This thesis analyzes and documents the splint armor material from Valsgärde 8 and Vendel I,X, and XI. This armor is then contextualized in the warrior institutions, weapon-systems, and fighting techniques of warbands from Central Sweden. Analogies for the splint armor are sought after with the closest parallels being found around the Black Sea area, associated with Byzantine, Sassanid, and Steppe-Nomadic martial cultures. The systems of exchange between these two regions are then analyzed in order to inform as to where this armor came from, whyit is there in Central Sweden, and what this can tell us about the development of military contacts between Central Sweden and the Black Sea area during the Vendel Period. / Denna uppsats berör analysen och dokumentationen av det Vendeltida skenpansarmaterialet från Valsgärde 8 och Vendel I, X och XI, där skenpansarna sätts i kontext med krigarinstitutioner, vapensystem och stridstekniker från krigsband i Centrala Sverige. Analogier för dessa skenpansar med närmaste paralleller har påträffats i Svartahavsområdet och associeras med Bysantinska, Sasanidiska och stäppnomadiska krigarkulturer. Utbytessystem mellan dessa två regioner analyseras för att få förståelse för var denna typ av rustning härrör ifrån, varför den har hamnat i Centrala Sverige och vad de kan säga om utvecklingen av militära kontakter mellan Centrala Sverige och Svartahavsområdet under Vendeltiden.

Long term data generated at four rural stations are compared to determine similarities and differences in aerosol compositions and factors contributing to observed differences at different regions in Turkey. The stations used in this study are located at Mediterranean coast (20 km to the west of Antalya city), Black Sea coast (20 km to the east of Amasra town), Central Anatolia (&Ccedil / ubuk, Ankara) and Northeastern part of the Anatolian Plateau (at Mt. Uludag). Data used in comparisons were generated in previous studies. However, some re-analysis of data were also performed / (1) to improve the similarities of the parameters compared and (2) to be able to apply recently-developed methodologies to data sets. Data from Mediterranean and Black Sea stations were identical in terms of parameters measured and were suitable for extensive comparison. However, fewer parameters were measured at &Ccedil / ubuk and Uludag stations, which limited the comparisons involving these two stations. Comparison included levels of major ions and elements, short-term and seasonal variations in concentrations, background (baseline) concentrations of elements, flow climatology of regions, correlations between elements, potential source areas affecting regions, and source types affecting chemical composition of particles. Comparison of levels of measured parameters in four regions showed that there are some differences in concentrations that arise from differences in the local characteristics of the sampling points. For example very high concentrations of elements such as Na and Cl in the Mediterranean region is attributed to closer proximity of the Antalya station to coast and not a general feature of the Mediterranean aerosol. There are also significant regional differences in the concentrations of measured elements and ions as well. Concentrations of anthropogenic elements are very similar at two coastal stations (Antalya and Amasra), but they are approximately a factor of two smaller at the two stations that are located on the Anatolian Plateau. This difference between coastal and high altitude plateau stations, which is common to all anthropogenic species, is attributed to different source regions and transport mechanisms influencing coastal regions and Anatolian Plateau. Some statistically significant differences were also observed in the temporal variations of elements and ions measured in different stations. The elements with crustal origin showed similar seasonal pattern at all stations, with higher concentrations in summer and lower concentrations in winter. This difference between summer and winter is attributed to suppression of re-suspension of crustal aerosol from wet or ice-covered surface soil in winter. Concentrations of anthropogenic elements, on the other hand, did not show a statistically significant seasonal trend at Amasra, &Ccedil / ubuk and Uludag stations, but they have higher concentrations during summer months at the Antalya station. This difference between Mediterranean aerosol and aerosol at the Central and Northern Turkey is due to influence of more local sources on &Ccedil / ubuk, Amasra and Uludag stations