Dietary habits in the endangered Bearded Vulture Gypaetus barbatus from Upper Pleistocene to modern times in Spain: a paleobiological conservation perspective

Although most Old World vulture species are declining or threatened in Asia and Africa, in Europe healthy vulture populations still exist. However, recent application of sanitary legislation that has greatly reduced the availability of animal carcasses is now a concern for conservationists. Until now, no studies have been undertaken to determine long-term dietary shifts in these species in Europe, but such studies are essential to optimising the resources invested in conservation and to anticipating the ecological needs of the target species. Here, we present a first attempt to examine the dietary variation in the Bearded Vulture Gypaetus barbatus from the late Pleistocene to the present day. Medium-size wild ungulates such as southern chamois Rupicapra pyrenaica, Spanish ibex Capra pyrenaica, red deer Cervus elaphus and roe deer Capreolus capreolus dominate the diet during the Pleistocene supporting the hypothesis that Bearded Vulture distribution was largely determined by the presence of such species. On the contrary, domestic species, such as sheep Ovis aries and goat Capra hircus, are the most common taxa in the diet in modern and historic periods. The actual dependence of the species on livestock, along with a restrictive sanitary legislation, threaten the conservation of this and other endangered avian scavengers in Europe. This new paleobiological conservation perspective confirms that efforts to establish a self-sustaining Bearded Vulture population should be enhanced by the widespread availability of medium-sized wild ungulates and by the presence of extensive and traditional grazing practice

SUBSILIENCE: Subsistencia y resiliencia humana ante los drásticos eventos climáticos acontecidos en Europa durante el Estadio Isotópico Marino 3

Climate has long been proposed as a possible trigger factor for the extinction of Neanderthals. Abrupt and acute oscillations of climate, as recorded from different climatic proxies such as Greenland polar ice sheets, are particularly threatening as they can push ecosystems towards catastrophic outcomes. Under these conditions, the survival of a species critically depends on their adaptive skills. Understanding the exact role that these episodes could have had on both Neanderthals and Anatomically Modern Humans (AMH) during the Middle to Upper Palaeolithic transition is, therefore, essential. SUBSILIENCE, a funded ERC project, is addressing this problem by assessing the behavioural flexibility and resilience of both human species based on their subsistence strategies, together with a newly obtained accurate climatic and environmental reconstruction across southern European peninsulas during MIS3. This novel approach will offer precise answers to questions concerning a) which particular subsistence patterns (if any) favoured AMH while coping with the changing environments and b) the extent to which climatic oscillations affected Neanderthal extinction. This it will be of relevance to the study of Prehistory on a pan- European scale.El clima se ha propuesto como uno de los posibles factores desencadenantes de la extinción de los Neandertales. Las oscilaciones rápidas y abruptas, registradas en diferentes registros climáticos del hemisferio norte, empujaron los ecosistemas hacia resultados catastróficos durante el Estadio Isotópico 3 (MIS3). En estas condiciones, la supervivencia de una especie dependió, fundamentalmente, de sus habilidades de adaptación. Comprender el rol que esos episodios tuvieron en la subsistencia de las ultimas poblaciones neandertales, pero también en la de los Humanos Anatómicamente Modernos en el continente europeo durante la transición del Paleolítico Medio al Superior es, por lo tanto, esencial. El proyecto SUBSILIENCE, financiado por el European Research Council (ERC), aborda esta cuestión mediante la evaluación de la flexibilidad del comportamiento y la resiliencia de ambas especies humanas analizando tanto su dieta como los diferentes patrones de subsistencia adoptados. A la vez, con base en los mismos elementos de su dieta, se centra en reconstruir las condiciones climáticas y ambientales a nivel local y regional. A partir del análisis de los materiales arqueozoológicos de más de 20 yacimientos localizados en las penínsulas del sur de Europa, este proyecto permitirá obtener respuestas sobre qué patrones de subsistencia particulares (si es que los hubo) favorecieron a nuestra especie en condiciones medioambientales tan cambiantes y a su vez, en qué grado las oscilaciones climáticas afectaron en la desaparición final de los Neandertales. La metodología, resultados y conclusiones de este proyecto serán relevantes para el estudio de la Prehistoria a escala paneuropea.&nbsp

