¿Centros de poder? Sociedad y poblamiento en la Meseta Norte española (ca. 800-400 a.C.)

[ES]La aparición de los primeros centros fortificados en la Meseta Norte durante la Primera Edad del Hierro es un proceso cuya comprensión se encuentra aún en sus inicios. No obstante, los resultados de las investigaciones arqueológicas más recientes proporcionan una imagen considerablemente mejorada sobre el desarrollo de estos sitios autosuficientes, algunos de los cuales se aglomeraron formando grupos mayores y más complejos al final del período. La configuración de asentamientos y comunidades, la interpretación sociológica de sus correspondientes necrópolis y los patrones regionales de poblamiento nos acercan a la organización social de las gentes que habitaron la Meseta en aquel período. [EN] The appearance of the first fortified settlements in the Northern Plateau (Spain) during the Early Iron Age is a process whose understanding is still far from resolved. We know when some small settlements were founded, but the evolution of these communities into other ones that were somewhat larger and more complex is not clear. However, the results of the latest archaeological research provide significantly improved image on the development of these sites, some of which were nucleated into larger and more complex groups at the end of this period. The configuration of settlements and communities, the sociological interpretation of their cemeteries and the regional settlement patterns reveal the social organisation of the people who inhabited the plateau in that period.

Il destino del Contra Celsum nel ‘400-‘700 in Europa

La tesi di dottorato del dott. Wu Gongqing è il frutto di un lavoro di studio e ricerca durato tre anni e condotto usufruendo delle strutture di ricerca della Fondazione per le Scienze Religiose Giovanni XXIII di Bologna. L'obiettivo del lavoro che il candidato presenta è quello di offrire un quadro della ricezione di una delle maggiori opere di Origene, il Contra Celsum, nella cultura dell'Europa moderna. Il punto di vista scelto per condurre questa indagine è quello delle edizioni e traduzioni che il testo conobbe a partire dal 1481 sino alla fine del Settecento. La scansione del lavoro segue il susseguirsi delle diverse edizioni, con un capitolo dedicato alle edizioni umanistiche e al loro impatto sulla cultura italiana ed europea fra Quattro e Cinquecento. Seguono i capitoli dedicati alle edizioni di Hoeschel, Spencer, Bouhéreau e Delarue, Mosheim e Tamburini. In ciascun capitolo il ricercatore prende in esame le diverse edizioni e traduzioni, analizzandone le caratteristiche letterarie principali, lo stile, il rapporto con la tradizione manoscritta, la diffusione e cercando di ricondurre ciascuna di esse al proprio specifico ambito storico-culturale.

Stratigraphic Variation Within Polar Firn Caused by Differential Accumulation and Ice Flow: Interpretation of a 400 Mhz Short-Pulse Radar Profile from West Antarctica

We investigate causes of the stratigraphic variation revealed in a 177 km, 400 MHz short-pulse radar profile of firn from West Antarctica. The profile covers 56 m depth, and its direction was close to those of the ice flow and mean wind. The average, near-surface accumulation rates calculated from the time delays of one radar horizon consistently show minima on leeward slopes and maxima on windward slopes, confirming an earlier study based on stake observations. The stratigraphic variation includes up to 30 m depth variation in individual horizons over tens of km, fold limbs that become progressively steeper with depth, and fold-hinge loci that change direction or propagate down-ice with depth over distances far less than predicted by the ice speeds. We use an accumulation rate model to show how local rate anomalies and the effect of ice speed upon a periodic variation in accumulation rate cause these phenomena, and we reproduce two key features seen in the stratigraphic variations. We conclude that the model provides an explanation of changes in spatial stratigraphy and local measures of accumulation history given the constraints of surface topography, ice and wind velocities, and a general accumulation rate for an area.

Stratigraphic Continuity in 400 Mhz Short-Pulse Radar Profiles of Firn in West Antarctica

We track dated firn horizons within 400 MHz short-pulse radar profiles to find the continuous extent over which they can be used as historical benchmarks to study past accumulation rates in West Antarctica. The 30-40 cm pulse resolution compares with the accumulation rates of most areas. We tracked a particular set that varied from 30 to 90 m in depth over a distance of 600 km. The main limitations to continuity are fading at depth, pinching associated with accumulation rate differences within hills and valleys, and artificial fading caused by stacking along dips. The latter two may be overcome through multi-kilometer distances by matching the relative amplitude and spacing of several close horizons, along with their pulse forms and phases. Modeling of reflections from thin layers suggests that the - 37 to - 50 dB range of reflectivity and the pulse waveforms we observed are caused by the numerous thin ice layers observed in core stratigraphy. Constructive interference between reflections from these close, high-density layers can explain the maintenance of reflective strength throughout the depth of the firn despite the effects of compaction. The continuity suggests that these layers formed throughout West Antarctica and possibly into East Antarctica as well.

