Search results for "Cyc"

showing 10 items of 11160 documents

Identification of processes that control the stable isotope composition of rainwater in the humid tropical West-Central Africa.

2020

12 pages; International audience; This study interprets 11 years (2006 to 2016) and 6 months (March to August in 2017) of respectively monthly and daily isotopic (δD and δ18O) monitoring of rain at Douala (Cameroon), a humid tropical station in Western Africa. The main scope is to analyze the climate controls on precipitation isotopes at different timescales. Firstly, we examine the annual cycles of δ18O. Over the 11 years of survey, the annual cycle exhibits a W shape that is quite reproducible from year to year, with two minima in spring and autumn periods. Based on back trajectory calculations and remote sensing observations of water vapor isotopic composition, we show that the observed …

010504 meteorology & atmospheric sciencesδ18O0207 environmental engineeringHumid subtropical climate02 engineering and technologyAtmospheric sciencesAir back trajectory01 natural sciencesGPCP precipitation[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrySpring (hydrology)Precipitation020701 environmental engineeringδ18OComputingMilieux_MISCELLANEOUSAir mass0105 earth and related environmental sciencesWater Science and TechnologyWater vapor[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_categoryStable isotope ratioAnnual cycleConvective activity[SDU]Sciences of the Universe [physics]13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyEnvironmental scienceWater vapor
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In situ carbon and oxygen isotopes measurements in carbonates by fiber coupled laser diode-induced calcination: A step towards field isotopic charact…

2021

International audience; Natural stable isotopes ratios (δ13Ccarb and δ18Ocarb) of carbonates archived in the geological record are routinely used to reconstruct local and global paleo temperatures and the secular evolution of the biogeochemical carbon cycle. The state-of-the-art technique, employed since the mid 20th century, to measure these isotopic ratios starts with field sampling followed by several steps of physical and chemical laboratory preparation including: (i) microdrilling and/or sawing and crushing, (ii) CO2 release by wet acid digestion, (iii) gas equilibration, purification and transfer, before (iv) gas phase IRMS measurements. While these steps are time and resource consumi…

010504 meteorology & atmospheric sciencesδ18OCarbonate mineralsAnalytical chemistryCarbonateschemistry.chemical_elementLaser010502 geochemistry & geophysics01 natural scienceslaw.inventionchemistry.chemical_compoundSideriteGeochemistry and Petrologylaw[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryCalcination0105 earth and related environmental sciencesCarbon isotopesGeologyCarbon cycleCalcium carbonatechemistry13. Climate actionCarbon dioxideOxygen isotopesCarbonateCarbonGeology
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Large-scale, millennial-length temperature reconstructions from tree-rings

2018

Supported by the German Science Foundation, grants # Inst 247/665-1 FUGG and ES 161/9-1. SSG acknowledges support by the Alexander von Humboldt Foundation, KJA by US National Science Foundation grants AGS-1501856 and NSF AGS-1501834, and JL and LS by the Belmont Forum and JPI-Climate, Collaborative Research Action INTEGRATE. Over the past two decades, the dendroclimate community has produced various annually resolved, warm season temperature reconstructions for the extratropical Northern Hemisphere. Here we compare these tree-ring based reconstructions back to 831 CE and present a set of basic metrics to provide guidance for non-specialists on their interpretation and use. We specifically d…

010506 paleontology010504 meteorology & atmospheric sciencesNDASPlant ScienceWarm season01 natural sciencesG1Extratropical cycloneddc:550Little ice ageBeneficial effectsWarm season temperatures0105 earth and related environmental sciencesNorthern Hemisphereddc:333.7-333.9EcologyNorthern HemisphereG Geography (General)Medieval Warm PeriodCovarianceTree-ring widthMaximum latewood densityTree (data structure)ClimatologyLittle Ice AgeScale (map)Geology
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Orbital forcing of tree-ring data

