Search results for "gla"

showing 10 items of 4378 documents

Effect of the Ordovician paleogeography on the (in)stability of the climate.

2014

The Ordovician Period (485–443 Ma) is characterized by abundant evidence for continental-sized ice sheets. Modeling studies published so far require a sharp CO2 drawdown to initiate this glaciation. They mostly used non-dynamic slab mixed-layer ocean models. Here, we use a general circulation model with coupled components for ocean, atmosphere, and sea ice to examine the response of Ordovician climate to changes in CO2 and paleogeography. We conduct experiments for a wide range of CO2 (from 16 to 2 times the preindustrial atmospheric CO2 level (PAL)) and for two continental configurations (at 470 and at 450 Ma) mimicking the Middle and the Late Ordovician conditions. We find that the temper…

010504 meteorology & atmospheric scienceslcsh:Environmental protectionStratigraphy010502 geochemistry & geophysics01 natural scienceslcsh:Environmental pollutionSea icelcsh:TD169-171.8Glacial periodlcsh:Environmental sciences0105 earth and related environmental scienceslcsh:GE1-350Global and Planetary Changegeographygeography.geographical_feature_categoryNorthern HemispherePaleontologyRadiative forcingOcean dynamics13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU]Sciences of the Universe [physics]Climatologylcsh:TD172-193.5OrdovicianIce sheet[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyGlobal coolingGeology[ SDU ] Sciences of the Universe [physics]
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Productivity modes in the Mediterranean Sea during Dansgaard–Oeschger (20,000–70,000 yr ago) oscillations

2013

The study of planktonic organisms during abrupt climatic variations of the last glacial period (Dansgaard-Oeschger oscillations, D-O) may reveal important insights on climatic, oceanographic and biological interactions. Here we present planktic foraminifera and coccolithophore data collected at the Ocean Drilling Program Site 963 (Sicily Channel), with a mean sampling resolution of respectively 43.5 and 98.9. yr, over the interval between 70,000 and 20,000. yr ago. The paleoenvironmental reconstruction suggests that three different scenarios can be seen across each D-O cycle: 1. oligotrophic surface water and a deep thermocline for the early Interstadials; 2. a Deep Chlorophyll Maximum and …

010506 paleontology010504 meteorology & atmospheric sciencesCoccolithophoreMediterraneanOceanography01 natural sciencesForaminifera/dk/atira/pure/sustainabledevelopmentgoals/life_below_waterWater columnMediterranean seaPaleoproductivity Dansgaard–Oeschger Mediterranean Planktonic Foraminifera CoccolithophoresCoccolithophores14. Life underwaterStadialGlacial periodSDG 14 - Life Below WaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesDeep chlorophyll maximumbiologyPaleontologybiology.organism_classificationOceanography13. Climate actionClimatologyPlanktonic ForaminiferaDansgaard-OeschgerThermoclineGeologyPaleoproductivityPalaeogeography, Palaeoclimatology, Palaeoecology
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The response of flood-plain ecosystems to the Late Glacial and Early Holocene hydrological changes: A case study from a small Central European river …

2016

Abstract We use a range of environmental variables to explore the possible drivers influencing the biota, especially the composition of aquatic invertebrates, during the Younger Dryas (YD) and Early Holocene (EH) in different river valley sites: a well-developed meandering river and the confluence zone of headwater streams. Using pollen, macrofossil, cladoceran, and chironomid as well as geochemical and lithological data as proxies for environmental factors (i.e., water depth and temperature), we attempt to show that these different sites display similar hydroclimatic signals (especially floods). The geochemical records in the studied valley are correlated with environmental factors, such a…

010506 paleontology010504 meteorology & atmospheric sciencesEnvironmental changeFloodplainta1171Fluvialpaleohydrology01 natural sciencesChironomidsYounger DryasGlacial periodHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesgeochemistryHydrologygeographygeography.geographical_feature_categoryFlood mythMacrofossil15. Life on landCladocera13. Climate actiondenudationfloodsta1181GeologyCATENA
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Age and sedimentary record of inland eolian sediments in Lithuania, NE European Sand Belt