What Neanderthals and AMH ate: reassessment of the subsistence across the Middle–Upper Palaeolithic transition in the Vasco‐Cantabrian region of SW Europe

ABSTRACT: Recent research in northern Spain has revealed the disappearance of Neanderthal populations in the Vasco‐Cantabrian region a few millennia earlier than in eastern and southern Iberia and discovered a short period of overlap with modern humans, at least, in terms of radiocarbon dates. However, the causes of Neanderthal decline understood as a regional and temporal process remain open. Despite the abundance of technological studies, modern‐quality chronological dating, and the availability of archaeofaunal and palaeoenvironmental data, there is a lack of consensus about how climatic and environmental conditions could have affected ungulate prey and, therefore, Neanderthal subsistence strategies. In this paper, an analytical summary of the archaeofaunal and taphonomic data available for the Vasco‐Cantabrian region, combined with the most recent chronological evidence, present general knowledge about animal biogeography and ecology during the Middle–Upper Palaeolithic transition, and provides an interpretation of the behaviour of both human species in the region. This work reviews the palaeomammal community of animals represented in the record as exploited by human groups in several caves and rock shelters and pointing to continuing lacunae in knowledge. Further research is needed to verify and potentially explain the apparent hominin population gap and the ultimate fate of the Neanderthals

Late Pleistocene Neanderthal exploitation of stable and mosaic ecosystems in northern Iberia shown by multi-isotope evidence

The carbon, nitrogen and sulphur stable isotope analyses and the stable isotope analyses of bioapatite carbonates were funded as part of the ABRUPT project (HAR2017-84997-P) funded by the Ministry of Science, Innovation and Universities and the SUBSILIENCE project funded by the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation programme (grant agreement no. 818299—ERC-2018-Consolidator), both awarded to ABM-A. SP was supported by the Max Planck Society and the University of Aberdeen during the time of this project, and the oxygen isotope analysis of bioapatite phosphates was funded by the Max Planck Society. Access to the archaeological collections was granted by the Museo de Arqueología de Bizkaia (Basque Government), and initial sampling for carbon and nitrogen isotope analysis was achieved by Hazel Reade funded by the FP7-PEOPLE-2012-CIG- 322112 project) and ABM-A. We appreciate Joseba Rios-Garaizar's advice about Axlor stratigraphy during the sampling process. We thank Ignacio Valera (IBBTEC, University of Cantabria) for kindly allowing the use of his laboratory facilities for collagen extraction. We thank Carlos Revilla Gómez (IBBTEC, University of Cantabria) for laboratory assistance during collagen extraction. Thanks are also due to Manuel Trost (MPI-EVA) for assistance during silver phosphate preparation and to Sven Steinbrenner for assistance with TC/EA-IRMS. KB is supported by a Philip Leverhulme Prize from the Leverhulme Trust (PLP-2019-284).Peer reviewedPublisher PD

Reassessing palaeoenvironmental conditions during the Middle-to-Upper Palaeolithic transition in the Cantabrian region (Southwestern Europe)

Climatic and environmental changes have been commonly proposed as driving factors behind the decline of Neanderthals in Europe. The Cantabrian region, in northern Iberia, is a key area for understanding the replacement of Neanderthals by Anatomically Modern Humans, where an early disappearance or Neanderthals in relation to other areas of Iberia has been proposed. To evaluate how climate might have influenced human behaviour during Marine Isotope Stage 3, an accurate review of palaeoecological conditions is required. For the first time, an assessment of the regional available terrestrial proxies linked to archaeo-palaeontological sites, including small vertebrate assemblages, pollen sequences, charcoal data and stable isotope studies on macromammals is undertaken in this region. In addition, records from macrofaunal assemblages and glacial records have also been considered. To standardise the information and allow inter-site comparison, data from pollen and small vertebrate sequences were transformed into quantitative climatic estimations of temperature and precipitation. Results show highly variable climatic shifts between archaeological levels, being consistent with the climatic fluctuations observed in the marine and ice core records. Small mammal assemblages reveal a mosaic landscape of open meadows followed by scattered forested areas. A progressive trend towards aridity from the end of the Mousterian to the early Aurignacian is reflected by changes in arboreal pollen, macromammal species and stable isotopes evidence on ungulates consumed by Neanderthals and Anatomically Modern Humans in the region. This review suggests a decrease in temperatures and rainfall from 48,000 to 44,000 cal BP (after Heinrich Event 5) which coincides with the late Neanderthals in the region and followed by a populational hiatus until 43,000 cal BP. Despite the multiple intra-site environmental proxies available, this study has challenged the fragmentary regional record during this key period for human evolution and reveals that further research is needed to obtain a complete regional high-resolution palaeoenvironmental and palaeoclimatic reconstruction

