Search results for "carbon"

showing 7 items of 6057 documents

The importance of phytoplankton production for carbon budgets in a semiarid floodplain wetland

2011

Phytoplankton production (PP) in wetlands is not measured as often as that of macrophytes. A three year-study during a period of sustained high flooding was undertaken in a central Spanish floodplain wetland (Las Tablas de Daimiel National Park) to determine net PP, its spatial heterogeneity and controlling factors, and compare it with primary production in macrophyte communities. This enabled us to estimate carbon budgets for each community. All PP variables showed high spatial and temporal variability among sites, resulting in low coherence even when flooding connected all sites. Net PP corresponded to 25- 36% of submerged plant production and 3-10% of helophyte production. Net PP was con…

zooplanktoncarbono orgánico disueltoFloodplainWetlandPlant Sciencebiomasa planctónicanutrientesnutrientslcsh:BotanyPhytoplanktonproducción primaria neta específica para la clorofilaEcology Evolution Behavior and Systematicsgeographymacrophyte productiongeography.geographical_feature_categoryPrimary producersEcologyHelophyteplankton biomassBotanydissolved organic carbonSpatial heterogeneityMacrophytelcsh:QK1-989Productivity (ecology)QK1-989zooplanctonEnvironmental sciencechlorophyll-specific net primary productionproducción de macrófitosAnales del Jardín Botánico de Madrid
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Browning-induced changes in trophic functioning of planktonic food webs in temperate and boreal lakes: insights from fatty acids

2022

AbstractThe effects of lake browning on trophic functioning of planktonic food webs are not fully understood. We studied the effects of browning on the response patterns of polyunsaturated fatty acids and n−3/n−6 ratio in seston and compared them between boreal and temperate lakes. We also compared the regional differences and the effects of lake browning on the reliance of zooplankton on heterotrophic microbial pathways and the mass fractions of eicosapentaenoic acid (EPA) and docosahexaenoic acid (DHA) in zooplankton. Lake browning was associated with increasing phytoplankton biomass and concentrations of EPA and DHA in both temperate and boreal lakes, but the seston n−3/n−6 ratio was low…

zooplanktonmikrobiekologialiuennut orgaaninen hiilieutrophicationrehevöityminenplanktonphytoplanktonmicrobial pathwaydissolved organic carbonEcology Evolution Behavior and SystematicsOecologia
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MOBILITY OF MERCURY IN THE VOLCANIC/GEOTHERMAL AREA OF NISYROS (GREECE)

2017

Το καλοκαίρι του 2013, προσδιορίστηκαν οι συγκεντρώσεις υδραργύρου στο έδαφος και τον αέρα του ενεργού ηφαιστείου της Νισύρου (Ελλάδα), το οποίο ανήκει στο ενεργό ηφαιστειακό τόξο του νοτίου Αιγαίου. 102 δείγματα εδάφους συλλέχθηκαν και 2119 αναλύθηκαν για υδράργυρο με τη χρήση ψυχρού ατμού ατομικής απορρόφησης αναλυτή, σύμφωνα με τη μέθοδο ΕΡΑ 7473. Ταυτόχρονα, στα ίδια σημεία πραγματοποιήθηκαν συγκεντρώσεις υδραργύρου στον αέρα, με φορητό φασματοφωτόμετρο (Lumex RA- 915M). Οι τιμές των εδαφικών συγκεντρώσεων υδραργύρου κυμαίνονται από 0.023 έως 13.7 mg/g. Οι συγκεντρώσεις υδραργύρου στον αέρα έδειξαν υψηλότερες τιμές υποβάθρου στην περιοχή Λακκί της καλδέρας, μεταξύ 21 και 36 ng/m3 και μέ…

ατμοσφαιρικός υδράργυροςυδροθερμικά αέριαatmospheric mercurycarbon dioxidesoil mercury atmospheric mercury hydrothermal gases carbon dioxide hydrogen sulphide010501 environmental sciences010502 geochemistry & geophysics01 natural sciencesεδαφικός υδράργυροhydrothermal gasesυδρόθειοMaterials Chemistrysoil mercuryTheologyδιοξείδιο του άνθρακαhydrogen sulphideGeomorphologyGeology0105 earth and related environmental sciencesBulletin of the Geological Society of Greece
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Late Jurassic (Kimmeridgian–Tithonian) stable isotopes (δ18O, δ13C) and Mg/Ca ratios: New palaeoclimate data from Helmsdale, northeast Scotland

