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Adriatic Sea) Using a Combined Observational Modeling Approach
Marine Chemistry 177 (2015) 742–752 Contents lists available at ScienceDirect Marine Chemistry journal homepage: www.elsevier.com/locate/marchem A comprehensive assessment of the mercury budget in the Marano– Grado Lagoon (Adriatic Sea) using a combined observational modeling approach Donata Melaku Canu a,⁎, Ginevra Rosati a, Cosimo Solidoro a,b, Lars-Eric Heimbürger c,e, Alessandro Acquavita d a OGS—National Institute of Oceanography and Experimental Geophysics, Borgo Grotta Gigane 42 c. Sgonico, Trieste, Italy b ICTP, The Abdus Salam International Centre for Theoretical Physics — Strada Costiera, 11 I-34151 Trieste, Italy c Geochemistry and Hydrogeology Group, Department of Geosciences, University of Bremen Klagenfurter Straße, 28359 Bremen, Germany d O.A.A. — Osservatorio Alto Adriatico Via Lamarmora, 13–34139 Trieste, TS, Italy e Mediterranean Institute of Oceanography Campus de Luminy, 13288 Marseille, France article info abstract Article history: In this study, a biogeochemical model of the mercury cycle is applied to the Marano–Grado Lagoon (North Received 29 May 2015 Adriatic Sea, Italy) to 1) integrate the ensemble of disconnected and snap shot measurements collected over Received in revised form 30 October 2015 the last decade into a common and coherent framework, 2) assess the concentration of mercury species (HgII, Accepted 30 October 2015 MeHg, Hg0) in water, sediment and particulates, and 3) quantify the mercury fluxes and budgets within the la- Available online 31 October 2015 goon and among the lagoon, the atmosphere and the Adriatic Sea. As a result of long-term industrial and natural Keywords: contamination, the Marano–Grado Lagoon is a hot spot of mercury contamination in the Mediterranean Region. -
Evaluating 87Sr/86Sr Isotope Ratios and Sr Mass Fractions in Otoliths Of
bioRxiv preprint doi: https://doi.org/10.1101/2021.07.23.453494; this version posted July 25, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. 1 Evaluating 87Sr/86Sr isotope ratios and Sr mass fractions in otoliths of different European freshwater 2 fish species as fishery management tool in an Alpine foreland with limited geological variability 3 Andreas Zitek1,2*, Johannes Oehm3, Michael Schober1, Anastassiya Tchaikovsky1, Johanna Irrgeher5, 4 Anika Retzmann5, Bettina Thalinger4, Michael Traugott3, Thomas Prohaska5 5 1University of Natural Resources and Life Sciences, Vienna, Department of Chemistry, Institute of 6 Analytical Chemistry, Muthgasse 18, 1190 Wien, Austria 7 2FFoQSI GmbH ‐ Austrian Competence Centre for Feed and Food Quality, Safety & Innovation, 8 Technopark 1D, 3430 Tulln, Austria 9 3University of Innsbruck, Department of Zoology, Technikerstraße 25, 6020 Innsbruck, Austria 10 4University of Guelph, 50 Stone Road East, Guelph, N1G2W1, Canada 11 5Department of General, Analytical and Physical Chemistry, Chair of General and Analytical Chemistry, 12 Montanuniversität Leoben, Franz Josef‐Straße 18, 8700 Leoben, Austria 13 14 *Corresponding author: [email protected] 15 16 Highlights 17 Otolith microchemistry applied in in area with limited geological variability 18 Fish transferred, stocked or migrated were identified 19 Regressions between Sr/Ca ratios in water predict Sr mass fractions in otoliths 20 Species specific Sr discrimination from water into otoliths 21 European freshwater fish species assigned to habitat clusters of origin 22 Keywords 23 Strontium isotopes, Sr elemental fingerprint, otolith microchemistry, freshwater fish species, fishery 24 management. -
NEWSLETTER Opening of Honorary Consulate in Michigan
