PUMA
Istituto di Scienze Marine     
Barsanti M., Delbono I., Schirone A., Langone L., Miserocchi S., Salvi S., Delfanti R. Sediment reworking rates in deep sediments of the Mediterranean Sea. In: Science of the Total Environment, vol. 409 (15) pp. 2959 - 2970. ELSEVIER SCIENCE BV, PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS, 2011.
 
 
Abstract
(English)
Different pelagic areas of the Mediterranean Sea have been investigated in order to quantify physical and biological mixing processes in deep sea sediments. Herein, results of eleven sediment cores sampled at different deep areas (>2000 m) of the Western and Eastern Mediterranean Sea are presented. (210)Pb(xs), and (137)Cs vertical profiles, together with (14)C dating, are used to identify the main processes characterising the different areas and, finally, controlling mixing depths (SML) and bioturbation coefficients (D(b)). Radionuclide vertical profiles and inventories indicate that bioturbation processes are the dominant processes responsible for sediment reworking in deep sea environments. Results show significant differences in sediment mixing depths and bioturbation coefficients among areas of the Mediterranean Sea characterised by different trophic regimes. In particular, in the Oran Rise area, where the Almeria-Oran Front induces frequent phytoplankton blooms, we calculate the highest values of sediment mixing layers (13 cm) and bioturbation coefficients (0.187 cm(2) yr(-1)), and the highest values of (210)Pb(xs) and (137)Cs inventories. Intermediate values of SML and D(b) (similar to 6 cm and similar to 0.040 cm(2) yr(-1), respectively) characterise the mesothrophic Algero-Balearic basin, while in the Southern Tyrrhenian Sea mixing parameters (SML of 3 cm and D(b) of 0.011 cm(2) yr(-1)) are similar to those calculated for the oligotrophic Eastern Mediterranean (SML of 2 cm and D(b) of similar to 0.005 cm(2) yr(-1)). (C) 2011 Elsevier B.V. All rights reserved.
DOI: 10.1016/j.scitotenv.2011.04.025
Subject (210)pb
(137)CS
Sediment Mixing Layer SML
Bioturbation coefficients D(b)


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