Zooarchaeological analysis of the Raşcov 8 Upper Palaeolithic site (Republic of Moldova)

The Palaeolithic site of Raşcov 8, discovered in the 1950's, was recently subjected to new investigations. It yielded archaeological layers from the Upper Pleniglacial. We used zooarchaeological methods to deepen knowledge about this site. We focused on the taphonomy, the anatomical representation of the different species and the anthropogenic activities to better determine the use of natural resources by humans, in particular of animal origin, to understand which strategies were used, the technocultural practices and territory occupation. The taphonomic observations are quite typical of a dry and cold environment. They also suggest that the 3 and 3a layers result from the same or chronogically closely occupations, affected by soil movements. Concerning the anthropogenic features, repeated short-term occupations, on a seasonal basis, mainly hunting and butchering activities of one or several small human groups have been highlighted. Whereas in the older layer humans exploited the carcass of a mammoth, in the other layers they hunted reindeer and horses and butchered the carcasses on the site, probably transporting some parts elsewhere. Whereas the lithic industries are different between layers 4/3-3a (Epiaurignacian) and 2/1 (Epigravettian), the subsistence behavior is similar and quite typical of Molodovian.     

A brachiopod shell show during the middle Cenomanian in the stratotype area (France) – exceptional residual colour pattern

The Mid. Cenomanian terebratulid brachiopod Sellithyris cenomanensis Gaspard, 1982 displays preserved residual colour patterns as pale radial bandings. A parallel is made with the common Triassic Coenothyris vulgaris (Schlotheim, 1820) and some extant species. The colour pattern is unequal comparing the dorsal and ventral valves of one specimen, and in the representatives of a sampled population. This ornamentation, not easily detected, is highlighted using ultraviolet (UV) light. Considerations concerning the pigments involved, their function and at least their alteration over time are tentatively analysed.     

Paleoecological and microenvironmental aspects of the first European hominids inferred from the taphonomy of small mammals (Sima del Elefante,Sierra de Atapuerca,Spain)

Unit TE9 of the Sima del Elefante (Sierra de Atapuerca, Burgos, Spain), where the remains of Homo sp. have been discovered (1.2–1.3 Ma), is also a level rich in small mammals. The taphonomic study of these small vertebrates sheds light on the landscape that provided the setting for the activities of these early hominids and allows us to describe what the cave was like during the formation of the level. Small mammal predators identified in the study indicate that during this period the Sierra de Atapuerca was part of a large biome consisting of semi-open riparian forests with meadows nearby. Postdepositional alterations reveal that the production of fossils took place outside the cave, being transported inside by water currents. During the formation of TE9, the cave presented conditions of high humidity, which made it difficult for hominids to establish occupations inside, although these conditions became somewhat less severe in TE9c, the sublevel where human remains are found.     

A palaeornithological assemblage from the early Pliocene of the Mediterranean island of Mallorca: Raptorial birds as bioaccumulators at Na Burguesa-1

A palaeornithological assemblage from the early Pliocene of Mallorca (Balearic Islands) is documented on 583 fossil bones from Na Burguesa-1 site. Ten different taxa have been identified: two Tytonidae, one small-sized Strigidae, one Phasianidae, one Charadriiform, and at least five Passeriformes. The specimens included in the Tytonidae correspond to a giant Barn Owl, Tyto sp. 1, with size similar to Tyto robusta, and a second Barn Owl, Tyto sp. 2, similar in size to Tyto sanctialbani. The small-sized Strigidae is attributed to Otus sp., although some of the pedal phalanges obtained are included only tentatively in this genus. The presence of these nocturnal raptorial birds combined with the prevalence of small vertebrates (mainly ranging from ca. 8 g to almost 1 kg) with practically unaltered bones suggests that this deposit was originated by the accumulation of prey remains of these owls.     

Rôle du gypaète barbu (Gypaetus barbatus) dans la constitution de l’assemblage osseux de la grotte du Noisetier (Fréchet-Aure,Hautes-Pyrénées,France)

Located in the Aure Valley (French central Pyrénées), the Noisetier cave opens at 825 m asl. This Middle Palaeolithic site has produced a Mousterian industry associated with a rich faunal assemblage. Bone remains are dominated by Chamois then Ibex and Red deer. Taphonomic analysis strongly suggests a human origin for the Ibex and the Red deer but questions arise for the Chamois. The chamois assemblage differed from the bones of both species by its low cut marks ratio. Semi-digested bones are particularly abundant. Differences are even more perceptible for skeletal portions. For Red deer and Ibex, long bone remains are mostly shaft portions whereas for Chamois, ends are the most abundant. Comparisons of the Noisetier cave bone assemblage with different present-day reference data leads to the conclusion that Chamois bones have mostly been accumulated by bearded vultures.     

