Hazardous Substances in the Mediterranean: a Spatial and Temporal Assessment
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Sediments and Pollution in the Northern Adriatic Seaa
Sediments and Pollution in the Northern Adriatic Seaa F. FRASCARI, M. FRIGNANI, S. GUERZONI, AND M. RAVAIOLI Zstituto di Geologia Marina Consiglio Nazionale delle Ricerche 40127 Bologna, Italy INTRODUCTION Most pollutants are known to have a strong tendency to interact with sus- pended organic and inorganic matter. Under certain conditions, the sediments may form deposits, where the sub- stances are stored and/or mineralized and removed from the external environ- ment. Various phenomena may, however, promote a pollutant release from the sediment towards the overlying waters. Molecular diffusion, bioturbation, resus- pension of bottom sediment and pumping due to low-intensity wave motion are phenomena that cause the transport of chemical species through the water-sedi- ment interface. The constituents that are mostly involved in these fluxes are the ones dissolved in the interstitial waters and those weakly linked to the solid. The fine mineral or flocculated sediments, which rapidly settle in the riverine prodelta,24 are the richest ones in easily exchangeable pollutants. On the other hand, the solid matter which sediments after a long transport attains a more stable equilibrium with the pollutants which are dissolved in the waters. The study of the sedimentation and transport processes of the particulate matter and associated pollutants is of great importance to understand the evolu- tion of the marine environmental quality. THE ADRIATIC SEA: GENERALITIES Problems of the open and coastal water pollution of the Adriatic Sea have been the concern of scientists and administrators for some time. Many national research programs, both related to the whole basin or with a more local concern, were called to study the Adriatic Sea, among which the applied program called “P.F. -
Nonindigenous Species Along the Apulian Coast, Italy
Chemistry and Ecology Vol. 26, Supplement, June 2010, 121–142 Nonindigenous species along the Apulian coast, Italy Cinzia Gravilia*, Genuario Belmontea, Ester Cecereb, Francesco Denittoa, Adriana Giangrandea, Paolo Guidettia, Caterina Longoc, Francesco Mastrototaroc, Salvatore Moscatelloa, Antonella Petrocellib, Stefano Pirainoa, Antonio Terlizzia and Ferdinando Boeroa aDipartimento di Scienze e Tecnologie Biologiche ed Ambientali, Università del Salento, Lecce, Italy; bIstituto Ambiente Marino Costiero, CNR, U.O.S. Taranto, Taranto, Italy; cDipartimento di Biologia Animale ed Ambientale, Università di Bari, Bari, Italy (Received 17 May 2009; final version received 14 December 2009) Thirty-eight nonindigenous marine species (NIS) (macroalgae, sponges, hydrozoans, molluscs, polychaetes, crustaceans, ascidiaceans and fish), are reported from the Apulian coast of Italy. Shipping, aquaculture and migration through the Suez Canal are the main pathways of introduction of the NIS. In Apulian waters, 21% of NIS are occasional, 18% are invasive and 61% are well-established. It is highly probable that more NIS will arrive from warm-water regions, because Mediterranean waters are warming. Furthermore, some of the successful NIS must have the ability to become dormant in order to survive adverse conditions, either seasonal or during long journeys in ballast waters. The identification of NIS depends greatly on the available taxonomic expertise; hence the paucity of taxonomists hinders our knowl- edge of NIS in our seas. We propose the creation and maintenance of a network of observatories across the Mediterranean to monitor the changes that take place along its coasts. Keywords: nonindigenous species (NIS); transport vectors; Apulian coast; Mediterranean Sea Downloaded By: [Gravili, Cinzia] At: 10:25 20 May 2010 1. -
Tharros – Capo San Marco in the Phoenician and Punic Age
