Niche conservatism in non-native birds in Europe: niche unfilling rather than niche expansion

Aim Niche conservatism, or the extent to which niches are conserved across space and time, is of special concern for the study of non-native species as it underlies predictions of invasion risk. Based on the occurrence of 28 non-native birds in Europe, we assess to what extent Grinnellian realized niches are conserved during invasion, formulate hypotheses to explain the variation in observed niche changes and test how well species distribution models can predict non-native bird occurrence in Europe. Location Europe. Methods To quantify niche changes, a recent method that applies kernel smoothers to densities of species occurrence in a gridded environmental space was used. This corrects for differences in the availability of environments between study areas and allows discrimination between 'niche expansion' into environments new to the species and 'niche unfilling', whereby the species only partially fills its niche in the invaded range. Predictions of non-native bird distribution in Europe were generated using several distribution modelling techniques. Results Niche overlap between native and non-native bird populations is low, but niche changes are smaller for species having a higher propagule pressure and that were introduced longer ago. Non-native birds in Europe occupy a subset of the environments they inhabit in their native ranges. Niche expansion into novel environments is rare for most species, allowing species distribution models to accurately predict invasion risk. Main conclusions Because of the recent nature of most bird introductions, species occupy only part of the suitable environments available in the invaded range. This signals that apart from purely ecological factors, patterns of niche conservatism may also be contingent on population-specific historical factors. These results also suggest that many claims of niche differences may be due to a partial filling of the native niche in the invaded range and thus do not represent true niche changes.

Triassic stratigraphic evolution of the Arabian-Greater India embayment of the southern Tethys margin

An exceptional, tectonically remarkably unaffected, nearly 200 m-thick continuous section of hemipelagic and turbiditic sediments, covering most of the Triassic is described from the Batain Complex of north-eastern Oman. According to conodont and radiolarian data the sequence spans the late Scythian to the early Norian, a time period of nearly 30 M. Coupled with a high resolution stratigraphy, the lithostratigraphy, sedimentology, as well as sequence and isotope stratigraphy of the section are documented. For the Triassic of the Batain Plain we propose the new name Sal Formation, which replaces the formerly used Matbat Formation, and subdivide it into three new members. The Sal Formation was deposited on the proximal continental margin of northeastern Arabia and records various depositional environments. The lower member is interpreted as the distal part of a homoclinal ramp which evolves to a distally steepened ramp during time of deposition of the middle member. The upper member displays a toe of slope position which is indicated by an increase of proximal turbidites. These sediments form part of a segment of the Neo-Tethyan embayment between Arabia and India. The stratigraphic analysis indicates highly varying sedimentation rates from a minimum of 2 m/M gamma around the Anisian/Ladinian boundary up to 15 m/M gamma during the Lower and Upper Triassic. Sequence-stratigraphically, the Sal section is subdivided into six third order cycles which are biochronologically well integrated into the global Triassic cycle chart. The mixed siliciclastic-calcareous upper member of the Sal Formation typically shows highstand related carbonate shedding. It is, therefore, an important test case for sequence-stratigraphic controlled carbonate export to mixed basin fills. The well developed sequence stratigraphic cycles are mirrored in the isotope patterns. Additionally, the carbon and oxygen isotope data from the Sal Formation record the same chemostratigraphic marker at the Spathian/Anisian boundary known from other Tethyan sections.

The borehole-fluid effect in electrical resistivity imaging

Fluid that fills boreholes in crosswell electrical resistivity investigations provides the necessary electrical contact between the electrodes and the rock formation but it is also the source of image artifacts in standard inversions that do not account for the effects of the boreholes. The image distortions can be severe for large resistivity contrasts between the rock formation and borehole fluid and for large borehole diameters. We have carried out 3D finite-element modeling using an unstructured-grid approach to quantify the magnitude of borehole effects for different resistivity contrasts, borehole diameters, and electrode configurations. Relatively common resistivity contrasts of 100:1 and borehole diameters of 10 and 20 cm yielded, for a bipole length of 5 m, apparent resistivity underestimates of approximately 12% and 32% when using AB-MN configurations and apparent resistivity overestimates of approximately 24% and 95% when using AM-BN configurations. Effects are generally more severe at shorter bipole spacings. We report the results obtained by either including or ignoring the boreholes in inversions of 3D field data from a test site in Switzerland, where approximately 10,000 crosswell resistivity-tomography measurements were made across six acquisition planes among four boreholes. Inversions of raw data that ignored the boreholes filled with low-resistivity fluid paradoxically produced high-resistivity artifacts around the boreholes. Including correction factors based on the modeling results fora ID model with and without the boreholes did not markedly improve the images. The only satisfactory approach was to use a 3D inversion code that explicitly incorporated the boreholes in the actual inversion. This new approach yielded an electrical resistivity image that was devoid of artifacts around the boreholes and that correlated well with coincident crosswell radar images.

