210Pb mass accumulation rates in the depositional area of the Magra River (Mediterranean Sea, Italy)
| Autor: | Antonio Schirone, Roberta Delfanti, Mattia Barsanti, F. Conte, Ivana Delbono |
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| Přispěvatelé: | Delfanti, R., Conte, F., Schirone, A., Barsanti, M., Delbono, I. |
| Jazyk: | angličtina |
| Rok vydání: | 2016 |
| Předmět: |
0106 biological sciences
010504 meteorology & atmospheric sciences 137Cs Sedimentation rate Aquatic Science Sediment cores Oceanography 01 natural sciences Ligurian Sea Sedimentary depositional environment Mediterranean sea 7Be River mouth 0105 earth and related environmental sciences geography geography.geographical_feature_category Flood myth Continental shelf 010604 marine biology & hydrobiology Sediment Geology Sedimentation rates 210Pb Current (stream) Sediment core Geochronology Physical geography 137C |
| Popis: | Nine sediment cores were collected between 2009 and 2012 in the inner continental shelf (Mediterranean Sea, Italy) mainly influenced by the Magra River, at water depths ranging from 11 to 64 m. Mass Accumulation Rates (MARs) were calculated through 210Pb analysed by Gamma spectrometry. Three different dating models (single and two-layer CF-CS, CRS) were applied to clay normalised 210Pbxs profiles and 137Cs was used to validate the 210Pb geochronology. The maximum MAR values (>2 g cm-2 yr-1) were found in the region adjacent to the Magra River mouth and outside the Gulf of La Spezia (0.9±0.1 g cm-2 yr-1 at St. 3-C6 and 4-C4). Results from 137Cs/210Pbxs ratios calculated in Surface Mixed Layers (SMLs) evidenced the coastal boundaries of the Magra River depositional area, which is very limited towards south. Differently, in the north-west sector, fine sediments are generally driven by the Ligurian Current and move towards north-west: at the deepest and most distant station from the River mouth, the MAR value is the lowest one in the study area.Few major Magra River floods occurred during the sediment core sampling period. By using the short-lived radioisotope 7Be as a tracer of river floods, a clear 7Be signature of 2009 flood is present at St. 1-SA1C. Finally, by analyzing the clay normalised 210Pbxs profiles, a decrease of its activity dating the years 1999 and 2000 is observed in four cores, corresponding to two major Magra River floods occurring in those years. © 2016 Elsevier Ltd. |
| Databáze: | OpenAIRE |
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