Archeologia e Calcolatori 28.2, 2017, 321-331 THARROS – CAPO SAN MARCO IN THE PHOENICIAN AND PUNIC AGE. GEOPHYSICAL INVESTIGATIONS AND VIRTUAL REBUILDING The Phoenician and Punic colony of Tharros in the Gulf of Oristano, in the mid-west of Sardinia, is distinguished by an archaic phase dating back to the beginning of the 7th century BC; it is documented by the tofet findings, on the hill of Murru Mannu, and by the incineration and inhumation tombs located in the cemeterial areas in Capo San Marco, to the S, and in the vil- lage of San Giovanni di Sinis to the N. The period of maximum development and monumentalization was during the 6th century BC, when Tharros was probably the Qarthadasht of Sardinia, the administrative capital of Carthage (Fariselli in press). A few sacred public buildings in the city center and multiple hypogeal funerary structures date back to the Punic phase, which is, therefore, only partially known for the site. The archaeological evidence in the urban area intra muros mainly refers to the Roman and early medieval periods. The city was definitively abandoned around the year 1000 AD due to likely geomorphological problems still to be fully defined, maybe land or mudslides towards the gulf. The Saracens’ incursions could also be one of the reasons of the progressive depopulation in favor of the more protected hinterland (Del Vais 2015, 44). The systematic spoliation of the city’s buildings, used as a quarry for a long time, make the reconstruction of the population and frequentation’s phases very complex. The Chair for Phoenician-Punic Archaeology at the University of Bolo- gna, under my own direction, has resumed investigations on the field since 2012. -
TC19 International Workshop on Metrology for the Sea (Metrosea
TC19 International Workshop on Metrology for the Sea ( MetroSea 2019) Genoa, Italy 3 -5 October 2019 ISBN: 978-1-7138-0205-1 Printed from e-media with permission by: Curran Associates, Inc. 57 Morehouse Lane Red Hook, NY 12571 Some format issues inherent in the e-media version may also appear in this print version. Copyright© (2019) by the International Measurement Confederation (IMEKO) All rights reserved. Printed with permission by Curran Associates, Inc. (2020) For permission requests, please contact the International Measurement Confederation (IMEKO) at the address below. IMEKO Secretariat Dalszinhaz utca 10, 1st floor, Office room No. 3 H-1061 Budapest (6th district) Hungary Phone/Fax: +36 1 353 1562 [email protected] Additional copies of this publication are available from: Curran Associates, Inc. 57 Morehouse Lane Red Hook, NY 12571 USA Phone: 845-758-0400 Fax: 845-758-2633 Email: [email protected] Web: www.proceedings.com TABLE OF CONTENTS MAKING DATA MANAGEMENT PRACTICES COMPLIANT WITH ESSENTIAL VARIABLES FRAMEWORKS: A PRACTICAL APPROACH IN THE MARINE BIOLOGICAL DOMAIN .................................. 1 Martina Zilioli, Alessandro Oggioni, Paolo Tagliolato, Cristiano Fugazza, Caterina Bergami, Alessandra Pugnetti, Paola Carrara METROLOGICAL ASPECTS OF THE TOMBOLO EFFECT INVESTIGATION – POLISH CASE STUDY .................................................................................................................................................................................... 7 Cezary Specht, Janusz Mindykowski, Pawel -
Is the Gulf of Taranto an Historic Bay?*
Ronzitti: Gulf of Taranto IS THE GULF OF TARANTO AN HISTORIC BAY?* Natalino Ronzitti** I. INTRODUCTION Italy's shores bordering the Ionian Sea, particularly the seg ment joining Cape Spartivento to Cape Santa Maria di Leuca, form a coastline which is deeply indented and cut into. The Gulf of Taranto is the major indentation along the Ionian coast. The line joining the two points of the entrance of the Gulf (Alice Point Cape Santa Maria di Leuca) is approximately sixty nautical miles in length. At its mid-point, the line joining Alice Point to Cape Santa Maria di Leuca is approximately sixty-three nautical miles from the innermost low-water line of the Gulf of Taranto coast. The Gulf of Taranto is a juridical bay because it meets the semi circular test set up by Article 7(2) of the 1958 Geneva Convention on the Territorial Sea and the Contiguous Zone. 1 Indeed, the waters embodied by the Gulf cover an area larger than that of the semi circle whose diameter is the line Alice Point-Cape Santa Maria di Leuca (the line joining the mouth of the Gulf). On April 26, 1977, Italy enacted a Decree causing straight baselines to be drawn along the coastline of the Italian Peninsula.2 A straight baseline, about sixty nautical miles long, was drawn along the entrance of the Gulf of Taranto between Cape Santa Maria di Leuca and Alice Point. The 1977 Decree justified the drawing of such a line by proclaiming the Gulf of Taranto an historic bay.3 The Decree, however, did not specify the grounds upon which the Gulf of Taranto was declared an historic bay. -
