Contribution à la connaissance des bivalves du Turonien d’Owendo dans le bassin côtier nord gabonais

The study of bivalves collected from Turonian deposits of Owendo region, within Gabonese coastal north basin, allows to identify 9 species belonging to 9 genera: Aphrodina dutrugei (Coquand 1862), Brachidontes eoexustus Klein and Ferreira 1979, Crassatella cf. pyrenaica d’Orbigny 1843, Entolium exilis (Reuss, 1854), Exogyra sp., Lopha sp., Mytilus cf. lineatus d’Orbigny 1844, Pholadomya adversa Riedel 1932 and Rastellum sp. Excepted A. dutrugei and P. adversa, which are known in Turonian localities of Gabon, other species are found here for the first time in Gabonese coastal basin. This is the same for genera named Brachidontes Swainson 1840, Entolium Meek, 1865 and Mytilus Linnée 1758. In Gabonese coastal basin, the stratigraphic and geographic ranges of the Crassatella genus are extended in Turonian and Owendo region respectively. The bivalve assemblage is dominated by specimens of Aphrodina genus. The bivalve specific diversity of Owendo region increase from 3 to 12 species.     

Rôle des organes pulsatiles thoraciques et du cœur pendant l'émergence et l'expansion des ailes des lépidoptères

Electrograms of the thoracic pulsatile organs and of the heart during emergence and expansion of the wings have been made. The mesotergal and metatergal organs function in a similar way: active periods are interrupted by short periods of rest, but the two organs contract with different but apparently independent rhythms. During emergence and expansion, the rate of contraction of the pulsatile organs increases twofold, and the resting periods disappear during the entire period of expansion of the wings. When the wings are removed or cut short, the activity of the pulsatile organs is inhibited.     

Tumeurs du grêle et du côlon : importance de l’anatomie en coupes

The aim of this article is to describe the anatomic specificities of each different digestive tumors in CT imaging and to show the interest of contrast-enhanced CT and bowel opacification. Some specific points about lymph nodes of the abdomen and peritoneum anatomy will be discussed.     

Effets du rubidium et du césium sur la croissance et la nutrition minerale des characees

Résumé Le rubidium et le césium introduits à l'état de chlorure dans le milieu de culture ont à faible dose un effet stimulant sur la croissance de Chara fragilis et de Chara vulgaris. La résistance de ces végétaux à l'action toxique des deux ions est accrue par l'addition de potassium au milieu.Les analyses chimiques confirment que le rubidium et le césium sont antagonistes vis-à-vis du potassium et du sodium alors qu'ils ne modifient pas de manière significative le taux de calcium.

---

Chara fragilis and Chara vulgaris were cultivated in a natural medium containing rubidium and caesium as chloride.The growth of Characeae was increased after culture in the solutions containing Rb and Cs in small amount. The resistance to the toxic effects of these two ions is enhanced if potassium chloride is added to the medium.Quantitative analyses indicate that Rb and Cs decrease the rate of Na and K but have no significative influence on the rate of Ca.

Université de Dijon, Laboratoire de Nutrition minérale des Végétaux     

Structure et fonctionnement des écosystèmes du Haut-Rhône français

Many abandoned stream channels are provided alternatively by river water or groundwater from the interstitial flow. The cyclopoid populations from an abandoned channel of the Rhône river are compared with those from a neighbouring interstitial station. Among the 18 species of cyclopoids found during the present study, only 4 are common to both stations. During 3 years of sampling, the populations living in interstitial waters were rather stable, while the epigean populations were more fluctuating. The latter seem to be influenced by the origin of the water.     

