Callinectes Sapidus Rathbun, 1896, After 70 Years from Its First Appearance in the Gulf of Trieste, Northern Adriatic Sea, Italy (Decapoda: Portunidae)

Total Page:16

File Type:pdf, Size:1020Kb

Callinectes Sapidus Rathbun, 1896, After 70 Years from Its First Appearance in the Gulf of Trieste, Northern Adriatic Sea, Italy (Decapoda: Portunidae) 12 6 2006 the journal of biodiversity data 2 December 2016 Check List NOTES ON GEOGRAPHIC DISTRIBUTION Check List 12(6): 2006, 2 December 2016 doi: http://dx.doi.org/10.15560/12.6.2006 ISSN 1809-127X © 2016 Check List and Authors The return of the Blue Crab, Callinectes sapidus Rathbun, 1896, after 70 years from its first appearance in the Gulf of Trieste, northern Adriatic Sea, Italy (Decapoda: Portunidae) Chiara Manfrin1*, Giovanni Comisso2, Andrea dall’Asta3, Nicola Bettoso4, and J. Sook Chung5 1 Department of Life Sciences, University of Trieste, via L. Giorgieri, 5, 34127, Trieste (Trieste), Italy 2 Riserva Naturale Regionale “Valle Canal Novo”, via delle Valli 2, 33050, Marano Lagunare (Udine), Italy 3 Civico Aquario Marino, Molo Pescheria, 2, 34123, Trieste (Trieste), Italy 4 Agenzia Regionale per la Protezione dell’Ambiente del Friuli Venezia Giulia, via A. La Marmora, 13, 34139 Trieste, Italy 5 Institute of Marine and Environmental Technology, University of Maryland Center for Environmental Science, 701 East Pratt Street Baltimore, MD 21202, USA * Corresponding author E-mail: [email protected] Abstract: Since August 2015, an increasing number al. 2000), Russia (Azov Sea) (Diripasko et al. 2009; of Blue Crabs, Callinectes sapidus Rathbun, 1896, have Pashkov et al. 2012), Ukraine (Monin 1984), and Georgia been reported in the Marano and Grado Lagoon, Gulf (Shaverdashvili and Ninua 1975). Records are being of Trieste, in the northern Adriatic Sea. This species is continuously updated, and the most recent sighting was not a new introduction and in fact the first record of C. off Turkey (Yağlıoğlu et al. 2014). sapidus in Italy and the entire Adriatic Sea dates back Callinectes sapidus reached the Mediterranean basin in to 1949 in the Grado Lagoon. Interestingly, no other ships’ ballast tanks (Holthuis and Gottlieb 1955), but the records of C. sapidus have been reported since the first timing is unknown (Castriota et al. 2012). This species record. Here, we note the re-appearance of C. sapidus in was in fact often mistaken for Portunus segnis (Forskål, the Gulf of Trieste. 1775) and often had been called Neptunus pelagicus or P. pelagicus (Linnaeus, 1758) until the P. pelagicus species Key words: invasive species; re-appearance; Marano complex was revised (Lai et al. 2010). and Grado Lagoon; Adriatic Sea Callinectes sapidus was reported from the Ebro delta, Spain (Tuncer 2008) and Guadalquivir, southern Ibe- ria (Cabal et al. 2006), suggesting an active expansion The American Blue Crab, Callinectes sapidus Rathbun, of range of this species toward southern latitudes in 1896 (Decapoda: Portunidae) is a euryhaline and eury- estuaries (Ribeiro and Veríssimo 2014). In the Mediter- thermal invasive species in Europe. Its native range is ranean, C. sapidus is known from Malta (Sciberras and the western North Atlantic Ocean from Nova Scotia to Schembri 2007), the Ligurian Sea (Tortonese 1965; Argentina. However, during the last decade, its range Bisconti and Silvi 2005), the Aegian-Levantine Sea has expanded, either accidentally or deliberately, into basin (Serbetis 1959; Enzenrob et al. 1997; Zaitsev and both Asia and Europe (Galil 2000). The first record in Öztürk 2001), and the Ionian Sea (Molnar et al. 2008; Western Europe was from the Biscay Gulf, France, in the Thessalou-Legaki et al. 2012). early 20th century (Bouvier 1901). Since then, this spe- In the Adriatic Sea, C. sapidus was first recorded cies has been