Hares and rabbits at Regourdou (Montignac-sur-Vézère, Dordogne, France): paleontological and taphonomic studies of two naturally-occurring bone accumulations

Depuis la fin du XIXe siècle, l’Europe occidentale a fait l’objet de très nombreux travaux pour étudier les modes de subsistance des sociétés préhistoriques. À partir du Paléolithique moyen, les Hommes vont alors s’intéresser au petit gibier, tels que les léporidés, taxons relativement abondants sur ce territoire. Or, distinguer l’origine de leur accumulation dans un site archéologique ne constitue pas une tâche aisée tant les agents pouvant en être responsables sont nombreux (i.e. mortalité naturelle, humains, carnivores terrestres, rapaces nocturnes ou diurnes). Dans cette contribution, nous avons mené des études taphonomique et paléontologique sur les léporidés de Regourdou, gisement moustérien ayant livré le squelette d’un Néandertalien. Les indices recensés suggèrent qu’aucun prédateur n’est intervenu dans les processus d’accumulation des restes de lièvres et de lapins, mais leurs assemblages seraient dus, respectivement, à une mortalité naturelle de type accidentelle et de type attritionnelle. La mise en évidence du premier processus montre que la cavité aurait fonctionné comme un aven-piège à un moment donné de son histoire, tandis que le second révèle l’existence d’une Garenne in situ, interprétée comme la dernière occupation du site durant le MIS 4 ou 3, avant la fin du comblement sédimentaire. Les variations morphologiques et de taille corporelle des individus permettent également de préciser les changements d’ordre paléo-environnementaux depuis le début du fonctionnement du site, confirmant l’attribution des niveaux inférieurs à la période tempérée du MIS 5, et les niveaux supérieurs à une phase plus récente du MIS 4 ou 3.Since the end of the nineteenth century, a great deal of work studying subsistence patterns of prehistoric societies in Western Europe has been done. During the Middle Paleolithic, humans were interested in small game, particularly the Leporidae, taxa that were abundant in their territories. However, distinguishing the exact nature of their origin in an archaeological site is not an easy task, given that numerous agents could be responsible for their accumulation (i.e., natural mortality, acquisition by humans and/or other terrestrial carnivores, or even nocturnal or diurnal raptors). In this contribution, we put forth a new taphonomic and paleontological study of the leporids of Regourdou, a Mousterian site that has yielded a Neandertal skeleton. This study suggests that no predators were involved in the accumulation of the hare or rabbit remains, but rather that they are due to natural (accidental) mortality for the former, and natural (attritional) mortality for the latter. Specifically, the evidence suggests that at one point in its history (for the hares), the cavity functioned as a natural pitfall trap, while for the rabbits it appears to show the existence of a warren, which we interpret as having existed during the last occupation of the site during MIS 4 or 3, before the end of the accumulation of sediments in the site. Morphological variation and body size of individuals also allows us to specify the order of paleoenvironmental changes since the site’s functional beginning, confirming the attribution of the inferior levels to the MIS 5 temperate period, and the upper levels to a more recent phase in MIS 4 or 3

Importance of field data for understanding a potential Mousterian funerary deposit : the case of the Regourdou 1 skeleton (Montignac-sur-Vézère, Dordogne, France)

