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Kinds of Morocco Selected AbstractsMOROCCO: Public Sector StrikeAFRICA RESEARCH BULLETIN: ECONOMIC, FINANCIAL AND TECHNICAL SERIES, Issue 2 2010Article first published online: 1 APR 2010 No abstract is available for this article. [source] MOROCCO: Expatriates Head HomeAFRICA RESEARCH BULLETIN: ECONOMIC, FINANCIAL AND TECHNICAL SERIES, Issue 5 2009Article first published online: 3 JUL 200 No abstract is available for this article. [source] MOROCCO,EU: Casablanca Conference Hears PlansAFRICA RESEARCH BULLETIN: ECONOMIC, FINANCIAL AND TECHNICAL SERIES, Issue 2 2009Article first published online: 7 APR 200 No abstract is available for this article. [source] MOROCCO: Industry Protection StrategyAFRICA RESEARCH BULLETIN: ECONOMIC, FINANCIAL AND TECHNICAL SERIES, Issue 1 2009Article first published online: 9 MAR 200 No abstract is available for this article. [source] A NEW TEREBRATULID BRACHIOPOD SPECIES FROM THE SIEGENIAN OF THE DRA VALLEY, MOROCCO, AND ITS STRATIGRAPHIC, PALAEOGEOGRAPHIC AND PHYLOGENETIC SIGNIFICANCEPALAEONTOLOGY, Issue 4 2008MENA SCHEMM-GREGORY Abstract:, A new terebratulid brachiopod species, Rhenorensselaeria jansenii, has been identified in the Merzâ-Akhsaï Formation of the Dra Valley, Morocco, and the Grauwacke de Montguyon of the Amorican Massif, France. It is compared with the other known species of Rhenorensselaeria from Europe, Rh. strigiceps and Rh. demerathia, as well as with Rh. macgerriglei from North America, from which it differs in being larger and having coarser costae. Its possible life habit in clusters and its fossil community are compared with those of Rh. strigiceps from the Rheinisches Schiefergebirge (,Rhenish Slate Mountains'), Germany, which it most resembles. A new phylogeny of the subfamily Rhenorensselaerinae is constructed. The close phylogenetic relationship between Rh. jansenii and Rh. strigiceps confirms close palaeobiogeographical relationships between North Africa, France and the Rheinisches Schiefergebirge as well as a wider relationship between Central Europe and Gaspé, eastern Canada, during the Early Devonian. Taxa of Rhenorensselaeria are mainly restricted to the Middle and Upper Siegenian, although rare individuals have been found in the Lower Emsian of Central Europe and North America. Because of their abundance in the Dra Valley and Rheinisches Schiefergebirge and their short life span, rhenorensselaerid taxa can be regarded as important stratigraphical markers of Middle,Late Siegenian and Early Emsian sediments in North Africa and Central Europe. [source] A LONG-SNOUTED DYROSAURID (CROCODYLIFORMES, MESOEUCROCODYLIA) FROM THE PALEOCENE OF MOROCCO: PHYLOGENETIC AND PALAEOBIOGEOGRAPHIC IMPLICATIONSPALAEONTOLOGY, Issue 2 2008STEPHANE JOUVE Abstract:, New material of a long-snouted dyrosaurid has been discovered in the Paleocene of Morocco. It consists of a well-preserved skull with embedded mandible and four dorsal vertebrae. The particularly elongate snout, proportionally the longest of all known dyrosaurids, allows precise identification of this material as Atlantosuchus coupateziBuffetaut, 1979a, and presentation of an emended diagnosis for this species previously known only from a mandibular symphysis. A phylogenetic analysis of the dyrosaurids indicates a close relationship between A. coupatezi and Rhabdognathus. It also confirms a previous hypothesis that Congosaurus is distinct from Hyposaurus. It is more closely related to Atlantosuchus than Hyposaurus. The analysis also allows palaeobiogeographic interpretations to be made. Dyrosaurids ranged from North Africa to other areas. They were rare during the Maastrichtian and endemic to each continent at this time. Competition with large marine reptiles, such as mosasaurs, limited their dispersal during the Late Cretaceous. The disappearance of these rivals during the ,K-T crisis' enabled their diversification and widespread dispersal during the Paleocene, with the same genera present on several continents. [source] CHEMICAL ANALYSIS OF GLASS BEADS FROM MEDIEVAL AL-BASRA (MOROCCO)ARCHAEOMETRY, Issue 3 2010P. ROBERTSHAW This paper reports the results of elemental analysis, using laser ablation , inductively coupled plasma , mass spectrometry (LA,ICP,MS), of 30 glass beads from an assemblage of beads excavated at medieval al-Basra, Morocco. Six chemical glass types are represented and their characteristics and geographical origins are discussed, with reference also to the techniques used to make the beads. The presence of numerous beads of lead,silica glasses is of particular interest. The morphological, technological and chemical analyses of the bead assemblage shed light on al-Basra's trade connections. [source] Speciation and Environmental Fate of Chromium in Rivers Contaminated with Tannery EffluentsENGINEERING IN LIFE SCIENCES (ELECTRONIC), Issue 2 2007J. Dominik Abstract Redox and size speciation of chromium in rivers contaminated with tannery wastewater was carried out to provide insight into its transport and removal mechanisms. Total chromium was determined with Inductively Coupled Plasma-Mass Spectrometry and Cr,(VI) with Catalytic Adsorption Stripping Voltammetry. For the size speciation, particles were retained with a cartridge filter (cut-off 1.2,,m) and the total filterable fraction was further fractionated with Tangential Flow Filtration to determine the concentrations of chromium associated with the High Molecular Weight Colloidal (HMWC), Low Molecular Weight Colloidal (LMWC) and Truly Dissolved (TD) fractions. Two fluvial systems of similar sizes, but located in contrasting climatic zones, were selected for comparison: the Sebou-Fez system in Morocco and Dunajec River-Czorsztyn Reservoir system in Poland. Particulate Cr dominated in the Sebou-Fez system (about 90,%); while in the Dunajec-Czorsztyn system, it represented only 17,53,% of the total chromium in raw water. Still, the partition coefficients [Kd] were of the same magnitude. Chromium,(III) was the only form detected in Sebou-Fez, whereas in Dunajec-Czorsztyn Cr,(VI) was also present with its proportion increasing downstream from the input of tannery wastewater due to the preferential removal of Cr,(III). In the filtered water in Morocco a