reported from the North Sea (Netherlands in 1949, as Neptunus pelagicus, from Grado Lagoon in 1932, Belgium in 1981, and Germany in 1965) (Den (Giordani Soika 1951). The correct identity was Hartog and Holthuis 1951; Kühl 1965; Adema 1991; established in 1993 following the discovery of two males Gollasch 1996) and in the Baltic Sea in 1951 (Denmark) in the Venice Lagoon in 1991 and 1992 (Mizzan 1993). (Wolff 1954; Knudsen 1989; Gollasch 1996). It has been Many records were reported from the Adriatic Sea, found along the coasts of Britain in 1982 (Clark 1984; along both western (Gennaio et al. 2006; Scaravelli and Minchin et al. 2013), Portugal (Gaudêncio and Guerra Mordenti 2007; Florio et al. 2008; Castriota et al. 2012; 1979), and Spain (Cabal et al. 2006). Mancinelli 2013; Cilenti et al. 2015; Manfrin et al. 2015) Starting in the late 1960s, C. sapidus was observed and eastern coasts (Tuncer 2008; Beqiraj and Kashta in Bulgaria (Black Sea) (Bulgurkov 1968; Petrescu et 2010; Dulčić et al. 2010; Dulčić et al. 2011). However, Check List | www.biotaxa.org/cl 1 Volume 12 | Number 6 | Article 2006 Manfrin et al. | The Blue Crab in the Northern Adriatic Sea Figure 1. Locations and year of first appearance of Callinectes sapidus in Europe and Italy. The literature on which this is based is cited in the text. no other C. sapidus have been collected from the Gulf identified in the state-sponsored ‘‘Natura 2000’’ survey of Trieste, until now. First records for C. sapidus in as a Site of Community Importance (SCIs IT3320037). European waters are summarized in Figure 1. The area is economically important, supporting tourism Here, we document the occurrence of C. sapidus in the and industry. There are recreational fisheries (mainly Gulf of Trieste, 66 years after the previous (and first) the Venerupis philippinarum [A.Adams & Reeve, 1850], record from the same area (Giordani Soika 1951). Manila Clam) and with fish farming (Acquavita et al. The Gulf of Trieste is divisible into two main sectors 2014). According to the Water Framework Directive that are separated by the Timavo River. The first sector 2000/60/EC, three main water types were identified in extends to the sandy Grado littoral zone at west, whereas the Marano and Grado Lagoon: mesohaline TME (5–20 the second sector extends from the Timavo River to the PSU), polyhaline TPO (20–30 PSU), and euhaline TEU Istrian littoral and is characterized by rocky coastline. (30–40 PSU) (Bettoso et al. 2010). The Gulf includes the Marano and Grado Lagoon. Five specimens of C. sapidus were collected between The Marano and Grado Lagoon is one of the most late August 2015 to September 2016 (Table 1) within the ecologically intact wetlands in the entire Mediterranean Marano and Grado Lagoon (Figure 2). area. The lagoon complex, between the deltas of the Collection of the specimens numbers 1, 2, 4, and Tagliamento and Isonzo rivers is approximately 32 5 (Table 1) was done using fyke nets with the help of km long, up to 5 km wide, and has an area of 160 km2. local anglers, A fyke net consists of a barrier of about The surrounding drainage basin (1,880 km2) delivers 60 m in length and 1.3 m in height, with a mesh size of important loads of both nutrients and pollutants (Covelli 1.6 cm, which leads fish and shrimp towards four cone- et al. 2012; Saccon et al. 2013). Since 1971, the lagoon shaped, unbaited traps also with the same mesh size. is protected by the Ramsar Convention. Following the This fishing gear, with the barriers set perpendicular implementation of the Habitats Directive (92/43/EC), to the tidal flow, takes advantage of tidal dynamics to which concerns the protection of biodiversity, it is also catch fish and shrimp (Malavasi et al. 2004). Specimen Table 1. Collection sites of each specimen, along with date of collection, size