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Well-preserved tracks of the wild boar Sus scrofa are described from the Matalascañas Trampled Surface (MTS) in the upper Pleistocene aeolian basal unit of the El Asperillo Cliff, Huelva (southwestern Spain). These are the first published tracks of suid pigs in the fossil record, here formally described as Suidichnus galani igen. and isp. nov. A revision of valid artiodactyl ichnogenera is provided for comparison. The large size of wild boar found in the Late Pleistocene of Spain contradicts the general trend towards smaller size known for the evolution of the species and the Bergmann's ecogeographical rule for the extant subspecies. In the present case, the remarkable large size that can be reached by these tracks is discussed as an ecomorphological adaptation of wild boars to either resource bonanza, and/or predation pressure during the Last Interglacial. The large S. scrofa scrofa identified in MTS corresponds to some of the earliest evidences known to this subspecies in Iberia.

The Golden Eagle has played a prominent part in the cultures and traditions of people across Eurasia and North America. The Neanderthals have for a long time been considered incapable of systematically catching birds of any description. Recent work has demonstrated that not only were they able to catch birds, they also took diurnal raptors. In this paper we show that Neanderthals selectively took the largest raptors at their disposal within Eurasia. Among these large raptors was the Golden Eagle, the most powerful and dominant of the raptors. Neanderthals and Golden Eagles co-shared the same habitats and landscapes across the Palaearctic region. We show that the long human/Golden Eagle association goes at least as far back as the Neanderthals.

Species present in the fossil record may continue to exist at an archaeological site, allowing study that fine-tunes our picture of the ecological past. A large wintering population of Eurasian Crag Martins Ptyonoprogne rupestris (ECM) roosts at the ‘Gorham’s Cave Complex’ UNESCO World Heritage site in Gibraltar, which is best known for its occupation by Neanderthals at times when ECMs were also present. Its complex geomorphology allows the study of use of different micro-sites (caves) within the roost. We used mark-recapture to test whether birds showed fidelity to micro-sites for roosting, and for differences in condition of birds across micro-sites. ECM showed very high fidelity towards micro-sites, within and between years, with > 90% chance of recapture at caves where they were first caught. Condition of birds differed between micro-sites, suggesting differences in roost quality between caves; birds were more likely to be recaptured at the micro-site where birds were in best condition, indicating higher survivorship. Our results demonstrate extremely fine-scale fidelity at the largest roosting site documented for ECM globally. Implications for conservation are discussed. The study provides current knowledge of a bird that has been using these caves since the Pleistocene and more generally on these caves as refuges.

Tracks and trackways of newborns, calves and juveniles attributed to straight-tusked elephants were found in the MIS 5 site (Upper Pleistocene) known as the Matalascañas Trampled Surface (MTS) at Huelva, SW Spain. Evidence of a snapshot of social behaviour, especially parental care, can be determined from the concentration of elephant tracks and trackways, and especially from apparently contemporaneous converging trackways, of small juvenile and larger, presumably young adult female tracks. The size frequency of the tracks enabled us to infer body mass and age distribution of the animals that crossed the MTS. Comparisons of the MTS demographic frequency with the morphology of the fore- and hind limbs of extant and fossil proboscideans shed light into the reproductive ecology of the straight-tusked elephant, Palaeloxodon antiquus. The interdune pond habitat appeared to have been an important water and food resource for matriarchal herds of straight-tusked elephants and likely functioned as a reproductive habitat, with only the rare presence of adult and older males in the MTS. The preservation of this track record in across a paleosol surface, although heavily trampled by different animals, including Neanderthals, over a short time frame, permitted an exceptional view into short-term intraspecific trophic interactions occurring in the Last Interglacial coastal habitat. Therefore, it is hypothesized that Neanderthals visited MTS for hunting or scavenging on weakened or dead elephants, and more likely calves. Research was possible thanks to the Delegaciones territoriales de Huelva, Consejería de Agricultura, Ganadería, Pesca y Desarrollo Sostenible and Consejería de Cultura (Junta de Andalucía), Servicio de Geodiversidad y Bio-diversidad (Dirección General de Medio Natural, Biodiversidad y Espacios Protegidos) and The National Park of Doñana. Thanks to Juan Jose Negro for several photos provided and Ramón López Romero during fieldwork. This work has been supported by the Research Groups RNM-293 and RNM-238, University of Huelva & Junta de Andalucía, and by the Fundação para a Ciência e Tecnologia, (with FEDER and COMPETE 2020 funds) under the project UIDB/MAR/04292/2020 (MARE — Marine and Environmental Sciences Centre). CNC would like to thank the financial support from the Câmara Municipal de Odemira. This work also received institutional support from the Naturtejo, E.I.M. (Naturtejo UNESCO Global Geopark). We would like to thank to all the colleagues who have collaborated in the field campaigns. The authors extend their warm appreciation to the Editorial Board member Matteo Belvedere and the reviewers Lara Sciscio and an anonymous that helped to significantly improve the present paper.