Eretria - Nea Psara : eine klassizistische Stadtanlage über der antiken Polis

Résumé: Le présent ouvrage propose une histoire de l'Erétrie moderne, de la redécouverte du site antique au projet urbanistique de 1834 pour une ville nouvelle destinée à accueillir les réfugiés de l'île de Psara - anéantie en 1824 par les Ottomans - et au développement urbain d'Erétrie/Nea Psara au XIXe et au XXe siècles. Le nom d'Erétrie englobe trois couches historiques distinctes: la cité antique, la ville néoclassique, dessinée par l'architecte allemand Eduard Schaubert (1804-1860), et le village moderne, issu de son projet. Chacune de ces strates - vestiges antiques, tissu urbain néoclassique et constructions plus récentes - est perceptible au sein de cet ensemble urbain et se trouve en relation constante avec les autres. L'exposé des recherches archéologiques - depuis la redécouverte du site antique par Ciriaco de' Pizzicolli d'Ancona (Cyriaque d'Ancône) en 1436 déjà, puis de manière systématique par des voyageurs-archéologues dès le XIXe siècle - comble une lacune dans l'historiographie de la cité antique. Cette approche met également en lumière la relation étroite entre archéologie et urbanisme au XIXe siècle. Si l'exploration de la Grèce avait été jusqu'à son indépendance en 1827 essentiellement le fait des archéologues, des historiens et des philologues, après cette date, des géologues, des ingénieurs et des topographes travaillant pour le développement économique du jeune Etat se mirent également à parcourir le pays, le regard tourné non plus seulement vers l'Antiquité, mais aussi vers l'avenir. L'histoire de la redécouverte d'Erétrie permet ainsi d'éclairer divers aspects liés à la gestation de l'Etat grec. Le projet conçu en 1834 par Ecluard Schaubert de ville néoclassique superposée aux ruines de la cité antique d'Erétrie s'inscrit dans un réseau de créations de villes nouvelles et de modernisations de villes existantes par le nouvel Etat grec, qui cherchait à fonder sa légitimité et son identité, après la domination ottomane, sur les valeurs idéales (ou idéalisées) de l'Antiquité classique. Dans le projet de développement urbain d'Erétrie, la relation étroite entre archéologie et urbanisme et, par conséquent, la référence à l'Antiquité sont évidentes: Eduard Schaubert commença par tracer sur son plan toutes les ruines antiques, dressant ainsi l'état des connaissances archéologiques du site. Sur cette base, l'architecte conçut la ville néoclassique en y incluant les principales ruines, qui devaient servir de repères visuels et qui concrétisaient ainsi le lien idéologique de la monarchie absolue avec l'Antiquité. A Erétrie, deux perspectives principales reliaient le port à l'acropole et l'Ecole navale au théâtre antique. L'intégration de ruines antiques dans un projet urbanistique avait été réalisée par Stamatios Kleanthes et Eduard Schaubert en 1831-1832 dans le plan de l'Athènes moderne, avant que celle-ci n'ait été promue capitale de la Grèce. Les deux architectes ont ainsi anticipé le caractère idéal d'Athènes dans le processus de gestation de l'Etat grec. L'importance de ce plan et de celui qu'ifs ont établi sur le même modèle pour le Pirée a été reconnue par les historiens de l'urbanisme. En revanche, le plan d'Erétrie, qui suit pourtant les mêmes principes, n'a été que partiellement étudié. Cette monographie montre que le projet d'Erétrie était le plus abouti des trois, qui tous se caractérisent par un système de routes rayonnant depuis le siège du gouvernement (résidences royales à Athènes et au Pirée, mairie à Erétrie). Cet éventail de rues ou u patte d'oie» embrasse à Athènes l'acropole et au Pirée fa baie du port, alors qu'a Erétrie il est double, axé en raison de la topographie sur l'acropole et sur Pa baie du port. Cette double patte d'oie crée ainsi le lien idéologique avec l'Antiquité et témoigne, par son ouverture sur le port, de l'essor économique souhaité par le gouvernement. Le plan d'Erétrie représente de manière exemplaire l'urbanisme programmatique de la Grèce sous Othon ler (1832-1862). L'ouvrage s'intéresse ensuite à la réalisation du projet de Schaubert, dont la mise en oeuvre n'a pas répondu aux attentes du Gouvernement. Le faible développement d'Erétrie s'explique principalement par le surdimensionnement du projet, des finances publiques modestes, la malaria endémique et une politique économique inadaptée aux traditions commerciales des Psariotes. Les lenteurs dans la réalisation du projet et même des régressions au cours du XIXe siècle et au début du XXe siècle, puis l'urbanisation accélérée d'Erétrie à partir des années 1960, ont eu pour conséquence que les historiens de l'urbanisme et les urbanistes ont sous-estimé, voire ignoré la valeur historique de ce concept Cependant, l'exécution du projet néoclassique s'est poursuivie de manière continue et des références au plan de Schaubert peuvent être observées dans l'aménagement récent de la localité aujourd'hui encore. Ainsi, des arbres ont été plantés dans les années 1960 le long de l'enceinte urbaine antique, à l'emplacement où Schaubert avait prévu la création d'une promenade arborée. Au centre d'Erétrie, là où l'agora principale aurait dû être aménagée, une grande place publique servant au marché hebdomadaire a été créée. Dans le quartier oriental, une petite église dédiée à la Pan hagia Paravouniotissa a été construite en 2001 sur la