Les ammonites traditionnellement regroupées dans la sous-famille des Bouleiceratinae (Hildoceratidae, Toarcien) : aspects phylogénétiques, biogéographiques et systématiques

The genera usually considered into the Bouleiceratinae subfamily belong in fact to different lineages of the Hildoceratidae family. An approach using paleogeographical, stratigraphical and morphological arguments on one hand and a cladistic approach on the other hand have allowed to separate 3 clusters with different paleogeographical and stratigraphical localisations. These are:

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the Bouleiceratinae s.s. (genera Bouleiceras, Nejdia and Kohaticeras) from lower Toarcian;

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the Leukadiellinae (genera Leukadiella and Renziceras) from middle Toarcian;

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and the Paroniceratinae (genera Frechiella, Paroniceras and Oxyparoniceras) from middle and upper Toarcian. These latters are mainly present and the Tethyan domain, but are also known in the NW of Europe and especially in France where new populations have been studied in the Causses, in the centre-ouest and in the Lyon area. New taxa have been erected here: Oxyparoniceras (Neoparoniceras) nov. sub. gen., O. (N.) brocardi nov. sp. and O. (N.) sciaui nov. sp.

     

Cristatopecten nov. gen. benoisti (Pectinidae, Bivalvia) du Chattien d'Aquitaine (France). Révision systématique et réflexions sur l'origine et l'évolution des Cristatopecten

The detailed study of a sample of “Pecten (Amussiopecten) benoisti” Cossmann and Peyrot (1914) from the Chattian outcrops of the Adour Basin, allowed to improve our knowledge of this species poorly known till now and to show its important ornamental variability. It follows that some nomenclatural points have been clarified at the generic level: we refute the attribution of this species to the genus Amussiopecten Sacco (1897) as used by authors—genus which was besides emended several times subsequently— and we propose its allocation to Cristatopecten nov. gen. Furthermore, this study allowed to remove the ambiguity existing originally as for the attribution of the species benoisti and burdigalensis to a same genus: our comparison of the latter two taxa shows that if benoisti has to be henceforth included in the new genus Cristatopecten (as its type species), burdigalensis (which is the type species of Amussiopecten) must be incorporated in the genus Flabellipecten Sacco (1897). The two genera Amussiopecten and Flabellipecten are therefore synonymous, as Depéret and Roman had already stated in 1910. The Cristatopecten from the Old World seem to be derived from a group of “Aequipecten” notably known in the Italian Rupelian, the group of “Aequipecten deletus” (Michelotti, 1861), of which we study here a sample from the Aquitaine Chattian. In the Aquitaine Basin, the Cristatopecten are represented, in the Chattian, by Cristatopecten benoisti (Cossmann and Peyrot, 1914); in the Lower Aquitanian, by C. praehaueri (Bongrain, Cahuzac and Freneix, 1994); in the Burdigalian-Langhian of the Saubrigues paleocanyon, by C. haueri (Michelotti, 1847) and C. miogallicus (Cossmann and Peyrot, 1914). During the whole Neogene, they spread and evolved in the Tethys and the Paratethys areas, and seem to have become extinct in the Pliocene with the disappearance of C. cristatus (Bronn, 1827), a species that we consider not as an Amusium s.s., but as the last representative of the Cristatopecten phylum.     

Diaceratherium massiliae nov. sp. des argiles oligocènes de Saint-André et Saint-Henri à Marseille et de Les Milles près d’Aix-en-Provence (SE de la France), premier grand Rhinocerotidae brachypode européen

A revision of all previously collected mammalian fossils from the two Late Oligocene sites of Saint-André and Saint-Henri in Marseille (both from the MP 26 reference-level) allows us to identify three Rhinocerotoidea species: Protaceratherium albigense, Ronzotherium romani, Diaceratherium massiliae nov. sp., and maybe a fourth one, Eggysodon cf. gaudryi. Only the first two were previously known there. D. massiliae nov. sp. is found together with R. romani; it is the first case of sympatry ever known between the two genera. D. massiliae nov. sp. is then the most ancient Diaceratherium in Europe, where the genus was previously unknown before the MP 29 reference-level. It is a very large species whose limb bones proportions foreshadow these of the later species of the genus, especially D. lemanense from the Late Oligocene-Early Miocene. This suggests a possible phylogenetic link between D. massiliae nov. sp. and D. lemanense, and the coexistence of at least two different but partially contemporaneous lineages among the European Diaceratherium. In Les Milles near Aix-en-Provence, also from the MP 26 reference-level, the three species P. albigense, R. romani and D. massiliae nov. sp. were also found.     