large fraction of Cr occurred in the HMWC fraction (50,70,%) at the two most contaminated sites, while the LMWC and TD forms prevailed at the non-contaminated sites in the Sebou River. At a very high concentration, in the water in the proximity of tanneries (well above the theoretical saturation level) Cr precipitated as polynuclear Cr-hydroxide. In Dunajec-Czorsztyn, the partition of Cr,(III) was approximately equal between the HMWC, LMWC and TD fractions, in contrast to Cr,(VI) which occurred almost exclusively in the TD fraction. In both systems, Cr,(III) was rapidly removed from the water to the sediments. The confluence of the Sebou with the Fez and the Czorsztyn reservoir trapped efficiently Cr,(III) preventing its spreading over long distances. Cr,(VI) showed conservative behavior and bypassed the Czorsztyn Reservoir. This study provides a first set of data on the partitioning of Cr,(III) and Cr,(VI) between the particulate, the colloidal and truly dissolved fractions in fluvial systems contaminated with tannery effluents. It also suggests that, in these systems, truly dissolved Cr,(III) can be adequately modeled from the total filterable concentrations. [source] Distribution patterns of the Q and B biotypes of Bemisia tabaci in the Mediterranean Basin based on microsatellite variationENTOMOLOGIA EXPERIMENTALIS ET APPLICATA, Issue 3 2007B. Simón Abstract At least five of the biotypes described in the Bemisia tabaci (Gennadius) (Homoptera: Aleyrodidae) complex are known to be present in the Mediterranean Basin area. Only two of them, however, are economically relevant, that is, biotypes B and Q. Biological and genetic differences between the two biotypes have been well studied, but less is known about their patterns of genetic variation and population structure. To address these issues, a study was undertaken based on variation at six microsatellite loci among a subset of nine B. tabaci populations (five belonging to the Q and four to the B biotype). The data obtained show that (i) these loci showed considerable polymorphism in the Q and B biotypes populations although the presence of null alleles can obscure the picture; (ii) the Iberian-Q, Canarian-Q, and Egyptian-B populations exhibit heterozygosity excess as a result of bottleneck events; (iii) the low genetic differentiation between the Israeli, Iberian Peninsula, and Italian populations suggest that these populations share a common gene pool; (iv) the genetic distances between the Canarian-Q population and the geographically close population from Morocco indicates spatial isolation and a limited gene flow; and finally (v) the microsatellite data for the B populations indicate that the whiteflies from Egypt and Israel have a close phylogenetic relationship, but the source of these biotype B invasions into the Mediterranean area remains unknown. [source] Toxicology of a Microcystis ichthyoblabe waterbloom from Lake Oued Mellah (Morocco)ENVIRONMENTAL TOXICOLOGY, Issue 1 2002Brahim Sabour Abstract In the Lake Oued Mellah cyanobacteria waterblooms occur periodically in late spring and summer with Microcystis ichthyoblabe as the main bloom-forming species. In 1999, a heavy waterbloom of M. ichthyoblabe occurred during May June with a maximal biomass of 298 mg/l. During this period, several bloom samples were collected. The toxicity assessment was done by mouse and brine shrimp (Artemia) bioassays. Apart from the sample collected on 15/06/1999, all the other samples were toxic by mouse bioassay. The LD50 determined by intraperitoneal injection to mice during active cyanobacterial growth and decline phases were 518 and 1924 mgDW/kg respectively. Using Artemia bioassay, the 24hLC50 varied from 6.0 to 40.6 mg/ml and the 48hLC50 ranged from 2.8 to 18.2 mg/ml. The separation and identification of microcystin variants was performed by high performance liquid chromatography,photodiode array detection. Eleven toxins were separated and preliminarily identified as microcystin variants as they exhibit a typical UV spectra like the microcystin-LR standard. The quantification of total microcystins determined by enzyme-linked immunosorbent assay showed that the contents were varied between 0.1 and 0.76 ,g/g DW. © 2002 by Wiley Periodicals, Inc. Environ Toxicol 17: 24,31, 2002 [source] Detection and quantification of microcystins from cyanobacteria strains isolated from reservoirs and ponds in MoroccoENVIRONMENTAL TOXICOLOGY, Issue 1 2002B. Oudra Abstract In Morocco, the occurrence of toxic cyanobacteria blooms is confirmed in some water bodies used for recreational and/or as drinking water reservoirs. According to WHO recommendations, the establishment of a monitoring program for microcystins is a necessity. This paper presents toxicological studies of 19 toxic cyanobacteria strains of Microcystis, Synechocystis, Pseudanabaena, and Oscillatoria. These strains were isolated from various water bodies including natural lakes, reservoirs, and ponds located in central regions of Morocco. The isolation, culture, and biomass production of these strains was made on Z8 or BG13 media under laboratory controlled conditions. The hepatotoxicity of cyanobacterial lyophilized material was confirmed by mouse bioassays. The amount of microcystins produced by each strain was determined by the enzyme-linked immunosorbent assay (ELISA). The detection and identification of microcystin variants was performed by high performance liquid chromatography (HPLC) with photodiode array detection. Almost all strains showed medium to high toxicity, the estimated LD50 i.p mice bioassay ranged between 28 to 350 mg/kg body weight. The concentrations of microcystins varied between 2.16 to 944 ,g/g and 26.8 to 1884 ,g/g dry weight determined by ELISA and HPLC, respectively. The screening of bloom-forming and microcystin producer cyanobacteria strains in these fresh water bodies leads us to propose the need for the establishment of a survey of cyanobacteria and a cyanotoxin-monitoring program. © 2002 by Wiley Periodicals, Inc. Environ Toxicol 17: 32,39, 2002 [source] TIME TO THE MOST RECENT COMMON ANCESTOR AND DIVERGENCE TIMES OF POPULATIONS OF COMMON CHAFFINCHES (FRINGILLA COELEBS) IN EUROPE AND NORTH AFRICA: INSIGHTS INTO PLEISTOCENE REFUGIA AND CURRENT LEVELS OF