UN Day: Letters to Santa Consulate Gen. Diplomats in in in NYC Schools Seattle, WA is Closing page 3 > page 7 > page 8 > NEWSLETTER OCTOBER 26, 2012, VOLUME 8, NUMBER 40 Opening of Honorary Consulate in Michigan On October 2223, Ambassador Roman Kirn and Consul General in Cleveland Honorary Consul of Slovenia Yousif B. Ghafari speaking at the opening, next to him Ambassador Roman Kirn and Congressman John David Dingell. Jure Žmauc visited the State of Michigan to open The offi cial opening of Representative from Michigan, a new Honorary Consulate, the consulate was attended John David Dingell. Ambassador headed by the former U.S. by the mayor of Dearborn Kirn was also a guest on the Paul Ambassador to Slovenia and John O`Reilly, local consuls, W. Smith radio show on Detroit’s a respectable businessman, Slovenian community and the WJR radio. Smith is known for Yousif B. Ghafari. The media, and was celebrated with hosting a number of notable Honorary Consulate is a fl ag-raising ceremony. people, including politicians, located in Dearborn, near During his visit, authors and business leaders Detroit, which is the center Ambassador Kirn also met within the automotive industry. of the American automotive with the Governor of Michigan, Furthermore, industry. Richard Dale Snyder and U.S. Ambassador Kirn spoke at the Embassy of Slovenia 2410 California Street, NW twitter.com/SLOembassyUSA Washington, D.C. 20008, USA T: +1 202 386 66 01 E: [email protected] facebook.com/SLOembassyUSA washington.embassy.si Ambassador Kirn and Ambassador Ghafari with Governor of Michigan Richard Dale Snyder, Consul General Jure Žmauc and participants of the business meeting. -
Entwurf Des Maßnahmenprogramms Für Den Bayerischen Anteil Am Flussgebiet Donau
Entwurf des Maßnahmenprogramms für den bayerischen Anteil am Flussgebiet Donau Bewirtschaftungszeitraum 2016–2021 Dokument zur Information und Anhörung der Öffentlichkeit Die Europäische Wasserrahmenrichtlinie und ihre Umsetzung in Bayern 1 Einführung Die Europäische Wasserrahmenrichtlinie verpflichtet die Mitgliedstaaten, für jede Flussgebietseinheit oder für den in ihr Hoheitsgebiet fallenden Teil einer internationalen Flussgebietseinheit ein Maßnahmenprogramm festzulegen, um die Ziele des Art. 4 WRRL zu verwirklichen. Explizit sind für Wasserkörper, die laut Risikoanalyse die Umweltziele gemäß WRRL bis 2021 voraussichtlich nicht erreichen, geeignete Maßnahmen vorzusehen bzw. die Inanspruchnahme von Ausnahmen nach Artikel 4 (4)/(5) WRRL zu prüfen. Der sachliche Inhalt des Maßnahmenprogramms sowie zugehörige Fristen werden durch Art. 11 WRRL bzw. § 82 Abs. 2 bis 6 WHG sowie § 84 WHG festgelegt. Der Begriff Maßnahme ist in der WRRL weit gefasst und umfasst nicht nur technische Maßnahmen, sondern auch rechtliche, administrative, ökonomische, kooperative, kommunikationsbezogene und sonstige Instrumente, die der Umsetzung der Richtlinie dienen. Grundsätzlich enthält das Maßnahmenprogramm folgende Arten von Maßnahmen (vgl. Art. 11 Abs. 3–5 WRRL): • Grundlegende Maßnahmen sind zu erfüllende Mindestanforderungen an den Gewässerschutz, die sich aus der Umsetzung bestehender gemeinschaftlicher, nationaler oder landesspezifischer Gesetzgebung – unabhängig von der WRRL – ableiten; • Ergänzende Maßnahmen sind Maßnahmen, die zusätzlich zu den grundlegenden -
Slovenian Alps
SLOVENIAN ALPS Mangart, Photo by Bor Rojnik Slovenian Alps are truly remarkable, easily discovered by road as well as by trails suitable for hikers and cyclists. Marvellous panoramas, blooming meadows, alpine pastures and forests are surely never to be forgotten and are one of the most fascinating tourist spots in Slovenia. The high summits of the Julian Alps, the Karavanken chain and the Kamnik-Savinja Alps, open up amazing panoramas of the surrounding territory. It is hardly to find such a blooming meadows, alpine pastures and forests, elsewhere in the world within easy reach. The Julian Alps are a mountain range of the great Alps that stretches from northeastern Italy to Slovenia. They cover an estimated 4400 km², of which 1542 km² lies in Slovenia, and rise to 2,864 m at Mount Triglav, the highest peak in Slovenia. The entire mountain range constitutes about 150 mountains and is divided into two sections - the Western Julian Alps and the Eastern Julian Alps. 1 The Triglav National Park, boasting a number of peculiarities, is the largest and the earliest protected natural heritage site in the country. It is located in the north-west of Slovenia, more precisely in the Julian Alps. The park was named after the highest mountain of Slovenia, the Triglav, which is located nearly at the center of the park. It is the only National Park in Slovenia and among the earliest European parks. Pokljuka, is the southernmost highland marsh in Europe and a natural habitat of sphagnum moss. Near Kranjska Gora you can find nature reserve, the Zelenci, whom lakes provide Sava Dolinka with its source. -
