This contribution studies some paleobiological aspects of Opisthodactylus kirchneri, a fossil rheid from the Late Miocene of northwestern Argentina. We estimate the body mass of this species using an allometric equation based on long-legged birds. Besides, we estimate the maximum running speed by applying a previously published biomechanical model to study other living and fossil running birds. We perform multivariate analyses with hindlimb measurements used as biomechanical model inputs to compare the fossil rheid with other living ratite species. We found that O. kirchneri would not have been a swift runner as living rheids of South America. We identify the presence of a long distal hindlimb segment correlated with a novel adaptation to paleoenvironmental conditions in southern South America during the Late Miocene. We propose alternative interpretations based on these results and the hindlimb bone proportions.

Biomechanical analyses suggest that adult large theropods, such as Tyrannosaurus rex, could not run, and its top speed probably was at most 10 m/s. This probably implied a speed disadvantage of adult T. rex compared with some smaller potential prey. Living predators at a disadvantage owing to speed or manoeuvrability sometimes use the environment or special techniques to minimize those differences. Here, I made a theoretical analysis of the possibility that adult large theropods, such as T. rex, could occasionally pursue prey in water to take advantage of their body size. There are arguments based on scaling laws to support this hypothesis. To give an example, I applied a biomechanical model to estimate the speed in a shallow-water environment of adult T. rex and two smaller dinosaurs, a juvenile Edmontosaurus annectens and Struthiomimus sedens. I conclude that by wading or swimming, the adult T. rex would have been faster than smaller prey in water. I also suggest that in water, adult large theropods, such as T. rex, were able to use a running gait that was probably precluded on land. Finally, I propose a near-shore hunting scenario for adult T. rex and other full-grown large theropods.

Macrauchenia patachonica Owen, 1838 was among the last and largest litopterns, an extinct order of South American native ungulates. Macrauchenia patachonica had anatomical peculiarities as extremely retracted nasals, enlarged cervical vertebrae, and limb bones proportions without good living analogs that lead to asking about its paleobiology. To quantitatively assess the strange combination of limb bone features in M. patachonica, we constructed an indicator of differences in anatomical adaptations for efficient running between forelimb and hind limb (IDFH). We also made a multivariate analysis using data on osteological ratios of living mammals and two other litopterns. We discuss several biomechanical and paleobiological implications of the striking differences between hind limb and forelimb design in M. patachonica. Our main suggestion is that M. patachonica, during fast locomotion, probably used a posture with the neck in a horizontal position. (C) 2021 Elsevier Masson SAS. All rights reserved.

The shear elastic modulus is one of the most important parameters to characterize the mechanical behavior of soft tissues. In biomechanics, ultrasound elastography is the gold standard for measuring and mapping it locally in skeletal muscle in vivo. However, their applications are limited to the laboratory or clinic. Thus, low-frequency elastography methods have recently emerged as a novel alternative to ultrasound elastography. Avoiding the use of high frequencies, these methods allow obtaining a mean value of bulk shear elasticity. However, they are frequently susceptible to diffraction, guided waves, and near field effects, which introduces biases in the estimates. The goal of this work is to test the performance of the non-ultrasound surface wave elastography (NU-SWE), which is portable and is based on new algorithms designed to correct the incidence of such effects. Thus, we show its first application to muscle biomechanics. We performed two experiments to assess the relationships of muscle shear elasticity versus joint torque (experiment 1) and the electromyographic activity level (experiment 2). Our results were comparable regarding previous works using the reference ultrasonic methods. Thus, the NU-SWE showed its potentiality to get wide the biomechanical applications of elastography in many areas of health and sports sciences.