MIGRATIONEVOLUTION, Issue 1 2002Cortland K. Griswold Abstract We analyzed sequences from a 275-bp hypervariable region in the 5, end of the mitochondrial DNA control region in 190 common chaffinches (Fringilla coelebs) from 19 populations in Europe and North Africa, including new samples from Greece and Morocco. Coalescent techniques were applied to estimate the time to the most recent common ancestor (TMRCA) and divergence times of these populations. The first objective of this study was to infer the locations of refugia where chaffinches survived the last glacial episode, and this was achieved by estimating the TMRCA of populations in regions surrounding the Mediterranean that were unglaciated in the late Pleistocene. Although extant populations in Iberia, Corsica, Greece, and North Africa harbor haplotypes that are basal in a phylogenetic tree, this information alone cannot be used to infer that these localities served as refugia, because it is impossible to infer the ages of populations and their divergence times without also considering the population genetic processes of mutation, migration, and drift. Provided we assume the TMRCAs of populations are a reasonable estimate of a population's age, coalescent-based methods place resident populations in Iberia, Corsica, Greece, and North Africa during the time of the last glacial maximum, suggesting these regions served as refugia for the common chaffinch. The second objective was to determine when populations began diverging from each other and to use this as a baseline to estimate current levels of gene flow. Divergence time estimates suggest that European populations began diverging about 60,000 years before present. The relatively recent divergence of populations in North Africa, Italy, and Iberia may explain why classic migration estimates based on equilibrium assumptions are high for these populations. We compare these estimates with nonequilibrium-based estimates and show that the nonequilibrium estimates are consistently lower than the equilibrium estimates. [source] Major discoveries on the dermal skeleton of fossil and Recent polypteriforms: a reviewFISH AND FISHERIES, Issue 2 2001Jacques Daget Abstract Following the discovery of the first living polypterid, Polypterus bichir, in 1802, almost two centuries later we now know of 15 living species (including four subspecies), 14 belonging to the genus Polypterus and one to the genus Erpetoichthys (Calamoichthys) all inhabiting intertropical Africa. The polypterid fossil record was for a long time reduced to some scarce, disarticulated bones, mainly scales, found in various African deposits covering a wider area than the actual geographical distribution. With the discovery, on one hand, of polypterid scales, vertebrae, dermal bones of the cranium and dorsal spiny rays in South America and, on the other hand, of scales and numerous dorsal spiny rays in Niger and Sudan, and two articulated fossils in Morocco, the story of the polypteriforms has revealed some of its mysteries. The discovery of isopedine between dentine and bony basal plate in the scales of living and fossil polypterid species is considered a synapomorphy of the group, and has been an important aid in discriminating polypterid scales from other ganoid scales. A review of the main findings during the last 20 years is presented. [source] Chemical composition of the essential oil of nine Eucalyptus species growing in MoroccoFLAVOUR AND FRAGRANCE JOURNAL, Issue 2 2004S. Zrira Abstract The essential oils obtained by steam distillation from the leaves of nine Eucalyptus species (E. cinerea F. Muell., E. baueriana F. Muell., E. smithii R. T. Baker, E. bridgesiana R. T. Baker, E. microtheca F. Muell., E. foecunda Schau., E. pulverulenta Sims, E. propinqua Deane and Maiden, E. erythrocorys F. Muell.) of Moroccan origin have been analysed using GC and GC,MS. A total of 83 constituents were identi,ed. All the species investigated were found to possess an oil rich in 1,8-cineole (>68%). In ,ve species (E. cinerea F. Muell., E. baueriana F. Muell., E. smithii R. T. Baker, E. bridgesiana R. T. Baker and E. microtheca F. Muell.), the 1,8-cineole content exceeded 80%. Copyright © 2004 John Wiley & Sons, Ltd. [source] Chemical composition of the essential oil of Pistacia lentiscus L. from Morocco,a seasonal variationFLAVOUR AND FRAGRANCE JOURNAL, Issue 6 2003S. Zrira Abstract Air-dried aerial parts of Pistacia lentiscus L. collected from different regions of Morocco (Mehdia, Oulmes and Chaouen) were water-distilled to produce oil in 0.2% yields. The chemical composition of P. lentiscus oils changes from a region to another. The variations in chemical composition are important between plant populations. A total of 45 constituents were identi,ed. The major oil components of P. lentiscus from Oulmes were , -pinene (16.5,38.5%), , -myrcene (10.2,11.5%) and limonene (6.8,9.8%), while terpinen-4-ol (32.7,43.8%), , -pinene (7.1,13.5%) and bornyl acetate (6.8,10.3%) were the main constituents of Chaouen oil. For P. lentiscus from Mehdia, terpinen-4-ol (14.5,19.3%), caryophyllene oxide (6.5,10.3%) and limonene (6.7,8.1%) were the major components. The effect of harvesting time on the oil production and chemical composition was also examined at different vegetative stages (December,June). For the three locations, the best oil content was obtained during the ,owering period March,June. Copyright © 2003 John Wiley & Sons, Ltd. [source] The Early Carboniferous (Mississippian) ammonoids from the Chebket el Hamra (Jerada Basin, Morocco)FOSSIL RECORD-MITTEILUNGEN AUS DEM MUSEUM FUER NATURKUNDE, Issue 2 2008Dieter Korn Abstract Five Late Viséan ammonoid assemblages of North Variscan provenance are described from the locality Chebket el Hamra (Jerada Basin, north-eastern Morocco). These assemblages are composed of 27 species of the genera Eoglyphioceras, Girtyoceras, Sulcogirtyoceras, Metadimorphoceras, Goniatites, Arnsbergites, Hibernicoceras, Paraglyphioceras, Lusitanoceras, Sudeticeras, Neoglyphioceras, Lusitanites, Ferganoceras, Praedaraelites, and Pronorites. The new subfamily Arnsbergitinae is described, as well as the thirteen new species Eoglyphioceras minutum n. sp., Girtyoceras ibnkhaldouni n. sp., Metadimorphoceras anguinosum