Aquatic Molluscs of the Mrežnica River
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Plitvice Lakes National Park, 96 Pp; I
WORLD HERITAGE NOMINATION - IUCN TECHNICAL EVALUATION PLITVICE LAKES EXTENSION (CROATIA) 1. DOCUMENTATION i) IUCN/WCMC Data Sheet: ii) Literature consulted: S. Bozicevic. (undated) The Plitvice Lakes, Plitvice Lakes National Park, 96 pp; I. Pevalak. 1968. The biodynamics of the Lakes of Plitvice and their protection; S. Bozicevic (ed). 1998. The Plitvice Lakes National Park – Natural History, Guide, Photomonography 96pp, Plitvice Lakes National Park; M. Schneider-Jacoby. 1996. A view from abroad: Nature Preservation in Croatia – An investment in the future of the country, Turizam Vol 44, No 11/12; B. Stilinovic and S. Bozicevic. 1988. The Plitvice Lakes – A natural phenomenon in the middle of the Dinaric Karst in Croatia, European Water Management, Vol 1, No 1. iii) Consultations: three external reviewers; Ministry of Environmental Protection and Physical Planning, Zagreb; Plitvice Lakes National Park, Plitvicka Jezero. iv) Field Visit: Michael Smart, March, 2000. 2. SUMMARY OF NATURAL VALUES The area inscribed on the World Heritage List in 1979 as Plitvice Lakes National Park (PLNP) covered 19,462ha. In 1997, the area of the National Park was extended by the Croatian Parliament to 29,482ha. The Croatian authorities have now proposed that the World Heritage site be extended to include this enlargement of the park by 10,020ha. PLNP is situated in the karst area of Croatia. It consists of a series of lakes in the valley of the Bijela rijeka (White River) and Crna rijeka (Black River), which join to become the Korana River, which flows into the River Kupa and eventually into the River Sava. The lakes are formed by barriers of travertine (or tufa) across the valley which create deep highly oligotrophic lakes. -
Article N° 09 Conf. CM², Split, Croatie, 2017
Conférence Méditerranéenne Côtière et Maritime EDITION 4, SPLIT, CROATIA (2017) Coastal and Maritime Mediterranean Conference Disponible en ligne – http://www.paralia.fr – Available online Adriatic karstic estuaries, their characteristics and evolution Mladen JURAČIĆ 1 1. University of Zagreb, Faculty of Science, Department of Geology, Horvatovac 102a, 10 000 Zagreb, Croatia. [email protected] Abstract: The coastal area of the eastern Adriatic is characterized with a prevalence of carbonate rocks and well-developed karst. Present freshwater input into the Adriatic is quite large, mostly through coastal and submarine springs. However, there are also a number of rivers debouching in the Adriatic from the eastern coast. Most of them have canyon like fluviokarstic valleys that were carved dominantly during Pleistocene and were drowned during post-LGM sea-level rise forming estuaries. These estuaries are filled to a different extent during Holocene highstand (last 7.500 years). The intraestuarine delta progradation is rather different in those estuaries depending on the quantity of the river- borne material. Human impact on progradation rate in some of the estuaries has been shown. Keywords: Estuaries, Sedimentation, Intraestuarine delta, Progradation, Allogenic river, Anthopo- genic influence. https://dx.doi.org/10.5150/cmcm.2017.009 45 Mediterranean rocky coasts: Features, processes, evolution and problems 1. Introduction Eastern Adriatic coastal area is formed predominantly in Mesozoic carbonate rocks with well-developed karst (PIKELJ & JURAČIĆ, 2013). Due to prevalent humid climatic conditions and karst maturation present freshwater input into the Adriatic is large, mostly through coastal and submarine springs (vruljas). However, there are also a number of rivers debouching into the Adriatic. -
