Search results for "Glacial period"

showing 10 items of 196 documents

Pleistocene paleoenvironmental reconstructions and mammalian evolution in South-East Asia: focus on fossil faunas from Thailand.

2006

16 pages; International audience; Mammalian faunal studies have provided various clues for a better reconstruction of hominid Quaternary paleoenvironments. Inthis work, two methods were used: (1) the cenogram method, based on a graphical representation of the mammalian communitystructure, and (2) the species richness of murine rodents to estimate climatic parameters. These methods were applied to Middle andLate Pleistocene mammalian faunas of South-East Asia, from South China to Indonesia. Special emphasis was laid on a fauna fromnorth-east Thailand dated back to approximately 170,000 years (i.e. a glacial period). This Thai fauna seems characteristic of aslightly open forested environment …

010506 paleontologyArcheologyPleistocene[SDE.MCG]Environmental Sciences/Global ChangesFauna010502 geochemistry & geophysics01 natural sciencesQuaternaryPaleontology[ SDV.EE.BIO ] Life Sciences [q-bio]/Ecology environment/BioclimatologyMammalian communityGlacial periodEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyPaleoenvironmementPalynologyGlobal and Planetary ChangeEcology[SDV.BID.EVO]Life Sciences [q-bio]/Biodiversity/Populations and Evolution [q-bio.PE]Geology15. Life on landThailand[ SDE.MCG ] Environmental Sciences/Global ChangesGeographyTaxon13. Climate actionInterglacialCenogram methodSpecies richness[SDV.EE.BIO]Life Sciences [q-bio]/Ecology environment/Bioclimatology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyQuaternarySpecies richness
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Diving into the Past: A Paleo Data–Model Comparison Workshop on the Late Glacial and Holocene

2019

Understanding changes in the climate of the late Pleistocene and the Holocene has long been a research topic. Studies rely on different sources of information, ranging from terrestrial and marine archives to a hierarchy of climate modeling activities. In contrast to the climate of the last millennium, novel approaches are necessary to bridge the different temporal and spatial representations of the various archives and the climate models, and to achieve a robust understanding of climate variability and climate processes on centennial-to-millennial time scales.

010506 paleontologyAtmospheric Science010504 meteorology & atmospheric sciences13. Climate actionPhysical geographyGlacial periodData model (GIS)01 natural sciencesGeologyHolocene0105 earth and related environmental sciences
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Late Quaternary palaeoenvironmental reconstruction of sediment drift accumulation in the Malta Graben (central Mediterranean Sea)

2018

The Malta Graben is a deep tectonic depression in the Sicily Channel, bounded by NW-SE normal faults and filled by thick Pliocene-Quaternary deposits. A previous analysis of a giant piston core (LC09) from the Malta Graben had revealed a wide range of sedimentary features (carbonate turbidites, bioturbated mud and scours), although the chronostratigraphic constraint of the stacking pattern has remained elusive. After establishing a reliable chronological framework based on seven radiocarbon dates for a shorter core from the Malta Graben (ANSIC03-735), a down-core analysis of planktonic foraminifer and coccolith abundance, stable isotopes and sediment grain size was carried out. Since the la…

010506 paleontologyDeep chlorophyll maximum010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaMalta Graben; Stratigraphy; Sedimentary FeaturesLast Glacial MaximumEnvironmental Science (miscellaneous)OceanographyGeotechnical Engineering and Engineering Geology01 natural sciencesGrabenPaleontologyMediterranean seaEarth and Planetary Sciences (miscellaneous)Glacial periodYounger DryasQuaternaryHoloceneGeology0105 earth and related environmental sciences
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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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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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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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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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Quartz OSL dating of late quaternary Chinese and Serbian loess: A cross Eurasian comparison of dust mass accumulation rates

2019

© 2018 Elsevier Ltd and INQUA. Reconstructing dust Mass Accumulation Rate (MAR) from loess deposits is critical to understanding past atmospheric mineral dust activity and requires accurate independent age models from loess deposits across Europe and Asia. Previous correlations of loess in Europe and China have tended to focus on multi-millennial timescales, with no detailed examination of dust MAR at the two ends of the Eurasian loess belt on shorter, sub-orbital scales. Here we present a detailed quartz optically stimulated luminescence (OSL) chronology from the Serbian Titel Loess Plateau (Veliki Surduk loess core) and the Chinese Loess Plateau (Lingtai section). The luminescence ages pa…

010506 paleontologyTitel loess plateau010504 meteorology & atmospheric sciencesOptically stimulated luminescenceOSL datingGeochemistryLoessDustMars Exploration ProgramMineral dust01 natural sciencesMARLoessChinese Loess PlateauGlacial periodQuaternary[PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph]QuartzGeologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesChronology
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Fire–vegetation relationships during the last glacial cycle in a low mountain range (Eifel, Germany)

2021

Abstract Lake sediments can provide useful archives to reconstruct past vegetation changes or fire history. To comprehend how vegetation and fire history have correlated during the last 130,000 years, we used two lake sediment records with known patterns of pollen and botanical macro remains and supplemented this data by analyses of lignin-derived phenols as markers for local vegetation inputs and by benzene polycarboxylic acids (BPCAs) as markers for total fire residue inputs (black carbon, BC). The two sediment archives originated from two maar lakes in the Eifel, which is part of the low mountain ranges in central Germany. A lignin-derived phenol index showed woody angiosperms and gymnos…

010506 paleontologygeographyEemiangeography.geographical_feature_categoryPaleontologySedimentVegetation010502 geochemistry & geophysicsOceanographymedicine.disease_cause01 natural sciencesMaarPollenInterglacialmedicineGlacial periodPhysical geographyEcology Evolution Behavior and SystematicsMountain rangeGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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