La Béringie, un vaste territoire qui s’étend de la Sibérie orientale au Territoire du Yukon, est perçue comme le point d’entrée des populations humaines en Amérique. A la fin du Pléistocène, ce territoire déglacé aurait constitué un refuge aux premières populations préhistoriques se dispersant hors d’Asie. Selon les données génétiques et paléo-génétiques, la Béringie fut occupée au cours du Dernier Maximum Glaciaire (19 000-23 000 cal BP, années calibrées Before Present) par une population humaine qui demeura génétiquement isolée durant près de 8000 à 9000 ans, donnant ainsi naissance à la lignée des Natifs Américains qui allaient se disperser, plus tard, au sud des masses glaciaires nordaméricaines et jusqu’en Amérique du Sud. Cette « Beringian standstill hypothesis », toutefois, ne trouva aucun soutien dans le registre archéologique : en Sibérie orientale, le plus ancien site est daté à 32 000 cal BP, tandis qu’en Alaska et au Yukon, la présence humaine ne remonte pas au-delà de 14 000 cal BP. Dans les années 70-80’s, le site des Grottes du Poisson-Bleu (Yukon) livra des outils en pierre et des ossements supposés modifiés par les humains, enfouis dans un dépôt loessique pléistocène ; les découvertes encouragèrent les archéologues J. Cinq-Mars et R. Morlan à évoquer l’hypothèse d’une occupation humaine sporadique dans le nord du Yukon entre 11 000 et 30 000 cal BP environ. La nature anthropogénique des échantillons osseux soumis aux datations radiocarbones ainsi que l’intégrité de la stratigraphie furent toutefois remises en question par une majorité d’archéologues. La présente dissertation propose une analyse archéozoologique et taphonomique rigoureuse et systématique des assemblages fauniques de mammifères des Grottes I et II dans le but d’appréhender les facteurs responsables de l’accumulation et de la modification du matériel osseux. De nouvelles datations radiocarbones effectuées par le laboratoire Oxford Radiocarbon Accelerator Unit sur des ossements portant des traces indéniablement culturelles permettent une datation précise de l’occupation humaine du site. Les résultats illustrent plusieurs traces de découpe sur des os de cheval, caribou, wapiti et possiblement bison et mouflon, tandis que des ossements de mammouth pourraient avoir été collectés pour l’industrie osseuse. Les nouvelles datations AMS suggèrent que les Grottes du Poisson-Bleu étaient occupées de façon sporadique entre 12 000 et 24 000 cal BP, soit pendant et après le Dernier Maximum Glaciaire. Le site offre ainsi un soutien archéologique à l’hypothèse de l’isolation génétique des populations béringiennes à l’origine des premières dispersions en Amérique. L’histoire taphonomique des Grottes du Poisson-Bleu rejoint celle des sites karstiques béringiens qui illustrent des occupations interspécifiques alternées entre carnivores et des fréquentations humaines de courte durée pour des activités de chasse. En outre, les altérations anthropiques sur des os de cheval des Grottes I et II ravivent le débat sur les extinctions de la mégafaune à la fin du Pléistocène (ca. 14 000 cal BP). Le site souligne l’incomplétude du registre archéologique et invite à multiplier les efforts de recherche en Béringie si l’on veut être à même de comprendre la préhistoire du peuplement des Amériques. / Beringia, a vast landscape stretching from eastern Siberia to the Yukon Territory, is thought to be the initial entry point of humans into North and South America. At the end of the Pleistocene, this unglaciated region constituted a refugium for the first prehistoric populations dispersing out of Asia. According to genetic and palaeogenetic data, Beringia was occupied during the Last Glacial Maximum (19 000-23 000 cal BP, calibrated years before present) by a human population that remained genetically isolated for about 8000 to 9000 years, leading to the divergence of the Native American lineage that would eventually disperse south of the ice-sheets into North and South America. The « Beringian standstill hypothesis » is not well supported in the archaeological record, however: in eastern Siberia, the oldest archaeological site is dated to 32 000 cal BP while in Alaska and the Yukon, evidence for a human presence doesn’t exceed 14 000 cal BP. Excavated in the 70s-80s, the Bluefish Caves site (Yukon) yielded stone tools and bone remains thought to have been culturally modified, buried in a Pleistocene loess deposit; the discovery encouraged archaeologists J. Cinq-Mars and R. Morlan to propose that humans occupied the caves sporadically between about 11 000 and 30 000 cal BP. The anthropogenic nature of the bone samples submitted for radiocarbon analysis and the