Catalogue des Vesperidae et des Cerambycidae de la faune de France (Coleoptera)

Ce catalogue des Vesperidae et Cerambycidae de la faune de France est fondé sur une vaste étude bibliographique et sur les observations des auteurs ainsi que celles, vérifiées, de nombreux amateurs. Les nombreuses modifications montrent la nécessité de la révision du dernier ouvrage de référence (Villiers 1978). Le bilan faunistique des recherches permet de dresser une liste de 251 taxa représentant 242 espèces actuellement présentes en France continentale et en Corse. Cette liste est sujette à de perpétuelles modifications liées aux fluctuations de populations, aux introductions et aux activités de recherche de nombreux amateurs. Ce travail de synthèse systématique, taxinomique et faunistique est une première étape pour la réalisation d’un atlas des Vesperidae et Cerambycidae de France et de Corse.     

Organisation de type tétracoralliaire des rides septales de Palaeacis (Cnidaria, Carbonifére)

Plusquellec, Y., Lafuste, J. & Webb, G. E. 1990 10 15: Organisation de type tétracoralliaire des rides septales de Palaeacis (Cnidaria, Carbonifére). Lethaia, Vol. 23, pp. 385–397. Oslo. ISSN 0024–1164. Precedemment signalée chez Kerforneidictyum (Pleurodictyforme dévonien), la rare disposition des rides septales suivant un mode tétracoralliaire est décrite chez un Palaeack sp. du Viséen d'Algérie et chez P. cuneiformis subsp. A du Viseen d'Australie. Chez Palaeacis sp. sont mises en evidence une ride septale cardinale forte en position externe opposée à une ride antipode déterminant un plan de symétrie bilatérale; de part et d'autre une zone systématiquement confuse marque l'emplacement des rides alaires. La reconnaissance des périantipodes prête à discussion et ce secteur présente une originalité certaine par rapport à celui des Tétracoralliaires. Chez P. cuneiformis subsp. A, une coupe transversale montre la présence de quatre rides proéminentes qui fusionnent dans I'axe du corallite et I'existence d'une symétrie bilatérale. La position systématique du genre Palaeacis est discutée: son attribution aux Tétracoralliaires est exclue, ancun caractére n'est incompatible avec le statut de Tabulé, la création d'une unité taxon-omique nouvelle regroupant Palaeacis, Trachypsammia et les Pleurodictyformes est envisageable mais actuellement prématurée. ? Palaeacis, Tabulata, Rugosa, rides septales, systématique, relations deparenré, Viséen. The tetracoral pattern of septal ridges described in Kerforneidictyum (Devonian Pleurodictyum-like coral) is scar'ce in the Tabulata, but has been found in Palaeacis sp. from the Visean of Algeria and in P. cuneiformis subsp. A from the Visean of Australia. Palaeacis sp. shows a strong cardinal septal ridge in peripheral position, just opposite the counter ridge. thus creating a plane of bilateral symmetry: an area on both sides. which is always blurred, indicates the position of the alar ridges. counter-lateral ridges are not easily identified and yield differing interpretation. Compared with the Rugosa this area presents distinctive features. In P. cuneiformis subsp. A, a transverse section exhibits four well-developed septal ridges that coalesce in the axis of the corallite with obvious bilateral symmetry. The systematic position of the genus Palaeacis is questioned: Rugosa it is not; it may belong to Tabulata: however, erecting a new higher taxon for Palaeacis, Trachypsammia and other Pleurodictyum-like corals is premature at our present state of knowledge. ? Palaeacis, Tabulata, Rugosa, septal ridges, systematic. affinities, Visean.     

Etude Ultrastructurale des Mérozoites et de la Schizogonie des Coccidies (Eimeriina): Eimeria magna (Perard 1925) de I'Intestin des Lapins et E. tenella (Railliet et Lucet, 1891) des Coecums des Poulets