parcelle où Schaubert en avait prévue une. D'importants éléments des projets de Schaubert, qui ne sont actuellement plus guère perceptibles à Athènes et au Pirée, le sont toujours à Erétrie. Les espaces verts, par exemple, occupent une place importante dans le domaine privé: malgré la densification du tissu urbain, des parcelles caractéristiques contiennent encore des maisons isolées d'un ou de deux niveaux côté rue, avec un grand jardin à l'arrière, séparé des parcelles voisines par un mur en pierre ou en brique crue. Erétrie mérite donc une reconnaissance plus considérable dans l'histoire de l'urbanisme, puisqu'elle contribue à faire mieux comprendre les projets de ses deux villes soeurs. L'étude du projet urbanistique est complétée par une approche typologique des constructions néoclassiques d'Erétrie qui souligne encore la valeur historique de cet ensemble. Comme la plupart des édifices sont, menacés de démolition, à l'exception d'un petit nombre d'entre eux qui bénéficient d'un bon entretien, un inventaire photographique des constructions d'Erétrie datant du XIXe et du début du XXe siècle a été constitué entre 1994 et 2005, complété par des photographies anciennes. Il en ressort que les formes et les techniques de construction sont représentatives de l'architecture privée à l'époque de la création de l'Etat. Enfin, le plan directeur d'Erétrie, réalisé en 1975-1976 par un séminaire du Département d'architecture de l'Ecole polytechnique fédérale de Zurich avec l'appui de l'Ecole suisse d'archéologie en Grèce, est publié ici intégralement pour la première fois. Le présent ouvrage rend ses lettres de noblesse à un ensemble urbain néoclassique, certes modeste, mais issu d'un projet urbanistique ambitieux, témoin significatif du programme politique du nouvel Etat grec. SUMMARY Translated by William Eisler This book gives an account of the history of modern Eretria. It encompasses the rediscovery of the ancient city, the 1834 urban plan for the new town designed to accommodate the refugees from the island of Psara - destroyed by the Ottomans in 1824 - and also the urban development of Eretria/Nea Psara in the 19th and 20th centuries. The name Eretria carries a rich heritage: the ancient city, the neoclassical town designed by the Germen architect Eduard Schaubert (1804-1860), and the modern village. These three distinct historical layers ancient ruins, neoclassical plan and more recent constructions - can be seen within this urban area and are interlinked with each other. The account of the archeological investigations fills a gap in the historiography of the ancient city. This started with the early rediscovery of the ancient site by Ciriaco de'Pizzicolli d'Ancona in 1436, and was followed by systematic research by travellers/ archeologists from the 19th century onward. Furthermore, this shows the close relationship between archeology and urbanism in the 19th century. The exploration of Greece prier te its independence in 1827 was mainly red by archeologists, historians and philologists. Subsequently, geologists, engineers and topographers working for the young state's economic development travelled across the country, with their attention focused not only on Antiquity but are on the future. The history of Eretria's rediscovery gives new insights on various aspects related to the development of the Greek state. In 1834, Eduard Schaubert's project, planning a neoclassical town built upon the ancient Eretria, took place alongside the development of other new cities and the modernization of existing ones du ring the Ottoman domination. By doing so, the new Greek state wanted to build its legitimacy and identity, based upon the ideal (or idealized) values of Classical Antiquity. In the urban development of Eretria, the close connection between archeology and urbanism, and the reference to Antiquity, are obvious. Eduard Schaubert began by tracing on his plan ail of the ancient ruins, thus showing the knowledge of the archeological site at that time. On this basis, the architect planned the neoclassical town, incorporating the principal ruins which were to serve as visual references embodying the ideological link between Antiquity and King Otto's absolute monarchy. In Eretria, two principal visual axes linked the port to the acropolis and the Naval School to the ancient theatre. The integration of ancient ruins in an urban project had already been achieved by Stamatios Kleanthes and Eduard Schaubert in 1831-1832 in their plan for modern Athens, before it became the capital of Greece. The two architects had therefore anticipated the ideal character of Athens at the beginning of the Greek state. The importance of this plan and that of Piraeus (designed along the same model) has long been recognized by urban historians. By contrast, the plan of Eretria based open the same principles has been only partly studied. This book explains clearly that the Eretria project was the most elaborate. The three cities are characterized by a system of roads radiating from the seat of government (the royal residences in Athens and Piraeus, the town hall in Eretria). This fan-like arrangement of streets includes the Acropolis in Athens and the harbour in Piraeus, whereas in Eretria it is twofold, orientated towards the acropolis and the harbour on account of the topography. This double fan-like arrangement shows the ideological link with