Environmental Science and Pollution Research
Environmental Science and Pollution Research Archaeometric Researches on the Provenance of Mediterranean Archaic Phoenician and Punic Pottery --Manuscript Draft-- Manuscript Number: ESPR-D-15-05757R1 Full Title: Archaeometric Researches on the Provenance of Mediterranean Archaic Phoenician and Punic Pottery Article Type: Research Article Corresponding Author: Maria Letizia Amadori, M.D. university of urbino Urbino, Pesaro ITALY Corresponding Author Secondary Information: Corresponding Author's Institution: university of urbino Corresponding Author's Secondary Institution: First Author: Maria Letizia Amadori, M.D. First Author Secondary Information: Order of Authors: Maria Letizia Amadori, M.D. Carla Del Vais, PhD Paola Fermo, PhD Paolo Pallante, PhD Order of Authors Secondary Information: Funding Information: Abstract: The aim of this study is to set up a first chemical database that could represent the starting point for a reliable classification method to discriminate between Archaic Phoenician and Punic pottery on the base of their chemical data. This database up to now can discriminate between several different area of production and provenance and can be applied also to unknown ceramic samples of comparable age and production areas. More than one hundred ceramic fragments were involved in this research, coming from various archaeological sites having a crucial importance in the context of the Phoenician and Punic settlement in central and western Mediterranean: Carthage (Tunisia), Toscanos (South Andalusia, Spain), Sulci, Monte Sirai, Othoca, Tharros and Pithecusa (Italy). Since long time archaeologists hypothesized that Mediterranean Archaic Phoenician and Punic pottery had a local or just a regional diffusion, with the exception of some particular class like transport amphorae. To verify the pottery provenance, statistical analyses were carried out to define the existence of different ceramic compositional groups characterized by a local origin or imported from other sites. -
FASTMIT Project Activities in the Apulia Platform: Evidence of an Active Fault System in the Salento Offshore (Ionian Sea) F.E
GNGTS 2017 SESSIONE 1.2 FASTMIT PROJECT ACTIVITIES IN THE APULIA PLATFORM: EVIDENCE OF AN ACTIVE FAULT SYSTEM IN THE SALENTO OFFSHORE (IONIAN SEA) F.E. Maesano1, V. Volpi2, R. Basili1, M.M. Tiberti1, M. Zecchin2, S. Ceramicola2, G. Rossi2 1 Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy 2 Istituto Nazionale di Oceanografia e Geofisica Sperimentale (OGS), Trieste, Italy The FASTMIT Project (FAglie Sismogeniche e Tsunamigeniche nei Mari Italiani) aims to widening and systematizing the knowledge on seismogenic and potentially tsunamigenic faults in the Italian marine areas, thereby taking the pledge to address compelling issues related to geohazards of coastal areas and offshore infrastructures. FASTMIT study areas straddle the Europe-Nubia plate boundary, with focus on the Adriatic Sea, the Gulf of Taranto, the Sicily Channel and the Southern Tyrrhenian Sea. Here we present the preliminary results in the Gulf of Taranto. This area has been recently studied in the framework of various national and international projects (e.g.: EC HERMES, MAGIC, RITMARE, CARG, DPC-INGV-S1), which highlighted its geological complexities. In this area, the Apulia Platform is inflected under the Calabrian Accretionary Wedge as a result of the subduction of the Ionian oceanic crust and the subsequent collision with the Apulia continental margin. The Apulia Platform units have been recognized under the allochthonous units of the accretionary wedge in all the Gulf of Taranto and in the offshore of Crotone where they are affected by transpressional structures (Maesano et al., 2017; Volpi et al., 2017), whereas in the foreland areas (Salento offshore) they are affected by normal faulting. -
Mineralogical-Petrographic and Physical-Mechanical Features
