Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8263
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dc.contributor.authorallRenzi, M.; Research Centre in Lagoon ecology, fishery and aquaculture (Ecolab) Polo Universitario Grossetano, University of Siena,en
dc.contributor.authorallRomeo, T.; ISPRA – Higher Institute for Environmental Protection and Research, STS Palermoen
dc.contributor.authorallGuerranti, C.; Department of Environmental Science, University of Siena,en
dc.contributor.authorallPerra, G.; Department of Environmental Science, University of Siena,en
dc.contributor.authorallItaliano, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallFocardi, S. E.; Department of Environmental Science, University of Siena,en
dc.contributor.authorallEsposito, V.; ISPRA – Higher Institute for Environmental Protection and Research, STS Palermoen
dc.contributor.authorallAndaloro, F.; ISPRA – Higher Institute for Environmental Protection and Research, STS Palermoen
dc.date.accessioned2012-10-18T07:23:50Zen
dc.date.available2012-10-18T07:23:50Zen
dc.date.issued2011en
dc.identifier.urihttp://hdl.handle.net/2122/8263en
dc.description.abstractDegassing activity from marine shallow-water hydrothermal vents represents a natural important source of trace elements of particular ecotoxicological concern, such as Hg, Cd, Pb, and As. In 2002, on November 3rd, a submarine area of the Aeolian Archipelago (Italy) was affected by an exceptional hydrothermal activity, presumably associated to a significant trace element release. This study developed in the highest impacted area, was focused on different environmental matrices (water, sediment, primary producers, and fishes) with the aim to evaluate on a statistical basis temporal dynamics involving trace elements closed to the emission source. Results evidenced that this event produced significant changes in water column, modifying the general assessment of the chemical descriptors selected (Na, K, Mg, Ca, Cl, Br, SO4 2-, HCO3 -). Furthermore, the degassing activity represents a significant input of Hg, Cd, Pb, and As for all of the sampled matrices, being it responsible of the higher levels observed in the study area compared to controls. Concentrations measured in sediments and biota (Cystoseira compressa, Serranus cabrilla) at temporal intervals of ten months distanced, supported the occurrence of different time scale dynamics which are both element and matrix-dependent. In particular, levels of Cd and As measured in liver tissues of S. cabrilla evidenced a significant trend to increase with the time, allowing to exclude a quick recovery of the study area. Measured values in edible fishes tissues are, also, notably higher than risk limits proposed by the 2001/22/CE Directive for human consumption, so, local-based caught have to be accurately regulated to avoid the occurrence of diet over-exposure.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofProcedia Earth and Planetary Scienceen
dc.relation.ispartofseries/4 (2011)en
dc.subjecttrace elementsen
dc.subjecthydrothermal ventsen
dc.titleTemporal trends and matrix-dependent behaviors of trace elements closed to a geothermal hot-spot source (Aeolian Archipelago, Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber10-28en
dc.subject.INGV03. Hydrosphere::03.04. Chemical and biological::03.04.06. Hydrothermal systemsen
dc.identifier.doi10.1016/j.proeps.2011.11.003en