Geological Excursion BASE-Line Earth
Geological Excursion BASE-LiNE Earth (Graz Paleozoic, Geopark Karavanke, Austria) 7.6. – 9.6. 2016 Route: 1. Day: Graz Paleozoic in the vicinity of Graz. Devonian Limestone with brachiopods. Bus transfer to Bad Eisenkappel. 2. Day: Visit of Geopark Center in Bad Eisenkappel. Walk on Hochobir (2.139 m) – Triassic carbonates. 3. Day: Bus transfer to Mezica (Slo) – visit of lead and zinc mine (Triassic carbonates). Transfer back to Graz. CONTENT Route: ................................................................................................................................... 1 Graz Paleozoic ...................................................................................................................... 2 Mesozoic of Northern Karavanke .......................................................................................... 6 Linking geology between the Geoparks Carnic and Karavanke Alps across the Periadriatic Line ....................................................................................................................................... 9 I: Introduction ..................................................................................................................... 9 II. Tectonic subdivision and correlation .............................................................................10 Geodynamic evolution ...................................................................................................16 Alpine history in eight steps ...........................................................................................17 -
The Marano and Grado Lagoon
The Marano and Grado lagoon THE MARANO AND GRADO LAGOON Annalisa Falace 1, Adriano Sfriso 2, Daniele Curiel 3, Giorgio Mattassi 4, Floriana Aleffi 4 1 Dipartimento di Scienze della Vita, Università di Trieste 2 Dipartimento di Scienze Ambientali, Università di Venezia 3 SELC-Coop. Soc., Venezia 4 ARPA Friuli-Venezia Giulia, Palmanova (UD) Riassunto La Laguna di Marano e Grado é parte del sistema deltizio lagunare del Nord Adriatico. È localizzata tra il fiume Isonzo ad Est ed il Tagliamento ad Ovest ed ha una superficie di circa 160 km2. I principali studi condotti sui due bacini riguardano aspetti idro-geo-sedimentologici, comunità macrozoobentoniche ed acquicoltura, mentre pochi sono i dati disponibili relativamente alle macroalghe ed alle fanerogame. I dati quali-quantitativi sulle macroalghe che vengono qui riportati si riferiscono principalmente a studi condotti negli anni 1992-93 sui substrati mobili dei due bacini. Sia i dati floristici che quelli quantitativi hanno evidenziato la dominanza di popolamenti a bassa diversità di Ulvales e Gracilariopsis longissima. Sono state riportate quattro specie di fanerogame, Cymodocea nodosa, Nanozostera noltii, Zostera marina e Ruppia maritima. Più di recente, nel luglio 2007, le macrofite bentoniche sono state raccolte in 19 stazioni al fine sia di aggiornare l’informazione esistente sulla flora e sulla vegetazione dei due bacini sia di stabilire il loro Stato Ecologico (SE) secondo quanto previsto dalla WFD (2000/60/EC). Il confronto con i dati precedenti evidenzia la riduzione sia del ricoprimento che della biomassa delle macrofite, in particolare dei popolamenti ad Ulvales, ed un incremento della ricchezza specifica. Ciononostante, poiché non sono disponibili dati storici sulle macrofite bentoniche della laguna di Marano e Grado, sono necessari ulteriori indagini su scale spaziali differenti per valutare meglio la dinamica e le caratteristiche biologiche di questi bacini. -
High-Mountain Permafrost in the Austrian Alps (Europe)