A Conservation Palaeobiological Approach to Assess Faunal Response of Threatened Biota Under Natural and Anthropogenic Environmental Change
Biogeosciences, 16, 2423–2442, 2019 https://doi.org/10.5194/bg-16-2423-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. A conservation palaeobiological approach to assess faunal response of threatened biota under natural and anthropogenic environmental change Sabrina van de Velde1,*, Elisabeth L. Jorissen2,*, Thomas A. Neubauer1,3, Silviu Radan4, Ana Bianca Pavel4, Marius Stoica5, Christiaan G. C. Van Baak6, Alberto Martínez Gándara7, Luis Popa7, Henko de Stigter8,2, Hemmo A. Abels9, Wout Krijgsman2, and Frank P. Wesselingh1 1Naturalis Biodiversity Center, P.O. Box 9517, 2300 RA Leiden, the Netherlands 2Palaeomagnetic Laboratory “Fort Hoofddijk”, Faculty of Geosciences, Utrecht University, Budapestlaan 17, 3584 CD Utrecht, the Netherlands 3Department of Animal Ecology & Systematics, Justus Liebig University, Heinrich-Buff-Ring 26–32 IFZ, 35392 Giessen, Germany 4National Institute of Marine Geology and Geoecology (GeoEcoMar), 23–25 Dimitrie Onciul St., 024053 Bucharest, Romania 5Department of Geology, Faculty of Geology and Geophysics, University of Bucharest, Balcescu˘ Bd. 1, 010041 Bucharest, Romania 6CASP, West Building, Madingley Rise, Madingley Road, CB3 0UD, Cambridge, UK 7Grigore Antipa National Museum of Natural History, Sos. Kiseleff Nr. 1, 011341 Bucharest, Romania 8NIOZ Royal Netherlands Institute for Sea Research, Department of Ocean Systems, 1790 AB Den Burg, the Netherlands 9Department of Geosciences and Engineering, Delft University of Technology, Stevinweg 1, 2628 CN Delft, the Netherlands *These authors contributed equally to this work. Correspondence: Sabrina van de Velde ([email protected]) and Elisabeth L. Jorissen ([email protected]) Received: 10 January 2019 – Discussion started: 31 January 2019 Revised: 26 April 2019 – Accepted: 16 May 2019 – Published: 17 June 2019 Abstract. -
Review of Research on Plitvice Lakes, Croatia in the Fields of Meteorology, Climatology, Hydrology, Hydrogeochemistry and Physical Limnology
GEOFIZIKA VOL. 35 2018 DOI: 10.15233/gfz.2018.35.9 Review paper Review of research on Plitvice Lakes, Croatia in the fields of meteorology, climatology, hydrology, hydrogeochemistry and physical limnology Zvjezdana Bencetić Klaić 1, Josip Rubinić 2 and Sanja Kapelj 3 1 Department of Geophysics, Faculty of Science, University of Zagreb 2 Faculty of Civil Engineering, University of Rijeka 3 Faculty of Geotehnical Engineering, University of Zagreb Received 16 April 2018, in final form 22 October 2018 In lakes, several physical, chemical, and biological processes occur simulta- neously, and these processes are interconnected. Therefore, the investigation of lakes requires a multidisciplinary approach that includes physics (including the physics of the atmosphere, i.e., meteorology), chemistry, geology, hydrogeology, hydrology and biology. Each of these disciplines addresses a lake from a different point of view. However, lake studies that primarily belong to one field, at least to some extent, report their findings in ways that are associated with other fields; this type of reporting is caused by the inherent interconnections between phe- nomena from different disciplines. Plitvice Lakes, Croatia, are composed of a unique cascading chain of karst lakes, and these lakes have been investigated by numerous authors. Here, we provide an overview of the studies of the Plitvice Lakes Area (PLA) that address meteorology, climatology, hydrology, hydrogeo- chemistry and physical limnology. Our aim is to synthesize the results from each of these disciplines and make them available to scientists from other related disciplines; thus, this review will facilitate further investigations of the PLA within the natural sciences. In addition, valuable results from early investiga- tions of Plitvice Lakes are generally unavailable to the broader scientific com- munity, and are written in Croatian. -
