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This paper presents the anthracological results of Cova de la Guineu. This cave, which is located at the NE of the Iberian Peninsula, has provided charcoal samples from the early Neolithic to the Iberian period enabling the identification of different phases on the basis of flora assemblage interpretation. The results show how Mediterranean forests have been present since the early Holocene stages. At the early phases of the sequence the assemblage records dominant meso-screrophyllous taxa (deciduous Quercus, Taxus baccata), then thermophilous taxa (evergreen Quercus) spread, and finally a late phase of transformation dominated by thermophilous and heliophilous taxa (Mediterranean Pinus). The interpretation and discussion deals with the development and transformation of primary and secondary forests due to human disturbances and climatic variations. The anthracological record from Cova de la Guineu suggests that both elements were important and define the evolution of vegetation during the Holocene in the region. [ABSTRACT FROM AUTHOR]

The debate over hominid–carnivore interactions during the Pleistocene has been mainly approached from a human perspective, with the aim of contributing to the knowledge of the evolution of human cultural capabilities in the different periods. Regarding the European Middle Palaeolithic, it is most commonly concluded that Neanderthals were clearly superior to carnivores in the context of competitive relationships, with respect to both prey and the occupied space. Therefore, the presence of some human groups in the environments usually inhabited by carnivores could be perceived, from an ecological point of view, as a disturbance in the balance of the ecosystems. In order to assess the ecological impact of these human groups, the present study analyses the Unit III of Teixoneres Cave (MIS 3; Moià, Barcelona, Spain) through a comparison of palaeoecological and archaeological data. The site is located in the highlands between the two main rivers connecting the central region of Catalonia with the Mediterranean coast: the Llobregat and the Ter. Palynological and paleontological data indicate a cold landscape dominated by woodlands and some wet meadows. The high vertebrate diversity recorded in this stratigraphic unit suggests an environment marked by a balanced predator–prey dynamic, which may have been interrupted by the occasional presence of small human groups. According to the archaeological data, these human groups tended to predate the same prey as did carnivores, which may have generated a certain perturbation in the system. However, the small size of the groups and the brevity of their visits to Teixoneres Cave seem to have minimised the perturbation, allowing the environment to recover its original balance. [ABSTRACT FROM AUTHOR]

Objective: To reconstruct the etiology of a perimortem injury observed on a Neolithic - Chalcolithic cranium (5060 - 4400 yrs cal. BP)., Materials: A cranium of an old adult male individual belonging to a collective burial from Cova Foradada site (Calafell, Tarragona, Spain)., Methods: The cranium was analyzed macroscopically and microscopically using micro-CT scan., Results: The fracture on the right parietal bone presents characteristics of perimortem trauma. The morphology of the point of impact allows for the interpretation of this fracture as a result of impact by an object with a straight and sharp edge. In addition, the same cranium presents two healed antemortem injuries., Conclusions: The object that most likely caused the cranial fracture was a stone adze. The blow occurred from behind the individual, possibly by a right-handed attacker., Significance: The potential to link cranial fractures with specific tools increases our understanding of interpersonal violence during the Neolithic., Limitations: It is not possible to infer if this cranial injury was related to a large-scale intergroup confrontation or an intragroup violent event., Suggestions for Further Research: To investigate additional similar sites in the northeastern Iberian Peninsula to better characterize the fracture pattern caused by stone axes and adzes as well as other objects used as weapons during the Neolithic - Chalcolithic ages., (Copyright © 2020 Elsevier Inc. All rights reserved.)

We assembled genome-wide data from 271 ancient Iberians, of whom 176 are from the largely unsampled period after 2000 BCE, thereby providing a high-resolution time transect of the Iberian Peninsula. We document high genetic substructure between northwestern and southeastern hunter-gatherers before the spread of farming. We reveal sporadic contacts between Iberia and North Africa by ~2500 BCE and, by ~2000 BCE, the replacement of 40% of Iberia's ancestry and nearly 100% of its Y-chromosomes by people with Steppe ancestry. We show that, in the Iron Age, Steppe ancestry had spread not only into Indo-European-speaking regions but also into non-Indo-European-speaking ones, and we reveal that present-day Basques are best described as a typical Iron Age population without the admixture events that later affected the rest of Iberia. Additionally, we document how, beginning at least in the Roman period, the ancestry of the peninsula was transformed by gene flow from North Africa and the eastern Mediterranean., (Copyright © 2019 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works.)