2015

We present a study based on four inland eolian locations in Eastern, Central and Southeastern Lithuania belonging to the northeastern part of the ‘European Sand Belt’ (ESB). Although there have been several previous studies of the ESB, this north-eastern extension has not been investigated before in any detail. The sedimentary structural–textural features are investigated and a chronology was derived using optically stimulated luminescence on both quartz and feldspar. The sedimentary structures and the rounding and surface characteristics of the quartz grains argue for a predominance of eolian transport. Additionally, some structural alternations and a significant contribution of non-eolian…

010506 paleontology010504 meteorology & atmospheric sciencesLithologyEuropean Sand BeltGeochemistryFeldspar01 natural sciencesSedimentary structuresTextural featuresArts and Humanities (miscellaneous)Optically stimulated luminescence datingGlacial periodSedimentologyGeomorphology0105 earth and related environmental sciencesEarth-Surface ProcessesLithuaniaStructural featuresvisual_artPeriod (geology)visual_art.visual_art_mediumGeneral Earth and Planetary SciencesAeolian processesEolian depositsSedimentary rockGeologyQuaternary Research
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Late glacial-postglacial North African landscape and forestmanagement : Palynological and anthracological studies in the caves of Kaf Taht el-Ghar an…

2021

This work presents the anthracological and archeopalynological results obtained within the project AGRIWESTMED (ERC AdG 230561), which has involved a comprehensive retrieval of archeobiological remains based on a systematic sampling strategy, beyond the recovery of the usual archeological materials. These surveys were conducted on three sites located in the North of Morocco: the cave of Kaf Taht-el-Ghar, 8 km southeast from Tetuan, and two caves within the El Khil complex, close to Tanger. Both plant micro- and macro-remains (charred wood) were studied through palynological and anthracological analyses, respectively.

010506 paleontology010504 meteorology & atmospheric sciencesPaleolític01 natural sciencesGrazing pressureCavePaleolithicAbies pinsapoGlacial periodNeolithicEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesPalynologyEpipaleolithicgeography.geographical_feature_categorybiologyEpipaleolithicPaleontologyVegetation15. Life on landbiology.organism_classificationNorthern MoroccoArchaeologyGeographyCharcoalPollenJuniper
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Carbon and oxygen stable isotope compositions of late Pleistocene mammal teeth from dolines of Ajoie (Northwestern Switzerland)

2014

AbstractFossils of megaherbivores from eight late Pleistocene 14C- and OSL-dated doline infillings of Ajoie (NW Switzerland) were discovered along the Transjurane highway in the Swiss Jura. Carbon and oxygen analyses of enamel were performed on forty-six teeth of large mammals (Equus germanicus, Mammuthus primigenius, Coelodonta antiquitatis, and Bison priscus), coming from one doline in Boncourt (~ 80 ka, marine oxygen isotope stage MIS5a) and seven in Courtedoux (51–27 ka, late MIS3), in order to reconstruct the paleoclimatic and paleoenvironmental conditions of the region. Similar enamel δ13C values for both periods, ranging from − 14.5 to − 9.2‰, indicate that the megaherbivores lived i…

010506 paleontology010504 meteorology & atmospheric sciencesPleistocenePaleoclimateRange (biology)[SDV]Life Sciences [q-bio]Tooth enamel01 natural sciencesIsotopes of oxygenPaleontologyArts and Humanities (miscellaneous)PaleoclimatologyEarly GlacialPaleodiet0105 earth and related environmental sciencesEarth-Surface ProcessesMiddle Pleniglacial[SDV.EE]Life Sciences [q-bio]/Ecology environmentbiologyEnamel paintStable isotope ratio[SDV.BA]Life Sciences [q-bio]/Animal biology15. Life on landbiology.organism_classificationEquusPaleoenvironment13. Climate actionvisual_artvisual_art.visual_art_mediumGeneral Earth and Planetary SciencesMammalGeologyMegaherbivores
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The north-eastern aeolian ‘European Sand Belt’ as potential record of environmental changes: A case study from Eastern Latvia and Southern Estonia

2016

Abstract The Latvian and Estonian inland dunes belong to the north-eastern part of the ‘European Sand Belt’ (ESB). These dunes are widely distributed over broad glaciolacustrine plains and Late Glacial alluvial deltas, considered to be potential sources for the aeolian material. Little is known about these aeolian sediments and their substratum; here we present a detailed sedimentary structural and textural characterisation together with a luminescence-based chronology. Through a comparison between grain-size, rounding of quartz grains and surface characteristics in medium/coarse (0.5–0.8 mm) sand, and the light mineral content, we found an alternation of aeolian and periglacial components.…

