Search results for " Foraminifera"

showing 10 items of 74 documents

Planktic foraminiferal changes in the western Mediterranean Anthropocene

2021

The increase in anthropogenic induced warming over the last two centuries is impacting marine environment. Planktic foraminifera are a globally distributed calcifying marine zooplankton responding sensitively to changes in sea surface temperatures and interacting with the food web structure. Here, we study two high resolution multicore records from two western Mediterranean Sea regions (Alboran and Balearic basins), areas highly affected by both natural climate change and anthropogenic warming. Cores cover the time interval from the Medieval Climate Anomaly to present. Reconstructed sea surface temperatures are in good agreement with other results, tracing temperature changes through the Co…

010504 meteorology & atmospheric sciencesLast 1500 yearsPopulationClimate change02 engineering and technologyOceanography01 natural sciencesWestern Mediterranean SeaForaminiferaMediterranean seaAtlantic multidecadal oscillation0202 electrical engineering electronic engineering information engineeringeducationAnthropogenic warming0105 earth and related environmental sciencesGlobal and Planetary Changeeducation.field_of_studybiology020206 networking & telecommunicationsLast 1500 yearGlobigerina bulloidesPlanktic foraminiferabiology.organism_classificationOceanographyNorth Atlantic oscillationUpwellingNatural variabilityMarine surface productionGeology
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Productivity modes in the Mediterranean Sea during Dansgaard–Oeschger (20,000–70,000 yr ago) oscillations

2013

The study of planktonic organisms during abrupt climatic variations of the last glacial period (Dansgaard-Oeschger oscillations, D-O) may reveal important insights on climatic, oceanographic and biological interactions. Here we present planktic foraminifera and coccolithophore data collected at the Ocean Drilling Program Site 963 (Sicily Channel), with a mean sampling resolution of respectively 43.5 and 98.9. yr, over the interval between 70,000 and 20,000. yr ago. The paleoenvironmental reconstruction suggests that three different scenarios can be seen across each D-O cycle: 1. oligotrophic surface water and a deep thermocline for the early Interstadials; 2. a Deep Chlorophyll Maximum and …

010506 paleontology010504 meteorology & atmospheric sciencesCoccolithophoreMediterraneanOceanography01 natural sciencesForaminifera/dk/atira/pure/sustainabledevelopmentgoals/life_below_waterWater columnMediterranean seaPaleoproductivity Dansgaard–Oeschger Mediterranean Planktonic Foraminifera CoccolithophoresCoccolithophores14. Life underwaterStadialGlacial periodSDG 14 - Life Below WaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesDeep chlorophyll maximumbiologyPaleontologybiology.organism_classificationOceanography13. Climate actionClimatologyPlanktonic ForaminiferaDansgaard-OeschgerThermoclineGeologyPaleoproductivityPalaeogeography, Palaeoclimatology, Palaeoecology
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The Uniqueness of Planktonic Ecosystems in the Mediterranean Sea: The Response to Orbital- and Suborbital-Climatic Forcing over the Last 130,000 Years

2016

AbstractThe Mediterranean Sea is an ideal location to test the response of organisms to hydrological transformations driven by climate change. Here we review studies carried out on planktonic foraminifera and coccolithophores during the late Quaternary and attempt the comparison of data scattered in time and space. We highlight the prompt response of surface water ecosystems to both orbital- and suborbital-climatic variations.A markedly different spatial response was observed in calcareous plankton assemblages, possibly due to the influence of the North Atlantic climatic system in the western, central and northern areas and of the monsoon system in the easternmost and southern sites. Orbita…

010506 paleontologyQE1-996.5010504 meteorology & atmospheric sciencesGeologyForcing (mathematics)Environmental Science (miscellaneous)Plankton01 natural scienceslate quaternaryMediterranean seaOceanographyplanktonic foraminiferaClimatologyGeneral Earth and Planetary SciencesEcosystemUniquenessmediterranean seacoccolithophoresGeology0105 earth and related environmental sciencesOpen Geosciences
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Integrated bio- and carbon-isotope stratigraphy of the Upper Cretaceous Gurpi Formation (Iran): A new reference for the eastern Tethys and its implic…

