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The emporion of Pech Maho was destroyed after a warlike event at the end of the third century BC. Shortly after that, around 200 BC, the site was resettled. This reuse is characterised above all by massive deposits of equid carcasses in various locations around the city. The conditions of these deposits are investigated in this paper. We focus on examining several biological parameters (weight, age and sex) of the equid population, as well as their feeding habits, using three different proxies: stable isotope, dental meso- and microwear. This interdisciplinarity gives us access to the overall equid diet, as well as to the diet during the last phases of their lives. This population is largely dominated by small size young adult males. Isotopic as well as morphometric analyses indicate that they were bred in various locations before being brought to Pech Maho. Dental wear analyses show that they experienced the same feeding throughout their lives and just before their death. The animals were all slaughtered within a short period of time. This study illustrates the advantages of combining proxies in order to enhance our understanding of the life and death conditions of Iron Age equids. [ABSTRACT FROM AUTHOR]

Despite the important role of livestock farming amongst Iron Age communities living in mountain regions, there is little information about livestock management, and particularly stabling practises, breeding systems, and grazing/foddering patterns. The study of the ground floor of Building G in Tossal de Baltarga has provided valuable insights into these important issues and has given us a better understanding of the social and economic patterns involved in all these livestock activities. It revealed the existence of a stable from the Late Iron Age, thanks to unique in situ finds of the stabled animals, including four sheep, a goat, and a horse, in addition to a range of organic remains preserved by fire and penning deposits. It is the first documented to date in the northeastern Iberian Peninsula. Through an integrated bio-geoarchaeological approach, combining a range of analytic procedures, including osteology, dental microwear, stable isotopes, phytoliths, dung spherulite analyses, and thin-section micromorphology, for the first time, this study has provided new, high-resolution evidence of livestock management strategies. Specifically, the research shed light on animal penning and feeding practises, revealing variable herbivorous regimes between species, the practise of seasonal movements, and the possible use of fodder as the main dietary regime of the animals stabled there. At the same time, the Baltarga case-study illustrates an indoor production unit that could reveal possible private control of some domestic animals in the Pyrenean Late Iron Age. [ABSTRACT FROM AUTHOR]

In recent years, paleodietary and paleoenvironmental studies have made great progress due to new techniques, such as the analysis of dental wear at micro and macro level and the analysis of stable isotopes of different elements in animal tissues. Recently, the combination of these proxies has substantially improved these types of studies, however, these analyses go hand in hand with biology and the animal behavior, so it is essential to understand the species studied previously. This paper describes the analyses commonly used in recent years in the Columbian mammoth (Mammuthus columbi) and the relationship that the biology of this species has with the correct application of these analyses. Likewise, the samples and measurements taken from these fossil individuals must be taken with care, since the peculiarities in dental ontogenesis, behavior and metabolism are key to the comprehension of the results obtained. [ABSTRACT FROM AUTHOR]

This study reconstructs Middle and Late Neolithic dietary practices in the area of the today Czech Republic and Lower Austria with a help of complementary evidence of stable isotope and dental microwear analysis. From a total of 171 humans, carbon and nitrogen isotopic values were measured in bone collagen of 146 individuals (accompanied by 64 animals) while 113 individuals were included into buccal dental microwear analysis. The samples were divided into two newly established chronological phases: Neolithic B (4900–4000 BC) and Neolithic C (3800–3400 BC) based on radiocarbon data modelling. Isotopic results show that the Neolithic diet was of terrestrial origin with a dominant plant component. A small but statistically significant shift in human carbon isotopic values to a higher δ13C was observed during the Neolithic C, probably reflecting an underlying change in plant growing conditions. Dental microwear results suggest a shift in adult diet and/or food preparation techniques between the Neolithic B and C, which, however, was not reflected in either the carbon or nitrogen isotopic values. The positive correlations between nitrogen isotopic values and the dental microwear variables (NV, XV, XT and NV/NT) observed in the adult sample suggest that meat rather than milk was the dominant source of animal protein, or that food enriched in 15N was processed specifically. Also, as both methods offer a snapshot of different periods of an individual’s life, the presence of a significant correlation may imply highly repetitive dietary behaviour during their lifetime. [ABSTRACT FROM AUTHOR]