A chrono-cultural reassessment of El Cuco rock-shelter: a new sequence for the Late Middle Paleolithic in the Cantabrian Region (northern Iberia)

A large number of sites dated to the Late Middle Paleolithic and the Early Upper Paleolithic have been recorded in the Cantabrian region (northern Iberia), making this area a key location to investigate the lifeways of the last Neanderthals and the first anatomically modern humans. The stratigraphic sequence from El Cuco rock-shelter was originally attributed to the Early Upper Paleolithic based on radiocarbon dates performed on bone apatite. However, new radiocarbon dates on shell carbonates from the lower levels produced inconsistent dates with those previously published. In order to clarify this anomaly, a reassessment of the chronology of levels VI to XIV was undertaken. The review was based on new radiocarbon dates performed on bones and shells, and a re-evaluation of the lithic assemblages. Bone samples did not produce radiocarbon dates due to lack of collagen preservation but radiocarbon dating of shell carbonates provided dates ranging from 42.3 to 46.4 ka BP. These dates are significantly older than that previously obtained for level XIII using biogenic apatite from bones (~30 ka uncal BP), suggesting that the bone apatite used for radiocarbon dating was rejuvenated due to contamination with secondary carbonate. Lithic assemblages, defined in the first place as Evolved Aurignacian, have now been now confidently attributed to the Mousterian techno-complex. These results suggest a Middle Paleolithic chronology for this part of the sequence. The new chronology proposed for El Cuco rock-shelter has significant implications for the interpretation of Neanderthal subsistence strategies and settlement patterns, especially for coastal settlement and use of marine resources, not only in northern Iberia, but also in Atlantic Europe

Investigation of late Pleistocene and early Holocene palaeoenvironmental change at El Mirón cave (Cantabria, Spain): insights from carbon and nitrogen isotope analysis of red deer

Abstract: El Mirón Cavewas occupied by humans for over 40,000 years. Evidence of LateMousterian,Gravettian, Solutrean, Magdalenian, Azilian, Mesolithic, Neolithic, Chalcolithic, Bronze Age and Mediaeval occupations has been found in the cave. Understanding the local environmental conditions during the occupations is crucial for gaining an insight into the lifeways of El Mirón's inhabitants as they relied on the surrounding region and its natural resources for their subsistence. 170 bones of hunted red deer recovered from the cave were sampled for carbon and nitrogen stable isotope analyses with the aim of reconstructing the palaeoenvironment and palaeoclimate during the human occupation. The results show that the surrounding landscape underwent considerable environmental change during the Late Pleistocene and Early to Mid-Holocene. Shifts in d13C values between the Last Glacial Maximum, Heinrich stadial 1, Heinrich event 1, the Late-glacial interstadial and the onset of the Holocene are likely to reflect changes in water availability and temperature. Deer d15N generally increased over time indicating the regeneration of soil biological activity and nitrogen cycling, which was temporarily halted during the Younger Dryas. Comparison of the El Mirón results with those of 300 deer from other regions of Europe shows geographical variations in the timing and magnitude of the variation in d13C and d15N values. This variation tracks local climate (temperature andwater availability) and environmental (vegetation and forest development) change