2018

29 pages; International audience; A high-resolution stratigraphic analysis of the Upper Cretaceous Gurpi Formation has been undertaken in the Shahneshin section (Zagros Basin, Iran). New results on calcareous nannofossils, planktic foraminifers, dinoflagellate cysts and high-resolution carbon and oxygen stable isotopes form the basis of a reference section for the eastern Tethys that spans the upper Coniacian to the late Danian. Carbon-isotope correlation to Gubbio, Italy and the NW German chalk allows for the identification of many isotopic events as well as for the definition of new events in the Campanian and Maastrichtian. Our results allow for a review of the accurate position of the C…

010506 paleontologyStructural basin010502 geochemistry & geophysics01 natural sciencesPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryStage (stratigraphy)Calcareous nannofossils14. Life underwater0105 earth and related environmental sciencesbiologyStable isotope ratioDinoflagellate cystsCarbon isotopesDinoflagellatePaleontologyPlanktic foraminiferaPlanktonbiology.organism_classificationZagrosCretaceousStratigraphy13. Climate actionIsotopes of carbonTethyan realm[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyConiacian–MaastrichtianGeologyCretaceous Research
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Biostratigraphy and isotope stratigraphy of upper Maastrichtian–Danian marine deposits of the Kopet-Dagh Basin, northeast Iran

2018

Abstract Biostratigraphy, using foraminifera and echinoids, plus high-resolution carbon isotope stratigraphy of the upper Maastrichtian–Danian interval in the western part of the Kopet-Dagh Basin in northeast Iran are outlined. Our study of shallow-marine carbonate platform deposits of the Kalat Formation, rich in larger benthic foraminifera (predominantly Clypeorbis mammillatus Schlumberger, Lepidorbitoides sp. and Siderolites calcitrapoides Lamarck), has allowed the definition of a C. mammillatus-S. calcitrapoides Assemblage Zone, of late Maastrichtian age. Clypeorbis mammillatus is here recorded for the first time from the Maastrichtian Kalat Formation and represents the most easterly fi…

010506 paleontologybiologyCarbonate platformMesozoic Cenozoic Clypeorbis mammillatus Kalat Formation Chehel Kaman Formation Planktonic foraminifera Isotope stratigraphy.PaleontologyBiozoneBiostratigraphy010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCretaceousForaminiferaPaleontologyStratigraphyEchinocorysCenozoicGeology0105 earth and related environmental sciences
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The response of cultured meiofaunal and benthic foraminiferal communities to lead exposure: Results from mesocosm experiments

2018

Lead (Pb) has been regarded as a very toxic element that poses a serious threat to biota. A mesocosm experiment is performed to assess the influence of Pb on meiofaunal (metazoans within 45-500 µm) and benthic foraminiferal (protozoans) communities. To this end, sediments bearing such communities are incubated in mesocosms, exposed to different levels of Pb in seawater, and monitored for up to eight weeks. Concentrations of Pb below 1 ppm in water do not promote a significant increase of this metal in sediments. Relatively high concentrations of Pb seem to affect meiofaunal and benthic foraminiferal communities by reducing their richness or diversity, and the abundance of the most sensitive…

0106 biological sciencesGeologic SedimentsHealth Toxicology and MutagenesisMeiobenthosmeiofauna; foraminifera; lead; mesocosm; sedimentForaminifera010501 environmental sciences01 natural sciencesMesocosmForaminiferaMediterranean SeaEnvironmental ChemistrySeawater0105 earth and related environmental sciencesPollutantDose-Response Relationship Drugbiology010604 marine biology & hydrobiologySedimentBiotaBiodiversityModels Theoreticalbiology.organism_classificationmesocosmsedimentLeadBenthic zoneEnvironmental chemistrymeiofaunaEnvironmental scienceSeawaterWater Pollutants ChemicalEnvironmental MonitoringEnvironmental Toxicology and Chemistry
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“Hidden invaders” conquer the Sicily Channel and knock on the door of the Western Mediterranean sea

2019

Abstract This study updates the current distribution, range expansion and establishment status of the non-indigenous species Amphistegina lobifera Larsen, 1976 and other foraminifera that are cryptogenic in the Sicily Channel. Prior to this study, amphisteginids were reported from the Levantine Basin, the Central Mediterranean (Tunisia, Malta, Pelagian islands) and the southern Adriatic Sea. Here, we provide new records documenting a north-western expansion in the Central Mediterranean. In summer-autumn 2017 and spring-summer 2018, we collected algae and sediment samples from shallow coastal habitats along the shores of the Maltese archipelago, southern and north-western Sicily, Pantelleria…