Birds are some of the most diverse organisms on Earth, with species inhabiting a wide variety of niches across every major biome. As such, birds are vital to our understanding of modern ecosystems. Unfortunately, our understanding of the evolutionary history of modern ecosystems is hampered by knowledge gaps in the origin of modern bird diversity and ecosystem ecology. A crucial part of addressing these shortcomings is improving our understanding of the earliest birds, the non‐avian avialans (i.e. non‐crown birds), particularly of their diet. The diet of non‐avian avialans has been a matter of debate, in large part because of the ambiguous qualitative approaches that have been used to reconstruct it. Here we review methods for determining diet in modern and fossil avians (i.e. crown birds) as well as non‐avian theropods, and comment on their usefulness when applied to non‐avian avialans. We use this to propose a set of comparable, quantitative approaches to ascertain fossil bird diet and on this basis provide a consensus of what we currently know about fossil bird diet. While no single approach can precisely predict diet in birds, each can exclude some diets and narrow the dietary possibilities. We recommend combining (i) dental microwear, (ii) landmark‐based muscular reconstruction, (iii) stable isotope geochemistry, (iv) body mass estimations, (v) traditional and/or geometric morphometric analysis, (vi) lever modelling, and (vii) finite element analysis to reconstruct fossil bird diet accurately. Our review provides specific methodologies to implement each approach and discusses complications future researchers should keep in mind. We note that current forms of assessment of dental mesowear, skull traditional morphometrics, geometric morphometrics, and certain stable isotope systems have yet to be proven effective at discerning fossil bird diet. On this basis we report the current state of knowledge of non‐avian avialan diet which remains very incomplete. The ancestral dietary condition in non‐avian avialans remains unclear due to scarce data and contradictory evidence in Archaeopteryx. Among early non‐avian pygostylians, Confuciusornis has finite element analysis and mechanical advantage evidence pointing to herbivory, whilst Sapeornis only has mechanical advantage evidence indicating granivory, agreeing with fossilised ingested material known for this taxon. The enantiornithine ornithothoracine Shenqiornis has mechanical advantage and pedal morphometric evidence pointing to carnivory. In the hongshanornithid ornithuromorph Hongshanornis only mechanical advantage evidence indicates granivory, but this agrees with evidence of gastrolith ingestion in this taxon. Mechanical advantage and ingested fish support carnivory in the songlingornithid ornithuromorph Yanornis. Due to the sparsity of robust dietary assignments, no clear trends in non‐avian avialan dietary evolution have yet emerged. Dietary diversity seems to increase through time, but this is a preservational bias associated with a predominance of data from the Early Cretaceous Jehol Lagerstätte. With this new framework and our synthesis of the current knowledge of non‐avian avialan diet, we expect dietary knowledge and evolutionary trends to become much clearer in the coming years, especially as fossils from other locations and climates are found. This will allow for a deeper and more robust understanding of the role birds played in Mesozoic ecosystems and how this developed into their pivotal role in modern ecosystems. Video abstract [ABSTRACT FROM AUTHOR]

We assess diet and economies of middle Holocene (~7,500 to 4,000 calibrated [cal] B.P.) humans at coexisting mound sites (Huaca Prieta and Paredones) in north coastal Peru and document regular consumption of maize by ~6,500 to 6,000 cal B.P. and its earliest use as a staple food in this area of the Andes between 5,000 and 4,500 cal B.P. Stable isotope data from enamel carbonates and dentin collagen (childhood diet) and dental microwear texture analysis (adult diet) demonstrate dietary and economic specialization. Previous studies revealed maize and mixed-food refuse at both sites, but this study documents actual food consumption, showing that these communities situated a few hundred meters apart had significantly distinct diets in childhood and adulthood. Huaca Prieta focused on marine resources, although there are some contributions from terrestrial meat. Paredones individuals primarily consumed maize during childhood (up to 70% of the juvenile diet), as shown by δ13C values, apatite-collagen spacing, and discriminant analysis of δ13Ccoll, δ13Ccarb, and δ15N values. Maize was likely used as a weaning food (e.g., gruel and/or chicha--a maize beverage), hinting at the significant role of breastfeeding mothers, weanling infants, and children in the development of maize as a staple crop. Additionally, dental microwear data show Paredones adult diets are high in abrasives, potentially from maize processing. The distinct foodways at these neighboring sites result from and also reflect their social and political distinctions. These differences in food production, distribution, and consumption generated opportunities for exchange, an interaction that bound them together in mutual benefit. [ABSTRACT FROM AUTHOR]