SYNOPSIS. An electron microscopic study is made of merozoites and schizogony of Eimeria magna and Eimeria tenella from rabbits and chickens infected 5 days before fixation.
The merozoite outer layer is formed by a unit membrane lined by a dense osmiophilic layer. A micropyle is present. The apical complex of the cell is constituted by a conoid surmounted by 2 rings and surrounded by another from which about 26 subpellicular, tubular fibrils start. Two "rhoptries" (= toxonemes) go thru the conoid to the apex of cell. Rare sarconemes (= convoluted tubes) are disseminated in the anterior part of merozoites. A nucleus with nucleolus, Golgi apparatus, mitochondria, endoplasmic reticulum, lipid globules and glucidic grains were observed.
Schizogony starts by the formation of a multinucleated schizont which has a centriolar structure. The new merozoites appear as evaginations of the schizont's membrane. Cellular organelles (conoid, rhoptries, micropyle, sarconemes) differentiate and the nuclei enter the diverticula of the schizont. Then the development of merozoites proceeds by "external budding".
The ultrastructural similarities between the merozoites of Eimeria and the endodyocytes of Toxoplasmea, appear to us to be extremely interesting and indicate a close relationship between the Toxoplasmea and the Coccidia.     

Remarques sur la stratigraphie des terrains tertiaires des bassins de Narbonne-Sigean et de Leucate (aude) a l'aide des micromammiferes

The discovery of rodents in the lacustrine and brackish deposits of the Narbonne-Leucate area classicaly dated as Oligocene, indicate that they are Oligocene and lower Miocene (Aquitanian) in the Narbonne-Sigean basin, and that the marls and limestones of the Leucate plateau and cliff are Pliocene.     

Préparation des Antigenes des Mycoplasmes (MLO) Pathogènes de la Flavescence Dorée, à Partir de Tissus Végétaux

Antigen preparation from plant tissues of pathogenic mycoplasms (MLO) causing flavescence doree disease Extraction and purification of plant yellow's pathogen mycoplasms (MLO) from plant tissues is a difficult problem. It concerns indeed non cultivable, heterogeneous and fragile organisms which are localized in the fibrous and resistant phloem tissue. In a work directed by an infectivity test by leafhopper injection, our laboratory investigated the best host plant and the best extraction method for this type of pathogen. Broad bean, Vicia faba gave better extracts than Vitis vinifera. Stems are better than petioles or lamina. The best results were obtained with the top region of the stem, at the level where symptoms are apparent on young plants. The most efficient mincing method is achieved with razorblades moved alternatively by the rapid vertical movement of an electric knife. The extraction medium already published (Caudwell and Kuszala 1986) has to be modified for plants by various additional components, histidine buffer, antioxidizers (glutathion 0.2 mg per ml) and polymers 0.5 to 1 p 100 PVP or Polyclar, 1–2 p 100 PEG). 1 g of plant infected tissue is minced in 4 ml of medium. The extracts are filtered through a 100 mesh nylon cloth. After this stage the purification method goes parallel to that used for leafhopper extracts (Caudwell and Kuszala 1986). It is possible to obtain 4 × 10⁶ infectious units from 1 g of broad bean stem (for calculation, see C 1986). It is possible to obtain 4 × 10⁶ infectious units from 1 g of broad bean stem (for calculation, see Caudwell 1977). The possibility to extract MLO, either from infectious leafhoppers or from diseased plants enabled cross immunological assays involving antigens from one host and antibodies directed towards the other host antigens. The first step was the successful ISEM visualization of ttie MLOs (Caudwell et al. 1982), the second is the immunoenzymatic MLO-detection (Boudon et al. 1986).     

Distribution et écologie des associations d’ostracodes récents de l’estuaire de Tahadart (Maroc Nord-Occidental)

Forty-five ostracod species were identified for the first time in the Tahadart estuary (NW Morocco). They can be grouped into five different ecological assemblages, which characterise four estuarine ecozones. A first ecozone occurs in temporary waters located between the tidal channels of the inner estuary and it is characterised by ostracod species typical of fresh to brackish waters. In the main estuary area, the ostracod fauna is dominated by clearly euryhaline species that account for nearly 70% of the entire fauna. The relative abundance of the different assemblages allows us to subdivide the estuarine environment along a longitudinal profile into mouth, outer and inner estuary. The estuary's mouth displays the highest values of marine euhaline, phytal and periphytal as well as ubiquitous species and the lowest values of very euryhaline species; the latter are the only species present in the inner estuary. The outer estuary exhibits intermediate percentages of the different ecological assemblages. This distribution, characterized by the absence of limnic species, points to the influence of marine waters in an open estuary with a low fresh water input. In the estuary's mouth, as well as in the outer estuary, where the slikke and schorre are well developed, the distance to the emersion line is underlined by the lower occurrence of marine and ubiquitous species and the higher occurrence of the very euryhaline ones. The Tahadart estuary displays a moderate to high ostracod diversity with distinct differences among the ecological zones. The stress of this environment is highlighted by the low diversity characteristics of extreme environments, alike in the inner estuary and in some areas located far from the emersion level. The relative position with respect to the emersion line, as well as the presence of gross detritic sediments and vegetation, appear to be of importance for the good development of the ostracods.     