Groundwater Bodies at Risk
Results of initial characterization of the groundwater bodies in Croatian karst Zeljka Brkic Croatian Geological Survey Department for Hydrogeology and Engineering Geology, Zagreb, Croatia Contractor: Croatian Geological Survey, Department for Hydrogeology and Engineering Geology Team leader: dr Zeljka Brkic Co-authors: dr Ranko Biondic (Kupa river basin – karst area, Istria, Hrvatsko Primorje) dr Janislav Kapelj (Una river basin – karst area) dr Ante Pavicic (Lika region, northern and middle Dalmacija) dr Ivan Sliskovic (southern Dalmacija) Other associates: dr Sanja Kapelj dr Josip Terzic dr Tamara Markovic Andrej Stroj { On 23 October 2000, the "Directive 2000/60/EC of the European Parliament and of the Council establishing a framework for the Community action in the field of water policy" or, in short, the EU Water Framework Directive (or even shorter the WFD) was finally adopted. { The purpose of WFD is to establish a framework for the protection of inland surface waters, transitional waters, coastal waters and groundwater (protection of aquatic and terrestrial ecosystems, reduction in pollution groundwater, protection of territorial and marine waters, sustainable water use, …) { WFD is one of the main documents of the European water policy today, with the main objective of achieving “good status” for all waters within a 15-year period What is the groundwater body ? { “groundwater body” means a distinct volume of groundwater within an aquifer or aquifers { Member States shall identify, within each river basin district: z all bodies of water used for the abstraction of water intended for human consumption providing more than 10 m3 per day as an average or serving more than 50 persons, and z those bodies of water intended for such future use. -
ACTIVE FLOOD DEFENCE in CROATIA: Regulatory Framework, Roles & Responsibilities
Workshop on Flood Risk Management measures & links to EU WFD November 11-12, 2015, Zagreb, Croatia ACTIVE FLOOD DEFENCE IN CROATIA: regulatory framework, roles & responsibilities Zoran Đurokovi ć, M.Sc.C.E. Croatian Waters Main Flood Protection Centre Head of Main Centre ∗ Climate change has intensified in recent years worldwide, including Croatia ∗ Extremely dry and wet periods have been alternating frequently in the last approximately 15 years ∗ Damage from extreme hydrological events is increasing ∗ “Average” or “normal” years are becoming increasingly rarer ∗ The frequency of high water waves and extreme water levels including floods is increasing ∗ There are almost no longer any rules concerning the occurrence of high water waves ∗ Forecasting climate models indicate increasingly frequent extreme climate events, both globally and locally ∗ Only in the last 15 years or so, the major part of the Croatian territory has experienced frequent extreme hydrological events which caused droughts in the years 2000, 2003, 2011 and 2012, but also floods in the years 2002, 2004, 2005, 2006, 2009, 2010, 2012, 2013, 2014 and 2015 ∗ Heavy damage is recorded, primarily in agriculture, but settlements, infrastructure and industrial facilities are also at risk ∗ Still, unlike in many other countries, major fatalities and disastrous damage in the urban areas have been avoided in Croatia ∗ Floods are natural phenomena which cannot be completely prevented. However, flood risks can be reduced to an acceptable level through constant development of flood -
