur paleoecology. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, Second Edition. Berkeley: University of California Press. pp. 614–626.DE FastovskyJB Smith2004Dinosaur paleoecology.DB WeishampelP. DodsonH. OsmólskaThe Dinosauria, Second EditionBerkeleyUniversity of California Press614626
- 138. Clauss M, Hummel J (2005) The digestive performance of mammalian herbivores: why big may not be that much better. Mammal Review 35: 174–187.M. ClaussJ. Hummel2005The digestive performance of mammalian herbivores: why big may not be that much better.Mammal Review35174187
- 139. Stephens DW, Krebs JR (1986) Foraging theory. Princeton: Princeton University Press. 247 p.DW StephensJR Krebs1986Foraging theoryPrincetonPrinceton University Press247
- 140. Myers JH, Bazely DR (1992) Thorns, spines, prickles and hairs: are they stimulated by herbivory and do they deter herbivores? In: Tallamy DW, Raupp NJ, editors. Phytochemical induction by herbivores. New York City: Wiley. pp. 325–344.JH MyersDR Bazely1992Thorns, spines, prickles and hairs: are they stimulated by herbivory and do they deter herbivores?DW TallamyNJ RauppPhytochemical induction by herbivoresNew York CityWiley325344
- 141. MacArthur RH, Pianka ER (1966) On optimal use of a patchy environment. The American Naturalist 100: 603–609.RH MacArthurER Pianka1966On optimal use of a patchy environment.The American Naturalist100603609
- 142. Jarman PJ, Sinclare ARE (1979) Feeding strategy and the pattern of resource-partitioning in ungulates. Zoological Journal of the Linnean Society 92: 267–284.PJ JarmanARE Sinclare1979Feeding strategy and the pattern of resource-partitioning in ungulates.Zoological Journal of the Linnean Society92267284
- 143. Foster JR (2003) Paleoecological analysis of the vertebrate fauna of the Morrison Formation (Upper Jurassic), Rocky Mountain Region, U.S.A. New Mexico Museum of Natural History and Science Bulletin 23: 1–95.JR Foster2003Paleoecological analysis of the vertebrate fauna of the Morrison Formation (Upper Jurassic), Rocky Mountain Region, U.S.A.New Mexico Museum of Natural History and Science Bulletin23195
- 144. Foster JR (2001) Relative abundances of the Sauropoda (Dinosauria, Saurischia) of the Morrison Formation and implications for Late Jurassic paleoecology of North America. Mesa Southwest Museum Bulletin 8: 47–60.JR Foster2001Relative abundances of the Sauropoda (Dinosauria, Saurischia) of the Morrison Formation and implications for Late Jurassic paleoecology of North America.Mesa Southwest Museum Bulletin84760
- 145. Tidwell WD (1990) Preliminary report on the megafossil flora of the Upper Jurassic Morrison Formation. Hunteria 2: 1–12.WD Tidwell1990Preliminary report on the megafossil flora of the Upper Jurassic Morrison Formation.Hunteria2112
- 146. Ash SR, Tidwell WD (1998) Plant megafossils from the Brushy Basin Member of the Morrison Formation near Montezuma Creek Trading Post, southeastern Utah. Modern Geology 22: 321–339.SR AshWD Tidwell1998Plant megafossils from the Brushy Basin Member of the Morrison Formation near Montezuma Creek Trading Post, southeastern Utah.Modern Geology22321339
- 147. Parrish JT, Peterson F, Turner CE (2004) Jurassic “savannah”—plant taphonomy and climate of the Morrison Formation (Upper Jurassic, Western USA). Sedimentary Geology 167: 137–162.JT ParrishF. PetersonCE Turner2004Jurassic “savannah”—plant taphonomy and climate of the Morrison Formation (Upper Jurassic, Western USA).Sedimentary Geology167137162
- 148. Turner CE, Peterson F (2004) Reconstruction of the Upper Jurassic Morrison Formation extinct ecosystem—a synthesis. Sedimentary Geology 167: 309–355.CE TurnerF. Peterson2004Reconstruction of the Upper Jurassic Morrison Formation extinct ecosystem—a synthesis.Sedimentary Geology167309355
- 149. Weishampel DB, Horner JR (1994) Life history syndromes, heterochrony, and the evolution of the Dinosauria. In: Carpenter K, Hirsch KF, Horner JR, editors. Dinosaur eggs and babies. Cambridge: Cambridge University Press. pp. 229–243.DB WeishampelJR Horner1994Life history syndromes, heterochrony, and the evolution of the Dinosauria.K. CarpenterKF HirschJR HornerDinosaur eggs and babiesCambridgeCambridge University Press229243
- 150. Whitlock JA, Harris JD (2010) A dentary of Suuwassea (Sauropoda: Diplodocoidea). Journal of Vertebrate Paleontology 30: 1637–1641.JA WhitlockJD Harris2010A dentary of Suuwassea (Sauropoda: Diplodocoidea).Journal of Vertebrate Paleontology3016371641
- 151. Hotton CL, Baghai-Riding NL (2010) Palynological evidence for conifer dominance within a heterogeneous landscape in the Late Jurassic Morrison Formation, U.S.A. In: Gee CT, editor. Plants in Mesozoic time: morphological innovations, phylogeny, ecosystems. Bloomington: Indiana University Press. pp. 295–328.CL HottonNL Baghai-Riding2010Palynological evidence for conifer dominance within a heterogeneous landscape in the Late Jurassic Morrison Formation, U.S.A.CT GeePlants in Mesozoic time: morphological innovations, phylogeny, ecosystemsBloomingtonIndiana University Press295328
- 152. Russell DA, Béland P, Mcintosh JS (1980) Paleoecology of the dinosaurs of Tendaguru (Tanzania). Mémoirs de la Société Géologique de France 1980: 169–175.DA RussellP. BélandJS Mcintosh1980Paleoecology of the dinosaurs of Tendaguru (Tanzania).Mémoirs de la Société Géologique de France1980169175
- 153. Aberhan M, Bussert R, Heinrich W-D, Schrank E, Schultka S, et al. (2002) Palaeoecology and depositional environments of the Tendaguru Beds (Late Jurassic to Early Cretaceous, Tanzania). Mitteilungen aus dem Museum für Naturkunde in Berlin Geowissenschaftliche Reihe 5: 19–44.M. AberhanR. BussertW-D HeinrichE. SchrankS. Schultka2002Palaeoecology and depositional environments of the Tendaguru Beds (Late Jurassic to Early Cretaceous, Tanzania).Mitteilungen aus dem Museum für Naturkunde in Berlin Geowissenschaftliche Reihe51944
- 154. Wilson JA (2005) Overview of sauropod phylogeny and evolution. In: Curry Rogers KA, Wilson JA, editors. The sauropods: evolution and paleobiology. Berkeley: University of California Press. pp. 15–49.JA Wilson2005Overview of sauropod phylogeny and evolution.KA Curry RogersJA WilsonThe sauropods: evolution and paleobiologyBerkeleyUniversity of California Press1549