Search results for "organic carbon"

showing 10 items of 319 documents

Whole-Lake Sugar Addition Demonstrates Trophic Transfer of Dissolved Organic Carbon to Top Consumers

2017

Terrestrial dissolved organic carbon (DOC) provides an external carbon source to lake ecosystems. However, there is ongoing debate about whether external DOC that enters a lake can pass up the food web to support top consumers. We show, from experimental manipulation of a whole lake, that externally loaded DOC can contribute appreciably to fish biomass. Monthly additions of cane sugar with a distinct carbon stable isotope value during 2 years rapidly enriched the 13C content of zooplankton and macroinvertebrates, with a more gradual 13C enrichment of fish. After sugar addition stopped, the 13C content of consumers reverted towards original values. A simple isotope mixing model indicated tha…

0106 biological scienceszooplanktonallochthonymacroinvertebratesBiomassstable isotopesjärvet010603 evolutionary biology01 natural sciencesDissolved organic carbonlakesEnvironmental ChemistrySugarEcology Evolution Behavior and SystematicskalatTrophic levelTotal organic carbonfishEcologyEcology010604 marine biology & hydrobiologyplanktonLake ecosystemPlanktonFood web13. Climate actionEnvironmental chemistryfood websEnvironmental sciencecane sugarravintoverkot
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Lake zooplankton delta13C values are strongly correlated with the delta13C values of distinct phytoplankton taxa

2016

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0106 biological scienceszooplanktonta1172boreal lakesBiology010603 evolutionary biology01 natural sciencesZooplanktonDissolved organic carbonPhytoplanktonEcology Evolution Behavior and SystematicsEmiliania huxleyiEcologyEcology010604 marine biology & hydrobiologySestonSpecial Featurebiology.organism_classification6. Clean watercarbon stable isotopesphotosynthetic fractionationLight intensityEnvironmental chemistryphytoplanktonta1181Biomarkers in Trophic EcologyHypolimnionEutrophication
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Specifications for carbonate content quantification in recent marine sediments using Rock-Eval pyrolysis

2019

11 pages; International audience; The amount of CaCO3 in sediments and/or sedimentary rocks is usually measured by calcimetry while the nature of the carbonates is determined by X-ray diffraction. Recently, a carbonate recognition method based on the results of Rock-Eval pyrolysis was proposed in 2014 by Pillot et al. [1]. Rock-Eval pyrolysis is also widely used for the characterization of recent sediments. However, later in 2015 Baudin et al. [2] noticed that some of the characteristics of recent sediments tended to produce different results from those of more classical Rock-Eval analyses, causing bias in interpretations.In this study, the thermal stability of fossil and recent marine carb…

020209 energyGeochemistrySalt (chemistry)Mineralogy[SDU.STU]Sciences of the Universe [physics]/Earth Sciences02 engineering and technologyAnalytical Chemistrychemistry.chemical_compound020401 chemical engineering[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry0202 electrical engineering electronic engineering information engineeringRecent sedimentsAcid attack0204 chemical engineeringChemical decompositionComputingMilieux_MISCELLANEOUSTotal organic carbonchemistry.chemical_classificationCalciteRock-EvalSedimentCarbonates decompositionFuel Technologychemistry13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateSedimentary rockRock evalClay mineralsPyrolysisGeologyPyrolysis
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Biological and physical modification of carbonate system parameters along the salinity gradient in shallow hypersaline solar salterns in Trapani, Ita…

2017

Abstract We investigated changes in the chemical characteristics of evaporating seawater under the influence of microbial activity by conducting geochemical analyses of the brines and evaporite sediments collected from solar salterns in Trapani, Italy. The microbial activity had a substantial effect on the carbonate system parameters. Dissolved inorganic carbon (DIC) was substantially removed from the brine during the course of evaporation from the seawater to the point where calcium carbonate precipitates, with an accompanying decrease in its carbon isotopic composition (δ 13 C DIC ) to as low as −10.6‰. Although the removal of DIC was due to calcium carbonate precipitation, photosynthesis…

