Deux nouvelles tortues de l'Éocène inférieur de Saint-Papoul (Aude, France)

Two new turtles from the Lower Eocene of Saint-Papoul (Aude, France). Among the fossil turtles from of the Lower Eocene of Saint-Papoul (Aude, France), two new taxa of freshwater Testudinoidea are described. The first is a new species of the genus Palaeoemys, known before in the Lutetian of Germany. The second taxon is a new genus, also described on material of Pépieux-Cesseras and Eygalayes. To cite this article: S. Hervet, C. R. Palevol 2 (2003).     

The subfossil occurrence and paleoecological implications of Macrotarsomys petteri (Rodentia: Nesomyidae) in extreme southeastern Madagascar

Remains of a large-bodied species of endemic nesomyid rodent, Macrotarsomys petteri Goodman and Soarimalala, 2005, were identified from subfossil deposits recovered from Andrahomana Cave in extreme southeastern Madagascar. This recently described extant species was previously only known from a single specimen collected at a site about 450 km northwest of Andrahomana and with distinctly different forest habitat than currently found in the vicinity of the cave. Radiocarbon dating of remains of M. petteri from the cave site indicates that it persisted in the region subsequent to human settlement. Previous reports of a large member of Macrotarsomys from other Quaternary sites in southern Madagascar are almost certainly of M. petteri. It is proposed that this species once had a broad distribution across the southern portion of the island during a more mesic period and subsequent aridification of the region has led to its local extirpation across most of its former range. To cite this article: S.M. Goodman et al., C. R. Palevol 5 (2006).     

New Catarrhine fossils from Moroto II, Early Middle Miocene (ca 17.5 Ma) Uganda

During the 1998–2003 field seasons of the Uganda Palaeontology Expedition, dental remains of three catarrhine species were recovered from Moroto II, Uganda. Micromammals from the locality indicate a late Early Miocene to basal Middle Miocene (ca 17.5–17 Ma) age, younger than Rusinga (17.8 Ma), but similar in age to Buluk (17.2 Ma) and Kalodirr (17.2 Ma). This paper describes and interprets new catarrhines from the site, one of which is a victoriapithecid monkey, the second a new genus and species of small-bodied ape, and the third a large hominoid. A fourth species collected in the 1960's is attibuted to Afropithecus turkanensis. To cite this article: M. Pickford et al., C. R. Palevol 2 (2003).     

Faunes et paléoenvironnements des principaux sites archéologiques plio-pléistocènes de la formation de Nachukui (Ouest-Turkana, Kenya)

Faunas and paleoenvironments from main archaeological Plio-Pleistocene sites of the Nachukui Formation (West Turkana, Kenya). The Nachukui Formation is currently under archaeological investigation, especially within the Kalochoro (2.35 – 1.9 Myr) and Kaitio (1.9 – 1.65 Myr) Members. Six main archaeological sites have been excavated from this time period, which yield rich vertebrate faunas collected in situ or in close vicinity to the site. Paleontological studies help to precise the specific diversity for each site and increase our documentation for each Member with the discovery of new taxa. They allow to provide new informations about the biotope diversities exploited by Hominids and show a climatic tendency towards more humid environment between the Members. To cite this article: J.-P. Brugal et al., C.R. Palevol 2 (2003).     

Orycteropus (Tubulidentata, Mammalia) from Langebaanweg and Baard's Quarry, Early Pliocene of South Africa

Fossil teeth and bones of aardvarks are relatively common at Langebaanweg, an Early Pliocene site in western Cape Province, South Africa. The remains are compatible in size and most details of morphology to extant Orycteropus afer, and are the earliest fossils attributed to this species. Other Late Miocene to Early Pliocene localities in Africa have yielded smaller species of aardvarks, suggesting that the extant lineage evolved in southern Africa. Morphologically the genus Orycteropus has been remarkably conservative since at least the Early Miocene but it witnessed an overall increase in size through the Neogene. The species O. afer has been morphometrically stable since the Early Pliocene. These observations indicate that the evolutionary process in aardvarks is extremely bradytelic. To cite this article: M. Pickford, C. R. Palevol 4 (2005).     

Exploitation de la vesce commune (Vicia sativa L.) au Néolithique moyen dans le Sud de la France. Données carpologiques du site de Claparouse (Lagnes, Vaucluse)

Common vetch (Vicia sativa L.) exploitation during middle Neolithic times in Southern France. Archaeobotanical data from Claparouse (Lagnes, Vaucluse). Beginnings of common vetch cultivation are poorly documented. Domestication could have occurred in various places. Common vetch is recorded by rare seeds in pre-Neolithic and Neolithic sites but firm evidence of cultivation does not seem available before Roman times. The Neolithic site of Claparouse is providing evidence of utilization and probable cultivation as early as some 6000 years ago. Even if this pulse is nowadays only a fodder plant, it was more likely used as human food at that time. We do not know whether it was introduced in western Europe from the Near East or locally domesticated. To cite this article: L. Bouby, V. Léa, C. R. Palevol 5 (2006).     

