0000000000620915

AUTHOR

Paolo Montagna

0000-0001-5598-2214

showing 12 related works from this author

The “chimney forest” of the deep Montenegrin margin, south-eastern Adriatic Sea

2015

A spectacular field of columnar carbonates has been discovered on the Montenegrin margin in the southern Adriatic Sea at a depth of about 450 m. The site exposes many columnar carbonates protruding from the substrate or abated on the bottom. Such carbonates attain maximum visible lengths of ca. 60 cm with diameters up to 20 cm; display an annular growth, and are either hollow or plugged by indurated sediment. Petrographic and geochemical analyses document the pervasive presence of dolomite, and delta C-13 values as low as -30%(0) VPDB. These 'chimneys' are therefore interpreted as former conduits related to hydrocarbon expulsion in this sector of the Adriatic basin. However, available data …

Adriatic SeaSessile fauna010504 meteorology & atmospheric sciencesHydrocarbonStratigraphyDolomite010502 geochemistry & geophysicsOceanography01 natural scienceslaw.inventionSedimentary depositional environmentchemistry.chemical_compoundPaleontologylawChimney14. Life underwaterGlacial periodRadiocarbon datingCarbonate chimneys[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentLithificationComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereSedimentGeology15. Life on landGeophysicschemistryROVCoralsCarbonateEconomic GeologyGeology
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A Review of 2000 Years of Paleoclimatic Evidence in the Mediterranean

2012

[EN] The integration of climate information from instrumental data and documentary and natural archives; evidence of past human activity derived from historical, paleoecological, and archaeological records; and new climate modeling techniques promises major breakthroughs for our understanding of climate sensitivity, ecological processes, environmental response, and human impact. In this chapter, we review the availability and potential of instrumental data, less well-known written records, and terrestrial and marine natural proxy archives for climate in the Mediterranean region over the last 2000 years. We highlight the need to integrate these different proxy archives and the importance for…

Mediterranean climateGeographyNatural rangeLand useClimatology550 Earth sciences & geologyPaleoclimatologyClimate sensitivityClimate model910 Geography & travelPhysical geographyTemporal scalesProxy (climate)
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Preservation of modern and mis 5.5 erosional landforms and biological structures as sea level markers: A matter of luck?

2021

The Mediterranean Basin is characterized by a significant variability in tectonic behaviour, ranging from subsidence to uplifting. However, those coastal areas considered to be tectonically stable show coastal landforms at elevations consistent with eustatic and isostatic sea level change models. In particular, geomorphological indicators—such as tidal notches or shore platforms—are often used to define the tectonic stability of the Mediterranean coasts. We present the results of swim surveys in nine rocky coastal sectors in the central Mediterranean Sea using the Geoswim approach. The entire route was covered in 22 days for a total distance of 158.5 km. All surveyed sites are considered to…

Marine isotope stageSettore BIO/07 - EcologiaErosion -- Mediterranean RegionBiological indicators; Coastal geomorphology; Geoswim; Landforms; Mediterranean Sea; MIS 5.5; Sea level change010504 meteorology & atmospheric sciencesGeography Planning and DevelopmentGeoswimAquatic ScienceCoastal geography010502 geochemistry & geophysicsBiological indicator01 natural sciencesBiochemistryNeotectonics -- Mediterranean RegionMediterranean seaMediterranean SeaSea level changeTD201-500Sea level0105 earth and related environmental sciencesWater Science and TechnologyShoregeographyPast sea levelgeography.geographical_feature_categorycoastal geomorphologyWater supply for domestic and industrial purposesCoast changes -- Mediterranean Region -- Case studiesSubsidenceHydraulic engineeringcoastal geomorphology MIS 5.5 landforms biological indicators sea level change Mediterranean Sea GeoswimSettore GEO/01 - Paleontologia E Paleoecologiabiological indicatorsCoastal geomorphologyMIS 5Sea level -- Mediterranean RegionMIS 5.5LandformInterglacialBeach erosion -- Mediterranean RegionPhysical geographyTC1-978landformssea level changeGeology
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Feasibility study for the measurement of πN transition distribution amplitudes at P¯ANDA in p¯p→J/ψπ0

