My GeoServer WFS This is a description of your Web Feature Server. The GeoServer is a full transactional Web Feature Server, you may wish to limit GeoServer to a Basic service level to prevent modificaiton of your geographic data. WFSWMSGEOSERVERWFS1.1.0NONENONE1.0.01.1.0text/xmltext/xml; subtype=gml/3.1.1resultshitstext/xml; subtype=gml/3.1.1GML2KMLSHAPE-ZIPapplication/gml+xml; version=3.2application/jsonapplication/vnd.google-earth.kml xmlapplication/vnd.google-earth.kml+xmlcsvexcelexcel2007gml3gml32jsontext/xml; subtype=gml/2.1.2text/xml; subtype=gml/3.22ALLSOMEresultshitstext/xml; subtype=gml/3.1.1GML2KMLSHAPE-ZIPapplication/gml+xml; version=3.2application/jsonapplication/vnd.google-earth.kml xmlapplication/vnd.google-earth.kml+xmlcsvexcelexcel2007gml3gml32jsontext/xml; subtype=gml/2.1.2text/xml; subtype=gml/3.2text/xml; subtype=gml/3.1.1GenerateNewUseExistingReplaceDuplicateALLSOMEQueryInsertUpdateDeleteLockgeonode:tempo_di_residenza_wrt_della_laguna_di_venezia_senza_le_strutture_fisse_del_mose Il tempo di residenza è stato calcolato sulla base della circolazione della laguna di Venezia riprodotta da un modello idrodinamico (SHYFEM) applicato nella sua versione tridimensionale barotropica sottoposto a di forzanti di marea e vento reali. La mappa riporta il tempo di residenza calcolato su tutti i livelli, l'unità di misura è il giorno. In questo caso il modello idrodinamico simula il tempo di residenza alla situazione antecedente la costruzione delle nuove strutture fisse del MOSE ed in particolare alle modifiche delle bocche di porto. urn:x-ogc:def:crs:EPSG:300412.11994208002764 44.98470608251249612.763688484548604 45.62845248703346http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=a2a35732-6fef-46eb-af52-e69a92b5b4afgeonode:ismarLocalizzazione della palazzina storica della Biblioteca degli studi Adriatici.ismarfeaturesurn:x-ogc:def:crs:EPSG:432612.3540027576525 45.430458980574512.3542027576525 45.430658980574506http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=817d407a-1991-11e5-9ab7-005056bd48e7geonode:velist_zooLa velocità istantanea è espressa in metri al secondo ed è stata calcolata in ogni punto della griglia all'interno della Laguna di Venezia e nella zona di mare antistante. Questi valori sono stati prodotti nel corso di uno studio modellistico della laguna utilizzando un modello di circolazione forzato con dati di livello e vento reali. urn:x-ogc:def:crs:EPSG:300412.112485799999995 45.09898579999999412.602514200000005 45.58901420000001http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=2c7b038f-2231-477c-a4b6-f3346eee9ca1geonode:capisaldi_1Reti di capisaldi di livellazione altimetrica per il monitoraggio della subsidenza dell'area circostante i bacini di stoccaggio dell'EDISON-GAS nella zona di Collalto-Montello.livallazionealtimetriacaposaldourn:x-ogc:def:crs:EPSG:300411.933046297575965 45.5678936881654612.503844095684558 46.13869148627406http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=0b8160f0-bed1-11e5-ac10-005056bd48e7geonode:ve_comuniNo abstract providedurn:x-ogc:def:crs:EPSG:300311.955479482173061 45.026787071159213.116563531424772 45.87795985818013http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=9a66aa82-b44e-49d8-822b-5ebdebe4dee7geonode:Copertura_Laguna_18cmNo abstract providedurn:x-ogc:def:crs:EPSG:3263312.00310717073821 45.07246064929269412.828923667488255 45.62353523569715http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=319bc4ac-2f96-44e4-a583-af9bb64b3c60geonode:copertura_radarDiagramma ipotizzato delle diverse coperture radar. Antenne HF COCONET e SSD pesca. Capacità di copertura 35 km.urn:x-ogc:def:crs:EPSG:432615.198990391305955 41.41583345934229516.601862537573084 42.21403254484217http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=47f885fe-2e14-4b89-a23f-5998335aa4a2shyfem:vel_correnteCorrenti all'interno della laguna di Venezia calcolate tramite il modello idrodinamico agli elementi finiti SHYFEM. La mappa viene aggiornata ogni trenta minuti, utilizzando le ultime osservazioni disponibili per forzare il modello.shyfem_shyfemoutputfeaturesurn:x-ogc:def:crs:EPSG:300411.995905745081727 45.02051592335913512.705347454603634 45.72995763288103http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=5abf1298-d90a-4846-a05a-70a0931d8402geonode:curve_di_livello_transetto_manfredoniaCurve di livello ottenute dall'interpolazione della profondità relativa alle 12 stazioni del transetto per il campionamento di benthos e sedimenti.urn:x-ogc:def:crs:EPSG:432615.9614 41.441416.3964 41.8104http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=e2dc3f78-f997-40b5-a4fc-23b716159fecgeonode:lesina_acquiferi_piano_tutela_acque_2009The Gargano aquifer consists of large, deep carbonate aquifers (of Jurassic-Oligocene and mainly Mesozoic age), and the predominant rock material is either limestone or limestone-dolomite. The aquifer is punctuated by karst and fractured phenomena; well below sea level. As is often the case in coastal lagoons, seawater underlies fresh groundwater due to density differences, and a freshwater lens is found. Aquifers underlying the Gargano Promontory are artesian, and have a pressure head above sea level except on a restricted coastline strip. The maximum piezometric head is about 50 m asl (Polemio et al. 2010). Sinking of the carbonate platform is observed along the borders between Tavoliere and Gargano. Successive layers of Pleio-Pleistocene clays, marly clays, sandstones and sands make up the base of the promontory. Other two aquifer lie in the lagoon area but contrary to the Gargano aquifer, they consist of alluvial material and the westernmost aquifer is fed by the Fortore River. All the springs in the eastern area of the lagoon belongs to the karst aquifer circulation of the Gargano aquifer Oblong aquifers in a NE-SW orientation are predominantly reported in the sandy layers of this succession (Balduzzi et al. 1982). Groundwater flowing through these 'intermediate" aquifers