Cave bears (Ursus spelaeus) from the Peştera cu Oase (Banat, Romania): Paleobiology and taphonomy

The 2002 discovery of the earliest European modern humans in the Peştera cu Oase (Romania) has led to systematic excavations of a bone bed (two levels), containing principally the remains of cave bears (ca. 5000 bones) and dated between 50 and 40 ka cal BP. The thanatocenosis corresponds mainly to a subadult and adult male utilization of the cavity. Levels 1 and 2 are distinguishable by different conservation processes demonstrating respectively low- and high-energy hydraulic transports. The heavy component of cannibalism may indicate bone processing for trace elements and/or a more omnivorous diet than is usually ascribed to cave bears. To cite this article: J. Quilès et al., C. R. Palevol 5 (2006).     

Le site de Tögi Ndrawa, île de Nias, Sumatra nord : les premières traces d'une occupation hoabinhienne en grotte en Indonésie

The site of Tögi Ndrawa, Island of Nias, North Sumatra: The first record of a Hoabinhian cave occupation in Indonesia. Although in Indonesia, Hoabinhian sites usually refer to large shell midden dated back from the Holocene period, the Tögi Ndrawa cave in the Island of Nias (North Sumatra) has revealed a thick shell accumulation, sealed in a cavity, and beginning with the end of the Late Pleistocene. Excavations have produced classical Hoabinhian pebble artefacts, a forest and coastal fauna, and human bones. Beyond the new chronological landmarks provided by these findings, they question the extension of the Hoabinhian phenomenon originating from continental Asia, and provide hints about human settlement and use of the environment at this period of prehistory. Pour citer cet article : H. Forestier et al., C. R. Palevol 4 (2005).     

Taxonomie du grand canidé de la grotte du Vallonnet (Roquebrune-Cap-Martin, Alpes-Maritimes, France)

The large canid of Vallonnet cave belongs to Xenocyon lycaonoides. Its remains are similar to the Xenocyon from Untermassfeld in Germany. X. Lycaonoides, and evoluated form of the Xenocyon genus, is characteristic of the second half of the Lower Pleistocene. The genus Xenocyon may be the ancestor of both Cuon and Lycaon.     

Nouvelle découverte dans le Nord-Ouest de Madagascar et répartition géographique des espèces du genre Palaeopropithecus

During the field-work of 2003 in the Narinda peninsula in the Province of Mahajanga (North-West of Madagascar), we found a Palaeopropithecus of large size in the new cave “Raulin Zohy”. This fossil differs in morphology and size from the remains coming from other sites of this area and belonging to a new yet undescribed species. This discovery proves that two species of this genus existed in the costal area of the Province of Mahajanga. This Palaeopropithecus attributed to maximus species allows a reconsideration of the geographical distribution of this subfossil lemur species, and asks an interesting question about the biogeography on the small new species.     

Nouvelles découvertes de dents d’hominidés dans le membre Kaitio de la formation de Nachukui (1,65–1,9 Ma), Ouest du lac Turkana (Kenya)

New hominid teeth from the Kaitio member (1.65–1.9 Myr) in West Turkana (Kenya). New hominid teeth have been recovered from the archaeological sites of Kokiselei 1 and Naiyena Engol 1. These two sites are located in the west side of the Turkana Basin and belong to the Kaitio member of the Nachukui Formation. They are dated between 1.65-1.79 and 1.7-1.8 Myr respectively. The four teeth (left maxillary canine and first molar, right maxillary third molar and left mandibular third molar) discovered in Kokiselei 1 are attributed to Australopithecus boisei. The right mandibular first premolar found in Naiyena Engol 1 is referred to Homo sp. aff. ergaster. To cite this article: S. Prat et al., C. R. Palevol 2 (2003).     

Invertébrés remarquables du Callovien inférieur de la Voulte-sur-Rhône (Ardèche, France)Remarkable Invertebrates from the Lower Callovian of la Voulte-sur-Rhône (Ardèche, France)

Remarkable Invertebrates from the Lower Callovian of la Voulte-sur-Rhône (Ardèche, France). The four-excavating field expeditions from 1983 to 1986 led to collect a considerable amount of new data from this exceptional paleontological site, which was neglected, and unexplored for the essential, until now. This paper presents a synthesis of the main available results. For the first time, the succession of the lithofacies is precised from all preserved deposits thick about 12 m. These observations reveal, on the whole, a great homogeneity of lithologic, paleobiologic or taphonomic characteristics, which denote a rather great constancy of the global environmental conditions. The lithofacies are schistous marls revealing former uncemented paleosubstrates, with clay very dominating (montmorillonite for 60–70%, calcium carbonate, siderite and limonite for less than 30% or 40%). The faunas are nearly exclusively composed of pelagic, nectopelagic or mesopelagic organisms (swimming in full water or dependent on free algal environments); they include very few benthic organisms. The marine water depth in this area would be estimated to have reached roughly 200 m. The surface and middle water strata, where lived the major part of organisms, must have been usually agitated, well oxygenated and illuminated. At the opposite side, the bottom water must have been very quiet and anoxic, in aphotic zona, which is responsible for the soft tissue mineralisation.     