During the sixteenth to eighteenth centuries, Spanish ships sailed around the globe connecting Spain to its colonies. While documentary records offer rich details concerning life on board ship, archaeological information is essential to generating a full picture of the past. The cemetery at Old St Bernard’s Hospital, Gibraltar, provides an opportunity to study the skeletal remains of sailors. Following previous osteological research, carbon, nitrogen, oxygen and strontium isotope analyses were undertaken on thirty-three of these individuals. The results show that the, largely male, individuals had various different diets during life and came from several different places. Diets were largely based on C3food chains; some individuals consumed C3foods with low δ13C values; others consumed some marine foods, and a few individuals had a high trophic level diet, through the consumption of either freshwater resources or a high proportion of animal protein. The individuals spent their childhoods in several different places, although these homelands do not correlate simply with dietary variation. This variety in diets and homelands is consistent with our expectations for this hospital site given its location in a post-mediaeval entrepôt. The interpretation of these results are greatly helped by the available historical information and this has broader implications for the interpretation of isotope data elsewhere where the historical context of the site and the mobility patterns of the individuals are less well known.

Vanguard Cave is an archaeological site located on the shoreline of the Rock of Gibraltar at the south-western extreme of the Iberian Peninsula. It is part of a limestone cave system facing the adjacent Governor's Beach on the south-eastern coast of Gibraltar and has been filled to the roof with more than 17 m of sedimentary deposits. Due to its long stratified sequence, comprising rich palaeoenvironmental and faunal records as well as multiple Palaeolithic occupation layers, Vanguard Cave provides valuable information for our understanding of human behaviour and dispersal across south-eastern Iberia in general and particularly about the strategic role of the promontory of Gibraltar for past human populations. The development of a reliable absolute chronology for the sedimentary sequence at Vanguard Cave is therefore of great importance in this context. In this study, we applied optically-stimulated luminescence dating to sand-sized quartz grains from the uppermost ∼4 m of the Vanguard Cave deposits, as well as from the Hyaena Cave sediments – a small niche adjacent to the main cave chamber. We use single-grain and multiple-grain dating to clarify the depositional history of the sedimentary sequence, as well as to assess the reliability of the two dating approaches and their potential for future chronological studies at the site. The single-grain and multi-grain ages are consistent with one another and indicate no partial bleaching or post-depositional mixing of the sediments. Our results suggest that Vanguard Cave experienced continuous sediment accumulation probably since the last sea-level highstand in MIS 5, and was completely filled by ∼43 ka (MIS 3). The eastern side of the Rock of Gibraltar faced an exposed coastal shelf covered with savannah and an active coastal dune system during MIS 3. Our results indicate that similar environmental conditions are likely to have persisted also during MIS 4 and large parts of MIS 5.

This paper presents pollen analyses on hyaena coprolites from Vanguard Cave, Gibraltar, with the aim of depicting the vegetation landscapes of the southern Iberian Neanderthals during the MIS 3. The Palaeolithic vegetation in the surroundings included pine, oak, juniper, Pistacia, and mixed woodlands, savannahs, riverine forest patches, heliophytic matorrals, rocky scrub with chamaephytes and hemicryptophytes, grasslands with heaths, shrubby grasslands, steppe-like saltmarshes, and littoral vegetation. We compare our results to those of previous palaeobotanical study in the adjacent Gorham's Cave providing data for the MIS 3 and MIS 2. Placing the palaeobotanical records of Vanguard and Gorham's Caves in European context, the southern coasts of Iberia emerge as the most thermic refugium of the Late Quaternary, which has important implications for existing arguments about the long survival of Neanderthals in the Iberian Peninsula. © 2018 Elsevier B.V.

The Mediterranean ribbed limpet Patella ferruginea Gmelin, 1791 is the most endangered marine invertebrate listed in the EU Habitats Directive. A diversity of anthropic pressures have reduced its present-day distribution to a fraction of its former size. Perhaps surprisingly, this highly protected species has successfully established along man-made harbour breakwaters, resulting in serious complications when these structures have required modification or repair, often leading to costly impasses due to the legal status of the species. Attempts to move the limpets to other locations have resulted in unacceptably high mortality rates. This article describes the result of a field experiment where 97 P. ferruginea individuals were transported to a new site, using a technique which involved carefully moving the limpets whilst inactive (during low tide), still attached to their home scars on breakwater boulders. The results of this experiment were significantly positive, with 87% of all translocated limpets still alive 10 mo after the move, a mortality rate which compared favourably with that obtained for the existing control population at the receptor site. We propose that this method could be a practical solution to address the conflicts generated by this endangered species’ preference for harbour constructs. We further propose that this method can be used as a management tool to enhance the species’ survival prospects, by creating ‘stepping stones’ of pockets of reproducing individuals that can connect currently fragmented populations to effect a population recovery of this threatened organism.

