31 research outputs found

    Designation of origine and geographical indication of olives and olive oils in Croatia

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    Europsko i svjetsko tržiÅ”te prehrambenih proizvoda zasićeno je novim proizvodima koji međusobno konkuriraju kakvoćom i cijenom. Nespecifični proizvodi nisu u mogućnosti nositi se s oÅ”trom konkurencijom sličnih proizvoda, a potroÅ”ači su često nesigurni u kakvoću onoga Å”to kupuju. Zbog toga se javila potreba za zaÅ”titom proizvoda visoke kakvoće i specifičnih karakteristika. U tu svrhu EU je 1992. godine stvorila sustave: PDO (Protected Designation of Origin odnosno Oznaka izvornosti), PGI (Protected Geographical Indication odnosno Oznaka zemljopisnog podrijetla) i TSG (Traditional Speciality Guaranteed odnosno Oznaka ā€žtradicionalni ugledā€œ). Od 2005. godine proizvođačima u Hrvatskoj omogućena je ista zaÅ”tita za proizvode koje imaju i proizvođači u zemljama EU, čime se podiže razina konkurentnosti domaće proizvodnje i prepoznatljivost domaćih proizvoda. Cilj ovog rada bio je pojasniti mogućnosti zaÅ”tite maslinovog ulja i stolnih maslina, te iznoÅ”enjem praktičnih primjera dati doprinos u bržem integriranju Hrvatske u europsko i svjetsko tržiÅ”te proizvoda od maslina.European and world market of foodstuffs is glutted with new products competing by quality and price. Non specific products are not able to deal with a sharp competition among similar products, and consumers are often uncertain about the quality of purchased goods. Therefore the EU created in 1992 three types of food quality system: PDO (Protected Designation of Origin), PGI (Protected Geographical Indication) and TSG (Traditional Speciality Guaranteed). From 2005 Croatian producers have the same possibility of protecting their products as the EU producers, raising the competitiveness and identity of domestic production and products. The aim of the present paper was to clarify the possibilities for olive oil and table oil protection, as well as to give a contribution to faster integration of Croatia in to European and world olive products market by giving practical examples

    Oil content in fruits of leading autochthonous olive varieties in Istria

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    Sadržaj ulja u plodu masline najvažniji je čimbenik koji određuje ekonomsku vrijednost pojedine sorte i jedan od kriterija za određivanje stupnja zrelosti ploda, odnosno karakterizaciju sorte. Određena je količina ulja u plodu vodećih autohtonih sorti maslina u Istri, tijekom 2004. i 2005. godine, pomoću Soxtec aparata. Dobiveni podaci u zasebnim godinama upućuju na povezanost sadržaja ulja sa sortom, no njihova varijabilnost između dvije godine za pojedinu sortu ukazuje na značajan utjecaj vanjskih čimbenika. Dobiveni rezultati variraju između 21 i 48% ulja u odnosu na suhu tvar ploda, Å”to ukazuje na značajan ekonomski potencijal ovih sorti.The oil content in an olive fruit is the most relevant factor determining the economic value of singular variety and one of the criteria for fruit maturity degree determination, and variety characterization as well. In this paper, the olive oil content in fruits of leading autochthonous olive varieties in Istria during crop seasons 2004 and 2005, using Soxtec apparatus, was determined. The results obtained reflect mostly the influence of the variety genetic potential on the oil content, when monitored in a single year, but its variation between the two years in a single variety shows the influence of external factors. The oil content on a dry weight basis in fruits of investigated varieties ranged from 21% to 48% which shows their high economic potential

    Cladribine tablets in people with relapsing multiple sclerosis : A real-world multicentric study from southeast European MS centers

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    Cladribine is an oral disease-modifying drug authorized by the European Medicine Agency for the treatment of highly active relapsing multiple sclerosis (MS).To provide real-world evidence of cladribine's effectiveness and safety in people with MS (pwMS).A retrospective observational multi-center, multi-national study of pwMS who were started on cladribine tablets in ten centers from five European countries.We identified 320 pwMS treated with cladribine tablets. The most common comorbidities were arterial hypertension and depression. Three patients had resolved hepatitis B infection, while eight had positive Quantiferon test prior to cladribine commencement. There were six pwMS who had malignant diseases, but all were non-active. During year 1, 91.6% pwMS did not have EDSS worsening, 86.9% were relapse-free and 72.9% did not have MRI activity. During the second year, 90.2% did not experience EDSS worsening, 86.5% were relapse-free and 75.5% did not have MRI activity. NEDA-3 was present in 58.0% pwMS in year 1 and in 54.2% in year 2. In a multivariable logistic regression model age positively predicted NEDA-3 in year 1. The most common adverse events were infections and skin-related adverse events. Lymphopenia was noted in 54.7% of pwMS at month 2 and in 35.0% at month 6. Two pwMS had a newly discovered malignant disease, one breast cancer, and one melanoma, during the first year of treatment.Our real-world data on the effectiveness and safety of cladribine tablets are comparable to the pivotal study and other real-world data with no new safety signals