HIGH-MOUNTAIN PERMAFROST IN THE AUSTRIAN ALPS (EUROPE) Gerhard Karl Lieb Institute of Geography University of Graz Heinrichstrasse 36 A-8010 Graz e-mail: [email protected] Abstract Permafrost research in the Austrian Alps (Eastern Alps) is based on a variety of methods, including at large scales, the measurement of the temperature of springs and of the base of winter snow cover, and at small scales, mainly an inventory of some 1450 rock glaciers. Taking all the information available into consideration, the lower limit of discontinuous permafrost is situated near 2500 m in most of the Austrian Alps. These results can be used for modelling the permafrost distribution within a geographical information system. Detailed investi- gations were carried out in the Doesen Valley (Hohe Tauern range) using additional methods, including several geophysical soundings. In this way, realistic estimates of certain permafrost characteristics and the volume of a large active rock glacier (some 15x106m3) were possible. This rock glacier has been chosen as a monitoring site to observe the effects of past and future climatic change. Introduction snow cover (BTS) and geophysical soundings, such as seismic, geoelectric, electromagnetic and ground pene- Although mountain permafrost in the Austrian Alps trating radar surveys have been published (survey and has caused construction problems and damage to buil- references in Lieb, 1996). The best results for mapping dings at several high-altitude locations, specific investi- the mere existence of permafrost were obtained by mea- gations of permafrost did not start until 1980. Since suring spring temperatures and BTS, both procedures then, studies of the distribution and certain characteris- being easily applicable and providing quite accurate tics of permafrost have been carried out at a number of interpretation. -
The Drava River and the Pohorje Mountain Range (Slovenia): Geomorphological Interactions
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Mitteilungen des naturwissenschaftlichen Vereins für Steiermark Jahr/Year: 2005 Band/Volume: 134 Autor(en)/Author(s): Sölva Helmuth, Stüwe Kurt, Strauss Phillip Artikel/Article: The Drava River and the Pohorje Mountain Range (Slovenia): Geomorphological Interactions. 45-55 © Naturwissenschaftlicher Verein für Steiermark; download unter www.biologiezentrum.at Mitt. naturwiss. Ver. Steiermark Band 134 S. 45–55 Graz 2005 The Drava River and the Pohorje Mountain Range (Slovenia): Geomorphological Interactions By Helmuth Sölva 1, Kurt Stüwe1 & Phillip Strauss2 With 6 figures Accepted on November, 16th, 2004 Zusammenfassung: Die Drau und das Bacher Gebirge in Slowenien: Geomorphologische Zusammenhänge. − In dieser geomorphologisch-tektonischen Studie untersuchen wir die domartige Struktur des slowenischen Bacher Gebirges (Pohorje) und seine Interaktion mit einem der bedeutendsten Flüsse der Alpen, der Drau. Geologisch befindet sich das Bacher Gebirge am südwestlichen Rand des steirischen Beckens und nahe einer tektonisch sehr aktiven Zone der Europäischen Alpen: das Periadri- atische Lineament. Etwa 10 km nordwestlich des Bacher Gebirges verlässt die Drau das Miozän-Pliozäne Klagenfurter Becken und verändert ihre Fliessrichtung von Ost nach Süd, der Lavanttal/Labot-Störung folgend. Am Nordwesteck der Antiform des Bacher Gebirges wird die Drau wieder in eine Ost-Richtung abgelenkt, anstatt dem tektonischen und geomorphologischen Lineament der Lavanttal-Störung weiter nach SE zu folgen. Ab diesem Knick fliesst die Drau parallel zur Längsachse durch den Dom nach Osten. Ge- omorphologische und sedimentologische Hinweise zeigen, dass das Flusstales der Drau im zentralen Bereich des Gebirges um 1 km nach Norden an seine heutige Position verlagert worden ist. -
LEGRAD, V2 0 0 0 0 5 5 1 1 3 3 1 1 5 5 LEGRAD - CROATIA Flood - 14/09/2014 N " 0 '
639000 640500 642000 643500 645000 646500 648000 649500 651000 16°48'0"E 16°49'0"E 16°50'0"E 16°51'0"E 16°52'0"E 16°53'0"E 16°54'0"E 16°55'0"E 16°56'0"E 16°57'0"E 16°58'0"E GLIDE number: N/A Activation ID: EMSR-101 Product N.: 03LEGRAD, v2 0 0 0 0 5 5 1 1 3 3 1 1 5 5 LEGRAD - CROATIA Flood - 14/09/2014 N " 0 ' 9 Delineation Map - Overview 1 ° 6 4 Production date: 18/09/2014 Austria Hungary N " 0 ' Slovenia 9 Serbia 1 Zagreb ° ^ 6 4 Bosnia Zala and Herzegovina Mur Nyugat-Dunantul Adriatic Sea Croatia Montenegro ! Medjimurska Italy 0 0 Somogy 0 0 0 0 zupanija 0 0 3 3 1 1 Drau 5 5 Legrad !( Del-Dunantul Koprivnicko-krizevacka zupanija N " 0 ' 8 Sjeverozapadna 1 ° 6 4 Hrvatska N " 0 ' 8 !( 1 ° Cartographic Information 6 4 1:20000 Full color ISO A1, low resolution (100 dpi) 0 ! 0 0 0 5 5 0 0,5 1 2 8 8 2 2 km 1 1 5 5 Grid: W GS 1984 UTM Zone 33N map coordinate system Tick marks: WGS 84 geographical coordinate system ± Legend Crisis Information Hydrology Flooded Area (18/09/2014) River General Information Stream Area of Interest N Canal " 0 ' 7 1 Settlements ! ° 6 Ditch 4 ! Populated Place Lake N " Residential 0 ' 7 0 0 River 1 0 0 ° 6 0 0 Agricultural 4 7 7 2 2 1 1 5 5 Cemetery Green Area Recreational Urbanized Multi-functional ! N " 0 0 0 ' 6 0 0 1 ° 5 5 6 5 5 4 2 2 Map Information 1 1 5 5 Due to severe raining in last days, extremely high water level is recorded on almost all rivers N in the northern part of Croatia. -
