Oldowayen archaïque et Oldowayen classique de l’Afrique à l’Europe méditerranéenne

Analyzing lithic industries of Lower Pleistocene and beginning of Middle Pleistocene times allows to define three groups not clearly chronological but which reflect the cognitive evolution of prehistoric Men who knapped them and the constraints of the environment: - “Archaic Oldowan” industries in which raw flakes are dominant and no small tools retouched on flakes or debris are present; - “Classical Oldowan” industries in which raw flakes are dominant and small tools retouched on flakes and debris – especially scrapers – are present; - “Acheulean industries”, in which bifaces are present – generally in small proportions – and small retouched tools are increasingly standardized.     

Woodworking activities by early humans: a plant residue analysis on Acheulian stone tools from Peninj (Tanzania)

The emergence of the Acheulian stone tool industry, between 1.7 and 1.5 m.y.a., constitutes one of the earliest evidences of complex behavior in the process of human evolution. The major technological breakthrough with the Acheulian industry was the beginning of the manufacture of bifacially shaped heavy-duty tools. Handaxes made with a predetermined form and a high degree of symmetry are the main characteristic of the Acheulian tradition. The tools are shaped through a long knapping sequence with a remarkable increase in the technical skills of the makers, compared with the older Oldowan tradition, implying a high degree of planning and foresight. Until recently, the function of these early bifacial tools remained unknown. A large number of these artefacts were found at Peninj in Tanzania, and phytolith analyses on handaxes have yielded for the first time unambiguous evidence of their function as woodworking tools.     

Atbarapur (Hoshiarpur district,Punjab), the Acheulian of the Siwalik Range within the South Asian context

The largest collection of Acheulian artefacts in the Siwalik region is from the site of Atbarapur in north-western India. The artefacts occur in reworked sediments of the Pinjore Formation, starting with the onset of the Pleistocene and continuing at places in this region till 0.6 Ma. The technical study shows two similar “chaînes opératoires”: one based on cobbles for making small flakes and the second based on boulders for large flakes. Both are short and simple: cores are not prepared and each of them produced about seven flakes. Handaxes and cleavers, typical Acheulian tools, are made on the large flakes, often struck from the ventral face of larger flakes (Kombewa method) or from split boulders. The technology compares well with the Lower Pleistocene Acheulian of peninsular India, but with slightly more refined bifaces. It also compares with assemblages from Africa and East Asia: Atbarapur stands as a milestone on the diffusion route(s) of the Acheulian.     

Diversity and multiplicity in the Asian Acheulian

The emergence of the Acheulian Techno-Complex in Asia appears to have occurred quasi-concurrently in the Levant, South Asia, East and South Africa. Throughout many parts of the huge geographical expanse of Asia, as elsewhere, this genesis was followed by the rapid diffusion of Acheulian techno-behaviors. This phenomenon of cultural radiation is attested in the archeological record throughout the Old World by an increased number of occurrences documenting growing demographic trends of Acheulian peoples, into the latter phases of the Middle Pleistocene. The “Homogeneity to Multiplicity Model” (HMM) is used here to provide a window for understanding the mechanisms behind the evolutionary changes observed throughout the very long duration and extensive geographical context of the Asian Acheulian. Since the beginning of the 19th century, Asia has continuously provided archeological evidence that is vital to our understanding of the “Acheulian revolution” and the plausible links it may have had with the appearance and evolution of Homo erectus s. l. The emphasis traditionally put on handaxes as hallmarks of Acheulian culture has falsely led many archeologists to propose models of cultural diffusion that have masked the true nature of the Acheulian as a worldwide phenomenon in which Asia has always played a key role.     

Dinosaur footprints from the Early Jurassic of Le Mazel (Lozère,Southern France)

During the 20^th century, the first dinosaur tracks of the Causses Basin were identified at Saint-Laurent-de-Trèves, in the Parc National des Cévennes (southern France). A recent excavation reveals a new theropod tracksite in the Hettangian deposits from Le Mazel, 2 km from the historical tracksite at Saint-Laurent-de-Trèves. The tracks are here described combining a biometric approach and 3D imaging photogrammetry. The main track-bearing surface bears 64 in situ tridactyl footprints preserved as concave epireliefs. Two morphotypes were identified, a “Grallatorid” morphotype and a “Kayentapus” morphotype. Footprints belonging to the first morphotype are closely similar to Grallator lescurei, Grallator minusculus, and Grallator sauclierensis. This study shows the difficulty to distinguish quite similar tridactyl tracks from an ichnotaxonomic point of view and highlights the importance of detailed biometric comparisons. Tracks are preserved in a brown to yellowish dolomudstone showing abundant cryptalgal laminites and mud cracks. These deposits were accrued in shallow environments such as intertidal and supratidal zones of a tidal flat.     

