Search results for "Sediment"

showing 10 items of 1648 documents

The history and impacts of farming activities in south Greenland: an insight from lake deposits.

2013

International audience; Agriculture in southern Greenland has a two-phase history: with the Norse, who first settled and farmed the region between 985ad and circa 1450ad, and with the recent reintroduction of sheep farming (1920ad to the present). The agricultural sector in Greenland is expected to grow over the next century as anticipated climate warming extends the length of the growing season and increases productivity. This article presents a synthesis of results from a well-dated 1500-year lake sediment record from Lake Igaliku, south Greenland (61°00′N, 45°26′W, 15m asl) that demonstrates the relative impacts of modern and Norse agricultural activities. Pollen, non-pollen palynomorphs…

010506 paleontology010504 meteorology & atmospheric sciences[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory[SDE.MCG]Environmental Sciences/Global ChangesGeography Planning and DevelopmentContext (language use)[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciences[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryCoprophilous fungi0105 earth and related environmental sciencesEcologybiologyEcologyGlobal warmingSedimentPlant communityδ15N15. Life on landbiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[ SDE.MCG ] Environmental Sciences/Global ChangesDiatomProductivity (ecology)13. Climate action[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and Prehistory[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeneral Earth and Planetary SciencesGeology
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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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Winter climate signal in boreal clastic-biogenic varves : a comprehensive analysis of three varved records from 1890 to 1990 AD with meteorological a…

2017

Clastic-biogenic varves are widely used for reconstructing past climate: in boreal environments, the accumulation of minerogenic clasts on the lake floor is generally considered a proxy for past variations in spring floods reflecting previous winter conditions. However, the physical mechanisms behind this winter climate sensitivity and the influence of catchment type on the varve formation are not fully investigated. Here, we present a winter climate record inferred from the clastic laminae of three lakes located on the region of fine-grained tills in Eastern Finland spanning from AD 1890 to 1990. The minerogenic varve data are compared with instrumental meteorological and hydrological time…

010506 paleontology010504 meteorology & atmospheric sciencesta1172ta1171Drainage basinlake sedimentsNorthern Europecatchment dynamics01 natural sciencesProxy (climate)clastic-biogenic varvesta2180105 earth and related environmental sciencesgeographyVarvegeography.geographical_feature_categoryPaleontologyGeology15. Life on landRadiative forcingSubarctic climateclimate forcingBoreal13. Climate actionClastic rockClimatologyfine-grained tillsClimate sensitivityGeologyboreal climateGFF
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North Atlantic Oscillation recorded in carbonate δ18O signature from Lagunillo del Tejo (Spain)

2016

Abstract Oxygen (δ18O) and carbon (δ13C) isotope compositions of authigenic carbonates measured in Lagunillo del Tejo sediment document precipitation variability during the last millennium in the Iberian Range. Modern water samples show that Lagunillo δ18O and δD plot below the Global Meteoric Water Line (GMWL). Sediment samples show a covariant trend between carbonate δ18O and δ13C, indicating that the precipitation/evaporation ratio has largely controlled the isotopic composition of this lake. This covariant trend is used to extract information about past lake level changes. Humid periods occurred around AD 1300–1450, AD 1620–1775 and AD 1950–1980, while the driest periods were concentrat…

010506 paleontology010504 meteorology & atmospheric sciencesδ13CGlobal meteoric water lineδ18OPaleontologySedimentAuthigenicOceanography01 natural scienceschemistry.chemical_compoundOceanographychemistryNorth Atlantic oscillationCarbonatePrecipitationEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface Processes
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Structural contacts in subduction complexes and their tectonic significance: the Late Palaeozoic coastal accretionary wedge of central Chile

2007

Understanding the contact between the very low-grade metagreywacke of the Eastern Series and high-pressure metamorphosed schist of the Western Series in the Late Palaeozoic accretionary wedge of central Chile is fundamental for the understanding of the evolution of ancient accretionary wedges. We show the progressive development of structures and finite strain from the least deformed rocks in the eastern part of the Eastern Series of the accretionary wedge to high-pressure schist of the Western Series at the Pacific coast. Upright chevron folds of sedimentary layering are associated with an axial-plane foliation, S1. As the F1 folds became slightly overturned to the west, S1 was folded abou…

010506 paleontologyAccretionary wedgePaleozoicMineralogy010502 geochemistry & geophysics55101 natural sciencesPaleontologyJungpaläozoikumVAE 50014. Life underwaterChile0105 earth and related environmental sciencesVariszisch-herzynische Orogene {Geologie}SubductionSchistChile {Geologie}Geotektonische Entwicklung der Erdkruste {Geologie}GeologyTectonicsShear (geology)38.36AkkretionskeilFoliation (geology)Sedimentary rockVEX 500VAE 812Geology
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Investigating the Local Reservoir Age and Stable Isotopes of Shells from Southeast Arabia

2016

AbstractWe recently started a systematic approach to determine the reservoir age in southeast Arabia and its dependence on mollusk species and their environment. This part of the study concentrates on local reservoir age and stable isotopes of the lagoonal species Terebralia palustris and Anadara uropigimelana at Khor Kalba, Oman Sea. Environmental and nutritive influences on mollusks are reflected in the radiocarbon and stable isotope signal. We found a local reservoir age of A. uropigimelana of about 940 yr and that of T. palustris as 800 yr. Sclerochronological analyses yielded information about seasonality of growth and death in A. uropigimelana. The modern shell of Periglypta reticulat…