stratigraphic integrity of the site didn’t convince the scientific community, however. The current dissertation proposes a rigorous archaeozoological and taphonomic analysis of the mammal bone assemblages of Caves I and II in order to identify the agents responsible for the accumulation and modification of the bone material. The results show several cut marks on bone specimens belonging to horse, caribou, wapiti and possibly bison and Dall sheep, while mammoth skeletal remains may have been collected for bone industry. New radiocarbon dates obtained by an Oxford laboratory (Oxford Radiocarbon Accelerator Unit) on bone bearing indisputable evidence of cultural modification allow the precise dating of the human occupation at the site. The AMS dates suggest that the Bluefish Caves were occupied sporadically between 12 000 to 24 000 cal BP, i.e., during and after the Last Glacial Maximum. The site, therefore, offers archaeological support for the Beringian standstill hypothesis. The taphonomic history of the Bluefish Caves, as well as other Beringian karstic sites, shows use of the caves by various carnivores and short-term human occupations for hunting activities. Moreover, cultural modifications on horse bone from Caves I and II enhance the debate surrounding the megafaunal extinctions at the end of the Pleistocene (ca. 14 000 cal BP). The site underlines the incompleteness of the archaeological record and invites us to expand research efforts in Beringia if we are to understand the prehistory of the first people of the Americas.

This thesis deals with systematic revision, evolutionary trends, palaeoecology and migration patterns of crustaceans (Cirripedia and Decapoda) from the Upper Cretaceous of the Bohemian Cretaceous Basin. Thesis is presented as a compilation of 9 papers that were published in scientific peer-reviewed journals and includes not only old museum material, but also numerous crustacean specimens which have been recovered in the last decade. Besides, short remarks on fossil crustaceans currently under study or in the process of being published (Paraclythia, Oncopareia, Acrothoracica) are also included in this thesis. In view of the fact that the fossil crustaceans from the BCB were most recently recorded in the turn of the 19th and the 20th centuries (and partially revised in the first half of the 20th century) and since the systematics and taxonomy have changed significantly, all papers presented here focus primarily on systematic revision and modern description. The essential part of the thesis thus deals with taphonomy and its bearing on the identification of fossil material. Thanks to a modern description, new species of Ctenocheles fritschi (axiidean shrimp), Archaeochionelasmus nekvasilovae (acorn barnacle), Myolepas reussi and Capitulum sklenari (pedunculate barnacles) were erected. C. fritschi is...

Ce projet contribue aux discussions en cours sur la transition du Paléolithique moyen au Paléolithique supérieur en Europe occidentale marquée par un tournant dans l’évolution de notre espèce, l’Homo sapiens. Alors que les Néandertaliens, nos plus proches cousins évolutionnaires disparaissent du registre fossile, les humains modernes qui ont migré hors d’Afrique, se dispersent rapidement à travers l’Eurasie. Les deux populations étaient exposées aux mêmes changements climatiques dramatiques caractéristiques de la transition, et pourtant, les Néandertaliens sont rapidement remplacés par les humains modernes. Par conséquent, ce phénomène suggère que les populations humaines modernes auraient pu être mieux adaptées face aux changements environnementaux. Puisque le régime alimentaire est un bon moniteur de l’adaptation, cette recherche compare les stratégies de subsistance des deux espèces humaines ayant tour à tour occupé le site de Riparo Bombrini (Balzi Rossi, Ligurie, Italie). Une analyse archéozoologique et taphonomique a été effectuée sur les collections fauniques du Moustérien tardif et du Proto-Aurignacien afin d’obtenir la première comparaison détaillée du régime alimentaire et des comportements de chasse des Néandertaliens et des humains modernes sur l’un des seuls sites du nord-ouest de l’Italie entièrement documenté avec des méthodes archéologiques modernes. Étant donné que la nature très fragmentée des ossements animaux sur le site a été un obstacle aux analyses fauniques dans le passé, les méthodes d’analyse archéozoologique ont été complétées par le « collagen fingerprinting » (c.