A geochemical and petrological study of volcanic rocks in the Beardmore-Geraldton Archaean Greenstone Belt, Northwestern Ontario

Three repetitive sequences of northward youngIng, east striking, linear, volcano-sedimentary units are found in the late Archaean BeardmoreGeraldton greenstone belt, situated within the Wabigoon subprovince of the Superior Province of northwestern Ontario. The volcanic components are characterised by basaltic flows that are pillowed at the top and underlain by variably deformed massive flows which may In part be intrusive. Petrographic examination of the volcanic units indicates regional metamorphism up to greenschist facies (T=3250 C - 4500 C, P=2kbars) overprinted by a lower amphibolite facies thermal event (T=5750 C, P=2kbars) confined to the south-eastern portion of the belt. Chemical element results suggest olivine, plagioclase and pyroxene are the main fractionating mineral phases. Mobility studies on the varIOUS chemical elements indicate that K, Ca, Na and Sr are relatively mobile, while P, Zr, Ti, Fet (total iron = Fe203) and Mg are relatively immobile. Discriminant diagrams employing immobile element suggests that the majority of the samples are of oceanic affinity with a minor proportion displaying an island arc affinity. Such a transitional tectonic setting IS also refle.cted in REE data where two groups of volcanic samples are recognised. Oceanic tholeiites are LREE depleted with [La/Sm] N = 0.65 and a relatively flat HREE profile with [Sm/Yb] N = 1.2. Island arc type basalts (calc-alkaline) are LREE enriched, with a [La/Sm] N = 1.6, and a relatively higher fractionated HREE profile with [Sm/Yb] N = 1.9. Petrogenetic modelling performed on oceanIC tholeiites suggests derivation from a depleted spinel lherzolite source which undergoes 20% partial melting. Island arc type basalts can be derived by 10% partial melting of a hypothetical amphibolitised oceanic tholeiite source. The majority of the volcanic rocks in the Beardmore-Geraldton Belt are interpreted to represent fragments of oceanic crust trapped at a consuming plate margin. Subsequent post accretionary intrusion of gabbroic rocks (sensu lato) with calc-alkaline affinity is considered to result in the apparent hybrid tectonic setting recognized for the BGB.

La présence phénicienne en Syrie du Nord à l’Âge du Fer, 1000-500 av. J.C.

RÉSUMÉ Cette étude porte sur la présence phénicienne en Syrie du Nord uniquement pendant la première moitié de l’Âge du Fer, i.e entre 1000 et 500 av. J.C. Elle est fondée sur l’analyse des données archéologiques et littéraires des principaux sites côtiers de cette région, al Mina, Ras el Bassit, Tell Kazel, Tell Soukas et Amrit. Après une présentation des caractéristiques culturelles de la civilisation phénicienne, j’aborde l’analyse de ces sites. Les données qui permettent de prouver une présence phénicienne dans la région s’avèrent nombreuses et j’en conclus que les Phéniciens devaient constituer une minorité importante de la population de ces sites, au même titre que les Grecs ou les Chypriotes, la majorité étant d’origine syrienne. Mais dans certains cas, notamment sur les sites les plus proches des grandes capitales phéniciennes, il n’est pas impossible qu’ils aient été majoritaires. L’étude illustrera par ailleurs l’importance du rôle des cités de la Syrie du Nord dans les échanges commerciaux et culturels avec les autres cultures du Sud-Est du bassin méditerranéen, notamment celles de la Grèce, île de Chypre, de la Cilicie et de la Syrie intérieure.

Craftsmanship as a means of empowerment for the traditional population of Guaraqueçaba : a case study

