Search results for " rat"

showing 10 items of 9334 documents

Revised phosphate-water fractionation equation reassessing paleotemperatures derived from biogenic apatite.

2010

8 pages; International audience; Oxygen isotopes of biogenic apatite have been widely used to reassess anomalous temperatures inferred from oxygen isotope ratios of ancient biogenic calcite, more prone to diagenetic alteration. However, recent studies have highlighted that oxygen isotope ratios of biogenic apatite differ dependent on used analytical techniques. This questions the applicability of the phosphate–water fractionation equations established over 25 years ago using earlier analytical techniques to more recently acquired data. In this work we present a new phosphate–water oxygen isotope fractionation equation based on oxygen isotopes determined on fish raised in aquariums at contro…

010506 paleontology[SDE.MCG]Environmental Sciences/Global ChangesMineralogyFractionation010502 geochemistry & geophysics01 natural sciencesIsotopes of oxygenApatitechemistry.chemical_compoundGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryEarth and Planetary Sciences (miscellaneous)paleotemperature14. Life underwaterfractionation0105 earth and related environmental sciencesCalciteoxygen isotopesOxygen isotope ratio cyclePhosphate[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryEquilibrium fractionationDiagenesis[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicschemistrySpace and Planetary Sciencevisual_artapatitevisual_art.visual_art_mediumGeology
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Lignin oxidation products as a vegetation proxy in stalagmite and drip water samples from the Herbstlabyrinth, Germany

2019

Here we present the first quantitative record of lignin oxidation products (LOPs) in a Holocene stalagmite from the Herbstlabyrinth Cave in central Germany, as well as LOP results from 16 months of drip water monitoring. Lignin is only produced by vascular plants and is therefore an unambiguous vegetation proxy, which can help to better interpret other vegetation and climate proxies in speleothems. We compared our results with stable isotope and trace element data from the same samples. The drip water monitoring reveals a seasonal pattern of LOPs in a fast drip site with low LOP concentrations in winter and higher LOP concentrations in summer, which is opposite to the behaviour of the drip …

010506 paleontologygeographygeography.geographical_feature_categoryStable isotope ratioTrace elementStalagmite01 natural scienceschemistry.chemical_compoundchemistryCaveEnvironmental chemistryLigninHolocene0105 earth and related environmental sciences
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Venerid bivalve Venus verrucosa as a high-resolution archive of seawater temperature in the Mediterranean Sea

2021

Abstract High-resolution stable isotope data (δ18O, δ13C) were used to study growth strategies of the bivalve Venus verrucosa collected from three sites of the eastern coast of the Adriatic Sea. The principal objectives of this study were to identify the main growing season and to evaluate the potential applicability of δ18Oshell values to reconstruct the seasonal temperature variability. Calcium carbonate for oxygen and carbon isotope analyses was obtained by drilling the outer shell layer. Temporal and spatial variations in temperature and salinity values at the study sites were simulated using the 3D numerical ocean model ROMS. Annual periodicity of growth patterns was confirmed by δ18Os…

010506 paleontologyδ13Cδ18OStable isotope ratioTemperature salinity diagramsPaleontologyGrowing season010502 geochemistry & geophysicsOceanography01 natural sciencesOceanographyMediterranean seaSeawater14. Life underwaterBayStable isotopes ; Paleotemperature ; Adriatic Sea ; Growth rateEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Soil physicochemical and microbial drivers of temperature sensitivity of soil organic matter decomposition under boreal forests

2020

Abstract Soil organic matter (SOM) in boreal forests is an important carbon sink. The aim of this study was to assess and to detect factors controlling the temperature sensitivity of SOM decomposition. Soils were collected from Scots pine, Norway spruce, silver birch, and mixed forests (O horizon) in northern Finland, and their basal respiration rates at five different temperatures (from 4 to 28 °C) were measured. The Q10 values, showing the respiration rate changes with a 10 °C increase, were calculated using a Gaussian function and were based on temperature-dependent changes. Several soil physicochemical parameters were measured, and the functional diversity of the soil microbial communit…

0106 biological sciences$Q_{10}$ metabolic coefficientQ10Soil ScienceSoil scienceglobal warmingcomplex mixtures010603 evolutionary biology01 natural sciences$CO_{2}$ evolutionbiologySoil organic matterTaigaScots pineCarbon sink$MicroResp^{TM}$04 agricultural and veterinary sciencesbiology.organism_classificationEnvironmental chemistrySoil watermicrobial functional diversity040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceSoil horizonMicroResp™Q10 metabolic coefficientRespiration rateCO2 evolutionPedosphere
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Effect of Intensity and Mode of Artificial Upwelling on Particle Flux and Carbon Export

2021

Reduction of anthropogenic CO2 emissions alone will not sufficiently restrict global warming and enable the 1.5°C goal of the Paris agreement to be met. To effectively counteract climate change, measures to actively remove carbon dioxide from the atmosphere are required. Artificial upwelling has been proposed as one such carbon dioxide removal technique. By fueling primary productivity in the surface ocean with nutrient-rich deep water, it could potentially enhance downward fluxes of particulate organic carbon (POC) and carbon sequestration. In this study we investigated the effect of different intensities of artificial upwelling combined with two upwelling modes (recurring additions vs. on…