is generally of artesian nature, and is subject to high pressure due to the confining action of the clay layers (Cotecchia and Magri 1996). This succession overlies a third deeper carbonate aquifer, which is a sunken carbonate platform. Data fromRegione Puglia 2007. Adozione, ai sensi dell’art.121 del D. Lgs. n.152/2006, del Progetto di Piano di Tutela delle Acque della Regione Puglia 2007 Regione Puglia (soc. Terna) 2009. Valutazione Ambientale del Piano di Sviluppo 2009 Rapporto Ambientale.urn:x-ogc:def:crs:EPSG:3263315.231518291318626 41.72226958891208415.712308023505644 41.92482822466006http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=1239c78e-6bf8-40c9-81ec-1a75fd2376a1geonode:batimetri_lesinaCurve di Livello della Laguna di Lesina. La Sacca orientale della Laguna di Lesina è riserva integrale e Zona 1 del Parco Nazionale del Gargano, non è stata digitalizzata.urn:x-ogc:def:crs:EPSG:300415.310101958236844 41.8602128320814215.543252414764302 41.91109690642894http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=0e76c7a7-2bb4-4b78-8b3f-bd8eaf6519dfgeonode:lesina_flooding_riskAccording to the Piano territioriale di Coordinamento Provinciale 2006 prepared by the Provincia di Foggia, the western part of the municipality of Lesina is included in an area that is at serious risk of flooding, because of the torrential regime of the river Fortore during exceptional precipitation events when the Occhito dam is not enough to contain the surplus of water. Therefore, the lagoon represents a natural detention basin and can be considered to provide a benefit by preventing flooding in the reclaimed areas situated below the sea level (preventive benefit or provisioning services). Data from: Regione Puglia 2007. Adozione, ai sensi dell’art.121 del D. Lgs. n.152/2006, del Progetto di Piano di Tutela delle Acque della Regione Puglia 2007 Regione Puglia (soc. Terna) 2009. Valutazione Ambientale del Piano di Sviluppo 2009 Rapporto Ambientale.urn:x-ogc:def:crs:EPSG:3263315.296840087810635 41.71611609001270415.575725023799539 41.91653432926174http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=f28da916-8b06-4d21-8c82-c6c2f4d51d0fgeonode:lesina_nitrate_vulnerabilityscientific studies agree in considering the lagoon as final receptor for nutrients (especially nitrate), playing in this way an important role in the natural attenuation of such contaminants. It is important to mention that the biodegradation capacity is limited by the efficiency and integrity of the ecosystems. Furthermore, the increasing conversion of land for agricultural use destroyed most of the riparian vegetation along the canals, which reduces their capacity to attenuate the discharge of nutrients, contaminants and sediments (from soil erosion) into the lagoon. This has led to an increase in the concentration of nutrients in the surface water. Canals also drain water from the very shallow aquifer, which is affected by nutrient leaching, as biodegradation is limited by the reduced extension of the vadose zone. Therefore, the lagoon acts as a sink of sediments and nutrients but it has a limited capacity to adsorb these quantities from its carriers. data from: Regione Puglia 2007. Adozione, ai sensi dell’art.121 del D. Lgs. n.152/2006, del Progetto di Piano di Tutela delle Acque della Regione Puglia 2007 Regione Puglia (soc. Terna) 2009. Valutazione Ambientale del Piano di Sviluppo 2009 Rapporto Ambientale.urn:x-ogc:def:crs:EPSG:3263315.258180411593399 41.8178899727703715.488356727681724 41.8869840095656http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=5e10fd86-b16d-46dd-a496-27d5e2b4731ageonode:lesina_piezometria_cotecchia_1996The Gargano aquifer consists of large, deep carbonate aquifers (of Jurassic-Oligocene and mainly Mesozoic age), and the predominant rock material is either limestone or limestone-dolomite. The aquifer is punctuated by karst and fractured phenomena; well below sea level. As is often the case in coastal lagoons, seawater underlies fresh groundwater due to density differences, and a freshwater lens is found. Aquifers underlying the Gargano Promontory are artesian, and have a pressure head above sea level except on a restricted coastline strip. The maximum piezometric head is about 50 m asl (Polemio et al. 2010). Sinking of the carbonate platform is observed along the borders between Tavoliere and Gargano. Successive layers of Pleio-Pleistocene clays, marly clays, sandstones and sands make up the base of the promontory. Other two aquifer lie in the lagoon area but contrary to the Gargano aquifer, they consist of alluvial material and the westernmost aquifer is fed by the Fortore River. Oblong aquifers in a NE-SW orientation are predominantly reported in the sandy layers of this succession (Balduzzi et al. 1982). Groundwater flowing through these 'intermediate" aquifers is generally of artesian nature, and is subject to high pressure due to the confining action of the clay layers (Cotecchia and Magri 1996). This succession overlies a third deeper carbonate aquifer, which is a sunken carbonate platform. Data from Cotecchia V. and Magri G. 1966. Idrogeologia del Gargano. Geol. Appl. e Idrogeol. 