Living elephants produce seismic waves during vocalizations and locomotion that are potentially detectable at large distances. In the Mesozoic world, seismic waves were probably a very relevant source of information about the behavior of large dinosaurs. In this work, we study the relationship between foot shape and the directivity pattern of seismic waves generated during locomotion. For enlarged foot morphologies (based on a morphological index) of theropod dinosaurs, there is a marked effect of seismic wave directivity at 20 m. This effect is not important in the foot morphologies of other dinosaurs, including the foot shapes of herbivores and theropods such as therizinosaurids. This directivity produces a lower intensity in the forward direction that would slightly reduce the probability of detection of an ambush predator. Even more relevant is the fact that during the approach of a predator, the intensity of seismic waves detected by potential prey remains constant in the mentioned distance range. This effect hides the predator's approach, and we call this "seismic wave camouflage". We also discuss the potential relationship of this effect with enlarged fossil footprints assigned to metatarsal support.

An exceptionally well-preserved skull of the Pliocene rodent Telicomys giganteus allowed the first estimation of body mass and analysis of the bite mechanics of this species of South American giant rodent. In this study, we reconstructed the main anatomical features of the skull of this Pliocene rodent and related them to the bite force at the incisors. The average of an estimation body mass gives 100 kg. We also estimated the bite force using three different techniques. Two methods suggest that bite forces at the incisors have a range of 500-1000 N. However, the incisors seem to be stronger than expected for this bite force, implying that the bite forces may have been greater than 2000 N. We consider the hypothesis of defense against predators or other agonistic behavior to explain our results.

The Miocene Santacrucian sloths are a very important assemblage because they represent the first major radiation among sloths and, therefore, they could provide many insights about sloth evolution and diversity. Based on other studies, the hearing capabilities of Pleistocene sloths were identified. For a deeper understanding of these capabilities from an evolutionary point of view, in this article we study the hearing capabilities of Santacrucian sloths. We estimate the frequency range and the best frequency of hearing of six species of stem-megatherines and one species of mylodont. In most cases, the best frequency of hearing is much lower than the expected value for the estimated body mass of the species. This general shift towards low values of frequency is different than the pattern observed in mammals where sound localisation is improved by an increased sensitivity to high frequencies. In this article, we also propose some palaeobiological inferences of the low-frequency shift of hearing range in Miocene Santacrucian sloths.

Mesosaurid biology has been subject of continuous debate since the first description of Mesosaurus tenuidens by Paul Gervais in 1867. Controversy surrounds their environmental and feeding preferences. Most studies suggested that mesosaurids were marine reptiles and perhaps piscivorous predators. Nonetheless, recent work suggests that they inhabited a salty, eventually hypersaline shallow epicontinental sea and that pygocephalomorph crustaceans were their preferred food item. Here, we present results of the first biomechanical study about optimal swimming capabilities in Mesosaurus tenuidens, which along with the comparative analysis of the limb morphology support the hypothesis that these animals were slow swimmers living in shallow waters. The study is based on the revision of several almost complete mesosaurid specimens and isolated, well-preserved bones housed in palaeontological collections in Uruguay, Brazil, France and Germany. We studied the relative size and proportions of the bones, as well as their morphology and anatomical position to produce a three-dimensional reconstruction of the original appearance of an undamaged, complete skeleton. Our results suggest a fairly low optimal swimming speed for mesosaurids, which is consistent with capture of fairly slow prey like pygocephalomorphs, possibly by filter-feeding, rather than by active pursuit of fast prey.

Josephoartigasia monesi , from the Pliocene of Uruguay, is the largest known fossil rodent, with an estimated body mass of 1000 kg. In this study, finite element analysis was used to estimate the maximum bite force that J. monesi could generate at the incisors and the cheek teeth. Owing to uncertainty in the model inputs, a sensitivity study was conducted in which the muscle forces and orientations were sequentially altered. This enabled conclusions to be drawn on the function of some of the masticatory muscles. It was found that J. monesi had a bite of 1389 N at the incisors, rising to 4165 N at the third molar. Varying muscle forces by 20% and orientations by 10° around the medio‐lateral aspect led to an error in bite force of under 35% at each tooth. Predicted stresses across the skull were only minimally affected by changes to muscle forces and orientations, but revealed a reasonable safety factor in the strength of the skull. These results, combined with previous work, lead us to speculate that J. monesi was behaving in an elephant‐like manner, using its incisors like tusks, and processing tough vegetation with large bite forces at the cheek teeth.