0106 biological sciences010504 meteorology & atmospheric sciencesPHYTOPLANKTON COMMUNITYScienceartificial upwellingchemistry.chemical_elementOcean EngineeringQH1-199.5Carbon sequestrationAquatic ScienceAtmospheric sciencesOceanography01 natural sciencesremineralization ratechemistry.chemical_compoundWater columnORGANIC-CARBONVDP::Matematikk og Naturvitenskap: 400::Geofag: 450particle propertiesOrganic matter1172 Environmental sciences0105 earth and related environmental sciencesWater Science and TechnologyCO2 CONCENTRATIONSTotal organic carbonchemistry.chemical_classificationGlobal and Planetary Change010604 marine biology & hydrobiologyQTECHNICAL NOTEUPPER OCEANGeneral. Including nature conservation geographical distributionsinking velocityPlanktoncarbon sequestrationMARINE SNOWBACTERIAL-GROWTHINVERSE RELATIONSHIPexport fluxchemistry13. Climate actionCarbon dioxideEnvironmental scienceUpwellingmesocosm studyremineralization depthCarbonTRANSPARENT EXOPOLYMER PARTICLESFrontiers in Marine Science
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Timing and duration of European larch growing season along altitudinal gradients in the Swiss Alps.

2009

The 2007 European larch (Larix decidua Mill.) growing season was monitored along two elevational transects in the Lotschental valley in the Swiss Alps. Phenological observations and weekly microcore sampling of 28 larch trees were conducted between April and October 2007 at seven study sites regularly spaced from 1350 to 2150 m a.s.l. on northwest- and southeast-facing slopes. The developmental stages of nearly 75,000 individual cells assessed on 1200 thin sections were used to investigate the links between the trees' thermal regimes and growth phases including the beginning and ending of cell enlargement, wall thickening and maturation of the stem wood. Needles appeared approximately 3-4 w…

0106 biological sciences010504 meteorology & atmospheric sciencesPhysiologyGrowing seasonLarixPlant Science01 natural sciencesAltitudeTransect0105 earth and related environmental sciencesbiologyPhenologyEcologyAltitudeEuropean LarchTemperatureLapse rateCell Differentiation15. Life on landbiology.organism_classificationAgronomyProductivity (ecology)13. Climate actionSeasonsLarchSwitzerland010606 plant biology & botanyTree physiology
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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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Drivers of shell growth of the bivalve, Callista chione (L. 1758) - Combined it environmental and biological factors

2018

WOS:000426027100014; Seasonal shell growth patterns were analyzed using the stable oxygen and carbon isotope values of live-collected specimens of the bivalve Callista chione from two sites in the Adriatic Sea (Pag and Cetina, Croatia). Micromilling was performed on the shell surface of three shells per site and shell oxygen isotopes of the powder samples were measured. The timing and rate of seasonal shell growth was determined by aligning the delta O-18(shell)-derived temperatures so that the best fit was achieved with the instrumental temperature curve. According to the data, shells grew only at very low rates or not at all during the winter months, i.e., between January and March. Shell…

0106 biological sciences010504 meteorology & atmospheric sciencesmussel mytilus-galloprovincialisCroatiaShell (structure)Oxygen IsotopesAquatic ScienceEnvironmentOceanography01 natural sciencesIsotopes of oxygenChionespisula-solidissimaBiological Factorswater temperatureSclerochronologySeasonal shell growth patternsSclerochronologycontinental-shelfBivalve molluskAnimals14. Life underwaterArctica islandicaparticulate organic-matter0105 earth and related environmental sciencesStable isotopesCarbon IsotopesBivalve mollusk ; Seasonal shell growth patterns ; Stable isotopes ; Sclerochronology ; Environment ; Biology ; Life history traitbiologyStable isotope ratiostable-isotope ratios010604 marine biology & hydrobiologyACLpopulation-dynamicsGeneral Medicineglycymeris-glycymerisLife history traitsbiology.organism_classificationPollutionBivalviaphacosoma-japonicumOceanographyIsotopes of carbonEnvironmental scienceSeawaterarctica-islandica[SDE.BE]Environmental Sciences/Biodiversity and Ecology
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The evolution of gigantism in active marine predators

2017

A novel hypothesis to better understand the evolution of gigantism in active marine predators and the diversity of body sizes, feeding strategies and thermophysiologies of extinct and living aquatic vertebrates is proposed. Recent works suggest that some aspects of animal energetics can act as constraining factors for body size. Given that mass-specific metabolic rate decreases with body mass, the body size of active predators should be limited by the high metabolic demand of this feeding strategy. In this context, we propose that shifts towards higher metabolic levels can enable the same activity and feeding strategy to be maintained at bigger body sizes, offering a satisfactory explanatio…

0106 biological sciences010506 paleontologyEcologyPaleontologiaBiologyBody sizemedicine.disease010603 evolutionary biology01 natural sciencesPredationGigantismMetabolic ratemedicineGeneral Agricultural and Biological Sciences0105 earth and related environmental sciencesHistorical Biology
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Evaluating the influences of temperature, primary production, and evolutionary history on bivalve growth rates

2019

AbstractOrganismal metabolic rates reflect the interaction of environmental and physiological factors. Thus, calcifying organisms that record growth history can provide insight into both the ancient environments in which they lived and their own physiology and life history. However, interpreting them requires understanding which environmental factors have the greatest influence on growth rate and the extent to which evolutionary history constrains growth rates across lineages. We integrated satellite measurements of sea-surface temperature and chlorophyll-a concentration with a database of growth coefficients, body sizes, and life spans for 692 populations of living marine bivalves in 195 s…

0106 biological sciences010506 paleontologyPhylogenetic inertiaEcologyPhylogenetic treeEcologyPaleontologyContext (language use)Biology010603 evolutionary biology01 natural sciencesTaxonProductivity (ecology)PhylogeneticsProduction (economics)Growth rateGeneral Agricultural and Biological SciencesEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesPaleobiology
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