1, pp. 1-80. urn:x-ogc:def:crs:EPSG:3263315.337924575370764 41.8253256299118215.483831112269277 41.86492818254522http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=9e472b6e-9801-44d4-9c12-dc027a3e8b70geonode:sedimenti_conisma_2000The textural characteristics of the sediments confirm that large percentages of coarse sand (up to 74%) present in some portions of the lagoon are attributed to the sediments composing the sandy ridges, which gradually closed the lagoon from the sea. Therefore, the muddy portion is interpreted as the product of recent sediments. The muddy fraction is minor in quantity where bedforms attributed to the relic spits exist. Much of the lagoon is marked by muddy sediments, with fine-grained clayey silt giving way to slightly coarser grained silts and fine sands near the two inlets. The finest material is found near the marshes on the eastern shore. The map of sediments from 2000 (Brambati 2002) is reported in the .shp. These fine sediments lead to sometimes turbid conditions during periods of heavy wind. Samples were collected in a campaign performed in 2000. Brambati A. 2002 Caratterizzazione morfologica di specchi d' acqua costieri ai fini di una caratterizzazione cartografica: Lago di Lesina.urn:x-ogc:def:crs:EPSG:3263315.309841129388488 41.86086453188594415.587197405468837 41.91552408535327http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=ecdbb1ea-4017-43a6-a465-3f939bb233a4geonode:metalli_acque_2004Campionamenti nella colonna d´acqua nel 2004. The Lesina lagoon is located on the southern Adriatic coast of Italy; many marine species, such as the shrimp M. kerathurus, use the Lesina lagoon as a nursery, spending their initial growth phase there. In order to assess the usefulness of migratory species as biomonitors of the environmental quality of this nursery area, we evaluated the metal content of the M. kerathurus juveniles at the end of their growth phase in the lagoon (October), when they are assumed to have bioaccumulated the maximum level of metals from the lagoon environment. The concentrations of Cr, Cd, Pb, Zn, Mn and Cu were measured in the muscle and exoskeleton of the shrimp, and in the sediments and waters of three areas of the Lesina Lagoon. Both the water and sediment levels of the investigated metals tended to fall within the ranges recorded for other lagoon environments characterized by similar anthropic impact and texturally similar sediment; the juveniles of the shrimp M. kerathurus proved to be strong bioaccumulators of heavy metals such as Zn and Cu (biota-sediment accumulation factors – BSAFs – 6.01 and 25.0 respectively), which derive from agricultural activities; therefore, at the end of their growing phase in the lagoon they can be considered useful biomonitors of metal contamination of agricultural origin in their nursery area. D´Adamo et al. 2008 DOI 10.1007/s10661-007-9944-3urn:x-ogc:def:crs:EPSG:3263315.314704874544585 41.8682187252197615.513717364628558 41.899847841225586http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=1c62a95b-0520-499c-b808-c1acb08b2cd6geonode:chl_a_dfferenti_campionamentiRange di distribuzione e variazione stagionale del fitoplancton nella laguna (dati per il 1994 e 1995 da report Marolla 1995; i dati per il 2003 e 2004 da report AGEI 2005 e Munari et al. 2009 mentre i dati del 2008 da Ludovisi et al. 2012). Concentrazioni in µg/lurn:x-ogc:def:crs:EPSG:3263315.347661394052208 41.86817917564026515.522512451878697 41.902175860501615http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=e16976f5-11be-4395-aa76-94e568196219geonode:lesina_monitoraggio_principali_immissariPortate complessive e concentrazione nutrienti rilevati allo sbocco dei principali tributari di acque dolci superficiali e di sorgente, della laguna di lesina. Campagna campionamenti aprile 2004 - gennaio 2008. urn:x-ogc:def:crs:EPSG:432615.36476862 41.8648260615.570889187437995 41.898623617184114http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=e9635e6b-9653-487e-b9aa-1f5267c9648fgeonode:lesina_biotic_indexNella tabella .dbf : species number (S); Shannon-Wiener’s diversity (H’); Confinement; Average depth (m); Seagrasses; Sediment type; ecological classification by expert judgement (EC); Chl-a (µg/g); Proteins (mgC/g); Carbohydrates (mgC/g); Lipids (mgC/g); Biopolymeric-C (mgC/g); Bioavailable-C (mgC/g); Sulphide (µgS/g); Salinity (PSU); Oxygen (mg/l); Ammonium (µg/l); Orthophosphate (lg/l); AMBI; BENTIX; BITS; BOPA; FINE index. The European Water Framework Directive (WFD, 2000 ⁄ 60 ⁄ EC) recommends the development of biotic indices for assessing the ecological quality status of water bodies. The Benthic Index based on Taxonomic Sufficiency (BITS) was specifically developed for lagoonal systems, according to the tolerant ⁄ opportunistic approach. Macrobenthic data, variables indicative of eutrophication and variables indicative of sedimentary organic matter quality were collected during 18 surveys carried out between 2004 and 2005 in three Adriatic coastal lagoons (Venice Lagoon, Sacca di Goro, Lesina Lagoon). The relationship between environmental variables and biotic indices (AMBI, BENTIX, BITS, BOPA and FINE) was tested using multivariate analyses. Indices based on species classification level appeared to relate better with the variables describing organic matter quality, whereas BITS, which is based on family classification level, seemed related to eutrophication indicative variables, such as sulphide, ammonium, dissolved oxygen and orthophosphate concentrations. The BITS approach reduces the costs associated with sorting and identification of organisms. Providing a rapid assessment of ecological quality, and producing an ecologically relevant classification, BITS seems a promising tool for monitoring programs of Adriatic lagoonal ecosystems. Its sensitivity in reflecting the field conditions elsewhere, however, remains to be assessed. Munari C., Manini E., Pusceddu A., Danovaro R., Mistri M. 2009. Response of BITS (a benthic index based on taxonomic sufficiency) to water and sedimentary variables and comparison with other indices in three Adriatic lagoons. Marine Ecology 30, 255–268.urn:x-ogc:def:crs:EPSG:3263315.347661394052208 41.8682091181054415.51584796374318 41.897917105907126http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=4c93ae38-ae6d-4e79-98af-1a955fa3cb4fgeonode:macrophytobenthos_2001Nella Tabella .dbf: Macrophytobenthos; Bottom Type. The benthic community of the lagoon of Lesina was studied from July 2000 to June 2001. The distribution of the main macrophytobenthic species was recorded by visual census at 24 stations in July 2000. The macrofauna, from both hard and soft substrates, was analyzed at five stations with seasonal frequency; in