Search results for "Climate"

showing 10 items of 4934 documents

Rhinocerotid tooth enamel 18O/16O variability between 23 and 12 Ma in southwestern France.

2006

Abstract The relationship between the oxygen isotope ratio of mammal tooth enamel and that of drinking water was used to reconstruct changes in the Miocene oxygen isotope ratio of rainfall (meteoric water δ 18 O MW ). These, in turn, are related to climatic parameters (temperature, precipitation and evaporation rate). δ 18 O values of rhinocerotid teeth from the Aquitaine Basin (southwestern France) suggest a significant climatic change between 17 and 12 Ma, characterized by cooling together with precipitation increase, in agreement with other terrestrial and oceanic records. To cite this article: I. Bentaleb et al., C. R. Geoscience 338 (2006).

010506 paleontologyGeochemistry010502 geochemistry & geophysicsPalaeoclimate01 natural sciencesIsotopes of oxygenMammal/dk/atira/pure/sustainabledevelopmentgoals/clean_water_and_sanitationPaleontologystomatognathic system[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryPaleoclimatologymedicinePrecipitation0105 earth and related environmental sciencesGlobal and Planetary ChangeEnamel paintStable isotope ratioAquitaineMioceneOxygen isotope ratio cycleTooth enamelstomatognathic diseasesmedicine.anatomical_structure13. Climate actionEnamelvisual_artOxygen isotopesMeteoric watervisual_art.visual_art_mediumGeneral Earth and Planetary Sciencessense organs[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologySDG 6 - Clean Water and SanitationGeology
researchProduct

Five centuries of Central European temperature extremes reconstructed from tree-ring density and documentary evidence

2010

Future climate change will likely influence the frequency and intensity of weather extremes. As such events are by definition rare, long records are required to understand their characteristics, drivers, and consequences on ecology and society. Herein we provide a unique perspective on regional-scale temperature extremes over the past millennium, using three tree-ring maximum latewood density (MXD) chronologies from higher elevations in the European Alps. We verify the tree-ring-based extremes using documentary evidences from Switzerland, the Czech Republic, and Central Europe that allowed the identification of 44 summer extremes over the 1550-2003 period. These events include cold temperat…

010506 paleontologyGlobal and Planetary Change010504 meteorology & atmospheric sciencesCentral EuropeClimate changeContext (language use)DendroclimatologyEuropean Alp15. Life on landOceanography01 natural sciencesDocumentary evidenceMaximum latewood densityDocumentary evidenceSpatial coherenceTemperature extremeGeographyPalaeoclimatology13. Climate actionClimatologyPaleoclimatologyPeriod (geology)Dendrochronology0105 earth and related environmental sciences
researchProduct

Experimental socioecology: Integrative science for anthropocene landscape dynamics

2016

Abstract The emergence of coupled natural and human landscapes marked a transformative interval in the human past that set our species on the road to the urbanized, industrial world in which we live. This emergence enabled technologies and social institutions responsible for human-natural couplings in domains beyond rural, agricultural settings. The Mediterranean Landscape Dynamics Project (MedLand) is studying the interacting social and biophysical processes associated with these novel socioecological systems and their long-term consequences using a new form of 'experimental socioecology' made possible by recent advances in computation. We briefly describe the MedLand modeling laboratory, …

010506 paleontologyGlobal and Planetary Change010504 meteorology & atmospheric sciencesEcologybusiness.industryEcologyEnvironmental resource managementVegetation15. Life on land01 natural sciencesNatural (archaeology)Landscape dynamicsTransformative learningGeography13. Climate actionAnthropoceneSustainabilityEarth and Planetary Sciences (miscellaneous)SocioecologyHerdingbusiness0105 earth and related environmental sciencesAnthropocene
researchProduct

2019

Abstract. Records of grape harvest dates (GHDs) are the oldest and the longest continuous phenological data in Europe. However, many available series, including the well-known (Dijon) Burgundy series, are error prone because scholars so far have uncritically drawn the data from 19th century publications instead of going back to the archives. The GHDs from the famous vine region of Beaune (Burgundy) were entirely drawn from the archives and critically cross-checked with narrative evidence. In order to reconstruct temperature, the series was calibrated against the long Paris temperature series comprising the 360 years from 1659 to 2018. The 664-year-long Beaune series from 1354 to 2018 is als…