Barogali et l’Oued Doure. Deux gisements représentatifs du Paléolithique ancien en République de Djibouti

In the Republic of Djibouti, surveys and excavations, carried out from 1985 to 1992, confirmed the presence of the pre-Acheulean (Oldowan) and Acheulean sites in the country. Three seasons of excavations (1985-1987 in the Gobaad Basin, have unearthed in a hardened compact clay strata of an ancient marshland dating to the Lower Pleistocene, the fossilized skeletal remains of an Elephas recki ileretensis. Numerous stone tools have been gathered with the bones. The E.S.R. dating the elephant’s lower third molar gave a date between 1,.6 and 1,.3 MY that would confirm its paleontological grouping and the membership of this butchery site to the Oldowan period. The animal appeared to have been lying on its left side. The cranial roof had been separated from the calvarium, perhaps to get at the brain; but the skull remains in anatomic connection with the tusks. The jaw (mandible) seems to have been broken to extract the tongue. Hominids, perhaps Homo ergaster, knapped tools from a nearly outcrop of poor quality lava. The tools were specifically adapted to their needs, such as scraping, chopping and scattering the bones. The site has yielded 569 artifacts: utilized material and hammerstones (121); pebble tools (32); cores (14); “debitage” products (366); retouched flakes (36). Artifacts are rarely retouched and often broken. Five different types of choppers have been classified. The polyedrons and one bola make up 22% of the pebble tools. The cores are divided into unipolar, centripetal and polyhedrical types. In another site, Haïdalo, an almost complete skeleton of an Elephas recki recki in anatomical connection and without any sign of predation, has been found at eight kilometers from Barogali. During surveys in the Ali Sabîh region (1990-1992) seven sectors have been discovered and prospected in the Oued Doure Basin. On the surface area and also in situ into some little pits, 345 rhiolitic Acheulean artifacts have been found, near rhyolitic outcrop. These artifacts are generally large. The choppers (18) can be dividended into 2 sets : side choppers (55%) and end choppers (27%), often with a bifacial cutting edge. There is only one polyedron, but we have found eight heavy scrapers. The Acheulean group is important (43 tools). The bifaces are varied and there are also a few cleavers and picks. Cores are numerous (92) and Levallois cores are preponderant (45%). We find also centripetal cores (27%) and so unipolar, bipolar and polyhedral cores. Tools made of flakes (118) are numerous: scrapers are typologically diversified. Some of them have a double utilization. Notch tools, denticulate tools are presents but also end scrapers, burin, borer, back knifes and scantily retouched flakes. The characters of this lithic material, large cores and big flakes, large bifaces of various types, cleavers and retouched flakes, indicates that they are Acheulean products. So, the Doure Site can be placed in the Middle / Upper Acheulean transition.     

Migratory history of Rhinogobius sp. OR morphotype “Shimahire” as revealed by otolith Sr:Ca ratios

The migratory history of the Rhinogobius sp. OR morphotype “Shimahire” collected from a slower current environment in the Maruyama River, the Ibo River, and the Kako River, Japan, was studied by examining the strontium and calcium concentrations in the otoliths. The otolith Sr:Ca ratios of almost all samples showed consistently low ratios from the core to the edge, reflecting the fact that the organisms had been living in a freshwater environment their entire lives. The ratios of Rhinogobius sp. CB and Rhinogobius flumineus living in the sympatric habitats with the Rhinogobius sp. OR morphotype “Shimahire” in the Kako River showed an amphidromous and fluvial life cycle, respectively. These findings suggest that the Rhinogobius sp. OR morphotype “Shimahire” has a freshwater resident life cycle.     