0301 basic medicine010504 meteorology & atmospheric sciencesEvaporiteMineralogyengineering.materialBiogeochemical cycle01 natural sciences03 medical and health scienceschemistry.chemical_compoundMicrobial matGeochemistry and PetrologyCompound-specific isotope analysishemic and lymphatic diseasesDissolved organic carbonPhotosynthetic pigmentSulfate0105 earth and related environmental sciencesHypersaline environmentSalinity030104 developmental biologyCalcium carbonatechemistryBiogeochemical cycle; Carbonate system; Compound-specific isotope analysis; Hypersaline environment; Microbial mat; Photosynthetic pigments;Photosynthetic pigmentsengineeringHaliteCarbonateSeawaterCarbonate systemCompound-specific isotope analysiGeologycirculatory and respiratory physiology
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Novel Autotrophic Organisms Contribute Significantly to the Internal Carbon Cycling Potential of a Boreal Lake

2018

ABSTRACT Oxygen-stratified lakes are typical for the boreal zone and also a major source of greenhouse gas emissions in the region. Due to shallow light penetration, restricting the growth of phototrophic organisms, and large allochthonous organic carbon inputs from the catchment area, the lake metabolism is expected to be dominated by heterotrophic organisms. In this study, we test this assumption and show that the potential for autotrophic carbon fixation and internal carbon cycling is high throughout the water column. Further, we show that during the summer stratification carbon fixation can exceed respiration in a boreal lake even below the euphotic zone. Metagenome-assembled genomes an…

0301 basic medicine030106 microbiologyHeterotrophDNA RibosomaljärvetMicrobiologyCarbon cycle03 medical and health sciencesWater columnTotal inorganic carbonRNA Ribosomal 16SVirologyCluster AnalysisPhotic zoneAnaerobiosis14. Life underwaterAutotrophFinlandPhylogeny030304 developmental biologyTotal organic carbon0303 health sciencesAutotrophic ProcessesmetagenomicsPhototroph030306 microbiologygreenhouse gas emissionsEcologyhiilen kiertoCarbon fixationSequence Analysis DNAiron oxidizers15. Life on landBiotaCarbonQR1-502Food webLakesMikrobiologi13. Climate actionmikro-organismitredox gradientEnvironmental sciencechemoautotrophyResearch ArticlemBio
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Contribution of aerobic anoxygenic phototrophic bacteria to total organic carbon pool in aquatic system of subtropical karst catchments, Southwest Ch…

2017

Aerobic anoxygenic phototrophic bacteria may play a particular role in carbon cycling of aquatic systems. However, little is known about the interaction between aerobic anoxygenic phototrophic bacteria and hydrochemistry in groundwater-surface water exchange systems of subtropical karst catchments. We carried out a detailed study on the abundance of aerobic anoxygenic phototrophic bacteria and bacterioplankton, hydrochemistry and taxonomy of bacterioplankton in the Maocun watershed, Southwest China, an area with karst geological background. Our results revealed that bacteria are the important contributors to total organic carbon source/sequestration in the groundwater-surface water of this …

0301 basic medicineAquatic OrganismsChinaNitrogen030106 microbiologyBiologyGlobal WarmingApplied Microbiology and BiotechnologyMicrobiologyCarbon cycle03 medical and health sciencesRNA Ribosomal 16SGroundwaterTotal organic carbonEcologyEcologyAquatic ecosystemBetaproteobacteriaBacterioplanktonbiology.organism_classificationCarbonBacteria AerobicOxygenPhototrophic Processes030104 developmental biologyAerobic anoxygenic phototrophic bacteriaProteobacteriaBacteriaPolynucleobacterFEMS Microbiology Ecology
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Evolution of organic carbon pools and microbial diversity in hyperarid anthropogenic soils

2016

Abstract We investigated the organic carbon pools and the microbial diversity and activity in anthropogenic terraced soils in a desert area of Southern Peru to highlight how the introduction of agriculture influences carbon evolution and storage and genetic and functional diversity of soil microbiota over time. Five sites were selected considering soils cultivated since 5, 15, 20, 35 and 65 years, sampled along the profile depth (0–20 and 20–40 cm layer). Soil and microbial parameters comprised by organic carbon pools, microbial respiration, microbial community physiological profile (CLPP) and microbial diversity (PCR-DGGE) were determined. The results showed that the highest C concentratio…

