A comparison of the processes of institutionalisation of political economy in Spain and Italy (1860-1900)

[spa] El estudio de los procesos a través de los cuales la economía política se ha transformado en una disciplina académica es un área de creciente interés en la historia del pensamiento económico. Dicho estudio se ha abordado a través del análisis de la importancia de la economía política en un conjunto de instituciones, consideradas clave en la expansión de la economía en las sociedades occidentales en la segunda mitad del siglo XIX y primeras décadas del XX: universidades, sociedades económicas, publicaciones periódicas de contenido económico y los parlamentos nacionales. Este papel presenta una comparación entre los desarrollos del proceso de institutionalización de la economía política en España e Italia, a través del estudio de la presencia de esta disciplina en las instituciones mencionadas para el periodo 1860-1900. El objetivo es medir la posible existencia de una vía común en la institucionalización de la economía política en ambos países, como un primer paso hacia la elaboración de un modelo supranacional de institucionalización de la economía en este periodo.

The First privatization : selling SOEs and privatizing public monopolies in fascist Italy, 1922-1925

[cat] El primer govern feixista d’Itàlia va aplicar una política de privatització a gran escala entre 1922 i 1925. El govern va privatitzar el monopoli estatal de llumins, el monopoli estatal d’assegurances de vida, va vendre la major part de la xarxa i serveis de telefònica pública a empreses privades, va reprivatitzar el major productor de productes metàl·lics, i va atorgar concessions a empreses privades per construir i explotar autopistes de peatge. Tot i que algunes consideracions ideològiques van poder tenir alguna influència, la privatització va ser usada sobre tot com un instrument polític per construir confiança amb els grans industrials i per augmentar el suport al govern i al Partito Nazionale Fascista. La privatització també va contribuir a equilibrar el pressupost públic, qüestió aquesta que va ser el principal objectiu de la primera fase de la política econòmica feixista.

Why Italy and not Spain?: comparing two industrialization processes from a dissagregate time-series perspective

This study presents new evidence concerning the uneven processes of industrialization innineteenth century Spain and Italy based on a disaggregate analysis of the productivesectors from which the behaviour of the aggregate indices is comprised. The use of multivariate time-series analysis techniques can aid our understanding and characterization of these two processes of industrialization. The identification of those sectors with key rolesin leading industrial growth provides new evidence concerning the factors that governed thebehaviour of the aggregates in the two economies. In addition, the analysis of the existenceof interindustry linkages reveals the scale of the industrialization process, and wheresignificant differences exist, accounts for many of the divergences recorded in the historiography for the period 1850-1913.

Carbon isotope stratigraphy and carbonate production during the Early-Middle Jurassic: examples from the Umbria-Marche-Sabina Apennines (Central Italy)

The carbon isotopic signature of carbonates depends on secular variations of organic carbon and carbonate carbon production/burial rates. A decrease in carbonate productivity makes the organic/carbonate carbon ratio unstable up to the point that even minor variations in the organic carbon reservoirs can provoke carbon isotopic shifts. The delta(13)C positive shifts of the middle Carixian (early Pliensbachian) and the early Bajocian recorded in the Umbria-Marche-Sabina domain represent a good example of this mechanism. Both sedimentology and lithostratigraphy of pelagic platform-basin carbonate systems in this area show that important changes in the source of carbonates correspond to the observed isotopic shifts. The middle Carixian event is in fact well correlatable to the drastic reduction of benthic carbonate production on rift-related intrabasinal highs, which then became pelagic carbonate platforms. The early Bajocian event is concomitant with the beginning of a long hiatus on the pelagic carbonate platforms and with a drop of the biodiversity of calcareous organisms followed by the onset of biosiliceous sedimentation in basins. (C) 2002 Elsevier Science B.V. All rights reserved.

Le prêt à intérêt dans l'Antiquité préchrétienne : Jérusalem, Athènes, Rome : étude juridique, philosophique et historiographique

Le prêt à intérêt était pratiqué par tous les peuples de l'Antiquité préchrétienne, à l'exception du peuple d'Israël. L'auteur examine d'abord l'interdiction du prêt à intérêt dans l'Ancien Testament. Il expose ensuite la pratique du prêt à intérêt en Grèce, avant de détailler les critiques d'Aristote. Enfin, l'auteur retrace l'évolution du prêt (mutuum) et de la réglementation de l'intérêt à Rome, des origines à Constantin. Il met l'accent sur trois grandes controverses parmi les romanistes modernes (XVIe - XXIe s.) : sur le nexum, sur la centesima et, surtout, sur le mystérieux fenus unciarium, le taux d'intérêt fixé par les Douze Tables, pour lequel l'éventail des interprétations va de 1 à 100 % par an ! L'auteur recense les opinions de plus de 400 juristes et historiens, discute les plus importantes et propose sa conclusion. The loan at interest was used by all the peoples of pre-Christian Antiquity, excepting the people of Israel. The author first focuses on the prohibition of lending at interest in the Old Testament. He then explores the use of loans at interest in Greece before examining Aristotle's criticism. Eventually, the author follows the evolution of loan (mutuum) and interest regulation in Rome, from the origins to Constantine. Three great controversies among modern Roman law scholars (16th - 21th) are considered: nexum, centesima and above all, the mysterious fenus unciarium, the interest rate defined by the Twelve Tables, for which the range of interpretations varies between 1 and 100% per year! The author gives an inventory of more than 400 opinions expressed by jurists and historians, discusses the most important ones and suggests a solution.

