Search results for "FACE"

showing 10 items of 11436 documents

Late Holocene seasonal temperature variability of the western Scottish shelf (St Kilda) recorded in fossil shells of the bivalve Glycymeris glycymeris

2021

Abstract The North Atlantic Ocean and adjacent shelf seas play a crucial role in global climate. To better constrain long-term natural variability and marine-terrestrial linkages in this region, a network of highly resolved marine archives from the open ocean and continental shelves is needed. In recent decades, bivalve sclerochronology has emerged as a field providing such records from the mid- to high latitudes. In May 2014, dead valves and young live specimens of the bivalve Glycymeris glycymeris were collected at St Kilda, Scotland. A floating chronology spanning 187 years was constructed with fossil shells and radiocarbon dated to 3910–3340 cal yr before present (BP), with a probabilit…

010506 paleontologyδ18O010502 geochemistry & geophysicsOceanography01 natural scienceslaw.inventionlawSclerochronology14. Life underwaterRadiocarbon datingEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesgeographyGlycymerisgeography.geographical_feature_categorybiologyContinental shelfPaleontologyBefore Presentbiology.organism_classificationOceanography13. Climate actionGeologyChronologyPalaeogeography, Palaeoclimatology, Palaeoecology
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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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Reprint of "Shell oxygen isotope values and sclerochronology of the limpet "Patella vulgata" Linnaeus 1758 from northern Iberia: Implications for the…

2017

Abstract: Understanding environmental conditions faced by hunter-fisher-gatherers during the Pleistocene and Holocene, and interpretation of subsistence strategies, social organisation and settlement patterns, are key topics for the study of past human societies. In this respect, oxygen isotope values (?18O) of mollusc shell calcium carbonate can provide important information on palaeoclimate and the seasonality of shell collection at archaeological sites. In this paper, we tested P. vulgata shells from northern Iberia as a paleoclimate archive through the study of shell oxygen isotope values and sclerochronology of modern samples. Results showed that limpets formed their shells close to is…

010506 paleontologyδ18OPalaeoclimate010502 geochemistry & geophysicsOceanography01 natural sciencesShellsIsotopes of oxygenSclerochronologyPaleoclimatologyMollusc shellEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyLimpet010401 analytical chemistryGrowth patternsPaleontologySeasonalitybiology.organism_classification0104 chemical sciencesGeochemistryOceanographyPatella vulgataGeologyPalaeogeography, Palaeoclimatology, Palaeoecology
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Applicability and consequences of the integration of alternative models for CO<sub>2</sub> transfer velocity into a process-based lake mo…

2019

Abstract. Freshwater lakes are important in carbon cycling, especially in the boreal zone where many lakes are supersaturated with the greenhouse gas carbon dioxide (CO2) and emit it to the atmosphere, thus ventilating carbon originally fixed by the terrestrial system. The exchange of CO2 between water and the atmosphere is commonly estimated using simple wind-based parameterizations or models of gas transfer velocity (k). More complex surface renewal models, however, have been shown to yield more correct estimates of k in comparison with direct CO2 flux measurements. We incorporated four gas exchange models with different complexity into a vertical process-based physico-biochemical lake mo…

0106 biological sciences010504 meteorology & atmospheric sciences010604 marine biology & hydrobiologyEddy covariancechemistry.chemical_elementAtmospheric sciences01 natural sciences6. Clean waterCarbon cycleAtmospherechemistry.chemical_compoundWater columnchemistryTotal inorganic carbon13. Climate actionGreenhouse gasCarbon dioxideEnvironmental scienceCarbonEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesBiogeosciences
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Summarizing the state of the terrestrial biosphere in few dimensions

2020

Abstract. In times of global change, we must closely monitor the state of the planet in order to understand the full complexity of these changes. In fact, each of the Earth's subsystems – i.e., the biosphere, atmosphere, hydrosphere, and cryosphere – can be analyzed from a multitude of data streams. However, since it is very hard to jointly interpret multiple monitoring data streams in parallel, one often aims for some summarizing indicator. Climate indices, for example, summarize the state of atmospheric circulation in a region. Although such approaches are also used in other fields of science, they are rarely used to describe land surface dynamics. Here, we propose a robust method to crea…

0106 biological sciences010504 meteorology & atmospheric sciencesAtmospheric circulationlcsh:Life0207 environmental engineering02 engineering and technology010603 evolutionary biology01 natural scienceslcsh:QH540-549.5Cryosphere020701 environmental engineeringEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesData stream mininglcsh:QE1-996.5BiosphereGlobal change15. Life on landAlbedolcsh:Geologylcsh:QH501-531Arctic13. Climate actionClimatologyEnvironmental sciencelcsh:EcologyHydrosphere
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The mapping of the Posidonia oceanica (L.) Delile barrier reef meadow in the southeastern Gulf of Tunis (Tunisia)

2016

Abstract Barrier reefs are among the most important ecomorphosis for Posidonia oceanica meadows and have long been subjected to anthropic pressures. The authors mapped the entire Sidi Rais (northeastern Tunisia) Posidonia oceanica barrier reef by means of remote sensing based on processing a satellite image acquired via Google Earth © software, coupled with field observations obtained by snorkeling. The map thus produced represents the P. oceanica barrier reef in its current state, covering a total area of 156.77 ha, the reef being divided into three distinct sections separated by reverse flows with each section subject to varied anthropic factors and disturbances.