Les plus anciennes industries paléolithiques en Russie

Early Paleolithic sites (Oldowan and Acheulian) in the European part of Russia are concentrated in the southern part of the Russian plain, in the piedmont of the Caucasus and in the North Caucasus, south from 50 N latitude. The Taman Paleolithic complex (sites of Bogatyri/Sinyaya Balka, Rodniki 1 and 2, Kermek; and localities of Tsymbal, Lisy and Peresyp), Akushin Paleolithic complex in Central Dagestan (sites of Aynikab 1, Mukhkay 1 and 2) and complex of sites in Maritime Dagestan (sites of Rubas 1, Darvagchay 1, Darvagchay-Zaliv 1 and 4) are discovered and studied. The initial human settlement of southern Russia began about 2 Ma and went through the Caucasian isthmus along the western shore of the Caspian Sea. The most ancient Homo of the first wave of settlement from the African ancestral homeland was able to reach the Caucasus and the southern part of the Russian plain by 2 Ma, as confirmed by the Liventsovka locality in the city of Rostov-on-Don. The Acheulian is represented by stratified sites of the Early Acheulian on the territory of Dagestan. At present, it can be argued that the territory of southern Russia was part of the area of initial human settlement from Africa. It is more difficult to estimate the time and ways of the initial human settlement of Northern Asia. The few sites attributed to the Lower Paleolithic are, for the most part, geologically unconnected or are questioned as to the authenticity of the artifacts. The only clearly stratified Middle Pleistocene site, Karama in the Altai, delivered a pebble tool industry. In addition, the finds of bifaces in Tuva, near the Mongolian border mark the northern limit of the distribution of the Acheulian in Asia.     

New Oldowan localities at high level within Kilombe Caldera,Kenya

New occurrences of early artefacts ascribed to the Oldowan tradition come from localities at high level within the caldera of the extinct Kilombe volcano, located in the central rift valley of Kenya. The trachyte cone and caldera of Kilombe volcano formed at ca. 2.5 Ma, and the record of >130 m of sediment-fill indicates that the caldera subsequently held a lake for long periods during the Early Pleistocene. The Oldowan artefact localities, dated by ⁴⁰Ar/³⁹Ar and palaeomagnetism to ～1.78 Ma, lie east of the centre of the caldera, on the west side of an ancient small lake, which later drained away as a gorge formed on the east side of the mountain. The artefacts are dominantly made of Kilombe trachyte, and are associated with a fauna of large animals including Hippopotamus gorgops. These are the first Oldowan localities to be discovered in a new area of the Kenyan rift valley in the last thirty years, and their presence at high level in rugged landscape indicates that the associated hominins were exploiting a full range of environments.     

First record of non-marine ostracods from the Paleogene “hamadian deposits” of Méridja area,west of Bechar (southwestern Algeria)

A new non-marine ostracod fauna from the Paleogene “hamadian deposits” outcropping west of Bechar (southwestern Algeria) has been recovered from lacustrine to fluvial deposits of the Oued Méridja section and fluvial deposits on the southern edge of the Hamada de Méridja section. Recently, these sections have been dated as late Thanetian – early Ypresian (latest Paleocene to earliest Eocene) and Ypresian – earliest Lutetian (early to earliest middle Eocene), respectively, based on charophytes. The associated ostracod fauna recovered consists of relatively mostly moderately to badly preserved specimens and comprises 14 taxa, none of which could be identified to species level in view of its poor state of preservation; we have nevertheless been able to identify and describe the following taxa: Herpetocypris sp., Cyprinotus? sp., Heterocypris? sp. 1 and sp. 2, Cypris? sp., Ilyocypris sp., Cytheroidea indet. sp. 1 and sp. 2, Limnocytheridae indet. sp. 1, Cypridoidea indet. sp. 1, Cyprididae indet. sp. 1, and Ostracoda indet. sp. 1, 2 and 3. Only Heterocypris sp. 1 occurs in both sections. Although the fauna can as yet not be related to the few other contemporaneous faunas reported from the wider palaeogeographic area, it adds important new information to our poor knowledge on Eocene non-marine ostracods in North Africa and southern Europe. The Méridja sections and area are promising regarding the discovery of more, better preserved material and further studies, and one main limitation to the correlation of the fauna is the hitherto insufficient taxonomic knowledge on many faunal elements of Eocene non-marine ostracods to which our section contributes considerably.     