and domination of more distant source in determining aerosol composition at the Mediterranean region. A similar conclusion of strong influence of local sources on chemical composition of particles at the Central Anatolia was also suggested by the comparison of baseline concentrations in each station. General features in flow climatology (residence times of upper atmospheric air masses) in each region are found to be similar with more frequent flow from W, WNW, NW and NNW wind sectors. Since these are the sectors that include high emitting countries in Eastern and Western Europe and Russia, transport from these sectors are expected to bring pollution from both distant European countries and more local Balkan countries and western parts of Turkey. Flow climatology in stations showed small, but statistically significant, differences between summer and winter seasons. These variations suggested that the station at the Central Anatolia and Black Sea (&Ccedil / ubuk Amasra and Uludag stations) are affected from sources located at the Western Europe in winter season and from sources located at the Eastern Europe in summer. Mediterranean aerosol, on the other hand, are affected from sources at the Western Europe and do not show any seasonal differences. This variation in flow climatology between summer and winter seasons (and lack of variation at the Mediterranean station) is supported by the seasonal variation (and lack of variation at the Mediterranean station) in SO42-/NO3- ratio measured at the stations. Potential source contribution function (PSCF) values are calculated for selected elements and ions in each station. Statistical significance of calculated PSCF values is tested using bootstrapping technique. Results showed that specific grids at Russia and at Balkan countries are common source regions affecting concentrations of anthropogenic elements at all four regions in Turkey. However, each station is also affected from specific source regions as well. Aerosol composition at the Anatolian Plateau are affected from sources closer to the sampling points whereas Mediterranean and Black Sea aerosol are affected from source regions that farther away from the receptors. It should be noted that the same conclusion is also reached in comparison of seasonal patterns and baseline concentrations at these stations. Types of sources affecting aerosol composition at Black Sea, Mediterranean and Central Anatolia are also compared. Source types affecting atmospheric composition in these regions were calculated using positive matrix factorization (PMF). The results showed that aerosol at the Black Sea, Central Anatolia and Mediterranean atmosphere consists of 8, 6 and 7 components, respectively. Two of these components, namely a crustal component and a long-range transport component are common in all three stations. The chemical compositions of these common components are shown to the same within 95% statistical significance interval. Three factors, namely a fertilizer factor, which is highly enriched in NH4+ ion, a sea salt component and an arsenic factor are common in the Mediterranean and Black Sea aerosol but not observed at the Central Anatolia. Other factors found in the regions are specific for that region.

The Black Sea, with its oxic, suboxic and anoxic layers, provides a unique environment for studying how biological and geochemical processes affect the composition of particulate matter. The elemental composition of particles in the Black Sea is controlled by their origin and sources. Particles from rivers are dominated by aluminosilicate material that has compositions similar to the earth&rsquo / s crust. In general this material is relatively unreactive. Biological processes in the upper oxic and suboxic layers of the water column result in enrichments of elements which used as nutrients. Cu, Ba and Mo have been proposed as tracers for planktonic material and new production. Geochemical processes like manganese and iron recycling between oxidized and reduced forms, metal sulfide formation, and biogenic matter decomposition can have a large impact on the composition of particles in the suboxic and anoxic zones. The aim of this thesis was to study the composition of particles suspended in the water column of the Black Sea, in regional rivers draining into the Black Sea, and of particles deposited in these rivers and Black Sea sediments. The objectives were to determine the chemical composition and distribution of particles supplied by rivers and produced in the Black Sea, and compare with those particles buried