Antiquity and, with its opening onto the harbour, the government's desire for economic development. The plan of Eretria is a typical ex- ample of the programmatic urbanism of Greece under Otto I (1832-1862). The book discusses the completion of Schaubert's project, which was not fully carried out as expected by the government. The poor development of Eretria can be explained primarily by the excessive scale of the project, the modest public finances, the endemic malaria and an economic policy unsuitable to the commercial traditions of the Psariotes. Delays, even regressions in the implementation of the project in the course of the 19th and the beginning of the 20th centuries, followed by the growing urbanization of Eretria starting in the 1960's, led urban historians and town planners to underestimate or even to ignore the historical value of this concept. Nevertheless, the neoclassical project was carried out steadfastly, and references to the Schaubert plan can still be seen in the modern layout of the town. Trees were planted in the 1960's all along the circumference of the ancient city, where Schaubert had planned a tree-lined promenade. A big public square serving as a weekly market place was created in the centre of Eretria, where the principal agora had been originally planned. In 2001 a small church dedicated to the Panhagia Paravouniotissa was built on a plot of land in the eastern district, where this had been intended by Schaubert. Important elements of Schaubert's projects, which are barely perceptible in modern-day Athens and Piraeus, remain visible in Eretria. Green areas, for example, occupy a significant place within the private properties. In spite of the urban densification, characteristic plots still include isolated houses of one or two stories facing the street, with large gardens in the rear, separated from neighbours by stone or mudbrick walls. Eretria therefore deserves a more prominent position in the history of urbanism, as it contributes to a better understanding of ifs two sister cities. The study of the urban project is enriched by a typological approach to the neoclassical constructions of Eretria, underlining once again the historical value of this heritage. Since only a small number of the buildings have benefited from good maintenance and the greater part is threatened with demolition, a photographic inventory of the constructions of Eretria dating from the 19tIt and early 20th centuries was produced between 1994 and 2005, supplemented by old photographs. This documentation clearly shows that the forms and techniques of construction are characteristic of private architecture at the beginning of modern Greece. Finally, the master plan of Eretria drafted in 1975-1976 by a seminar of the Department of Architecture of the Swiss Federal Institute of Technology, Zurich, with the support of the Swiss School of Archeology in Greece, is published here in full for the first time. This book gives credit to a neoclassical urban heritage which, although modest in scale, derives from an ambitious project that embodies the political programme of the new Greek state. ΠΕΡΙΛΗΨΗ Μετάβραση Ελενή Δημητρακοπούλου Η παρούσα εργασία προτείνει μια. ιστορία της σύγχρονης πόλης της Ερέτριας, ξεκινώντας από την αποκάλύψη του αρχαιολογικού χώρου, περνώντας από την σύνταξη, το 1834, του ρυμοτομικού σχεδίου για μια νέα. πόλη που σκοπό είχε να υποδεχθεί τούς πρόσφυγες από τα Ψαρά. - που καταστράφηκαν ολοσχερώς το 1824 από τούς Οθωμανούς - και εξετάζοντας τέλος την πολεοδομική εξέλιξη της Ερέτριας/Νέων Ψαρών κατά τον 19° και τον 20° αι. Πίσω από το όνομα της Ερέτριας κρύβονται τρία διαφορετικά. ιστορικά στρώματα,: η αρχαία πόλη, η νεοκλασική πόλη πού σχεδιάστηκε από τον γερμανό αρχιτε κτονα "Εντοναρντ Σάουμπερτ (1804-1860) και η σύγχρονη πόλη που κτίστηκε πάνω στά. σχέδια του τελευταίού. Κάθε ένα από αυτά τα στρώματα - αρχαία κατάλοιπα. νεοκλασικός πολεοδομικός ιστός και νεώτερα κτίσματα - γίνεται αντιληπτό στο πλαίσιο αυτού του πολεοδομικού συνόλου και βρίσκεται σε άμεση σχέση με τα άλλα δύο. Ηπαρονσίαση των αρχαιολογικών ερευνών, που ξεκινούν το 1436 με την αποκάλυψη τον αρχαιολογικού χώρού από τον Ciriaco de' Pizzicolli d'Ancona (Κυριάκος ο Αγκωνίτης) και συνεχίζονται συστηματικά. από περιηγητές_αρχαιολόγούς κατά το 19° αι., καλύπτει ένα κενό στην ιστοριογραφία της έρεύνας της αρχαίας πύλης. Η προσέγγιση αυτή φωτίζει επίσης τη στενή σχέσημεταξύαρχαιολογίας και πολεοδομίας κατά τον 190 αι. Αν η εξερεύνηση της Ελλάδος, ως την ανεξαρτησία της το 1827, ήταν έργο κνρϊως αρχαιολόγων, ιστορικών και φιλολόγων, μετά από αυτήν την χρονολογία., γεωλόγοι, μηχανικοί και τοπογράφοι που εργάζονταν για την οικονομική ανάπτυξη τον νεοσύστατου Ελληνικού Κράτούς, άρχισαν επίσης να περιτρέχονν όλη την χώρα., με το βλέμμα. στραμμένο όχι μόνο προς την Αρχαιότητα, αλλά και προς το μέλλον. Η ιστορία της αποκάλυψης της Ερέτριας φωτίζει έτσι και διάφορες όψεις που συνδέονται με την γένεση του Ελληνικού Κράτους. Το 1834, υ 'Εντοναρντ Σάουμπερτ εκπόνησε το σχέδιο μιας νεοκλασικής πόλης που Θα επικαθόταν στα; ερείπια. της αρχαίας Ερέτριας?