The ALPS in 25 MAPS Imprint
The ALPS in 25 MAPS Imprint Editor: Coordination: Permanent Secretariat of the Alpine Convention Marianna Elmi (Permanent Secretariat of the Alpine Convention) Thomas Streifeneder (Institute for Regional Development, Eurac Research) Editing: Marianna Elmi Cartographic coordination: Elisa Ravazzoli (Institute for Regional Development, Eurac Research) Contributors: Marianna Elmi (Permanent Secretariat of the Alpine Convention) Thomas Streifeneder, Elisa Ravazzoli, Peter Laner (Institute for Regional Development, Eurac Research) Marcello Petitta, Kathrin Renner (Institute for Earth Observation, Eurac Research) Giulia Garegnani, Valentina D’Alonzo (Institute for Renewable Energy, Eurac Research) Alice Brambilla, Bruno Bassano (Alpine Wildlife Research Centre, Gran Paradiso National Park, IT) and Main office: Achaz von Hardenberg (Conservation Biology Research Group, Department of Biological Sciences, University of Chester, UK) Herzog-Friedrich-Straße 15 Dominik Cremer-Schulte, Maša Klemenčič (ALPARC) A-6020 Innsbruck Austria In cooperation with Branch office: English revision: iui – innsbruck university innovations Viale Druso - Drususallee 1 I-39100 Bolzano - Bozen Graphic design: De Poli e Cometto - Printing: Stampatori della Marca - Cover photo: Shutterstock Italy ISBN: 9788897500438 www.alpconv.org [email protected] Facebook: Alpine Convention © Permanent Secretariat Twitter: @alpconv of the Alpine Convention, 2018 ALPINE CONVENTION The ALPS in 25 MAPS Foreword The Alps belong to our collective imagination. It is virtually impossible to repercussions. Mapping these phenomena comes almost as a first instinct speak about the Alps without evoking specific memories of places, sounds and allows us to represent them in a simple, immediate way. It lets us and tastes in individuals with different experiences and perspectives. If interpret spatial impacts, sometimes down to a very fine level of detail. -
Evaluation of Wetlands and Floodplain Areas in the Danube River Basin Final Report May 1999
DANUBE POLLUTION REDUCTION PROGRAMME EVALUATION OF WETLANDS AND FLOODPLAIN AREAS IN THE DANUBE RIVER BASIN FINAL REPORT MAY 1999 Programme Coordination Unit UNDP/GEF Assistance prepared by WWF Danube-Carpathian-Programme and WWF-Auen-Institut (Germany) DANUBE POLLUTION REDUCTION PROGRAMME EVALUATION OF WETLANDS AND FLOODPLAIN AREAS IN THE DANUBE RIVER BASIN FINAL REPORT MAY 1999 Programme Coordination Unit UNDP/GEF Assistance prepared by WWF Danube-Carpathian-Programme and WWF-Auen-Institut (Germany) Preface The "Evaluation of Wetlands and Flkoodplain Areas in the Danube River Basin" study was prepared in the frame of the Danube Pollution Reduction Programme (PRP). The Study has been undertaken to define priority wetland and floodplain rehabilitation sites as a component of the Pollution reduction Programme. The present report addresses the identification of former floodplains and wetlands in the Danube River Basin, as well as the description of the current status and evaluation of the ecological importance of the potential for rehabilitation. Based on this evaluation, 17 wetland/floodplain sites have been identified for rehabilitation considering their ecological importance, their nutrient removal capacity and their role in flood protection. Most of the identified wetlands will require transboundary cooperation and represent an important first step in retoring the ecological balance in the Danube River Basin. The results are presented in the form of thematic maps that can be found in Annex I of the study. The study was prepared by the WWF-Danube-Carpathian-Programme and the WWF-Auen-Institut (Institute for Floodplains Ecology, WWF-Germany), under the guidance of the UNDP/GEF team of experts of the Danube Programme Coordination Unit (DPCU) in Vienna, Austria.