expressed as carapace width and sex. Voucher ID ZI-06635 is within the collection of the Museo Friulano di Storia Naturale of Udine (via Sabbadini, 32, 33100, Udine, Italy), while voucher ID c485 is stored and is part of the collection of the Civico Museo di Storia Naturale of Trieste (via dei Tominz, 4, 34139, Trieste, Italy). Pictures of each specimen are reported in Figure 3. Site no. Site Geographic coordinates Date collected Carapace width (mm) Sex Voucher Figure 1 Marano Lagoon 45.70° N, 013.11° E 27 August 2015 160 ♂ ZI-06635 Figure 3a 2 Marano Lagoon 45.70° N, 013.20° E 30 September 2015 176 ♀ — Figure 3b 3 Grado Lagoon 45.70° N, 013.35° E 29 October 2015 190 ♂ c485 Figure 3c 4 Marano Lagoon 45.70° N, 013.08° E 26 August 2016 177 ♂ — Figure 3d 5 Marano Lagoon 45.70° N, 013.20° E 9 September 2016 158 ♂ — Figure 3e Check List | www.biotaxa.org/cl 2 Volume 12 | Number 6 | Article 2006 Manfrin et al. | The Blue Crab in the Northern Adriatic Sea Figure 2 Map of the Gulf of Trieste showing collecting sites (white dots) for each of the five specimens (site numbers correspond to those in Table 1). number 3 was collected in water about 4 m deep by About 70 years ago one specimen of C. sapidus was mean of trammel net. found near Grado (Giordani Soika 1951). Subsequent to Specimens (Figure 3) were identified according to this record, no additional specimes of C. sapidus have Williams (1974) and Galil et al. (2002). We identified been found in the Gulf of Trieste until now. the species in loco and later one of us (JSC) confirmed According to the Harding’s (2003) classification, the identificiation using photographs. The carapace crabs can be divided into three size groups (small, CW width (CW, maximal distance between the posterior < 80 mm; medium, CW 80–120 mm; and large, CW > 120 anterolateral spines; Table1) and sex were recorded for mm) and our specimens are fit the large category. All the each specimen. Callinectes sapidus is characterized by an specimens were caught in water where salinity is greater intense blue color of the appendix. The remainder of the than 30. Dulčić et al. (2011) observed that populations exoskeleton is olive-brown. As with other portunid crabs, of C.
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Acrocephalus 30 140 02.Indd
    Acrocephalus 30 (140): 17−23, 2009 doi: 10.2478/v10100-009-0002-9 Interactions between fi sh resources and Cormorants Phalacrocorax carbo in the Grado and Marano lagoon (NE Italy) Interakcije med ribogojni{tvom in kormorani Phalacrocorax carbo v lagunah Grado in Marano (SV Italija) Mauro Cosolo, Paolo Utmar, Flavio Roppa & Stefano Sponza University of Trieste, Department of Life Sciences – CSEE (Centre of Etho-Ecological Studies), via Giorgieri 9, I–34127 Trieste, Italy, e–mail: [email protected]; [email protected]; roppafl [email protected]; [email protected] Th e aim of this study was to determine the importance of diff erent environments for Cormorant Phalacrocorax carbo biology in the Grado and Marano lagoon (Friuli Venezia Giulia, NE Italy, Upper Adriatic Sea), and to estimate the levels of fi sh removal within such areas. Data were collected on Cormorant abundance and the amount of fi sh consumed in two fi shing valli (Valle Noghera and Valle Artalina) and in three tidal areas (Goppion, Cavanata sea, Grado and Marano lagoon). Th e number of Cormorants per 100 ha was relatively low in all the study areas. Th e highest density of feeding cormorants in November (24 birds/100 ha) was in Valle Noghera. Th e latter is ascribed to an isolated event of 50 birds in social fi shing activity. During the rest of the November survey time (72% of the total), lower densities were noted (2.5 birds/100 ha). Fish consumption was also relatively low. In Valle Artalina the maximum was 6.8 kg/100 ha in December.