-à-d. zooarchéologie par spectrométrie de masse, ou ZooMS) afin d’assurer l’identification d’un maximum de spécimens pour atteindre une précision accrue de l’identification taxonomique. La préservation différentielle du collagène dans les restes squelettiques a également justifié le développement d’une méthode novatrice de dépistage du collagène utilisant la spectroscopie FTIR-ATR pour la présélection d’échantillons ZooMS. Les résultats montrent que, tandis que Néandertal et Homo sapiens ont continuellement chassé les taxons ongulés disponibles à proximité de Riparo Bombrini, les niveaux de Moustérien tardif indiquent un rétrécissement du tableau de chasse associé à un mode de subsistance hyperlocal. En revanche, les spectres fauniques se sont considérablement élargis dans le plus ancien Proto-Aurignacien, lorsque Riparo Bombrini était occupé comme camp de base logistique à long terme associé à un vaste territoire de subsistance. Les résultats fournissent également les premières données détaillées sur la subsistance des populations humaines durant la transition dans la région de l’arc liguro-provençal, établissant ainsi de nouvelles hypothèses à tester dans de futurs travaux concernant la nature changeante de leurs écologies. / This project contributes to the ongoing debates over the Middle-Upper Paleolithic transition in Western Europe, which marks a turning point in the evolution of our species, Homo sapiens. While Neanderthals, our closest evolutionary relatives, went extinct at that time, modern humans who had migrated out of Africa dispersed very rapidly across Eurasia. While both populations were exposed to the same dramatic climatic shifts at the time, it is only the Neanderthals that quickly disappeared from the archeological record, suggesting that modern human populations may have been better adapted to react to environmental changes than Neanderthals. Since diet is a good monitor of adaptation, this research compares the subsistence strategies of both human groups as they occupied, in quick succession, the site of Riparo Bombrini (Balzi Rossi, Liguria, Italy). An archeozoological and taphonomic analysis was conducted on Late Mousterian and Proto-Aurignacian faunal collections to produce the first direct comparison between Neanderthal and modern human diets and hunting strategies at one of the only sites in Northwest Italy entirely excavated using modern documentation methods. Because the highly fragmented nature of the animal bones at the site has hindered faunal analysis in the past, these approaches were complemented by collagen fingerprinting (i.e., Zooarcheology by Mass Spectrometry, or ZooMS) to identify as many specimens as possible as to species, thus yielding unprecedented accuracy in taxonomic identification. The challenging collagen preservation state also required developing a screening method using FTIR-ATR spectroscopy prior to ZooMS. The results show that, while Neanderthals and modern humans continuously hunted prime-aged ungulate taxa available in a close range of Riparo Bombrini, the Late Mousterian levels indicate a narrower diet associated with a hyper-local subsistence range. In contrast, the faunal spectra broadened noticeably in the earliest Proto-Aurignacian, when Riparo Bombrini was occupied as a long-term logistical base camp within an extensive land-use strategy. The results also provide the first high-resolution view of human subsistence during the transition in the Liguro-Provençal arc region and set up test hypotheses about the changing nature of hominin behavioural ecology that can be further tested in future work.

No description available.

Applications in paleontological research are far from being limited to taxonomic collection and identification. Nor is such research limited to working solely on fossil data. Actualistic paleontology is the study of modern or recent organisms and processes to better understand those of the past. The bulk of this body of research falls under the category of actualistic paleontology, and examines geochronological methods and error biases in dating biological specimens ranging in age from modern to thousands of years old. Although such methods are arguably not perfect, error rates of ± a few hundred to few thousand years can be extremely important when considering ecological relationships among both Holocene taxa and time-averaged paleocommunities, but quite diminished when considering implications on more traditional dating techniques for ancient strata. Regardless, understanding implications of time resolution is important in analyses of and comparisons between any biological dataset. The following chapters are united by quantitative and statistical management of data with varying levels of temporal resolution, and represent four manuscripts that either are in press or soon to be submitted for publication. / Ph. D.