2017

The exclusive charmonium production process in (P) over barp annihilation with an associated pi 0 meson (p) over barp -> J/psi pi(0) is studied in the framework of QCD collinear factorization. The feasibility of measuring this reaction through the J/psi -> e(+) e(-) decay channel with the AntiProton ANnihilation at DArmstadt ((P) over bar ANDA) experiment is investigated. Simulations on signal reconstruction efficiency as well as the background rejection from various sources including the (P) over barp -> pi(+)pi(-)pi(0) and (p) over barp -> J/psi pi(0)pi(0) reactions are performed with PANDAROOT, the simulation and analysis software framework of the (P) over bar ANDA experiment. It is show…

Quantum chromodynamicsPhysicsParticle physicsLuminosity (scattering theory)AnnihilationMeson010308 nuclear & particles physics7. Clean energy01 natural sciencesParticle identificationNuclear physicsFactorizationAntiproton0103 physical sciencesHigh Energy Physics::Experiment010306 general physicsBar (unit)Physical Review D
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NEW RESULTS ON NONMESONIC WEAK DECAY OF Lambda HYPERNUCLEI WITH FINUDA

2010

The FINUDA experiment has performed a systematic study of the NonMesonic Weak Decay (NMWD) of Λ hypernuclei analizing all the data collected from 2003 up to 2007. The results of a measurement of the spectra of protons coming from the NMWD of [Formula: see text], [Formula: see text], [Formula: see text], [Formula: see text], [Formula: see text], [Formula: see text], [Formula: see text] and [Formula: see text] are the subject of this paper.

Nuclear physicsPhysicsNuclear and High Energy PhysicsFINUDAHypernuclei; nonmesonic weak decay; proton spectraHypernucleiGeneral Physics and AstronomySpectral linenonmesonic weak decayproton spectra
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Recent results on mesonic weak decay of Λ-hypernuclei

2010

The FINUDA experiment has performed a systematic study of mesonic weak decay of p-shell Λ-hypernuclei. Recent results on the mesonic decay spectra and ratios are illustrated and discussed.

Hypernuclei; mesonic weak decayPhysicsNuclear and High Energy PhysicsFINUDANuclear TheoryLambda-hypernucleiΛ-hypernucleiGeneral Physics and AstronomyLambda-hypernuclei; mesonic decay; spin assignmentAstrophysicsMesonic decayLambdaSpectral lineNuclear physicsSpin assignmentmesonic weak decayΛ-hypernuclei; Mesonic decay; Spin assignmentHypernucleiHigh Energy Physics::ExperimentNuclear Experiment
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Assessing vermetid reefs as indicators of past sea levels in the Mediterranean

2020

Abstract The endemic Mediterranean reef building vermetid gastropods Dendropoma petraeum complex (Dendropoma spp) and Vermetus triquetrus develop bio-constructions (rims) on rocky shorelines at about Mean Sea Level (MSL) and are therefore commonly used as relative sea-level (RSL) markers. In this study, we use elevations and age data of vermetid reefs to (1) re-assess the vertical uncertainties of these biological RSL indicators, and (2) evaluate the vertical growth rates along a Mediterranean east-west transect, in attempt to explain the differences found in both growth rates and uncertainties. In Israel, Differential Global Positioning System (DGPS) and laser measurements relative to the …

Settore BIO/07 - EcologiaMediterranean climateDendropoma petraeumTidal range010504 meteorology & atmospheric sciencesVermetid reefsSettore GEO/04 - Geografia Fisica E GeomorfologiaIntertidal zone010502 geochemistry & geophysicsOceanography01 natural sciences1907Geochemistry and PetrologyGrowth ratesMediterranean SeaReef1906Sea level0105 earth and related environmental sciencesgeographyBio-markers Growth rates Mediterranean Sea Past sea-level Vermetid reefsgeography.geographical_feature_categorybiologyDendropomaGeologybiology.organism_classificationOceanography1910Bio-markersSpatial variabilityPast sea-levelGeologyMarine Geology
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A stalactite record of four relative sea-level highstands during the Middle Pleistocene Transition