Stratigraphie, paléoécologie et foraminifères du paléogène des Alpes Maritimes et des Alpes de Haute-Provence (Sud-Est de la France)

Paleogene sedimentation in the Alpes Maritimes and Alpes de Haute Provence regions is composed of one complete sedimentary sequence. This sequence begins with the continental Formation from Microcodium and continues with the Cerithium layers, the Calcaires Nummulitiques and the Marnes Bleues, which are overlaid by the turbidites of the Grès d’Annot Formation. Sedimentation starts in the Nummulites perforatus zone close to the base of ‘the Truncorotaloides rohri zone (P 14) and ends in the Cassigerinella chipolensis-Pseudohastigerina micra zone (P 18) and the NP21 zone in the upper part of the Grès d’Annot. More biomarkers were used in order to define a more detailed local biozonation (biozones AMP 1 to AMP 7). Four local zones were also defined by the last occurrence of Nummulites millecaput and N. perforatus-N. ptukhiani and then by the first appearance of N. retiatus (AMGF 1-4). The evolution of benthic foraminiferal assemblages shows an increase in bathymetry from the internal platform in the Cerithium layers to the calcareous platform with large foraminifers, then to the external platform and the deep offshore environment of the Marnes Bleues and Grès d’Annot. Low faunal diversity in the Grès d’Annot together with the predominance of agglutinated species indicates a poorly oxygenated, organic rich and turbidite environment. Seven steps (SD 1 to SD 7) in the Eocene marine transgression are shown from East to West by detailed local biozonation and sequence analysis. Grès d’Annot sedimentation is also diachronous, beginning within the Truncorotaloides rohri zone (P 14, AMP 1) in the East and ending within the Pararotalia opima opima zone (P 20, middle Rupelian) in the West (Barrême). Small foraminifer Paleogene fauna from the Alpes Maritimes and Alpes de Haute Provence was studied from 400 samples. It is composed of 378 species. Two new taxa are proposed: Fissurina niceana n. sp. and Globocassidulina alpina n. sp. The species from the Escarène and Gorbio neighborhood described by M. von Hantken (1884) were re-examined.     

L'ichthyofaune des marnes messiniennes des environs de Gabbro (Toscane,Italie): Signification paleoecologique

Five species of fossil Fishes, of which three are new (Aphanius italicus nov. sp., Palaeoatherina etrusca nov. sp. and Gobius ignotus nov. sp.) occur in the Messinian marls from Gabbro (Tuscany, Italy). This association allows to consider this locality as constituted in a continental basin with a variable salt content.     

L’étude des conditions d’habitabilité des établissements préhistoriques : à propos des amas coquilliers mésolithiques de la région cantabrique occidentale (Nord de l’Espagne)

We show the methodology we followed in order to reliably estimate a factor that, to our judgement, is fundamental for the assessment of the characteristics of a prehistoric settlement: the conditions of exposure to the sun. This methodology is applied to the study of Mesolithic shell middens in the North of Spain, with the aim to introduce a new kind of information in the debate about the meaning of shell middens. Throughout this century, different ways to understand the behaviour these remains conceal have been proposed. Our thesis with regard to it, presented in this paper, is based on the observation of a series of variables, among which we can find the exposure to the sun the settlements undergo. We therefore show in the last part of the paper, how to join the information from the proposed analysis with the other data subsequent from the study of other variables such as the environmental conditions prevailing during the period of formation of the sites; the situation of the settlements; the location of the remains in the caves; the entity of the occupations; and the energy spent on the transportation of the aquatic resources from the coast towards the places where their rests are found nowadays. In short, we propound a methodology for the study of one of the variables that falls upon the habitability of a prehistoric settlement and we point out the contribution that the incorporation of an analysis of this kind means for the research of Mesolithic shell middens in the North of Spain.