2012

Based on an analysis of maximum latewood density data from northern Scandinavia, along with published dendrochronological records, this study finds evidence that previous tree-ring-reliant reconstructions of large-scale near-surface air temperature underestimated long-term pre-industrial warmth during Medieval and Roman times. Solar insolation changes, resulting from long-term oscillations of orbital configurations1, are an important driver of Holocene climate2,3. The forcing is substantial over the past 2,000 years, up to four times as large as the 1.6 W m−2 net anthropogenic forcing since 1750 (ref. 4), but the trend varies considerably over time, space and with season5. Using numerous hi…

010506 paleontology010504 meteorology & atmospheric sciencesOrbital forcingGlobal changeEnvironmental Science (miscellaneous)01 natural sciencesLatitudeCarbon cycleBorealArctic13. Climate actionClimatologyTree ring dataSocial Sciences (miscellaneous)GeologyHolocene0105 earth and related environmental sciencesNature Climate Change
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Oxygen isotope compositions of phosphate from arvicoline teeth and Quaternary climatic changes, Gigny, French Jura

2004

Oxygen isotope compositions of biogenic phosphates from mammals are widely used as proxies of the isotopic compositions of meteoric waters that are roughly linearly related to the air temperature at high- and mid-latitudes. An oxygen isotope fractionation equation was determined by using present-day European arvicoline (rodents) tooth phosphate: δ18Op = 20.98(±0.59) + 0.572(±0.065) δ18Ow. This fractionation equation was applied to the Late Pleistocene karstic sequence of Gigny, French Jura. Comparison between the oxygen isotope compositions of arvicoline tooth phosphate and Greenland ice core records suggests to reconsider the previously established hypothetical chronology of the sequence. …

010506 paleontology010504 meteorology & atmospheric sciencesPleistoceneGeochemistryFractionationOxygen isotope ratio cyclePhosphate01 natural sciencesIsotopes of oxygenchemistry.chemical_compoundPaleontologyArts and Humanities (miscellaneous)chemistryIce coreGeneral Earth and Planetary SciencesQuaternaryGeology0105 earth and related environmental sciencesEarth-Surface ProcessesChronologyQuaternary Research
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Annual 14C Tree-Ring Data Around 400 AD: Mid- and High-Latitude Records

2019

ABSTRACTTwo tree-ring series, one from a high-latitude pine tree (located in northern Scandinavia) and one from a mid-latitude oak tree (located in eastern Germany) were analyzed for radiocarbon (14C) at annual resolution. The new records cover the calendar date ranges 290–460 AD and 382–486 AD, respectively, overlapping by 79 yr. The series show similar trends as IntCal13. However, some significant deviations around 400 AD are present with lower Δ14C (higher 14C ages). An average offset between the two new series and IntCal13 of about 20 years in conventional 14C age is observed. A latitudinal 14C offset between the tree sites in central and northern Europe, as would be expected due to the…

010506 paleontologyArcheologyCalendar dateSeries (stratigraphy)010504 meteorology & atmospheric sciencesMagnitude (mathematics)01 natural sciencesSolar cyclelaw.inventionlawHigh latitudeDendrochronologyGeneral Earth and Planetary SciencesRadiocarbon datingPhysical geographyTree ring dataGeology0105 earth and related environmental sciencesRadiocarbon
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Seasonality and Intensity of Shellfish Harvesting on the North Coast of British Columbia

2013

ABSTRACT Biogeochemical and growth increment analyses show contrasting seasonal patterns of butter clam collection and rates of harvest intensity between archaeological shell midden sites from the Dundas Islands archipelago and the mainland coast in Prince Rupert Harbour, northern British Columbia. Growth increment analysis shows more intensive clam harvest in the Dundas Islands in comparison to the residential sites in Prince Rupert Harbour. Stable oxygen isotope analysis shows multi-seasonal collection of clams in the Dundas Islands and a more seasonally specific emphasis in Prince Rupert Harbour. Comparison of these results to those of similar studies in the Namu region on the central co…

010506 paleontologyArcheologyHistoryBiogeochemical cycleanimal structuresOceanography01 natural sciencesmedicine0601 history and archaeology14. Life underwaterShellfishComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencescomputer.programming_languageIsotope analysisgeography.geographical_feature_category060102 archaeologyEcology06 humanities and the artsSeasonalitymedicine.diseaseMiddenFisheryGeographyOceanographyHarbourArchipelago[SDE]Environmental Sciencescomputer
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Astrochronology of the Valanginian Stage from reference sections (Vocontian Basin, France) and palaeoenvironmental implications for the Weissert Even…