Cette recherche consiste en une étude de cas sur un groupe d’artisans qui a réussi à transformer sa production artisanale en importante source de revenus. Ces artisans, de culture caiçara, ont formé une coopérative dans la municipalité de Guaraqueçaba, dans l’État du Paraná au Brésil. Caiçara est le nom de la population traditionnelle métisse qui habite dans les zones côtières du Sud et Sud-est du Brésil. La région de Guaraqueçaba abrite des écosystèmes de biodiversité extrêmement riche et précieuse, dont la conservation est une priorité à l’échelle mondiale. Afin de réguler l’utilisation des ressources naturelles de ces écosystèmes, une aire protégée a été créée en 1985. Par la suite, de sévères restrictions entourant les moyens de subsistance ont été imposées aux communautés caiçaras, ayant comme conséquences leur appauvrissement, la discontinuation de leur mode de vie et des dommages à leur culture. Cette étude de cas s’est penchée sur une population traditionnelle luttant pour améliorer ses conditions de vie par le biais du design, activité par laquelle nous créons de la culture matérielle. L’objectif de cette recherche est de comprendre comment la création d’artisanat destiné à la vente peut être un vecteur d’autonomisation et de valorisation de la culture locale. L’approche de la collecte des données sur le terrain, inspiré de l’ethnographie, a utilisé les méthodes suivant : des entrevues (non structurées et semi-dirigées), des observations (participantes et non participantes) et des photos. Ayant un caractère exploratoire, l’étude a exploré des questions liées à l’autonomisation et la culture avec le but d’encourager et de préparer le terrain pour des recherches futures.

Les Néerlandais en exemple : l’image des Néerlandais dans les écrits religieux français portant sur les Antilles et la Côte Sauvage sud-américaine au XVIIe siècle

Cette étude se penche sur les représentations des Néerlandais véhiculées par les chroniques missionnaires écrites par les religieux français de passage aux Antilles et sur la Côte Sauvage sud-américaine au XVIIe siècle et au début du XVIIIe siècle. En repérant et en analysant l’évolution de ces représentations, il appert que l’altérité néerlandaise était, entre 1640 et 1670, l’altérité européenne que les chroniqueurs religieux mettaient avantageusement de l’avant comme modèle de réussite économique et colonial pour modeler l’entreprise de colonisation française aux Antilles. C’est notamment le cas des écrits du dominicain Jean-Baptiste du Tertre (1654, 1667-1671), missionnaire bien au fait de l’altérité néerlandaise. Cependant, avec la marginalisation de la présence néerlandaise dans les Petites Antilles à la fin du xviie siècle, l’examen de la chronique de Jean-Baptiste Labat (1722) révèle que l’altérité néerlandaise a été remplacée par l’altérité anglaise lorsqu’il s’agit de proposer un modèle de réussite économique et colonial aux Français.

La lucha de la Unión Europea contra el crimen organizado transnacional. Estudio de caso: tráfico ilegal de armas pequeñas y ligeras provenientes de Albania y Kosovo (2001-2005)

En el contexto de la lucha de la Unión Europea contra el crimen organizado transnacional, el tráfico ilegal de armas pequeñas y ligeras proveniente de los grupos criminales albaneses y kosovares, es uno de los delitos a los que la Unión Europea ha tenido que hacer frente. Así pues, esta investigación logró analizar cómo la falta de coordinación de las políticas europeas implementadas para luchar contra el tráfico ilegal de armas pequeñas y ligeras y la corrupción estatal en Albania y Kosovo, fueron los dos factores de mayor influencia para evidenciar el impacto a la efectividad de dichas políticas implementadas. Para esto se debió comprender las dinámicas de los grupos criminales y la influencia de la corrupción en su actuar, y después examinar las políticas implementadas por la Unión Europea y los factores que no permitieron que existiera coordinación entre ellas.

Participació de les aigües subterrànies en la gènesi d'ambients palustres continentals: el cas dels prats de Sant Sebastià (Caldes de Malavella, Girona)

The area known as 'prats de Sant Sebastià' is in Caldes de Malavella. It is part of the wetlands located in the south-eastern end of the Selva Basin. Several areas with unusually high conductivity (EC up to 24,500 uS/cm) have been identified in this place. This fact allows highly specialised and comparatively rare botanical species to grow in this area. These saline soils follow a north-south line-up. The geophysical data, obtained with a field conductivemeter (EM 31), show that this superficial line-up continues in the subsoil. In addition to this, the conductivity cartography, made for an electromagnetic exploration depth of 6 meters, shows that the width of the region where these salinity anomalies take place increases in depth. When included in the hidrogeological context of this sector of the Selva Basin, these data bring new elements for the study of the genesis and working of these marshy environments. The model that future research will have to confirm, maintains that the groundwater discharges coming from the underlying hydrogeothermal aquifer are a conditioning factor of the aforementioned phenomenon. This ascending flow of highly mineralised waters (TDS of about 3,500 mg/l) can produce and keep stable the soil salinity