n. sp., Arnsbergites ferrus n. sp., Arnsbergites proiecturus n. sp., Arnsbergites rufus n. sp., Hibernicoceras touissitense n. sp., Hibernicoceras artilobatum n. sp., Paraglyphioceras celeris n. sp., Lusitanoceras zirari n. sp., Sudeticeras ibnbajjahi n. sp., Sudeticeras horoni n. sp., and Pronorites owodenkoi n. sp. (© 2008 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim) [source] Alpinites and other Posttornoceratidae (Goniatitida, Famennian)FOSSIL RECORD-MITTEILUNGEN AUS DEM MUSEUM FUER NATURKUNDE, Issue 1 2002R. Thomas Becker Abstract The rediscovery of the supposedly lost type allows a revision of Alpinites Bogoslovskiy, 1971, the most advanced genus of the Posttornoceratidae. The type-species, Alp. kayseri Schindewolf, 1923, is so far only known from the Carnic Alps. Alp. schultzei n. sp. from the eastern Anti-Atlas of Morocco is closely related to Alp. kajraktensis n. sp. (= Alp. kayseri in Bogoslovskiy 1971) from Kazakhstan. A second new and more common species of southern Morocco, Alp. zigzag n. sp., is also known from the Holy Cross Mountains (Poland). The taxonomy and phylogeny of other Posttornoceratidae are discussed. The holotype of Exotornoceras nehdense (Lange, 1929) was recovered and is re-illustrated; it is conspecific with Exot. superstes (Wedekind, 1908). The genus and species is also here first recorded from Morocco. Post. weyeri Korn, 1999 is a subjective synonym of Post. posthumum (Wedekind, 1918) in which strongly biconvex growth lines, as typical for the family, are observed for the first time. Goniatites lenticularis Richter, 1848 is a nomen dubium within Discoclymenia, Clymenia polytrichus in Richter (1948) is a Falcitornoceras. It seems possible to distinguish an extreme thin and trochoid Disco. haueri (Münster, 1840) from the tegoid Disco. cucullata (v. Buch, 1839). Various taxa are excluded from the Posttornoceratidae. Posttornoceras sapiens Korn, 1999 forms the type-species of Maiderocera n. gen., Discoclymenia n. sp. of Müller (1956) is assigned to Maid. muelleri n. sp. Disco. cornwallensis is the type-species of Selwoodites n.gen (Sporadoceratidae) which also occurs in the Rhenish Massive. Durch Auffinden des verschollen geglaubten Typus-Exemplares wird eine Revision der Gattung Alpinites Bogoslovskiy, 1971, der höchst entwickelten Gattung der Posttornoceratidae, möglich. Die Typus-Art, Alp. kayseri Schindewolf, 1923, kommt gesichert bisher nur in den Karnischen Alpen vor. Alp. schultzei n. sp. aus dem östlichen Anti-Atlas (Marokko) ist nah mit Alp. kajraktensis n. sp. aus Kazakhstan (= Alp. kayseri in Bogoslovskiy 1971) verwandt. Eine zweite, aber häufigere neue Art Süd-Marokkos, Alp. zigzag n. sp., wird auch im Heiligkreuzgebirge (Polen) nachgewiesen. Die Taxonomie und Phylogenie anderer Vertreter der Posttornoceratidae werden diskutiert. Der verschollen geglaubte Holotypus von Exotornoceras nehdense (Lange, 1929) wird neu abgebildet und ist conspezifisch mit Exot. superstes (Wedekind, 1908). Die Gattung und Art wird erstmals auch in Marokko nachgewiesen. Post. weyeri Korn, 1999 ist ein subjektives Synonym von Post. posthumum (Wedekind, 1918) bei dem erstmals die Familien-typischen, stark biconvexen Anwachsstreifen beobachtet wurden. Goniatites lenticularis Richter, 1848 ist ein nomen dubium innerhalb von Discoclymenia, Clymenia polytrichus in Richter (1848) ein Falcitornoceras. Es scheint möglich, eine extrem dünne, trochoide Disco. haueri (Münster, 1840) von der tegoiden Disco. cucullata (v. Buch, 1839) zu trennen. Verschiedene Taxa werden aus den Posttornoceratidae ausgeschlossen. Post. sapiens Korn, 1999 wird als Typus-Art zu Maideroceras n. gen. gestellt. Discoclymenia n. sp. in Müller (1956) wird als Maid. muelleri n. sp. neu beschrieben. Disco. cornwallensis Selwood, 1960 bildet die Typusart von Selwoodites n. gen. (Sporadoceratidae), welches auch im Rheinischen Schiefergebirge vorkommt. [source] Taxonomy, evolutionary History and Distribution of the middle to late Famennian Wocklumeriina (Ammonoidea, Clymeniida)FOSSIL RECORD-MITTEILUNGEN AUS DEM MUSEUM FUER NATURKUNDE, Issue 1 2000R. Thomas Becker Abstract Old collections, new records, and data from global literature are used for taxonomic revisions and for a new reconstruction of the evolutionary history of the triangularly coiled clymenids, the Wocklumeriaceae, and their ancestors. Epiwocklumeria applanata is first reported from the topmost Wocklum Limestone at Hasselbachtal and Drewer, and this supports the distinction of an applanata Subzone just prior to the global Hangenberg Event which wiped out the whole group. The Wocklumeriaceae and Glatziellidae record of the famous Oberrödinghausen Railway Cut and of other Rhenish sections is revised. The Maïder of Southern Morocco has yielded first Parawocklumeria patens, paprothae, Wocklumeria sphaeroides plana, Kielcensia ingeniens n. sp., and Synwocklumeria mapesi n. sp. Parawocklumeria distributa Czarnocki forms the type-species of Tardewocklumeria n. gen. Lecto- and neotypes for several taxa are designated. The variability and paedomorphic patterns of Wo. sphaeroides are discussed. The Wocklumeriaceae represent the terminal Famennian (Upper Devonian VI-C/D) radiation of a long-ranging lineage which evolved in parallel to other clymenid groups. They are characterized by sutural features and by longidomic and very slowly expanding whorls. The polyphyletic traditional Gonioclymeniina are divided into the suborder Wocklumeriina (with Wocklumeriaceae, Glatziellaceae n.superfam. and Biloclymeniaceae) and into the Gonioclymeniaceae of the Clymeniina. Gyroclymenia Czarnocki is regarded as a junior synonym of Pleuroclymenia Schindewolf which, however, does not include the ,Pleuro.' americana and eurylobica groups. Pleuroclymenia represents the ancestral form of the Wocklumeriina and also the phylogenetical link with Platyclymenia (Varioclymenia) of the Clymeniaceae. The Gonioclymeniaceae had their roots in advanced Platyclymeniidae. Alte Aufsammlungen, Neunachweise und globale Literaturdaten werden für taxonomische Revisionen und für eine neue Rekonstruktion der Evolution der Dreiecksclymenien (Wocklumeriaceae) und ihrer Vorfahren benutzt. Epiwocklumeria applanata wird zum ersten Mal im Hasselbachtal und bei Drewer nachgewiesen, und