Nouvelles données sur le genre Imerites Rouchadzé, 1933 (Ammonitida,Ancyloceratina) ; réponses et précisions apportées au travail de Bert,Delanoy et Canut, 2009

This work is mainly an answer to the work of Bert, Delanoy and Canut, on the genus Imerites Rouchadzé, and we add also some points to the knowledge of this genus. An answer is given for the implication of one of the authors (J.V.) of this present work, about the origin of the genus Imerites Rouchadzé, and some significant bibliographic references, not named in the 2009 work, are specified and placed in their context. The characteristics of the ornamental stage “Pseudoshasticrioceras” mainly defined by an oval and compressed section of the whorls and by regular ventrolateral clavi, well marked, which frame the venter in a typical way (Bert et al., p. 181), don’t allow to affirm the presence of this stage during the ontogeny of all species of the genus Imerites Rouchadzé, contrary to what Bert, Delanoy and Canut (p. 30, 31) wrote. The type-species of the genus Imerites Rouchadzé is made clear by the application of the rules of the I.C.Z.N. code. The article 23, with the paragraph 23.1 of the I.C.Z.N. code, imply the senior synonymy of Imerites cristatus (Orbigny) on Imerites giraudi (Kilian), even if the Kilian's species is still the type species of the genus Imerites Rouchadzé. The taxinomical validity of the species Imerites cristatus (Orbigny) is confirmed. Its morphological variability is clarified by the distinction of four referential morphotypes, Cristatus, Giraudi, Favrei and Raricostatum. Consequently, the assumption of a shape-dimensional dimorphism into the populations of the genus Imerites Rouchadzé is rejected, awaiting irrefutable proof. A new species, Imerites stephaniae sp. nov., is described. It was collected in the Gerhardtia sartousiana Zone, in the uppermost part of the Gerhardtia provincialis Subzone, and it is a probable ancestor of the cogeneric species of the Imerites giraudi Zone.     

Les Megacricetodon du gisement karstique miocène moyen de Blanquatère 1 (Pyrénées-Orientales, Sud de la France) : nouvelles espèces, implications biochronologique et phylogénique

Three Megacricetodon species are recognized in the Middle Miocene locality of Blanquatère 1 (Languedoc-Roussillon province, France). Two are new, the small-sized M. tautavelensis nov. sp. the medium to large-sized M. aunayi nov. sp., the third one being the already known M. “collongensis-gersii”, a medium-sized species found in other Miocene localities of the area. Size and morphology differentiate these species. Such a high number of contemporaneous species of the genus Megacricetodon is found for the first time in a Miocene locality in the region and indicate that the evolution of this genus in western Europe is likely more complicated. It may testify both of a biogeographical differentiation and of migration events. According to our calibration charts, the deposit is dated ca. 16 Ma ago. The position of Vieux-Collonges (MN 5) and Sansan (MN 6) on the biochronological scale is also discussed, as well as the estimated age of the biozonal boundaries MN 3/MN 4, MN 4/MN 5 and MN 5/MN 6.     

Le Middle Stone Age de la grotte du Porc-Épic (Dire Dawa, Éthiopie) : gestion des matières premières et comportements techniques

With the emergence of Modern Humans in Africa a new post-Acheulean culture seems to take form: the Middle Stone Age. Although the geo-chronological limits of this period remain unclear, it may however be characterised by behavioural modifications, in particular an important change in the relationship between humans and their environment. Theses changes may partially result from the diversification of stone-tool production techniques, as well as socio-economical conditions. Sites dating of this period show that flake types are more abundant and result from exploitation methods that become gradually more sophisticated from about 300ka.In this context, study of the lithic assemblage from Porc-Epic Cave in Ethiopia contributes to the knowledge about operative methods used during the Middle Stone Age. The combined production of flakes, blades, bladelets and points using various methods, a differential economy towards raw materials and the diversity of tool types produced, underline the large extent of technological variability that the Porc-Epic tool-makers were capable of. We may conclude that, in spite of certain differences concerning raw material acquisition, a chronological homogeneity exists in the production modes and their variability. This apparent homogeneity throughout the stratigraphical sequence underlines the difficulty of attributing a cultural characteristic to stone assemblages of this period.     