A Comparison of Complications in 400 Patients After Native Nail Versus Silicone Nail Splints for Fingernail Splinting After Injuries

BACKGROUND The fingertip is the most commonly injured part of the hand and is an important aesthetic part of the hand. METHODS In this retrospective study we analyzed data from 700 patients operated on between 1997 and 2008 for complications after nail splinting with native nail or silicone nail. Inclusion criteria were patients living in Bern/Berner Land, complete documentation, same surgical team, standard antibiotics, acute trauma, no nail bed transplantation, and no systemic diseases. Groups were analyzed for differences in age, gender, cause and extension of trauma, bony injury and extent, infection, infectious agent, and nail deformities. Statistical analysis was done using the χ (2) test, Fisher's exact test, and Pearson correlation coefficients. RESULTS A total of 401 patients, with a median age of 39.5 years, were included. There were more men with injured nails. Two hundred forty native nails and 161 silicone splints were used. There were 344 compression injuries, 44 amputations, and 13 avulsion injuries. Forty-three patients had an infection, with gram-positive bacteria (Staphylococcus aureus) causing most infections. A total of 157 nail dystrophies were observed, split nails most often. The native nail splint group showed significantly (p < 0.015) fewer nail deformities than the silicone nail splint group; otherwise, there were no statistical differences. However, there were twice as many infections in the silicone nail group. CONCLUSION It seems to be advantageous to use the native nail for splinting after trauma, when possible. In case of a destroyed and unusable nail plate, a nail substitute has to be used.

Talmudische "Weisheit" : 400 höchst interessante märchenhafte Aussprüche der Rabbinen ; direkt aus der Quelle geschöpft und dem christlichen Volke vorgetragen

von Justus [d.i. August Briemann]

New insights into the reconstructed temperature in Portugal over the last 400 years

The consistency of an existing reconstructed annual (December–November) temperature series for the Lisbon region (Portugal) from 1600 onwards, based on a European-wide reconstruction, with (1) five local borehole temperature–depth profiles; (2) synthetic temperature– depth profiles, generated from both reconstructed temperatures and two regional paleoclimate simulations in Portugal; (3) instrumental data sources over the twentieth century; and (4) temperature indices from documentary sources during the late Maunder Minimum (1675–1715) is assessed. The low-frequency variability in the reconstructed temperature in Portugal is not entirely consistent with local borehole temperature–depth profiles and with the simulated response of temperature in two regional paleoclimate simulations driven by reconstructions of various climate forcings. Therefore, the existing reconstructed series is calibrated by adjusting its low-frequency variability to the simulations (first-stage adjustment). The annual reconstructed series is then calibrated in its location and scale parameters, using the instrumental series and a linear regression between them (second-stage adjustment). This calibrated series shows clear footprints of the Maunder and Dalton minima, commonly related to changes in solar activity and explosive volcanic eruptions, and a strong recent-past warming, commonly related to human-driven forcing. Lastly, it is also in overall agreement with annual temperature indices over the late Maunder Minimum in Portugal. The series resulting from this post-reconstruction adjustment can be of foremost relevance to improve the current understanding of the driving mechanisms of climate variability in Portugal.

Synoptic drivers of 400 years of summer temperature and precipitation variability on Mt. Olympus, Greece

The Mediterranean region has been identified as a global warming hotspot, where future climate impacts are expected to have significant consequences on societal and ecosystem well-being. To put ongoing trends of summer climate into the context of past natural variability, we reconstructed climate from maximum latewood density (MXD) measurements of Pinus heldreichii (1521–2010) and latewood width (LWW) of Pinus nigra (1617–2010) on Mt. Olympus, Greece. Previous research in the northeastern Mediterranean has primarily focused on inter-annual variability, omitting any low-frequency trends. The present study utilizes methods capable of retaining climatically driven long-term behavior of tree growth. The LWW chronology corresponds closely to early summer moisture variability (May–July, r = 0.65, p < 0.001, 1950–2010), whereas the MXD-chronology relates mainly to late summer warmth (July–September, r = 0.64, p < 0.001; 1899–2010). The chronologies show opposing patterns of decadal variability over the twentieth century (r = −0.68, p < 0.001) and confirm the importance of the summer North Atlantic Oscillation (sNAO) for summer climate in the northeastern Mediterranean, with positive sNAO phases inducing cold anomalies and enhanced cloudiness and precipitation. The combined reconstructions document the late twentieth—early twenty-first century warming and drying trend, but indicate generally drier early summer and cooler late summer conditions in the period ~1700–1900 CE. Our findings suggest a potential decoupling between twentieth century atmospheric circulation patterns and pre-industrial climate variability. Furthermore, the range of natural climate variability stretches beyond summer moisture availabilityobserved in recent decades and thus lends credibility to the significant drying trends projected for this region in current Earth System Model simulations.