Le statuts y stématique du Genévrier oxycédre Junyperus oxycedrus L. (Cupressacées): une contribution d'ordre biochimique et biométrique

Dimensiosis des galbules et/ou teneur en prodelphinidine des aiguilles permettent trés généralement de déterminer les sous-espéces oxycedrus et macrocarpa, respectivement septentrionale-continentale et méridionale-insulaire, du Genévrier oxyeédre Juniperus oxycedrus L. Parcontre, la sous-espéce nord-africaine rufescens (en montagne) ne parah pas distinguable à ces titres de la sous-espéce type. Mais l’étude biochimique plus approfondie d’une (méta)population languedocienne montre l’existence d’un polymorphisme proanthocyanique indépendant de la taille des galbules. Les deux sous-espéces classiquement reconnues pourraient donc n’étre que les formes extremes, homozygotes pour le caractére chimique considéré, d’un méme génóme spécifique. Si les spécimens littoraux (Corse, Majorque, Maghreb) correspondent bien à la pleine expression (= prodelphinidine forte) de ce polymorphisme, certains échantillons «péri-littoraux» (Baléares et Languedoc) trahissent une introgression (actuelle ou ancienne) ayee appartion d’individus hétérozygotes, aux teneurs intermédiaires: des génes «macrocarpa» sont done bien presents au nord de la Méditerranée, méme si le phénoméne n’est pas morphologiquement décelable, et ne mérite pas d’étre formalisé en termes systématiques.

L'influence atlantique dans les montagnes portugaises au sud duTage

Prenant la flore et la végétation comme des indicateurs du climat local, on fait une analyse abrégée de l'influence atlantique sur quatre montagnes portugaises, s¡tuées au sud du fleuve Tage, en plain domaine méditerranéen. Elles sont distríbuées depuis le nord-est de l‘Alentejo jusqu’a l’extreme sud-ouest du territoire.L'observation des données floristiques a montré que la dominance des espéces méditerrennes est générale, bien que entre un mínimum de 34.0% à S. Mamede et un maximum de 48.9 % à Portel. On a vérifié aussi, en commun, un trés faible degré d'endémisme, lequel atteint la valeur la plus élevée -1.2%-, dans la montagne de Monchique. 

Fossil associations from the middle and upper Eocene strata of the Pamplona Basin and surrounding areas (Navarre, western Pyrenees)

Fossil associations from the middle and upper Eocene (Bartonian and Priabonian) sedimentary succession of the Pamplona Basin are described. This succession was accumulated in the western part of the South Pyrenean peripheral foreland basin and extends from deep-marine turbiditic (Ezkaba Sandstone Formation) to deltaic (Pamplona Marl, Ardanatz Sandstone and Ilundain Marl formations) and marginal marine deposits (Gendulain Formation). The micropalaeontological content is high. It is dominated by foraminifera, and common ostracods and other microfossils are also present. The fossil ichnoasssemblages include at least 23 ichnogenera and 28 ichnospecies indicative of Nereites, Cruziana, Glossifungites and ?Scoyenia-Mermia ichnofacies. Body macrofossils of 78 taxa corresponding to macroforaminifera, sponges, corals, bryozoans, brachiopods, annelids, molluscs, arthropods, echinoderms and vertebrates have been identified. Both the number of ichnotaxa and of species (e. g. bryozoans, molluscs and condrichthyans) may be considerably higher. Body fossil assemblages are comparable to those from the Eocene of the Nord Pyrenean area (Basque Coast), and also to those from the Eocene of the west-central and eastern part of South Pyrenean area (Aragon and Catalonia). At the European scale, the molluscs assemblages seem endemic from the Pyrenean area, although several Tethyan (Italy and Alps) and Northern elements (Paris basin and Normandy) have been recorded. Palaeontological data of studied sedimentary units fit well with the shallowing process that throughout the middle and late Eocene occurs in the area, according to the sedimentological and stratigraphical data.

Revisiting the Late Jurassic-Early Cretaceous of the NW South Iberian Basin: new ages and sedimentary environments

The study of the Upper Jurassic-Lower Cretaceous deposits (Higueruelas, Villar del Arzobispo and Aldea de Cortés Formations) of the South Iberian Basin (NW Valencia, Spain) reveals new stratigraphic and sedimentological data, which have significant implications on the stratigraphic framework, depositional environments and age of these units. The Higueruelas Fm was deposited in a mid-inner carbonate platform where oncolitic bars migrated by the action of storms and where oncoid production progressively decreased towards the uppermost part of the unit. The overlying Villar del Arzobispo Fm has been traditionally interpreted as an inner platform-lagoon evolving into a tidal-flat. Here it is interpreted as an inner-carbonate platform affected by storms, where oolitic shoals protected a lagoon, which had siliciclastic inputs from the continent. The Aldea de Cortés Fm has been previously interpreted as a lagoon surrounded by tidal-flats and fluvial-deltaic plains. Here it is reinterpreted as a coastal wetland where siliciclastic muddy deposits interacted with shallow fresh to marine water bodies, aeolian dunes and continental siliciclastic inputs. The contact between the Higueruelas and Villar del Arzobispo Fms, classically defined as gradual, is also interpreted here as rapid. More importantly, the contact between the Villar del Arzobispo and Aldea de Cortés Fms, previously considered as unconformable, is here interpreted as gradual. The presence of Alveosepta in the Villar del Arzobispo Fm suggests that at least part of this unit is Kimmeridgian, unlike the previously assigned Late Tithonian-Middle Berriasian age. Consequently, the underlying Higueruelas Fm, previously considered Tithonian, should not be younger than Kimmeridgian. Accordingly, sedimentation of the Aldea de Cortés Fm, previously considered Valangian-Hauterivian, probably started during the Tithonian and it may be considered part of the regressive trend of the Late Jurassic-Early Cretaceous cycle. This is consistent with the dinosaur faunas, typically Jurassic, described in the Villar del Arzobispo and Aldea de Cortés Fms.

Contribution to the ethnobotanical study of antidiabetic medicinal plants of the Central Middle Atlas region (Morocco)

An ethnobotanical survey of medicinal plants was carried out in the Central Middle Atlas in the years 2013 and 2014 to establish the catalog of medicinal plants used in traditional medicine in the treatment of diabetes. Thus, 1560 people were interviewed, using questionnaires. The latter enabled us to gather information on traditional healing practices of the local population including scientific name, French name, vernacular name, plant parts used , therapeutic indications , revenues and mode of administration. The results show that 76 medicinal species were inventoried in the study area. These plant species are included into 67 genus and 40 families. The most represented families are: Lamiaceae (12 species), Asteraceae and Brassicaceae species with 14 each. Of 76 medicinal species found in the region, four species are reported for the first time in the traditional treatment of diabetes in Morocco. They are Pistacia atlantica, Ptychotis verticillata, Anacyclus pyrethrum, Alyssum spinosum, Cistus albidus, Juniperus thurifera, Ephedra nebrodensis, Thymus algeriensis, Th. munbyanus, Th. zygis, Abelmoschus esculentus, Fraxinus augustifolia, Sorghum vulgare and, Eriobotrya japonica. The leaves are the most used organs (38%). The decoction is the dominant mode of preparation (50%) and administration is mostly for oral use (97%).