Avaliação escolar no ensino superior de letras: entre o discurso e a prática

O objeto desta pesquisa é a avaliação da aprendizagem, tendo como foco central a análise dos discursos e práticas dos professores de Cursos de Licenciatura de Letras. Este estudo foi desenvolvido com docentes de duas instituições de ensino superior do interior do estado da Paraíba, localizado no nordeste brasileiro. O objetivo geral deste estudo é: analisar as semelhanças, diferenças e contradições resultantes da comparação entre os discursos e o que se pratica na avaliação da aprendizagem dos professores de Letras do Ensino Superior de uma instituição de ensino superior particular de Patos/PB e os de uma pública de Catolé do Rocha/PB. Esta foi uma pesquisa qualitativa com uma amostra de cinco docentes de cada estabelecimento de ensino superior, somando-se dez ao todo. Foram feitas entrevistas com perguntas abertas e fechadas, cujas respostas tiveram uma análise de conteúdo, e o resultado desta foi confrontado com os dados da observação das práticas de sala de aula dos professores da amostra. Constatou-se que há casos de professores que têm discursos diferentes da sua prática de avaliação da aprendizagem. Há também problemas de interação entre docentes e discentes em relação à avaliação da aprendizagem que aumentam o índice de reprovação do alunado, o que poderia ser evitado. No entanto, de modo geral há um compromisso com a qualidade de ensino dos docentes entrevistados. Os autores e teóricos que inspiraram esta pesquisa foram: Wachowicz (2000), Castanho (2000), Berbel (2001), Sacristán e Gómez (1998), Hoffman (1996 e 2003), Luckesi (1994), Vasconcelos (2000) e Villas Boas (2000), entre outros.

Working in partnership with the Museum Training Institute providing in service training for museum personnel

The South Eastern Museums Service is one of ten Area Museums Councils in Great Britain. They are partnerships; membership organizations to which the 2 000 + museums belong. They provide advice, support, technical services, information and training for their members. They are the principal channel of government grant-in-aid to local government, university and independent museums. This funding comes from the Department of National Heritage via the Museums & Galleries Commission. At the South Eastern Museums Service I am responsible for the development and delivery of training for 600 museums in our region and the provision of information about museums and of interest to museums. This paper explains how we approach in-service training and the value of the definition of national standards for our work. It will pose some questions: What is training? What is a training need? and describe a new initiative, the development of training materials and their delivery.

The water quality of the LOCAR Pang and Lambourn catchments

The water quality of the Pang and Lambourn, tributaries of the River Thames, in south-eastern England, is described in relation to spatial and temporal dimensions. The river waters are supplied mainly from Chalk-fed aquifer sources and are, therefore, of a calcium-bicarbonate type. The major, minor and trace element chemistry of the rivers is controlled by a combination of atmospheric and pollutant inputs from agriculture and sewage sources superimposed on a background water quality signal linked to geological sources. Water quality does not vary greatly over time or space. However. in detail, there are differences in water quality between the Pang and Lambourn and between sites along the Pang and the Lambourn. These differences reflect hydrological processes, water flow pathways and water quality input fluxes. The Pangs pattern of water quality change is more variable than that of the Lambourn. The flow hydrograph also shows both a cyclical and 'uniform pattern' characteristic of aquifer drainage with, superimposed, a series of 'flashier' spiked responses characteristic of karstic systems. The Lambourn, in contrast, shows simpler features without the 'flashier' responses, The results are discussed in relation to the newly developed UK community programme LOCAR dealing with Lowland Catchment Research. A descriptive and box model structure is provided to describe the key features of water quality variations in relation to soil, unsaturated and groundwater flows and storage both away from and close to the river.