Among the great diversity of the order Rodentia, the “New World Hystricognathi”, or caviomorphs are a very characteristic group from the Neotropical region. This group, whose fossil record begins in the late Eocene (Antoine et al., 2011), and is included in the infraorder Hystricognathi (Huchon and Douzery, 2001; Woods and Kilpatrick, 2005), comprises more than 50 genera in 13 families. One of the peculiarities of the extant caviomorphs is their wide range of size, between ∼200 g and ∼60 kg (Sánchez-Villagra et al., 2003). The latter is the maximum body mass among extant rodents (Mones and Ojasti, 1986) and occurs in Hydrochoerus hydrochaeris (known colloquially as capybaras), considered the giant of the group. South America is also home of the pacarana, Dinomys branickii, a large, enigmatic caviomorph rodent that can be found in the rainforests of Brazil, Bolivia, Colombia, Ecuador and Peru (Figure 6.1). This is the only living member of the family Dinomyidae, which is notorious for its great past diversity (Frailey, 1986; Mones, 1986; Rinderknecht et al., 2011).

The caracaras represent a characteristic faunal element of the Neotropics. Recently, a very large fossil species Caracara major from late Pleistocene of Uruguay was considered the largest known falconid. In the present contribution we describe a larger specimen belonging to a Caracara form from the late Pleistocene of the Buenos Aires province. The body mass estimation of this specimen clearly exceeds that of living caracaras species and, represents the largest known falconid (lowest body mass estimation nearly of 4500 grams). The diversification and extinction of large sized caracaras may be correlated with the abundance of very large mammals, which may provide abundant large carcasses as a food resource, in the late Pleistocene-early Holocene.

In the evolution of crocodylomorphs, there were at least three giant-dimension genera: Deinosuchus from late Cretaceous of North America, Sarcosuchus from middle Cretaceous of Africa and South America, and Purussaurus from Miocene of South America. It has been suggested that these predators could have fed on very large prey as dinosaurs and megamammals. The ‘death roll’ is a spinning manoeuver executed to subdue and dismember large prey; therefore, it has been previously suggested that giant cocrodylomorphs may have used this manoeuver. However, this manoeuver can generate torsional stresses in the skull. We propose a biomechanical model to estimate the capability of a crocodylomorphs for withstanding this torsional stresses. Our results show a good correlation between a ‘death roll’ capability indicator and the feeding categories related with the actual use of ‘death roll’ in 16 living species. Here, for the first time, we propose a biomechanical approach of the implications of ‘death roll’ in fossil crocodylomorphs. We suggest that Deinosuchus and Purussaurus were able to execute death roll over dinosaurs and large mammals, respectively, but Sarcosuchus probably was not. We also found some allometry effects and, finally, we discuss palaeobiological implications based on our results.

Arctotherium angustidens Gervais and Ameghino, 1880 (the South American giant short-faced bear) is known for being the earliest (Ensenadan Age, early to middle Pleistocene) and largest (body mass over 1 ton) of five described Arctotherium species endemic to South America. Here we assess the diet of this bear from multiple proxies: morphology, biomechanics, dental pathology, stable isotopes and a previous study using geometric morphometric methodology. Results favor the idea of animal matter consumption, probably from large vertebrates in addition to vegetable matter consumption. Most probably, active hunting was not the unique strategy of this bear for feeding, since its large size and great power may have allowed him to fight for the prey hunted by other Pleistocene carnivores. However, scavenging over mega mammal carcasses was probably another frequent way of feeding. South American short- faced bears adjusted their size and modified their diet through Pleistocene times, probably as a response to the diversification of the carnivore guild (from the few precursory taxa that crossed the Panamanian Isthmus during the Great American Biotic Interchange).

Although the growth and development of tissues and organs of extinct species cannot be directly observed, their fossils can record and preserve evidence of these mechanisms. It is generally accepted that bone architecture is the result of genetically based biomechanical constraints, but what about osteoderms? In this article, the influence of physical constraints on cranial osteoderms growth is assessed. Comparisons among lepidosaurs, synapsids, and archosaurs are performed; according to these analyses, lepidosaur osteoderms growth is predicted to be less energy demanding than that of synapsids and archosaurs. Obtained results also show that, from an energetic viewpoint, ankylosaurid osteoderms growth resembles more that of mammals than the one of reptilians, adding evidence to debate whether dinosaurs were hot or cold blooded.