2017

International audience; Ice-sheet and sea-level fluctuations during the Early and Middle Pleistocene are as yet poorly understood. A stalactite from a karst cave in North West Sicily (Italy) provides the first evidence of four marine inundations that correspond to relative sea-level highstands at the time of the Middle Pleistocene Transition. The speleothem is located ∼97 m above mean sea level as result of Quaternary uplift. Its section reveals three marine hiatuses and a coral overgrowth that fixes the age of final marine ingression at 1.124 ± 0.2, thus making this speleothem the oldest stalactite with marine hiatuses ever studied to date. Scleractinian coral species witness light-limited…

Marine isotope stageArcheology010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia Strutturale010502 geochemistry & geophysics01 natural sciencesSea level changeStable isotopesGlobal and Planetary Changegeography.geographical_feature_categoryEcologyArcheology (arts and humanities)Geology87Sr/86Sr ageSpeleothemStable isotopePleistocene87Sr/86Sr agesOceanographyArchaeology[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologySr/Sr agesPaleogeographyCoralsGeologyStalactitePleistoceneEvolutionSpeleothemWestern Europecoastal/dk/atira/pure/sustainabledevelopmentgoals/life_below_water87Sr/86 41 Sr agesPaleontologyInterglacial(s)Behavior and Systematics14. Life underwaterSDG 14 - Life Below Water[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentSea levelEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesU-Th datinggeographyGeomorphologySettore GEO/01 - Paleontologia E PaleoecologiaKarstEcology Evolution Behavior and SystematicSpeleothems87Sr/86Sr ages;Corals;U-Th dating;Pleistocene;Stable isotopes;Western Europe;Interglacial(s);Sea level changes;SpeleothemsSea level changesCoralQuaternaryGlobal and Planetary ChangeSettore ICAR/06 - Topografia E Cartografia
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Calcification is not the Achilles' heel of cold-water corals in an acidifying ocean

2015

Ocean acidification is thought to be a major threat to coral reefs: laboratory evidence and CO2 seep research has shown adverse effects on many coral species, although a few are resilient. There are concerns that cold-water corals are even more vulnerable as they live in areas where aragonite saturation (?ara) is lower than in the tropics and is falling rapidly due to CO2 emissions. Here, we provide laboratory evidence that net (gross calcification minus dissolution) and gross calcification rates of three common cold-water corals, Caryophyllia smithii, Dendrophyllia cornigera, and Desmophyllum dianthus, are not affected by pCO2 levels expected for 2100 (pCO2 1058 ?atm, ?ara 1.29), and nor a…

CnidariaSettore BIO/07 - EcologiaCaryophyllia smithiiCoralcold-water coralsocean acidificationengineering.materialCaryophyllia smithiiDendrophyllia cornigeraCold-water coralcalcification and dissolutionCalcification PhysiologicAnthozoaTheoryofComputation_ANALYSISOFALGORITHMSANDPROBLEMCOMPLEXITYComputingMethodologies_SYMBOLICANDALGEBRAICMANIPULATIONMediterranean SeaAnimalsEnvironmental ChemistrySeawaterGlobal ChangeReefDesmophyllum dianthuGeneral Environmental ScienceGlobal and Planetary ChangegeographyDesmophyllum dianthusgeography.geographical_feature_categorybiologyEcology2300EcologyAragoniteOcean acidificationfungiCalcification and dissolutionOcean acidificationCoral reefbiochemical phenomena metabolism and nutritionCarbon DioxideHydrogen-Ion Concentrationbiology.organism_classificationAnthozoaOceanographyengineeringCold-water coralsgeographic locationsMathematicsofComputing_DISCRETEMATHEMATICS
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Submerged speleothems and sea level reconstructions: a global overview and new results from the Mediterranean Sea

2021

This study presents a global overview of the submerged speleothems used to reconstruct paleo sea levels and reports new results from two stalactites collected in the Mediterranean Sea. Coastal cave deposits significantly contributed to the understanding of global and regional sea-level variations during the Middle and Late Quaternary. The studied speleothems cover the last 1.4 Myr and focused mainly on Marine Isotope Stages (MIS) 1, 2, 3, 5.1, 5.3, 5.5, 7.1, 7.2, 7.3 and 7.5. The results indicate that submerged speleothems represent extraordinary archives that can provide detailed information on former sea-level changes. The two stalactites collected in the central Mediterranean Sea, at Fa…