010506 paleontologyGlobal and Planetary ChangeVine010504 meteorology & atmospheric sciencesPhenologyStratigraphyPaleontology01 natural sciencesFifth percentileGeography13. Climate actionHomogeneousHigh pressureHarvestPhysical geography0105 earth and related environmental sciencesClimate of the Past
researchProduct

Coarsely crystalline cryogenic cave carbonate – a new archive to estimate the Last Glacial minimum permafrost depth in Central Europe

2012

Abstract. Cryogenic cave carbonate (CCC) represents a specific type of speleothem whose precipitation is triggered by freezing of mineralized karst water. Coarsely crystalline CCC, which formed during slow freezing of water in cave pools, has been reported from 20 Central European caves located in Germany, the Czech Republic, Slovakia and Poland. All these caves are situated in an area which was glacier-free during the Weichselian. Whereas the formation of usual types of speleothems in caves of this region usually ceased during the glacials, coarsely crystalline CCC precipitation was restricted to glacial periods. Since this carbonate type represents a novel, useful paleoclimate proxy, data…

010506 paleontologyGroundwater flowStratigraphylcsh:Environmental protectionGeochemistryAquifer010502 geochemistry & geophysicsPermafrost01 natural scienceslcsh:Environmental pollutionLatent heatlcsh:TD169-171.8Glacial periodGeomorphologylcsh:Environmental sciences0105 earth and related environmental scienceslcsh:GE1-350Global and Planetary ChangegeographyHydrogeologygeography.geographical_feature_categoryPaleontology13. Climate actionlcsh:TD172-193.5QuaternaryGroundwaterGeologyClimate of the Past
researchProduct

Recent advances in paleoflood hydrology: From new archives to data compilation and analysis

2018

8 pags, 4 figs

010506 paleontologyHistory010504 meteorology & atmospheric sciencesFlood frequency analysismedia_common.quotation_subjectFluvialManagement Monitoring Policy and LawOceanography01 natural sciencesNatural (archaeology)ScarcityHydrology (agriculture)ddc:550ChallengesWaste Management and Disposal0105 earth and related environmental sciencesWater Science and Technologymedia_commonHydrologyddc:333.7-333.9Paleoflood hydrologyFlood mythField historyAdvances13. Climate actionFlood hazardData compilationFlood hazardNatural archives
researchProduct

Conjunctive use of spectral gamma-ray logs and clay mineralogy in defining late Jurassic-early Cretaceous palaeoclimate change (Dorset, U.K.).

2006

Abstract Detrital clay mineralogy is controlled by weathered source rock, climate, transport and deposition that in turn influence the spectral gamma-ray (SGR) response of resultant sediments. Whilst a palaeoclimate signal in clay mineralogy has been established in some ancient successions, the SGR response remains contentious, largely because the data sets have yet to be collected at the same or appropriate vertical scales to allow comparison. In addition, the influence of organic matter on SGR is not always considered. Here, we present clay mineralogical, total organic carbon (TOC) and SGR analyses from the late Jurassic and early Cretaceous of the Wessex Basin, a period of previously doc…

010506 paleontologyJurassic-Cretaceous boundary[SDE.MCG]Environmental Sciences/Global ChangesSpectral gamma raychemistry.chemical_elementStructural basin010502 geochemistry & geophysicsOceanographyPalaeoclimate[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontology[SDE.MCG.CG]Environmental Sciences/Global Changes/domain_sde.mcg.cgDorsetKaoliniteOrganic matter[ SDE.MCG.CG ] Environmental Sciences/Global Changes/domain_sde.mcg.cg[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/MineralogyEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesTotal organic carbonchemistry.chemical_classificationPaleontologyThoriumClay mineralogyCretaceous[ SDE.MCG ] Environmental Sciences/Global ChangesSource rockchemistry[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyPurbeck facies[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyClay minerals[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
researchProduct

High-resolution geochemical and biotic records of the Tethyan 'Bonarelli Level' (OAE2, latest Cenomanian) from the Calabianca-Guidaloca composite sec…