    [Show full text]
  • Recent Contamination of Mercury in an Estuarine Environment (Marano Lagoon, Northern Adriatic, Italy)
    Estuarine, Coastal and Shelf Science 82 (2009) 273–284 Contents lists available at ScienceDirect Estuarine, Coastal and Shelf Science journal homepage: www.elsevier.com/locate/ecss Recent contamination of mercury in an estuarine environment (Marano lagoon, Northern Adriatic, Italy) Stefano Covelli a,*, Alessandro Acquavita b, Raffaella Piani a, Sergio Predonzani b, Cinzia De Vittor c a Dipartimento di Scienze Geologiche, Ambientali & Marine, Universita` di Trieste, Via E. Weiss 2, 34127 Trieste, Italy b ARPA-FVG, Agenzia Regionale per la Protezione dell’Ambiente del Friuli-Venezia Giulia, Osservatorio Alto Adriatico, Via Cairoli 14, 33057 Palmanova (Udine), Italy c Dipartimento di Oceanografia Biologica, Istituto Nazionale di Oceanografia e Geofisica Sperimentale, Via A. Piccard 54, 34014 Trieste, Italy article info abstract Article history: The Marano Lagoon, in the northern Adriatic Sea (Italy), has been affected by mercury (Hg) contami- Received 9 October 2008 nation from industrial and mining activities. It has been estimated that 186,000 kg of Hg were deliber- Accepted 13 January 2009 ately discharged into the main drainage system (Aussa–Corno River) by a chlor-alkali plant (CAP) from Available online 31 January 2009 1940s to 1984. The lagoon has also experienced a secondary long-term Hg input, originated from mining activity in Idrija (Slovenia), due to the supply of fluvial suspended particles carried by the Isonzo River in Keywords: the Gulf of Trieste. Since local fishing activities are extensively conducted, there is great concern on the mercury risk posed by potentially harmful effects of Hg to the trophic chain. chlor-alkali À1 À1 estuary Present inputs of this metal, both in dissolved (52.4–4.1 ng L ) and particulate (130.8–3.4 ng L ) phases, biogeochemical cycling were preliminary investigated in the water column.
    [Show full text]
  • MAP Technical Reports Series No. 106 UNEP
    MEDITERRANEAN ACTION PLAN MED POL UNITED NATIONS ENVIRONMENT PROGRAMME FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS ASSESSMENT OF THE STATE OF EUTROPHICATION IN THE MEDITERRANEAN SEA EVALUATION DE L'ETAT DE L'EUTROPHISATION EN MER MEDITERRANEE by/par R.A. Vollenweider, A. Rinaldi, R. Viviani and E. Todini MAP Technical Reports Series No. 106 In cooperation with: En coopération avec: WHO/OMS UNEP Athens, 1996 Note: The designations employed and the presentation of the material in this document do not imply the expression of any opinion whatsoever on the part of UNEP, FAO or WHO concerning the legal status of any State, Territory, city or area, or of its authorities, or concerning the delimitation of their frontiers or boundaries. This document was prepared by Professor R.A. Vollenweider, National Water Research Institute Burlington, Canada; Dr. A. Rinaldi, Laboratory "M.N. Daphne", Region of Emilia-Romagna, Italy; Professor R. Viviani of the University of Bologna; and Professor E. Todini of the University of Bologna. The overall technical responsibility was entrusted to FAO (Responsible Officer: G.P. Gabrielides). Note: Les appelations employées dans ce document et la présentation des données qui y figurent n'impliquent de la part du PNUE, de la FAO ou de l'OMS, aucune prise de position quant au statut juridique des Etats, territoires, villes ou zones, ou de leurs autorités, ni quant au tracé de leurs frontières ou limites. Le présent document a été préparé par M. le Professeur R.A. Vollenweider, National Water Research Institute Burlington (Canada), M. A. Rinaldi, Laboratoire "M.N. Daphne", Région Emilie- Romagne (Italie), M.