European arrival into Australia had large‐scale impacts on the local flora and fauna. Most notably, Europeans brought with them numerous non‐native species, including the European red fox (Vulpes vulpes), European rabbit (Oryctolagus cuniculus), and the goat (Capra hircus) among many others. The introduction of these species had significant consequences on native Australian mammals, causing some small‐ to medium‐sized herbivores to become geographically restricted to primarily islands. Here, we examined the dietary ecology of the quokka (Setonix brachyurus), a native marsupial herbivore with a restricted geographic range in Western Australia before and after European arrival. Fossils from south‐western Australia and modern specimens were examined via dental microwear texture analysis and stable isotope analysis to assess whether the diet of the quokka had changed dramatically over time. Collectively, we help clarify whether there were any ecological reasons as to why this marsupial became geographically restricted, aside from the presence of invasive predators on mainland Australia. The quokka maintains a browsing diet from the Pleistocene to the present on the mainland, but modern island populations eat drier and tougher foods when living on islands lacking invasive mammals. There is also an apparent shift in the feeding environment of the quokkas on mainland Australia, from more open forests/shrublands in the Pleistocene to denser and wetter forests. Multi‐proxy data collectively indicate that the restricted range of the quokka today is most likely a result of predation from non‐native taxa and/or other human influences—not because of a lack of suitable habitat. [ABSTRACT FROM AUTHOR]

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Proboscideans are so-called ecosystem engineers and are considered key players in hypotheses about Late Pleistocene megafaunal extinctions. However, knowledge about the autoecology and chronology of the proboscideans in South America is still open to debate and raises controversial views. Here, we used a range of multiproxy approaches and new radiocarbon datings to study the autoecology of Chilean gomphotheres, the only group of proboscideans to reach South America during the Great American Biotic Interchange (~3.1 to 2.7 million years before present). As part of this study, we analyzed stable isotopes, dental microwear, and dental calculus microfossils on gomphothere molars from 30 Late Pleistocene sites (31° to 42°S). These proxies provided different scales of temporal resolution, which were then combined to assess the dietary and habitat patterns of these proboscideans. The multiproxy study suggests that most foraging took place in relatively closed environments. In Central Chile, there is a positive correlation between lower δ13C values and an increasing consumption of arboreal/scrub elements. Analyses of dental microwear and calculus microfossils have verified these leaf-browsing feeding habits. From a comparative perspective, the dietary pattern of South American gomphotheres appears to be constrained more by resource availability than by the potential dietary range of the individual taxa. This multiproxy study is aimed at increasing knowledge of the life history of gomphotheres and thus follows an issue considered one of the greatest challenges for paleontology in South America, recently pointed out by the need to thoroughly understand the role of ecological engineers before making predictions about the consequences of ecosystem defaunation. [ABSTRACT FROM AUTHOR]