Karta – Nordijsko Hodanje I Pješačenje
Begovo Brdo Begovo Brdo Snos Polojski Varoš Batnoga Donja Glina Ponor Snos Polojski Varoš [email protected] WWW.TZ-SLUNJ.HR | SL6A Batnoga KUPALIŠTE Donja Glina Ponor TEL. 047/777-630 TEL. SLUNJ 47240 7, RADIĆ BRAĆE ULICA | Kutanja JEZERO Cetingrad TOURIST OFFICE SLUNJ OFFICE TOURIST TURISTIČKA ZAJEDNICA GRADA SLUNJA GRADA ZAJEDNICA TURISTIČKA SL6A GRADA SLUNJA GRADA TURISTIČKA ZAJEDNICA TURISTIČKA KUPALIŠTE Kutanja Delić Poljana KUPALIŠTE TC MIRJANA JEZERO Cetingrad KARAČA SL6 CT1 Delić Poljana SL5 KUPALIŠTE GlinskoTC MIRJANAVrelo KARAČA D1 SL6B CRKVA Donji Nikšić SV. NIKOLE SL6 CT1 KOSOVI Donji Cerovac SL5 Glinsko Vrelo MLINOVI Strmačka D1 SL6B CRKVA Gornja Glina SV. NIKOLE KOSOVI Donji Nikšić Donji Cerovac RESTORAN Gornji Cerovac Strmačka PINO MLINOVI Gornja Glina STARI GRAD Gornji Nikšić CETIN RESTORAN Gornji Cerovac MarindolskoPINO Gornje Podcetin NERALIĆ Brdo MLIN Tatar Varoš Gnojnice STARI GRAD SL7 Gornji Nikšić CETIN GRŽANOVE Cvitović Marindolsko Cetinska Varoš Gornje Podcetin LUKE D1 NERALIĆ Brdo MLIN Tatar Varoš Gnojnice Donji Kremen SL7 Gnojnice Bilo GRŽANOVE Cvitović Zečev Varoš Gornje LUKEMali Vuković D1 Cetinska Varoš Taborište Miljevac Donje Donji Kremen Gnojnice Bilo Taborište Sadikovac Zečev Varoš Gornje MaliDonje Vuković Gnojnice Taborište Donje Miljevac SL8 SL1 Taborište KUPALIŠTE Kapljuv Sadikovac Gornji Kremen GNOJNICE Donje Gnojnice Rastoke SL2 KUPALIŠTE KUTEREVČEVA CT2 KOTLAC PEĆINA SALOPEK SL8 MLINSL1 KUPALIŠTE Kapljuv Gornji Kremen Kestenje GNOJNICE Rastoke SLUNJ SL2 KUPALIŠTE KUTEREVČEVA CT2 KOTLAC PEĆINA SALOPEK MLIN Kestenje MATEŠIĆEVA PEĆINA SL3 SLUNJ Lađevačko Srednje Selo Podmelnica Selište SLUNJ RASTOKE RUTA BR. / ROUTE NO. 1 Dubrava Rastočka rapsodija | Rastoke Rhapsody MATEŠIĆEVA ID: SL1 | D: 2.4 km PEĆINA SL3 Luke Gornji Popovac Lađevačko KARTA ZA NORDIJSKO HODANJE I PJEŠAČENJE | NORDIC WALKING AND HIKING D1 RUTA BR. -
Diversity of Alien Macroinvertebrate Species in Serbian Waters
water Article Diversity of Alien Macroinvertebrate Species in Serbian Waters Katarina Zori´c* , Ana Atanackovi´c,Jelena Tomovi´c,Božica Vasiljevi´c,Bojana Tubi´c and Momir Paunovi´c Department for Hydroecology and Water Protection, Institute for Biological Research “Siniša Stankovi´c”—NationalInstitute of Republic of Serbia, University of Belgrade, Bulevar despota Stefana 142, 11060 Belgrade, Serbia; [email protected] (A.A.); [email protected] (J.T.); [email protected] (B.V.); [email protected] (B.T.); [email protected] (M.P.) * Correspondence: [email protected] Received: 29 September 2020; Accepted: 7 December 2020; Published: 15 December 2020 Abstract: This article provides the first comprehensive list of alien macroinvertebrate species registered and/or established in aquatic ecosystems in Serbia as a potential threat to native biodiversity. The list comprised field investigations, articles, grey literature, and unpublished data. Twenty-nine species of macroinvertebrates have been recorded since 1942, with a domination of the Ponto-Caspian faunistic elements. The majority of recorded species have broad distribution and are naturalized in the waters of Serbia, while occasional or single findings of seven taxa indicate that these species have failed to form populations. Presented results clearly show that the Danube is the main corridor for the introduction and spread of non-native species into Serbia. Keywords: Serbia; inland waters; allochthonous species; introduction 1. Introduction The Water Framework Directive (WFD) [1] represents key regulation and one of the most important documents in the European Union water legislation since it was adopted in 2000. -