The taxonomy,chronostratigraphy and paleobiogeography of glyptosaurine lizards (Glyptosaurinae,Anguidae)

Glyptosaurine lizards (Glyptosaurinae, Anguidae) are an extinct group of heavily armored lizards known from North America, Europe and Asia. Glyptosaurine lizards, taxa that possess fully developed tuberculated dermal armor, appear to have been established in North America by late early Puercan time (To3). “Proxestops,” a taxon distinguished by a combination of vermiculate and tuberculated osteoderm sculpturing, is considered to be a non-glyptosaurine, a sister taxon of the Glyptosaurinae. Known from only fragmentary remains, its wide chronostratigraphic distribution suggests that “Proxestops” is a form genus that, in all probability, represents more than one taxon, that ranges from the middle Paleocene to the early Eocene of North America. Moreover, the taxa Odaxosaurus piger, Parodaxosaurus sanjuanensis and “Proxestops” are best considered “proto-glyptosaurines”. “Melanosaurins” and glyptosaurins were well-established by the early Eocene, especially in North America, and are here documented by their type species and chronostratigraphic levels. Both tribes are present in Europe (MP7), too, but the record is not as estensive as that of North America. The North American taxon Gaultia silvaticus (Wa0) is transitional between a “melanosaurin” and glyptosaurin. Because it lacks the well-defined hexagonal osteoderms that characterize the Glyptosaurini, it is removed from that group and considered to be a “melanosaurin”. The “melanosaurin” taxon “Xestops” savagei (Wa4–Wa6) cannot be referred to Xestops (Br2) based on non-corresponding elements and because superficial similarity does not justify assignment to this taxon. Arpadosaurus sepulchralis (Wa6?), whose holotype is a fragmentary right frontal, is considered a subjective junior synonym of A. gazinorum, based on minor differences in the epidermal scale pattern that probably represent individual variation. “Glyptosaurus” agmodon (Wa6?), based on a partial right maxilla, cannot be referred to Glyptosaurus (sensu stricto), and the material upon which this taxon is based bears strong resemblance to material identified as cf. “?Paraglyptosaurus” yatkolai (Wa5–Wa6). “Glyptosaurus” rhodinos (Wa5) is based on an incomplete parietal, and its reference to Glyptosaurus is considered problematic. Eoglyptosaurus donohoei (Wa7) is probably valid and is re-established here. Glyptosaurus (sensu stricto) is known solely from the middle Eocene (Br2) by G. sylvestris. Dimetoposaurus wyomingensis (Br3) is removed from Xestops vagans because its synonymy was based on superficial similarities. Helodermoides tuberculatus, the largest and last glyptosaurin (Ch3), is restricted to the Chadronian of North America. Only the “melanosaurin” Peltosaurus granulosus (Or2–Or3), which includes the species P. abbotti, seems to have crossed the Eocene-Oligocene boundary, and appears to be largely restricted to the Orellan, but extended into the Arikareean. European glyptosaurines are also represented by both glyptosaurins and “melanosaurins” early in the Eocene (MP7). Placosauriops-like “melanosaurins” are known from Dormaal (MP7), and the glyptosaurin taxon?Placosaurus ragei occurs at the same level. “Placosauriops abderhaldeni” has been identified from the Grube Messel (MP11), but this assignment remains dubious because the species has not been adequately diagnosed, and the holotype species is from the Geiseltal (MP13), which is some 4.5 million years younger. Placosauriops weigelti (MP13) is the only valid species of this genus. Paraxestops stehlini (MP14) is not referable to the North American taxon Xestops, and its relationship to Placosauriops has not been studied. The late Eocene glyptosaurins Placosaurus estesi (MP17) and P. rugosus (MP18) are the last glyptosaurines known from Europe and appear to have gone extinct at the Eocene-Oligocene boundary, casulties perhaps of the “Grande Coupure”. Asian glyptosaurines are known solely from one species, Stenoplacosaurus mongoliensis, from the middle Eocene (Sharamurunian) of China. Glyptosaurines most likely originated in North America, diversified by late Paleocene time, and rapidly spread across the North Atlantic into Europe by the early Eocene. Both “melanosaurins” and glyptosaurins took a foothold in Europe by the early Neustrian, but the glyptosaurins, aside from one occurrence (Dormaal, MP7), were conspicuously absent for most of Neustrian through early Robiacian time. In North America, glyptosaurins diversified during the early and middle Eocene, while in Europe small “melanosaurins” were a prominent part of the paleoherpetofauna, and glyptosaurins are unknown for most of the Neustrian through the Geiseltalian, in both the fossilferous Lagerstätten of Messel and Geiseltal. Stenoplacosaurus is the only known glyptosaurin glyptosaurine from Asia, and its abrupt appearance during the late Eocene suggests the possiblity of a Beringian dispersal from North America into Asia.     