addition, themain hydrologic parameters were recorded monthly. The lagoon was mainly characterized by brackish water, with salinity values decreasing from west to east (annual mean: 23.3 psu). It showed mild water temperatures throughout the year (annual mean: 19.8 °C) and moderately high values of dissolved oxygen (annual mean: 9.9 ppm). No dystrophic crises were observed during the period of study. In the eastern basin, Zostera noltii Hornemann, Lissara and Ruppia cirrhosa (Patagna) Grande were the most abundant species of macrophytobenthos. Their distributional pattern was coherent with literature data. Soft bottoms of the western basin were largely occupied by the benthopleustophytic alga Valonia aegagropila C. Agardh, which during the last decade had almost completely replaced Cladophora prolifera (Roth) Kützing and Gracilaria confervoides Greville, the latter of which was previously very abundant in the lagoon. Macrozoobenthos consisted of 53 species (1 sponge, 2 cnidarians, 11 molluscs, 14 annelids, 21 crustaceans, 1 insect, 1 bryozoan, 1 echinoderm, 1 tunicate), most of which are typical of brackish water. Highest abundances were found in the eastern area of the basin. Some marine species were recorded in the western area. In contrast with the dramatic changes observed in the floral assemblage, a large amount of species had already been recorded in the lagoon during the last 10 years, pointing out the persistence of the macrozoobenthic community. Nevertheless, the distribution of benthic macrofauna seemed to be greatly influenced by the presence of Valonia aegagropila, as shown in an ordination model, where station-points were segregated by the presence of the alga rather than by hydrologic parameters. The impact of biotic factors on the community, such as non-indigenous species invasions, was suggested as constraints inducing the temporal variations of benthos. Data digitized from Marzano et al. 2003. Distribution, persistence and change in the macrobenthos of the lagoon of Lesina (Apulia, southern Adriatic Sea). Oceanologica Acta 26 (2003) 57–66 DOI:10.1016/S0399-1784(02)01229-Xurn:x-ogc:def:crs:EPSG:3263315.34354619040815 41.8709580288812315.516351023673467 41.90336282565041http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=edc506de-1986-40ae-9de1-65d15834bcf0geonode:macrophytobenthos_cozzolino_1995Nella Tabella .dbf: Macrophytobenthos. In the eastern basin, Zostera noltii, Lissara and Ruppia cirrhosa were the most abundant species of macrophytobenthos. Their distributional pattern was coherent with literature data. Soft bottoms of the western basin were largely occupied by the benthopleustophytic alga Valonia aegagropila, which during the last decade had almost completely replaced Cladophora prolifera and Gracilaria confervoides, the latter of which was previously very abundant in the lagoon. Macrozoobenthos consisted of 53 species (1 sponge, 2 cnidarians, 11 molluscs, 14 annelids, 21 crustaceans, 1 insect, 1 bryozoan,1 echinoderm, 1 tunicate), most of which are typical of brackish water. Highest abundances were found in the eastern area of the basin. Some marine species were recorded in the western area. Cozzolino, G.C., 1995b. Macrofitobenthos della laguna di Lesina: cartografia estiva. Biol. Mar. Medit. 2 (2), 361–363. urn:x-ogc:def:crs:EPSG:3263315.309841764917492 41.8610881168403915.543618523779559 41.910577124786904http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=71957527-b7ad-42cd-94c1-008414247db1geonode:lesina_metals_muscles_m_kerathurus_data_digitized__1In order to assess the usefulness of migratory species as biomonitors of the environmental quality of this nursery area, we evaluated the metal content of the M. kerathurus juveniles at the end of their growth phase in the lagoon (October), when they are assumed to have bioaccumulated the maximum level of metals from the lagoon environment. The concentrations of Cr, Cd, Pb, Zn, Mn and Cu were measured in the muscle and exoskeleton of the shrimp, and in the sediments and waters of three areas of the Lesina Lagoon. Concentrations of metals represent the mean value over the numer of samples at the same site.urn:x-ogc:def:crs:EPSG:3263315.354385503030544 41.8886116413387715.505373302898374 41.90304551024871http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=4fe27fb0-f611-4fad-8795-d32d4feaa450geonode:lesina_metals_muscles_m_kerathurus_data_digitized_In order to assess the usefulness of migratory species as biomonitors of the environmental quality of this nursery area, we evaluated the metal content of the M. kerathurus juveniles at the end of their growth phase in the lagoon (October), when they are assumed to have bioaccumulated the maximum level of metals from the lagoon environment. The concentrations of Cr, Cd, Pb, Zn, Mn and Cu were measured in the muscle and exoskeleton of the shrimp, and in the sediments and waters of three areas of the Lesina Lagoon. Concentrations of metals represent the mean value over the numer of samples at the same site.urn:x-ogc:def:crs:EPSG:3263315.354385503030544 41.8886116413387715.505373302898374 41.90304551024871http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=295da968-f3b0-4e6e-82d4-e83e17a80584geonode:sorgenti_contaminazioneNella tabella .dbf: Nome sorgente contaminazione (Source); Tipo sorgente contaminante (Type). Potenziali sorgenti di contaminazione inland per la laguna di Lesinaurn:x-ogc:def:crs:EPSG:3263315.309683213099554 41.8515780797818415.5563051180839 41.913421141455245http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=2bd448ae-76f8-4e1e-927d-4d1f4f4eb008geonode:lesina_trophic_index_2004Nella Tabella .dbf: Temperatura (T °C); Salinità (ppt); Oxygen saturation (%); DIN (µM); DIP (µM); Total Chl a (µg/l); Taxon (no.); Weight (pgC/cell); TRIX The lagoon of Lesina is classified into different categories depending on which trophic state indices are applied. These indices all describe conditions governed by the temporal