Nas últimas décadas, os Lagerstätten estiveram no centro das discussões relativas à história paleobiológica e geológica da Terra. Em particular, o Membro Crato da Formação Santana (Bacia do Araripe, Nordeste do Brasil) é um dos mais significantes Lagerstätten do Cretáceo já que registra invertebrados, vertebrados e plantas excepcionalmente preservados em sedimentos carbonáticos de um palaeolago. O principal objetivo desta dissertação é lançar luz sobre os processos de preservação responsáveis pela fossilização de insetos e peixes com tecidos moles em 3D. Lâminas petrográficas e diversas técnicas paleométricas - micro-Espectroscopia Raman, Fluorescência de raios-X (FRX) convencional, micro-FRX com fonte de luz sincrotron (RS-µFRX), emissão de Raios-X induzida por partículas (PIXE), microscopia eletrônica de varredura (MEV) e espectroscopia de energia dispersiva de Raios-X (EDS) - foram empregadas para caracterizar a rocha matriz, a morfologia e fidelidade de preservação dos tecidos moles e as composições elementares e moleculares dos fósseis em escala de centímetros e mícron. Os resultados revelam que, enquanto insetos e tecidos moles de peixes encontrados nos denominados calcários beges (BL) são substituídos por pseudomorfos de pirita framboidal (após oxidação da pirita), os quais ocorrem juntamente com possíveis substâncias poliméricas extracelulares secretadas por bactérias (EPS), tecidos de peixes dos calcários cinza (GL) são querogenizados. Em insetos, existe variação de tamanho dos framboides para dentro dos fósseis, que é aqui interpretada como produto do equilíbrio entre as taxas de difusão e de nucleação dos minerais. Além disso, a distribuição preferencial de Zn e Cu em estruturas piritizadas de insetos e peixes em comparação com a sua matriz é aqui considerada como sendo o resultado da fixação de elementos químicos em biofilmes bacterianos. Zn concentrado nos ossos de peixes com querogenizados e Fe/Cu observados em seus tecidos moles são considerados como tendo sido incorporados durante a vida dos peixes. No caso particular de peixes, modelo originalmente proposto para a preservação de metazoários do Pré-cambriano é aqui aplicado para explicar a variação de fossilização entre as fácies BL e GL. Lâminas petrográficas revelam que os GL têm geralmente teor de argila/matéria orgânica maior do que os BL, implicando que as taxas de soterramento poderiam ter sido mais intensas nos GL. Isto teria colocado carcaças em decomposição mais rapidamente na zona sedimentar de metanogênese, sendo formado o querogênio. Por outro lado, carcaças depositadas na fácies BL poderiam ter passado período mais longo na zona de redução de sulfato, o que teria levado à piritização generalizada. Além disso, a baixa porosidade do microespato, o cimento e a argila poderiam ter diminuído a migração de aceptores de elétrons dos processos de respiração bacteriana anaeróbia - particularmente redução de sulfato (RS) e metanogênese - e de seus produtos biogeoquímicos, estreitando a zona de RS, o que teria reduzido a influência da piritização em alguns níveis. Enquanto que a piritização resultou na preservação de fibras musculares em 3D, sarcolema, possíveis núcleos celulares, tendões e olhos, a querogenização preservou tecidos conjuntivos, tegumento e fibras musculares distorcidas e compactadas. Em conclusão, é aqui proposto que fácies influenciadas por processos paleoambientais e geobiológicos produziram fósseis com gradiente diferencial de fidelidade de preservação de acordo com cada via tafonômica seguida. / Over the past decades, the so-called Fossil Lagerstätten have been in the core of discussions concerning the palaeobiological and geological history of the Earth. In particular, the Crato Member from the Santana Formation (Araripe Basin, north-east Brazil) is one of the most significant Cretaceous Lagerstätten since it records exceptionally well-preserved fossil invertebrates, vertebrates, and plants, deposited in palaeolake carbonate beds. The main aim of this dissertation is to shed light on the preservational processes responsible for the fossilization of insects and fishes still retaining 3D soft tissues. Petrographic thin sections and several palaeometric techniques - micro-Raman Spectroscopy, conventional X-ray Fluorescence (XRF), Synchrotron micro-XRF (SR-µXRF), Particle-Induced X-ray Emission (PIXE), Scanning Electron Microscopy (SEM), and Energy-Dispersive X-ray Spectroscopy (EDS) - have been employed to characterize the host rock, soft-tissue morphology and preservational fidelity, and fossil elemental and molecular compositions in centimetre to micrometre scale. The results reveal that while insects and fish soft-tissues found in the so called beige limestones (BL) are replaced by framboidal pyrite pseudomorphs (after pyrite oxidation) occurring together with putative bacterially-secreted extracellular polymeric substances (EPS), labile tissues of fishes from the grey limestones (GL) are kerogenized. In insects, there is a variation of framboid size inward the fossils, which is here interpreted as a product of the balance between