dc.relation.referencesStumm W, Morgan JJ. Aquatic chemistry: chemical equilibria and rates in natural waters, 3rd ed.; 1995. [2] Italiano F, Nuccio PM. Geochemical investigations on submarine volcanic exhalations to the East of Panarea, Aeolian Islands, Italy. J Volc & Geoth Res 1991; 46: 125-141. [3] Stuben D, Glasby GP. Geochemistry of shallow submarine hydrothermal fluids from Paleohori Bay, Milos, Aegean Sea. Exp Min Geol 1999; 8: 273–287. [4] Hannington M, Herzig P, Stoffer P, Scholten J, Botz R, Garbe-Schonberg D, Jonasson IP, Roest W. The Shipboard Scientific Party, First observations of high-temperature submarine hydrothermal vents and massive anhydrite deposits off the north coast of Iceland. Mar Geol 2001; 177: 199–120. [5] Hall-Spencer JM, Rodolfo-Metalpa R, Martin S, Ransome E, Fine M, Turner SM, Rowley SJ, Tedesco D, Buia MC. Volcanic carbon dioxide vents reveal ecosystem effects of ocean acidification. Nature 2008; 454, 96–99. [6] Vizzini S, Tommasello A, Di Malda G, Pirrotta M, Mazzola A, Calvo S. Effect of explosive shallow hydrothermal vents on 􀄯13C and growth performance in the seagrass Posidonia oceanica. J Ecol 2010; 98: 1284-1291. [7] Dando PR, Stùben D, Varnavas SP. Hydrothermalism in the Mediterranean Sea. Prog Oceanogr 1999; 44: 333-367.Price RE, Pichler T. Distribution, speciation and bioavailability of arsenic in a shallow-water submarine hydrothermal system, Tutum Bay, Ambitle Island, PNG. Chem Geol 2005; 224: 122-135. [9] Varnavas SP, Cronan DS (1988) Arsenic, antimony and bismuth in sediments and waters from the Santorini hydrothermal field, Greece. Chem Geol 1988; 67: 295-305. [10] Vidal VMV, Vidal FV, Isaacs JD. Coastal submarine hydrothermal activity off northern Baja California. J Geoph Res 1978; 83(B4): 1757-1774. [11] Lantzy RL, MacKenzie FT. Global cycles and assessment of man's impact. Geochim. Cosmochim. Acta 1979; 43: 511-515. [12] Price R, Pichler T. Measuring toxic elements and toxicity in marine shallow-water hydrothermal systems. In: Merkel BJ, Schipek M, editors. Research in shallow marine and fresh water systems. 1st International Workshop Proceedings, FOG Freiberg Online Geology. 2009, ISSN 1434-7512. 22: 82-86. [13] Gabbianelli G, Gillot PY, Lanzafame G, Romagnoli C, Rossi P L (1990) Tectonic and volcanic evolution of Panarea (Aeolian Islands, Italy). Mar. Geol. 92: 313-326. [14] Kokelaar P, Romagnoli C (1995) Sector collapse, sedimentation and clast population evolution at an active island-arc volcano: Stromboli, Italy. Bull. Volc. 57: 240-262. [15] Sedwick PN, Stuben D (1996) Chemistry of shallow submarine warm springs in an arc-volcanic setting: Volcano Island, Aeolian Archipelago, Italy. Mar. Chem. 53: 147-161. [16] Inguaggiato S., Italiano F Proceeding of the 9th International Symposium on Water-Rock Interaction-WRI9, 30 March–3 April 1998, Taupo, New Zealand, Arehart andHulston Rotterdam, 1998, p. 727–730. [17] Lucchi F. Late-Quaternary terraced marine deposits as tools for wide-scale correlation of unconformity-bounded units in the volcanic Aeolian archipelago (southern Italy). Sed. Geol. 2009; 216: 158–178. [18] Italiano F. Gas exhalation from the sea floor. Invited lecture at 25th course: Observational database and mechanisms of climate, Erice, Sicily, 21-27 November, 1998. [19] Chiocci FL, Bosman A, Romagnoli C, Tommasi P, De Alteris G. The December 2002 Sciara del Fuoco (Stromboli Island) submarine landslide: a first characterisation. EGS-AGU-EUG Joint Assembly, Nice, France, April 2003, Geophysical Research Abstracts. CDROM Version.Vol.5. [20] Gamberi F, Marani PM, Savelli C. Tectonic, volcanic and hydrothermal features of a submarine portion of the Aeolian arc (Tyrrhenian Sea). Mar Geol 1997; 140: 167-181. [21] Esposito A, Giordano G, Anzidei M. The 2002-2003 submarine gas eruption at Panarea volcano (Aeolian Islands, Italy): Volcanology of the seafloor and implications for the hazard