Intérêt de la TEP/TDM dans le bilan d’extension et le suivi des lésions osseuses du myélome multiple

Multiple myeloma (MM) is a malignant hemopathy characterized by a pathologic proliferation of plasmocyts in bone marrow. Detection of bone lesion is of great importance in initial extension screening and for the follow-up because it has an impact on therapeutic strategy. Plain radiographs do not have a good sensitivity for the detection of such lesions. Magnetic resonance imaging (MRI) is an interesting tool to detect diffuse bone marrow infiltration. We propose, based on the experience of our center and through a comprehensive review of the literature, to present the potential of [¹⁸F]-FDG PET/CT for the detection and the therapeutic strategy of bone lesions in MM.     

Les pistes dinosauroïdes du Trias moyen français : interprétation et réévaluation de la nomenclature

Numerous dinosauroid footprints which showing sometimes manus imprint mark were gathered, since 1960, from the lower sandstones Triassic formations of the eastern border of the Massif Central (France). Tracks bearing levels are dated from palynological, micropalaeontological and palichnological data. They belong to the period upper Anisian-lower Ladinian. The paleontological results show bipedal digitigrade reptiles with erected, long hind limbs, having also pentadactyl mani and (II-IV) tridactyl feet. The osteological feet inferred structure is like that of Ceratosauria of Late Triassic age. The skeletons of first Dinosauria, diversified already well, are known in summit Ladinian and lower Carnien and those of their ancestors, Dinosauriformes, in Ladinian. And, for this reason, the aniso-ladinian dinosauroid footprints are ascribed to these last animals which thus appeared earlier, to Anisan even to late Olenekian. The chirotheroid hands show a “pseudosuchian” origin which possibly took place during the late Olenekian; feet modifications of these Crurotarsi being characterized by I and V digits reduction and a meso-tarsal joint. The Anisian-Ladinian dinosauroid footprints are ascribed to the ichnospecies Coelurosaurichnus perriauxi and Anchisauripus bibractensis. The discriminant analysis computed from these latter ichnospecies, and others from the German Triassic, French and USA Hettangian indicate that C. perriauxi and A. bibractensis can not be included into Grallator sensu Lull, 1953 or Coelurosaurichnus of Franconie. By this way, these taxa are well original and till now, there was no reason to change their nomenclature. Nevertheless because the numerous changes of Grallator which gathers now, most of dinosauroid footprints, it could be possible to include them into Grallator for the feet and into Atreipus when the manus trace is connected with the foot.     

Un habitat de la fin du Mésolithique dans le Centre-Ouest de la France : L’Essart à Poitiers (Vienne)

The excavation of L’Essart (Poitiers) makes it possible for the first time in the west of France to understand a very particular habitat, along a river and very much marked by the firing activities. The substrate of the site assigns the shape of a dome surrounded to the east by the Clain River, to the west by a channel. Abundant vestiges allotted to the recent Neolithic lay in the lower half of a layer of brown silts. Immediately subjacent, a level of ten centimetres, located at the top of orange silts, contained burnt stones structures: 39 hearths (circular area posed flat approximately one meter of diameter) and 14 dismantled hearths. It is dated from the final Mesolithic by the extremely abundant lithic material discovered in the layer. Lithic industry is carried out in a preferential way on bajocians flints available on the slope (62%) and oxfordians flints (8%) known to approximately two kilometres. The principal characters of this industry are a frontal exploitation of core, a production of prismatic blades, many notches of Montbani type on the blades, asymmetrical trapezoids with concave truncations (of which Trapezoids of Payré), right-angled trapezoids with concave truncations, scalene triangles with flat retouches and arrows of Montclus. The analogies with Retzian (Vendée and Loire-Atlantique) are certainly numerous, but it is rather about a relationship in a vaster unit that remains to define. The non anecdotic presence of the arrows of Montclus involves the discussion on the question of the zones of contacts between Neolithic and Mesolithic of the second half of the VI^th millenium BC.     

Les sciuridés des gisements karstiques du Miocène inférieur à moyen du sud de la France : nouvelles espèces, phylogénie, paléoenvironnement

We describe sciurids from Lower and Middle Miocene karstic sites located in the south of France. Four new taxa are recognized here: Atlantoxerus martini nov. sp., Atlantoxerus sp. 1, Freudenthalia cuencae nov. sp. and Aragoxerus nov. sp. The last two genera are recognized for the first time in the south of France. A comparison with the Iberian peninsula is carried out, it tackles the problems of diversity, phylogeny and settlement. Hypothesis concerning the predation of these terrestrial squirrels and paleoenvironment is proposed.     

