Search results for "Chronology"

showing 10 items of 338 documents

The SISAL database: a global resource to document oxygen and carbon isotope records from speleothems

2018

Stable isotope records from speleothems provide information on past climate changes, most particularly information that can be used to reconstruct past changes in precipitation and atmospheric circulation. These records are increasingly being used to provide “out-of-sample” evaluations of isotope-enabled climate models. SISAL (Speleothem Isotope Synthesis and Analysis) is an international working group of the Past Global Changes (PAGES) project. The working group aims to provide a comprehensive compilation of speleothem isotope records for climate reconstruction and model evaluation. The SISAL database contains data for individual speleothems, grouped by cave system. Stable isotopes of oxyg…

010506 paleontologyClimate Research010504 meteorology & atmospheric sciencesClimate changeSpeleothemF800010502 geochemistry & geophysicscomputer.software_genre01 natural sciencesKlimatforskningCavePaleoclimatologylcsh:Environmental sciences0105 earth and related environmental scienceslcsh:GE1-350geographygeography.geographical_feature_categoryDatabaseStable isotope ratiospeleothemsPALEOCLIMATOLOGIAlcsh:QE1-996.5lcsh:GeologyMetadata13. Climate actionGeneral Earth and Planetary SciencesEnvironmental scienceClimate modelcomputerChronologyEarth System Science Data
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A low seasonality scenario in the Mediterranean Sea during the Calabrian (Early Pleistocene) inferred from fossil Arctica islandica shells

2017

Understanding past seasonal temperature variability in the ocean is essential to evaluate the effects of future climate change on marine ecosystems. Here, we estimate seasonal water temperature amplitudes from stable oxygen isotope (δ18Oshell) values of fossil shells of Arctica islandica (assuming δ18Owater= + 0.9 ± 0.1‰ V-SMOW). Specimens were collected from three Pleistocene successions (Emilian and Sicilian substages of the Calabrian) in Central and Southern Italy (i.e., Rome, Lecce and Sicily). Biostratigraphic analyses from Rome Quarry deposits indicate an age between 1.6 and 1.2 Ma, whereas Sicily and Lecce successions are slightly more recent (between 1.1 and 0.62 Ma). Prior to …

010506 paleontologyEarly PleistoceneStable oxygen isotope010504 meteorology & atmospheric sciencesPleistoceneengineering.materialOceanography01 natural sciencesPaleontologyMediterranean seaSclerochronologySclerochronology14. Life underwaterGlacial periodArctica islandicaSicilyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyAragonitePaleontologybiology.organism_classificationEcology Evolution Behavior and Systematiclanguage.human_languagePaleotemperature reconstructionOceanography13. Climate actionEarth-Surface ProcesseengineeringlanguageSicilianGeology
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New research on the development of high-resolution palaeoenvironmental proxies from geochemical properties of biogenic carbonates

2017

Abstract Geochemical signatures from biogenic carbonates are being increasingly employed as palaeoenvironmental proxies. In turn, many of these proxy archives including mollusc shells, corals, and otoliths have periodic growth structures, which allow the reconstruction of chronologically constrained records of palaeoenvironmental variability at unparalleled high temporal resolution. Studying the growth and chemistry of these periodic growth structures is known as sclerochronology. Biogenic hard parts accumulate in geological or archaeological deposits, and can be directly dated using radiometric and racemisation methods. They therefore offer the opportunity for high-resolution palaeoenviron…

010506 paleontologyEnvironmental changebiologyPaleontologyClimate change010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesProxy (climate)OceanographyMediterranean seaSclerochronologyClimate modelRadiometric datingArctica islandicaEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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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
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The ELSA tephra stack: Volcanic activity in the Eifel during the last 500,000 years

2016

Abstract Tephra layers of individual volcanic eruptions are traced in several cores from Eifel maar lakes, drilled between 1998 and 2014 by the Eifel Laminated Sediment Archive (ELSA). All sediment cores are dated by 14C and tuned to the Greenland interstadial succession. Tephra layers were characterized by the petrographic composition of basement rock fragments, glass shards and characteristic volcanic minerals. 10 marker tephra, including the well-established Laacher See Tephra and Dumpelmaar Tephra can be identified in the cores spanning the last glacial cycle. Older cores down to the beginning of the Elsterian, show numerous tephra sourced from Strombolian and phreatomagmatic eruptions,…

010506 paleontologyGlobal and Planetary Changegeographygeography.geographical_feature_categoryEarth scienceGeochemistry010502 geochemistry & geophysicsOceanography01 natural sciencesLapilliStrombolian eruptionMaarVolcanoMagmaPhreatomagmatic eruptionTephraTephrochronologyGeology0105 earth and related environmental sciencesGlobal and Planetary Change
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Annually resolved δ<sup>2</sup>H tree-ring chronology of the lignin methoxyl groups from Germany reflects averaged Wester…