Le contrôle automatique du flux lumineux dans l'oeil composé des Diptères

In the compound eye of the fly Musca, tiny pigment granules move within the cytoplasm of receptor cells Nos. 1–6 and cluster along the wall of the rhabdomeres under light adaptation, thus attenuating the light flux to which the visual pigment is exposed (Kirschfeld and Franceschini, 1969). Two recently developed optical methods (the neutralization of the cornea and the deep pseudopupil) combined with antidromic and orthodromic illumination of the eye (Fig. 1) make it possible to analyse the properties of the mechanism at the level of the single cell, in live and intact insects (Drosophila and Musca). The mechanism is shown to be an efficient attenuator in the spectral range (blue-green) where cells Nos. 1–6 have been reported to be maximally sensitive (Figs. 4c and d, 5b and 11b). In spite of the fact that the granules do not penetrate into the rhabdomere, the attenuation spectrum they bring about closely matches the absorption spectrum of the substance of which they are composed (ommochrome pigment, dotted curve in Fig. 11b). The dramatic increase in reflectance of the receptors after light adaptation (Figs. 3, 4b, 5a and 11a) can be explained as a mere by-product of the high absorption index of the ommochrome pigment, especially if one takes into account the phenomenon of anomalous dispersion (Chapter 8). The vivid green or yellow colour of the rhabdomeres would thus have a physical origin comparable to a metallic glint. Contrasting with the lens eye in which the pupillary mechanism is a common attenuator for both receptor types (rods and cones), the compound eye of higher Diptera is equiped with two types of pupils adapted respectively to both visual subsystems. A scotopic pupil is present in each of the six cells (Nos. 1–6) whose signals are gathered in a common cartridge of the first optic ganglion. This pupil comes into play at a moderate luminance (0,3 cd/m² in Drosophila; 3 to 10 cd/m² in Musca. Figs 13, 14, 15, 16). A photopic pupil is present in the central cell No. 7 whose signal reaches one column of the second optic ganglion. Attenuating the light flux for both central cells 7 and 8, the photopic pupil has its threshold about two decades higher than the scotopic pupil, just at the point where the latter reaches saturation (Fig. 3b, e-State II of Figs. 6b and 15). The photopic pupil itself saturates at a luminance one to two decades higher still (Fig. 3c, f=State III of Figs. 6c and 15). The two-decades-shift in threshold of these pupil-mechanisms supports the view that receptors 1–6 are a scotopic subsystem, receptors 7 and 8 a photopic subsystem of the dipteran eye. The luminance-threshold of the scotopic pupil (as determined with the apparatus described in Fig. 2) appears to be located at least 3.5 decades (Drosophila) or even 5 decades (Musca) higher than the absolute threshold of movement perception (Fig. 16). After a long period (1 hr) of darkness a light step of high intensity can close the scotopic pupil within about 10 sec (time constant 2 sec as in Fig. 9) and the photopic pupil within no less than 30–60 sec. Some mutants of Drosophila possess only a scotopic pupil (w , Figs. 4 and 5) whereas ommochrome deficient mutants lack both types of pupil (v, cn, see Fig. 7c, d). Comparable reflectance changes, accomplished within about 60 sec of light adaptation, are described for two insects having fused rhabdomes: the bee and the locust (Fig. 17).     

Sur la disparition progressive de Laminaria digitata sur les côtes du Calvados (France)

In comparison with results from 1983–1988, when a cartographic study was made on the distribution of the Laminariales and of Sargassum muticum in Lower Normandy (France), we note, on the Calvados coast, a regression of Laminaria digitata which has almost disappeared on the Grandcamp rocks. On the contrary, the growth of the populations of Sargassum muticum is very spectacular at Grandcamp; in summer, 80 % of the substratum in the lower parts of the intertidal zone and in the subtidal are covered by this species.     

Étude palynologique du pliocène de la côte d'azur (France) et du littoral ligure (Italie)

Pollen analysis of Pliocene marine clays in coastal Alps paleogulfs is supported by biostratigraphic records according to foraminifers and accessorily to nannoplankton. From the seashore up to elevated areas, the region was occupied by forests mostly constituted by Gymnosperms (Taxodiaceae particularly). The Lower Pliocene vegetation was also characterized by local differences related to the substratum. Pollen assemblages changed in the Earliest Piacenzian; this event is probably to be related to a climatic fluctuation already evidenced in the Northwestern Mediterranean region.     