diffusion and mineral nucleation rates. Moreover, the preferential distribution of Zn and Cu in pyritized insect/fish labile structures in comparison to their rock matrix is here considered as being the result of element fixation in bacterial biofilms. Zn concentrated in bones of kerogenized fishes and Fe/Cu occurring in their soft tissues are considered to have been incorporated during fish life. In the particular case of fishes, a model originally proposed for metazoan preservation in the Precambrian is here applied to explain the variation of fossilization between the BL and GL facies. Petrographic thin sections reveal that GL have generally higher clay/organic matter contents than BL, thus implying that burial rates might have been more intense in the former. This could have placed decaying carcasses more quickly in the methanogenesis sedimentary zone, in that way being kerogenized. On the other hand, carcasses deposited in the BL facies could have spent a longer period in the sulphate-reduction zone, which would have accounted for pervasive pyritization. Additionally, microspar low porosity, cement and clay could have diminished both downward migrations of electron acceptors for anaerobic bacterial respiration processes - particularly sulphate-reduction (SR) and methanogenesis - and of their biogeochemical products, narrowing the SR zone, which would have lowered the impact of pyritization in some levels. While pyritization has recorded 3D muscle fibres, sarcolemma, putative cell nuclei, tendons and eyes, kerogenization has yielded connective tissues, integument and compressed/distorted muscle fibres. In conclusion, it is here proposed that palaeoenvironmental/geobiological-influenced facies have yielded fossils with a variable preservational-fidelity gradient, accordingly to each taphonomic pathway followed.

Culture types in Pacific Northwest archaeology are characteristic artifact assemblages distinguishing different prehistoric periods. Assemblages indicate a culture type transition during the 2,630 BP–270 BP occupation of Willows Beach (DcRt-10), southeastern Vancouver Island. Faunal remains could reveal links to subsistence patterns, following Croes’s theory that culture type change reflects subsistence intensification. Five dated DcRt-10 faunal assemblages underwent taxonomic and size classification, weighing and MNI calculation. Vertebrate weight and NISP percentages were compared between stratigraphic units associated with the later Gulf of Georgia and earlier Locarno Beach culture types. The youngest assemblage contains a smaller proportion of land mammal bone, suggesting increased sea mammal, fish, and bird procurement. Faunal remains also suggest a greater variety of taxa exploited over time. Faunal assemblages suggest that culture type change at DcRt-10 is the product of subsistence change, increasing knowledge of the culture historic sequence of this region.

No description available.

Pour l’extrême ouest eurasiatique, le problème demeure de savoir selon quelles modalités anthropologiques Neandertal et l’Homme d’Anatomie Moderne (HAM) se sont succédés, lors d’une sous-époque artificiellement qualifiée de « Transition ». Une solution pourrait selon nous venir d’une approche globale du système techno-économique nomade, là où l’approche technologique des industries lithiques, mise en oeuvre de façon privilégiée jusqu’à aujourd’hui, a montré ses limites. Notre thèse applique cette échelle systémique aux industries lithiques châtelperroniennes,depuis le nord de la France jusque dans la corniche vasco-cantabrique. Le Châtelperronien est pa railleurs une culture emblématique du problème évoqué. Nous avons placé la tracéologie lithiqueainsi que l’expérimentation au coeur de notre méthodologie analytique, afin de cerner à la fois les stratégies industrielles et les activités outillées des communautés châtelperroniennes. Tandis que nous nous sommes basé sur des modèles théoriques explicites pour appréhender plus généralement leur système de fonctionnement économique relativement à leur mode de nomadisme. Nous avons également utilisé la tracéologie afin d’éclaircir la problématique taphonomique spécifique au Châtelperronien.Nos observations sur l’état de surface des collections nous pousse finalement à suggérer que la dichotomie entre «sites à indices de passage » et « sites à dépôt archéologique » ne serait pas le résultat taphonomique d’évènements climatiques induisant une érosion à géométrie variable(i.e. intersites et/ou intrasites), comme nos prédécesseurs concevaient habituellement cette problématique spécifique. Au contraire, elles témoigneraient bien d’un mode d’occupation très contrasté du territoire. L’analyse fonctionnelle des industries, de son côté, abonde également dans ce sens en révélant que les stratégies industrielles reflètent une double partition, à la fois humaine et économique.En effet, d’une part, le « support de Châtelperron » équipe notamment des individus missionnés sur des sites logistiques tels que des haltes de chasse, afin qu’ils fabriquent et utilisent tour à tour des armatures