2013

12 pages; International audience; High-resolution gamma-ray measurements performed on five biostratigraphically well-dated reference sections from the Vocontian Basin (south-eastern France) are used to develop a new astrochronology of the Valanginian Stage and its subdivisions (i.e. ammonite and calcareous nannofossil zones and subzones). Spectral analyses show a pervasive dominance of 405-kyr eccentricity cycles with the expression of 100-kyr eccentricity, obliquity and precession. Previous rough estimates of Valanginian Stage duration ranged from 3.9 to 6.5 myr but were generally based on less reliable or indirect methods. This study provides a precise duration of 5.08 myr, tuning the ser…

010506 paleontologyBiozone[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysicsOceanographyPalaeoclimate01 natural sciencesPaleontologyGeologic time scaleStage (stratigraphy)Ecology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesAmmoniteAstrochronologySeries (stratigraphy)High-resolution gamma-rayParaná-EtendekaPaleontologyCyclostratigraphylanguage.human_languageVocontian BasinStratigraphy13. Climate actionValanginian[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphylanguageGeologyWeissert Event
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Drowning of a carbonate platform as a precursor stage of the Early Toarcian global anoxic event (Southern Provence sub-Basin, South-east France)

2011

The Toarcian Oceanic Anoxic Event is well-known as coinciding with a carbonate crisis, coupled with organic matter accumulation and perturbation of the carbon cycle expressed by carbon-isotope excursions. In this palaeoenvironmental setting, the present research attempts to better constrain the palaeoenvironmental conditions leading to the drowning of a carbonate platform during Late Pliensbachian to Early Toarcian times. This study is based on the integrated sedimentological, diagenetic and geochemical (stable isotopes and Rock-Eval pyrolysis) analysis of several stratigraphic successions located in the Southern Provence sub-Basin (South-east France). Eodiagenetic ferroan calcite cements b…

010506 paleontologyCarbonate platformStratigraphyGeology15. Life on land010502 geochemistry & geophysicsCarbonate hardgrounds01 natural sciencesAnoxic watersCarbon cycleDiagenesisSedimentary depositional environmentPaleontologychemistry.chemical_compoundchemistry13. Climate actionCarbonateSedimentary rock14. Life underwaterGeology0105 earth and related environmental sciencesSedimentology
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Detailed record of the mid-Oxfordian (Late Jurassic) positive carbon-isotope excursion in two hemipelagic sections (France and Switzerland): A plate …

2007

14 pages; International audience; The Oxfordian (Late Jurassic) was a time of widespread change in Jurassic marine (carbonate) sedimentation patterns. A marked positive excursion in δ13C is dated as Middle Oxfordian in age. In this study we investigate if changes in carbonate sedimentation coincided with altered carbon cycling and climate. We use C-isotope records as a proxy for the evolution of the carbon cycle and compare δ13C-trends with the evolution of sedimentation in a segment of the opening Tethys seaway. One of the studied sections is located in the Subalpine basin of France (Trescléoux and Oze), the other in the Swiss Jura mountains (Liesberg). Carbon-isotope stratigraphy of carbo…

010506 paleontologyClimate[SDE.MCG]Environmental Sciences/Global ChangesCarbon stable isotopes010502 geochemistry & geophysicsOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciences[ SDE.MCG.CPE ] Environmental Sciences/Global Changes/domain_sde.mcg.cpeCarbon cycleOxfordianchemistry.chemical_compoundPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwaterTethysEcology Evolution Behavior and SystematicsSea level[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography0105 earth and related environmental sciencesEarth-Surface ProcessesTotal organic carbon[ SDU.STU.OC ] Sciences of the Universe [physics]/Earth Sciences/OceanographyOcean currentGlobal warmingExcursionPaleontologyCarbon cycle[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryPlate tectonics[ SDE.MCG ] Environmental Sciences/Global ChangeschemistryPalaeo-oceanography13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateGeology
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