The La Brea Tar Pits are a highly fossiliferous late Pleistocene locality, with over 230 vertebrate species, and the potential to help clarify the ecology of Pleistocene megafauna prior to their extinction. Here, we analyze dental microwear textures, dental mesowear, and stable carbon isotopes to assess the dietary behavior of the three most abundant ungulates at La Brea. We examined Bison antiquus , Camelops hesternus , and Equus occidentalis teeth from pits spanning the latest Pleistocene, focusing on pit 77 (~ 35 Ka, glacial period), and pits 61/67 (~ 11.5 Ka, interglacial period). Dental microwear attributes demonstrate that B . antiquus and E . occidentalis consumed foods with similar textural properties to those preferred by mixed feeding and browsing bovids, as well as significantly different food textures than the diet of modern bison and horses. Camelops hesternus has attributes most similar to modern browsing bovids and giraffes, revealing that all taxa studied likely consumed at least some woody browse. Complexity values ( Asfc ) in B . antiquus and E . occidentalis are significantly greater at pit 77 than at pits 61/67 and modern populations, suggesting a dietary decrease in woody vegetation and shrubs from the glacial to interglacial period. Dental mesowear values further indicate that B . antiquus and C . hesternus consumed woody vegetation, whereas E . occidentalis grazed. The different dietary interpretation for E . occidentalis may reflect a discrepancy between its average diet inferred from mesowear and its most recent diet inferred from microwear. Lastly, stable carbon isotopes reveal diets composed mostly of C 3 vegetation, with B . antiquus incorporating significantly more C 4 vegetation than either of the other dominant herbivores during the accumulation of both assemblages. Collectively, these data suggest that the dietary ecology of the dominant La Brea herbivores was more nuanced than previously thought, shifting coincident with changing climates, and not necessarily predictable from morphology or any one proxy method. [ABSTRACT FROM AUTHOR]

There has been much discussion of the role of behaviour in evolution, especially its potential to lead morphological evolution by placing the organism in a novel selective environment. Many adaptations of living species can be imagined to have originated in this way, although documented examples are relatively few. A fruitful arena for testing hypotheses about behavioural innovation is the fossil record. Traditionally, the behaviour of fossil species has been deduced from their morphology, precluding the observation of a behavioural lead preceding morphological evolution. This circularity can be broken by examining behavioural proxies independent of the adaptive morphology itself. Examples applicable to fossil remains include dietary information (e.g. wear traces on teeth, stable isotopes) and trace fossils indicating locomotor mode (footprints). The signature of a behavioural lead would be an observed shift in behaviour from one horizon (or taxon) to another, followed later by a functionally-related morphological change. This pattern can be sought either in finely-stratified anagenetic sequences of fossils (stratophenetic approach) or among fossils with well-resolved species-level phylogenies (cladistic approach). An array of case studies from the literature is presented. These include feeding shifts in finely-resolved sequences of vertebrates ranging from freshwater fish to terrestrial ungulates, as well as locomotor changes crucial to major evolutionary transitions in the origin of tetrapods, birds, and humans. The latter examples highlight the role of behaviour in initiating exaptation (the requisitioning of structure for a new function). The case studies also illustrate the challenges of using fossil sequences to elucidate behavioural roles, including insufficient stratigraphic resolution and uncertainty over the adaptive function of observed traits. By the same token, they suggest criteria for choosing promising cases for research, as well as for formulating testable hypotheses about evolutionary modes. © 2013 The Linnean Society of London, Biological Journal of the Linnean Society, 2014, 112, 315-331. [ABSTRACT FROM AUTHOR]

Abstract: Bioarchaeology is a powerful tool in the examination of prehistoric collections of human skeletal remains. Application of a few bioarchaeological techniques (ancient DNA, carbon and nitrogen stable isotopes, and dental micro-wear) to the human osteological remains from the Early Neolithic LBK settlement of Vedrovice (Moravia), has allowed us to reconstruct not only broad cultural patterns but also the life histories of the individuals with insights into diet, migrations, ancestry, personal identity, social position and life experience. Vedrovice acted as a gateway settlement for a farming community with close ties to western Hungary and northeast Bohemia. The individuals showed clear differences in status and migration histories, giving glimpses of more complex social practices and patterns than could have been determined through the traditional culture-historical studies. [Copyright &y& Elsevier]