The work in the inner area of Gorham’s Cave, Gibraltar, has added to the Palaeolithic art located in the cave. Although work continues on the surveying and the study of the evidence found up to now, we present here a preview consisting of a representation of a red deer, and also a hand stencil, alongside numerous marks which have been found scattered throughout the inner cave. In this paper we present new data on the Upper Palaeolithic rock art in Gorham’s Cave (Gibraltar) including direct dating of a hand stencil. Situating this dating in the archaeological context of the stencil, we conclude that it is associated with the Solutrean technocomplexe. This is particularly significant in the light of recent reviews which put European hand stencils in the context of the Early or Initial Upper Palaeolithic. In this context, the Gorham data opens the discussion on the systematic chronological correlation of all hands in negatives of European Palaeolithic rock art.

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., J.M.F., F.J.L.-C., J.I.M., F.X.O., J.D., and M.S.B. were supported by HAR2017-86509-P, HAR2017-87695-P, and SGR2017-11 from the Generalitat de Catalunya, AGAUR agency. C.L.-F. was supported by Obra Social La Caixa and by FEDER-MINECO (BFU2015- 64699-P). L.B.d.L.E. was supported by REDISCO-HAR2017-88035-P (Plan Nacional I+D+I, MINECO). C.L., P.R., and C.Bl. were supported by MINECO (HAR2016-77600-P). A.Esp., J.V.-V., G.D., and D.C.S.-G. were supported by MINECO (HAR2009-10105 and HAR2013-43851-P). D.J.K. and B.J.C. were supported by NSF BCS-1460367. K.T.L., A.W., and J.M. were supported by NSF BCS-1153568. J.F.-E. and J.A.M.-A. were supported by IT622-13 Gobierno Vasco, Diputación Foral de Álava, and Diputación Foral de Gipuzkoa. We acknowledge support from the Portuguese Foundation for Science and Technology (PTDC/EPH-ARQ/4164/2014) and the FEDER-COMPETE 2020 project 016899. P.S. was supported by the FCT Investigator Program (IF/01641/2013), FCT IP, and ERDF (COMPETE2020 – POCI). M.Si. and K.D. were supported by a Leverhulme Trust Doctoral Scholarship awarded to M.B.R. and M.P. D.R. was supported by an Allen Discovery Center grant from the Paul Allen Foundation, NIH grant GM100233, and the Howard Hughes Medical Institute. V.V.-M. and W.H. were supported by the Max Planck Society.

S. Fernández, J.S. Carrión, J. Ochando, P. González-Sampériz, M. Munuera, G. Amorós, J.M. Postigo-Mijarra, C. Morales-Molino, P. García-Murillo, G. Jiménez-Moreno, J.A. López-Sáez, F. Jiménez-Espejo, L.M. Cáceres, J. Rodríguez-Vidal, G. Finlayson, S. Finlayson, C. Finlayson Erratum to “New palynological data from the Late Pleistocene glacial refugium of South-West Iberia: The case of Doñana” [Review of Palaeobotany and Palynology (2021) PALBO 104431] Review of Palaeobotany and Palynology, Volume 296, January 2022, Pages 104566, The Doñana area in southern Iberia is one of the most renowned protected areas of Europe, mostly due to the diversity and value of its wetland ecosystems. The large biogeographical significance of this territory and the outstanding availability of sedimentary archives have made this region a hotspot of paleobotanical research in the Iberian Peninsula. Specifically, the organic deposits on El Asperillo Cliff have been studied during the past few decades from the geomorphological and paleobotanical (pollen, macrofossils) points of view. However, large uncertainties remain concerning the chronology of certain sections of the exposed profile and the paleobotanical potential of this site has not been fully exploited yet. In this study, we revisited El Asperillo with the aims of completing the paleobotanical record and refining the chronology of this site. The age of the studied deposits ranges from ca. 22,000 to 30,900 cal. yr BP according to the radiocarbon dates obtained, thus embracing the particularly cold and dry Heinrich Event 2 and the Last Glacial Maximum. Our palynological results allow inferring the presence of a coastal marshland system. Additionally, the new pollen records highlight the relevance and diversity of pines (Pinus nigra-sylvestris type, P. pinaster, P. halepensis-pinea type) in the Late Pleistocene landscape of Doñana, reinforcing the native status of pines. Last but not least, the results stress the persistence of a highly diverse woody flora in Doñana during the harshest periods of the last glacial cycle, highlighting the importance of this enclave in postglacial vegetation recolonization of the Iberian Peninsula., The development of this work was supported by Projects FEDER/Ministry of Science and Innovation, Agencia Estatal de Investigación CGL-BOS2015-68604-P and PID2019-1049449GB-I00), 261-2011 Organismo Autónomo de Parques Nacionales and Fundación Séneca grant 20788/PI/18