Les sites archéologiques plio-pléistocènes de la formation de Nachukui, Ouest-Turkana, Kenya : bilan synthétique 1997–2001

Plio-Pleistocene archaeological sites in the Nachukui Formation, West Turkana, Kenya: synthetic results 1997–2001. Stretched along the western side of the Turkana Basin, the Nachukui Formation preserves a large number of Plio-Pleistocene archaeological sites. Research carried out by the WTAP documents hominid behavioral evolution and technical diversity, through a time period ranging from 2.35 Myr to 0.7 Myr and within a relatively precise chronostratigraphic and paleoenvironmental frame. This work is based on comprehensive excavations conducted between 1997 and 2001 at the Late Pliocene and Early Pleistocene site complexes of the formation. To cite this article: H. Roche et al., C.R. Palevol 2 (2003).     

Hyaenictitherium minimum, a new ictithere (Mammalia, Carnivora, Hyaenidae) from the Late Miocene of Toros-Menalla, Chad

A new species of Hyaenidae, Hyaenictitherium minimum, is described in the carnivore fauna of the Late Miocene layers of Toros-Menalla (Chad). Its size is similar to that of a jackal and it had probably a similar ecological niche. It is found in several fossil-bearing localities of this area. The genus Hyaenictitherium is known from the early Late Miocene in Eurasia from China to Spain; the Chadian material is, perhaps with some specimens from Sahabi and Lothagam, the earliest occurrence of the genus in Africa. It results certainly from Eurasian migration, which will have to be taken into account for the analysis of the bulk of the fauna. To cite this article: L. de Bonis et al., C. R. Palevol 4 (2005).     

Étude taphonomique, paléoécologique et archéozoologique des faunes de grands mammifères de la seconde moitié du Pléistocène inférieur de la grotte du Vallonnet (Roquebrune-Cap-Martin, Alpes-Maritimes, France)

Vallonnet cave (Alpes-Maritimes, France) provided archaic lithic tools together with a big amount of large mammals of the end of lower pleistocene. At the crossing of diverse ecological niches in time and space, three main levels and within them several smaller units were distinguished. The poorly mineralized bones witnessed a huge diagenetic fragmentation. The presence of the animals in the cave seems to be linked to the reasons of their death. The exhaustive and systematic observation of the bones, like the bears probably used to die inside the cave. Some other carnivores especially hyenas, used the cave as a nursery. Man also occupied the cave and had an activity mainly on large cervid bones and on some other species as well. The very progressive deposit gave a way for carnivores and porcupine to gnaw the bones on the ground before their burial. The succession of actions (man, carnivores and porcupine) on the same bones is characteristic on Vallonnet large mammals bones.     

Indications for a humid climate in the Western Desert of Egypt 11–10 Myr ago: evidence from Galagidae (Primates, Mammalia)

The timing of desertification of the Sahara Desert is poorly understood, with recent estimates indicating an onset of hyper-aridity during the Latest Miocene. Field work in Egypt in 2005 has led to the discovery of evidence that indicates that 11–10 Ma the Western Desert was covered in woodland. Fossiliferous cave breccia at Sheikh Abdallah, Western Desert, Egypt, has yielded a Late Miocene (11–10 Ma) microvertebrate fauna, which contains Galagidae, Microchiroptera, Macroscelididae, Soricidae, Erinaceidae, and Rodentia. The locality also yielded the remains of frogs, snakes, lizards, and birds. The fauna indicates a mean annual rainfall in excess of 500 mm and perhaps as much as 1,200 mm. This palaeoclimatic information is important because it reveals that the Sahara Desert, which is today the largest in the world, was either considerably smaller during the Late Miocene than it is today, or that it did not yet exist as a continuous hyper-arid belt right across the continent. This data accords with estimates of a Latest Miocene (8–7 Ma) increase in aridity in the Sahara. To cite this article: M. Pickford et al., C. R. Palevol 5 (2006).     

L'espace minéral au Paléolithique moyen dans le Sud du Massif central : premiers résultats pétroarchéologiques

The Middle Palaeolithic mineral environment in the South of the Massif Central: preliminary petroarchaeological results. Five Middle-Palaeolithic assemblages coming from archaeological sites in the Haute-Loire and Ardèche dated to isotopic stages 7 to 5 have been studied using a petroarchaeological method based on the optimization of observation techniques at different scales with respect to genetic and postgenetic characteristics of flint raw materials. The method reveals a relatively large collection area for the middle mountain sites (Sainte-Anne I, Baume-Vallée, Le Rond-de-Saint-Arcons, Rochelimagne), but apparently a smaller one for the site of Payre, located nearby the side of the Rhône Valley. For all sites, gathering is predominantly local, but some distant sources are utilised too. The rare exogenous materials, for example the Bedoulian flint from Ardèche identified in the Velay assemblages (Sainte-Anne I, Baume-Vallée) are in fact located in the heart of the massif as well as in secondary deposits and thus do not allow one to establish firm circulation routes for, or certain contact between the relevant human groups. To cite this article: P. Fernandes et al., C. R. Palevol 5 (2006).