in the sediments. The chemical distributions can help us to understand the biogeochemical processes taking place. The ultimate goal is to understand if there is a chemical signature that characterizes sediments deposited in anoxic basins that can be used to determine if ancient sedimentary rocks were deposited under such conditions. Water column filter samples were collected from the central western basin and along transects to the SW shelf regions during several research cruises of R/V Bilim and R/V Knorr in the Black Sea. Samples were taken by using both in situ large volume filtration systems and on deck vacuum filtration of discrete samples. River samples were collected by hand from the bank of four Turkish rivers and the Danube River. Sediment samples were obtained from 0 - 25 cm interval of a box core from the deep western basin. All samples were digested and analyzed by inductively coupled plasma - mass spectrometry and combination of atomic absorption (flame &amp / graphite furnace) instruments. The elements analyzed included Al, Ti, V, Cr, Mn, Fe, Ni, Co, Cu, Zn, Mo, Ag, Cd, Ba, Pb, and U. Great care was taken to avoid contamination and to obtain the highest level of precision and accuracy. The precision was typically about 5% for most elements. The accuracy, determined using standard reference materials, was also usually better than 5%. Another goal of this research was to determine the metal concentrations and best digestion methods using different types of filter materials. Blank filters were digested and analyzed and the analyses of various filter blanks are presented in the thesis. The analyses showed that the particulate matter data from Turkish Rivers were very similar to the composition of global average riverine particulate material and global average crust. The Danube River had elevated concentrations for some elements that were probably due to anthropogenic contamination. The Turkish river samples were closer to (but still higher than) the averages for the world&rsquo / s rivers but many elements in the Danube were much higher. These high values determined for major elements in the Danube samples strongly suggest considerable contamination of the Danube as compared to the Turkish Rivers. The Danube River samples were especially enriched in Pb, Zn, Ag, Cu, Cd, and Mn and slightly enriched with Cr and Ni. The first five elements, in particular, are well known indicators of pollution. The particulate matter in the water column of the Black Sea was influenced by lithogenic input from rivers, biological processes and geochemical processes. In order to examine the biogeochemical processes extensively, all the data were plotted as Metal/Al (Me/Al) ratios and compared with the ratios of the average crust and Turkish Rivers. Deviations were used to examine the anomalies due to biological and geochemical processes. In addition, the Al content of individual sample and the Me/Al ratio of crust or rivers were used to subtract the lithogenic component from the total composition. Enrichments due to biological processes were observed for Ba &gt / Fe &gt / Cr &gt / Mn &gt / Zn &gt / Ni &gt / Cu &gt / Mo &gt / V &gt / Co &gt / Cd &gt / U for the overall biogenic composition. Enrichments due to biology are most evident for Ba, Fe, Cr and Mn. This is a unique data set as there have been few previous analyses of biological enrichment for most of these elements. The results of particulate matter analyses showed that some elements including U, V, Cr, Ni, Cu, Co, Zn, Ba and Mo were enriched in the set of samples from the euphotic zone. Redox cycling in the suboxic zone was observed, as expected, for Mn and Fe, whose oxides play an important role in scavenging processes. The redox dependent processes in the suboxic &ndash / anoxic interface influence the vertical distribution of U, Ni, Co, Cu, Zn, Ba and possibly Mo, Cr and V. Elements influenced by sulfide formation in the anoxic layer are Fe, Cr, Ni, Co, Mo, and presumably Ag. The sediment data were also examined based on the same approaches. The elements Zn, Pb, U and Cd decreased with sediment depth over the top 5 cm suggesting that they were remobilized out of the sediments. In general the sediments from the Black Sea have Me/Al ratios very similar to local Turkish Rivers and average crust. There is no unique sediment signature (except possibly for Mo) indicating that these sediments were deposited under sulphidic conditions. This study does not support the hypothesis that the composition of ancient rocks can be used to characterize the environment of deposition.

