Search results for "Foraminifera"

showing 10 items of 144 documents

Calcareous nannofossil response to Late Cretaceous climate change in the eastern Tethys (Zagros Basin, Iran)

2020

Abstract Coniacian to Maastrichtian changes in calcareous nannofossil assemblages have been investigated in the eastern Tethyan Shahneshin section (central Zagros Basin, Iran). The nannofossil assemblages are mainly composed of Watznaueria spp. (avg. 54%), Retecapsa spp (avg. 7.9%), Cribrosphaerella ehrenbergii (avg. 7.7%) and Micula spp. (avg. 5.7%). Throughout the late Campanian, there is a trend to lower abundances in Watznaueria spp. together with increasing abundances of C. ehrenbergii and Arkhangelskiella cymbiformis, which are considered in this basin as the main cool-water taxa. Our results reveal that, despite a diagenetic impact on calcareous nannoflora, a number of primary paleoe…

010506 paleontologybiologyδ13CPaleontologyStructural basin010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesCretaceousDiagenesisForaminiferaPaleontologyBorealBenthic zoneCalcareousEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Planktonic foraminifera biozones and isotope stratigraphy of the Cenomanian-Turonian boundary in the western part of the Kopet-Dagh Basin, NE Iran

2018

Abstract A biostratigraphic study based on the planktonic foraminifera and isotope stratigraphy of the Cenomanian-Turonian interval has been undertaken in the western part of the Kopet-Dagh Basin (NE Iran). In this research, two stratigraphic sections including: Maraveh Tappeh and Qareh Galdy have been sampled and studied. Based on planktonic foraminifera, three biozones were assigned to this interval. These are the Rotalipora cushmani Zone, Whiteinella archaeocretacea Zone and Helvetoglobotruncana helvetica Zone, These biostratigraphic data confirm a gradual faunal turnover of planktonic foraminifera, at the Cenomanian-Turonian boundary in Whiteinella archaeocretacea Zone characterized by:…

010506 paleontologybiologyδ18OGeologyBiozoneBiostratigraphyStructural basin010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesForaminiferaPaleontologyStratigraphyBiostratigraphy Light isotopes Cenomanian-Turonian boundary Kopet-Dagh basin NE IranCenomanianSiltstoneGeology0105 earth and related environmental sciencesEarth-Surface ProcessesJournal of African Earth Sciences
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Biostratigraphy, Chronostratigraphy and Paleonvironmental Reconstruction of the Palermo Historical Centre Quaternary succession

2016

Marine deposits from the Palermo Plain were historically relevant for the Quaternary Period definition. Here we show lithostratigraphic, biostratigraphic and chronostratigraphic data collected on three boreholes in the Palermo historical centre that recovered 36.8, 42.0 and 52.0 metres of sediments overlaying the Numidian Flysch. Marine sedimentary sequences span from the Calabrian Stage (calcareous nannofossil Zone MNN 19d) to the Middle Pleistocene (dominance of medium-sized gephyrocapsids within the MNN 19f Zone) and also include a short Holocene depositional event. Calcareous nannofossil, benthic and planktonic foraminifera assemblages point to a shallow coastal environment, possibly < …

010506 paleontologycalcareous nannofossilsFlyschPleistocenebiologyGeologyBiostratigraphy010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesForaminiferaSedimentary depositional environmentPaleontologyStage (stratigraphy)Quaternary.General Earth and Planetary SciencesbiostratigraphyChronostratigraphyQuaternaryPalermo historical centre calcareous nannofossils biostratigraphy Quaternary.Palermo historical centreGeology0105 earth and related environmental sciences
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Isotopic seawater temperatures in the Albian Gault Clay of the Boulonnais (Paris Basin): Palaeoenvironmental implications

2016

13 pages; International audience; Oxygen isotopes were measured on several types of fossil hardparts from the Gault Clay Formation including benthic and planktonic foraminifera, belemnite guards, and fish small-teeth. Belemnites δ18O values indicate low temperatures (13.5–19.3 °C) with an increase from the Middle to Late Albian. Foraminifera provide variable δ18O values, some too low to be relevant in terms of temperature (until 42 °C). These low values probably result from a diagenetic alteration of the foraminiferal tests even though SEM observations revealed well-preserved microstructures. However, higher foraminiferal δ18O values recorded in some levels indicate temperatures in the rang…