010506 paleontology010504 meteorology & atmospheric sciencesThermoluminescence datingEuropean Sand BeltGeochemistrySedimentGeologyOptically stimulated luminescence01 natural sciencesEastern LatviaSouthern EstoniaSedimentary featuresAeolian depositsAeolian processesSedimentary rockAlluviumAeolian landformGlacial periodGeomorphologyGeology0105 earth and related environmental sciencesEarth-Surface ProcessesChronologyAeolian Research
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Summer air temperature, reconstructions from the last glacial stage based on rodents from the site Taillis-des-Coteaux (Vienne), Western France.

2014

AbstractThe oxygen isotope composition of phosphate from tooth enamel of rodents (δ18Op) constitutes a valuable proxy to reconstruct past air temperatures in continental environments. This method has been applied to rodent dental remains from three genera, Arvicola sp., Microtus sp. and Dicrostonyx sp., coming from Taillis-des-Coteaux, Vienne, France. This archaeological site contains an exceptionally preserved sedimentary sequence spanning almost the whole Upper Palaeolithic, including seven stratigraphic layers dated from 35 to 17 cal ka BP. The abundant presence of rodent remains offers the opportunity to quantify the climatic fluctuations coeval of the various stages of human occupation…

010506 paleontology010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesClimatePhosphate01 natural sciencesIsotopes of oxygenPaleontologyArts and Humanities (miscellaneous)Late Pleistocene[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryGlacial periodMicrotus0105 earth and related environmental sciencesEarth-Surface Processes[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyRodentbiologyLast Glacial Maximum15. Life on landbiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryOxygen isotopestomatognathic diseases[ SDE.MCG ] Environmental Sciences/Global ChangesAir temperatureArvicolaGeneral Earth and Planetary SciencesSedimentary rock[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyHeterochronyGeology
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High-frequency climate fluctuations over the last deglaciation in the Alboran Sea, Western Mediterranean: Evidence from calcareous plankton assemblag…

2018

Abstract A high resolution study, with a centennial scale resolution, has been performed on the calcareous plankton assemblage (coccolithophores and planktonic foraminifera) at Ocean Drilling Program Site 976, Alboran Sea (Western Mediterranean), focusing on the interval between 20 and 9 ka, in order to reconstruct changes in surface and subsurface water dynamics and productivity. The biotic surface water proxies integrate the extremely detailed (multi-decadal scale) geochemical data set and the pollen record already available at the core, thus providing a complete paleoenvironmental/paleoceanographic reconstruction. The results highlight the sensitivity of the calcareous plankton in record…

010506 paleontology010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesOceanography01 natural sciencessapropel Holocene sapropel S1Deglaciation14. Life underwaterStadialGlacial periodYounger DryasMeltwaterEcology Evolution Behavior and SystematicsHoloceneComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesPaleontologyWesterliesSettore GEO/01 - Paleontologia E Paleoecologia15. Life on land6. Clean waterOceanography13. Climate actionUpwellingGeology
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The response of a shallow lake and its catchment to Late Glacial climate changes — A case study from eastern Poland

2015

In this study we investigate how climate fluctuation in the Late Glacial period influenced the development of a lake and its catchment located in the East European Plain. We analyzed the sediments of the lake for pollen, subfossil Cladocera, macrofossils and chemical composition. We aimed at disentangling: (1) the climate changes and their limno-ecological responses, (2) temperature dynamics with the use of Cladocera-based transfer function (MJT) and macrofossil-based reconstruction of mean minimum July temperature (MMJT), (3) timing of the response of different proxies to environmental changes. The results of multiproxy analyses explicitly suggest that the main driver for changes in aquati…

010506 paleontology010504 meteorology & atmospheric sciencesta1171lake sedimentsDrainage basinClimate change01 natural sciencesAllerød oscillationGlacial periodYounger Dryas0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categorySubfossilMacrofossil15. Life on landcatchment developmentsubfossil cladocera13. Climate actionClimatologylate glacialmulti-proxy analysista1181Terrestrial ecosystemPhysical geographyEast European plainGeology
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