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).     

New Late Cretaceous dinosaur findings from northwestern Transylvania (Romania)

In 1905, Nopcsa tentatively identified a fragmentary rib from the Jibou Formation at Someş Odorhei as belonging to an ornithopod dinosaur. Therefore, he concluded that the base of this formation is Late Cretaceous, but this hypothesis was subsequently ignored or rejected by other authors. New dinosaur bones discovered in this locality by new excavations are here interpreted as belonging to the euornithopod Zalmoxes shqiperorum Weishampel, Jianu, Csiki and Norman, 2003. The base of the Jibou Formation can therefore be regarded as Maastrichtian, correlative to the Sânpetru Formation and to the middle member of the Densuş Ciula Formation from the Haţeg Basin, as well as the base of the Şard Formation in the southwestern Basin of Transylvania, in the Alba Iulia area. The presence of Zalmoxes at Someş Odorhei also confirms the northeastern extension for the ‘Haţeg Island’ in Transylvania.     

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.     

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).     

Crocodilian remains from the Upper Eocene of Dor-El-Talha, Libya

Study of undescribed material from Dor-El-Talha (Libya, Upper Eocene) reveals the existence of at least three different crocodilian taxa at this locality: a gavialid, a tomistomine and a mesosuchian represented by just one amphicoelous vertebra. Most of this material is fragmentary and it includes mainly fragments of snouts and lower jaws. The crocodilian fauna from this locality shows similarities with that from the contemporaneous El Fayum locality (Egypt).

Résumé

L’étude du matériel inédit provenant de Dor-El-Talha (Libye, Éocène supérieur) indique l’existence d’au moins trois taxons différents de crocodiliens : un gavialidé, un tomistomine et un mésosuchien représenté par une seule vertèbre amphicoele. La plupart de ces matériaux est fragmentaire et elle comprend principalement des fragments de museaux et mandibules. La faune crocodilienne de ce gisement montre des ressemblances avec celle provenant du gisement contemporain du Fayum (Egypte).     

La grotte Marcel Clouet à Cognac (Charente)

The Marcel Clouet Cave in Cognac (Charente) is a small cavity, more a shelter than a true cave, in the Cretaceous limestone cliffs along the Antenne, a tributary of the Charente River. The site suffered from a number of clandestine excavations before the work of C. Burnez, who was then followed by one of us (A.D.). The material recovered in stratigraphic context represents both Middle and Upper Paleolithic. The former is an example of Mousterian of Acheulian Tradition (MTA), while the latter includes Aurignacian (probably early) and Perigordian (probably Châtelperronian Gravettian), as well as some Solutrean objects recovered outside of stratigraphic context. It is important to note that this is one of only a few Charentian rockshelter sites, which has yielded an example of MTA.     

Le Moustérien en Croatie

This paper summarises results of the research on Middle Paleolithic of Croatia with a focus on Mousterian industry. The Hrvatsko zagorje (northwestern, continental part of Croatia) and Adriatic coast with its hinterland are physically divided by the Dinarid mountains, and present two different landscapes for the adaptation of Mousterian people. The sites in northwestern Croatia are represented by cave sites, while in Dalmatia, where the climate is milder, open-air sites are more frequent than the caves. During the early Mousterian of northwestern Croatia, Levallois method at Krapina and Vindija sites and cobble wedge method at Krapina [Journal of human evolution 32 (1997) 561-75] were used. Levallois debitage was also present in the late Mousterian assemblages from eastern Adriatic sites, but is absent in the late Mousterian of Hrvatsko zagorje. Sites on the eastern Adriatic coast are often characterized by tools of small size (like the ones of the so-called Micromousterian) and significant presence of denticulates and notched pieces. In both northwestern Croatia and Dalmatia Mousterian people effectively exploited local raw material sources and successfully adapted to different environmental conditions of these regions.     

Les derniers Homo heidelbergensis et leurs descendants les néandertaliens : datation des sites d’Orgnac 3, du Lazaret et de Zafarraya

This article presents the dating results recently obtained on three archaeological sites in Europe. At Orgnac 3 (Ardèche, France) from where the last Homo heidelbergensis fossils are associated with the first evidence of levallois technique, two speleothem formations from the 5b–6–7^th layers were U-Th dated with MC-ICPMS, giving an age range of 319–255 ka (2σ) (MIS 8–9), while the volcanic ash-bearing second layer was dated by ⁴⁰Ar/³⁹Ar, obtaining a preliminary date of 308.2 ± 6.8 ka (2σ). The combined ESR/U-Th dating of red deer enamel teeth from Lazaret cave (Alpes-Maritimes, France) attributed ages of 120–190 ka to the Acheulean and pre-Mousterian layers (MIS 6), which is in agreement with previous TIMS U-Th dates between 108 and 44 ka on calcite samples from the overlying TRA trench (MIS 5, 4, 3). At Zafarraya (Andalousie, Espagne), a number of ¹⁴C measurements on charcoal samples as well as combined ESR/U-Th dates on Capra and Equus dental enamels assigned the Mousterian artefacts and neandertalian fossils-bearing deposits an age interval between 42 and 34 ka (MIS 3).     

