Search results for "Carbon isotope ratio"

showing 4 items of 4 documents

Annually resolved δ13Cshell chronologies of long-lived bivalve mollusks (Arctica islandica) reveal oceanic carbon dynamics in the temperate North Atl…

2011

Abstract The ability of the ocean to absorb carbon dioxide is likely to be adversely affected by recent climate change. However, relatively little is known about the spatiotemporal variability in the oceanic carbon cycle due to the lack of long-term, high-resolution dissolved inorganic carbon isotope ( δ 13 C DIC ) data, especially for the temperate North Atlantic, which is the major oceanic sink for anthropogenic CO 2 . Here, we report shell carbon isotope values ( δ 13 C shell ), a potential proxy for δ 13 C DIC , of old-grown specimens of the long-lived bivalve mollusk, Arctica islandica . This paper presents the first absolutely dated, annually resolved δ 13 C shell record from surface …

010504 meteorology & atmospheric sciences010502 geochemistry & geophysicsOceanography01 natural sciencesCarbon cycleSuess effectSclerochronologySclerochronology14. Life underwaterArctica islandicaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesPolar frontStable carbon isotope ratiobiologyOcean currentOceanic Suess effectPaleontologybiology.organism_classificationDissolved inorganic carbonOceanographyCarbon dioxide13. Climate actionIsotopes of carbon[SDE]Environmental SciencesOceanic carbon cycleGeology
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Microstructure-specific carbon isotopic signatures of organic matter from ∼3.5 Ga cherts of the Pilbara Craton support a biologic origin.

2016

21 pages; International audience; The ∼3.5 Ga Dresser Formation from the North Pole Dome of the Pilbara Craton (Western Australia) contains some of the oldest evidence for life on Earth. Here, we present a detailed study of microstructure-specific carbon isotopic composition of organic matter (OM) preserved in Dresser Formation bedded cherts and hydrothermal chert vein using in situ Secondary-Ion Mass Spectrometry (SIMS). The OM in these rocks occurs mainly as clots that, together with minor fine OM layers and laminae, are considered primary textures formed prior to host rock lithification. Other than rare OM-rich stylolites, no evidence was found for later OM migration beyond the micromete…

Carbon isotope ratio010504 meteorology & atmospheric sciencesMetamorphic rockPilbara CratonMineralogy010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesMicrofossilsPilbara cratonGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryDresser FormationOrganic matterLithificationAnkerite0105 earth and related environmental scienceschemistry.chemical_classificationδ13CGeology15. Life on land[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrychemistry13. Climate actionStylolite[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOrganic matterVein (geology)SIMSGeology
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Carbon and nitrogen isotopic values in Lithops aucampiae during leaf development.

2021

Abstract Lithops (Aizoaceae) are succulent plants consisting of a pair of opposite succulent leaves inserted on an extremely short stem. The apical meristem produces a new leaf pair that develops between the older pair, recycling water and metabolites. This peculiar anatomy and growth form make ecophysiological studies quite challenging. Lithops are considered to have CAM metabolism, though experimental evidence is scarce. We followed the changes in carbon and nitrogen isotopic values in mature leaves, young leaves and roots, with the aim of investigating how the use of resources is optimized to achieve survival in extremely arid environments. Two-year-old plants of Lithops aucampiae were g…

Settore BIO/07 - EcologiaIrrigationCarbon isotope ratioPhysiologyNitrogenPlant ScienceBotanyGeneticsSettore BIO/04 - Fisiologia VegetaleSucculentsNitrogen isotope ratioCarbon IsotopesLeaf developmentδ13CbiologyNitrogen Isotopesδ15NLithopsMeristembiology.organism_classificationAridIsotopes of nitrogenCarbonPlant LeavesLithops aucampiaeSettore BIO/03 - Botanica Ambientale E ApplicataAizoaceaeAizoaceaeCAM metabolismPlant physiology and biochemistry : PPB
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Origin and distribution of suspended organic matter as inferred from carbon isotope composition in a Mediterranean semi-enclosed marine system

1999

The origin and distribution of suspended organic matter, the trophic features and the stable carbon isotopic composition of particulate organic carbon (POC) were studied monthly in a Western Mediterranean semi-enclosed basin. Sampling stations were selected as a function of wind-exposure and the degree of vegetation cover and then compared with an adjacent unvegetated site. The predominant vegetation was seagrass (Posidonia oceanica and Cymodocea nodosa) and Caulerpa prolifera. Water samples were analyzed for total suspended matter (inorganic and organic fractions), photosynthetic pigments (chlorophyll-a and phaeopigments), dissolved organic carbon, particulate organic carbon and their isot…

Total organic carbonchemistry.chemical_classificationEcologybiologyCymodocea nodosachemistry.chemical_elementCaulerpa proliferabiology.organism_classificationOceanographyMediterranean seachemistryPosidonia oceanicaEnvironmental chemistryDissolved organic carbonGeneral Earth and Planetary SciencesEnvironmental scienceorganic matter sources carbon isotope ratio DOC POC MEDOrganic matterCarbonEcology Evolution Behavior and SystematicsGeneral Environmental Science
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