Search results for "Period"

showing 10 items of 4072 documents

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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Cultural evolution and environmental change in Central Europe between 40 and 15 ka

2020

The role of environmental change in the evolution of cultural traits is a topic of long-standing scientific debate with strongly contrasting views. Major obstacles for assessing environmental impacts on the evolution of material culture are the fragmentary nature of archaeological and – to a somewhat lesser extent – geoscientific archives and the insufficient chronological resolution of these archives and related proxy data. Together these aspects are causing difficulties in data synchronization. By no means does this paper attempt to solve these issues, but rather aims at shifting the focus from demonstrating strict chains of causes and events to describing roughly contemporaneous developm…

010506 paleontologyEnvironmental changemedia_common.quotation_subjectArchaeological recordBig Five personality traits and culture010502 geochemistry & geophysics01 natural sciencesCausality[SDE.ES]Environmental Sciences/Environmental and SocietyGeographyScientific debateEconomic geographySociocultural evolutionPeriod (music)ComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesDiversity (politics)media_common
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REWORKING OF FUSULINIDS AND CALCIPHAERIDS IN THE LERCARA FORMATION (SICILY, ITALY); GEOLOGICAL IMPLICATIONS

2004

Different fusulinids have been identified in the Lercara Formation (Sicily). They are: Reichelina sp., Schubertella paramelonica, Toriyamaia (?) sp., Neofusulinella lantenoisi, Yangchienia compressa, Rauserella staffi, Darvasites contractus, Chalaroschwagerina (Taiyuanella?) aff. davalensis, Levenella aff. evoluta, Pamirina darvasica, and Neoschwagerina ex gr. craticulifera. Small Permian foraminifers, as well as the calcispherid Asterosphaera pulchra also exist. The microfossils indicate reworking of different Permian stages, at different periods of time, and possibly also of the Mississippian (Early Carboniferous). All these resediments have been deposited within the Lercara Formation, a …

010506 paleontologyFusulinidaePaleozoicPermianForaminifèresPermianForaminiferaBiostratigraphy010502 geochemistry & geophysics01 natural sciencesPermienForaminiferaPaleontologyPalaeobiogeographyCarboniferousPhanerozoicddc:550TriasFusulinid14. Life underwaterSicilyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesbiologyRemaniementsReworkGeneral Engineeringbiology.organism_classificationTriassicFusulinesSicile[SDU]Sciences of the Universe [physics]Period (geology)GeologyPaléobiogéographie
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The Late Ordovician glacial sedimentary system of the North Gondwana platform.

2009

International audience; The Late Ordovician (Hirnantian) glaciation is examined through the North Gondwana record. This domain extended from southern high palaeo-latitudes (southeastern Mauritania, Niger) to northern lower palaeo-latitudes (Morocco, Turkey) and covered a more than 4000 km-wide section perpendicular to ice-flow lines. A major mid-Hirnantian deglaciation event subdividing the Hirnantian glaciation in two first-order cycles is recognised. As best illustrated by the glacial record in western Libya, each cycle comprises 2-3 glacial phases separated by ice-front retreats several hundreds kilometres to the south. From ice-proximal to ice-distal regions, the number of glacial surfa…

010506 paleontologyGlacial landformsequence stratigraphyHirnantianLast Glacial MaximumPost-glacial rebound15. Life on land010502 geochemistry & geophysicsNorth Africa01 natural sciencesU-shaped valleyPaleontology[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyInterglacialDeglaciationWisconsin glaciationGlacial period[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/GlaciologyGlacial recordice streamGeology0105 earth and related environmental sciences
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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-Flood-Stack: A reconstruction from the laminated sediments of Eifel maar structures during the last 60 000 years

2016

Abstract This study reconstructs the main flood phases in central Europe from event layers in sediment cores from Holocene Eifel maar lakes and Pleistocene dry maar structures. These reconstructions are combined with recent gauge time-series to cover the entire precipitation extremes of the last 60 000 years. In general, Eifel maar sediments are perfectly suited for the preservation of event layers since the deep water in the maar lakes is seasonal anoxic and therefore, bioturbation is low. However, the preservation of annual lamination is only preserved in Holzmaar and Ulmener Maar; the other cores are dated by 14C, magnetostratigraphy, tephra markers and ice core tuning. The cores were dr…