and spatial variability of the system, and highlight distinctive properties of the areas near the freshwater inputs (Roselli et al. 2009). Lugoli et al. (2012) applied a new multimetric phytoplankton index, which integrates simple size spectra metrics, size class sensitivity to anthropogenic disturbance, phytoplankton biomass (Chl-a) and taxonomic richness thresholds. ISS-Phyto was originally developed for transitional waters but it can also be an adequate assessment tool of ecological status in coastal marine waters to describe within ecosystem disturbance gradients. The fact that it is mainly based on the phytoplankton size rather than taxonomic studies makes it an effective tool to assess the ecological status of transitional water. data from Lugoli F., Garmendiad M., Lehtinenb S., Kauppilab P., Monchevac S., Revillad M., Roselli L., Slabakovac N., Valenciad V., Dromphe K.M., Basset A. 2012. Application of a new multimetric phytoplankton index to the assessment of ecological status in marine and transitional waters. Ecological Indicators 23, 338–355.urn:x-ogc:def:crs:EPSG:3263315.349257527684 41.7921378935558315.54039548648509 41.98327585235691http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=573b8efc-f0f4-4056-9a59-2b46aa15c2bcgeonode:lesina_metalli_sedimenti_2004Nella Tabella .dbf: Cd (µg/g); Pb (µg/g); Cu (µg/g); Mn (µg/g); Zn (µg/g); Cr (µg/g); Name of the station sampled. The distribution of Cd (0.4–1.3 μg/g) and Mn (63–160 μg/g in the sediment was found to be relatively homogeneous across sampling sites and the main source of these metals could not be identified. Cr (0.4–31 μg/g) and Zn (2–23 μg/g) were mainly recorded near the mouths of the channels, while Pb (0.6–28 μg/g) and Cu (0.4–14 μg/g) were found mainly in the central area of the lagoon and near the points of entry of urban and agricultural runoff. Higher concentrations of metals are found in sediments compared to within the cell structure of Melicertus kerathurus. Concentrations of most metals have not changed markedly in the last decade (i.e., from the study of De Benedictis 1996 to the most recent), while Zn levels (255–1,155 μg/g) have considerably decreased. Metals in sediments are relatively conservative and therefore one can compare changes in time with more certainty than when looking at nutrient variation (D’Adamo 2008). Also in the more current study, metal content of the sediments proved to be lower than concentrations in water. And these values remain lower than or similar to those recorded by other authors for similar environments (Vazquez et al. 1999; Chou et al. 2004). Results of the investigations showed that the concentrations of all the investigated metals in the sampled sites of the Lesina lagoon were found to be independent of salinity. Data digitized from D’Adamo R., Di Stasio M., Fabbrocini A., Petitto F., Roselli L., Volpe M.G. 2008. Migratory crustaceans as biomonitors of metal pollution in their nursery areas. The Lesina lagoon (SE Italy) as a case study. Environ Monit Assess 143,15–24. doi10.1007/s10661-007-9944-3. urn:x-ogc:def:crs:EPSG:3263315.314704874544585 41.8681316139678115.532854397641144 41.899847841225586http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=7900f156-4486-4f81-aedc-6d0582e8974fgeonode:lesina_salt_water_intrusionClean drinking water is provided to the settlements along the lagoon through pipes from the Occhito dam, which also supplies agriculture and small industries. However, a huge density of wells is recorded in the area but they are mostly used for agriculture, especially during drought periods. The presence of numerous karst springs has also contributed to the development of inland aquaculture farms, which utilize groundwater for their pools. Data from: Regione Puglia 2007. Adozione, ai sensi dell’art.121 del D. Lgs. n.152/2006, del Progetto di Piano di Tutela delle Acque della Regione Puglia 2007 Regione Puglia (soc. Terna) 2009. Valutazione Ambientale del Piano di Sviluppo 2009 Rapporto Ambientale.urn:x-ogc:def:crs:EPSG:3263315.3567915576392 41.80313407272516515.636238256505504 41.926599454896404http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=db880ff6-cdf8-48b8-b8e1-ed59d9e0641fgeonode:lesina_benthic_ciliates_mayjune2004_data_digitizedSample collections were made during early May and the end of July 2004 at Lesina lagoon. During the investigation period, 63 ciliate taxa belonging to 41 genera were found: 38 were observed at Sacca di Goro stations, 33 were observed at Lesina stations, and 8 were common to the two lagoons. In the .dbf Table data refer to sediments collected in Spring and Summer: Porosity (ml/ml); Density (g/cm3); Redox (mV); Bacterial biomass (µgC/g); Chlorophyll a (µg/g) and Ciliates. Data digitized from Madoni 2006. Benthic ciliates in Adriatic Sea lagoons. European Journal of Protistology 42 (2006) 165–173urn:x-ogc:def:crs:EPSG:3263315.347687933130146 41.8731969979980115.495200984605047 41.88789301364476http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=423b6a01-072b-4364-978c-ceae19f639bfgeonode:lesina_samples2008_2009_data_digitized_from_borja_Caratteristiche chimico fisiche dei siti di campionamento. Le stazioni sono in ordine di distanza dalla sorgente di pressione antropica. NA – informazini non disponibili. TOC – Carbonio Organico Totale. In the .dbf Table: Depth (m); Distance to the pressure (km); Salinity; Redox potential (mV); Gravel (%); Sand (%); Mud (%); Organic content (%) Data digitized from A. Borja et al. 2011. Response of single benthic metrics and multi-metric methods to anthropogenic pressure gradients, in five distinct European coastal and transitional ecosystems. Marine Pollution Bulletin 62 (2011) 499–513urn:x-ogc:def:crs:EPSG:3263315.347214371471647 41.8650453647784715.538521584928217 41.902422845206125http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=50430f91-7aea-494b-9624-c46357738d2egeonode:lesina_old_inlets_data_fidelibus_et_al_2011Nella Tabella .dbf: Nome