À la période Archaïque, la colonisation grecque avait pour but l’expansion et l’exportation des coutumes sociales des diverses cités États à travers différentes régions. Bien que le sujet de la colonisation grecque soit abondamment basé sur des sources primaires biaisées, causant une confusion concernant l’établissement du lien entre une cité mère et ses colonies, il demeure néanmoins qu’une connexion entre la cité de Milet et les colonies de la Mer Noire est observée au sein des institutions religieuses instaurées sur ces territoires. Le culte d’Apollon fut prédominant tout au long des périodes Archaïque, Classique et Hellénistique de la Grèce antique. À l’époque de la colonisation par Milet, la cité avait pour divinité principale Apollon qui était également dieu de la colonisation et dieu de la navigation. Pour les milésiens, Apollon autorisait et sanctionnait le droit de coloniser et d’y instaurer de nouveaux cultes. Dans les colonies fondées le long de la côte de la Mer Noire, une influence claire du culte de cette divinité est discernable dans la tradition littéraire, ainsi que dans les registres archéologiques. Grâce à un catalogue raisonné, concernant seize colonies dites milésiennes situées autour de la Mer Noire, unissant toute l’information archéologique et littéraire pertinente relatif au culte d’Apollon, ce mémoire propose qu’une forte représentation de ce culte dans cette région est attribuable à son instauration par les Milésiens dans l’espoir que les institutions religieuses des colonies reflètent celles de la cité mère. Il en découle qu’Apollon devint, par le fait même, la divinité principale de la majorité des colonies milésiennes de la Mer Noire. / Greek colonisation in the Archaic period had as its goal the expansion and the exportation of a city state’s social and religious customs into different regions. Although the subject of Greek colonisation is often vague, and based on erroneous, and generous primary sources, which can confound links between the colonies and their apparent mother city, a connection can nevertheless be established between the colonies in the Black Sea and the mother city of Miletus through the religious institutions that were installed upon colonisation. The cult of the god Apollo was prevalent throughout the ancient Greek world during the Archaic, Classical and Hellenistic periods. For the Archaic period colonizing Greek city state of Miletus, Apollo was patron deity, the god of colonisation, as well as the god of seafaring. For the Milesians, Apollo was the deity who sanctioned the right to set up new cults in new locations, as well as authorising the very act of establishing colonies. In the colonies founded by Miletus located along the coast of the Black Sea, there is a clear disposition towards the cult of Apollo in the literary tradition, as well as in the archaeological record. This thesis proposes, by means of a well-defined catalogue uniting all pertinent archaeological and literary information relating to the cult of Apollo in 16 colonies located around the Black Sea said to have been colonies of Miletus, that the reason for such a strong representation of the cult of Apollo in these colonies is a result of the Milesians installing the cult of their patron deity Apollo with the wish that the colonies’ religious institutions mirror that of the metropolis. The inventory demonstrates that Apollo was the patron deity of the majority of Miletus’s colonies in the Black Sea. This thesis will also propose that a proper study of religious trends found in city states and their supposed colonies can act as a methodology for identifying which colonies belonged to which mother city, as I propose that the patron deity in a city state will be the patron deity in their colony.

Classiquement étudié par différentes disciplines scientifiques, le domaine de l'eau est au cœur des préoccupations environnementales contemporaines. En Europe, l'évaluation et le suivi de l'état écologique des "masses d'eau" sont désormais exigés par la législation communautaire, la directive cadre sur l'eau (DCE - 2000/60/CE) fixant des objectifs pour leur préservation ou leur restauration le cas échéant. Dans ce contexte, des expériences d'utilisation de l'imagerie satellitaire en appui au suivi écologique des eaux se sont succédées en Europe, notamment pour les masses d'eau côtières et pour les grands lacs. Malgré cela, la précision spatiale de l'imagerie utilisée pour ce type de suivi ne permet pas l'observation fine de secteurs littoraux très proches de la côte ou de lacs avec une surface réduite (par ex. inférieure à 5 km²). Pour ces espaces aquatiques particuliers, pourtant très nombreux, l'utilisation de la télédétection satellitaire est moins sollicitée. Cette recherche doctorale a été réalisée sur une zone littorale réunissant plusieurs de ces espaces aquatiques peu investigués par la télédétection satellitaire. Situé à la frontière orientale de l'Europe et à distance égale du pôle nord