Stable isotope analysis can be used to document dietary changes within the lifetimes of individuals and may prove useful for investigating fallback food consumption in modern, historical, and ancient primates. Feces, hair, and enamel are all suitable materials for such analysis, and each has its own benefits and limitations. Feces provide highly resolved temporal dietary data, but are generally limited to providing dietary information about modern individuals and require labor-intensive sample collection and analysis. Hair provides less well-resolved data, but has the advantage that one or a few hair strands can provide evidence of dietary change over months or years. Hair is also available in museum collections, making it possible to investigate the diets of historical specimens. Enamel provides the poorest temporal resolution of these materials, but is often preserved for millions of years, allowing examination of dietary change in deep time. We briefly discuss the use of carbon isotope data as it pertains to recent thinking about faliback food consumption in ancient hominins and suggest that we may need to rethink the functional significance of the australopith masticatory package. [ABSTRACT FROM AUTHOR]

Abstract: A multi proxy approach was performed to characterize vegetation in southwestern Bulgaria during the end of the Early and the Middle Turolian (8.7–7.0 Ma). This period was marked by eustatic fluctuations in the Mediterranean Sea that are well documented. In order to estimate the impact of these marine events on continental landscapes, dental microwear and stable isotope profiles in enamel were used to characterize feeding habits of extinct bovids, and in turn vegetation. Analyses were made on permanent molars of fossil bovids from two Late Miocene localities: Hadjidimovo-1 (Early/Middle Turolian) and Kalimantsi (Middle Turolian). Carbon isotopes profiles of Tragoportax rugosifrons and Miotragocerus gaudryi from the Hadjidimovo-1 indicate a pure C3-based diet for the two boselaphini. Large inter-individual differences in absolute δ 18O values were found for M. gaudryi suggesting little reliance on drinking water due to a browsing diet. Dental microwear shows that none of the bovid species exclusively grazed. In Hadjidimovo-1, microwear evidence suggests mixed feeding habits for Tragoportax rugosifrons, Gazella sp., and Palaeoreas lindermayeri and a leaf browsing diet for Miotragocerus gaudryi. Palaeoreas lindermayeri from Hadjidimovo-1 has a bimodal pattern indicating that its feeding preferences were tied to seasonal food availabilities. At Kalimantsi, Miotragocerus gaudryi show variations between individuals whereas Tragoportax cf. amalthea was an exclusive browser. Palaeoreas lindermayeri and Gazella sp. were also mixed feeders in Kalimantsi. Our combined approach shows no evidence for dense forested environments during the Early and Middle Turolian, and then supports previous hypotheses based on faunal analyses. Our results rather suggest that southwestern Bulgaria was dominated by open wooded landscapes where C3 graminoids grew in abundance among the herbaceous layer. Finally, microwear data suggest that the proportion of dicotyledons such as forbs, bushes or shrubs was probably higher in the plant communities of Kalimantsi than in those of Hadjidimovo-1. [Copyright &y& Elsevier]

San Luis de Apalachee, one of a chain of Roman Catholic missions established in Spanish Florida (modern states of Georgia and Florida) in the sixteenth and seventeenth centuries, was the principal center of missionization of native populations in the Florida pan-handle. Paleoethnobotanical remains yield evidence of production of various kinds of crops at the site, typical of nearly all mission period sites in the area. Stable isotope (carbon and nitrogen) analysis and dental caries evidence suggest that maize was not as important in the diet at San Luis as in other contemporary settings in the region. Ethnohistorical research indicates a heavier reliance on meat consumption compared to other mission settings. This study examines dental microwear of occlusal surfaces of maxillary molars from San Luis and five other Native American mission period sites in Spanish Florida. Epoxy casts of molar crushing facets were photographed under 500× magnification, using a scanning electron microscope. Photomicrographs were digitized using Microware 4.02 (Ungar [2002a]) and statistically evaluated using one-way AN OVA and post hoc Tukey's multiple comparisons tests. These analyses reveal that the frequency of pitting on the San Luis molars is significantly greater than for other mission period sites. Consistent with bioarchaeological, historical, and archaeological documentation, these findings suggest that diets were different in the San Luis natives in comparison with the other native populations in Spanish Florida. Various dietary factors likely came into play, resulting in these differences, and may have included significantly greater meat consumption at San Luis. [ABSTRACT FROM AUTHOR]