0106 biological sciences010504 meteorology & atmospheric sciencesCymodocea nodosaBarrier reefSnorkeling01 natural sciences[ SDE ] Environmental SciencesSatellite image14. Life underwaterBarrier reef mappingReef0105 earth and related environmental sciencesEarth-Surface ProcessesgeographyCymodocea nodosageography.geographical_feature_categorybiologybusiness.industry010604 marine biology & hydrobiologyPosidonia oceanicaGeologybiology.organism_classificationCurrent (stream)OceanographyRemote sensing (archaeology)Anthropic impactPosidonia oceanica[SDE]Environmental SciencesbusinessGeologyJournal of African Earth Sciences
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A combination of dichogamy and herkogamy mediates reproductive success in the desert shrub Zygophyllum fabago

2020

Abstract Zygophyllum fabago is a species within the arid-adapted family Zygophyllaceae. The species is characterized by the co-occurrence of dichogamy and herkogamy. In order to understand the effect of these two complementary anti-selfing mechanisms in reproductive success, we conducted a detailed study of floral biology in Z. fabago. Our results indicated an incomplete separation of the female and male phases which is referred to as partial dichogamy. We found two floral morphs with distinct stigma position: the Central-morph (C-morph) and the Lateral-morph (L-morph). The stigma-stamen distance in the L-morph was significantly larger than in the C-morph in early, mid, and late male stages…

0106 biological sciences010504 meteorology & atmospheric sciencesEcologybiologyReproductive successZoologySelfingOutcrossingDeserts and xeric shrublandsmedicine.disease_causebiology.organism_classification010603 evolutionary biology01 natural sciencesZygophyllum fabagoHerkogamyZygophyllaceaePollenmedicineEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesJournal of Arid Environments
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Understanding the uncertainty in global forest carbon turnover

2020

Abstract. The length of time that carbon remains in forest biomass is one of the largest uncertainties in the global carbon cycle, with both recent historical baselines and future responses to environmental change poorly constrained by available observations. In the absence of large-scale observations, models used for global assessments tend to fall back on simplified assumptions of the turnover rates of biomass and soil carbon pools. In this study, the biomass carbon turnover times calculated by an ensemble of contemporary terrestrial biosphere models (TBMs) are analysed to assess their current capability to accurately estimate biomass carbon turnover times in forests and how these times a…

0106 biological sciences010504 meteorology & atmospheric sciencesEnvironmental changelcsh:Life01 natural sciencesCarbon cyclelcsh:QH540-549.5ddc:550Baseline (configuration management)Ecology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processes[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereBiomass (ecology)lcsh:QE1-996.5BiosphereSoil carbon15. Life on landPlant functional typelcsh:GeologyEarth scienceslcsh:QH501-531[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology13. Climate actionTurnoverlcsh:EcologyPhysical geography010606 plant biology & botanyBiogeosciences
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Warming in the Agulhas Current system since the 1980's

2009

International audience; Since the 1980's, the sea surface temperature of the Agulhas Current system has increased significantly. The warming is due to an augmentation of its transport in response to an increase in wind stress curl in the South Indian Ocean at relevant latitudes. This causes an increase in the fluxes of salt and heat into the Atlantic Ocean and in the transfer of energy from the ocean to the atmosphere. Therefore, the changes we are witnessing in the region could have far reaching consequences on top of the regional impacts on ecosystem and climate. The increase in wind stress curl is consistent with a poleward shift of westerly wind in the Southern Hemisphere reported by ot…

0106 biological sciences010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global Changes010604 marine biology & hydrobiologyClimate changeAgulhas current01 natural sciencesLatitudeAtmosphereSea surface temperature[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsOceanography[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology13. Climate actionClimatologyGeneral Earth and Planetary SciencesThermohaline circulationEcosystem[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologySouthern HemisphereGeology0105 earth and related environmental sciences
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Coastal Oceanic climate change and variability from 1982 to 2009 around South Africa

2010

Changes and fluctuations in sea surface temperature (SST) around the South African coast are analysed at a monthly scale from 1982 to 2009. There is a statistically significant negative trend of up to 0.5 °C per decade in the southern Benguela from January to August, and a cooling trend of lesser magnitude along the South Coast and in the Port Elizabeth/Port Alfred region from May to August. The cooling is due to an increase in upwelling-favourable south-easterly and easterly winds. There is a positive trend in SST of up to 0.55 °C per decade in most parts of the Agulhas Current system during all months of the year, except for  KwaZulu-Natal where warming is in summer. The warming was attri…

0106 biological sciences010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesClimate changeAquatic Science01 natural sciencesLatitudeBenguela upwellingAgulhas CurrentSouthernEcology Evolution Behavior and Systematics0105 earth and related environmental sciences010604 marine biology & hydrobiologyGlobal warmingOceanic climateSouthern Annular ModeWesterliesAgulhas currentAnnular ModeSea surface temperature[ SDE.MCG ] Environmental Sciences/Global Changesclimate changeOceanography[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology13. Climate actionClimatologyEnvironmental scienceUpwelling[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyENSO
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