We compare the Middle Palaeolithic sites of Gibraltar and Zafarraya in southern Iberia. We use birds as indicators of environmental quality and demonstrate huge differences between coastal and inland, mountain, sites separated by less than 150 km. We conclude that the Gibraltar sites represented locations of repeated occupation by Neanderthals over tens of millennia whereas Zafarraya represents a site of sporadic visits for particular prey. This is in response to very different climatic conditions. Our results show how important ecological quality is in understanding Palaeolithic sites and metapopulations and how birds are particularly informative in our understanding of the ecology of such sites.

The aeolian Pleistocene deposits recorded in the Rock of Gibraltar (S Iberian Peninsula) present a significant sedimentary thickness that fills the wide sea caves and covers its steep slopes. In Catalan Bay these deposits register the development of cliff-foot and rampant dunes that form a 35° sand ramp, 1 km long and up to 300 m in height formed by moderately to well-sorted sands, slightly carbonated and weakly cemented. This morphosedimentary evidence is associated with MIS 5−2 sea level fluctuations. Its internal structure shows lamination sets of 2–3 m in thickness and planar and trough cross-bedding. In these beds, five morphotypes of mammalian footprints have been recognized in vertical cross sections and convex hyporeliefs. Most of them present a moderate degree of conservation due to the poor cementation of the sands. These icnites are related to the activity of terrestrial mammals, possibly belonging to Homininae, Proboscidea, Artiodactila and Carnivora. The affinity between the footprints and their tracemakers has been established in the basis of their physical parameters, the shape of the footprints, their comparison with similar footprints and the correlation with the fossil fauna of vertebrates described for the Late Pleistocene in Gibraltar. These findings represent the first palaeoichnological record in the aeolian sediments of Gibraltar and indirectly corroborate the occupation of the coastal dune landscape by several terrestrial mammals during the Late Pleistocene. In addition, they help reconstructing the animal behaviour and interaction with the extensive dune systems that developed at the foot of the Rock slopes. The age of the tracks has been established within the MIS 2, during the probable Middle-Upper Palaeolithic transition in the climate refuge of Gibraltar., Research supported by the Spanish MICINN-FEDER Project CGL2010-15810/BTE, This study is part of the activities of the Research Group RNM 293 “Geomorfología Ambiental y Recursos Hídricos”, University of Huelva. Comments of two anonymous reviewers have been very useful and constructive. This paper is dedicated to the memory of Dr. Richard Bromley.

The Rock of Gibraltar, at the south-western extreme of the Iberian Peninsula and 21. km from the North African coast, is a 6-km long limestone peninsula which was inhabited by Neanderthals from MIS 5e until the end of MIS 3. A total of 8 sites, either with Neanderthal fossils or their Mousterian lithic technology, have been discovered on the Rock. Two, Gorham's and Vanguard Caves, are the subject of ongoing research. These caves are currently at sea level, but during MIS 3 faced an emerged coastal shelf with the shoreline as far as 5. km away at times. They hold a unique archive of fauna and flora, in the form of fossils, charcoal and pollen, helping environmental reconstruction of now-submerged shelf landscapes. In addition, geological and geomorphological features - a 300-metre dune complex, elevated aeolian deposits, raised beaches, scree, speleothems - complement the biotic picture.The work is further complemented by a study of the ecology of the species recorded at the site, using present-day observations. The species composition in this fossil record closely matches the present day fauna and vegetation of the Doñana National Park, SW Spain: a mosaic of pine groves, coastal dunes, shrubland and seasonal wetlands and currently the richest reserve in terms of biodiversity in the Iberian Peninsula, located only 100. km to the northwest from Gibraltar.All this information permits, for the first time, the quantification of the vegetation structure of the ancient coastal plain and the modelling of the spatio-temporal dynamics of the MIS 3 coastal shelf off Gibraltar

Las excavaciones en la Cueva de Bray en Gibraltar han documentado una serie de enterramientos de la Edad de Bronce, esto supone una nueva aportación al conocimiento de la ocupación prehistórica del Peñón de Gibraltar y se convierte en una referencia regional para el estudio de los rituales funerarios de este período.