scenario. Mar Geol 2006; 227: 119-134. [22] Gugliandolo C, Italiano F, Maugeri T. The submarine hydrothermal system of Panarea (southern Italy): biogeochemical processes at the thermal fluids - sea bottom interface. Ann Geophys 2006; 49(2/3): 783-792. [23] Buccianti A, Tassi F, Vaselli O. Compositional changes in a fumarolic field, Vulcano Island, Italy: a statistical case study. In: Buccianti A, Mateu-Figueras G, Pawlowsky-Glahn V (Eds) Compositional data analysis in the geoscience: from theory to practice. Geological Society, London, Special Publications. ISBN: 1-86239-205-6. http://www.geolsoc.org.uk 2006; 264: 67-77. [24] Caliro S, Caracausi A, Chiodini G, Ditta M, Italiano F, Longo M, Minopoli C, Nuccio PM, Paonita A, Rizzo A. Evidence of a recent input of magmatic gases into the quiescent volcanic edifice of Panarea, Aeolian Islands, Italy. Geophysic Res Lett 2004; 31(7): L07619. doi: 10.1029/2003GL019359 [25] Bauer K, Bauer D, Barth G. Flow rate measurements at submarine volcanic gas emissions. In: Merkel BJ, Schipek M, editors. Research in shallow marine and fresh water systems. 1st International Workshop Proceedings, FOG Freiberg Online Geology. ISSN 1434-7512. 2009; 22: 112-117. [26] Sieland R, Steinbrückner D, Hamel M, Merkel B, Schipek M. Geochemical investigations and gas quantification of submarine fluid discharges in the hydrothermal system of Panarea (Aeolian Islands, Italy) In: Merkel BJ, Schipek M (Eds) Research in shallow marine and fresh water systems. 1st International Workshop Proceedings, FOG Freiberg Online Geology. ISSN 1434- 7512. 2009; 22: 87-93. [27] Underwood AJ. On Beyond BACI: Sampling designs that might reliably detect environmental disturbances. Ecol Appl 1994; 4: 4-15.Underwood AJ, Chapman MG. Power, precaution, Type II error and sampling design in assessment of environmental impacts. J. Exp. Mar. Biol. Ecol. 2003; 296: 49-70. [29] Benedetti-Cecchi L. Experimental design and hypothesis testing in ecology. Biol Mar Medit 2004; 11(1): 407-455. [30] Sternbeck J, Östlund P. Metals in sediments from the Stockholm region: Geographical pollution patterns and time trends.Water Air Soil Pollut Focus 2001; 1: 151-165. [31] Zhang L, Ye X, Feng H, Jing Y, Ouyang T, Yu X, Liang R, Gao C, Chen W. Heavy metal contamination in western Xiamen Bay sediments and its vicinity, China. Mar Poll Bull 2007; 54: 974-982. [32] Clarke KR, Warwick RM. Change in marine communities: an approach to statistical analysis and interpretation. 2nd Edition. Primer-E: Plymouth 2001. [33] Somerfield PJ, Clarke K.R. A comparison of some methods commonly used for the collection of sublittoral sediments and their associated fauna. Mar Environ Res 1995; 43: 143-156. [34] Andaloro F, Romeo T, Renzi M, Guerranti C, Perra G, Consoli P, Perzia P, Focardi SE. Alteration of trace element levels in sediments and biota from the Aeolian Archipelago (Italy) following an episode of intense volcanic activity. Environ Monit Assessm 2011 (in press). [35] Pichler T. Marine shallow-water hydrothermal systems as natural laboratories. In: Merkel BJ, Schipek M (Eds) Research in shallow marine and fresh water systems. 1st International Workshop Proceedings, FOG Freiberg Online Geology. ISSN 1434-7512. 