Engastando una piedra preciosa = The setting of a jewel

Engastando una piedra preciosa

Induction of ovulation in rabbits by adding Lecirelin to the seminal dose: In vitro and in vivo effects of different excipients.

This study evaluates the effect of Lecirelin (Dalmarelin®, Fatro, Italy) diluted in different excipients (benzilic alcohol, benzoic acid and paraben) added to a seminal dose on LH concentrations, progesterone concentrations and ovarian status in rabbits. The in vitro effect on spermatozoa was also tested. A total of 100 multiparous female rabbits were divided into 5 groups, which at the moment of AI, received 0.2 mL (5 μg/dose) intramuscular (im) inoculation of Lecirelin (control) or the same Lecirelin dose administered intravaginally (iv) with the seminal dose alone (Lecirelin group) or with benzilic alcohol (Lecirelin BA group), benzoic acid (Lecirelin BAc group) or parabens (Lecirelin PA group) as an excipient. After 7 days, 10 rabbits per group were euthanized to analyze their ovarian status. In the control group, a high LH peak was detected 30 min post AI, while in the iv groups a slight increase in LH occurred after 120 min. The ovulation and fertility rate was similar in control and Lecirelin groups, while the lowest fertility rate was detected in the Lecirelin BA group. In a second experiment, the semen samples collected from male rabbits were diluted in TALP (control) or mixed with the 5 μg of Lecirelin solutions used in the first experiment. The highest percentage of capacitated sperm (68.3%) was recorded in the Lecirelin PA. The lowest percentages were observed in the Lecirelin BA and BAc groups. In conclusion, the iv administration of Lecirelin represents an alternative method for simplifying rabbit insemination procedures.

Planning and management of mobility in natural protected areas

The final purpose is the identification of: a) the effects of various choices in transport planning, both at long term and strategic level; b) the most effective policies of mobility management. The preliminary work was articulated in the following steps: 1) definition of protected area on the basis of ecological and socio-economic criteria and legislative constraints; 2) analysis of mobility needs in the protected areas; 3) reconstruction of the state of the art of mobility management in natural parks at European level; 4) analysis of used traffic flows measurement methods; 5) analysis of environmental impacts due to transport systems modelling (limited to air pollution and noise); 6) identification of mitigation measures to the potentially applied. The whole methodology has been firstly tested on the case study of the National Park of ?Gran Sasso and Monti della Laga? and further validated on the National Park of ?Gargano?, both located Italy: i) the concerned area has been zoned according to the land-use peculiarities; ii) the local situations of transport infrastructure (roads and parking), services (public transport systems) and rules (traffic regulations) have been mapped with references to physical and functional attributes; iii) the mobility, both systematic and touristic, has been synthetically represented in an origin-destination matrix. By means of an assignment model it has been determined the distribution of flows and the corresponding average speeds to quantify gaseous and noise emissions. On this basis the environmental criticalities in the reference scenario have been highlighted, as well as some alternative scenarios including both operational and infrastructural measures have been identified. The comparison between the projects and the reference scenario allowed the quantification of the effects (variation of emissions) for each scenario and a selection of the most effective management actions to be taken.

A general system of nature, through the three grand kingdoms of animals, vegetables, and minerals, systematically divided into their several classes, orders, genera, species, and varieties, with their habitations, manners, economy, structure and peculiarities. /

v. 7 (1806)

Rome, Italy, 1823 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Nuova pianta di Roma Moderna, estratta dalla grande del Nolli corretta ed accresciuta de nomi delle contrade indicati al loro rispettivo sito in Roma; Pietro Ruga incise. It was published by Venanzio Monaldini Libraio e Cartolaro in 1823. Scale [ca. 1:9,120]. Covers Rome, Italy and Vatican City. The image inside the map neatline is georeferenced to the surface of the earth and fit to the "European Datum 1950 UTM Zone 33N" coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, city districts, walls, gates, and fortifications, selected buildings, and more. Relief is shown by hachures. Includes index and inset plans: Pianta della Chiesa di S. Lorenzo fuori le mura -- Mausoleo di S. Costanza -- Pianta della Basilica di S. Paolo -- Pianta del Pantheon, degli avanzi delle Terme di Agrippa, e dé ruderi scoperti recentemente. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Rome, Italy, 1832 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Pianta della citta di Roma : con la indicazione di tvtte le antichita e nvovi abbellimenti nell anno MDCCCXXXII, Pietro Ruga incise. It was published by Venanzio Monaldini libraio e cartolaro in 1832. Scale [ca. 1:5,066]. Covers Rome, Italy and Vatican City.The image inside the map neatline is georeferenced to the surface of the earth and fit to the "European Datum 1950 UTM Zone 33N" coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, city districts, walls, gates, and fortifications, selected buildings, and more. Relief is shown by hachures. Includes indices and architectural engravings at left and right margins: Basilica di S. Giovanni -- Interno di S. Giovanni -- Basilica di S. Paolo -- Interno di S. Paolo -- Campidoglio Moderno -- Anfiteatro Favio -- Primaide di C. Cestio -- Foro Trajano -- Basilica di S. Pietro -- Interno di S. Pietro -- Basilica di S. M.a Maggiore -- Interno di S. M.a Maggiore -- Pantheon di Agrippa -- Interno del Pantheon -- Monte Cavallo -- Foro Romano. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Rome, Italy, 1862 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Pianta di Roma, Giovanni Montiroli inv. e dis. le vedute; Augusto Fornari incise; Domenico Feltrini scrisse. It was published by Luigi Piale in nell' anno MDCCCLXII [i.e., 1862]. Scale [ca. 1:8,500,000]. Covers Rome, Italy and Vatican City. The image inside the map neatline is georeferenced to the surface of the earth and fit to the "European Datum 1950 UTM Zone 33N" coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, city districts, walls, gates, and fortifications, selected buildings, and more. Relief is shown by hachures. Includes indices and inset: Controni di Roma.This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Rome, Italy, 1881 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Pianta della città di Roma, 1881. It was published by Libreria Spithöver in 1881. Scale 1:8,800. Covers also Vatican City.The image inside the map neatline is georeferenced to the surface of the earth and fit to the "European Datum 1950 UTM Zone 33N" coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, aqueducts, city walls, gates, and fortifications, selected buildings, villas, and points of interest, and more. Relief is shown by hachures. Indices at margins.This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