[Illustrations de Rome et l'Italie méridionale.] / J.D. Harding, dess. ; L. De Sivry, aut. du texte

Comprend : [pl. en reg. de la page de titre : vue du Château Saint-Ange, du pont des Anges et du Tibre à Rome. [Cote K 1728/Microfilm R 122016] ; [Fig. au titre : vue de la ville de Sorrente.] Sorrente. [Cote K 1728/Microfilm R 122016] ; [pl. en reg. p.17 :] Rome (Vue de l'Eglise St-Pierre et de la Place du Vatican). [Cote K 1728/Microfilm R 122016] ; [pl. en reg. p.27. Chapitre III : Saint-Pierre de Rome.] [Cote K 1728/Microfilm R 122016] ; [pl. en reg. p.49 : le Forum de Rome.] [Cote K 1728/Microfilm R 122016] ; [pl. en reg. p.197. Chapitre XII : vue de Tivoli.] [Cote K 1728/Microfilm R 122016] ; [pl. en reg. p.247. Chapitre XIV : paysage du Sud de l'Italie. Environs de Naples avec vue sur le Golfe.] [Cote K 1728/Microfilm R 122016] ; [pl. en reg. p.264 : Naples et le Pausilippe (tombeau de Viegile) et la plage de la Mergellina.] [Cote K 1728/Microfilm R 122016] ; [pl. en reg. p.276 : paysage du lac Lucrin et le Monte-Nuovo (?) qui jaillit en une nuit, en 1538, d'une éruption volcanique et engloutit le village de Tripergola] [Cote K 1728/Microfilm R 122016] ; [pl. en reg. p.279 : une île du Golfe de Naples (Ischia?).] [Cote K 1728/Microfilm R 122016] ; [pl. en reg. p.296 : vue de l'intérieur de l'église du Carmine à Naples] [Cote K 1728/Microfilm R 122016] ; [pl. en reg. p.305 : vue d'Herculanum] [Cote K 1728/Microfilm R 122016] ; [pl. en reg. p.327 : vue d'Amalfi et de son couvent des Capucins suspendu aux flancs de la montagne.] [Cote K 1728/Microfilm R 122016] ; [pl. en reg. p.331. Chapitre XX : vue de vestiges de temples antiques dans la région de Paestum (?).] [Cote K 1728/Microfilm R 122016] ; [pl. en reg. p.339 : vue du Couvent de Saint-Martin, non loin de Palerme, en Sicile.] [Cote K 1728/Microfilm R 122016]

Family history of cancer and the risk of laryngeal cancer: a case-control study from Italy and Switzerland.

Only limited data is available on the relationship between family history of laryngeal and other neoplasms and laryngeal cancer risk. We investigated the issue using data from a multicentre case-control study conducted in Italy and Switzerland between 1992 and 2009 including 852 cases with histologically confirmed laryngeal cancer and 1970 controls admitted to hospital for acute, non neoplastic conditions. Unconditional logistic regression models adjusted for age, sex, study center, education, tobacco smoking, alcohol drinking and number of siblings were used to estimate the odds ratios (ORs) of laryngeal cancer. The multivariate OR was 2.8 (95% confidence interval [CI], 1.5-5.3) in subjects reporting a first-degree relative with laryngeal cancer, as compared to subjects with no family history. The OR was higher when the relative was diagnosed before 60 years of age (OR = 3.5, 95% CI 1.4-8.8). As compared to subjects without family history, non-smokers, and moderate drinkers, the OR was 37.1 (95% CI 9.9-139.4) for current smokers, heavy drinkers, with family history of laryngeal cancer. Family history of colorectal (OR = 1.5, 95% CI 1.0-2.3) and kidney (OR = 3.8, 95% CI 1.2-12.1) cancer were also associated to an increased risk of laryngeal cancer, while no significant increase in risk was found for family history of cancer at all sites, excluding the larynx (OR = 1.1).

Dissolution-reprecipitation of zircon at low-temperature, high-pressure conditions (Lanzo Massif, Italy)

An eclogite facies meta-plagiogranite from the Lanzo massif (western Alps, Italy) contains crystals of zircon intimately associated with allanite. Zircon displays different microtextures ranging from pristine, euhedral, and magmatic to fractured, porous varieties with mosaic zoning, and pervasive recrystallization into euhedral microcrystals. Fractures and voids in the recrystallized zircon microcrystals are mainly filled by high-pressure Na-rich pyroxene. Electron backscattered diffraction analysis revealed a similar crystallographic orientation for primary magmatic zircon crystals and microcrystals, with less than 2 degrees misorientation among neighboring microdomains. The textural change is coupled with chemical and isotopic modifications: recrystallized zircon domains contain significantly less Th and light- to mid-REE, but are richer in Sr than magmatic zircon crystals. Magmatic zircon preserves the protolith U-Pb age of 163.5 +/- 1.7 Ma, whereas zircon microcrystals have a mean age of 55 +/- 1 Ma. The coexisting allanite also contains inclusions of Na-rich pyroxene and has chemical features (elevated Sr and Ni contents and lack of Eu anomaly) indicating formation at high pressure. Despite being associated texturally with zircon, allanite yields a younger Th-Pb age of 46.5 +/- 3.0 Ma, suggesting that the Lanzo unit remained at relatively high pressure conditions for similar to 8 m.y. Zircon recrystallization proceeded with volume reduction and loss of material to an alkaline metamorphic fluid that acted as the agent for a coupled dissolution-reprecipitation process. Recrystallization occurred with minimum transport, in a low-strain environment, and was not significantly enhanced by metamictization. The source of the fluid for zircon recrystallization is most probably related to prograde devolatilization reactions in the surrounding serpentinite.