2010

Abstract The data presented here provide the first detailed stable isotope ( δ 18 O, δ 13 C) and geochemical (Mg/Ca) investigation of Kimmeridgian–Tithonian belemnites from the Helmsdale Coast, Scotland, UK. Oxygen and carbon stable isotope values from well preserved specimens range from − 2.8 to + 0.3‰ and from − 2.3 to + 2.8‰ respectively. The oxygen isotope data are consistent with palaeotemperatures of up to 24 °C in the Early Kimmeridgian cymodoce Zone and down to 11 °C in the Mid Tithonian rotunda–fittoni Zones. These estimates are strongly supported by the Mg/Ca data, which also indicate a cooling episode (and very similar palaeotemperatures, 11–22 °C) at this time. The cooling event…

δ13Cbiologyδ18OStable isotope ratioPaleontologyOceanographybiology.organism_classificationIsotopes of oxygenPaleontologyIsotopes of carbonChemostratigraphyPaleoclimatologyBelemnitesEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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A 2600-year record of past polycyclic aromatic hydrocarbons (PAHs) deposition at Holzmaar (Eifel, Germany)

2014

Polycyclic aromatic hydrocarbons (PAHs) are a proxy for climate- and human-related historical fire activity which has rarely been used beyond 1800 AD. We explored the concentration and composition patterns of PAHs together with other proxies (charcoal, C, N, S, δ13C, δ15N, and δ34S) in a sediment core of Holzmaar as indicators of variations in climate and anthropogenic activity over the past 2600 years. The concentrations of pyrogenic PAHs remained low (< 500 ng g− 1) from the pre-Roman Iron Age (600 BC) until the first significant increases to ca. 1000–1800 ng g− 1 between 1700 and 1750 AD related to regional iron production. The highest increases in pyrogenic PAH concentrations occurred w…

δ13Cbusiness.industryPaleontologyδ15NOceanographyδ34SIron AgeEnvironmental chemistryvisual_artvisual_art.visual_art_mediumSedimentary organic matterCoalPolycyclic HydrocarbonsbusinessCharcoalEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Carbon cycle and sea-water palaeotemperature evolution at the Middle-Late Jurassic transition, eastern Paris Basin (France).

2014

14 pages; International audience; A very high-resolution carbon and oxygen stable isotope analysis (bulk-carbonate) of a biostratigraphically well-constrained Callovian-Oxfordian series is provided here for the first time. The homogeneity of the clayey series and the weak diagenetic alteration allow the isotopic signal variations to be considered as primary in origin. A prominent and brief negative excursion in the δ13C curve (−2‰), occurring at the start of the Middle Callovian (Jason Zone - Obductum Subzone) and correlated regionally, suggests a possible methane release. The increasing δ13C values thereafter up to the Early Oxfordian, concomitant with a warming episode, highlight the buri…

δ18OStratigraphy[SDE.MCG]Environmental Sciences/Global ChangesCallovianOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyIsotopes of oxygenCarbon cycleOxfordianPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwaterIsotope analysisδ13CbiologyCarbon isotopesGeologybiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySea-water paleotemperatures[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsPaleoenvironmental changes13. Climate actionIsotopes of carbon[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOxygen isotopesEconomic GeologyGlobal coolingBelemnitesGeology
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GEOCHEMISTRY OF THE GAS MANIFESTATIONS OF GREECE: METHANE AND LIGHT HYDROCARBONS

2017

Το σύνθετο γεωδυναμικό καθεστώς της Ελλάδας πηγάζει από την πολύπλοκη γεωλογική της ιστορία, η οποία χαρακτηρίζεται από έντονη σεισμική δραστηριότητα και ενισχυμένη γεωθερμική βαθμίδα. Αυτή η δραστηριότητα σε συνδυασμό με το ενεργό ηφαιστειακό τόξο, ευνοεί την ύπαρξη πολλών εκπομπών αερίων, με αποτέλεσμα την κατηγοριοποίηση σε CO2-, N2- και CH4-αέρια, ανάλογα με το επικρατών είδος. Η παρούσα εργασία επικεντρώνεται στο μεθάνιο και τους ελαφρούς υδρογονάνθρακες (C2-C6) με σκοπό τον προσδιορισμό της προέλευσή τους. Οι συγκεντρώσεις του CH4 (&lt;2 έως 915,200 μmol/mol) και η ισοτοπική του αναλογία (δ13C -79.8 έως +16.9 ‰, δD -298 έως +264‰) καλύπτουν ένα ευρύ φάσμα τιμών, που υποδεικνύει διαφορ…

υδροθερμικά αέρια010504 meteorology & atmospheric sciencesπροέλευση υδρογονανθράκωνMineralogyΕλληνική περιοχή010502 geochemistry & geophysics01 natural sciencesMedicinal chemistryLight hydrocarbonsSettore GEO/08 - Geochimica E Vulcanologiahydrothermal gasesεκπομπές ψυχρών αερίωνHellenic territoryorigin of hydrocarbon gasesHellenic territory hydrothermal gases cold gas emissions origin of hydrocarbon gasesMaterials Chemistrycold gas emissionsGeology0105 earth and related environmental sciences
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