το έργο εντάσσεται στο δίκτυο δημιουργίας νέων πόλεων και εκσυγχρονισμού των υπαρχυυσών από το νεοσύστατο Ελληνικό Κράτος. το οποίο, μετά την Οθωμανική κυριαρχία, επεδίωκε να Θεμελιώσει την νομιμότητα και την ταυτότητά του πάνω στις ιδανικές ή εξιδανικευμένες αξίες της κλασικής αρχαιότητας. Στο σχέδιο της πολεοδομικής ανάπτυξης της Ερέτριας, η στενή σχέση μεταξύ αρχαιολογίας και πολεοδομίας και, κατ επέκταση. οι σαφείς αναφορές στην Αρχαιότητα. είναι εμφανείς: ο Εντοναρντ Σάουμπερτ άρχισε σχεδιάζοντας στο τοπογραφικό τον όλα τα αρχαία. ερείπια, καταγράφοντας έτσι τις τότε αρχαιολογικές γνώσεις για, το χώρο. Σε αυτή τη βάση, ο αρχιτέκτονας συνέλαβε την νεοκλασική πόλη εντάσσοντας σε αυτήν τα κυριότερα αρχαία μνημεία, τα οποία χρησίμευαν ως οπτικά σημεία αναφοράς, ενώ συγχρόνως υλοποιούσαν την ιδεολογική σχέση της απόλύτης μοναρχίας με την Αρχαιότητα. Στην Ερέτρια, δυο βασικοί άξονες συνέδεαν το λιμάνι με την Ακρόπολη και τη Ναυτική Σχολή με το Αρχαίο Θέατρο. Η ένταξη αρχαίων ερειπίων σε ένα πολεοδομικό σχέδιο είχε ήδη πραγματοποιηθεί από τούς Σταμάτιο Κλεάνθη και'Εντουαρντ Σάουμπερτ στα 1831-1832, στον σχεδιασμό της νέας Αθήνας, πριν αυτή ανακηρυχθεί σε πρωτεύουσα. της Ελλάδος. Οι δυο αρχιτέκτονες προεξόφλησαν έτσι τον συμβολικό χαρακτήρα της Αθήνας στην διαδικασία. γένεσης του Ελληνικού Κράτούς, Η σημασία αυτού τον σχεδίου καθώς και εκείνου που συνέταξαν, πάνω στο ίδιο πνεύμα, για τον Πειραιά έχει αναγνωριστεί από τους σύγχρονούς πολεοδόμους. Αντίθετα, το σχέδιο της Ερέτριας, παρ όλο που ακολούθεί τις ίδιες αρχές, μελετήθηκε πολύ λίγο. Η παρούσα μονογραφία δείχνει ότι το σχέδιο της Ερέτριας ήταν το πιο ολοκληρωμένο από τα τρία. Βασικό χαρακτηριστικό των σχεδίων αυτών είναι ένα σύστημα οδών που αναπτύσσονται ακτινωτά από το κέντρο εξουσίας (βασιλική κατοικία στην Αθήνα και τον Πειραιά, δημαρχείο στην Ερέτρια). Αυτή η ακτινωτή διάταξη των οδών συμπεριλαμβάνει στην Αθήνα την Ακρόπολη και στον Πειραιά το λιμάνι, ενώ στην Ερέτρια είναι αμφίροπη, προσανατολισμένη, λόγω της τοπογραφίας, προς την ακρόπολη αλλά και προς τον όρμο του λιμανιού. Αυτή η διπλή ακτινωτή διάταξη από τη μια δημιούργεί τον ιδεολογικό δεσμό ιιε την Αρχαιότητα, ενώ από την άλλη τονίζει, με το άνοιγμά της προς το λιμάνι, την οικονομική άνθηση της πόλης που επιθυμούσε η κεντρική εξουσία. Τα σχέδιο της Ερέτριας αποτελεί αντιπροσωπευτικό δείγμα της προγραμματικής πολεοδομίας της Ελλάδος κατά τα, χρόνια της Βασιλείας του "Οθωνος (1832-1862). Η υλοποίηση του σχεδίου του Σάουμπερτ δεν ανταποκρίθηκε στις προσδοκίες της κυβέρνησης. Η μικρή ανάπτύξη της Ερέτριας οφείλεται κυρίως στούς ανεδαφικούς, μεγαλεπί βολονς στόχους του σχεδίού, στα μέτρια δημόσια οικονομικά, στην ενδημική ελονοσία λόγω των υφισταμένων ελών καθώς και σε μια, οικονομική πολιτική που ήταν ξένη στις εμπορικές παραδόσεις των Ψαριανών. Οι αργοί ρυθμοί της πραγματοποίησης του σχεδίού και μάλιστα κάποιες περικοπές τον κατά τη διάρκεια τον 19°ν και στις αρχές του 2θ αι., και στη συνέχεια η ταχεία πολεοδομική εξέλιξη της Ερέτριας από τη δεκαετία του 1960, είχαν σαν συνέπεια να υποτιμηθεί ή κατ να αγνοηθεί η ιστορική αξία του πολεοδομικού σχεδίου από τους ιστορικούς της πολεοδομίας. Ωστόσο, η εκτέλεση τον νεοκλασικού σχεδίου ακολουθήθηκε με συνέπεια, ενώ αναφορές στο σχέδιο του Σάουμπερτ μπορούν να παρατηρηθούν, ακόμα. και σήμερα. στις νεώτερες διευθετήσεις τον χώρου. Ετσι, στη δεκαετία του 1960, κατά μήκος του αρχαίού τείχούς της πόλης φυτεύθηκαν δέντρα, στη Θέση όπού ο Σάουμπερτ είχε προβλέψει τη δημιουργία ενός δεντροφυτεμένου περιπάτου. Στο κέντρο της Ερέτριας, εκεί όπου Θα έπρεπε να διαμορφωθεί η κύρια αγορά της πόλης, δημιουργήθηκε μια μεγάλη δημόσια πλατεία όπου γίνεται η εβδομαδιαία λαϊκή αγορά. Στην ανατολική συνοικία, χτίστηκε, το 2001, μια μικρή εκκλησία αφιερωμένη στην Παναγία, την Παραβοννιώτισσα, στο οικόπεδο όπου ο Σάουμπερτ είχε προβλέψει μια εκκλησία. Σημαντικά στοιχεία των σχεδίων του Σάουμπερτ, που δεν γίνονται πια καθόλου αντιληπτά στην ΑΘήνα και στον Πειραιά, μπορούν να παρατηρηθούν στην Ερέτρια. Το πράσινο, για παράδειγμα, καταλαμβάνει σημαντική Θέση τον ιδιωτικού χώρου: παρά την πύκνωση τον πολεοδομικού ιστού, χαρακτηριστικά είναι τα οικόπεδα που περιέχούν ακόμα μεμονωμένα σπίτια, μονώροφα ή διώροφα, επί προσώπου οδού, με ένα μεγάλο κήπο στο πίσω μέρος, που χωρίζονται από τα, γειτονικά οικόπεδα με ένα μαντρότοιχο πέτρινο ή από ωμές πλίνθους. Η Ερέτρια οφείλει λοιπόν να λάβει τη Θέση που της αξίζει στην ιστορία της Νεοελληνικής πολεοδομίας, εφόσον συμβάλλει στην καλύτερη κατανόηση των σχεδίων των δυο αυτών αδελφών πόλεων. Η μελέτη τον πολεοδομικού σχεδίού συμπληρώνεται από μια τυπολογική προσέγγιση των νεοκλασικών κτηρίων της Ερέτριας, η οποία υπογραμμίζει ακόμα περισσότερο την ιστορική αξία του συνόλου αυτού. Καθώς τα περισσότερα κτήρια απειλούνται με κατεδάφιση, με εξαίρεση λίγα από αυτά που είχαν την τύχη να συντηρούνται σωστά, μεταξύ 1994 και 2005, καταρτίστηκε ένα φωτογραφικό αρχείο των κτιρίων της Ερέτριας που χρονολογούνται στο 19° και στις αρχές τον 200υ αι., συμπληρωμένο και από παλιές φωτογραφίες. Από αυτό προκύπτει ότι οι μορφές κατ οι τεχνικές δομήσεως είναι αντιπροσωπευτικές της ιδιωτικής αρχιτεκτονικής κατά την εποχή της σύστασης τον Ελληνικού Κράτους. Τέλος, το γενικό ρυθμιστικό σχέδιο της Ερέτριας, που εκπονήθηκε στα 1975-1976 από μελετητική ομάδατης σχολής Αρχιτεκτόνων του Ομοσπονδιακού Πολυτεχνείου της Ζυρίχης, με την υποστήριξη της Ελβετικής Αρχαιολογικής Σχολής στην Ελλάδα., δημοσιεύεται εδώ για πρώτη φορά στην πλήρη μορφή του. Η παρούσα εργασία, αφορά ένα νεοκλασικό πολεοδομικό σύνολο, ταπεινό ίσως, αλλά αποτέλεσμα ενός φιλόδοξου πολεοδομικού σχεδιασμού, ο οποίος αποτελεί σημαντικό μάρτυρα του πολιτικού προγράμματος τον νεοσύστατού Ελληνικού Κράτους.