2009; 22: 77-81. [36] Fehn U, Cathles LM. The influence of plate movement on the evolution of hydrothermal convection cells in the oceanic crust. Tectonophysics 1986; 125: 289-312. [37] Capaccioni B, Tassi F, Vaselli O, Tedesco D, Poreda R. Submarine gas burst at Panarea Island (southern Italy) on 3 November 2002: A magmatic versus hydrothermal episode. J Geophysic Res Solid Earth 2007; 112: 1-15. [38] Prokop Z, Vangeheluwe ML, Van Sprang PA, Janssen CR, Holoubek I. Ecotox Environ Saf 2003; 34: 65. [39] Romano E, Ausili A, Nadezhda Z, Magno MC, Pavoni B, Gabellini M. Marine sediment contamination of an industrial site at Porto of Bagnoli, Gulf of Naples, Southern Italy. Mar Poll Bull 2004; 49: 487-495. [40] Barghigiani C, Ristori T, Lopez-Arenas J. Mercury in marine sediments from a contaminated area of the northern Tyrrhenian Sea: <20 _m grain-size fraction and total sample analysis. Sci Total Environ 1996; 192, 63–73. [41] Borghini F. Gli elementi in tracce negli ecosistemi costieri dell'Argentario. At Soc Tos Sci Nat Mem 1988; 105(A): 9-16. [42] Dalman Ö, Demirak A, Balci A. Determination of heavy metals (Cd, Pb) and trace elements (Cu, Zn) in sediments and fish of the Southeastern Aegean Sea (Turkey) by atomic absorption spectrometry. Food Chem 2005; 95(1): 157-162. [43] Storelli MM, Storelli A, Marcotrigiano GO. Heavy metals in the aquatic environment of the Southern Adriatic Sea, Italy. Macroalgae, sediments and benthic species. Environ Int 2001; 26: 505-509. [44] Volpi Ghirardini A, Birkemeyer T, Arzzi Novelli A, Delaney E, Pavoni B, Ghetti PF. An integrated approach to sediment quality assessment: the Venetian lagoon as a case study. Aquat Ecosyst Health Manage 1999; 2: 435-447. [45 Leoni L, Sartori F, Damiani V, Ferretti O, Viel M. Trace element distributions in surficial sediments of the northern Tyrrhenian Sea: contribution to heavy-metal pollution assessment. Environ Geol Wat Sci 1991; 17: 103-116. [46] Pichler T, Veizer J, Hall GEM.The chemical composition of shallow-water hydrothermal fluids in Tutum Bay, Ambitle Island, Papua New Guinea and their effect on ambient seawater. Mar Chem 1999; 64(3): 229-252. [47] Henley RW, Ellis AJ. Geothermal systems ancient and modern: a geothermical review. Earth-Science Rev 1983; 19: 1-50. [48] Nicholson K. Geothermal fluids. Springer-Verlag. 1992. [49] Sadiq M. Solubility equilibria of major elements in seawater and marine sediments, Toxic metal chemistry in marine environments. Dekker, M. Inc., New York. 1992. [50] Amodio-Cocchieri R, Amoroso S, Arnese A, Cirillo T, Montuori P, Triassi M. Pollution by Mercury, Arsenic, Lead, Chromium, Cadmium, and Polycyclic Aromatic Hydrocarbons of Fish and Mussels from the Gulf of Naples, Italy. Bull Environ Contam Toxicol 2003; 71: 551–560. [51] Abdallah M. Trace element levels in some commercially valuable fish species from coastal waters of Mediterranean Sea, Egypt. J Mar Syst 2008; 73: 114–122.Celik U, kran Cakli S, Oehlenschl J. Determination of the lead and cadmium burden in some northeastern Atlantic and Mediterranean fish species by DPSAV. Eur Food Res Technol 2004; 218: 298–305. [53] Pérez Cid B, Boia C, Pombo L, Rebelo E. Determination of trace metals in fish species of the Ria de Aveiro (Portugal) by electrothermal atomic absorption spectrometry. Food Chem 2001; 75: 93-100. [54] Bordajandi LR, Gomez G, Fernandez MA, Abad E, Rivera J, Gonzales MJ. Study on PCBs, PCDD/Fs, organoclorinepesticides, heavy metals and arsenic content in freshwater fish species from the River Turia (Spain). Chemosp 2003; 53: 163-171. [55] Usero J, Izquierdo C, Morillo J, Gracia I. Heavy metals in fish (Solea vulgaris, Anguilla anguilla and Liza aurata) from salt marshes on the southern Atlantic coast of Spain. Environ Int 2003; 29: 949-956. [56] Ureña R, Peri S, del Ramo J, Torreblanca A. Metal and metallothionein content in tissues from wild and farmed Anguilla anguilla at commercial size. Environ Int 2007; 33: 532-539. [57] Renzi M, Specchiulli A, Baroni D, Scirocco T, Cilenti L, Focardi S, Breber P, Focardi SE Trace elements in sediments and bioaccumulation in fish (Anguilla anguilla) in a Mediterranean lagoon (SE Italy) Int J Environ Anal Chem 2011 (in press). [58] Geeraerts C, Belpaire C. The effects of contaminants in European eel: A review. Ecotoxicol 2010; 19: 239-266. [59] Golovandova IL. Effects of heavy metals on the physiological and biochemical status of fishes and aquatic invertebrates. Inland Water Biol 2008; 1(1): 93-101. [60] Miller PA, Munkittrick KR, Dixon DG. Relationship between concentrations of copper and zinc in water, sediment, benthic invertebrates, and tissues of white sucker (Catostomus commersoni) Can J Fish Aquat Sci 1992; 49: 978-984. [61] Carlson E, Zelikoff JT. The immune system of fish: a target organ of toxicity. In: Di Giulio RT, Hinton DE (Eds). The toxicology of fishes. CRC Press, USA, 2008, p. 489-529. [62] Gony S. Short note on the effects of cadmium on the gill of the glass eel (Anguilla anguilla). Int Rev Gen Hydrobiol 1990; 75(6): 835-836. [63] Pierron F, Baudrimont M, Bossy A, Bourdinaud JP, Elie P, Massabuau JC. Impairment of lipid storage by cadmium in the European eel (Anguilla anguilla). Aquat Toxicol 2007; 81: 304-311. [64] Santos MA, Hall A. Influence of inorganic lead on the biochemical blood composition of the eel, Anguilla anguilla L. Ecotoxicol Environ Saf 1990; 20:7-9. [65] Food Standards Agency and the Department of Health (UK). Scientific Advisory Committee on Nutrition Metals and other elements in processed fish and fish products. Available online at http://www.food.gov.uk/science 2006.en
dc.description.obiettivoSpecifico1.8. Osservazioni di geofisica ambientaleen
dc.description.journalTypeN/A or not JCRen
dc.description.fulltextrestricteden
dc.relation.eissn1878-5220en
dc.contributor.authorRenzi, M.en
dc.contributor.authorRomeo, T.en
dc.contributor.authorGuerranti, C.en
dc.contributor.authorPerra, G.en
dc.contributor.authorItaliano, F.en
dc.contributor.authorFocardi, S. E.en
dc.contributor.authorEsposito, V.en
dc.contributor.authorAndaloro, F.en
dc.contributor.departmentResearch Centre in Lagoon ecology, fishery and aquaculture (Ecolab) Polo Universitario Grossetano, University of Siena,en
dc.contributor.departmentISPRA – Higher Institute for Environmental Protection and Research, STS Palermoen
dc.contributor.departmentDepartment of Environmental Science, University of Siena,en
dc.contributor.departmentDepartment of Environmental Science, University of Siena,en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentDepartment of Environmental Science, University of Siena,en
dc.contributor.departmentISPRA – Higher Institute for Environmental Protection and Research, STS Palermoen
dc.contributor.departmentISPRA – Higher Institute for Environmental Protection and Research, STS Palermoen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptResearch Centre in Lagoon ecology, fishery and aquaculture (Ecolab) Polo Universitario Grossetano, University of Siena,-
crisitem.author.deptISPRA – Higher Institute for Environmental Protection and Research, STS Palermo-
crisitem.author.deptDepartment of Environmental Science, University of Siena,-
crisitem.author.deptDepartment of Environmental Science, University of Siena,-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptDepartment of Environmental Science, University of Siena,-
crisitem.author.deptIstituto Superiore per la Protezione e la Ricerca ambientale (ISPRA), Milazzo, Italy; Sezione Oceanografia - OGS, Trieste, Italy-
crisitem.author.deptISPRA – Higher Institute for Environmental Protection and Research, STS Palermo-
crisitem.author.orcid0000-0002-9465-6398-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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