010506 paleontologyδ18OGault Clay FormationForaminifera010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesIsotopes of oxygenForaminiferaPaleontologyPalaeotemperatureBelemnites guardsParis BasinFish teeth14. Life underwaterComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesbiologyfungiSelachian teethPaleontologyGeologyPelagic zoneAlbianbiology.organism_classificationDiagenesisSea surface temperature13. Climate actionBenthic zone[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOxygen isotopes[ SDU.STU.HY ] Sciences of the Universe [physics]/Earth Sciences/HydrologyBelemnitesGeology
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Oxygen respiration rates of benthic foraminifera as measured with oxygen microsensors

2011

Abstract Oxygen respiration rates of benthic foraminifera are still badly known, mainly because they are difficult to measure. Oxygen respiration rates of seventeen species of benthic foraminifera were measured using microelectrodes and calculated on the basis of the oxygen fluxes measured in the vicinity of the foraminiferal specimens. The results show a wide range of oxygen respiration rates for the different species (from 0.09 to 5.27 nl cell−1 h−1) and a clear correlation with foraminiferal biovolume showed by the power law relationship: R = 3.98 10−3 BioVol0.88 where the oxygen respiration rate (R) is expressed in nl O2 h−1 and in μm3 biovolume (BioVol) (n = 44, R2 = 0.72, F = 114, p

0106 biological sciences010504 meteorology & atmospheric sciencesbiology010604 marine biology & hydrobiologyRhizariachemistry.chemical_elementAquatic Sciencebiology.organism_classification01 natural sciencesOxygenForaminifera[SDE.BE] Environmental Sciences/Biodiversity and EcologychemistryBenthic zoneEnvironmental chemistryRespirationBotany[SDE.BE]Environmental Sciences/Biodiversity and EcologyRespiration rateEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS0105 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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Environmental Quality Assessment of Bizerte Lagoon (Tunisia) Using Living Foraminifera Assemblages and a Multiproxy Approach.

2015

This study investigated the environmental quality of the Bizerte Lagoon (Tunisia) through an integrated approach that combined environmental, biogeochemical, and living benthic foraminiferal analyses. Specifically, we analyzed the physicochemical parameters of the water and sediment. The textural, mineralogical, and geochemical characteristics of the sediment, including total organic carbon, total nitrogen, simultaneously extracted metals (SEM), acid volatile sulfides (AVS), chlorophyll a, CaCO3, and changes in bacterial populations and carbon isotopes were measured. The SEM/AVS values indicated the presence of relatively high concentrations of toxic metals in only some areas. Foraminiferal…

0106 biological sciencesMediterranean climateBiogeochemical cycleTunisiaStatistics as Topiclcsh:MedicineEnvironmental pollutionForaminifera010501 environmental sciences01 natural sciencesForaminifera14. Life underwaterWater pollutionlcsh:Science0105 earth and related environmental sciencesTotal organic carbonMultidisciplinarybiologyEcology010604 marine biology & hydrobiologylcsh:RSedimentbiology.organism_classification6. Clean water13. Climate actionBenthic zoneEnvironmental sciencelcsh:QEnvironmental PollutionResearch ArticleEnvironmental MonitoringPLoS ONE
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Reconstructing Bioinvasion Dynamics Through Micropaleontologic Analysis Highlights the Role of Temperature Change as a Driver of Alien Foraminifera I…

2021

Invasive alien species threaten biodiversity and ecosystem structure and functioning, but incomplete assessments of their origins and temporal trends impair our ability to understand the relative importance of different factors driving invasion success. Continuous time-series are needed to assess invasion dynamics, but such data are usually difficult to obtain, especially in the case of small-sized taxa that may remain undetected for several decades. In this study, we show how micropaleontologic analysis of sedimentary cores coupled with radiometric dating can be used to date the first arrival and to reconstruct temporal trends of foraminiferal species, focusing on the alien Amphistegina lo…

0106 biological sciencesSciencesea warmingPopulationBiodiversityOcean EngineeringQH1-199.5Aquatic ScienceOceanography010603 evolutionary biology01 natural sciencesInvasive speciesinvasive speciesradiometric datingForaminiferaMediterranean seaforaminifera invasive species lessepsian invasion Mediterranean Sea radiometric dating sea warming SSTMediterranean SeaeducationForaminifera -- Mediterranean SeaWater Science and TechnologyGlobal and Planetary Changeeducation.field_of_studybiologyEcology010604 marine biology & hydrobiologyQforaminiferaGeneral. Including nature conservation geographical distributionSettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationSSTSea surface temperatureGeographyTaxonIntroduced organisms -- Mediterranean SeaRadiometric datingRadioactive datingFrontiers in Marine Science
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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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