diese Funde bestätigen die Abtrennung einer applanata -Subzone im unmittelbar Liegenden des Hangenberg-Event, welcher zum Aussterben der gesamten Gruppe führte. Die Verbreitung von Wocklumeriaceae und Glatziellidae im klassischen Profil des Bahneinschnittes bei Oberrödinghausen und an anderen Fundorten im Rheinischen Schiefergebirge wird revidiert. Der Maïder in Süd-Marokko lieferte erstmalig Parawocklumeria patens, paprothae, Wocklumeria sphaeroides plana, Kielcensia ingeniens n. sp. und Synwocklumeria mapesi n. sp. Parawocklumeria distributa Czarnocki bildet die Typus-Art von Tardewocklumeria n.gen. Weiterhin werden die Variabilität und paedomorphe Erscheinungen bei Wo. sphaeroides diskutiert. Die Wocklumeriaceae repräsentieren im höchsten Famennium (UD VI-C/D) die Radiationsphase einer langlebigen phylogenetischen Linie, die sich parallel zu anderen Clymenien entwickelte. Sie ist durch Suturmerkmale und lange Wohnkammern bei niedrigmündigen Gehäusen charakterisiert. Die als polyphyletisch erkannten Gonioclymeniina werden in die Wocklumeriina (mit Wocklumeriaceae, Glatziellaceae n.superfam. und Biloclymeniaceae) und in die Gonioclymeniaceae der Clymeniina geteilt. Gyroclymenia Czarnocki ist ein jüngeres Synonym von Pleuroclymenia Schindewolf, umfasst jedoch nicht die ,Pleuro.' americana -und ,Pleuro.' eurylobica -Artgruppen. Die Gattung ist die ursprünglichste Form der Wocklumeriina und stellt gleichzeitig das Bindeglied zu Platyclymenia (Varioclymenia) der Clymeniaceae dar. Die Gonioclymeniaceae wurzeln in fortgeschrittenen Platyclymeniidae. [source] The microstratigraphic record of abrupt climate changes in cave sediments of the Western MediterraneanGEOARCHAEOLOGY: AN INTERNATIONAL JOURNAL, Issue 5 2001Marie-Agnès Courty The purpose of this paper is to illustrate how calcareous sediments from Pleistocene and Holocene rockshelters and open caves of the Western Mediterranean can provide a stratigraphic record of abrupt climate change. The method proposed here is based on microstratigraphic examination of sedimentary sequences using microscopic techniques. The most important processes for characterizing the sensitivity of each cave to climate variables are: (1) the modes and rate of carbonate sediment production, (2) the nature and intensity of the pedogenic processes responsible for the synchronous alteration of carbonate materials (either those derived from the cave walls or those deposited on the ground surface), and (3) the supply of allogenic sediments, particularly by eolian activity. The cave sediment sequences presented record the marked coolings known as Dansgaard-Oeschger stadials and Heinrich events that occurred during the Pleistocene and the Holocene, as demonstrated by the high resolution records from ice and deep sea cores. At Abric Romanì in northeastern Spain, a series of sharp climatic deteriorations of increasing severity is shown to have occurred synchronously with the transition from the Middle to the Upper Paleolithic, with a period of seasonal frost and strong winds at ca. 37,000 yr B.P., tentatively correlated with Heinrich event 4. At Pigeon Cave, Taforalt (northern Morocco), the transition from the Aterian to Ibero-Maurusian/Epipalaeolithic cultures is dated to around 24,000,20,000 yr B.P. and is punctuated by a series of short cold pulses with evidence for seasonal freezing, soil erosion, and minimal evapotranspiration. In El Miron cave in north-central Spain, the exceptional nature of the Younger Dryas cooling produced a marked destabilization of the cave walls and roof. At El Miron, the stratigraphic evidence for sediment removal due to the rapid percolation of snow melt under a degraded soil cover allows us to reconstruct the nature of the negative excursion at ca. 8200 yr B.P. This example also illustrates how climate-controlled pedogenic processes can create a stratigraphic signature which has often been confused with a sedimentary hiatus. We conclude that cave sediments provide a valuable record of Pleistocene and Holocene climate changes. In appropriate contexts, these sequences allow us to examine the ecological stress generated by these unique global events at a local and regional level and improve our understanding of the complex anthropological processes that occurred at the same time. © 2001 John Wiley & Sons, Inc. [source] The sedimentary records in Mediterranean rockshelters and caves: Archives of environmental changeGEOARCHAEOLOGY: AN INTERNATIONAL JOURNAL, Issue 4 2001Jamie C. Woodward It is important to develop rigorous methods and robust conceptual models for the interpretation of rockshelter and cave sediment records so that the cultural sequences they contain can be considered in their proper environmental context. Much of what we know about the prehistory of the Mediterranean region and adjacent areas has largely been pieced together from materials excavated from sedimentary sequences in these environments. The rockshelters and caves of the region form important environmental and sedimentary archives. Recent work has begun to consider if the remarkable climatic variability evident in the high resolution lacustrine and ice core records is manifest in the rockshelter and cave sediment records of the area. In this context, the two main characteristics of a rockshelter or cave site which control its usefulness as an archive of environmental change are the temporal resolution of the sedimentary record and the environmental sensitivity of the site. Many rockshelters and caves can be described as either Active Karst Settings (AKS) or Passive Karst Settings (PKS) and site type is an important influence on climatic sensitivity with a direct influence upon the usefulness of the sedimentary sequence as a proxy record of climate change. It is now clear that some sites may preserve detailed paleoclimatic records and the climatic signal may be represented by distinctive suites of micromorphological features, by variations in the input of allogenic sediment, or by fluctuations in the mineral magnetic properties of the fine sediment fraction. It can be argued that data derived from the analysis of bulk coarse-grained samples often lacks the stratigraphic resolution and environmental sensitivity that can be obtained from other