del canale (Name); Fonte dati (Source). Canali che precedentemente collegavano la laguna di Lesina al mare ed ora interrati. Data da Fidelibus et al. 2011 (Human-induced hydrogeological changes and sinkholes in the coastal gypsum karst of Lesina Marina area) doi:10.1016/j.enggeo.2010.12.003urn:x-ogc:def:crs:EPSG:3263315.292608614701685 41.8908687782788215.550083684124651 41.91662233385399http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=fddae8db-c9ab-48e4-86f8-51dca40cefc4geonode:lesina_macrobenthos_february1997_data_digitized_frNella tabella .dbf: Number of repeated samples; Number of Species; Density ind/m2; Biomass g/m2; Dominanza ind; Dominanza biomass; Shannon Diversity Index individual (H); H min - H max; Pielou Index (J). Variazione spazio-temporale delle comunitá macrozoobentiche della Laguna di Lesina. Campionamenti In Aprile 1997 in 3 siti. Piscitelli et al. 2000. Macrobenthos of soft bottoms of the Lesina lagoon. Biol. Mar. Medit. (2000), 7(1): 723-727 urn:x-ogc:def:crs:EPSG:3263315.347214371471647 41.8655289791144715.422765724057394 41.89123233311332http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=e60e1f93-e3e8-46fa-b75c-f3a70dad279fgeonode:lesina_indice_biocenotico_aprile1997_data_digitizeNella tabella .dbf: Number of repeated samples; Number of Species; Density ind/m2; Biomass g/m2; Dominanza ind; Dominanza biomass; Shannon Diversity Index individual (H); H min - H max; Pielou Index (J). Variazione spazio-temporale delle comunitá macrozoobentiche della Laguna di Lesina. Campionamenti In Aprile 1997 in 3 siti. Piscitelli et al. 2000. Macrobenthos of soft bottoms of the Lesina lagoon. Biol. Mar. Medit. (2000), 7(1): 723-727urn:x-ogc:def:crs:EPSG:3263315.347214371471647 41.8655289791144715.422765724057394 41.89123233311332http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=2863f2b8-8ab7-4372-87bb-15b1d1c96cdcgeonode:lesina_macrobenthos_july1997_data_digitized_from_pNella tabella .dbf: Number of repeated samples; Number of Species; Density ind/m2; Biomass g/m2; Dominanza ind; Dominanza biomass; Shannon Diversity Index individual (H); H min - H max; Pielou Index (J). Variazione spazio-temporale delle comunitá macrozoobentiche della Laguna di Lesina. Campionamenti In Aprile 1997 in 3 siti. Piscitelli et al. 2000. Macrobenthos of soft bottoms of the Lesina lagoon. Biol. Mar. Medit. (2000), 7(1): 723-727 urn:x-ogc:def:crs:EPSG:3263315.347214371471647 41.8655289791144715.422765724057394 41.89123233311332http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=bee480c5-5c27-4ca4-a04f-edb8594966e3geonode:lesina_macrobenthos_nov1997_data_digitized_from_piNella tabella .dbf: Number of repeated samples; Number of Species; Density ind/m2; Biomass g/m2; Dominanza ind; Dominanza biomass; Shannon Diversity Index individual (H); H min - H max; Pielou Index (J). Variazione spazio-temporale delle comunitá macrozoobentiche della Laguna di Lesina. Campionamenti In Aprile 1997 in 3 siti. Piscitelli et al. 2000. Macrobenthos of soft bottoms of the Lesina lagoon. Biol. Mar. Medit. (2000), 7(1): 723-727 urn:x-ogc:def:crs:EPSG:3263315.347214371471647 41.8655289791144715.422765724057394 41.89123233311332http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=54945d4f-8b1e-4c81-b539-77bcfcbf6566geonode:lesina_metals_sediments_data_from_andresini28 Campioni di sedimento 28. Analisi granulometrica e dei metalli. Data di campionamento non riportata nel poster di Andresini da cui sono stati presi i dati. Nella Tabella dbf le concentrazioni di metalli sono espresse in ppmurn:x-ogc:def:crs:EPSG:3263315.31678548912879 41.8684084528260615.542161000307264 41.909070951352575http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=05f651fa-9ab3-4f73-8105-25ed52a8a63ageonode:nutrients_march_1995_data_sogesidCampagna di campionamento condotta nel marzo 1995 dalla SOGESID (Bari) per la Regione Puglia (Report: Sogesid 2002, Regione Puglia, Commissario delegato per l’emergenza ambientale, Presidente della Regione Puglia 2002. (Ordinanza del Ministro dell'Interno n° 3184 del 22/3/2002). Attivita’ connesse alla redazione del apiano di tutela delle acque (D. Lgs. 152/99 e successive modifiche ed integrazioni). Piano direttore a stralcio del piano di tutela della acque- Piano Generale). Parametri misurati: T (°C), Salinity (I), Dissolved Oxygen (ppm),pH, NH4 (µg/l), NO2(µg/l), NO3(µg/l);PO4(µg/l), Ptot(µg/l), Esaclorobenzene(µg/l), Lindano(µg/l), p p-DDT(µg/l), p p-DDE(µg/l), PCB 1260(µg/l), BHC(µg/l); Suspended solids (mg/l), solid sediment (ml/l), Tot COliform (MPN/100 ml), Fecal Cliform (MPN/100 ml), Tot Strept. (MPN/100 ml), fecal Strept. (MPN/100 ml), Chlorophyl A (µg/l]urn:x-ogc:def:crs:EPSG:3263315.319334726927858 41.86817917564026515.522512451878697 41.9022582111448http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=ba59d19d-1351-4454-bd1d-5f021e1ee61fismar:wrt_venicecoastlineNo abstract providedurn:x-ogc:def:crs:EPSG:300412.132440758470514 45.1733323028710312.603499582435893 45.57028207680584http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=6c10a3cf-8e28-4c6f-8773-4c3346cfea76geonode:minio_and_spada_collection_v1Sampling stations in the Minio and Spada Collection, Algarium Veneticumminio_and_spada_collection_v1featuresurn:x-ogc:def:crs:EPSG:432612.270489692688 45.203647613525412.3794603347778 45.4623641967773http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=01c358a2-dc17-11e6-897d-005056bd48e7shyfem:shyfem_venicecoastlineIl layer mostra l'area di lavoro utilizzao dal modello di calcolo SHYFEMshyfem_venicecoastlinefeaturesurn:x-ogc:def:crs:EPSG:300412.132286118476452 45.18093047102091512.568994573393807 45.56954926806243http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=95353cbe-b4c0-4c17-99d3-412245c0fd04geonode:operational_lagoonal_units_lagoon_of_veniceNo abstract providedurn:x-ogc:def:crs:EPSG:300412.12221325422575 45.1464817379700112.579554478665461 