Sea level change010506 paleontologyStalactitevertical tectonic movementGeography Planning and DevelopmentAquatic Science010502 geochemistry & geophysics01 natural sciencesBiochemistryMediterranean seaCaveSea-level changeSea cave14. Life underwaterTD201-500Sea levelPhreatic[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/OceanographySea caves0105 earth and related environmental sciencesWater Science and Technology[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsgeographygeography.geographical_feature_categoryWater supply for domestic and industrial purposesPhreatic speleothemHydraulic engineeringFavignana; Phreatic speleothem; Sea caves; Sea-level change; Submerged speleothem; Ustica; Vertical tectonic movementsFavignanaOceanographyUsticaQuaternaryFavignana Phreatic speleothem Sea caves Sea-level change Submerged speleothem Ustica Vertical tectonic movementsTC1-978Submerged speleothemVertical tectonic movementsGeology
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The large-scale evolution of neodymium isotopic composition in the global modern and Holocene ocean revealed from seawater data and other records

2017

International audience; The large-scale evolution of neodymium isotopic composition in the global modern and Holocene ocean revealed from seawater data and other records. Kazuyo Tachikawa and project members Neodymium isotopic compositions (143 Nd/ 144 Nd or ε Nd) have been used as a tracer of water masses and lithogenic inputs to the ocean. To further evaluate the faithfulness of this tracer, we have updated a global seawater ε Nd database and combined it with hydrography parameters (temperature, salinity, nutrients and oxygen concentrations), carbon isotopic ratio and radiocarbon of dissolved inorganic carbon. Archive ε Nd data are compiled for leachates, foraminiferal tests, deep-sea cor…

[SDU.STU] Sciences of the Universe [physics]/Earth Sciences[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
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Calcification is not the Achilles'heel of cold-water corals in an acidifying ocean

2015

Ocean acidification is thought to be a major threat to coral reefs: laboratory evidence and CO2 seep research has shown adverse effects on many coral species, although a few are resilient. There are concerns that cold-water corals are even more vulnerable as they live in areas where aragonite saturation (Omega ara) is lower than in the tropics and is falling rapidly due to CO2 emissions. Here, we provide laboratory evidence that net (gross calcification minus dissolution) and gross calcification rates of three common cold-water corals, Caryophyllia smithii, Dendrophyllia cornigera, and Desmophyllum dianthus, are not affected by pCO2 levels expected for 2100 (pCO2 1058 µatm, Omega ara 1.29),…

Dissolution rateOcean Acidification International Coordination Centre (OA-ICC)TemperateIdentificationSalinityBicarbonate ion standard deviationinorganicAlkalinity total standard deviationAlkalinityExperimentTemperature waterCarbon inorganic dissolvedCalculated using seacarb after Nisumaa et al 2010Aragonite saturation stateRespiration rate oxygenAlkalinity totaltotalDesmophyllum dianthuspHRespirationTemperatureCalcification rate of calcium carbonatedissolvedLaboratory experimentCarbonate ionDeep seaPartial pressure of carbon dioxide (water) at sea surface temperature (wet air)Field experimentCarbon dioxide standard deviationTemperature water standard deviationContainers and aquaria 20 1000 L or 1 m 2Respiration rateEarth System ResearchContainers and aquaria (20-1000 L or &lt; 1 m**2)standard deviationCalcification/DissolutionPotentiometric titrationCalcite saturation statePotentiometricwaterPartial pressure of carbon dioxideCaryophyllia smithiiContainers and aquaria (20-1000 L or < 1 m**2)Dendrophyllia cornigeraFigureAragonite saturation state standard deviationBenthosCnidariaOcean Acidification International Coordination Centre OA ICCMediterranean SeaAnimaliaBicarbonate ionCalculated using seacarb after Nisumaa et al. (2010)SpeciesCalculated using CO2SYSfungiEvent labelDeep-seaPartial pressure of carbon dioxide standard deviationCarbonate system computation flagpH standard deviationCarbonate ion standard deviationbiochemical phenomena metabolism and nutritionFugacity of carbon dioxide (water) at sea surface temperature (wet air)CarbonTreatmentPartial pressure of carbon dioxide water at sea surface temperature wet airCarbon dioxideSingle speciesCalcification DissolutionFugacity of carbon dioxide water at sea surface temperature wet airBenthic animalsoxygen
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