Palaeogenomics of Upper Palaeolithic to Neolithic European hunter-gatherers

Modern humans have populated Europe for more than 45,000 years. Our knowledge of the genetic relatedness and structure of ancient hunter-gatherers is however limited, owing to the scarceness and poor molecular preservation of human remains from that period. Here we analyse 356 ancient hunter-gatherer genomes, including new genomic data for 116 individuals from 14 countries in western and central Eurasia, spanning between 35,000 and 5,000 years ago. We identify a genetic ancestry profile in individuals associated with Upper Palaeolithic Gravettian assemblages from western Europe that is distinct from contemporaneous groups related to this archaeological culture in central and southern Europe, but resembles that of preceding individuals associated with the Aurignacian culture. This ancestry profile survived during the Last Glacial Maximum (25,000 to 19,000 years ago) in human populations from southwestern Europe associated with the Solutrean culture, and with the following Magdalenian culture that re-expanded northeastward after the Last Glacial Maximum. Conversely, we reveal a genetic turnover in southern Europe suggesting a local replacement of human groups around the time of the Last Glacial Maximum, accompanied by a north-to-south dispersal of populations associated with the Epigravettian culture. From at least 14,000 years ago, an ancestry related to this culture spread from the south across the rest of Europe, largely replacing the Magdalenian-associated gene pool. After a period of limited admixture that spanned the beginning of the Mesolithic, we find genetic interactions between western and eastern European hunter-gatherers, who were also characterized by marked differences in phenotypically relevant variants.Open access funding provided by Max Planck Society. This project has received funding by the European Research Council under the European Union’s Horizon 2020 research and innovation programme under grant agreements no. 803147-RESOLUTION (to S.T.), no. 771234-PALEoRIDER (to W.H.), no. 864358 (to K.M.), no. 724703 and no. 101019659 (to K.H.). K.H. is also supported by the Deutsche Forschungsgemeinschaft (DFG FOR 2237). E.A. has received funding from the Van de Kamp fonds. PACEA co-authors of this research benefited from the scientific framework of the University of Bordeaux’s IdEx Investments for the Future programme/GPR Human Past. A.G.-O. is supported by a Ramón y Cajal fellowship (RYC-2017-22558). L. Sineo, M.L. and D.C. have received funding from the Italian Ministry of University and Research (MUR) PRIN 2017 grants 20177PJ9XF and 20174BTC4R_002. H. Rougier received support from the College of Social and Behavioral Sciences of CSUN and the CSUN Competition for RSCA Awards. C.L.S. and T. Saupe received support from the European Union through the European Regional Development Fund (project no. 2014-2020.4.01.16-0030) and C.L.S. received support from the Estonian Research Council grant PUT (PRG243). S. Shnaider received support from the Russian Science Foundation (no. 19-78-10053).Peer reviewe

Palaeogenomics of Upper Palaeolithic to Neolithic European hunter-gatherers

: Modern humans have populated Europe for more than 45,000 years1,2. Our knowledge of the genetic relatedness and structure of ancient hunter-gatherers is however limited, owing to the scarceness and poor molecular preservation of human remains from that period3. Here we analyse 356 ancient hunter-gatherer genomes, including new genomic data for 116 individuals from 14 countries in western and central Eurasia, spanning between 35,000 and 5,000 years ago. We identify a genetic ancestry profile in individuals associated with Upper Palaeolithic Gravettian assemblages from western Europe that is distinct from contemporaneous groups related to this archaeological culture in central and southern Europe4, but resembles that of preceding individuals associated with the Aurignacian culture. This ancestry profile survived during the Last Glacial Maximum (25,000 to 19,000 years ago) in human populations from southwestern Europe associated with the Solutrean culture, and with the following Magdalenian culture that re-expanded northeastward after the Last Glacial Maximum. Conversely, we reveal a genetic turnover in southern Europe suggesting a local replacement of human groups around the time of the Last Glacial Maximum, accompanied by a north-to-south dispersal of populations associated with the Epigravettian culture. From at least 14,000 years ago, an ancestry related to this culture spread from the south across the rest of Europe, largely replacing the Magdalenian-associated gene pool. After a period of limited admixture that spanned the beginning of the Mesolithic, we find genetic interactions between western and eastern European hunter-gatherers, who were also characterized by marked differences in phenotypically relevant variants