Search results for "planktonic"

showing 10 items of 32 documents

Orbital variations in planktonic foraminifera assemblages from the Ionian Sea during the Middle Pleistocene Transition

2013

Abstract The Middle Pleistocene Transition (1.2–0.7 Ma) is the most recent re-organization of the global climate system which includes variations in the frequency and amplitude of glacial/interglacial cycles, increased ice sheet volume, sea surface temperature cooling and a significant drop in the CO 2 atmospheric levels. Here we present high-resolution planktonic foraminifera data (mean sampling resolution of about 780 years) from core LC10 recovered in the Ionian Sea (eastern Mediterranean), between 1.2 and 0.9 Ma. Selected taxa, among them G. ruber , T. quinqueloba and G. bulloides , show significant periodicities that can be associated to orbital cycles, mainly precession and obliquity.…

Planktonic foraminifera010504 meteorology & atmospheric sciencesPleistoceneMiddle Pleistocene Transition010502 geochemistry & geophysicsOceanography01 natural sciencesForaminiferaPaleontology14. Life underwaterGlacial periodEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesgeographyOrbital climate variabilitygeography.geographical_feature_categorybiologyPaleontologySapropelIonian SeaPlanktonic Foraminifera Eastern Mediterranean Middle Pleistocene transitionbiology.organism_classificationNeogloboquadrina pachyderma sinistral coilingSea surface temperatureOceanography13. Climate actionInterglacialIce sheetQuaternaryGeology
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The late Messinian "Lago-Mare" event and the Zanclean Reflooding in the Mediterranean Sea: New insights from the Cuevas del Almanzora section (Vera B…

2020

Abstract The return to normal marine conditions in the Mediterranean Sea after the end of the Messinian Salinity Crisis (MSC), that led to the deposition of thick evaporitic succession followed by settlement of brackish to freshwater conditions of the “Lago-Mare”, is still subject to extensive debate between two opposite scenarios. One scenario implies an abrupt reflooding through the Gibraltar gateway of the Mediterranean Sea previously disconnected from the world ocean and partly desiccated. The second scenario postulates that the Mediterranean Sea kept a high-water level throughout the Messinian Salinity Crisis and was connected continuously to the Atlantic Ocean and to the Paratethys. T…

Planktonic foraminifera010504 meteorology & atmospheric sciences[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]010502 geochemistry & geophysics01 natural sciencesLago-Mare event Mediterranean Sea Messinian-Zanclean transition Ostracods Oxygen and carbon stable isotopes of planktonic foraminifera Paleoenvironmental changes Planktonic foraminifera Zanclean refloodingForaminiferaPaleontologyMediterranean seaOstracodMediterranean SeaLago-Mare eventOxygen and carbon stable isotopes of planktonic foraminifera14. Life underwaterChronostratigraphyMessinian-Zanclean transitionGlobigerinoidesComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesMilankovitch cyclesbiologyBrackish waterOstracodsGlobigerina bulloidesbiology.organism_classificationPaleoenvironmental changes13. Climate actionGeneral Earth and Planetary SciencesZanclean refloodingGeology
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Cyclic fluctuations, climatic changes and role of noise in planktonic foraminifera in the Mediterranean Sea

2005

The study of Planktonic Foraminifera abundances permits to obtain climatic curves on the basis of percentage ratio between tropical and temperate/polar forms. Climatic changes were controlled by several phenomena as: (i) Milankovitch's cycles, produced by variations of astronomical parameters such as precession, obliquity and eccentricity; (ii) continental geodynamic evolution and orogenic belt; (iii) variations of atmospheric and oceanic currents; (iv) volcanic eruptions; (v) meteor impacts. But while astronomical parameters have a quasi-regular periodicity, the other phenomena can be considered as "noise signal" in natural systems. The interplay between cyclical astronomical variations, t…

Planktonic foraminiferaStochastic resonanceGeneral MathematicsGeneral Physics and AstronomyAtmospheric sciencesQuantitative Biology - Quantitative MethodsPhysics::GeophysicsForaminiferaMediterranean seaGlacial periodQuantitative Biology - Populations and EvolutionPlanktonic foraminifera; Climatic changes; Stochastic resonancePhysics::Atmospheric and Oceanic PhysicsQuantitative Methods (q-bio.QM)Milankovitch cyclesbiologyOcean currentPopulations and Evolution (q-bio.PE)biology.organism_classificationSettore FIS/07 - Fisica Applicata(Beni Culturali Ambientali Biol.e Medicin)Climatic changeOceanographyFOS: Biological sciencesInterglacialPrecessionAstrophysics::Earth and Planetary AstrophysicsGeologyStochastic resonance
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Turonian-Maastrichtian biostratigraphy and isotope stratigraphy of the Kopet-Dagh Basin deposits, northeastern Neo-Tethys, Iran