article i nfo This study utilizes geomorphology, marine sediment data, environmental reconstructions and the Gorham's Cave occupational record during the Middle to Upper Paleolithic transition to illustrate the impacts of climate changes on human population dynamics in the Western Mediterranean. Geomorphologic evolution has been dated and appears to be driven primarily by coastal dune systems, sea-level changes and seismo-tectonic evolution. Continental and marine records are well correlated and used to interpret the Gorham's Cave sequence. Specific focus is given to the three hiatus sections found in Gorham's Cave during Heinrich periods 4, 3 and 2. These time intervals are compared with a wide range of regional geomorphologic, climatic, paleoseismic, faunal and archeological records. Our data compilations indicate that climatic and local geo- morphologic changes explain the Homo sapiens spp. occupational hiatuses during Heinrich periods 4 and 3. The last hiatus corresponds to the replacement of Homo neanderthalensis by H. sapiens. Records of dated cave openings, slope breccias and stalactite falls suggest that marked geomorphologic changes, seismic activ- ity and ecological perturbations occurred during the period when Homo replacement took place.

This paper deals with the so-called Middle Pleistocene revolution, that is, the transition between the Early and Middle Pleistocene between 1.2 and 0.5 million years ago. Our knowledge about biotic changes during this transition has been so far largely based on studies of large mammals. Here we address the issue whether all faunal groups were equally affected. Three datasets have been used: (a) European large mammals present in the Middle and Late Pleistocene, (b) European fossil bird species recorded from the Early, Middle and Late Pleistocene of Europe, and (c) present-day birds currently classified in subfamilies that contain at least one Palaearctic representative species. Each species was allocated to all those geographical areas, climates, habitats in which it is present today; migratory status was also recorded. These datasets serve to undertake a biochronological analysis of mammal and bird groups, thus establishing patterns and processes of extinction and survival at the genus and species levels. The end of the Middle Pleistocene appears to have been a significant boundary in respect of herbivorous mammals, which suffered considerable depletion. In contrast, most genera and species of European birds in the Middle Pleistocene survived into the Late Pleistocene, even to the present day. Furthermore, at least 58% of the Middle–Pleistocene bird species were already present in the Early Pleistocene record. The most successful survivors in the Palaearctic Pleistocene were species from genera that had been the most climatically-tolerant during the late Cenozoic, usually from speciose and widely-distributed genera. We conclude that major transitions in Earth history have leant largely on biochronology and the perceived turnovers of faunas. Boundaries have usually depended heavily on changes to specific taxa of organisms. In this paper we show that what may appear as epic boundaries are largely scale- and taxon-dependent. Their usefulness must therefore be open to question. Here we advocate an individualistic and taxon specific approach in understanding the major ecological changes that have marked the history organisms.

Gorham’s Cave (Gibraltar) is currently the site with the most recent dates for Neanderthal presence in the world. The stratigraphy of late Neanderthal occupation of Gorham’s Cave is dated between 33 and 24 ka BP. This paper presents the analysis of the lithic industry from these statigraphic levels. This study establishes that this assemblage is undoubtedly Mousterian.

Although hardly applied to human palaeoecology, bird fossils offer a unique opportunity for quantitative studies of the hominin habitat. Here we reconstruct the Homo habitat niche across a large area of the Palaearctic, based on a database of avian fauna for Pleistocene sites. Our results reveal a striking association between Homo and habitat mosaics. A mix of open savannah-type woodland, wetlands and rocky habitats emerges as the predominant combination occupied by Homo across a wide geographical area, from the earliest populations of the Lower Palaeolithic to the latest hunter-gatherer communities of the Upper Palaeolithic. This observation is in keeping with the view that such landscapes have had long standing selective value for hominins.

Using data collected from existing habitats found in the southwestern Iberian Peninsula, and including data collected in the Biological Reserve of the Parque Nacional de Donana, Spain, this study considers the seasonal and inter-annual variability of a thermo-Mediterranean, subhumid, environment and the significance of the presence of surface water in the system. This extant environment is then used together with the fossil record from Gorham's Cave in Gibraltar, where Neanderthals lived, as a proxy for the ecology of the emerged landscape outside the cave.

In this paper, we describe a new method for quantitative reconstruction of bioclimate using a combination of multi-scale ecological datasets of present-day distributions of species with fossil plant and bird data derived from cave deposits of known age. In the specific case of Gorham's Cave, Gibraltar, we make predictions as to the prevailing climate during the Last Glacial Maximum (LGM). Our results indicate only slight variations compared to present-day climate. The present-day climatic regime is encompassed by a wider regime during the LGM. The importance of caves as climate archives is highlighted and our results additionally give focus to the generally underestimated importance of small-scale refugia during glacials.