45.60382296240972http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=d11b9008-c3a5-479d-9728-2b223f48fda4geonode:venice_lagoon_ecosystem_project_palude_della_rosa__macrozoobenthos_sampling_stationsProgetto Sistema Lagunare Veneziano (UNESCO - MURST). Comunità macrozoobentonica in Palude della Rosa, 1991, 42 stazioni di campionamento.urn:x-ogc:def:crs:EPSG:300412.409609955382903 45.49752515788958412.441019108335375 45.52787618767852http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=c94e36b7-c906-4cc8-a8b3-35064876eca0geonode:layer_4891bc9c_ac9f_96d4_24cf_321dd8fc1ad1Location, functionality, and condition of public drinking fountains in Venice, Murano, Burano, Mazzorbo, Torcello, Vignole, and Sant'Erasmo. Collected in 2014 by students from Worcester Polytechnic Institute's Venice Project Center.layer_4891bc9c_ac9f_96d4_24cf_321dd8fc1ad1featuresurn:x-ogc:def:crs:EPSG:432612.312986 45.4244942612.419411 45.497866http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=0ad100c0-853e-11e4-bc7c-005056bd48e7geonode:ritmare_sp3_wp3_tsunami_italiaNo abstract providedurn:x-ogc:def:crs:EPSG:43267.702819 36.70230318.496408 45.649972http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=bd1f9f16-f3f2-4888-9e26-c5d63643be5cgeonode:retepozziIdentificazione e attributi dei pozzi appartenenti alla rete di monitoraggio della falda artesiana. La rete è stata istituita già nel 1970 da ISMAR Venezia al fine di poter seguire l’evoluzione delle pressioni di strato e, in caso di nuovi abbattimenti piezometrici, poter intervenire per tempo e prevenire nuovi conseguenti abbassamenti del suolo.urn:x-ogc:def:crs:EPSG:300412.046106099667254 45.18706665279060512.568767987599458 45.5638126262061http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=caee8466-958d-472a-95f5-7be3c23a2235geonode:retepozzi_v2Il layer permette di individuare la localizzazione dei pozzi e di vederne la monografia (una volta a perta la mappa). I pozzi sono tutti afferenti la falda artesiana a diverse profondità nel sottosuolo della provincia di Venezia. freatimetropressionepozzofaldaurn:x-ogc:def:crs:EPSG:432612.0507253440007 45.192267383848412.5567646416736 45.5614267507769http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=bedcb436-c8f6-11e5-ae6d-005056bd48e7geonode:ssd_pesca_transetto_12_stazioni_golfo_di_manfreson Transetto costa-largo: Profondità misurate di 12 Stazioni della campagna oceanografica, per l'approfondimento delle analisi di batimetria, analisi sedimenti. urn:x-ogc:def:crs:EPSG:432615.96145 41.4414316.39715 41.81052http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=1b104a07-9b8f-4290-97fe-0e426563ab41geonode:siti_osservativi_fissi_nel_golfo_di_manfredonia_teMeda Gargano e Antenne H/F in SSD Pescaurn:x-ogc:def:crs:EPSG:432615.35148261531889 41.54564148923109516.192216218849165 41.928658970803944http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=882cb3a9-3474-47fb-abaa-532d479e0ef5geonode:transetti_campionamento_golfo_di_manfredonia_campaCoordinate dei punti di campionamento 42 stazioni: transetti del Golfo di Manfredonia prima campagna marzo 2012. Le stazioni sono utilizzate per le campagne oceanografiche e il rilevamento dei parametri ambientali, in alcune stazioni il benthos, la chla e il fitoplancton. Ismar Lesina, in collaborazione con l U.O.S. di Ancona.urn:x-ogc:def:crs:EPSG:432615.961449 41.29295616.714904 41.889614http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=3e89e0c4-0f78-4c43-b338-853e6ebc2270geonode:stazioni_3_12Identificazione delle stazioni di misura del progetto CORILA 3.12: STRUTTURA, DINAMICA E CARATTERISTICHE FUNZIONALI DELLE COMUNITÀ BIOLOGICHE DOMINATE DA MACROFITE E DA ALGHE PLANCTONICHE urn:x-ogc:def:crs:EPSG:432612.26 45.39312.426 45.499http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=8fb12d3c-4020-4486-8513-886a8b249d83geonode:wrt_zooIl tempo di residenza è stato calcolato sulla base della circolazione della laguna di Venezia, con le strutture fisse del mose, riprodotta da un modello idrodinamico (SHYFEM) applicato nella sua versione tridimensionale barotropica sottoposto a di forzanti di marea e vento reali. La mappa riporta il tempo di residenza calcolato su tutti i livelli, l'unità di misura è il giorno. urn:x-ogc:def:crs:EPSG:300412.132440808758249 45.0399355209403612.751189755817993 45.57322304860559http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=f9efdb2a-b0e0-4e9f-80d3-24ff31f5ee0fgeonode:singlebeam_bathymetry_adriaticseaThe Istituto di Scienze Marine (ISMAR-CNR) conducted several research projects in the Italian side of the Adriatic Sea over more than 15 years collecting bathymetric, geophysical, and sediment core data to perform multidisciplinary studies of the modern sediment dynamics and of past environmental changes during the last eustatic cycle. A crucial step in this direction was the construction of a detailed bathymetry, a time-consuming task due to the extensive shallow water portion of the basin. Given the setting of the Adriatic Sea and the long-lasting research effort, the bathymetric map is necessarily based on heterogeneous data with uneven spatial distribution of Single Beam echosoundings.featuressinglebeam_bathymetry_adriaticseaurn:x-ogc:def:crs:EPSG:432612.2524776713704 40.81591231997819.1205814070133 45.773596072888http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=e207f87a-e152-11e5-bad5-005056bd48e7geonode:uso_del_suolo_provincia_di_foggiaIl layer dell'uso del suolo è stato fornito dalla Provincia di Foggiaurn:x-ogc:def:crs:EPSG:3263315.083154782624021 41.79710377563300515.667386522082428 41.94909987175373http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=388efa57-23e2-4f97-b72f-ba9d6bf5938bgeonode:varano_curve_di_livelloCurve di livello della Laguna di Varano (FG).urn:x-ogc:def:crs:EPSG:300415.678251058199834 41.844232164383315.810458063867806 41.91357364804438http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=80864c35-80f7-4800-a972-5e75cf7e594avpc:layer-fc0de2ed-5d1d-dcdb-9248-db43599a8ce8Islands of Venice in 1125 based on information found in