Sodium sensing in neurons with a dendrimer-based nanoprobe.

Ion imaging is a powerful methodology to assess fundamental biological processes in live cells. The limited efficiency of some ion-sensing probes and their fast leakage from cells are important restrictions to this approach. In this study, we present a novel strategy based on the use of dendrimer nanoparticles to obtain better intracellular retention of fluorescent probes and perform prolonged fluorescence imaging of intracellular ion dynamics. A new sodium-sensitive nanoprobe was generated by encapsulating a sodium dye in a PAMAM dendrimer nanocontainer. This nanoprobe is very stable and has high sodium sensitivity and selectivity. When loaded in neurons in live brain tissue, it homogenously fills the entire cell volume, including small processes, and stays for long durations, with no detectable alterations of cell functional properties. We demonstrate the suitability of this new sodium nanosensor for monitoring physiological sodium responses such as those occurring during neuronal activity.

Reorganization of a deeply incised drainage: role of deformation, sedimentation and groundwater flow

Deeply incised drainage networks are thought to be robust and not easily modified, and are commonly used as passive markers of horizontal strain. Yet, reorganizations (rearrangements) appear in the geologic record. We provide field evidence of the reorganization of a Miocene drainage network in response to strike-slip and vertical displacements in Guatemala. The drainage was deeply incised into a 50-km-wide orogen located along the North America-Caribbean plate boundary. It rearranged twice, first during the Late Miocene in response to transpressional uplift along the Polochic fault, and again in the Quaternary in response to transtensional uplift along secondary faults. The pattern of reorganization resembles that produced by the tectonic defeat of rivers that cross growing tectonic structures. Compilation of remote sensing data, field mapping, sediment provenance study, grain-size analysis and Ar(40)/Ar(39) dating from paleovalleys and their fill reveals that the classic mechanisms of river diversion, such as river avulsion over bedrock, or capture driven by surface runoff, are not sufficient to produce the observed diversions. The sites of diversion coincide spatially with limestone belts and reactivated fault zones, suggesting that solution-triggered or deformation-triggered permeability have helped breaching of interfluves. The diversions are also related temporally and spatially to the accumulation of sediment fills in the valleys, upstream of the rising structures. We infer that the breaching of the interfluves was achieved by headward erosion along tributaries fed by groundwater flow tracking from the valleys soon to be captured. Fault zones and limestone belts provided the pathways, and the aquifers occupying the valley fills provided the head pressure that enhanced groundwater circulation. The defeat of rivers crossing the rising structures results essentially from the tectonically enhanced activation of groundwater flow between catchments.

Tax simulation in the SHP

This paper describes a simulation package designed to estimate the annual income taxes paid by respondents of the Swiss Household Panel (SHP). In Switzerland, the 26 cantons have their own tax system. Additionally, tax levels vary between the over 2000 municipalities and over time. The simulation package takes account of this complexity by building on existing tables on tax levels which are provided by the Swiss Federal Tax Administration Office. Because these are limited to a few types of households and only 812 municipalities, they have to be extended to cover all households and municipalities. A further drawback of these tables is that they neglect several deductions. The tax simulation package fills this gap by taking additionally account of deductions for children, double-earner couples, third pillar and support for dependent persons according to cantonal legislation. The resulting variable on direct taxes not only serves to calculate household income net of taxes, but can also be a variable for analysis by its own account.