A new Mastodonsauroid Temnospondyl from the Triassic of Algeria: Implications for the biostratigraphy and palaeoenvironments of the Zarzaïtine Series,northern Sahara

We describe a new species of mastodonsauroid temnospondyl from Algeria, Stanocephalosaurus amenasensis nov. sp., on the basis of two exquisite skulls from a Lagerstätte found in the lowermost formation of the Zarzaïtine Series, Illizi Basin, in the area of “La Reculée”, In Amenas region, Algeria. The new species is characterized by subtriangular nostrils with concave lateral borders; small orbits; postfrontals posteriorly very wide; very elongate parietals; smoothly concave posterior margin of the skull; ovoid anterior palatal vacuities; very posteriorly pointed choanae; oval interpterygoid fenestrae; and a short anterior extension of the cultriform process of the parasphenoid. S. amenasensis is different than the Algerian taxa previously erected by Lehman (1971)–“Parotosaurus lapparenti” and “Wellesaurus bussoni”–which we consider nomina dubia. It enlarges the distribution of the genus in northern Gondwana and supports the Early-Middle Triassic age of the lowermost formation of the Zarzaïtine Series. It also suggests that the local palaeoclimate was very seasonal and these aquatic amphibians died massively in a dewatering sebkha.     

L'Ariétitidé du Lias de Corse

Only one piece of liassic ammonite is known in Corsica (SE of St. Florent in the “unité of Tuda”). It is a Arietitidae, probably Paltechioceras or Vermiceras (top or bottom of Sinemurian). The Lias of Tuda, similar to that of “écailles de Corté”, belongs to parautochtonous external realm.     

Secondary osteon size and collagen/lamellar organization (“osteon morphotypes”) are not coupled,but potentially adapt independently for local strain mode or magnitude

In bone, matrix slippage that occurs at cement lines of secondary osteons during loading is an important toughening mechanism. Toughness can also be enhanced by modifications in osteon cross-sectional size (diameter) for specific load environments; for example, smaller osteons in more highly strained “compression” regions vs. larger osteons in less strained “tension” regions. Additional osteon characteristics that enhance toughness are distinctive variations in collagen/lamellar organization (i.e., “osteon morphotypes”). Interactions might exist between osteon diameter and morphotype that represent adaptations for resisting deleterious shear stresses that occur at the cement line. This may be why osteons often have a peripheral ring (or “hoop”) of highly oblique/transverse collagen. We hypothesized that well developed/distinct “hoops” are compensatory adaptations in cases where increased osteon diameter is mechanically advantageous (e.g., larger osteons in “tension” regions would have well developed/distinct “hoops” in order to resist deleterious consequences of co-existing localized shear stresses). We tested this hypothesis by determining if there are correlations between osteon diameters and strongly hooped morphotypes in “tension”, “compression”, and “neutral axis” regions of femora (chimpanzees, humans), radii (horse, sheep) and calcanei (horse, deer). The results reject the hypothesis—larger osteons are not associated with well developed/distinct “hoops”, even in “tension regions” where the effect was expected to be obvious. Although osteon diameter and morphotype are not coupled, osteon diameters seem to be associated with increased strain magnitudes in some cases, but this is inconsistent. By contrast, osteon morphotypes are more strongly correlated with the distribution of tension and compression.     

Lochkovian (earliest Devonian) miospores from the Solimões Basin,northwestern Brazil