minerals Article Mineralogical-Petrographic and Physical-Mechanical Features of the Construction Stones in Punic and Roman Temples of Antas (SW Sardinia, Italy): Provenance of the Raw Materials and Conservation State Stefano Columbu , Emanuela Gaviano, Luca Giacomo Costamagna and Dario Fancello * Dipartimento di Scienze Chimiche e Geologiche, University of Cagliari, Cittadella Universitaria di Monserrato, Monserrato, 09042 Cagliari, Italy; [email protected] (S.C.); [email protected] (E.G.); [email protected] (L.G.C.) * Correspondence: [email protected] Abstract: The Antas site (SW Sardinia, Italy) is of fundamental cultural importance because it testifies the presence of Nuragic, Punic and Roman civilizations from the second millennium to the third century BC. This work focuses on the Punic and the Roman temples and aims to define their conservation state and provenance of construction materials through their minero-petrographic and physical-mechanical characterization. In addition, artificial geomaterials used in restoration works comprising a partial anastylosis and a consolidation intervention on the monument, were investigated to evaluate the aesthetic, petrographic and petrophysical compatibility with the original materials. The results indicate that Punic builders preferred to use a porous sandstone coming from Citation: Columbu, S.; Gaviano, E.; at least few kilometres away from the site. By contrast, Roman builders opted for the use of the less Costamagna, L.G.; Fancello, D. porous and harder local metadolostones, more difficult to quarry and to hew but promptly available Mineralogical-Petrographic and Physical-Mechanical Features of the in the surrounding area. The Roman temple still preserves decorative architectural elements (as Construction Stones in Punic and the Pronao threshold and the mosaic tesserae) whose source is definitely not local, suggesting the Roman Temples of Antas (SW import of these materials. -
Romanisation in the Brindisino, Southern Italy: a Preliminary Report Douwe Yntema
BaBesch 70 (1995) Romanisation in the Brindisino, southern Italy: a preliminary report Douwe Yntema I. INTRODUCTION Romanisation is a highly complicated matter in southern Italy. Here, there was no culture dialogue Romanisation is a widely and often indiscrimi- involving two parties only. In the period preceding nately used term. The process expressed by the the Roman incorporation (4th century B.C.) this word involves at least two parties: one of these is area was inhabited by several different groups: rel- the Roman world and the other party or parties is ative latecomers were the Greek-speaking people or are one or more non-Roman societies. These who had emigrated from present-day Greece and are the basic ingredients which are present in each the west coast of Asia Minor to Italy in the 8th, 7th definition, be it explicit or implicit, of that term. and 6th centuries; they lived mainly in the coastal Many scholars have given their views on what strip on the Gulf of Taranto. Other (‘native') they think it should mean. Perhaps the most satis- groups had lived in southern Italy since the Bronze factory definition was formulated by Martin Age. Some groups in present-day Calabria and Milett. In his view, Romanisation is not just Campania displayed initially close links with the another word to indicate Roman influence: ‘it is urnfield cultures of Central Italy. Comparable a process of dialectical change rather than the groups, living mainly in present-day Apulia and influence of one … culture upon others' (Millett Basilicata and having closely similar material cul- 1990). -
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UNIVERSITÀ DEGLI STUDI DI NAPOLI “FEDERICO II” PhD thesis “Marine organisms model species for the assessment of biological, environmental and economic impacts on marine aquaculture in Campania” Coordinatore Candidato Tutor Prof. Dott. ssa Dott. Giuseppe Cringoli Sara Fioretti Francesco Paolo Patti Prof. Aniello Anastasio “First, think. Second, believe. Third, dream. And finally, dare. If you can dream it, you can do it” Walt Disney Index Abbreviations list ......................................................................................13 Figures list .................................................................................................15 Tables list ...................................................................................................17 Abstract .....................................................................................................19 