Objectives: We provide the description and comparative analysis of all the human fossil remains found at Axlor during the excavations carried out by J.M. Barandiarán from to 1974: a cranial vault fragment and eight teeth, five of which likely belonged to the same individual, although two are currently lost. Our goal is to describe in detail all these human remains and discuss both their taxonomic attribution and their stratigraphic context. Materials and methods: We describe external and internal anatomy, and use classic and geometric morphometrics. The teeth from Axlor are compared to Neandertals, Upper Paleolithic and recent modern humans. Results: Three teeth (a left dm 2 , a left di 1 , and a right I 1) and the parietal fragment show morphological features consistent with a Neanderthal classification, and were found in an undisturbed Mousterian context. The remaining three teeth (plus the two lost ones), initially classified as Neandertals, show morphological features and a general size that are more compatible with their classification as modern humans. Discussion: The combined anatomical and stratigraphic study suggest that the remains of two different adult Neandertals have been recovered during the old excavations performed by Barandiarán: a left parietal fragment (level VIII) and a right I 1 (level V). Additionally, two different Neandertal children lost deciduous teeth during the formations of levels V (left di 1) and IV (right dm²). In addition, a modern human individual is represented by five remains (two currently lost) from a complex stratigraphic setting. Some of the morphological features of these remains suggest that they may represent one of the scarce examples of Upper Paleolithic modern human remains in the northern Iberian Peninsula, which should be confirmed by further testing.
A detailed geomorphological study was performed in the Atxurra‐Armiña cave system (northern Iberian Peninsula) to decode landscape evolution, palaeoenvironmental changes and human use of a cave within an Inner Archaeological Context. The results show an average incision rate of the river of <0.083 mm a–1 for at least the last 419 ka, with interruptions due to sedimentary inputs. Moreover, allostratigraphic units comprising fluviokarstic deposits at the base and flowstone formation at the top have been shown to be climatically controlled, formed either during glacial–interglacial cycles or during interstadial cycles. Finally, when the cave was used by humans in the Late Magdalenian, the lower entrance was closed, and they must therefore have entered the cave through the upper entrance. To reach the sectors selected to decorate the panels, they probably travelled from the upper cave level, as the current crawlway was wider than today, according to our U/Th dating. Once these visitors reached the panels, the floor in the main gallery would have been around 15 cm lower than at present. However, the morphology of the conduit was similar; this has significant implications for understanding and interpreting the human use of the cave during the Palaeolithic.
Cold-adapted faunal populations shifted southwards during the coldest episodes of the Middle and Late Pleistocene, reaching the Iberian Peninsula. In this context, some of these species, such as Coelodonta antiquitatis and Mammuthus primigenius extended throughout the territory, leaving evidence in, at least, 35 and 29 sites, respectively; however, in most cases, the evidence is scarce. Here we present the fossil assemblage from Mainea cave (Uitzi, Navarre, northern Iberian Peninsula), one of the sites yielding cold-adapted faunal remains closer to the Pyrenees. The cave possibly acted as a natural trap due to its external geomorphology (a sinkhole) and the absence of aerial exposure, anthropogenic marks or evidence compatible with this site being a hyena den. This site has yielded the most evidence of Coelodonta antiquitatis remains (NISP = 190) and one of the most abundant in terms of number of individuals (five, each with different ages at death) for the Iberian Peninsula, five remains attributed to a single Mammuthus primigenius and a single Cervus elaphus remain. The direct dating of a woolly rhinoceros tooth (46 354-44 428 2r cal. a BP) places Mainea within MIS 3, between the H4 and H5 Heinrich Events, during the Middle to Upper Palaeolithic transition, within a context of changes in human behaviour and human species replacement in Europe. We have performed the first collagen isotopic analysis for a woolly rhinoceros from the Iberian Peninsula. The d 13 C and d 15 N values of the Coelodonta antiquitatis remains are similar to other European sites, thus suggesting the presence of Mammoth steppe environments at relatively high altitudes, which would compensate for the southern latitude. This would be consistent with the presence of open environments in lower altitudes. This site expands our understanding of the ecology of coldadapted faunas at their furthest southern range limit during the Middle to Upper Palaeolithic transition.
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