2004

Abstract High-resolution micropalaeontological and chemostratigraphic records for the upper Cenomanian portion of the Calabianca–Guidaloca composite section (NW Sicily) provide new insight into the palaeoclimatic and palaeoceanographic evolution of the Tethys Ocean. The Bonarelli Level equivalent was identified on the basis of lithology and well constrained by calcareous plankton biostratigraphy and radiolarian assemblages, as well as by the δ 13 C curve showing a marked positive excursion (up to 4.7‰). The Bonarelli Level equivalent deposition is characterized by highly eutrophic conditions as testified by radiolarian proliferation. Black shale samples from the Calabianca–Guidaloca composi…

010506 paleontologyLithologyBiostratigraphy010502 geochemistry & geophysicsOceanography01 natural sciencesMicrofossilsCretaceousForaminiferaPaleontologyPalaeoceanography14. Life underwaterSicilyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyPaleontologyCretaceous Sicily Corg-rich deposits Bonarelli level equivalent Microfossils Geochemical proxies Palaeoceanography15. Life on landbiology.organism_classificationTethys OceanAnoxic watersCretaceous13. Climate actionBenthic zone[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyBonarelli level equivalentCenomanianGeology
researchProduct

Carbon, nitrogen and oxygen isotope fractionation during food cooking: Implications for the interpretation of the fossil human record.

2017

13 pages; International audience; ObjectivesStable isotope data provide insight into the reconstruction of ancient human diet. However, cooking may alter the original stable isotope compositions of food due to losses and modifications of biochemical and water components.MethodsTo address this issue, carbon, nitrogen and oxygen isotope ratios were measured on meat aliquots sampled from various animals such as pork, beef, duck and chicken, and also from the flesh of fishes such as salmon, European seabass, European pilchard, sole, gilt-head bream, and tuna. For each specimen, three pieces were cooked according to the three most commonly-known cooking practices: boiling, frying and roasting on…

010506 paleontologyMeatSwine[SHS.ANTHRO-BIO]Humanities and Social Sciences/Biological anthropologyEUROPEAN PILCHARDBiology01 natural sciencesIsotopes of oxygenAnthropology PhysicalIsotopesSalmon[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistrymedicinestable isotopeAnimals0601 history and archaeologyFood sciencehumans0105 earth and related environmental sciencesRoasting2. Zero hungerCooking Practices060101 anthropologycookingδ13CStable isotope ratioFossilsFleshfoodfood and beverages06 humanities and the arts[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrymedicine.drug_formulation_ingredient13. Climate actionAnthropology[ SHS.ANTHRO-BIO ] Humanities and Social Sciences/Biological anthropologyCattleAnatomyTunadietChickensFood Analysis
researchProduct

Influence of dissolved organic matter on rare earth elements and yttrium distributions in coastal waters

2010

International audience; Data collected during this study indicate that dissolved Y and REE (rare earth element) behaviour can be monitored through shale-normalised ratios. Relationships occurring between these ratios suggest that leaching from lithogenic materials is the main source of REE in the studied area. This process involves riverine detrital matter in the inner area of the Gulf of Palermo. Features of shale-normalised patterns and the relationship recognised between dissolved Fe and Y/Ho suggest that REE are released from Fe-rich coatings of atmospheric dust. Observed similarities between dissolved Fe and chlorophyll- content suggest that leaching of Fe-rich atmospheric particulates…

010506 paleontologyMineralogyrare earth elementsMediterranean010502 geochemistry & geophysics01 natural sciencesMediterranean seaDissolved organic carbonMediterranean Sea[SDV.BBM]Life Sciences [q-bio]/Biochemistry Molecular BiologyOrganic matter14. Life underwaterScavengingEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGeneral Environmental Sciencechemistry.chemical_classificationEcologyRare-earth elementAuthigenicParticulatesREE; Mediterranean; Ce anomalyREESettore GEO/08 - Geochimica E VulcanologiachemistryCe anomaly13. Climate actionEnvironmental chemistryGeneral Earth and Planetary SciencesSeawaterchlorophyll-YREE Ce anomaly Central Mediterranean late Quaternary Palaeoenvironmental reconstructionGeologyChemistry and Ecology
researchProduct