Introduction ..............................................................................................23 I Aquaculture in Campania: from the origin to the current times ..........25 II Aquaculture today: global and European trend ..................................27 III Aquaculture in Italy ...........................................................................30 IV Aquaculture in Campania ..................................................................31 V Mussel farms: breeding systems .........................................................33 VI Mussel farms threats and future perspectives for the Campanian industries ................................................................................................35 -
Phoenician and Punic Amphorae from S'urachi
Phoenician and Punic Amphorae from S’Urachi (San Vero Milis, Sardinia) Andrea Roppa, Emanuele Madrigali, Alfonso Stiglitz, and Peter van Dommelen Context Amphora typologies: chronological aspects The site of S’Urachi in west-central Sardinia was continuously inhabited between the Bronze Age and the Roman early Slightly later is the chronology of a rim fragment of a T-2.1.1.1. = B5 amphora type, which goes back to the first half of the 7th The overall distribution of Phoenician and Punic amphora types from the excavations in sectors E and D at S’Urachi points to Imperial period. Past research at the site has already shed light on the gradual transformations the settlement underwent century BC. From the western Mediterranean, traditionally associated to production areas at the Phoenician settlements in a substantial increase in the presence of amphorae from the late 7th century BC, as shown by the chronological profile based throughout the Iron Age, when interaction with Phoenician newcomers resulted in substantial changes in the indigenous Andalusia, are two rim fragments of type T-10.1.2.1., dated to the mid 7th – early 6th century BC. on a weighted mean of a 25-year chronological reference unit (fig. 6). community (fig. 1). Since 2013 ongoing excavations, jointly supported by the museum of San Vero Milis and the Joukowsky From the late 7th century BC and throughout the 6th century BC, Phoenician amphorae were much more abundant at Phoenician and Punic Amphorae. Institute of Brown University have brought to light securely stratified contexts and a large assemblage of primarily ceramic S’Urachi, as is evident from 18 fragments of type T-2.1.1.2. -
Changes in the Benthic Algae Along the Adriatic Sea in the Last Three Decades
Chemistry and Ecology Vol. 26, Supplement, June 2010, 77–90 Changes in the benthic algae along the Adriatic Sea in the last three decades A. Falacea*, G. Alongib, M. Cormacib, G. Furnarib, D. Curielc, E. Cecered and A. Petrocellid aDepartment of Life Sciences, University of Trieste, Trieste, Italy; bDepartment of Botany, University of Catania, Catania, Italy; cSELC – Venezia-Marghera, Italy; d IAMC-CNR Talassografico ‘A. Cerruti’, Taranto, Italy (Received 25 May 2009; final version received 22 January 2010) This article gives an up-to-date review of the status of and main changes in benthic algal flora that have occurred in recent decades along the Italian Adriatic coastline. Common traits among the main structural/functional changes observed and their causes are discussed. A synthesis of the challenges to and prospects of filling gaps in the data, ecological knowledge and protection measures are also given. Keywords: biodiversity; flora; macrophytobenthos; Adriatic Sea; ecosystem functioning 1. Introduction Over the past three decades, it has been recognised worldwide that spatial and temporal distribution patterns of organisms, species diversity and physical and biological habitat structure have changed as a result of anthropogenic disturbances, defined as any potential source of stress caused by Downloaded By: [Falace, Annalisa] At: 10:44 20 May 2010 human activities. However, change is a main feature of evolution [1], and the number of species in a region is set by a balance between speciation, extinction and the migration of species between regions, all of which can operate over long natural or short man-made time scales. Besides, on a small scale, species composition can be naturally highly variable and rare species may become abundant and vice versa.