010506 paleontologyGlobal and Planetary Change010504 meteorology & atmospheric sciencesFlood mythOceanography01 natural sciencesMaarIce corePaleoclimatologyPhysical geographyYounger DryasStadialGlacial periodGeomorphologyGeologyHolocene0105 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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Évolution rétrograde de Neospathodus au cours de la crise Permo - Triasique

2016

The Permian - Triassic evolution of platform conodonts (Gondolellidae) consists mainly in developing the carina and the platform. During the sublethal environmental stress conditions subsequent to the Permian - Triassic extinction, the Wuchiapingian - Griesbachian Clarkina lineage is replaced by the primitive looking platform-lacking Dienerian - Aegean Neospathodus kummeli - Kashmirella timorensis lineage. Moreover, above Jinogondolella denticulata, end of the Capitanian Jinogondolella lineage, “Neospathodus” arcucristatus, an atavistic blade-like homeomorph that lacks a platform, underlies Protoclarkina crofti, of the base of the anagenetic Clarkina lineage. These primitive-looking forms a…

010506 paleontologyLineage (genetic)ExtinctionPermianbiologyEvolutionTriasConodontsPaleontologyÉvolutionProteromorphosis010502 geochemistry & geophysicsbiology.organism_classificationTriassic01 natural sciencesEnvironmental stressPaleontologyPhylogenèseTriasAtavismPeriod (geology)ConodontesProtéromorphosePhylogeny0105 earth and related environmental sciencesRevue de Micropaléontologie
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Pre-Hirnantian (latest Ordovician) benthic community assemblages: controls and replacements in a siliciclastic-dominated platform of the eastern Anti…

2007

17 pages; International audience; Lower-middle Ashgill sedimentary strata from the Mediterranean region have recorded a key episode of temperate-to-cold water, carbonate productivity predating the onset of the Hirnantian glaciation. The latitudinal position of the Moroccan margin of North Gondwana during Ashgill should have been adequate for the recorded development of carbonate factories. However, carbonate productivity was neither homogeneous nor laterally persistent, as documented in the eastern Anti-Atlas. Whereas in the Erfoud area, the bryozoan-dominated limestones of the Ashgill Khabt-el-Hajar Formation indicate the intensive activity of carbonate factories, these were dramatically r…

010506 paleontologyNorthern Gondwana010502 geochemistry & geophysicsOceanographyCarbonate factory[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesUnconformitychemistry.chemical_compoundPaleontologyBenthic communities14. Life underwaterGlacial periodCoquinaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesLate OrdovicianPaleontologyGondwanaMoroccochemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOrdovicianCarbonateSedimentary rockSiliciclasticGeology
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Introducing the Human Factor in Predictive Modelling: a Work in Progress

2012

International audience; In this paper we present the results of a study into integrating socio-cultural factors into predictive modelling. So far, predictive modelling has largely neglected the social and cultural dimensions of past landscapes. To maintain its value for archaeological research, therefore, it needs new methodologies, concepts and theories. For this study, we have departed from the methodology developed in the 1990s during the Archaeomedes Project. In this project, cross-regional comparisons of settlement location factors were made by analyzing the environmental context of Roman settlements in the French Rhône Valley. For the current research, we expanded the set of variables…

010506 paleontologyOperations researchregional comparison[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryComputer sciencefacteurs socio-culturelsSubject (philosophy)0211 other engineering and technologies02 engineering and technology01 natural sciencesdiachronic comparisonCultural heritage managementcomparaison diachronique0601 history and archaeology0105 earth and related environmental sciences021101 geological & geomatics engineeringcomparaison régionale[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and Prehistory060102 archaeologyPredictive modellingRoman period.Cultural resources managementpériode romaine.06 humanities and the artsWork in processPopularityEpistemologysocio-cultural factors[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and PrehistoryCriticismArchaeological heritageModélisation prédictivePredictive modelling
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