    Trans-border (south-east Serbia/west Bulgaria) correlations of the Jurassic sediments: Infra-Getic Unit

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    The Infra-Getic Unit is a palaeogeographic unit, predestined by palaeotectonics. From the point of view of geological heritage, it represents a geosites framework. For the purpose of the correlation, the Serbian sections of Lukanja, Bogorodica Monastery, Rosomač and Senokos, as well as the Bulgarian sections of Komshtitsa, Gintsi, and Stanyantsi were used. The Jurassic sediments of the Infra-Getic Unit crop out on the southern slops of the Stara Planina Mountain in east Serbia and west Bulgaria. The Lower Jurassic started with continental and continental-marine sediments (clays and sandstones) (Lukanja clastics and Lukanja coal beds in Serbia and the Tuden Formation in Bulgaria) and continue with Lukanja quartz sandstones (Serbia) and the Kostina Formation (Bulgaria). These sediments are covered by Lukanja brachiopod beds and Lukanja limestones (Serbia) and the Romanov Dol, Ravna and Dolni Loukovit Members of the Ozirovo Formation (Bulgaria) predominantly consist of bioclastic limestones. The sedimentations follow with Lukanja belemnites-gryphaea beds (marls and clayey limestones), which in Bulgaria correspond to the Bukorovtsi Member (also marls and clayey limestones) of the Ozirovo Formation. The Middle Jurassic sedimentation started with black shales with Bossitra alpine. These sediments are individualized in Serbia as Senokos aleurolites and clays and in Bulgaria they are known as the Etropole Formation. In Serbia the section continues with sandstones called Vodenički sandstones of Bajocian age, known in Bulgaria as the Dobrogled Member of the Polaten Formation. However, in Bulgaria, the age is Upper Bajocian-Lower Bathonian, and it cover the marls of the lower member (Gornobelotintsi Member) of the Bov Formation and is covered by the upper member - alternation of marls and clayey limestones - the Verenitsa Member of the Bov Formation. The Vodenički sandstones-Dobrogled Member which ended their distribution in the section of Komshtitsa, to the east (in the Gintsi section), they are not represented - build a body of sandstones, a prodelta coming from the west to the east. The Bov Formation corresponds to the Senokos ammonite beds in east Serbia. The upper boundary of the Senokos ammonite beds and of the Bov Formation is sharp. It is covered by grey limestones of the Yavorec Formation in Bulgaria and by the Kamenica limestones in eastern Serbia. They are covered by grey or red nodular/lithoclastic limestones ("ammonitico rosso" type) of the Gintsi Formation in Bulgaria and the Pokrovenik ammonitic (acanthicum) limestones in Serbia. The Jurassic section in the Infra-Getic ended with grey micritic and lithoclastic limestones, which belong to the Rosomač and Rsovci limestones in east Serbia and to the Glozhene Formation in Bulgaria

    Trans-border (east Serbia/west Bulgaria) correlation of the Jurassic sediments: Main Jurassic paleogeographic units

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    In the region across the Serbian/Bulgarian state border, there are individualized 5 Jurassic paleogeographic units (from West to East): (1) the Thracian Massif Unit without Jurassic sediments; (2) the Lužnica-Koniavo Unit - partially with Liassic in Grsten facies and with deep water Middle Callovian-Kimmeridgian (p. p) sediments of the type "ammonitico rosso", and Upper Kimmeridgian-Tithonian siliciclastics flysch; (3) The Getic Unit subdivided into two subunits - the Western Getic Sub-Uni - without Lower Jurassic sediments and the Eastern Getic Sub-Unit with Lower Jurassic continental and marine sediments, which are followed in both sub-units by carbonate platform limestones (type Stramberk); (4) the Infra (Sub)-Getic Unit - with relatively deep water Liassic and Dogger sediments (the Dogger of type "black shales with Bossitra alpine") and Middle Callovian-Tithonian of type "ammonitico rosso"; (5) the Danubian Unit - with shallow water Liassic, Dogger and Malm (Miroč-VrÅ”ka Čuka Zone, deep water Dogger and Malm (Donjomilanovačko-Novokoritska Zone)

    Microfossils and brachiopods from the Lower Barremian at Prekonozi, eastern Serbia

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    This paper presents the results of an integral biostratigraphical study based on orbitolinids and other benthic foraminifers, brachiopods and algae of a part of the Prekonozi section, eastern Serbia. The species identified are: Paracoskinolinal jourdanensis Foury & Moullade, P. sunnilandensis (Maync), Orbitolinopsis debelmasi Moullade & Thieuloy, Alpillina antiqua FOURY, Pfenderina globosa FOURY, Mayncina bulgarica Leug, Peibernes & Rey, Charentia cuvilleri Neumani and other foraminifers, and brachiopods: Cyclothyrisl pancici (Antula), Sellithyris sella (J. DE C. Sowerby), Dictyothyris elongata Smirnova, and Psilothyris tamarindus (J. de C. Sowerby). The examined limestones based on orbitolinids, are assigned to the Lower Barremian, earlier dated Upper Barremian/Lower Aptian
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