The emblematic statement of the Nobel Peace Prize. Jean Monnet/Robert Schuman Paper Series Vol. 13 No. 1, January 2013

From the Introduction. On October 12th the Nobel Committee announced that the annual Nobel Peace Prize would be awarded to the European Union for, “promoting peace, democracy and human rights over six decades”.1 This was a bit of good news for the EU who had produced nothing but bad press with the Euro Crisis, the bailouts of struggling countries like Greece, and protests in the southern member states of Spain, Portugal, and Italy. At such a momentous occasion the EU’s next challenge was to figure out who would be the rightful head of the EU to accept the award. The EU has made their decision by opting to send its top three officials Jose Manuel Barroso the President of the European Commission, Herman Van Rompuy the President of the European Council, and Martin Schulz the President of the European Parliament2 as a sign that the EU is not headed by one person but instead is an supranational economic and political bloc that seeks to unify the European continent. Their symbolic acceptance of the award is in response to what Geir Lundestad, the Secretary of the Norwegian Nobel Committee, called, “an accumulated record.”3 This record has ushered the EU into the international spotlight as a beacon for countries in the EU’s periphery to want to join the bloc.

The Impact of the SFP System on Italian Farmland Prices and Tenure Contracts. Factor Markets Working Document No. 65, August 2013

EDITED VERSION TO BE PUBLISHED SOON. The aim of this paper is to contribute to the estimation of the potential effects of the CAP reform on propensity to transaction, particularly comparing the effect of different new instruments/policy settings with the current policy (CAP health check) used as a baseline. The work is focused on three of new policy instruments within the post 2013 CAP reform proposal: regionalization, greening and capping. The first and second are analysed in more detail. The analysis will be based on a survey of farmers in the Province of Bologna, Emilia Romagna, Italy. The questionnaire focuses on mechanism of access to land and related incentives towards different land use/economic behaviour. The survey includes information about respondent characteristics (farm, farmer, household and payments received) and stated intention about potential changes in land operated under alternative agricultural policy scenarios (particularly the post-2013 reform proposals).

(Table 1) Comparison of three chronologies for the sapropel series of cores KC01-KC01b

The Quaternary climate of southern Europe (south Italy and Greece) is investigated by pollen analysis of the sapropels which were deposited in the deep eastern Mediterranean Sea during the last 1 million year (Ma). The time-scale of core KC01b in the Ionian Sea has been established by tuning its oxygen isotopic record to the ice volume model of Imbrie and Imbrie (1980, doi:10.1126/science.207.4434.943). For the last 250,000 year (250 ka), the previous pollen studies and astronomical tuning have been confirmed. Sapropels were deposited under a large range of Mediterranean climates: fully interglacial, fully glacial, and intermediary, as revealed mainly by the balance between the respective pollen abundances of oak (Quercus) and sage-brush (Artemisia). The high value of the oak reveals the warm and wet climate of an Interglacial, and the high value of the sage-brush, the dry and cold climate of a Glacial. Whereas the Mediterranean climate is directly related to the variation of the high-latitude ice sheets, the deposition of sapropels is not so. In contrast with the wide climatic range, sapropels were deposited only when summer insolation in the low latitudes reached its highest peaks. However, between 250 ka and 1 Ma, that stable pattern is not yet established. Only six sapropels are observed, many expected ones do not appear, even as ghosts signalled by peaks of barium abundance, that remain after the post-deposition oxidation of organic matter. The pattern of sapropel formation in stable and direct relationship to highest insolation does not seem to apply. For five of those sapropels, neither climate extremes are observed; they mainly formed during intermediary types of Mediterranean climate. In contrast, one sapropel (and one ghost) relates to a relatively low peak of insolation, and its climate is of a unique, composite type not seen later. This might suggest an unsuspected, more complex pattern linking the formation of Mediterranean sapropels to the astronomical configuration.