    [Show full text]
  • Water Flow in the Inlets of the Marano-Grado Lagoon System (Ne Italy) 135
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Scientific Open-access Literature Archive and Repository IL NUOVO CIMENTO Vol. 36 C, N. 4 Luglio-Agosto 2013 DOI 10.1393/ncc/i2013-11548-8 Communications: SIF Congress 2012 Water flow in the inlets of the Marano-Grado lagoon system (NE Italy) ∗ I. Mancero-Mosquera( ) Istituto Nazionale di Oceanografia e di Geofisica Sperimentale - Trieste, Italy ricevuto il 25 Febbraio 2013 Summary. — Water flow in the inlets of Grado and Lignano of the Marano- Grado Lagoon system was measured between July 2010 and September 2011, to study the water exchange between the lagoon and the Adriatic Sea. The average magnitude of the flow is about 500 mm/s in Grado and 400 mm/s in Lignano. The tidal forcing accounts for about 90% of the variability, with the semi-diurnal M2 and S2 contributing over 75%. They behave almost in phase with Lignano leading Grado by about 20 seconds. K1, the strongest diurnal constituent, contributes 7.4% to the energy, and shows a phase difference of about 10 minutes with the Grado response leading Lignano. Adriatic Seiches are found with periodicities of 21.14, 10.92, 7.04, 5.24, 4.29 and 3.59 hours, accounting for most of the non-tidal energy. PACS 92.10.-c – Physical oceanography. PACS 92.10.Sx – Coastal, estuarine, and near shore processes. PACS 91.50.Cw – Beach and coastal processes. PACS 92.10.A- – Circulation and currents. 1. – Introduction The Marano-Grado Lagoon system is located in the northern shore of the Adriatic Sea (fig.
    [Show full text]
  • Integrated Monitoring Programme Albania
    Integrated Monitoring Programme Albania Logos en anglais, avec versions courtes des logos ONU Environnem ent et PAM La version longue des logos ONU Environnem ent et PAM doit être utilisée February 2021dans les docum ents ou juridique Ls.a v ersio ncour te des logos est destin e tous les produit sde com m unicati otonurn s vers le public. Impressum Lead Coordinator: Nada Krstulović Project team coordination: Zamir Dedej, Marina Marković, Anis Zarrouk, Ivan Sekovski, Rezart Kapedani, Daniel Cebrian Authors: EO1: Lefter Kashta, Ferdinand Bego, Enerit Sacdanaku, Ivan Guala, Draško Holcer, Yakup Kaska, Marco Zenatello EO2: Sajmir Beqiraj, Argyro Zenetos EO3: Rezart Kapedani, Anis Zarouk EO5: Arjana Ylli, Robert Precali EO7: Hamdi Beshku, Petrit Llaveshi, Olivier Brivois EO8: Odhise Zoto, Ivan Sekovski EO9: Edlira Baraj, Raimonda Lilo, Carlos Guitart EO10: Magdalena Cara, Eduart Cani, Christos Ioakemidis Maps: Robert Precali Editing: Cover design: swim2birds.co.uk Graphic design: Ljudomat Proofreading: Cakum-Pakum d.o.o. Cover photograph: Caretta caretta © SPA/RAC, Artescienza The designations employed and the presentation of the material in this document do not imply the expression of any opinion whatsoever on the part of UNEP/MAP concerning the legal status of the country, territory, city or area or its authorities, or concerning the delimitation of their frontiers or boundaries. This study was prepared by PAP/RAC, SPA/RAC, UNEP/MAP and the Ministry of Tourism and Environment with the National Agency for Protected Areas of Albania within the GEF Adriatic Project and supported by the Global Environment Facility (GEF). Document citation: UNEP/MAP-PAP/RAC-SPA/RAC, MET and NAPA (2021).