Aside from the work of Bonifay (see Bonifay et al. 2007 for one of the more recent papers) and various articles following these earlier works (e.g., Binant 1991, Defleur 1993, Maureille et Vandermeersch 2007, Pettitt 2011, see also May 1986 for a more critical analysis), the in situ position of the remains of Regourdou 1 from layer 4 has never actually been discussed on the basis of available data from the salvage operation carried out in October 1957 by E. Bonifay and G. Laplace-Jauretche, under the administrative authority of François Bordes, or from the subsequent, more systematic, excavations directed by E. Bonifay between 1961 and 1964. Via the compilation of available information from a number of unpublished documents (François Bordes’ field notes, drawings made during the salvage operation, photographs taken in 1957, 1961 and 1962, as well as databases from the 1961 to 1964 excavations), and also a new inventory of human remains (both previously known and recently discovered), it is now possible to more accurately reconstruct the position of the human remains in a Cartesian system. In this, we assume that the concentration of remains uncovered during the salvage operation was in square G2, according to the preliminary systematic excavations carried out in 1961. They also bring to light that while practically no anatomical connections can be demonstrated with any certainty – and despite significant disruptions (all of the hominin remains are spread over 9 squares : G1 to G3, F1 to F3, E1 and E2, D2) – they are mainly positioned in squares G2 and G3 to some degree with respect to the anatomical logic of the human body. We therefore assume that Regourdou 1 was lying flat, with its head to the west – perhaps upon its trunk – close to the wall of the cavity. This result is different from the fetal position hypothesis proposed in Bonifay et al. (2007). Moreover many post-depositional (albeit Pleistocene) disturbances are also evident. We believe that they were likely the result of the utilization and modification of the cavity by brown bears and lagomorphs.Only new excavations at the site, and a better taphonomic understanding of Bonifay’s (1964) layer 4 (in which Regourdou 1 was found), and the exact role of humans in its formation, i.e., their anthropic impact on the layer, will allow us to discuss in more detail the nature of the deposition of the body, and, hopefully, the absence of the skull

Lièvre et lapin à Regourdou (Montignac-sur-Vézère, Dordogne, France) : études paléontologique et taphonomique de deux accumulations osseuses d’origine naturelle.

23 pagesSince the end of the nineteenth century, a great deal of work studyingsubsistence patterns of prehistoric societies in Western Europe has been done. During the Middle Paleolithic, humanswere interested in small game, particularly the Leporidae, taxa that were abundant in their territories. However,distinguishing the exact nature of their origin in an archaeological site is not an easy task, given that numerous agentscould be responsible for their accumulation (i.e., natural mortality, acquisition by humans and/or other terrestrialcarnivores, or even nocturnal or diurnal raptors). In this contribution, we put forth a new taphonomic and paleontologicalstudy of the leporids of Regourdou, a Mousterian site that has yielded a Neandertal skeleton. This study suggests thatno predators were involved in the accumulation of the hare or rabbit remains, but rather that they are due to natural (accidental) mortality for the former, and natural (attritional) mortality for the latter. Specifically, the evidence suggests thatat one point in its history (for the hares), the cavity functioned as a natural pitfall trap, while for the rabbits it appears toshow the existence of a warren, which we interpret as having existed during the last occupation of the site during MIS 4or 3, before the end of the accumulation of sediments in the site. Morphological variation and body size of individuals alsoallows us to specify the order of paleoenvironmental changes since the site’s functional beginning, confirming theattribution of the inferior levels to the MIS 5 temperate period, and the upper levels to a more recent phase in MIS 4 or 3.Depuis la fin du XIXe siècle, l’Europe occidentale a fait l’objet de très nombreux travaux pour étudier les modesde subsistance des sociétés préhistoriques. À partir du Paléolithique moyen, les Hommes vont alors s’intéresser au petitgibier, tels que les léporidés, taxons relativement abondants sur ce territoire. Or, distinguer l’origine de leur accumulationdans un site archéologique ne constitue pas une tâche aisée tant les agents pouvant en être responsables sontnombreux (i.e. mortalité naturelle, humains, carnivores terrestres, rapaces nocturnes ou diurnes). Dans cettecontribution, nous avons mené des études taphonomique et paléontologique sur les léporidés de Regourdou, gisementmoustérien ayant livré le squelette d’un Néandertalien. Les indices recensés suggèrent qu’aucun prédateur n’estintervenu dans les processus d’accumulation des restes de lièvres et de lapins, mais leurs assemblages seraient dus,respectivement, à une mortalité naturelle de type accidentelle et de type attritionnelle. La mise en évidence du premierprocessus montre que la cavité aurait fonctionné comme un aven-piège à un moment donné de son histoire, tandis quele second révèle l’existence d’une Garenne in situ, interprétée comme la dernière occupation du site durant le MIS 4 ou3, avant la fin du comblement sédimentaire. Les variations morphologiques et de taille corporelle des individuspermettent également de préciser les changements d’ordre paléo-environnementaux depuis le début du fonctionnementdu site, confirmant l’attribution des niveaux inférieurs à la période tempérée du MIS 5, et les niveaux supérieurs à unephase plus récente du MIS 4 ou 3