et de la ligne de l'équateur, le delta du Danube, en tant qu'espace naturel remarquable, bénéficie de différents statuts de protection (réserve de biosphère, site RAMSAR, patrimoine mondial naturel de l'UNESCO). Ceux-ci s'expliquent en grande partie par la forte diversité d'espaces aquatiques aussi bien sur la plaine deltaïque que sur la zone côtière adjacente (bras de fleuve, chenaux, lacs, baies, golfes, marais, îles-barrières). Ce continuum hétérogène, constituant l'hydrosystème du delta du Danube, et son prolongement en mer côtière, sont l'objet principal de ce doctorat. La notion d'échelle occupe une place centrale dans notre démarche d'analyse puisque l'on est à l'intersection de deux grands systèmes (le bassin versant du Danube et la mer Noire) dont les étendues sont de deux ordres de grandeurs plus vastes que celle du delta ; la dimension temporelle est aussi fondamentale dans la mesure où les processus de morphogénèse et de remaniement (naturels et anthropiques) se font fortement ressentir et se traduisent par une mobilité importante des formes de relief ainsi que des éléments de l'hydrographie deltaïque. Au delà des évolutions sur le moyen et long terme, la variabilité spatio-temporelle contemporaine des eaux au pas de temps intra-annuel (saisonnier et intra-saisonnier), jusque-là peu étudiée, a également été appréhendée dans cette thèse. Par son côté exploratoire, la mise en place d'une chaîne de traitements d'images satellitaires adaptée à l'étude des eaux deltaïques représente, en soi, l'objectif méthodologique principal de ce doctorat. Dans cette voie, différents lots d'images ont été mobilisés : en fonction des fluctuations du niveau d'eau du Danube, nous avons retenu la période 2006-2009, étudiée à travers un total de 85 images satellitaires, dont 52 à moyenne résolution spatiale (MERIS) et 33 à haute résolution spatiale (ALOS AVNIR-2, SPOT HRVIR, Landsat TM et ETM+) ; à ce premier lot s'ajoute une soixantaine de prises de vue "historiques" couvrant la période comprise entre 1972 et 2005 (capteurs de la série Landsat MSS, TM et ETM+), ainsi que, pour la période plus récente, cinq images Landsat TM de 2010 et 2011. Trois procédés distincts mais complémentaires ont été mis en œuvre pour traiter cet ensemble hétérogène d'images. L'analyse intégrée des résultats obtenus avec des données hydrologiques et météo-océanographiques nous a permis d'apporter des nouveaux éléments de compréhension sur le fonctionnement actuel et passé du delta du Danube. / The Danube River and its contributors cross nineteen European countries before reaching the West coast of the Black Sea. In the context of the Black Sea drainage basin, the Danube River is the most important source of liquid and solid discharges. The fluvial-marine contact zone is quite large because Danube splits up itself into multiple distributaries across a wide deltaic plain (4,142 km²) shared among Romania and Ukraine. Vast areas of compact reedbeds usually surround the three hundred freshwater lakes of the delta. Many of these shallow lakes are connected to channels or canals providing turbid water from the Danube, while others depend on flood events to be supplied by the turbid waters coming from the river. Important seasonal growth of floating and submerged macrophytes also occurs in the majority of the lakes. Thus, Danube Delta presents a complex hydrosystem which has been greatly modified since the first navigation works in the nineteenth century. Since the beginning of the nineties, the Danube Delta became a Biosphere Reserve (MAB-UNESCO), a RAMSAR site and was included on the list of the World Natural Heritage (UNESCO). Analyzing spatial patterns in complex environments, like Danube Delta and its coastal zone, requires non traditional approaches. Remote sensing multi-sensor techniques offer reliable advantages to observe and understand intricate processes operating on different space-time scales and especially in large areas with difficult and sometimes restricted access (e.g. Biosphere Reserve core areas). The main methodological objective of this thesis was to create a procedure for processing heterogeneous optical satellite images. By studying the Danube Delta area (hydrosystems principally) through different space-time scales, we worked with several types of high and moderate spatial resolution images. Based on Danube water levels, we analyzed 85 satellite images from the period 2006-2009 (52 medium resolution images - MERIS and 33 high resolution images - ALOS AVNIR-2, SPOT HVIR, Landsat TM / ETM+). This main satellite data set was completed with more than sixty "historical" images (1972-2005) acquired with the Landsat sensors (MSS, TM and ETM+). Three distinct, but complementary, approaches were used to process the satellite images. The integrated analysis of the satellite results with hydrological and meteo-oceanographical data series enabled us to bring new elements of explanation about the past and present dynamics of Danube Delta.