de sagaie ou des couteaux de boucherie. D’autre part, d’autres haltes logistiques sont conçues comme la conjonction entre le renouvellement de l’industrie lithique et la réalisation d’activités spécialisées à caractère vivrier (boucherie) et artisanal (peausserie, et très probablement industrie osseuse). Quant aux campements résidentiels, manifestement très rares et alors sous abris rocheux, ils accueillent l’ensemble du groupe et sont le lieu où sont mis en oeuvre l’ensemble des industries lithique et osseuse, ainsi que la parure, reflétant le panel probablement complet des activités de ces communautés.En somme, il ressort une spécialisation des outils au Châtelperronien, et plus généralement une spécialisation cynégétique du système technique lithique, couplées à un mode logistique de nomadisme sur de vastes territoires. Ceci pourrait refléter une segmentation du groupe par spécialistes, et notamment une partition sociologique dans laquelle la figure du chasseur occupe une place majeure.Enfin, la confrontation de notre modèle châtelperronien spécifique avec les principales cultures de la Transition sur notre aire géographique fait ressortir une définition restrictive du Paléolithique supérieur. En effet, la spécialisation cynégétique du système technique lithique et, corrélativement,celle du statut de chasseur parmi les membres du groupe, représentent selon nous deux traits singularisant les communautés du Paléolithique supérieur. / At the far west of Eurasia, questions persist regarding what factors led anatomically modernhuman groups to succeed Neanderthals during the so called “Middle to Upper PaleolithicTransition.” Technological approaches to lithic analysis, which have until recently been the principal mean used to investigate these questions, have now shown their limitations. Instead, we suggest amore global approach, which examines both techno-economic and settlement systems.Here, we apply this mode of analysis to the Châtelperronian industry, which is found from northernFrance to the Vasco-Cantabrian region of northern Spain and is emblematic of the above-mentionedproblems. Methodologically, we approach this lithic industry by way of use wear analysis andexperimental archaeology. Our aim is to understand both overarching industry strategies and theways in which specific tools were used. We use theoretical models to investigate the relationshipbetween Châtelperronian functional economy and their mode of nomadism, and use traceology to clarify taphonomic problems specific to the Châtelperronian.We observed, using different levels of magnification, that the natural texture of most lithic artifacts appears to be surprisingly well preserved. This leads us to the conclusion that contrary to previous understandings, the perceived dichotomy between “sites à indices de passage” (i.e. coarse grained assemblages) and “sites à dépôt archéologique” (i.e. fine grained assemblages), cannot be the resultof climatic events resulting in different degrees of intersite and/or intrasite erosion. Instead, we suggest that this be the result of different pattern of movement of Châtelperronian groups. Additionally,the results of our use wear analysis suggest that Châtelperronian industrial strategies were the resultof a division in both human and economic terms.We hypothesize that individuals carried lithic blanks to logistical sites (e.g. hunting camps), manufactured so called “Châtelperronian points”, and used these tools as both projectile points and knives for butchery. This type of specialized activity hints at segmentation within a given group. Different type of logistical sites can be associated with different combinations of activities performed at them including the rejuvenation of lithic tools (i.e. flint knapping), the production of food (i.e.butchery), and other craft activities (i.e. hide working and the production of bone and antler tools).In contrast, residential sites were likely home to entire groups. These are rare in the archaeological record, and are always associated with rock shelters. These sites contain lithic and bone tools, as well as personal ornaments, which were manufactured on site. These residential sites can be considered good representations of the Châtelperronian industry as a whole, and likely reflect nearly the entire range of daily activities performed.In sum, Châtelperronian tools were specialized elements of a lithic industry focused on hunting within a system of logistical mobility spanning vast territories. This could reflect a social division of Châtelperronian groups into specialists, with the role of the hunter occupying a primary position. Finally, a comparison of our model of the Châtelperronian to that of other “transitional” cultures of western Eurasia leads us to propose a more restrictive definition of the Upper Paleolithic. We posit that hunting specialization, both in terms of lithic technology and the status of the hunter relativeto other members of the group, represent the only traits which set apart Upper Paleolithic societies. / En el caso del extremo occidental de Eurasia, la