Search results for " Stable Isotopes"

showing 10 items of 83 documents

Inter-habitat connectivity in a tropical ecosystem (Gazi Bay, Kenya) as revealed by ichthyofauna

2010

Settore BIO/07 - Ecologiafish mangrove coral reef seagrass stable isotopes organic matter export
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Spatial variations in habitat use and food habits of juvenile and adult fishes in a mangal ecosystem (Gazi Bay, Kenya)

2009

Settore BIO/07 - Ecologiafood webs mangroves coral reefs stable isotopes
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Exploitation of food sources by ichthyofauna in the Acquatina coastal system (Apulia, Italy)

2010

Settore BIO/07 - Ecologiafood webs stable isotopes fush niche partitioning spatial variations coastal pond Mediterranean
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Diet and trophic interactions of Paracentrotus lividus and Arbacia lixula in two alternative stable states of the Mediterranean rocky sublittoral com…

2010

Settore BIO/07 - Ecologiasea urchins food habits stable isotopes Mediterranean
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Stable carbon and nitrogen ratios (δ13Corg and δ15Ntot) of core sediments from the Gulf of Palermo (NW Sicily): implications for the carbon source

2010

Settore BIO/07 - Ecologiasedimentary records contamination trace metals organic matter stable isotopes urbanised areasSettore GEO/08 - Geochimica E Vulcanologia
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Habitat effect on distribution and feeding of Ophidiaster ophidianus (Lmk.) (Asteroidea)

2016

The purple starfish Ophidiaster ophidianus is an Atlanto-Mediterranean starfish protected under the EU’s Habitats Directive. Despite the wide distribution and the current range expansion of this warm affinity species in the northern Mediterranean areas, nothing is known about its diet. Using field observations and carbon (δ13C) and nitrogen (δ15N) stable isotopes, we explored possible changes in density and diet of O. ophidianus in relation to two different Mediterranean habitats: the coralline barren and the macro algae forest. Data were collected at the Marine Protected Area of Ustica Island (Southern Tyrrhenian Sea) from June to September 2009. Starfish density was not affected by the ha…

Settore BIO/07 - Ecologiathermophilic barren forest feeding stable isotopes
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Paleoenvironmental changes during the calcare di base deposition a prelude to the Messinian salinity crisis.

2006

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaMessinian Salinity Crisis Stable isotopes ForaminiferaSettore GEO/01 - Paleontologia E PaleoecologiaSettore GEO/08 - Geochimica E Vulcanologia
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Carbonate stromatolites from a Messinian hypersaline setting in the Caltanissetta Basin, Sicily: petrographic evidence of microbial activity and rela…

2010

Lower Messinian stromatolites of the Calcare di Base Formation at Sutera in Sicily record periods of low sea-level, strong evaporation and elevated salinity, thought to be associated with the onset of the Messinian Salinity Crisis. Overlying aragonitic limestones were precipitated in normal to slightly evaporative conditions, occasionally influenced by an influx of meteoric water. Evidence of bacterial involvement in carbonate formation is recorded in three dolomite-rich stromatolite beds in the lower portion of the section that contain low domes with irregular crinkly millimetre-scale lamination and small fenestrae. The dominant microfabrics are: (i) peloidal and clotted dolomicrite with c…

Settore GEO/07 - Petrologia E PetrografiaCalcare di Base Messinian microbial carbonate petrography rare earth elements Sicily stable isotopes stromatolitesSettore GEO/08 - Geochimica E Vulcanologia
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Nitrogen stable isotopes as tracers of biodeposition from a tuna farm in the Western Mediterranean

2007

Tuna farming stable isotopes Mediterranean Sea Thunnus thynnus
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Sea-level changes during the last 41,000 years in the outer shelf of the southern Tyrrhenian Sea: Evidence from benthic foraminifera and seismostrati…

2011

Abstract An integrated high resolution study based both on a seismostratigraphic approach and on a sedimentary core (VIB 10), collected in the outer shelf (127 m depth) from the southern Tyrrhenian Sea (Gulf of Termini, Sicily), provides new data about climatic, eustatic and paleoenvironmental changes during the last ∼41,000 years. The results based on the interpretation of a seismic profile, on benthic foraminifera assemblages and on δ18O records, allowed recognition of two drastic sea-level falls during the Last Glacial Maximum (LGM) and the Younger Dryas (YD). The short deglacial event, between LGM and YD, known as Bolling/Allerod, played an important role in the sea-level rise that prod…

Tyrrhenian Sea010506 paleontologySettore GEO/02 - Geologia Stratigrafica E Sedimentologicaδ18O[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Holocene climatic optimumbenthic foraminifera[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]010502 geochemistry & geophysics01 natural sciencesAllerød oscillationstable isotopes.ForaminiferaSea-level changeSea-level changes; Tyrrhenian Sea; benthic foraminifera; seismostratigraphic analysis; stable isotopes.14. Life underwaterYounger DryasSea levelComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyLast Glacial MaximumSettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationOceanography13. Climate actionBenthic zoneseismostratigraphic analysiGeology
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