The photographic series Ideal Cities that I started in 2011 is inspired by the conflict between my idea of the “west” and my evolving experience in the United States. What struck me was the popularity of what I see as model experience – a spatial experience controlled by the Spectacle. In the terms of the Situationist International and its most prominent figure Guy Debord, the Spectacle is the collapse of reality into the streams of images, products and activities sanctioned by centralized monopolist business or state bureaucracy. Thus, personal experience is replaced with preconceived notions, which control the way people perceive and understand their surroundings.

No description available.

The thesis deals with phylogeny, taxonomy and nomenclature of selected groups of the lichen genus Caloplaca. Particularly, the C. cerina group was closely investigated using molecular methods (ITS sequences), morphology and chemistry, based on material from Europe, and to some extent also from North America and western Asia. This approach resulted in the description of three new species (C. sterilis, C. subalpina, C. thracopontica), and detected an unexpected richness of lineages. Nomenclature, taxonomy, morphology and ecology of C. aurantia and C. flavescens from the C. aurantia group were studied in detail, including selection of the neotype of the former species. Their distribution was reviewed for the territory of the Czech Republic. Poorly known taxon C. aurantiomurorum from Algeria was lectotypified and synonymized with C. aurantia. Apart from the two groups, C. phlogina and C. scythica, differing partly in thallus colour and distinctly in distribution, were examined using both molecular (ITS sequences) and phenotypic data and found to be conspecific.

This thesis, structured in two parts, addresses a series of problems of relevance in the field of Spatial Geodesy. The first part delves into the application of satellite gravity data to enhance our understanding of water transport dynamics. Here, we present two significant contributions. Both are based on satellite gravity data but stem from different mission concepts with distinct objectives: time-variable gravity monitoring and high-resolution, accurate static geoid modelling. First, the fundamental notions about gravity are introduced and a brief summary is made of the different gravity satellite missions throughout history, with emphasis on the GRACE/GRACE-FO and GOCE missions, whose data are the basis of this work. The first application focuses on estimating water transport and geostrophic circulation in the Southern Ocean by leveraging a GOCE geoid and altimetry data. The Volume Transport across the Antartic Circumpolar Current is analyzed and the resulsts are validated validated using the in-situ data collected during the multiple campaigns in the DP. The second application uses time-variable gravity data from the GRACE and GRACE-FO missions to estimate the water cycle in the Mediterranean and Black Sea system, a critical region for regional climate and global ocean circulation. The analysis delves into the analysis of the different components of the hydrological cycle within this region, including the water flow across the Gibraltar Strait, examining their seasonal variations, climatic patterns, and their connection with the North Atlantic Oscillation Index. The second part of the thesis is more focused on data analysis, with the objective of developing mathematical methods to estimate the cross correlation function between two time series that are both unevenly spaced spaced (the sampling is not uniform over time) and observed at unequal time scales (the set of time points for the first series is not identical to the set of time points of the second series). Such time series are frequently encountered in geodetic surveys, especially when combining data from different sources. The estimation of the the cross correlation function for these time series presents unique challenges and requires the adaptation of traditional analysis methods designed for evenly spaced and synchronized time series. The two main contributions in this context are: (i) the study of the asymptotic properties of the Guassian Kernel estimator, that is the recommended estimator for the cross correlation function when the two time series are observed at unequal time scales; (ii) an extension of the stationary bootstrap that allows to construct bootstrap-based confidence intervals for the cross correlation function for unevenly spaced time series not sampled on identical time points.