Alcaloïdes du Pandaca ochrascens

From leaves and root bark of Pandaca ochrascens ten alkaloids were isolated: apparicine, akuammicine, dehydro-19,20 condylocarpine, akuammidine, epi-16 dehydro-14,15 vincamine, ibogaine, iboluteine, ibogaline and also two new alkaloids, epi-19 ibogaine or (19R) 19-hydroxyibogaine and epi-19 iboxygaline or (19R) 19-hydroxyibogaline. The absolute configuration at C₁₉ of these new alkaloids and other alkaloids hydroxylated on 19 of the Iboga type is discussed.     

Eco-éthologie des nouveaux ravageurs invasifs des eucalyptus du Maroc

Trois nouveaux ravageurs invasifs ont été observés au cours de cette dernière décennie dans les peuplements d’eucalyptus de la région du Gharb au Maroc. Un premier gallicole, Leptocybe invasa Fisher & La Salle 2004 (Hymenoptera: Eulophidae), a été repéré dès 2002, tandis que son parasitoïde Megastigmus sp. (Chalcidoidea: Torymidae) a été identifié en 2009. Les deux autres ravageurs, Ctenarytaina eucalypti (Maskell 1890) et Glycaspis brimblecombei Moore 1964 (Hemiptera: Psyllidae), ont été découverts respectivement en 2008 et 2009. Quelques paramètres bio-écologiques relatifs au développement de L. invasa ont été mesurés au laboratoire et sur le terrain, tandis que le taux d’infestation de jeunes eucalyptus a été suivi pendant trois années successives. Les stratégies de lutte envisagées contre ces nouveaux ravageurs sont discutées.     

Dynamique des populationsd'un ravageur des pins:Pissodes notatus F. [Col.: Curculionidae] II. — Rôle du parasitisme

Résumé L'étude examine l'influence du cortège parasitaire dans la dynamique des populations deP. notatus dans une forêt de pin maritime du sud-ouest de la France. De 1968 à 1977, le niveau du parasitisme apparent total à l'émergence a varié, mais est resté le plus souvent compris entre 20 et 30%. Les parasito?des les plus abondants appartenant aux genresEubazus etCoelo?des se sont montrés densito-dépendants par rapport à leur h?te et le rapport entre leurs effectifs respectifs est resté assez constant au cours des 10 années d'observation. Un calcul basé sur l'évolution théorique des populations deP. notatus au vours de leur développement a permis d'estimer qu'en moyenne 16% seulement des charan?ons étaient détruits chaque année par l'ensemble des parasito?des alors que dans cet habitat le taux de parasitisme annuel moyen à l'émergence a été de 0,28.      

L'âge du complexe récifal des côtes de meuse entre verdun et commercy et la stratigraphie de l'oxfordien dans l'est du bassin de Paris

The question of the age of «Hauts de Meuse coral rag is studied again using new faunas of brachiopods and ammonites collected above, below and inside the coral rag. Ammonites fauna of the well known «Calcaires de Creuë is revised. Results obtained agree closely.The «Hauts de Meuse coral rag grew up during Middle Oxfordian time; and extend part of the Plicatilis zone (Antecedens Subzone) and the whole Transversarium Zone up to the basis of the Bifurcatus Zone, for the first time identified in Lorraine. So it span a short depositional time, about 1 MY, with a high deposition rate, the thickness of the coral rag being more than 100 meters, reaching 150 meters in Saint-Mihiel area. Towards SE, on the other side of the Marne Gap, the sudden change into basinal facies go with a reducing of thickness and deposition rate.Upper Oxfordian deposits show a relative uniformity of facies and thickness. At the top of Middle Oxfordian limestones, the age of the discontinuity and the Sequanian renewal of deposition is basal Bifurcatus Zone. Erosional renewal and terrigeneous deposits are a wide spread event by the beginning of Upper Oxfordian.In the paleontological part, species upon which are based new ages and interpretations are only figured, except the species new or with new paleontological data, which are described. Type specimen of Perisphinctes mosensisBayle, from the «Calcaires de Creuë, is described and photographically figured for the first time.