010506 paleontologyArcheology010504 meteorology & atmospheric sciencesbiologyStable isotope ratioSedimentbiology.organism_classification01 natural sciencesArchaeologylaw.inventionOceanographyHabitatlawSclerochronologyTerebralia palustrisAnadaraGeneral Earth and Planetary SciencesEnvironmental scienceRadiocarbon datingMangrove0105 earth and related environmental sciencesRadiocarbon
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Land use change, soil erosion and alluvial dynamic in the lower Doubs Valley over the 1st millenium AD (Neublans, Jura, France)

2003

International audience; Geochemical and particle size analyses, surface scanning magnetic susceptibility, microscopic charcoal counting and pollen analysis, have been carried out on two cores from the lower Doubs valley in order to reconstruct the land use history. The interpretation of anthropogenic pollen indicators and micro-charcoal deposits is discussed in relation to the lithological variation of sedimentary accumulation and evolution of the settlement. The environmental changes which occurred during the 1st and the 6th century AD reflect the impact of human activities on the landscape in the immediate surroundings of the site. Multiproxy indicators indicate that soil erosion as a con…

010506 paleontologyArcheology010504 meteorology & atmospheric sciencespalaeogeographymedicine.disease_cause01 natural sciences[ SHS.ENVIR ] Humanities and Social Sciences/Environmental studies[SHS.ENVIR] Humanities and Social Sciences/Environmental studiesPollenmedicineLand use land-use change and forestryCharcoalpalynologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesHydrologyLand useSurface scanningsedimentology15. Life on landerosionPerturbation (geology)1st millenium ADvisual_art[SHS.ENVIR]Humanities and Social Sciences/Environmental studiesvisual_art.visual_art_mediumAlluviumSedimentary rockPhysical geographyFranceGeologyfire
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A 2000-year record of lake ontogeny and climate variability from the north-eastern European Russian Arctic

2016

A lake sediment record from the north-eastern European Russian Arctic was examined using palaeolimnological methods, including subfossil chironomid and diatom analysis. The objective of this study is to disentangle environmental history of the lake and climate variability during the past 2000 years. The sediment profile was divided into two main sections following changes in the lithology, separating the limno-telmatic phase between ~2000 and 1200 cal. yr BP and the lacustrine phase between ~1200 cal. yr BP and the present. Owing to the large proportion of semi-terrestrial chironomids and poor modern analogues, a reliable chironomid-based temperature reconstruction for the limno-telmatic p…

010506 paleontologyArcheology010504 meteorology & atmospheric sciencesta1171chironomidsClimate change01 natural sciencesdiatomsPrecipitation0105 earth and related environmental sciencesEarth-Surface ProcessesGlobal and Planetary ChangeSubfossilEcologybiologyPaleontologySedimentpalaeolimnologybiology.organism_classificationArctic RussiaEastern europeanclimate changequantitative reconstructionDiatomArctic13. Climate actionClimatologyPeriod (geology)ta1181Physical geographyGeologyThe Holocene
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Meteorological validation of chironomids as a paleotemperature proxy using varved lake sediments

2016

In order to improve the reliability of climate models in their projections for the future, spatially and temporally detailed paleoclimate proxy data are needed. In this study, we examined annually laminated sediments from Lake Nurmijärvi (Finland) for their fossil Chironomidae assemblages over a time period with available meteorological observational data (since 1830s). In doing so, we correlated chironomid-based inferences of summer air temperatures against instrumentally measured values using two different reconstruction approaches, namely, calibration-in-space (CiS, multilake training set) and calibration-in-time (CiT, calibration of time series data against meteorological data). The re…

010506 paleontologyArcheology010504 meteorology & atmospheric sciencesta1171sedimentit01 natural sciencesPaleolimnologycalibration-in-timevarved sedimentsProxy (climate)Paleoclimatologypaleoclimatesurviaissääsket0105 earth and related environmental sciencesEarth-Surface ProcessesHydrologyGlobal and Planetary ChangechironomidaeVarveEcologypaleolimnologyPaleontologypaleolimnologiatemperature reconstructionEnvironmental scienceta1181paleoklimatologiaClimate modellämpötilaPhysical geographyHolocene
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Dating Bulk Sediments from Limnic Deposits Using a Grain-Size Approach

2013

Radiocarbon measurements on bulk subaqueous sediments typically provide ages significantly older than actual time of deposition. This is generally caused by the presence of reworked organic compounds, which are depleted in 14C. To explore this issue of age heterogeneity, we collected 4 organic-rich samples from varying depths in a lake sediment core at the Gemündener Maar (Eifel, Germany), a lake of volcanic origin. We divided each sample into 5 standard grain-size fractions: gravel, sand, silt, clay, and 1 fraction smaller than 0.45 μm. These were cleaned separately using a standard acid-alkali-acid treatment. The highly organic gravel-size fraction provided the youngest 14C ages of all gr…

010506 paleontologyArcheology060102 archaeologyGeochemistryMacrofossilSediment06 humanities and the artsSiltSedimentation01 natural sciencesGrain sizeDeposition (geology)Maarlaw.inventionlawGeneral Earth and Planetary Sciences0601 history and archaeologyRadiocarbon datingGeomorphologyGeology0105 earth and related environmental sciencesRadiocarbon
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