Genetic structure and systematic relationships within the Ophrys fuciflora aggregate (Orchidaceae: Orchidinae): high diversity in Kent and a wind-induced discontinuity bisecting the Adriatic

A recent phylogenetic study based on multiple datasets is used as the framework for a more detailed examination of one of the ten molecularly circumscribed groups identified, the Ophrys fuciflora aggregate. The group is highly morphologically variable, prone to phenotypic convergence, shows low levels of sequence divergence and contains an unusually large proportion of threatened taxa, including the rarest Ophrys species in the UK. The aims of this study were to (a) circumscribe minimum resolvable genetically distinct entities within the O. fuciflora aggregate, and (b) assess the likelihood of gene flow between genetically and geographically distinct entities at the species and population levels. Fifty-five accessions sampled in Europe and Asia Minor from the O. fuciflora aggregate were studied using the AFLP genetic fingerprinting technique to evaluate levels of infraspecific and interspecific genetic variation and to assess genetic relationships between UK populations of O. fuciflora s.s. in Kent and in their continental European and Mediterranean counterparts. The two genetically and geographically distinct groups recovered, one located in England and central Europe and one in south-eastern Europe, are incongruent with current species delimitation within the aggregate as a whole and also within O. fuciflora s.s. Genetic diversity is higher in Kent than in the rest of western and central Europe. Gene flow is more likely to occur between populations in closer geographical proximity than those that are morphologically more similar. Little if any gene flow occurs between populations located in the south-eastern Mediterranean and those dispersed throughout the remainder of the distribution, revealing a genetic discontinuity that runs north-south through the Adriatic. This discontinuity is also evident in other clades of Ophrys and is tentatively attributed to the long-term influence of prevailing winds on the long-distance distribution of pollinia and especially seeds. A cline of gene flow connects populations from Kent and central and southern Europe; these individuals should therefore be considered part of an extensive meta-population. Gene flow is also evident among populations from Kent, which appear to constitute a single metapopulation. They show some evidence of hybridization, and possibly also introgression, with O. apifera.

Using the significant dust deposition event on the glaciers of Mt. Elbrus, Caucasus Mountains, Russia on 5 May 2009 to develop a method for dating and "provenancing" of desert dust events recorded in snow pack

A significant desert dust deposition event occurred on Mt. Elbrus, Caucasus Mountains, Russia on 5 May 2009, where the deposited dust later appeared as a brown layer in the snow pack. An examination of dust transportation history and analysis of chemical and physical properties of the deposited dust were used to develop a new approach for high-resolution “provenancing” of dust deposition events recorded in snow pack using multiple independent techniques. A combination of SEVIRI red-green-blue composite imagery, MODIS atmospheric optical depth fields derived using the Deep Blue algorithm, air mass trajectories derived with HYSPLIT model and analysis of meteorological data enabled identification of dust source regions with high temporal (hours) and spatial (ca. 100 km) resolution. Dust, deposited on 5 May 2009, originated in the foothills of the Djebel Akhdar in eastern Libya where dust sources were activated by the intrusion of cold air from the Mediterranean Sea and Saharan low pressure system and transported to the Caucasus along the eastern Mediterranean coast, Syria and Turkey. Particles with an average diameter below 8 μm accounted for 90% of the measured particles in the sample with a mean of 3.58 μm, median 2.48 μm. The chemical signature of this long-travelled dust was significantly different from the locally-produced dust and close to that of soils collected in a palaeolake in the source region, in concentrations of hematite. Potential addition of dust from a secondary source in northern Mesopotamia introduced uncertainty in the “provenancing” of dust from this event. Nevertheless, the approach adopted here enables other dust horizons in the snowpack to be linked to specific dust transport events recorded in remote sensing and meteorological data archives.

Using the significant dust deposition event on the glaciers of Mt. Elbrus, Caucasus Mountains, Russia on 5 May 2009 to develop a method for dating and provenancing of desert dust events recorded in snow pack.