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).     

Faunal and taphonomic analyses of a Late Pleistocene bird-bone assemblage from a cave deposit in north-west Hungary

The paper presents a faunal and taphonomic discussion of the Late Pleistocene bird-bone assemblages excavated in Kálvária Cave n^o 4 near the city of Tatabánya in north-west Hungary. A total of 1150 complete and fragmentary avian remains were recovered from two locations on two separate occasions. Of these, 873 bones could be identified on the species-, family- or order-level. Fifteen of the identified 19 bird taxa could be determined on the species level and they indicate a habitat typical of forest margins. Several species yielded juvenile or subadult specimens, which in view of the breeding period means that these birds died during the summer, most probably between July and September.Each of the two assemblages had distinct characteristics. The high number of kestrel (Falco tinnunculus) long bones in Assemblage I generally included complete skeletal parts from subadult birds, suggesting a colony which bred in the cave, whose chicks died of natural causes. Even though the bones were exposed to a certain degree of water transport and soil corrosion, they were generally well preserved in the cave sediment. Size-characteristic analyses demonstrated that, in spite of the undeveloped morphological features, the sizes of limb bones usually corresponded to those of adult birds.The greater part of the material in Assemblage II originated from a stratified deposit and was dominated by small and fragmented remains of various taxa. The taxa which could be identified and the taphonomic features of the remains suggest that owl pellets formed the core of this bone assemblage.     

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).     

Le « Moustérien » de Tipasa et de Ténès (littoral ouest algérois) dans la lecture climatique du second pléniglacaire

The excavations that we undertook, in 1985, in the prehistoric site of Sidi Saïd, in Tipasa (Algeria), allowed us to observe an unusual archaeological stratigraphy. An aterian industry with pedunculated pieces, surmounted by a Mousterian, rich in scrapers and single-sided retouching points, almost systematically in flint, with reduced shapes and strongly reduced (Aterian under Mousterian). This unusual case has led us to consider the reading of the Mousterian-Aterian/Ibéromaurusien passage in a different way and at the same time to take a new look at the work carried out so far on the west coast of Algiers, especially those of Lower cave of the Tenes lighthouse, west of Tipasa. An attempt to compare and correlate the site of Sidi Said and the Lower Cave of the Ténès lighthouse, enabled us to consolidate our conviction on the existence of an aterian stratigraphically below the Mousterian and to discover an original lithic industry of Mousterian tradition, with strongly reduced forms, which would be placed between stratigraphically between the Aterian and the Iberomaurusian. This industry which does not yet have a name or place in the chronology, “curiously” recalls the case of the Middle Solutrean of southwestern Europe, in the context of the second pleniglacial.     

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).     

Sequencing mtDNA of the cave bearUrsus spelaeus from the Bavarian Alps is feasible by nested and touchdown PCR

Ancient DNA from bones of the extinctUrsus spelaeus Rosamueller et Hainroth, 1794 found in the Bavarian Alps has been amplified by PCR. Two out of five samples yielded a distinct band of 135 bp originating from the mtDNA control region. A combination of nested and touchdown PCR supported the amplification. Analysis of the nucleotide sequences revealed four transitions compared to the French cave bear sequence, the only cave bear data known so far (Genbank database X80259, AF121779). The consensus distant matrix tree clustered the two cave bears next to the brown bearUrsus arctos Linnaeus, 1758.     

A new baurusuchid crocodyliform (Archosauria) from the Late Cretaceous of Patagonia (Argentina)

A new baurusuchid, Wargosuchus australis gen. et sp. nov., coming from the Bajo de La Carpa Formation, Neuquén Province (Argentina), is described. This new taxon is based on a fragment of snout and a portion of the cranial roof. Wargosuchus differs from other crocodyliforms by possessing a deep median groove on the frontals, a contact between nasals and frontals extremely reduced, a large depression for the olfactory bulbs, three large foramina surrounding the large, smooth perinarial depression, and a hypertrophied, conical last premaxillary tooth followed by a large paracanine fossa. The finding of Wargosuchus in Patagonia (Argentina), a taxon with a strong resemblance to Brazilian baurusuchids, reinforces the hypothesis of a similar biota between both regions by the Late Cretaceous. Wargosuchus and Cynodontosuchus represent the only Argentinian mesoeucrocodylians to be included within Baurusuchidae. This finding extends the number of crocodyliforms from the Bajo de la Carpa Formation, which, in turn, corresponds to the most taxonomically diverse one in Argentina.     

