Chronological records of metal deposition in sediments from the Strait of Sicily, central Mediterranean: Assessing natural fluxes and anthropogenic alteration

TitleChronological records of metal deposition in sediments from the Strait of Sicily, central Mediterranean: Assessing natural fluxes and anthropogenic alteration
Publication TypeArticolo su Rivista peer-reviewed
Year of Publication2010
AuthorsTranchida, G., Bellanca A., Angelone Massimo, Bonanno A., Langone L., Mazzola S., Neri R., and Patti B.
JournalJournal of Marine Systems
Volume79
Pagination157-172
ISSN09247963
Keywords<sup>210</sup>Pb chronology, Accumulation rate, Agricultural chemicals, algorithm, Anthropogenic inputs, Background value, Box-core sediments, Central Mediterranean, Chemical variability, Chromium, coastal zone, Combined effect, Current flowing, data set, Data sets, Element distribution, Flow currents, In-situ, Landforms, Lead, Magmatic activity, Major and trace elements, Mercury (metal), Metal deposition, Metal recovery, Morphology, Natural fluxes, Sea floor, sediment chemistry, sediment core, Sedimentology, Sediments, Statistical algorithm, statistical analysis, Strait of Sicily, Thermohaline, Trace analysis, trace element, Trace elements, Trace metal, Water depth
Abstract

Sediment box-cores were recovered from the Strait of Sicily along two onshore-offshore transects in water depths of 29-500 m. Samples were dated by 210Pb and analysed for major and trace elements. Inspections of chronological profiles integrated with application of statistical algorithms to the geochemical dataset and supported by in situ hydrological observations were used to assess factors driving element distributions. Mineralogical and chemical variability of sediments offshore of the southwestern Sicily coast reflect the irregular sea floor morphology of the Adventure Bank. Anthropogenic inputs explain enrichments with respect to background values for Sb, As, Pb, and Hg, that become more marked since approximately the 1960s. Clear fluctuations of major and trace element concentrations along a + 150 year record and high background values of some trace metals (notably Cr, Ni, and locally As) are interpreted as signals of geothermal and/or magmatic activities in the Strait of Sicily. A combined effect of current flowing, sea floor morphology and thermohaline gradient appears to encourage trace metal accumulation in front of the southern coast of Sicily. © 2009 Elsevier B.V. All rights reserved.

Notes

cited By 10

URLhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-70350780189&doi=10.1016%2fj.jmarsys.2009.08.001&partnerID=40&md5=4d8e737d59c54919f176090ade86cd31
DOI10.1016/j.jmarsys.2009.08.001