approaches. The most favorable sites for detailed paleoclimatic reconstruction appear to be in active karst settings such as Theopetra Cave (Greece) and Pigeon Cave (Morocco) where micromorphological analyses offer insights into the stratigraphic record that are not otherwise obtainable. The temporal resolution of a site can only be established through a rigorous stratigraphic analysis and a comprehensive dating program. These are fundamental considerations in the study of rockshelter sediment records, especially when attempting to correlate between sites and draw comparisons with other proxy records of environmental change derived from sedimentary environments with rather different characteristics. Rockshelters and caves are part of a wider sediment system, and their investigation must be accompanied by detailed geomorphological, sedimentological, paleoecological, and geochronological studies of the off-site Quaternary record. © 2001 John Wiley & Sons, Inc. [source] Geological evolution and structural style of the Palaeozoic Tafilalt sub-basin, eastern Anti-Atlas (Morocco, North Africa)GEOLOGICAL JOURNAL, Issue 1 2008E. A. Toto Abstract The Tafilalt is one of a number of generally unexplored sub-basins in the eastern Anti-Atlas of Morocco, all of which probably underwent a similar tectono-stratigraphic evolution during the Palaeozoic Era. Analysis of over 1000,km of 2-D seismic reflection profiles, with the interpretation of ten regional seismic sections and five isopach and isobath maps, suggests a multi-phase deformation history for the Palaeozoic-aged Tafilalt sub-basins. Extensional phases were probably initiated in the Cambrian, followed by uniform thermal subsidence up to at least the end of the Silurian. Major extension and subsidence did not begin prior to Middle/Upper Devonian times. Extensional movements on the major faults bounding the basin to the north and to the south took place in synchronisation with Upper Devonian sedimentation, which provides the thickest part of the sedimentary sequence in the basin. The onset of the compressional phase in Carboniferous times is indicated by reflectors in the Carboniferous sequence progressively onlapping onto the Upper Devonian sequence. This period of compression developed folds and faults in the Upper Palaeozoic-aged strata, producing a structural style characteristic of thin-skinned fold and thrust belts. The Late Palaeozoic units are detached over a regional décollement with a northward tectonic vergence. The folds have been formed by the process of fault-propagation folding related to the thrust imbricates that ramp up-section from the décollement. Copyright © 2007 John Wiley & Sons, Ltd. [source] Electrodynamic Disaggregation: Does it Affect Apatite Fission-Track and (U-Th)/He Analyses?GEOSTANDARDS & GEOANALYTICAL RESEARCH, Issue 1 2010Jörg Giese désagrégation électrodynamique; analyse des traces de fission sur apatite; recuit; analyse (U-Th)/He; diffusion de l'He Apatite fission-track and (U-Th)/He analyses require the liberation of intact idiomorphic apatite grains from rock samples. While routinely being carried out by mechanical methods, electrodynamic disaggregation (ED) offers an alternative approach. The high-voltage discharges produced during the ED process create localised temperature peaks (10000 K) along a narrow plasma channel. In apatite, such high temperatures could potentially reduce the length of fission tracks, which start to anneal at temperatures > 60 °C, and could also enhance He diffusion, which becomes significant at 30,40 °C over geological time scales. A comparison of fission-track analyses and (U-Th)/He ages of apatites prepared both by mechanical (jaw crusher, disk mill) and ED processing provides a way of determining whether heating during the latter method has any significant effect. Apatites from three samples of different geological settings (an orthogneiss from Madagascar, the Fish Canyon Tuff, and a muscovite-gneiss from Greece) yielded statistically identical track length distributions compared to samples prepared mechanically. Additionally, (U-Th)/He ages of apatites from a leucogranite from Morocco prepared by both methods were indistinguishable. These first results indicated that during electrodynamic disaggregation apatite crystals were not heated enough to partially anneal the fission tracks or induce significant diffusive loss of He. Les analyses des traces de fission et des rapports isotopiques (U-Th)/He sur apatite nécessitent la séparation de grains intacts et automorphes d'apatite à partir des échantillons de roche. La désagrégation électrodynamique (DE) offre une approche alternative aux méthodes mécaniques utilisées actuellement en routine. Les décharges de haute tension produite pendant le processus de DE entrainent la formation de pics de température (10000 K) localisés le long d'un étroit canal de plasma. Dans l'apatite, de telles températures peuvent potentiellement réduire la longueur des traces de fission, qui commencent à recuire à des températures > 60 °C, et peuvent aussi favoriser la diffusion de l'Hélium, qui devient significative à des températures de 30,40 °C sur des échelles de temps géologiques. Une comparaison des résultats obtenus à partir des analyses des traces de fission et des âges (U-Th)/He sur des apatites séparées par des moyens mécaniques (concasseur à mâchoires, broyeur à disque) et sur d'autres séparées par la méthode de désagrégation électrodynamique offre un moyen de déterminer si le chauffage lié,à la seconde méthode a un effet significatif. Les apatites séparées par la méthode DE à partir de trois échantillons provenant de différents contextes géologiques (un orthogneiss de Madagascar, le tuf de Fish Canyon et un gneiss à muscovite de Grèce) fournissent des distributions de longueurs de trace de fission statistiquement identiques par rapport à des échantillons préparés mécaniquement. En outre, des âges (U-Th)/He obtenus à partir d'apatites provenant d'un leucogranite du Maroc et préparées par les deux méthodes (DE et mécaniques) sont indiscernables. Ces premiers résultats indiquent que, pendant la désagrégation électrodynamique, les cristaux d'apatite n'ont pas été suffisamment chauffés pour soit recuire partiellement les traces de fission