Homo species were exposed to a new biogeochemical environment when they began to occupy caves. Here we report the first evidence of palaeopollution through geochemical analyses of heavy metals in four renowned archaeological caves of the Iberian Peninsula spanning the last million years of human evolution. Heavy metal contents reached high values due to natural (guano deposition) and anthropogenic factors (e.g. combustion) in restricted cave environments. The earliest anthropogenic pollution evidence is related to Neanderthal hearths from Gorham's Cave (Gibraltar), being one of the first milestones in the so-called “Anthropocene”. According to its heavy metal concentration, these sediments meet the present-day standards of “contaminated soil”. Together with the former, the Gibraltar Vanguard Cave, shows Zn and Cu pollution ubiquitous across highly anthropic levels pointing to these elements as potential proxies for human activities. Pb concentrations in Magdalenian and Bronze age levels at El Pirulejo site can be similarly interpreted. Despite these high pollution levels, the contaminated soils might not have posed a major threat to Homo populations. Altogether, the data presented here indicate a long-term exposure of Homo to these elements, via fires, fumes and their ashes, which could have played certain role in environmental-pollution tolerance, a hitherto neglected influence., SCOPUS: ar.j, info:eu-repo/semantics/published

The production of purposely made painted or engraved designs on cave walls-a means of recording and transmitting symbolic codes in a durable manner-is recognized as a major cognitive step in human evolution. Considered exclusive to modern humans, this behavior has been used to argue in favor of significant cognitive differences between our direct ancestors and contemporary archaic hominins, including the Neanderthals. Here we present the first known example of an abstract pattern engraved by Neanderthals, from Gorham's Cave in Gibraltar. It consists of a deeply impressed cross-hatching carved into the bedrock of the cave that has remained covered by an undisturbed archaeological level containing Mousterian artifacts made by Neanderthals and is older than 39 cal kyr BP. Geochemical analysis of the epigenetic coating over the engravings and experimental replication show that the engraving was made before accumulation of the archaeological layers, and that most of the lines composing the design were made by repeatedly and carefully passing a pointed lithic tool into the grooves, excluding the possibility of an unintentional or utilitarian origin (e.g., food or fur processing). This discovery demonstrates the capacity of the Neanderthals for abstract thought and expression through the use of geometric forms.

[EN] This paper presents an updated overview of the ongoing archaeological research carried out in the Protohistoric sanctuary of Gorham’s Cave (Gibraltar). It is based on the results of recent excavations, focusing on incised pottery with inscriptions or other marks. The catalogue of inscriptions includes both Phoenician and Graeco-Iberian examples, which could be related with the deposition of votive offerings from Archaic to Hellenistic periods., [ES] El artículo presenta un nuevo estado de la cuestión arqueológico sobre el santuario protohistórico de la Cueva de Gorham (Gibraltar) a la luz de los resultados de las recientes campañas de excavación y estudia los materiales cerámicos con inscripciones u otro tipo de marcas hallados en la cueva. El catálogo incluye un nuevo grafito fenicio y una inscripción greco-ibérica que se relacionan con las ofrendas depositadas en el lugar desde época arcaica hasta el periodo helenístico

The evidence for Neanderthal lithic technology is reviewed and summarized for four caves on The Rock of Gibraltar: Vanguard, Beefsteak, Ibex and Gorham’s. Some of the observed patterns in technology are statistically tested including raw material selection, platform preparation, and the use of formal and expedient technological schemas. The main parameters of technological variation are examined through detailed analysis of the Gibraltar cores and comparison with samples from the classic Mousterian sites of Le Moustier and Tabun C. The Gibraltar Mousterian, including the youngest assemblage from Layer IV of Gorham’s Cave, spans the typical Middle Palaeolithic range of variation from radial Levallois to unidirectional and multi-platform flaking schemas, with characteristic emphasis on the former. A diachronic pattern of change in the Gorham’s Cave sequence is documented, with the younger assemblages utilising more localized raw material and less formal flaking procedures. We attribute this change to a reduction in residential mobility as the climate deteriorated during Marine Isotope Stage 3 and the Neanderthal population contracted into a refugium.