Hypertrophied canines evolved several times among mammalian carnivores. Several palaeobiological hypotheses related to sabretooth evolution and killing behaviours have been suggested based on biomechanical and functional considerations. However, the lack of well-studied extant analogues makes it difficult to test these hypotheses. Here we propose the South American short-tailed opossum Monodelphis dimidiata as a living analogue of extinct sabretooth predators. Our morphological analysis shows that M.dimidiata not only has relatively the largest canines among extant marsupial carnivores, but they are also within the range of those of sabretooth predators. It also has cranial adaptations for a wide gape typical of sabretooth carnivores. The small body size of this species allows further biological studies that can provide useful information to understand the evolution, behaviour and physiology of extinct sabretooth carnivores.

The caracaras belong to a group of falconids with widespread geographical distribution in the Western Hemisphere, particularly in South America. Here we report fossil remains of a new species attributed to the genus Caracara from the late Pleistocene of Uruguay. This bird would have had an estimated body mass of 3700 grams, a value that greatly exceeds the maximum body mass reported for living falconids. Apparently, it would have had flying capabilities, in contrast to another paleospecies recently described from the Holocene of Jamaica. This fossil bird was found in association with mammal megafaunal remains and could offer new insights about the role of carnivorous birds in late Pleistocene environments of South America.

Blanco R.E., Rinderknecht, A. & Lecuona, G. 2011: The bite force of the largest fossil rodent (Hystricognathi, Caviomorpha, Dinomyidae). Lethaia, Vol. 45, pp. 157–163. An exceptionally well-preserved skull of the largest fossil rodent Josephoartigasia monesi allows the first analysis of the bite mechanics of this group of South American giant rodents. In this study, we reconstructed the main anatomical features of the skull of this Pliocene rodent, relating them to the bite force at incisors. Bite force was estimated using three different techniques. Two methods suggest that bite forces at incisors of around 1000 N were possible for these mammals. However, the incisors seem to be stronger than expected for this bite force implying that the bite forces may have been greater than 3000 N. We consider three hypotheses: allometric effects, teeth digging or defence against predators, to explain our results. □Bite force, Dinomyidae, incisors, largest rodent, Pliocene.

Recently discovered stapes of Pleistocene South American ground sloths of the genera Lestodon and Glossotherium are studied. Available body mass estimates are larger for Lestodon (4100 kg) than for Glossotherium (1500 kg), reflecting the obvious difference in the overall size of the skull and other bones. However, as previously reported, the absolute size of incus and malleus is very similar in both genera. In a previous work, the frequency range of Glossotherium (from 44 Hz to 15,489 Hz) was estimated quantitatively from well-preserved tympanic ring dimensions. For the first time the frequency ranges of hearing in both genera are estimated by a method based on the footplate area of the stapes. The obtained frequency ranges are consistent with the previous estimation for Glossotherium and are similar in both genera, giving evidence of a frequency range of hearing independent of body size in this group of mammals. Some possible paleobiological implications of the results may include adaptation to some specific sound source, fossoriality, or long-range communication. (C) 2012 Academie des sciences. Published by Elsevier Masson SAS. All rights reserved.

Borhyaenoids were marsupial predators that inhabited South America during the Cenozoic. They were very significant because no other mammals rivaled them as terrestrial hunters of large prey. Here we estimate the bite force of three species of borhyaenoids by two different methods to infer predatory behaviour in extinct taxa. One of the methods uses mainly the skull and only some simple measurements of the mandible; the other uses several measurements within the dentary. The results show that bite forces are very high in comparison to predators of the order Carnivora, a feature manifest by several other living and extinct marsupial predators. Differences in size, bite mechanics and special adaptations among the borhyaenoids suggest a very wide range of predatory behaviours that rival those represented in the extant families of the Order Carnivora.