The scimitar-toothed cat Homotherium was one of the most cosmopolitan cats of the Pleistocene, present throughout Eurasia, Africa, and the Americas until at least ~28 thousand years ago. 1–3 Friesenhahn Cave (Bexar County, Texas) contains some of the best-preserved specimens of Homotherium serum alongside an abundance of juvenile mammoths, leading some to argue that H. serum preferentially hunted juvenile mammoths. 1,4 Dietary data of Homotherium are rare, with their ecology inferred from morphological, taphonomic, and genetic data. 1,3–10 Here, we use a multi-proxy approach to clarify the dietary ecology of H. serum as compared to extinct and extant cats and their relatives. Dental microwear texture analysis (DMTA) reveals that H. serum consumed soft and tough foods, similar to the extant cheetah, which actively avoids bone, 11,12 but in stark contrast to extant lions and hyenas, which are observed to engage in durophagy (i.e., bone processing). 11–14 DMTA data are consistent with taphonomic evidence of bone defleshing and the absence of bone-crunching behavior in H. serum. Stable carbon isotope values of H. serum indicate a clear preference for C 4 grazers including juvenile mammoths, in agreement with taphonomic evidence suggestive of a " Homotherium den" 1,4 and morphological data indicative of a relatively cursorial lifestyle. 6–8 Notably, the inferred diet of H. serum contrasts with the extinct dirk-tooth sabertooth cat Smilodon fatalis , which preferred forest/woodland prey and engaged in bone processing. 15–19 Homotherium serum exhibited a novel combination of morphological adaptations for acquiring open-country prey, consuming their soft and tough flesh—including the tough flesh of juvenile mammoths. [Display omitted] [Display omitted] • Dietary ecology inferred via dental microwear textures and stable isotopes • Homotherium ate tough flesh and open-habitat grazers, including juvenile mammoths • Homotherium serum exhibited disparate hunting behavior from Smilodon fatalis • Moderate cursoriality and unique hunting behavior in Homotherium DeSantis et al. clarify the dietary ecology of Homotherium serum from Friesenhahn Cave in Texas via the analysis of dental microwear textures and stable isotopes of tooth enamel. Analyses indicate that H. serum was a cursorial predator unlike any living cat and ate tough flesh of open-habitat prey—including the flesh of juvenile mammoths. [ABSTRACT FROM AUTHOR]

We investigate if and how diets of gray wolves from the Yukon Territory, Canada, have changed from the Pleistocene (>52.8 ka BP to 26.5 ka BP [±170 y BP]) to the recent Holocene (1960s) using dental microwear analysis of carnassial teeth and stable isotope analyses of carbonates (δ13C CO3 and δ18O CO3) and collagen (δ13C col and δ15N col) from bone. We find that dental microwear patterns are similar between the Pleistocene and Holocene specimens, indicating that there has been no change in carcass utilization behaviours, where flesh, not bone, is primarily consumed. Based on minimal changes in δ13C CO3 and δ13C col values, we find that, over thousands of years, Yukon gray wolves have remained generalist predators feeding upon several large ungulate species. Interestingly, δ15N col values suggest that the extinction of megafaunal species at ~11.7 Ka induced a shift from a diet comprised primarily of horse (Equus sp.) to one based on cervids (i.e. moose and caribou). Survival of large-bodied cervids, such as caribou (Rangifer tarandus), was likely key to wolf survival. Although gray wolves survived the end Pleistocene megafauna extinction and demonstrate a degree of ecological flexibility, we suggest that failure to preserve major elements of their current niche (e.G. caribou) may result in continued population declines, especially in the face of increasing anthropogenic influences. • Stable isotopes and dental microwear reveal diets of ancient and modern gray wolves. • Yukon gray wolves remained large ungulate specialists from Pleistocene to present. • Yukon gray wolves have remained primarily flesh-consumers. • Yukon gray wolves transitioned from diets mostly composed of horse to cervids. • Conservation efforts in the Yukon should focus on ungulate populations. [ABSTRACT FROM AUTHOR]