soit provoquer une perte significative par diffusion de l'He. [source] Post-return experiences and transnational belonging of return migrants: a Dutch,Moroccan case studyGLOBAL NETWORKS, Issue 4 2010JUNE DE BREE Abstract In this article we explore the links between return migration, belonging and transnationalism among migrants who returned from the Netherlands to northeast Morocco. While transnationalism is commonly discussed from the perspective of a receiving country, this study shows that transnationalism also plays a vital role in reconstructing post-return belonging. Return migration is not simply a matter of ,going home', as feelings of belonging need to be renegotiated upon return. While returnees generally feel a strong need to maintain various transnational practices, the meanings they attach to these practices depend on motivations for return, gender and age. For former (male) labour migrants, transnational practices are essential for establishing post-return belonging, whereas such practices are less important for their spouses. Those who returned as children generally feel uprooted, notwithstanding the transnational practices they maintain. The amount of agency migrants are able to exert in the return decision-making process is a key factor in determining the extent to which returnees can create a post-return transnational sense of home. [source] Reformulating tradition and modernity: Moroccan migrant women and the transnational division of ritual spaceGLOBAL NETWORKS, Issue 3 2002Ruba Salih In this article I analyse the rituals that transnational migrants who live and work in Europe (mainly Italy) perform in Morocco during their return there for summer holidays. The transnational dimension of rituals and ceremonies reveals the diverse ways in which Moroccan families gain social recognition across transnational space. I explore how migrants construct and display their identities contextually and in opposition to multiple Others. By performing the traditional rituals associated with important turning points in their lives in Morocco, migrants seek to reintegrate themselves and maintain their membership of their community of origin. At the same time, however, these performances bring to the surface a hidden agenda: the assertion and exhibition of migrants' differences with respect to those who have stayed behind. These rituals, which provide a perspective through which to analyse the intersection of global and local interconnections, also reveal complex and shifting interpretations of ,tradition' and ,modernity', and the practices in which these are embedded. I conclude by suggesting that, in this process, migrants develop a creative interplay with ,traditional practices' by subverting, reformulating and giving new creative shape to their meaning and content. [source] Controls on Ground Water Chemistry in the Central Couloir Sud Rifain, MoroccoGROUND WATER, Issue 2 2010Lahcen Benaabidate Irrigation, urbanization, and drought pose challenges for the sustainable use of ground water in the central Couloir sud rifain, a major agricultural region in north-central Morocco, which includes the cities of Fès and Meknès. The central Couloir is underlain by unconfined and confined carbonate aquifers that have suffered declines in hydraulic head and reductions in spring flow in recent decades. Previous studies have surveyed ground water flow and water quality in wells and springs but have not comprehensively addressed the chemistry of the regional aquifer system. Using graphical techniques and saturation index calculations, we infer that major ion chemistry is controlled (1) in the surficial aquifer by cation exchange, calcite dissolution, mixing with deep ground water, and possibly calcite precipitation and (2) in the confined aquifer and warm springs by calcite dissolution, dolomite dissolution, mixing with water that has dissolved gypsum and halite, and calcite precipitation. Analyses of 2H and 18O indicate that shallow ground water is affected by evaporation during recharge (either of infiltrating precipitation or return flow), whereas deep ground water is sustained by meteoric recharge with little evaporation. Mechanisms of recharge and hydrochemical evolution are broadly consistent with those delineated for similar regional aquifer systems elsewhere in Morocco and in southern Spain. [source] Withanolides from Withania adpressaHELVETICA CHIMICA ACTA, Issue 2 2007Hasna Abdeljebbar, Lalla Abstract From the leaves of Withania adpressa, a plant endemic to Sahara of Morocco and Algeria, the novel steroidal lactone (22R)-14,,15,,17,,20, -tetrahydroxy-1-oxowitha-2,5,24-trien-26,22-olide (=,(15S,17S)-14,15,17,20-tetrahydroxy-22,26-epoxyergosta-2,5,24-triene-1,26-dione; 1), was isolated, along with three known compounds, withanolides F (2), J (3), and oleanolic acid. Their structures were mainly solved by in-depth 1D- and 2D-NMR (including ADEQUATE) experiments, as well as by HR-MS analyses and chemical evidence. [source] Understanding hydrological processes with scarce data in a mountain environmentHYDROLOGICAL PROCESSES, Issue 12 2008A. Chaponnière Abstract Performance of process-based hydrological models is usually assessed through comparison between simulated and measured streamflow. Although necessary, this analysis is not sufficient to estimate the quality and realism of the modelling since streamflow integrates all processes of the water cycle, including intermediate production or redistribution processes such as snowmelt or groundwater flow. Assessing the performance of hydrological models in simulating accurately intermediate processes is often difficult and requires heavy experimental investments. In this study, conceptual hydrological modelling (using SWAT) of a semi-arid mountainous watershed in the High Atlas in Morocco is attempted. Our objective is to analyse whether good intermediate processes simulation is reached when global-satisfying streamflow simulation is possible. First, parameters presenting intercorrelation issues are identified: from the soil, the groundwater and, to a lesser extent, from the snow. Second, methodologies are developed to retrieve information from accessible intermediate hydrological processes. A geochemical method is used to quantify