Restes humains dans les sédiments du Pléistocène inférieur de la région d'Orce et de Cueva Victoria (sud-est de l'Espagne)

This paper describes the human remains and other evidence of human presence (lithic artifacts) located in the early Pleistocene deposits of Orce and Cueva Victoria (SE Spain). We also discuss the age of those sites.     

Les cétacés des gravures rupestres néolithiques de Bangu-dae (Corée du Sud) et les débuts de la chasse à la baleine dans le Pacifique nord-ouest

The Neolithic site of Bangu-dae (6000-1000 B.C.), south-east of the Korean peninsula, presents numerous rock carvings of cetaceans (n = 46, 19.9% of the figures), and especially large species. Among these two families of baleen whales (Balaenidae and Balaenopteridae) and the sperm whale can be identified. This site also presents whaling scenes suggesting that the Neolithic populations who lived along the coast of Korea were among the first to take advantage of coastal whales. All these carvings give exceptional evidence on the prehistoric beginning of whaling.     

Les Spatangus du Miocène et du Pliocène de l’Ouest de la France

Numerous fragments of spatangoid echinoids have been discovered in the Pliocene deposits of Challans, in Vendée (western France). In spite of the fragmentary data of the samples, a reconstitution of a complete test could be realized using the different fragments and their symetrization. The general shape of the test, and its architectural and ornemental characters allow establishing the presence of the genus Spatangus in western France during the end of Neogene. It allows to precise the biogeography of the genus Spatangus and of the morphological group S. (S.) purpureus on the Atlantic coast after the Messinian crisis. The Pliocene species is compared to the Miocene Spatangus (Phymapatagus) brittanus, abundant in Anjou, Brittany and Touraine. This older species was refered to the subgenus Phymapatagus according to the presumed lack of primary tubercles on its posterior interambulacrum. The discovery of well-preserved specimens, with primary tubercles on every parts of the test, in the Middle Miocene of Brittany allows to refute this subgeneric distinction and to refer the species brittanus to the subgenus Spatangus (Spatangus). The presence of this subgenus in western France is finally confirmed from Middle Miocene to Pliocene.     

Caméras hybrides TEMP-TDM et semi-quantification du I-FPCIT : évaluation de l’apport de la TDM

Objectives

Tomoscintigraphy of dopamine transporters with ¹²³I-FP-CIT is nowadays essential to visualise impairment of nigro-striatal system for the diagnosis of parkinsonism and for the differential diagnosis of dementia. With the development of hybrid cameras (SPECT-CT), the CT contribution in nuclear neurology needs to be assessed in diagnostic and semi-quantification performances. The main purpose of our study is to compare attenuation correction using CT to attenuation correction using the linear algorithm of Chang. SPECT-CT with parallel collimation results were also weighed against fan beam collimation and the contribution of partial volume effect correction was studied in secondary objective.

Materials and methods

We used a trilinear phantom to define spatial resolution and an anthropomorphic striatal phantom to quantify the activity in striatal cavities. We compared the impact of attenuation and scatter correction on spatial resolution and semi-quantification in striatum. We performed the partial volume effect correction on reconstructed images according to the method of Rousset.

Results

Attenuation correction by CT did not improve significantly spatial resolution compared to the algorithm of Chang. The semi-quantification of ¹²³I-FPCIT in striata was not significantly different according to the various CA, but was significantly improved with CT attenuation and scatter correction. Partial volume effect correction improved the quantification from 40 to 60% in the striatal structures, when the activity was superior in at least twice the background noise.

Conclusion

SPECT-CT hybrid cameras increase spatial resolution and improve semi-quantification of ¹²³I-FPCIT because of CT attenuation and scatter correction. Another use of CT is the possibility of calibrating anatomic segmentation of striata for partial volume effect correction. Partial volume effect correction improves quantification and is essential for early diagnosis of nigro-striatal disease.     

Signification paléoécologique des assemblages de diatomées du Messinien dans le bassin de Melilla-Nador (Rif Nord-Oriental, Maroc)

In the Melilla-Nador basin, the diatomites represent one of the main sedimentary components of the Messinian together with reefal carbonate platforms. Two vertical sections were realised in the diatomitic levels from distal platform. Diatom assemblages are for the first time described in this basin. A total of 125 diatom species were determined: 73 centrics and 52 pennates. Significant diatom assemblages defined from the statistical analysis indicate ecological variations concerning diatomitic levels or parts of diatomitic levels. Using the data sets we propose paleoenvironmental models showing the complexity of the ecological interactions. This study point the permanence of opened marine environment, the impulse of cold waters from Atlantic origin, a general decrease in bathymetry in the Messinian marls-diatomitic series, the influence of the carbonate platform progradation and the occurrence of upwelling systems.     