A new primitive hadrosauroid dinosaur from the Early Cretaceous of Inner Mongolia (P.R. China)

The right dentary of a new hadrosauroid dinosaur, Penelopognathus weishampeli, has been discovered in the Bayan Gobi Formation (Albian, Lower Cretaceous) of Inner Mongolia (P.R. China). This new taxon is characterised by its elongated, straight dental ramus, whose lateral side is pierced by about 20 irregularly distributed foramina. Its dentary teeth appear more primitive than those of Probactrosaurus, but more advanced than those of Altirhinus, both also from the Lower Cretaceous of the Gobi area. Non-hadrosaurid Hadrosauroidea were already well diversified in eastern Asia by Early Cretaceous time, suggesting an Asian origin for the hadrosauroid clade. To cite this article: P. Godefroit et al., C. R. Palevol 4 (2005).     

Determination of the evolutionary mode of Austrian alpine cave bears by uranium series dating

Middle and Late Pleistocene sediments in many caves in Central and South Europe contain large numbers of bones and teeth of the cave bear (Ursus spelaeus). The cave bear differs in many characteristics from the recent brown bear and shows a rapid evolution especially in the changes of the teeth due to adaptation to pure herbivorous nutrition. The shifts of the morphotype frequencies of the fourth premolar from the upper jaw were used as a measure of the evolution. The uranium series method is the only suitable tool for the absolute age determination of the fossil bones with ages beyond the time range accessible to the radiocarbon method. By applying this method to the Herdengel cave profile the evolutionary rate of the cave bears was determined. Uranium series data from the fossil bones were partly verified by an independent carbonate speleothem age. For both, bone layers and carbonate formation found in stratigraphic relation, the determined ages correspond to a normal time sequence. According to the relatively fine time scale obtained by absolute dating, the evolutionary mode of the cave bears was determined as gradual. The main novelty of this study is the dating of the successive layers of the Herdengel cave and the determination of evolutionary stages of the cave bear in them.     

The last hadrosaurid dinosaurs of Europe: A new lambeosaurine from the Uppermost Cretaceous of Aren (Huesca, Spain)

A new hadrosaurid dinosaur, Arenysaurus ardevoli gen. et sp. nov., from the Late Maastrichtian of Aren (Huesca, South-central Pyrenees) is described on the basis of a partial, articulated skull, mandibular remains and postcranial elements, including vertebrae, girdle and limb bones. Arenysaurus is characterized by having a very prominent frontal dome; nearly vertical prequadratic (squamosal) and jugal (postorbital) processes, and deltopectoral crest of the humerus oriented anteriorly. Moreover, it possesses a unique combination of characters: short frontal (length/width approximately 0.5); midline ridge of parietal at level of the postorbital-squamosal bar; parietal excluded from the occiput; squamosal low above the cotyloid cavity. A phylogenetical analysis indicates that Arenysaurus is a rather basal member of Lambeosaurinae and the sister-taxon to Amurosaurus and the Corythosaurini-Parasaurolophini clade. The phylogenetic and biogeographical relationships of Arenysaurus and other lambeosaurines suggest a palaeogeographical connection between Asia and Europe during the Late Cretaceous.     

Révision taphonomique et techno-typologique des deux ensembles attribués au Châtelperronien de la Roche-à-Pierrot à Saint-Césaire

The Chatelperronian from la Roche-à-Pierrot in Saint-Césaire is characterized by its strong “Mousterian component”. It was discovered in a layer named Ejop, which had originally been sub-divided in two parts (Ejop SUP and Ejop INF). Up to now, the industry coming from these two sub-layers had been analyzed together without discriminating lithics discovered within the upper part from the ones discovered within the lower part. Here we present the results of our taphonomical and techno-typological analysis of the lithic industry attributed to each of the two sub-layers, including the artifacts discovered in 1993, in order to test if the strong “Mousterian component” of Ejop is shared by Ejop SUP as well as by Ejop INF. We show that the raw materials used at the site originate mostly from the local environment in both sub-layers, and that they are from a relatively low quality. Despite the small number of artifacts coming from Ejop INF, they are characteristics from a technological and typological point of view of the Mousterian, and not of the Chatelperronian. In contrast, the analyses of Ejop SUP cores show that method (volumetric blade production) and technic (marginal percussion) used are characteristic of the Chatelperronian. In Ejop SUP, scrapers still count for about half of the retouched stone-tools. Morphology and debitage technique for retouched stone-tools vary depending on the stone-tool type (end-scrapers and Chatelperron backed pieces are usually made out of blades removed with marginal percussion). Yet, it is not possible to separate within Ejop SUP two components, one Mousterian and the other one specific of the Chatelperronian, according to edge and surface damages of retouched stone-tools. We show that that Saint-Césaire Ejop layer contains two different sub-layer, a Mousterian one Ejop INF, and a Chatelperronian one, Ejop SUP. In the current state of knowledge on the site, it is not possible to decide whether the high proportion of scrapers in Ejop SUP is a testimony of retention of ancient method of production (if not ancient way of using stone-tools as hypothesized by Guilbaud et al.) or of post-depositional integration of Mousterian objects within a Chatelperronian context.