the contribution of a superficial and a deep reservoir to streamflow. It is shown that, for this specific process, the model formalism is not adapted to our study area and thus leads to poor simulation results. A remote-sensing methodology is proposed to retrieve the snow surfaces. Comparison with the simulation shows that this process can be satisfyingly simulated by the model. The multidisciplinary approach adopted in this study, although supported by the hydrological community, is still uncommon. Copyright © 2007 John Wiley & Sons, Ltd. [source] Contribution of genetic and environmental factors in the pathogenesis of Crohn's disease in a large family with multiple casesINFLAMMATORY BOWEL DISEASES, Issue 5 2007Marie Joossens MSc Abstract Background: A large family of Moroccan immigrants was investigated. In this family the father developed Crohn's disease (CD) after moving from Morocco to Belgium and successively 4 of his 8 children subsequently developed CD. There was no previous history of familial CD. Methods: The family was interviewed at their home and an elaborated questionnaire was completed. The food and sanitation characteristics of the family were investigated. Moreover, serological markers were tested in all family members, including ASCA, ASCAg, ALCA, ACCA, Omp, and ANCA, using enzyme-linked immunosorbent assay and indirect immunofluorescence. Genetic variants in CARD15, TLR4, NOD1, CARD8, and DLG5 associated with CD were tested as well. The complete medical history of all patients was reviewed. Results: There were no known genetic variants associated with CD in this family. None of the serological antibodies could discriminate between patients and unaffected family members, although the antibody titers were higher in diseased family members as compared with the healthy family members. Conclusion: The occurrence of 5 new cases of CD within 1 Moroccan family after immigration to Belgium cannot be explained by the known genetic susceptibility factors, and thus suggests a major environmental factor probably not related to sanitation in childhood. (Inflamm Bowel Dis 2007) [source] Decadal changes in the link between El Niño and springtime North Atlantic oscillation and European,North African rainfallINTERNATIONAL JOURNAL OF CLIMATOLOGY, Issue 11 2003Peter Knippertz Abstract The link between El Niño,southern oscillation (ENSO) variability in boreal winter (represented by the NIÑO3 index, i.e. East Pacific sea-surface temperature anomalies) and the large-scale circulation and weather conditions over Europe,northwest Africa in spring is explored, considering station reports of precipitation, sea-level pressure (SLP) anomalies and two North Atlantic oscillation (NAO) indices. It is found that these relations have undergone consistent and simultaneous changes in the 20th century. Three characteristic periods can be identified. During 1900,25 and 1962,87, positive NIÑO3 index values are associated with enhanced precipitation over central Europe and reduced rainfall in southern Europe and northern Africa. The ENSO influence on precipitation over Scotland and Norway is small. The rainfall anomalies can be explained from the advective and dynamical implications of a north,south dipole in SLP correlations (warm ENSO events followed by low pressure in northern Europe and high pressure over the Mediterranean Sea,North Africa). This dipole hardly projects on the commonly used NAO centres (Iceland and Azores/Gibraltar) and thus ENSO,NAO correlations are insignificant. During 1931,56 the NIÑO3 index reveals little influence on precipitation over the Iberian Peninsula and Morocco, but there are large negative correlations with precipitation over Scotland and Norway. This is related to an alteration of the NIÑO3,SLP correlation pattern, which implies high pressure over northern Europe and low pressure over central Europe after warm events, and thus a virtually inverted dipole with respect to the other two periods. The large westward extension of the dipole leads to a significant NAO,NIÑO3 correlation of r = ,0.5. These alterations were accompanied by substantial large-scale circulation changes during the period 1931,56, as revealed by anomalously high pressure and dry conditions over central,western Europe, a change in precipitation-producing SLP patterns for Morocco and an anomalously low number of positive NAO and NIÑO3 index values. It is left for discussion as to whether the decadal variations described are due to a change in the physics of the teleconnection or to stochastic fluctuations. Copyright © 2003 Royal Meteorological Society [source] Reconstruction of the North Atlantic Oscillation, 1429,1983INTERNATIONAL JOURNAL OF CLIMATOLOGY, Issue 12 2001Mary F. Glueck Abstract The North Atlantic Oscillation (NAO) is considered to be the dominant mode of winter atmospheric variability in the Northern Hemisphere (Barnston AG, Livezey RE. 1987. Classification, seasonality and persistence of low frequency atmospheric circulation patterns. Monthly Weather Review115: 1083,1126), especially in the North Atlantic region. A better understanding of its recent variability in the context of pre-instrumental period variations is critical for prediction purposes. A 555-year (1429,1983) multi-proxy reconstruction of the cool season NAO, calibrated against the Lisbon,Iceland (LISJHI) NAO, is presented. Predictor variables include tree-ring chronologies from Morocco and Finland, GISP2 ,18O annual series, and a GISP2 snow accumulation record. Although the reconstructed values are generally lower than the instrumental values during the calibration period (1863,1983), the final reconstruction does capture the low frequency of the instrumental NAO. The reconstruction compares favourably with existing shorter NAO reconstructions and with the instrumental NAO. The variability in the reconstructed NAO is also discussed within the context of lengthy regional climate records. Results suggest that the occurrence and length of the recent persistently high phase of the NAO are not unusual over the 555-year period of time, but that the magnitude of some of the instrumental values may, in fact, be unique. Copyright © 2001 Royal Meteorological Society [source] | |||||||||||||||||||||||||||||||||||||||||||