0301 basic medicineBiodiversitychemistry.chemical_element03 medical and health sciencesMicrobial dynamicEcology Evolution Behavior and SystematicsEarth-Surface ProcessesTotal organic carbonAnthropogenic soilEcologySoil organic carbonEcologySoil organic matterSoil chemistry04 agricultural and veterinary sciencesSoil carbon030104 developmental biologyMicrobial population biologychemistrySettore AGR/14 - PedologiaEnvironmental chemistrySoil water040103 agronomy & agricultureArid environment0401 agriculture forestry and fisheriesEnvironmental scienceCarbonJournal of Arid Environments
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Influence of Altered Microbes on Soil Organic Carbon Availability in Karst Agricultural Soils Contaminated by Pb-Zn Tailings.

2018

Soil organic carbon (SOC) availability is determined via a complex bio-mediated process, and Pb-Zn tailings are toxic to the soil microbes that are involved in this process. Here, Pb-Zn-tailings- contaminated karst soils with different levels (paddy field > corn field > citrus field > control group) were collected to explore the intrinsic relationship between Pb-Zn tailings and microbes due to the limited microbial abundance in these soils. The SOC concentration in the paddy fields is the highest. However, based on the soil microbial diversity and sole-carbon-source utilization profiles, the rate of SOC availability, McIntosh index, Shannon-Wiener diversity index, Simpson’s diversi…

0301 basic medicineMicrobiology (medical)Pb-Zn tailingsbiologylcsh:QR1-502Soil carbonbiology.organism_classificationMicrobiologyTailingskarst surface soillcsh:MicrobiologyActinobacteriasoil organic carbon03 medical and health sciencesDiversity index030104 developmental biologyAgronomylong-term acclimationSoil waterPaddy fieldEnvironmental scienceProteobacteriamicrobial communityAcidobacteriaFrontiers in microbiology
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Influence of environmental pollution with creosote oil or its vapors on biomass and selected physiological groups of microorganisms

2017

Survival of microorganisms in soils from treatment facility and landfill of wooden railway sleepers contaminated with creosote oil as well as in two types of soils with different content of organic carbon, treated with creosote oil vapors, was assessed. Microbiological assays including determination of: the biomass of living microorganisms method and the number of proteolytic, lipolytic and amylolytic microorganisms were carried out under laboratory conditions. Chromatography analysis of the soil extract from railway sleepers treatment facility was performed using GC/MS. The highest biomass and the number of tested microorganisms were determined in soils from wooden railway sleepers landfil…

0301 basic medicineTotal organic carbonMicroorganism030106 microbiologyBiomassEnvironmental pollutionContaminationSoil typecomplex mixtureslaw.inventionEnvironmental sciences03 medical and health sciences030104 developmental biologyCreosotelawEnvironmental chemistrySoil waterEnvironmental scienceGE1-350E3S Web of Conferences
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Organic carbon dynamics in soil particle-size separates of sandy Spodosols when forest is cleared for maize cropping

2003

Summary In southwest France, much of the forest lands on sandy Spodosols has been converted to continuous maize cropping in the last few decades. To evaluate the impacts of such change on the content and properties of the soil organic matter, we compared the amount of organic carbon and 13C natural abundance in soil and particle-size separates at three locations, selected on the basis of different contents of 0–50 μm particles (clay + silt). After three decades of cultivation, the amount of carbon from the forest pools (Cf) decreased by about 60%, attributable mainly to easily degradable material in sand-sized fractions (−70%). However, a recalcitrant residue remained in soil at a constant …

2. Zero hungerTotal organic carbonchemistry.chemical_classification010504 meteorology & atmospheric sciencesSoil textureSoil organic matterSoil ScienceMineralogyForestry04 agricultural and veterinary sciencesMineralization (soil science)Soil carbon15. Life on land01 natural sciencesPodzolchemistry040103 agronomy & agriculture0401 agriculture forestry and fisheriesOrganic matterMonoculture0105 earth and related environmental sciencesEuropean Journal of Soil Science
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