    [Show full text]
  • 5.1 Evolution of Italian Aquaculture Within the Mediterranean Region Cataudella S., Crosetti D
    Chapter 5 Aquaculture 5.1 Evolution of Italian aquaculture within the Mediterranean region Cataudella S., Crosetti D. Origins Italian marine aquaculture has ancient origins (Cataudella & Bronzi, 2001) and the richness of historical evidences, ancient manuscripts, mosaics and handicrafts from Etruscan and Ancient Roman time perfectly depict the attention dedicated to fish production in the history of the Mediterranean region. Italian aquaculture has grown as a highly diversified activity, thanks to the high environmental diversity that characterizes Italian landscape. Italian traditional marine fish culture was born in coastal lagoons and reached the most modern model in the north Adriatic valliculture in the late 1960s. The implementation of mass production techniques developed in the 1970s gave rise to modern marine fish culture in Italy (Ravagnan, 1978; 1992). Italian shellfish culture also originated in protected confined coastal areas, such as coastal lagoons, sheltered gulfs and harbours. Marine aquaculture started with the rearing of those species that naturally hung about in confined estuarine coastal areas, as they are able to withstand stress due to temperature and salinity variations. Such species, as European sea bass, gilthead sea bream and eels, showed to be more adapted to withstand handling by man, such as fry and juveniles collection, transport, grading, transfer to wintering ponds and from one pond to another, and culture in ponds. Tradition and market: a good starting point Italian contribution to modern marine aquaculture development has been fundamental for the ancient Italian tradition, both for the public commitment in sustaining development in this sector, and for the push of curious and passionate entrepreneurs. Italian role was also linked to the high demand of the national market interested in the production of European sea bass, gilthead sea breams and eels, species that have always been greatly appreciated in Italian fish markets, especially at Christmas time.
    [Show full text]
  • Raporti Vjetor 2011-Red.Pmd
    AKADEMIA E SHKENCAVE E SHQIPËRISË ACADEMY OF SCIENCES OF ALBANIA Raport VJETOR 2011 ANNUAL Report Tiranë, 2012 1 Përgatitur nga: Kryesia e Akademisë së Shkencave e Shqipërisë Seksioni i Shkencave Natyrore dhe Teknike Seksioni i Shkencave Shoqërore dhe Albanologjike Nën drejtimin e: Akad. Prof. Dr. Salvatore Bushati Prepared by: Presidency of Academy of Sciences of Albania Section of Natural and Technical Sciences Section of Albanological and Social Sciences Përkthimi në anglisht / Translated in English by Esmeralda Aliaj Kompjuterizimi / Computer setting: Enkelejda Misha Address: Akademia e Shkencave e Shqipërisë Academy of Sciences of Albania Sheshi Fan S. Noli, Tirana, Albania Tel: 00355 4 2259657 Tel/Fax: 00355 4 2227476 Shtypur në shtypshkronjën “Kristalina KH” Tiranë, 2012 2 Acad. Prof. Dr. Gudar Beqiraj President of ASA I nderuar lexues, Dear Reader, Analiza e veprimtarisë vjetore të institucioneve të The analysis of the annual activity of the institutions sistemit të shkencës dhe teknologjisë, nuk duhet parë of Science and Technology system should not be seen si një proces thjesht i zakonshëm i raportimit të punës simply as a routine process of the survey for the work së bërë, por si një element i rëndësishëm për një analizë done, but as an important element for a profound të thellë të arritjeve në kërkimin shkencor e ndikimin e analysis of the achievements in the scientific research tyre në zhvillimin teknologjik e inovativ e refleksion and their impact on the innovative technological mbi atë çka duhet bërë në të ardhmen për përmbushjen development and also the reflection of what should be e misionit. done in the future to fulfill the mission they have.
    [Show full text]
  • The Impacts of Climate Change on Agriculture and Other Economic Activities in Coastal Areas: the Case of Grado-Marano Lagoon
    The impacts of Climate Change on Agriculture and other economic activities in coastal areas: the case of Grado-Marano lagoon. By Elena Claire Ricci1,2, Michela Catenacci2 and Chiara M. Travisi2, 1: Department of Economics, Management and Quantitative Methods (DEMM), University of Milan, Italy; 2: Fondazione Eni Enrico Mattei (FEEM), Italy Climate Change (CC) poses significant threats to coastal areas, with the main impacts being sea-level-rise (SLR) and the consequent loss of land. Much work has been done to evaluate effective adaptation strategies, but further research is needed. This paper aims at analyzing the costs of CC and SLR in the Grado-Marano lagoon, and at proposing an example of methodology based on an economic evaluation of damages related to: loss of land on the basis of different land-uses (i); loss of non-use values (ii); losses in productivity/use values via Bayesian Networks (iii); and on a multi-criteria-analysis able to integrate different (monetary and non-monetary) criteria focused on three pillars of sustainability (iv) to compare adaptation- strategies. We find that the larger impacts are on residential and tertiary sectors, even if most of the area has an agricultural vocation, and that the best adaptation- strategy is beach-nourishment even if rankings depend on criteria weights. 1. Introduction Coastal areas and their local communities are particularly vulnerable to the expected future effects of climate change (CC) which must be carefully evaluated in order to optimize strategies of risk management. Indeed, societies in such areas are faced with the double effort of having to both mitigate and adapt to climate change.