Rate and processes of river network rearrangement during incipient faulting: The case of the Cahabon river, Guatemala

Deeply incised river networks are generally regarded as robust features that are not easily modified by erosion or tectonics. Although the reorganization of deeply incised drainage systems has been documented, the corresponding importance with regard to the overall landscape evolution of mountain ranges and the factors that permit such reorganizations are poorly understood. To address this problem, we have explored the rapid drainage reorganization that affected the Cahabon River in Guatemala during the Quaternary. Sediment-provenance analysis, field mapping, and electrical resistivity tomography (ERT) imaging are used to reconstruct the geometry of the valley before the river was captured. Dating of the abandoned valley sediments by the Be-10-Al-26 burial method and geomagnetic polarity analysis allow us to determine the age of the capture events and then to quantify several processes, such as the rate of tectonic deformation of the paleovalley, the rate of propagation of post-capture drainage reversal, and the rate at which canyons that formed at the capture sites have propagated along the paleovalley. Transtensional faulting started 1 to 3 million years ago, produced ground tilting and ground faulting along the Cahabon River, and thus generated differential uplift rate of 0.3 +/- 0.1 up to 0.7 +/- 0.4 mm . y(-1) along the river's course. The river responded to faulting by incising the areas of relative uplift and depositing a few tens of meters of sediment above the areas of relative subsidence. Then, the river experienced two captures and one avulsion between 700 ky and 100 ky. The captures breached high-standing ridges that separate the Cahabon River from its captors. Captures occurred at specific points where ridges are made permeable by fault damage zones and/or soluble rocks. Groundwater flow from the Cahabon River down to its captors likely increased the erosive power of the captors thus promoting focused erosion of the ridges. Valley-fill formation and capture occurred in close temporal succession, suggesting a genetic link between the two. We suggest that the aquifers accumulated within the valley-fills, increased the head along the subterraneous system connecting the Cahabon River to its captors, and promoted their development. Upon capture, the breached valley experienced widespread drainage reversal toward the capture sites. We attribute the generalized reversal to combined effects of groundwater sapping in the valley-fill, axial drainage obstruction by lateral fans, and tectonic tilting. Drainage reversal increased the size of the captured areas by a factor of 4 to 6. At the capture sites, 500 m deep canyons have been incised into the bedrock and are propagating upstream at a rate of 3 to 11 mm . y(-1) deepening at a rate of 0.7 to 1 5 mm . y(-1). At this rate, 1 to 2 million years will be necessary for headward erosion to completely erase the topographic expression of the paleovalley. It is concluded that the rapid reorganization of this drainage system was made possible by the way the river adjusted to the new tectonic strain field, which involved transient sedimentation along the river's course. If the river had escaped its early reorganization and had been given the time necessary to reach a new dynamic equilibrium, then the transient conditions that promoted capture would have vanished and its vulnerability to capture would have been strongly reduced.

Lower Triassic bryozoan beds from Ellesmere Island, High Arctic, Canada

In the Sverdrup Basin (Canadian Arctic), the Lower Triassic Blind Fiord Formation, comprising siltstone and shale, overlies various Middle to Late Permian (post-Wordian) sedimentary units. This formation is subdivided into three members: the Confederation Point, Smith Creek and Svartfjeld members of, respectively, Griesbachian-Dienerian, Smithian-Spathian and Spathian ages. Lower Triassic bryozoan beds are known from many sections of Ellesmere Island, but have never been studied in detail. During the Early Triassic biotic recovery interval, immediately following the Permian/Triassic extinction event, only one new bryozoan genus evolved in the Boreal region: Arcticopora. The first lower Triassic bryozoan bed appears in the upper part of the Confederation Point Member, and is dated as late Dienerian. Succeeding bryozoan levels occur in the upper Smith Creek Member, and are late Smithian-early Spathian in age. Bryozoan beds occupy a similar stratigraphic position in Spitsbergen. There, they occur scattered in silt to coarse sandstone beds, but also in bryozoan-dominated packstone beds resembling the packstone units in the uppermost part of the Confederation Point Member of Ellesmere Island. Previously, bryozoan-rich beds of Triassic age have not been reported, and the present work fills an important time gap in the bryozoan carbonate database

Evolution and sedimentology of a channel fill in the sandy braided South Saskatchewan River and its comparison to the deposits of an adjacent compound bar

The depositional stratigraphy of within-channel deposits in sandy braided rivers is dominated by a variety of barforms (both singular `unit' bars and complex `compound' bars), as well as the infill of individual channels (herein termed `channel fills'). The deposits of bars and channel fills define the key components of facies models for braided rivers and their within-channel heterogeneity, knowledge of which is important for reservoir characterization. However, few studies have sought to address the question of whether the deposits of bars and channel fills can be readily differentiated from each other. This paper presents the first quantitative study to achieve this aim, using aerial images of an evolving modern sandy braided river and geophysical imaging of its subsurface deposits. Aerial photographs taken between 2000 and 2004 document the abandonment and fill of a 1 3 km long, 80 m wide anabranch channel in the sandy braided South Saskatchewan River, Canada. Upstream river regulation traps the majority of very fine sediment and there is little clay (<1%) in the bed sediments. Channel abandonment was initiated by a series of unit bars that stalled and progressively blocked the anabranch entrance, together with dune deposition and stacking at the anabranch entrance and exit. Complete channel abandonment and subsequent fill of up to 3 m of sediment took approximately two years. Thirteen kilometres of ground-penetrating radar surveys, coupled with 18 cores, were obtained over the channel fill and an adjacent 750 m long, 400 m wide, compound bar, enabling a quantitative analysis of the channel and bar deposits. Results show that, in terms of grain-size trends, facies proportions and scale of deposits, there are only subtle differences between the channel fill and bar deposits which, therefore, renders them indistinguishable. Thus, it may be inappropriate to assign different geometric and sedimentological attributes to channel fill and bar facies in object-based models of sandy braided river alluvial architecture.

