0000000000718746

AUTHOR

Lucilla Capotondi

0000-0003-3282-7910

showing 2 related works from this author

Possible impacts of Hg and PAH contamination on benthic foraminiferal assemblages: An example from the Sicilian coast, central Mediterranean

2007

The Palermo and Augusta urban/industrial areas (Sicily) are examples of contaminated coastal environments with a relatively high influx of unregulated industrial and domestic effluents. Three sediment box-cores were collected offshore of these urban/industrial areas in water depths of 60-150 m during two cruises (summers 2003/2004), dated by (210)Pb and (137)Cs, and analysed for total mercury concentration and total polycyclic aromatic hydrocarbon (PAH) concentration. Benthic foraminiferal assemblages were also examined (in terms of their distribution and morphology) to assess the potential use of benthic foraminifera as bioindicators of pollutant input and environmental change in these Med…

Mediterranean climateGeologic SedimentsmercuryEnvironmental Engineeringbenthic foraminiferachemistry.chemical_elementZooplanktonForaminiferaMediterranean seaMediterranean SeaAnimalsEnvironmental ChemistryDominance (ecology)Polycyclic Aromatic HydrocarbonsSicilyWaste Management and DisposalMercury PAHs 210Pb and 137Cs dating Benthic foraminifera Marine sediments SicilybiologyfungiPaleontologySedimentLead Radioisotopesbiology.organism_classificationPollutionMercury (element)PAHSOceanographychemistryCesium RadioisotopesBenthic zoneBioindicatorWater Pollutants ChemicalPb-210 and Cs-137 datingGeologyEnvironmental MonitoringScience of The Total Environment
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Globorotalia truncatulinoides in the Mediterranean Basin during the Middle–Late Holocene: Bio-Chronological and Oceanographic Indicator

2022

The planktonic foraminiferal species Globorotalia truncatulinoides is widely used as a biostratigraphic proxy for the Quaternary in the Mediterranean region. High-resolution quantitative studies performed on sediment cores collected in the central and western Mediterranean Sea evidence a significant abundance of G. truncatulinoides during the Middle Holocene. The robust chronological frame allows us to date this bio-event to 4.8–4.4 ka Before Present (BP), very close to the base of the Meghalayan stage (4.2 ka BP). As a consequence, we propose that G. truncatulinoides can be considered a potential marker for the Middle–Late Holocene chronological subdivision. G. truncatulinoides is a deep-d…

<i>Globorotalia truncatulinoides</i>; Meghalayan stage; 4.2 event; vertical mixing; Mediterranean SeaGloborotalia truncatulinoides4.2 eventGloborotalia truncatulinoides; Meghalayan stage; 4.2 event; vertical mixing; Mediterranean Seavertical mixingMediterranean SeaGeneral Earth and Planetary SciencesMeghalayan stageSettore GEO/01 - Paleontologia E Paleoecologia
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