2021

Abstract Planktonic foraminiferal biostratigraphy and isotope stratigraphy analyses of Turonian-Maastrichtian deposits have been carried out in the western part of the Kopet-Dagh Basin. The identification of the planktonic foraminiferal assemblages has led to the recognition of twelve Upper Cretaceous zones (Helvetoglobotruncana helvetica Zone to the Contusotruncana contusa-Abathomphalus mayaroensis zone) from the Tethyan realm. The obtained stable carbon isotope profile correlates with other reference curves, revealing many Late Cretaceous events including the Hitchwood, Navigation, Light Point, East Cliff, White Fall, Late Campanian Event (LCE), Campanian-Maastrichtian Boundary Event (CMB…

Planktonic foraminiferageographygeography.geographical_feature_categoryStable isotope ratioPalaeoenvironmental conditionsPaleontologyBiostratigraphyStructural basinOceanographyStable isotopeUpper cretaceousCretaceousTectonicsPaleontologyStratigraphyIsotopes of carbonCliffEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Millenial-scale paleoenviromental changes in the central Mediterranean during the Last Interglacial: comparison with European and North Atlantic reco…

2010

Abstract The environment of the central Mediterranean Sea is investigated on the basis of high-resolution planktonic foraminifera and calcareous nannofossil data (mean sampling resolutions of about 80 and 160 yr, respectively). MIS 5 is characterized by warm, oligotrophic and stratified waters, while coccolithophore communities developed a vertical zonation that, in today's oceans, is typical of the low-latitude gyres. The temperate-subtropical configuration of planktonic foraminifera and calcareous nannofossil assemblages is repeatedly transformed into a temperate-subpolar one during the suborbital cooling episodes C25-C18. A comparison with European pollen sequences and North Atlantic cor…

Planktonic foraminiferageographygeography.geographical_feature_categorybiologyNorthern HemispherePaleontologybiology.organism_classificationLast InterglacialForaminiferaCentral MediterraneanOceanographyMediterranean seaSpace and Planetary ScienceOcean gyrePaleoceanographyCalcareous nannofossilsInterglacialPaleoclimatologySuborbital climatic fluctuationsQuaternaryGeology
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Climatic variability and anthropogenic signatures in the Gulf of Salerno (southern-eastern Tyrrhenian Sea) during the last half-millennium

2012

Tyrrhenian Seaplanktonic foraminiferapaleoceanographylate Holocene
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Distribution and ecology of the Globigerinoides ruber — Globigerinoides elongatus morphotypes in the Azores region during the late Pleistocene-Holoce…

2018

Abstract Globigerinoides ruber is the dominant taxon in the North Atlantic Subtropical Gyre, nowadays limited to the north by the Azores Current. It is highly sensitive to recent and late Pleistocene Azores Front Current System variability. In this study, we analyse the distribution of five individual morphotypes of the G. ruber – G. elongatus plexus (G. ruber s.s., G. ruber cyclostoma type, G. elongatus, G. elongatus cf.1, G. elongatus pyramidical type) and G. ruber kummerform gr. in a core (ATA13-OF-KT1) collected southwest of the Azores islands and located in a strategical position near the present-day boundary of the Subtropical Gyre/Azores Front Current System (STG/AFCS). Micropaleonto…

[ SDU.OCEAN ] Sciences of the Universe [physics]/Ocean AtmospherePlanktonic foraminifera010506 paleontology010504 meteorology & atmospheric sciencesPleistoceneCyclostomaOceanography01 natural sciencesPaleontologyPaleoceanographyOcean gyre[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environment14. Life underwaterGlacial periodPaleoclimatology[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentRelative species abundanceEcology Evolution Behavior and SystematicsHoloceneGlobigerinoidesComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface Processes[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_categorybiologyEcologyAzores front/current systemPaleontology15. Life on landbiology.organism_classificationStable isotopeEcology Evolution Behavior and SystematicOceanographyEarth-Surface ProcesseInterglacialSubtropical gyreGeology
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Climatic changes during Late Pliocene and Early Pleistocene at Capo Rossello (Sicily, Italy): response from planktonic foraminifera

2004

climatic changeplanktonic foraminiferaMilankovitch periodicitiePlio/Pleistocene boundarySettore GEO/01 - Paleontologia E Paleoecologia
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Paleoenvironmental and climatic changes during the last 25 ky along a W-E transect across the Mediterranean Sea.

2012

climatic changeplanktonic foraminiferastable isotopeMediterranean Seapaleoenvironmental change
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Chemical Transfers Occurring Through

2019

Chardonnay wine malolactic fermentations were carried out to evaluate the chemical transfers occurring at the wood/wine interface in the presence of two different bacterial lifestyles. To do this, Oenococcus oeni was inoculated into must and wine in its planktonic and biofilm lifestyles, whether adhering or not to oak chips, leading to three distinct enological conditions: (i) post-alcoholic fermentation inoculation in wine in the absence of oak chips, (ii) post-alcoholic fermentation inoculation in wine in the presence of oak chips, and (iii) co-inoculation of both Saccharomyces cerevisiae and O. oeni directly in Chardonnay musts in the presence of oak chips. Classical microbiological and …

optical indicesmalolactic fermentationfood and beverageschemical transfersplanktonicO. oenibiofilmNutritionOriginal ResearchwoodFrontiers in nutrition
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