0106 biological sciencesMediterranean climate010504 meteorology & atmospheric sciencesRange (biology)Species distributionAquatic ScienceOceanography01 natural sciencesForaminiferaCentral mediterraneanMediterranean seaA0105 earth and related environmental sciencesShoregeographygeography.geographical_feature_categorybiology010604 marine biology & hydrobiologyBenthic foraminiferaAmphistegina lobiferaSettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationDistribution modelOceanographyArchipelagoNon-indigenous speciesChannel (geography)
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Seaweed fails to prevent ocean acidification impact on foraminifera along a shallow-water CO2 gradient

2014

Ocean acidification causes biodiversity loss, alters ecosystems, and may impact food security, as shells of small organisms dissolve easily in corrosive waters. There is a suggestion that photosynthetic organisms could mitigate ocean acidification on a local scale, through seagrass protection or seaweed cultivation, as net ecosystem organic production raises the saturation state of calcium carbonate making seawater less corrosive. Here, we used a natural gradient in calcium carbonate saturation, caused by shallow-water CO2 seeps in the Mediterranean Sea, to assess whether seaweed that is resistant to acidification (Padina pavonica) could prevent adverse effects of acidification on epiphytic…

0106 biological sciencesSettore BIO/07 - Ecologia010504 meteorology & atmospheric sciencesPadina pavonica01 natural sciencesForaminiferaBlue carbonchemistry.chemical_compoundEcosystem14. Life underwaterEcology Evolution Behavior and SystematicsOriginal Research0105 earth and related environmental sciencesNature and Landscape ConservationBlue carbonbiologyEcologyEcologyShallow-water CO<inf>2</inf> seep010604 marine biology & hydrobiologyOcean acidificationBenthic foraminiferaCoastal communitieshallow-water CO2 seepsOcean acidification15. Life on landbiology.organism_classificationcoastal communitiesEcology Evolution Behavior and SystematicSeagrassCalcium carbonatechemistry13. Climate actionCalcareous
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Assessing the effect of mercury pollution on cultured benthic foraminifera community using morphological and eDNA metabarcoding approaches

2018

Mercury (Hg) is a highly toxic element for living organisms and is known to bioaccumulate and biomagnify. Here, we analyze the response of benthic foraminifera communities cultured in mesocosm and exposed to different concentrations of Hg. Standard morphological analyses and environmental DNA metabarcoding show evidence that Hg pollution has detrimental effects on benthic foraminifera. The molecular analysis provides a more complete view of foraminiferal communities including the soft-walled single-chambered monothalamiids and small-sized hard-shelled rotaliids and textulariids than the morphological one. Among these taxa that are typically overlooked in morphological studies we found poten…

0301 basic medicinePollutionmercury pollutionGeologic Sedimentsmedia_common.quotation_subjectbenthic foraminiferaBenthic foraminifera Biomonitoring Mercury pollution MetabarcodingForaminifera010501 environmental sciencesAquatic ScienceOceanography01 natural sciencesMesocosmForaminifera03 medical and health sciencesBiomonitoringMediterranean SeaDNA Barcoding TaxonomicEnvironmental DNASeawatermetabarcoding biomonitoring0105 earth and related environmental sciencesmedia_commonbiologyEcologyBenthic foraminiferaBiodiversityMercuryDNA ProtozoanMercury pollutionbiology.organism_classificationPollutionBenthic foraminifera; Biomonitoring; Mercury pollution; Metabarcoding030104 developmental biologyItaly13. Climate actionBenthic zoneBioaccumulationbenthic foraminifera; mercury pollution; metabarcoding biomonitoringBiomonitoringMetabarcodingBioindicatorWater Pollutants ChemicalEnvironmental Monitoring
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A SMALL INVADER CONQUERS SICILY: AMPHISTEGINA LOBIFERA (FORAMINIFERA: AMPHISTEGINIDAE)

2018

The highly invasive Amphistegina lobifera (Larsen, 1976), a benthic foraminiferal species native to the Red Sea, has colonized the Eastern Mediterranean through the Suez Canal and altered the native community structure. More recently, it has been reported from Malta and the Pelagian Islands within the Sicily channel. Here, we report new records from the southern coasts of Sicily, where we found it abundant both in the soft-bottom sediment and as epiphyt on algae. The occurrence of A. lobifera in Pantelleria and Favignana islands represents the Mediterranean westernmost record of this non-indigenous species.

Benthic foraminifera Lessepsian invasion Sicily Channel Central Mediterranean Sea
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