Search results for "Hang"

showing 10 items of 6341 documents

The ELSA - Stacks (Eifel-Laminated-Sediment-Archive): An introduction

2016

010506 paleontologyGlobal and Planetary Change010504 meteorology & atmospheric sciencesGeochemistrySedimentOceanography01 natural sciencesGeology0105 earth and related environmental sciencesGlobal and Planetary Change
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Climate indices in historical climate reconstructions: a global state of the art

2021

Narrative evidence contained within historical documents and inscriptions provides an important record of climate variability for periods prior to the onset of systematic meteorological data collection. A common approach used by historical climatologists to convert such qualitative information into continuous quantitative proxy data is through the generation of ordinal-scale climate indices. There is, however, considerable variability in the types of phenomena reconstructed using an index approach and the practice of index development in different parts of the world. This review, written by members of the PAGES (Past Global Changes) CRIAS working group – a collective of climate historians a…

010506 paleontologyGlobal and Planetary ChangeIndex (economics)Data collection010504 meteorology & atmospheric sciencesStratigraphymedia_common.quotation_subjectPaleontology01 natural sciencesEnvironmental protectionEnvironmental pollutionEnvironmental sciencesDocumentary evidenceState (polity)TD172-193.5Multidisciplinary approachTD169-171.8GE1-350Physical geography0105 earth and related environmental sciencesmedia_commonClimate of the Past
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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
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Timber Logging in Central Siberia is the Main Source for Recent Arctic Driftwood

2015

Abstract Recent findings indicated spruce from North America and larch from eastern Siberia to be the dominating tree species of Arctic driftwood throughout the Holocene. However, changes in source region forest and river characteristics, as well as ocean current dynamics and sea ice extent likely influence its spatiotemporal composition. Here, we present 2556 driftwood samples from Greenland, Iceland, Svalbard, and the Faroe Islands. A total of 498 out of 969 Pinus sylvestris ring width series were cross-dated at the catchment level against a network of Eurasian boreal reference chronologies. The central Siberian Yenisei and Angara Rivers account for 91% of all dated pines, with their oute…

010506 paleontologyGlobal and Planetary Changegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesbiologyLoggingDrainage basinDriftwoodbiology.organism_classification01 natural sciencesArcticBorealClimatology550 Earth sciences & geologySea icePhysical geographyLarchEcology Evolution Behavior and SystematicsGeologyHolocene0105 earth and related environmental sciencesEarth-Surface Processes
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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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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
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Estimating “land use heritage” to model changes in archaeological settlement patterns

2016

International audience; In this paper, we present a method to calculate a “land use heritage map” based on the concept of “memory of landscape”. Such a map can be seen as one variable among others influencing site location preference, and can be used as input for predictive models. The computed values equate to an index of long-term land use intensity. We will first discuss the method used for creating the land use heritage map, for which kernel density estimates are used.We will then present the use of these land use heritage maps for site location analysis in two study areas in SE France. Earlier analyses showed that the influence of the natural environment on settlement location choice i…

010506 paleontologyIndex (economics)[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory01 natural sciences[ SHS.GEO ] Humanities and Social Sciences/Geographysocio-cultural variablesOrder (exchange)memory of landscape0601 history and archaeologyRural settlement[ SHS.STAT ] Humanities and Social Sciences/Methods and statistics0105 earth and related environmental sciencesheritage map[SHS.STAT]Humanities and Social Sciences/Methods and statistics060102 archaeologyLand usePredictive modelling06 humanities and the arts[SHS.GEO]Humanities and Social Sciences/Geography15. Life on landArchaeologyPreferenceVariable (computer science)Geography[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and Prehistorysettlement pattern analysisSettlement (trust)Predictive modelling
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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
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Climatic fluctuations and seasonality during the Late Jurassic (Oxfordian–Early Kimmeridgian) inferred from delta18O of Paris Basin oyster shells.

2008

10 pages; International audience; Oxygen isotope data from biostratigraphically well-dated oyster shells from the Late Jurassic of the eastern Paris Basin are used to reconstruct the thermal evolution of western Tethyan surface waters during the Early Oxfordian–Early Kimmeridgian interval. Seventy eight oyster shells were carefully screened for potential diagenetic alteration using cathodoluminescence microscopy. Isotope analyses were performed on nonluminescent parts of shells (n=264). Intra-shell δ18O variability was estimated by microsampling along a transect perpendicular to the growth lines of the largest oyster shell. The sinusoidal distribution of the δ18O values along this transect …

010506 paleontologyOysterδ18O[SDE.MCG]Environmental Sciences/Global ChangesJurassic010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesIsotopes of oxygenPaleontologycarbonateGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistrybiology.animalParis BasinEarth and Planetary Sciences (miscellaneous)medicinepaleotemperatureBathymetry14. Life underwaterTransect0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologybiologyoxygen isotopesSeasonalitymedicine.disease[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryDiagenesisWaves and shallow water[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsOceanography13. Climate actionSpace and Planetary Science[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphyoysters[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Continental-scale temperature variability during the past two millennia

2013

Past global climate changes had strong regional expression. To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to two millennia. The most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multi-decadal to centennial scales, temperature variability shows distinctly different regional patterns, with more similarity within each hemisphere than between them. There were no globally synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period or Little Ice Age, but all reconstructi…

010506 paleontologyPALAEOCLIMATE AND PALAEOCENOGRAPHYPaleoclimate010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Climate change[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]910 Geography & travel01 natural sciencesCiencias de la Tierra y relacionadas con el Medio AmbienteInvestigación ClimatológicaCentennial550 Earth sciences & geology540 ChemistryPaleoclimatologyIce ageEarth temperaturePaleoclimatologySouthern Hemisphere0105 earth and related environmental sciencesCLIMATE SCIENCEAtmospherePaleoclimate; Temperature; Little Ice Age; Medieval Warm PeriodsTemperatureNorthern HemisphereClimatic changesScale (music)ClimatologyMedieval Warm PeriodsLittle Ice AgePeriod (geology)570 Life sciences; biologyGeneral Earth and Planetary SciencesCIENCIAS NATURALES Y EXACTASGeologyNature Geoscience
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