0000000001321479

AUTHOR

Maurizio Ribera D'alcala

showing 2 related works from this author

(Table 1) Trace element/Ca ratios of Orbulina universa shells from late Neogene Mediterranean samples

2008

A Mediterranean composite sedimentary record was analyzed for Ba/Ca ratios on carbonate shells of Orbulina universa planktonic foraminifer (Ba/Ca)carb providing the opportunity to study and assess the extent of freshwater inputs on the basin and possible impacts on its dynamics during the Tortonian to Recent period. A number of scanning electron microscope analyses and auxiliary trace element measurements (Mn, Sr, and Mg), obtained from the same samples, exclude important diagenetic effects on the studied biogenic carbonates and corroborate the reliability of (Ba/Ca)carb ratios in foraminifera calcite as indicators of seawater source components during the studied interval. A long-term trend…

Leg160Longitude of eventLithology composition faciesInductively coupled plasma - mass spectrometry (ICP-MS)Barium Calcium ratioOcean Drilling Program (ODP)Latitude of eventManganese/Calcium ratioOrbulina universa Barium/Calcium ratioAGEOrbulina universaLeg107Inductively coupled plasma mass spectrometry ICP MSOutcrop sampleManganese Calcium ratioSample code/labelEvent labelJoides ResolutionLithology/composition/faciesSample code labelStrontium/Calcium ratioDrilling/drill rigDrilling drill rigOrbulina universa δ13COrbulina universa Magnesium/Calcium ratioδ13CEarth System ResearchOcean Drilling Program ODPMagnesium Calcium ratioStrontium Calcium ratioComposite Core
researchProduct

Chemistry of Globigerinoides ruber shells from ODP Site 160-963

2013

Here we present a high-resolution faunal, floral and geochemical (stable isotopes and trace elements) record from the sediments of Ocean Drilling Program Site 963 (central Mediterranean basin), which shows centennial/millennial-scale resemblance to the high-northern latitude rapid temperature fluctuations documented in the Greenland ice cores between 20 and 70 kyr BP. Oxygen and carbon isotopes, planktic foraminifera and calcareous nannofossil distributions suggest that Dansgaard-Oeschger (D/O) and Heinrich events (HE) are distinctly expressed in the Mediterranean climate record. Moreover, recurrent though subdued oscillations not previously identified in the Lateglacial Mediterranean sedim…

Leg160Joides ResolutionOcean Drilling Program (ODP)Composite Core
researchProduct