Case Study of Kupa River Watershed in Croatia
J. Hydrol. Hydromech., 67, 2019, 4, 305–313 DOI: 10.2478/johh-2019-0019 Long term variations of river temperature and the influence of air temperature and river discharge: case study of Kupa River watershed in Croatia Senlin Zhu1, Ognjen Bonacci2, Dijana Oskoruš3, Marijana Hadzima-Nyarko4*, Shiqiang Wu1 1 State Key Laboratory of Hydrology-Water resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, China. 2 Faculty of Civil Engineering and Architecture, University of Split, Matice hrvatske 15, 21000 Split, Croatia. 3 Meteorological and Hydrological Service, Gric 3, 10000 Zagreb, Croatia. 4 Josip Juraj Strossmayer University of Osijek, Faculty of Civil Engineering and Architecture Osijek, Vladimira Preloga 3, 31000 Osijek, Croatia. * Corresponding author. E-mail: [email protected] Abstract: The bio-chemical and physical characteristics of a river are directly affected by water temperature, which therefore affects the overall health of aquatic ecosystems. In this study, long term variations of river water temperatures (RWT) in Kupa River watershed, Croatia were investigated. It is shown that the RWT in the studied river stations in- creased about 0.0232–0.0796ºC per year, which are comparable with long term observations reported for rivers in other regions, indicating an apparent warming trend. RWT rises during the past 20 years have not been constant for different periods of the year, and the contrasts between stations regarding RWT increases vary seasonally. Additionally, multi- layer perceptron neural network models (MLPNN) and adaptive neuro-fuzzy inference systems (ANFIS) models were implemented to simulate daily RWT, using air temperature (Ta), flow discharge (Q) and the day of year (DOY) as predic- tors. -
Olm, Proteus Anguinus
Olm, Proteus anguinus Compiler: Jelić, D. Contributors: Jelić, D.; Jalžić, B.; Kletečki, E.; Koller, K.; Jalžić, V.; Kovač-Konrad, P. Suggested citation: Jelić, D. (2014): A survival blueprint for the olm, Proteus anguinus. Croatian Institute for Biodiversity, Croatian Herpetological Society, Zagreb, Croatia. 1. STATUS REVIEW 1.1 Taxonomy: Chordata > Amphibia > Caudata > Proteidae > Proteus > anguinus Most populations are assigned to the subterranean subspecies Proteus anguinus anguinus. Unlike the nominate form, the genetically similar subspecies P.a. parkelj from Bela Krajina in Slovenia is pigmented and might represent a distinct species, although a recent genetic study suggests that the two subspecies are poorly differentiated at the molecular level and may not even warrant subspecies status (Goricki and Trontelj 2006). Isolated populations from Istria peninsula in Croatia are genetically and morphologically differentiated as separate unnamed taxon (Goricki and Trontelj 2006). Croatian: Čovječja ribica English: Olm, Proteus, Cave salamander French: Protee Slovenian: Čovješka ribica, močeril German: Grottenolm 1.2 Distribution and population status: 1.2.1 Global distribution: Country Population Distribution Population trend Notes estimate (plus references) (plus references) Croatia 68 localities (Jelić 3 separate Decline has been et al. 2012) subpopulations: observed through Istria, Gorski devastation of kotar and several cave Dalmatia systems in all regions (Jelić et al. 2012) Italy 29 localities (Sket Just the A decline has been 1997) easternmost observed in the region around population of Trieste, Gradisce Goriza (Italy) (Gasc and Monfalcone et al. 1997). Slovenia 158 localities 4 populations A decline has been (Sket 1997) distributed from observed in the Vipava river in the population in west (border with Postojna (Slovenia) Italy) to Kupa (Gasc et al. -