Genome sequence of the Drosophila melanogaster male-killing Spiroplasma strain MSRO endosymbiont.

Spiroplasmas are helical and motile members of a cell wall-less eubacterial group called Mollicutes. Although all spiroplasmas are associated with arthropods, they exhibit great diversity with respect to both their modes of transmission and their effects on their hosts; ranging from horizontally transmitted pathogens and commensals to endosymbionts that are transmitted transovarially (i.e., from mother to offspring). Here we provide the first genome sequence, along with proteomic validation, of an endosymbiotic inherited Spiroplasma bacterium, the Spiroplasma poulsonii MSRO strain harbored by Drosophila melanogaster. Comparison of the genome content of S. poulsonii with that of horizontally transmitted spiroplasmas indicates that S. poulsonii has lost many metabolic pathways and transporters, demonstrating a high level of interdependence with its insect host. Consistent with genome analysis, experimental studies showed that S. poulsonii metabolizes glucose but not trehalose. Notably, trehalose is more abundant than glucose in Drosophila hemolymph, and the inability to metabolize trehalose may prevent S. poulsonii from overproliferating. Our study identifies putative virulence genes, notably, those for a chitinase, the H2O2-producing glycerol-3-phosphate oxidase, and enzymes involved in the synthesis of the eukaryote-toxic lipid cardiolipin. S. poulsonii also expresses on the cell membrane one functional adhesion-related protein and two divergent spiralin proteins that have been implicated in insect cell invasion in other spiroplasmas. These lipoproteins may be involved in the colonization of the Drosophila germ line, ensuring S. poulsonii vertical transmission. The S. poulsonii genome is a valuable resource to explore the mechanisms of male killing and symbiont-mediated protection, two cardinal features of many facultative endosymbionts. IMPORTANCE: Most insect species, including important disease vectors and crop pests, harbor vertically transmitted endosymbiotic bacteria. These endosymbionts play key roles in their hosts' fitness, including protecting them against natural enemies and manipulating their reproduction in ways that increase the frequency of symbiont infection. Little is known about the molecular mechanisms that underlie these processes. Here, we provide the first genome draft of a vertically transmitted male-killing Spiroplasma bacterium, the S. poulsonii MSRO strain harbored by D. melanogaster. Analysis of the S. poulsonii genome was complemented by proteomics and ex vivo metabolic experiments. Our results indicate that S. poulsonii has reduced metabolic capabilities and expresses divergent membrane lipoproteins and potential virulence factors that likely participate in Spiroplasma-host interactions. This work fills a gap in our knowledge of insect endosymbionts and provides tools with which to decipher the interaction between Spiroplasma bacteria and their well-characterized host D. melanogaster, which is emerging as a model of endosymbiosis.

Data Envelopment Analysis and non-discretionary inputs : How to select the most suitable model using multi-criteria decision analysis

Within Data Envelopment Analysis, several alternative models allow for an environmental adjustment. The majority of them deliver divergent results. Decision makers face the difficult task of selecting the most suitable model. This study is performed to overcome this difficulty. By doing so, it fills a research gap. First, a two-step web-based survey is conducted. It aims (1) to identify the selection criteria, (2) to prioritize and weight the selection criteria with respect to the goal of selecting the most suitable model and (3) to collect the preferences about which model is preferable to fulfil each selection criterion. Second, Analytic Hierarchy Process is used to quantify the preferences expressed in the survey. Results show that the understandability, the applicability and the acceptability of the alternative models are valid selection criteria. The selection of the most suitable model depends on the preferences of the decision makers with regards to these criteria.

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This clinical handbook is a valuable resource for any health professional who works with adolescents and young adults, whether in paediatric or adult acute care facilities or in the community. As a handbook it provides ready access to practical, clinically relevant and youth specific information. This clinical handbook fills a clear gap, as most adolescent texts are primarily directed at paediatricians. This handbook extends its scope beyond paediatrics for three important reasons. First, many adolescents are managed by adult trained clinicians who have not had much exposure to or training in adolescent health. Secondly, the important health conditions of adolescents are often the important health conditions in young adults. Thirdly, with increased survival rates in chronic illness over the last two to three decades, it is becoming essential that clinicians in adult health care are able to assess and manage conditions that have their origins in childhood.

Emotions in International Politics. Beyond Mainstream International Relations

In recent years, social scientists have increasingly recognized the interconnectedness of thought on emotions. Nowhere is the role of passions more evident than international politics, where pride, anger, guilt, fear, empathy, and other feelings are routinely on display. But in the absence of an overarching theory of emotions, how can we understand their role at the international level? Emotions in International Politics fills the need for theoretical tools in the new and rapidly growing subfield of international relations. Eminent scholars from a range of disciplines consider how emotions can be investigated from an international perspective involving collective players, drawing evidence from such emotionally fraught events as the Rwandan genocide, World War II, the 9/11 attacks, and the Iranian nuclear standoff. The path-breaking research collected in Emotions in International Politics will be a valuable theoretical guide to understanding conflict and cooperation in international relations.