Evidence of the AD 1755 tsunami consisting of the same type of accretions produced by the re-deposition of earlier sediments, has been recorded at three different height along the coast of Gibraltar: Along a shallow sandy shore, the tsunami wave reached a run-up of 2–3 m, whereas along steep, cliff–lined shores (Rosia Bay) it surpassed 5 m. An overwash deposit was also identified at the bottom of a lagoon (The Inundation), at 0.5 m b.s.l., on the isthmus that joins the Rock with the mainland. Southern submerged platforms (Vladi’s Reef) were also affected by the erosional backwash to a depth of 22 m. The tsunamigenic sediments exhibit a bimodal granulometry, mainly composed of sands with a coarser fraction composed of marine faunal shells remains, together with larger clasts derived from the rocky substrate. All remobilized sediments were dated by historical methods and radiocarbon dating. Se han registrado evidencias del tsunami de 1755 localizadas a tres alturas diferentes a lo largo de la costa de Gibraltar, todas ellas como resultado del mismo tipo de acreción producida por el re-depósito de sedimentos previos. A lo largo de las costas bajas y arenosas estudiadas, la ola del tsunami alcanzó una altura de 2 a 3 m, mientras que en litorales acantilados y con fuertes pendientes sobrepasó los 5 m. Se ha identificado un posible registro sedimentario en el fondo de una laguna costera (Inundation), a 0.5 m b.n.m., en el istmo que une la Roca con el continente. Por otro lado, las plataformas sumergidas, como la meridional de Vladi’s Reef, sufrieron erosión por la retirada de las olas a una profundidad de hasta 22 m. Los sedimentos tsunamigénicos poseen una granulometría bimodal, compuesta principalmente de arenas con una fracción más gruesa de restos de conchas marinas, junto con cantos mayores de rocas provenientes del sustrato. Todos los sedimentos removilizados por el tsunami han sido datados por métodos históricos y de radiocarbono. Research supported by the Spanish-FEDER Project CGL2010-15810/BTE, AHRC Research Grants (AH/E009409/1), and COST-action TD0902 SPLASHCOS (Submerged Prehistoric Archeology and Landscapes of the Continental Shelf). We thank reviewers and guest-editors for helpful comments. It is a contribution to IGCPs 526 (Risks, resources, and record of the past on the continental shelf), 567 (Earthquake Archaeology and Palaeoseismology), and 588 (Preparing for coastal change).

Cortés-Sánchez, Miguel et al., Numerous studies along the northern Mediterranean borderland have documented the use of shellfish by Neanderthals but none of these finds are prior to Marine Isotopic Stage 3 (MIS 3). In this paper we present evidence that gathering and consumption of mollusks can now be traced back to the lowest level of the archaeological sequence at Bajondillo Cave (Málaga, Spain), dated during the MIS 6. The paper describes the taxonomical and taphonomical features of the mollusk assemblages from this level Bj19 and briefly touches upon those retrieved in levels Bj18 (MIS 5) and Bj17 (MIS 4), evidencing a continuity of the shellfishing activity that reaches to MIS 3. This evidence is substantiated on 29 datings through radiocarbon, thermoluminescence and U series methods. Obtained dates and paleoenvironmental records from the cave include isotopic, pollen, lithostratigraphic and sedimentological analyses and they are fully coherent with paleoclimate conditions expected for the different stages. We conclude that described use of shellfish resources by Neanderthals (H. neanderthalensis) in Southern Spain started ~150 ka and were almost contemporaneous to Pinnacle Point (South Africa), when shellfishing is first documented in archaic modern humans., The works at Bajondillo Cave and the shellfish harvesting in the Natural Park of Maro-Cerro Gordo were approved by the Junta de Andalucía (Spain). The manuscript was greatly improved by the instructive comments and suggestions of two anonymous reviewers.

Debates surrounding Neanderthals and Anatomically Modern Humans (AMH) tend to focus primarily on discussions of cognitive ability, as exemplified by perceived differences in stone tool technology, behaviour and extinction outcomes. One of the primarily cited differences involves the subsistence strategies practised by these different groups of humans (Brown 2009).

8 pages, 4 figures, 1 table., The stratigraphy of the late Neanderthal occupation of Gorham's Cave, Gibraltar, between 33 and 24 ka BP, the latest known site of Neanderthal occupation, is discussed. Level IV at Gorham's Cave exclusively records Neanderthal occupation and is characterised by Mousterian technology and a sequence of 22 AMS dates. The overlying Level III is Upper Palaeolithic, and the earliest diagnostic culture is the Solutrean at around 18.5 ka BP. A dating interval of over four thousand years separates these two horizons. The ecological and bioclimatic characteristics of the site are considered as an explanation for the late survival of the Neanderthals in the region.