Rabbits in the grave! Consequences of bioturbation on the Neandertal "burial" at Regourdou (Montignac-sur-Vézère, Dordogne)

17 pagesInternational audienceThe understanding of Neanderthal societies, both with regard to their funerary behaviors and their subsistence activities, is hotly debated. Old excavations and a lack of taphonomic context are often factors that limit our ability to address these questions. To better appreciate the exact nature of what is potentially the oldest burial in Western Europe, Regourdou (Montignac-sur-Vézère, Dordogne), and to better understand the taphonomy of this site excavated more than 50 years ago, we report in this contribution a study of the most abundant animals throughout its stratigraphy: the European rabbit (Oryctolagus cuniculus). In addition to questions surrounding the potential bioturbation of the site's stratigraphy, analysis of the Regourdou rabbits could provide new information on Neandertal subsistence behavior. The mortality profile, skeletal-part representation, breakage patterns, surface modification, and comparison with modern reference collections supports the hypothesis that the Regourdou rabbit remains were primarily accumulated due to natural (attritional) mortality. Radiocarbon dates performed directly on the rabbit remains give ages ranging within the second half of Marine Isotope Stage 3, notably younger than the regional Mousterian period. We posit that rabbits dug their burrows within Regourdou's sedimentological filling, likely inhabiting the site after it was filled. The impact of rabbit activity now brings into question both the reliability of the archaeostratigraphy of the site and the paleoenvironmental reconstructions previously proposed for it, and suggests rabbits may have played a role in the distribution of the Neandertal skeletal remains

Late Pleistocene (MIS 3-4) climate inferred from micromammal communities and δ18O of rodents from Les Pradelles, France.

12 pagesInternational audienceThe middle Paleolithic stratigraphic sequence of Les Pradelles (Charente, France) spans from the end of Marine Isotope Stage (MIS) 4 until the middle of MIS 3. Micromammal remains are present in all the stratigraphic levels, offering a rare opportunity to address the questions of both environmental and climatic fluctuations throughout this period. Climate modes were studied through the taphonomy, biodiversity and oxygen isotope compositions of phosphate (δ18Op) from 66 samples of rodent tooth enamel. The δ18Op values from the lower sedimentary levels provide summer mean air temperatures of 19 ± 2°C (level 2/1) and of 16 ± 2°C (levels 2A, 2B and 4A). Within the middle of sequence (level 4B), a paleobiodiversity change can be identified with an increase of Dicrostonyx torquatus, which is associated with the largest amplitude in δ18Op values and the highest maximal δ18Op values. At the top of the sequence (level 5-2), a biodiversity change is observed with the increase of Microtus arvalis, but without any change in δ18Op values. The association of cold rodent species with unexpected high and large amplitudes in the δ18Op values of their teeth, possibly indicative of aridity, suggests their deposition during a Heinrich event

Le Moustier : un siècle après Peyrony, la reprise des fouilles.

2 pagesNational audienc

Record of Nile seasonality in Nubian neonates.

20 pagesInternational audienceThe oxygen isotope compositions of bones (n = 11) and teeth (n = 20) from 12 Sudanese individuals buried on Sai Island (Nubia) were analysed to investigate the registration of the evolution of the Nile environment from 3700 to 500 years BP and the potential effects of ontogeny on the oxygen isotope ratios. The isotopic compositions were converted into the composition of drinking water, ultimately originating from the Nile. δ(18)O values decrease during ontogeny; this is mainly related to breastfeeding and physiology. Those of neonates present very large variations. Neonates have a very high bone turnover and are thus able to record seasonal δ(18)O variations of the Nile waters. These variations followed a pattern very similar to the present one. Nile δ(18)O values increased from 1.4 to 4.4 ‰ (Vienna Standard Mean Ocean Water) from the Classic Kerma (∼3500 BP) through the Christian period (∼1000 BP), traducing a progressive drying of Northeast Africa