Session 4 SRB Assessment
Status of transboundary waters in South Eastern Europe Characterization Report on the Sava River Basin Dejan Komatina, Ph.D. Civ. Eng., Secretary, ISRBC General description of the basin • The Sava River Basin as a Danube sub-basin – Basin area: 95 720 km 2 (the second largest, after the Tisza basin) – Average flow (at the mouth): 1722 m 3/s (the largest tributary) – River length: 940 km (586 km of which were navigable before the war) Country Share of the Share of the basin (%) territory (%) Albania 0.1 0.5 Bosnia & Herzegovina 40 76 Croatia 26 45 Montenegro 7.5 52 Serbia 15.4 17 Slovenia 11 53 Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 2 Overview (location) of the SRB Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 3 Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 4 Values / uses / threats Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 5 Values / uses / threats Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 6 Values / uses / threats Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 7 Values / uses / threats Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 8 Values / uses / threats Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 9 Values / uses / threats Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 10 Land cover/land use in the SRB Land class % Artificial surfaces 2,23 Agricultural areas 42,36 Forests and semi natural areas 54,71 Wetland 0,08 Inland water 0,63 Int. -
The Morphological Plasticity of Theodoxus Fluviatilis (Linnaeus, 1758) (Mollusca: Gastropoda: Neritidae)
Correspondence ISSN 2336-9744 (online) | ISSN 2337-0173 (print) The journal is available on line at www.ecol-mne.com The morphological plasticity of Theodoxus fluviatilis (Linnaeus, 1758) (Mollusca: Gastropoda: Neritidae) PETER GLÖER 1 and VLADIMIR PEŠI Ć2 1 Biodiversity Research Laboratory, Schulstraße 3, D-25491 Hetlingen, Germany. E-mail: [email protected] 2 Department of Biology, Faculty of Sciences, University of Montenegro, Cetinjski put b.b., 81000 Podgorica, Montenegro. E-mail: [email protected] Received 19 January 2015 │ Accepted 3 February 2015 │ Published online 4 February 2015. Theodoxus fluviatilis is a widely distributed species, ranging from the Ireland (Lucey et al . 1992) to Iran (Glöer & Peši ć 2012). The records from Africa were considered as doubtful (Brown 2002), but recently the senior author found this species in Algeria (Glöer unpublished record). The species prefers the lowlands (in Switzerland up to 275 m a.s.l., Turner et al . 1998), and calcium-rich waters, living on hard benthic substrates, typically rocks. On the territory of the Central and Eastern Balkans three species are present (Markovi ć et al . 2014): Theodoxus fluviatilis (Linnaeus, 1758), T. danubialis (C. Pfeiffer, 1828) and T. transversalis (C.Pfeiffer, 1828). For Montenegro, Wohlberedt (1909), Karaman & Karaman (2007), Glöer & Peši ć (2008), and Peši ć & Glöer (2013) listed only Theodoxus fluviatilis . Figures 1-4. The operculum. 1: Theodoxus fluviatilis (Linnaeus, 1758); 2: T. danubialis (C. Pfeiffer, 1828); 3-4: Rib shield of T. fluviatilis . Abbreviations: ca = callus, eo = embryonic operculum, la = left adductor, p = peg, r = rib, ra = right adductor, rp = rib pit, rs = rib shield. The shell of adults of Theodoxus fluviatilis is 4.5–6.5 mm high and 6–9 mm broad, exceptionally up to 13 mm, and consists of 3–3.5 whorls, including protoconch, with a usually low spire.