Palaeobotanical (pollen, charcoal) data from Gorham's Cave reveals a diversified landscape in the Gibraltar region during the Middle (c. 32 560-23 780 year BP) and Upper Palaeolithic (c. 18 440-10 880 BP). Inferred vegetation types include oak, pine, juniper, and mixed woodlands and savannahs, grasslands with heaths, heliophytic matorrals, phreatophytic formations (e.g. riverine forests, wetlands), and thermomediterranean coastal scrub. A revision of palaeoecological data suggests that patches of trees persisted even in northern and continental territories of the Iberian Peninsula during the cold stages of OIS3 and OIS2. However, a southern Mediterranean coastal shelf extending from Gibraltar to Málaga, and probably further north up to Murcia, was unique in its combination of thermo-, meso-, and supramediterranean plant and animal species. Given the composition of these assemblages, this shelf and its adjacent mountains represented a crucial reservoir of biodiversity during the Upper Pleistocene. It is within this physiographically complex context with its diversity of resources where the last Neanderthals extraordinarily survived until c. 24 000 BP, that is over 10 000 years later than the disappearance of Neanderthals from elsewhere in temperate Europe. © 2008 Elsevier Ltd. All rights reserved., This research has been funded by the projects CGL-2006-2956-BOS (Ministerio de Educación y Ciencia, Madrid), EU MEDOC Interreg IIIB 2002-02-4, PalaeoMED 1-U-048, and PI-00369/FS/04 and Paleodiversitas Network (Fundación Séneca, Murcia).

6 figures, 1 table, Paleoclimate records from the western Mediterranean have been used to further understand the role of climatic changes in the replacement of archaic human populations inhabiting South Iberia. Marine sediments from the Balearic basin (ODP Site 975) was analysed at high resolution to obtain both geochemical and mineralogical data. These data were compared with climate records from nearby areas. Baexcces was used to characterize marine productivity and then related to climatic variability. Since variations in productivity were the consequence of climatic oscillations, climate/productivity events have been established. Sedimentary regime, primary marine productivity and oxygen conditions at the time of population replacement were reconstructed by means of a multiproxy approach. Climatic/oceanographic variations correlate well with Homo spatial and occupational patterns in Southern Iberia. It was found that low ventilation (U/Th), high river supply (Mg/Al), low aridity (Zr/Al) and low values of Baexcess coefficient of variation, may be linked with Neanderthal hospitable conditions. We attempt to support recent findings which claim that Neanderthals populations continued to inhabit southern Iberia between 30 and 28 ky cal BP and that this persistence was due to the specific characteristics of South Iberian climatic refugia. Comparisons of our data with other marine and continental records appear to indicate that conditions in South Iberia were highly inhospitable at 24 ky cal BP. Thus, it is proposed that the final disappearance of Neanderthals in this region could be linked with these extreme conditions., This work was financed by Projects REN2003-09130-CO2-01 and CGL2006-13327-C04-04 (MEC), project RNM 432 and Research Group RNM 179 (Junta de Andalucía). We also thank project CSD2006-00041 (TOPOIBERIA). We would like to thank the ODP Core Repository (Bremen, Germany) for their assistance with sampling, and the university of Bremen for the use of the XRF core scanner. Other geochemical analyses were performed at the “Centro de Instrumentación Científica” (University of Granada), the Department of Mineralogy and Petrology (University of Granada), and the Japan Agency for Marine–Earth and Science Technology (JAMSTEC) laboratories. Our thanks to E. Abarca, E. Holanda, J. Montes, C. Niembro and D. Ortega for their laboratory assistance. Dr. J.S. Carrion and one anonymous reviewer are greatly thanked for constructive comments and reviews. The authors also are grateful to P. González-Sampériz and A. Moreno for their stimulating suggestion. Thorough editing of the original English manuscript was done by M. Bettini.

4 pages, 1 table, 1 figure., The late survival of archaic hominin populations and their long contemporaneity with modern humans is now clear for southeast Asia1. In Europe the extinction of the Neanderthals, firmly associated with Mousterian technology, has received much attention, and evidence of their survival after 35 kyr BP has recently been put in doubt2. Here we present data, based on a high-resolution record of human occupation from Gorham’s Cave, Gibraltar, that establish the survival of a population of Neanderthals to 28 kyr BP. These Neanderthals survived in the southernmost point of Europe, within a particular physiographic context, and are the last currently recorded anywhere. Our results show that the Neanderthals survived in isolated refuges well after the arrival of modern humans in Europe., We thank all those who have participated in this project. The project Palaeomed was co-funded by the Government of Gibraltar and the European Union Interreg IIIB Programme Medocc. Palynological and geochemical investigations were funded by Fundación Séneca, Murcia, Spain, and Ministerio de Educación y Ciencia, DGI, Spain, respectively. Geomorphological work was funded by Ministerio de Educación y Ciencia, DGI, Spain.