2019

Abstract. Stable hydrogen isotopes ratios of lignin methoxyl groups (expressed as δ2HLM) of wood have been shown to reflect the climate-sensitive δ2H values of precipitation (expressed as δ2Hprecip) modulated by a large uniform negative isotope fractionation. However, a detailed calibration study among temporal variabilities of δ2HLM in tree-ring series, site-specific δ2Hprecip and climate parameters has not been performed yet. Here, we present annually resolved δ2HLM values from nine tree-ring series (derived from four Fagus sylvatica L. trees) collected near stations of the Global Isotope Network of Isotopes in Precipitation (GNIP) and the Deutsche Wetterdienst (DWD) meteorological observ…

010506 paleontologyIsotopebiologybiology.organism_classificationAtmospheric sciences01 natural scienceschemistry.chemical_compoundSurface air temperatureIsotope fractionationFagus sylvaticachemistryMeteorological observatoryEnvironmental scienceLigninPrecipitation0105 earth and related environmental sciencesChronology
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ESR/U-series chronology of early Neanderthal occupations at Cova Negra (Valencia, Spain)

2019

Abstract The spatiotemporal repartition of Neanderthal populations throughout the late Middle and early Upper Pleistocene is of great interest for our understanding of human evolution. Establishing a reliable chronology for human-bearing layers from prehistoric sites is thus essential for the study of Neanderthal population dynamics prior to modern human arrival in Europe. Cova Negra (Valencia, Spain) is one of the richest sites documenting Neanderthal fossil bones in the Iberian Peninsula (Arsuaga et al., 1989, 2007; Villaverde et al., 2014). The stratigraphic sequence includes 15 Middle Palaeolithic layers. Among them, four were dated by the ESR/U-series dating method on enamel from six h…

010506 paleontologyNeanderthalPleistocene[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryStratigraphyPopulation010502 geochemistry & geophysics01 natural sciences[SHS]Humanities and Social SciencesPrehistoryCavebiology.animalEarth and Planetary Sciences (miscellaneous)RepartitioneducationComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesgeographyeducation.field_of_studygeography.geographical_feature_categorybiologyGeologyArchaeologyHuman evolutionGeologyChronology
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Rereading a tree-ring database to illustrate depositional histories of subfossil trees

2017

Late Quaternary tree-ring chronologies have been constructed using data collected from subfossil trees preserved under favourable conditions in lake sediments and peat deposits. Tree-ring widths and densities are commonly used for reconstructions of past climate variability. An alternative way of using these data is to explore the replication curves of these chronologies. Here, we make use of previously collected data that is currently available from tree-ring databases to demonstrate the depositional histories of pine trees once accumulated into the sediment in lake (i.e., riparian trees) and peatland sites. Divergent courses of depositional histories were obtained for different sedimentar…

010506 paleontologyPeattaphonomic gain010504 meteorology & atmospheric sciencesPopulationpalaeobotanytree-ringOceanographycomputer.software_genre01 natural sciencespalaeohydrologySedimentary depositional environmentPaleoclimatologyDendrochronologyeducation0105 earth and related environmental sciencesRiparian zoneeducation.field_of_studygeographygeography.geographical_feature_categorySubfossilDatabasepalaeoecologypaleoklimatologiaQuaternarycomputerGeology
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Using growth and geochemical composition of Clathromorphum compactum to track multiscale North Atlantic hydro-climate variability

2020

International audience; Records of ocean/atmosphere dynamics over the past centuries are essential to understand processes driving climate variability. This is particularly true for the Northwest Atlantic which is a key region with an essential role in global climate regulation. Over the past two decades, coralline red algae have been increasingly used as environmental and climatic archives for the marine realm and hold the potential to extend long-term instrumental measurements. Here, we investigate the possibility to extract climate and environmental information from annual growth patterns and geochemical composition of the coralline red algae, Clathromorphum compactum, from Saint-Pierre …

010506 paleontologyPopulationClimate change010502 geochemistry & geophysicsOceanography01 natural sciencesCoralline algaeAtmosphereSclerochronologyEnvironmental reconstructionSclerochronologyClathromorphum compactumClimate change14. Life underwatereducationArctica islandicaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processeseducation.field_of_studygeographygeography.geographical_feature_categorybiologyACLEnvironmental proxyPaleontologyCoralline algaebiology.organism_classification13. Climate actionArchipelagoPhysical geography[SDE.BE]Environmental Sciences/Biodiversity and EcologyGeology
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Detrital-zircon geochronology and provenance of the El Oro Metamorphic Complex, Ecuador: Geodynamic implications for the evolution of the western Gon…

2019

Abstract The El Oro Metamorphic Complex (EOMC) in SW Ecuador has been the subject of debate for several decades. While previous studies have focused on the metamorphic and deformation history of the complex to determine its geodynamic evolution, the pre-metamorphic history and its association to units in the north-central Andes remains poorly understood. Here we present a U-Pb detrital zircon provenance study to provide insights into the depositional history and the geodynamic setting of the EOMC. Our results imply that the southern portion of the EOMC (the Tahuin division) is composed of an older Palaeozoic (pre-Famatinian) sequence in the south (El Tigre unit; c. 525-510 Ma), and younger …

010506 paleontologyProvenancePaleozoicGeology15. Life on land010502 geochemistry & geophysics01 natural sciencesSedimentary depositional environmentPaleontologyGondwana13. Climate actionGeochronologyddc:550Sedimentary rockGeology0105 earth and related environmental sciencesEarth-Surface ProcessesTerraneZircon
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