cuestión reside en establecer los factores antropológicos que llevaron a la sucesión Neanderthal-“Humanos Anatómicamente Modernos”durante la transición entre el Paleolítico Medio y el Superior. Estimamos que una vía de acercamiento puede derivar de un análisis más global del sistema tecnoeconómico nómada, alejándose deuna perspectiva tecnológica sobre la industria lítica demasiado restringida.Nuestra perspectiva se ha aplicado al estudio de una cultura característica del periodo, el Chatelperroniense,introduciendo un énfasis particular en el análisis funcional de los utillajes líticos y en elestudio de los patrones territoriales de los asentamientos. Para abordar los patrones territoriales,hemos recurrido a modelos teóricos explícitos que los relacionan con sistemas económicos específicos.En el caso del análisis funcional, hemos situado la observación de las huellas de uso y unimportante referencial experimental como núcleo de la metodología desarrollada. En este caso el objetivo es doble ya que se trata de reconocer las estrategias técnicas aplicadas a los propios utillajesde piedra y de reconocer también estas estrategias en los procesos técnicos en los que estos utillajeshan participado. El estudio traceológico ha servido asimismo para abordar cuestiones tafonómicasrelativas a la conservación de los yacimientos estudiados gracias a la lectura de las alteraciones sufridas por las superficies de los utillajes de piedra. Estas evidencias sugieren una conservación inesperadamente buena de los contextos arqueológicos. Ello viene a demostrar que las diferencias entre tipos de yacimientos que se habían observado –que se atribuían a alteraciones tafonómicas diferenciales- son en realidad el resultado de comportamientos y modos de ocupación diferentes ybien contrastados en cada uno de ellos.Por otra parte, los resultados generales del análisis funcional redundan en esta percepción, la deuna partición doble –humana y económica- en el seno de las estrategias técnicas. Nuestros resultadossugieren que existe una primera estrategia que implica una circulación en el territorio depuntas-cuchillos de chatelperron, probablemente transportados por individuos que se desplazana ocupaciones especializadas, como los campamentos de caza; estos instrumentos se utilizarían como cuchillos de carnicería y también como parte de elementos de proyectil. Algunas de estas ocupaciones especializadas reunirían un conjunto algo más complejo de funciones incluyendo larenovación del utillaje lítico agotado y algunos trabajos especializados relacionados con la subsistencia–carnicería- o actividades de elaboración de algunos productos (en piel y materias óseas). Los campamentos residenciales son muy escasos, casi siempre en abrigos y cuevas, y en ellos se llevarían a cabo el conjunto de tareas necesarias para estas comunidades y, en este sentido, puedenconsiderarse representativas de los comportamientos generales durante el periodo.En conjunto, se aprecia una especialización del utillaje durante el Chatelperroniense, muy orientada hacia las actividades cazadores en el marco de un sistema territorial que implica una gran movilidad logística. Ello podría reflejar una segmentación social interna de las comunidades con la apariciónde especialistas entre los que jugaría un papel importante la figura del cazador.Como conclusión, la comparación del modelo que emerge acerca de los comportamientos chatelperronienses con los propios de otras culturas de este periodo de transición en torno al 40.000nos lleva a proponer una definición más restrictiva para caracterizar al conjunto del Paleolítico Superior.En este sentido, planteamos que la especialización cazadora, tanto en lo que afecta al sistema técnico lítico como al estatus del cazador respecto a los otros miembros del grupo, representa el rasgo diferencial esencial que define a las comunidades humanas del Paleolítico superior.

Indiana University-Purdue University Indianapolis (IUPUI) / Research conducted during 2011 and 2012 at the Mississippian site of Angel Mounds outside of Evansville, IN sheds light on an often overlooked portion of the site that falls outside of the palisade wall – the 3rd Terrace. Through a magnetometer survey, a shovel test survey, and a reanalysis of a 1939 legacy collection from the 3rd Terrace, new interpretations about this peripheral area of the site will help to expand our ideas about Mississippian daily life in a wider geographic area and may help to better understand a transitional period in the history of Angel Mounds. In addition to the creation of a magnetic survey for use by the Angel Mounds State Historic Site, the use of minimally invasive and non-invasive research methods paired with previously excavated and curated collections allows for new research to be conducted with minimal disturbance to the archaeological site. While this research is a preliminary investigation of the archaeological potential for the 3rd Terrace, it also provides a solid basis for future research in the area and contributes to the wider understanding of Angel Mounds and the Mississippian world.