ancient manuscripts.featureslayer-fc0de2ed-5d1d-dcdb-9248-db43599a8ce8urn:x-ogc:def:crs:EPSG:38571.10670693247E-4 4.098176130183E-41.11044715199E-4 4.099611871241E-4http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=c534338e-43d8-45f8-bfc8-c55afd5c359cvpc:layer-9baa93b4-ee30-9540-feb0-f25490f104a7Islands of Venice in 1200 based on information found in ancient manuscripts.layer-9baa93b4-ee30-9540-feb0-f25490f104a7featuresurn:x-ogc:def:crs:EPSG:385712.315768447429747 45.6206880006103912.361441151239104 45.63667059641184http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=908acb11-d242-423d-bf6a-66e7552decbdgeonode:vessel_tracksTracce del traffico navale per l'alto Adriatico elaborate sulla base dei dati AIS. Layer creato a scopo dimostrativo e divulgativo.urn:x-ogc:def:crs:EPSG:43269.778472222222224 41.1375833333333316.87097222222222 45.80197222222222http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=e21e3060-4351-4368-bfca-1c1ee9c11017geonode:issos_dataissos_datafeaturesurn:x-ogc:def:crs:EPSG:432612.1458806991577 45.066902160644512.6547193527222 45.5704956054688geonode:serie_parcoNo abstract providedurn:x-ogc:def:crs:EPSG:2303211.66011578727203 45.81849601579562412.545774062783993 46.58002746534099http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=7581d215-5b8c-4c0c-a159-8080dce9b25fgeonode:lineaLinea di livellazione della rete di monitoraggio altimetrico denominata "Collalto Montello" con in evidenza i poligoni della Linea.featureslineaurn:x-ogc:def:crs:EPSG:432612.1385137677199 45.799833569643712.2981877906205 45.9037247103468http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=1fb364cc-be97-11e5-b9f9-005056bd48e7geonode:macrophytobenthos_campionamento_2001_marzano_et_alNo abstract providedmacrophytobenthos_campionamento_2001_marzano_et_alfeaturesurn:x-ogc:def:crs:EPSG:3263315.34354619040815 41.8709580288812315.516351023673467 41.90336282565041http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=5f45b5c7-9a1b-4012-bd89-de9e5cdfff15geonode:bocca_porto_mose_chioggiaStazioni Campionamento Chioggia-Bocca di Lido: progressi nel contesto delle linee di ricerca CORILA 3.15 e 1.16, inerenti le origini della sabbia ed il suo trasporto alle bocche della laguna di Venezia. L’approccio scelto è molto vario ed include lunghe serie temporali di misure alle bocche, inferenze sulle variazioni morfologiche del fondale, misure dirette del trasporto di sabbia e misure geofisiche per il monitoraggio delle più importanti strutture. Dai risultati ottenuti sino ad oggi si rileva chiaramente un ingresso di sabbia all’interno della Laguna di Venezia lungo il margine nord della bocca di Lido, e si ha invece un export di sabbia altrove. Alla bocca di Lido, circa 2 giorni dopo un evento di grande portata fluviale, riscontriamo un significante ingresso d’acqua dolce, sedimento fino e materia vegetale. Questo flusso d’acqua dolce ricco di materia vegetale si ritrova in prossimità del fondo ed è più abbondante durante le piena montante, mentre il particellato fine si muove nello strato superficiale e si dirige verso l’interno della laguna.lagunaVeneziadiurn:x-ogc:def:crs:EPSG:432612.253838 45.21929212.309157508412 45.300647http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=7f636fb6-112b-11e6-9f18-005056bd48e7geonode:venice_fountainNo abstract providedvenice_fountainfeaturesurn:x-ogc:def:crs:EPSG:432612.31505121 45.4244942612.36021812 45.44727348http://cigno.ve.ismar.cnr.it/catalogue/csw?outputschema=http%3A%2F%2Fwww.opengis.net%2Fcat%2Fcsw%2Fcsdgm&service=CSW&request=GetRecordById&version=2.0.2&elementsetname=full&id=bc2fabf4-68cf-11e4-b783-005056bd48e7gml:Envelopegml:Pointgml:LineStringgml:PolygonLessThanGreaterThanLessThanEqualToGreaterThanEqualToEqualToNotEqualToLikeBetweenNullCheckabsabs_2abs_3abs_4acosAddCoveragesAffineAggregateAreaarea2AreaGridasinatanatan2BandMergeBandSelectBarnesSurfaceBatchDownloadbetweenboundaryboundaryDimensionBoundsbufferBufferFeatureCollectionbufferWithSegmentsCategorizeceilcentroidclassifyClipCollectGeometriesCollection_AverageCollection_BoundsCollection_CountCollection_MaxCollection_MedianCollection_MinCollection_NearestCollection_SumCollection_UniqueConcatenatecontainsContourconvertconvexHullcosCountCropCoveragecrossesdateFormatdateParsedensifydifferencedimensiondisjointdisjoint3Ddistancedistance3Ddouble2boolendAngleendPointenvenvelopeEqualIntervalequalsExactequalsExactToleranceequalToexpexteriorRingFeaturefloorgeometryTypegeomFromWKTgeomLengthGeorectifyCoverageGetFullCoveragegetGeometryNgetXgetYgetzgreaterEqualThangreaterThanGridHeatmapidIEEEremainderif_then_elseImportin10in2in3in4in5in6in7in8in9InclusionFeatureCollectionint2bboolint2ddoubleinteriorPointinteriorRingNInterpolateintersectionIntersectionFeatureCollectionintersectsintersects3DisClosedisCoverageisEmptyisInstanceOfisLikeisNullisometricisRingisSimpleisValidisWithinDistanceisWithinDistance3DJenkslengthlessEqualThanlessThanlistlogLRSGeocodeLRSMeasureLRSSegmentmaxmax_2max_3max_4minmin_2min_3min_4mincircleminimumdiameterminrectanglemoduloMultiplyCoveragesNearestnotnotEqualTonumberFormatnumberFormat2numGeometriesnumInteriorRingnumPointsoctagonalenvelopeoffsetoverlapsPagedUniqueparameterparseBooleanparseDoubleparseIntparseLongpiPointBufferspointNPointStackerPolygonExtractionpolygonizepowpropertyPropertyExistsQuantileQueryrandomRangeLookupRasterAsPointCollectionRasterZonalStatisticsRecodeRectangularCliprelaterelatePatternreprojectReprojectGeometryrescaleToPixelsrintroundround_2roundDoubleScaleCoveragesdo_nnsetCRSsimplifysinSnapsplitPolygonsqrtStandardDeviationstartAnglestartPointStoreCoveragestrCapitalizestrConcatstrEndsWithstrEqualsIgnoreCasestrIndexOfstringTemplatestrLastIndexOfstrLengthstrMatchesstrPositionstrReplacestrStartsWithstrSubstringstrSubstringStartstrToLowerCasestrToUpperCasestrTrimstrTrim2StyleCoveragesymDifferencetantoDegreestoRadianstouchestoWKTTransformunionUnionFeatureCollectionUniqueUniqueIntervalVectorToRasterVectorZonalStatisticsverticeswithin