Comparaisons taphonomiques de sites magdaléniens du Bassin parisien : les faunes de Ville-Saint-Jacques (Seine-et-Marne) et Étiolles (Essonne)

The preservation of faunal remains in the Magdalenian sites of the Paris Basin only occurs for one third of the cases. This taphonomic bias is very likely in relation with the open-air locations where the majority of regional sites have been discovered. Nevertheless, the Magdalenian settlement shows a certain variability across the landscape: lowland sites, hillside sites, rock shelter sites. This paper aims to highlight the potential interactions between such physical context variability and the taphonomical features of Magdalenian faunal preservations. The issues presented here mainly focus on the comparison of the two faunal remains’ assemblages of Étiolles (a lowland site of the Seine valley) and Ville-Saint-Jacques (hill side site closed to the Seine valley). These faunal assemblages have been studied using the same set of qualitative and quantitative criteria in order to facilitate direct comparisons. This paper must be viewed as the first step of a more systematical survey of Magdalenian faunal assemblages in the Paris Basin. Finally, the main goal of this survey aims to point out the respective zooarchaeological potential of such sites, and by the way, to reach their global socioeconomic significations.     

The Montceau-les-Mines Lagerstätte (Late Carboniferous,France)

The Montceau-les-Mines Lagerstätte (Late Stephanian, Late Carboniferous) is located northeast of the French Massif Central. Situated at equatorial latitudes during the Pennsylvanian, this Lagerstätte, probably a freshwater environment, preserves a rich and diverse flora (lycopsids, sphenopsids, ferns, pteridosperms, and cordaites) and fauna (bivalves, annelids, crustaceans, myriapods, insects, chelicerates, myxinoids, actinopterygians, sarcopterygians and tetrapods). These exceptionally preserved fossils can be found either flattened in shales or three-dimensionally preserved in sideritic nodules. The fossils from the nodules are exceptional for at least two reasons: the absence of major disarticulation of their body structure and the preservation of soft parts and extremely fragile cuticular structures. Such preservation was made possible by the combination of several factors: rapid burial in fine anoxic mud, early siderite precipitation (inducing the nodule formation) and phosphatization of cuticles and soft-bodied features.     

Fossil bats from the Late Pleistocene site of the Aguilón P7 Cave (Zaragoza,Spain)

Bats (Chiroptera, Mammalia) are a valuable and independent source of palaeoenvironmental information in Quaternary sites because bat assemblages are not necessarily produced by the same processes as those of other small mammals. Here, we report a small collection of bats (MNI 15) from a cave infill of the Aguilón P7 (AGP-7) site (Zaragoza, Spain) dated Late Pleistocene (MIS 3). This is one of the rare localities south of the Ebro River (right bank) with Neanderthal tracks; therefore, the palaeoenvironmental data provided here may help us to understand Neanderthal history. Nine bat taxa were identified, viz. Rhinolophus ferumequinum, R. hipposideros, Myotis gr. myotis/blythii, M. cf. bechsteinii, M. emarginatus, M. daubentonii, Plecotus gr. auritus/austriacus, Hipsugo savii vel. Pipistrellus kuhlii/nathusii, and Miniopterus schreibersii. The presence of a high number of yearlings of the former four species suggests the presence of breeding colonies. The surprisingly high diversity of the sample indicates a variegated vegetation cover and relatively high humidity for the MIS 3 stage in the region.     

L’Homme fossile d’Asselar (actuel Mali). Étude critique,mise en perspective historique et nouvelles interprétations

During the well known Augiéras-Draper mission which took place in 1927 and 1928 between Dakar and Alger through the Sahara desert, T. Monod and V. Besnard discovered a human skeleton near the military post of Asselar in French Sudan (current Mali). Back in France, the fossil was given to the Institut de Paléontologie Humaine where M. Boule and H. Vallois were in charge of its study. This work was then published in 1932. After this first exhaustive study, Asselar man was barely used in anthropological studies, with the exception of O. Dutour's works in the 90's. The goal of this study is to understand why, despite some prestige, this fossil didn’t have the importance he was fated with its geographical and chronological position. Publications of the first third of the twentieth century, archives about this discovery and the skeleton it-self are in the center of this new analysis. Results show that because of the lack of specification about its unearthing and its dating, Asselar fossil is hardly usable in an anthropological perspective. It although shows that Boule et Vallois limited the study of this fossil to a discussion about the Grimaldi “race”, designation not use anymore. This race was created in 1906 by R. Verneau and the discussion of the relation between Asselar man and Grimaldi race was a virulent debate at this time. Finally, the study of Asselar skeleton with archeo-anthropological principles gave the opportunity to demonstrate, for the first time, a sepulchral context. This rehabilitation of Asselar fossil gives new perspectives which would be investigate with new approaches in dating, genetics, 3D imaging… and will fully contribute to discussions about North Africa peopling.