Le genre d'échinide s dans les dans les localités du Pliocène et du Pléistocène d'Emilie (Italie du Nord)

The study of well-preserved Pliocene and Pleistocene s from Emi from Emilia is used to analyze the morphological variations of Mediterranean populations, to depict the relationship between fasciole shape and other morphological characteristics and to describe previously unpublished pedicellar valves. These new data allow to be two species distinguished: s (Müller) a (Müller) and s Pomel; six s Pomel; six species closely related to s are synonymi are synonymized: s and it and s Pomel, i Pomel, i and itS. and s Checchia-R Checchia-Rispoli, x Simonelli a Simonelli and the recent species from Mediterranean, s Mortensen Mortensen. s can be disti can be distinguished from s by its hear by its heart-shaped subanal fasciole, when the s one is reni one is reniform. Moreover, the frontal groove of s is deeper, t is deeper, the primary tubercles of the interambulacra 1 and 4 are less numerous, the petals are shorter and narrower, the labrum is shorter. As far as pedicellariae are concerned, the jags of the large tridentate ones are stronger and the base of the globiferous ones is bigger. Palaeoecological observations on outcrops of the Stirone River, in Parme region, show similar environmental affinities between fossil populations and recent populations from Mediterranean. The s fossils fossils seem to be preserved within their life environment, that is to say in shore sandy substrates.

Résumé

L'étude d'un groupe de spécimens bien conservés appartenant au genre Spatangus, trouvés, dans des localités pliocènes et pléistocènes de l'Émilie, permet d'exposer l'étendue de la variation dans les populations fossiles méditerranéennes, de rechercher les relations entre la forme du fasciole sous-anal et les autres caractères morphologiques et de décrire les valves des pédicellaires, qui n'étaient pas connues jusqu'alors. Ces nouvelles données conduisent à reconnaître deux espèces différentes : s (Müller) e (Müller) et s Pomel ; six Pomel ; six espèces voisines de s doivent prob doivent probablement tomber en synonymie : s et itS et s Pomel, i Pomel, i et itS. a et s Checchia-R Checchia-Rispoli, x Simonelli e Simonelli et l'espèce vivant actuellement en Méditerranée, s Mortensen Mortensen. Des observations paléoécologiques sur un échantillon fossile récolté sur les bords de la rivière Stirone près de Parme montrent des affinités bionomiques semblables chez les populations fossiles et celles vivant en Méditerranée.     

Le rôle des exploitations minières de la région d’Autun dans la constitution des collections paléontologiques

The birth of the oil shale industry, in the Autun basin (Saône-et-Loire, department in Burgundy), at the beginning of the 1830s, corresponded to a time during which the scientific progress in geology and paleontology was quite fast-paced. The development of the schist industry happened at a time when landmark works were published such as those by Louis Agassiz or Adolphe Brongniart. These scientists relied upon the on-going findings in the Autunois area. An outstanding dynamics was on its way. It brought about the updating of many samples sparking off important paleontological studies. A remarkable coordination set up between the industrial workers of the schist industry, the local scholars on the one hand and the National Museum of Natural History in Paris on the other hand. There resulted from it a frequent if not constant interest in the discovery of the fossils that the layers of schists – exploited with the aim of obtaining oil used as a quaffing product – can contain. This dynamics kept going on till the beginning of the 19th century. It was carried out by outstanding personalities such as Bernard Renault or Auguste Roche who were at the origin of the first collections gathered by the Society of Natural History in Autun, founded in 1886. But then, the findings were made rare. The mechanization of the chopping down and crushing of the schist did not any more offer the suitable conditions to discover new specimens. Anyway, the accumulated collections are already considerable and make of the Autunois one of the major places of great French paleontological progress in the years 1870 and 1880.     

Note sur la position de la tubérosité deltoïdienne (tuberositas deltoidea) et ses conséquences fonctionnelles

This work presents a study related to the position of the humeral tuberosity in hominoids, spider monkeys and some cercopithecoids. Results show that the most distal humeral tuberosities are not associated to extreme brachiator behaviours, contrary to great apes and human. The shortest extension of the deltoid’s insertion area on the brachiator primates’ humerus can be associated to the need of those ones to develop a strong brachialis anticus. Indeed, this muscle is very important for arm movements when brachiating.