    [Show full text]
  • Essd-2017-135.Pdf
    Discussions Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2017-135 Earth System Manuscript under review for journal Earth Syst. Sci. Data Science Discussion started: 18 December 2017 c Author(s) 2017. CC BY 4.0 License. Open Access Open Data Thickness of marine Holocene sediment in the Gulf of Trieste (Northern Adriatic Sea) Trobec, Ana1, Busetti, Martina2, Zgur, Fabrizio2, Baradello, Luca2, Babich, Alberto2,3, Cova, 5 Andrea2, Gordini, Emiliano2, Romeo, Roberto2, Tomini, Isabella2, Poglajen, Sašo4, Diviacco, Paolo2, Vrabec, Marko1 1University of Ljubljana, Faculty of Natural Sciences and Engineering, Department of Geology, Privoz 11, 1000 Ljubljana, Slovenia 10 2OGS – Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Borgo Grotta Gigante 42/c, 34010 Sgonico, Trieste, Italy 3Università di Trieste, Dipartimento di Matematica e Geoscienze, Via Weiss 2, 34127 Trieste, Italy 4Harpha Sea d.o.o., Čevljarska ulica 8, 6000 Koper, Slovenia 15 Correspondence to: Ana Trobec ([email protected]) Abstract. We use various geophysical datasets (multibeam and singlebeam echosounder data, sub-bottom profiling Chirp and sonar data and very high resolution boomer seismic data) along with published 20 sedimentological data and depth data from nautical charts in order to create models of the depth of the seafloor and the base of Holocene marine sediment in the Gulf of Trieste. The two models are later used in order to calculate the thickness of marine Holocene sediment which has been depositing on the Late Pleistocene alluvial plain since the Holocene transgression in the Italian and Slovenian part of the gulf. Thicker Holocene marine sedimentary sequences averaging at around 5 meters are characteristic for the SE part of the gulf.
    [Show full text]
  • Adriatic Marbled Bush-Cricket (Zeuneriana Marmorata)
    Adriatic Marbled Bush-Cricket (Zeuneriana marmorata) A National Action Plan for Slovenia 2016-2022 Edited by Axel Hochkirch, Stanislav Gomboc, Paul Veenvliet, Gregor Lipovšek Edited by Axel Hochkirch (Trier University (DE), Chair of the IUCN SSC Grasshopper Specialist Group and IUCN SSC Invertebrate Conservation Sub-Committee) Stanislav Gomboc (Grasshopper Specialist Group, SLO) Gregor Lipovšek (Javni zavod krajinski park Ljubljansko barje, SLO) Paul Veenvliet (Zavod Symbiosis, SLO) In collaboration with Francesca Tami (Associazione Studi Ornitologici e Ricerche Ecologiche del Friuli Venezia Giulia, IT) Yannick Fannin (IT) Andrea Colla (Museo Civico di Storia Naturale di Trieste, IT) Citation: Hochkirch A., Gomboc S., Veenvliet P. & Lipovšek G. 2017. Adriatic Marbled Bush- cricket (Zeuneriana marmorata), A National Action Plan for Slovenia 2016-2022. IUCN-SSC & Javni zavod krajinski park Ljubljansko barje, Ljubljana, Slovenia. 52 pp. Cover photo ©A. Hochkirch 2 CONTENTS INTRODUCTION ....................................................................................................................................... 4 STATUS REVIEW ....................................................................................................................................... 6 Species description .............................................................................................................................. 6 Systematics / Taxonomy .................................................................................................................
    [Show full text]