Eighteen core samples from PETROBRAS well 1-JD-1-AM (Jandiatuba area, Solimões Basin, northwestern Brazil) have been studied for miospores. Fifty-three species are identified. This assemblage is tentatively correlated with the Z Phylozone of the BZ Oppel Zone (Steemans, P., 1989. Palynostratigraphie de l'Eodévonien dans l'ouest de l'Europe. Professional Paper. Mémoires Explicatifs pour les Cartes Géologiques and Minéralogiques de la Belgique, 27, pp. 453.), dated late Lochkovian. This is in accordance with previous age determinations based on chitinozoans and acritarchs. Numerous representatives of the miospore genus Dictyotriletes are observed. These enable recognition of the Dictyotriletes emsiensis morphon, an informal classification unit which includes Dictyotriletes granulatus, D. emsiensis, Dictyotriletes cf. subgranifer, specimens previously misassigned to D. subgranifer and some Dictyotriletes spp. provisionally left in open nomenclature. Since all intermediate forms from typical D. granulatus to typical D. emsiensis coexist, it is currently difficult to determine the base of “E” Interval Biozone in South America as originally defined in Western Europe. It is suggested, therefore, that the base of the “Ems” Biozone defined in Brazil cannot be correlated with the base of the “E” Biozone. Instead, it should be included in an interval of uncertainty ranging from the European “Si” to “E” Biozones. Indeed, the underlying “NsZ” Biozone from South America contains species not known below the “Si” Biozone. Here, the D. emsiensis morphon Assemblage Zone is erected, which may be coeval with the “N” through “E” Biozones of Western Europe. The PISA palynoflora from the Paraná Basin is also attributed to this new biozone. However, in the absence of species observed in the “BZ” Biozone (and also in the Solimões Basin), the PISA assemblage could be somewhat older than that of well 1-JD-1-AM.     

Hand pressure distribution during Oldowan stone tool production

Modern humans possess a highly derived thumb that is robust and long relative to the other digits, with enhanced pollical musculature compared with extant apes. Researchers have hypothesized that this anatomy was initially selected for in early Homo in part to withstand high forces acting on the thumb during hard hammer percussion when producing stone tools. However, data are lacking on loads experienced during stone tool production and the distribution of these loads across the hand.Here we report the first quantitative data on manual normal forces (N) and pressures (kPa) acting on the hand during Oldowan stone tool production, captured at 200 Hz. Data were collected from six experienced subjects replicating Oldowan bifacial choppers. Our data do not support hypotheses asserting that the thumb experiences relatively high loads when making Oldowan stone tools. Peak normal force, pressure, impulse, and the pressure/time integral are significantly lower on the thumb than on digits 2 and/or digit 3 in every subject. Our findings call into question hypotheses linking modern human thumb robusticity specifically to load resistance during stone tool production.     

陕西洋县绿豆梁旧石器遗址出土的石制品

洋县绿豆梁遗址位于汉水北部一级支流金水河左岸的第四级阶地上。为了配合国家重点工程项目——南水北调西线“引汉济渭”工程的建设,2014～2015年对该地点进行了发掘,揭露面积126 m2,出土和采集不同类型的石制品656件。研究显示,早期人类加工石制品的原料来自于河漫滩或阶地古老砾石层中的砾石,岩性包括石英、石英岩、硅质灰岩、石英砂岩、花岗岩等。硬锤打击法是最主要的剥片方式。石制品包含石锤、石核、石片、石器、断块和碎屑等类型。遗址石器组合中既包括刮削器、尖状器、石钻等尺寸较小的轻型石器,也包含重型刮削器、砍砸器等重型石器。通过与位于相同阶地部位、相距2 km的金水河口遗址的测年数据和地层堆积序列对比,绿豆梁遗址的年代属于中更新世时期或更早的时段。     

Les organismes constructeurs dans les Annales de Paléontologie

Due to the variety of their systematic origins, the building organisms constitute a heterogeneous entity whose treatment in the “Annales de Paléontologie” can be appreciated according to multiple keys. The general systematic trend expressed through 100 years of history of the review is illustrated by many and rich monographic articles. The building organisms were only very rarely studied on their building capacity point of view. Thus the microbial organisms were only recently approached, with the study of the carbonated non-marine buildups, primarily resulting from the activity of cyanobacteries and algae. However various methods and approaches leaded significantly advances in the debate concerning taxonomic affinities of various building organisms as archeocyathids, stromatoporoids and chaetetids. Regarding the corals, the major contributions in the “Annales de Paléontologie” concern the methods privileging the skeletal microstructures analysis and the paleoecological considerations. Among the bivalves, the group of the rudists, which played an important role in the genesis of builded masses in Mesozoïc times, is treated under paleobiological point of view. Finally, acting of the building organisms, the “Annales de Paléontologie” reflects very well the topics of a paleontological community attached to the best possible use of effective systematic tools.     

The stone tools of capuchins (Cebus apella)

We examined the production of stone took by capuchins (Cebus apella). Eleven subjects used five reduction techniques to produce 346 stone tools (48 cores and 298 flakes). They produced a sharp edge on 83% of the cores and largest flakes. Three monkeys later used a sample of these objects as cutting tools. These results demonstrate that monkeys produce lithic tools analogous to those produced by Oldowan hominids.