A significant desert dust deposition event occurred on Mt. Elbrus, Caucasus Mountains, Russia on 5 May 2009, where the deposited dust later appeared as a brown layer in the snow pack. An examination of dust transportation history and analysis of chemical and physical properties of the deposited dust were used to develop a new approach for high-resolution provenancing of dust deposition events recorded in snow pack using multiple independent techniques. A combination of SEVIRI red-green-blue composite imagery, MODIS atmospheric optical depth fields derived using the Deep Blue algorithm, air mass trajectories derived with HYSPLIT model and analysis of meteorological data enabled identification of dust source regions with high temporal (hours) and spatial (ca. 100 km) resolution. Dust, deposited on 5 May 2009, originated in the foothills of the Djebel Akhdar in eastern Libya where dust sources were activated by the intrusion of cold air from the Mediterranean Sea and Saharan low pressure system and transported to the Caucasus along the eastern Mediterranean coast, Syria and Turkey. Particles with an average diameter below 8 μm accounted for 90% of the measured particles in the sample with a mean of 3.58 μm, median 2.48 μm and the dominant mode of 0.60 μm. The chemical signature of this long-travelled dust was significantly different from the locally-produced dust and close to that of soils collected in a palaeolake in the source region, in concentrations of hematite and oxides of aluminium, manganese, and magnesium. Potential addition of dust from a secondary source in northern Mesopotamia introduced uncertainty in the provenancing of dust from this event. Nevertheless, the approach adopted here enables other dust horizons in the snowpack to be linked to specific dust transport events recorded in remote sensing and meteorological data archives.

Development of warm SST errors in the southern tropical Atlantic in CMIP5 decadal hindcasts

SST errors in the tropical Atlantic are large and systematic in current coupled general-circulation models. We analyse the growth of these errors in the region of the south-eastern tropical Atlantic in initialised decadal hindcasts integrations for three of the models participating in the Coupled Model Inter-comparison Project 5. A variety of causes for the initial bias development are identified, but a crucial involvement is found, in all cases considered, of ocean-atmosphere coupling for their maintenance. These involve an oceanic “bridge” between the Equator and the Benguela-Angola coastal seas which communicates sub-surface ocean anomalies and constitutes a coupling between SSTs in the south-eastern tropical Atlantic and the winds over the Equator. The resulting coupling between SSTs, winds and precipitation represents a positive feedback for warm SST errors in the south-eastern tropical Atlantic.

Marine Isotope Stage 9 environments of fluvial deposits at Hackney, north London, UK

Middle Pleistocene deposits at Hackney, north London comprise a thick unit of organic sands and silts occupying a channel near the confluence of the River Thames in south-eastern England and its left-bank tributary the River Lea. They represent a short time interval, perhaps no more than a few years, within a late Middle Pleistocene interglacial. The organic sediments are overlain by unfossiliferous sands and gravels indicating deposition on the floodplain of a braided river under cool or cold climatic conditions. The fossil plant, insect, mollusc and vertebrate remains from the interglacial deposits all indicate climatic conditions with summers warmer than the present in SE England, and winters with a similar thermal climate. The biostratigraphic evidence suggests that the time period represented by the organic unit is part of MIS 9, although the geochronological evidence for such an age is inconclusive. The palaeontological evidence strongly suggests that this temperate stage was warmer than the succeeding temperate stage MIS 7 or the Holocene, and approaching the Ipswichian (MISs 5e) in its warmth. The multidisciplinary description of the Hackney deposits is one of the first to reconstruct terrestrial conditions in Marine Isotope Stage 9 in Western Europe.

The central European floods of August 2002: Part 2 - Synoptic causes and considerations with respect to climatic change

In the first part of this paper (Ulbrich et al. 2003), we gave a description of the August 2002 rainfall events and the resultant floods, in particular of the flood wave of the River Elbe. The extreme precipitation sums observed in the first half of the month were primarily associated with two rainfall episodes. The first episode occurred on 6/7 August 2002. The main rainfall area was situated over Lower Austria, the south-western part of the Czech Republic and south-eastern Germany. A severe flash flood was produced in the Lower Austrian Waldviertel (`forest quarter’ ). The second episode on 11± 13 August 2002 most severely affected the Erz Mountains and western parts of the Czech Republic. During this second episode 312mm of rain was recorded between 0600GMT on 12 August and 0600GMT on 13 August at the Zinnwald weather station in the ErzMountains, which is a new 24-hour record for Germany. The flash floods resulting from this rainfall episode and the subsequent Elbe flood produced the most expensive weatherrelated catastrophe in Europe in recent decades. In this part of the paper we discuss the meteorological conditions and physical mechanisms leading to the two main events. Similarities to the conditions that led to the recent summer floods of the River Oder in 1997 and the River Vistula in 2001 will be shown. This will lead us to a consideration of trends in extreme rainfall over Europe which are found in numerical simulations of anthropogenic climate change.