Search results for "Geology"

showing 10 items of 6012 documents

Signals and memory in tree-ring width and density data

2015

It has been suggested that maximum latewood density (MXD) should be used instead of tree-ring width (TRW) data to reconstruct post-volcanic cooling effects. A thorough assessment of high frequency signals and potentially differing memory effects in long MXD and TRW chronologies, in response to large volcanic eruptions, is still missing, however. We here present a compilation of MXD and TRW chronologies from 11 sites in the Northern Hemisphere, covering the past 750+ years, and containing significant June–August temperature signals. Basic assessment of the data using Superposed Epoch Analysis reveals a temporally extended response in TRW, by 2–3 years, to large volcanic eruptions, though pos…

geographygeography.geographical_feature_categoryVulcanian eruptionEcologyAtmosphereDendroclimatologyNorthern HemisphereClimate changeGeologyPlant ScienceDendroclimatologyClimatic changesLatitudeEnvironmental sciencesVolcanoClimatologyPaleoclimatologyDendrochronologyWeather--Effect of volcanic eruptions onPaleoclimatologyGeologyDendrochronologia
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Flow changes and geochemical anomalies in warm and cold springs associated with the 1992-1994 seismic sequence at Pollina, Central Sicily, Italy

2007

During a three-year discontinuous geochemical monitoring of some warm springs and cold discharges located in central-northern Sicily, some hydro-geochemical changes were observed. Excluding a possible related to a moderate seismic activity were accidentally identified. The observed anomalies showed amplitudes that were modulated by the different geometries and volumes of the feeding aquifers. A poroelastic aquifer contraction, a shaking-induced dilatancy theory as well as seismogenetic-induced changes in the properties of the aquifers have been proposed as possible mechanisms for the water flow and hydro-geochemical changes. These preliminary results could be used to design a monitoring net…

geographygeography.geographical_feature_categoryWater flowEarthquake predictionAquiferInduced seismicityCrustal stressGeophysicsGeochemistry and PetrologyPetrologyGroundwaterGeologySeismologyEarthquake Prediction Flow Change Geochemical Parameter Geochemical Anomaly Crustal Stress
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2017

Abstract. The aim of this study is to present a framework that provides new ways to characterize the spatio-temporal variability of lateral exchanges for water flow and solute transport in a karst conduit network during flood events, treating both the diffusive wave equation and the advection–diffusion equation with the same mathematical approach, assuming uniform lateral flow and solute transport. A solution to the inverse problem for the advection–diffusion equations is then applied to data from two successive gauging stations to simulate flows and solute exchange dynamics after recharge. The study site is the karst conduit network of the Fourbanne aquifer in the French Jura Mountains, wh…

geographygeography.geographical_feature_categoryWater flowSinkhole0208 environmental biotechnologyAquifer02 engineering and technologyGroundwater recharge6. Clean water020801 environmental engineeringInfiltration (hydrology)Electrical conduit13. Climate actionVadose zoneGeomorphologyGeologyPhreaticHydrology and Earth System Sciences
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Des particules charbonneuses, t�moins des variations de l'�rosion chimique d'un bassin versant calcaire durant l'holoc�ne (bassin de chaillexon, doub…

1999

Matter fluxes result from chemical and mechanical weathering that vary as a function of climate, relief, lithology and human activities. The aim of this paper is to characterize chemical weathering variations in the past using coaly particles found in both the geological substratum and the Holocene lacustrine sediments of a calcareous basin (Chaillexon lake, Doubs, France). Results point out that chemical weathering was the predominant erosional process in the watershed, which may be due to the calcareous nature of the bedrock. The significant variability of this process relative to mechanical weathering during the Holocene period can be interpreted as a consequence of the development of th…

geographygeography.geographical_feature_categoryWatershedBedrockDrainage basinOcean EngineeringWeatheringErosionSedimentary rockQuaternaryGeomorphologyEcology Evolution Behavior and SystematicsHoloceneGeologyComptes Rendus de l'Acad�mie des Sciences - Series IIA - Earth and Planetary Science
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Application of field portable EDXRF spectrometry to analysis of pigments of Levantine rock art

2010

The results of the analyses of elemental composition of red and black pigments of Levantine rock art from La Saltadora rock shelters (Valltorta gorge, Castellon, Spain) are presented in this paper. Nondestructive analyses were carried out using a portable energy dispersive X-ray fluorescence (EDXRF) spectrometer developed for in situ analysis. The results revealed the strong presence of calcium in all the analyzed locations due to the contribution of the underlying calcareous bedrock and the overlying crust. Iron is the main element detected in red pigments and manganese in black pigments. Iron and calcium ratios have been found indicative of the degree of preservation of the pictorial laye…

geographygeography.geographical_feature_category[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory060102 archaeologyBedrock010401 analytical chemistryMineralogychemistry.chemical_elementPigment composition06 humanities and the artsManganeseMass spectrometry01 natural sciences0104 chemical sciencesPigmentchemistry[CHIM.ANAL]Chemical Sciences/Analytical chemistryIn situ analysisvisual_artvisual_art.visual_art_medium0601 history and archaeologyRock artCalcareousSpectroscopyGeologyX-Ray Spectrometry
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Rhine flood deposits recorded in the Gallo-Roman site of Oedenburg (Haut-Rhin, France).

2006

13 pages; International audience; From the first to the fourth century AD, the Gallo-Roman town of Oedenburg developed in the alluvial landscape of the southern Upper Rhine Graben. Throughout this period, the landscape mosaic, composed of palaeochannels, stable palaeoislands and river terraces, continued to evolve. A district of this town, situated on a lateral Rhine channel system, was archaeologically excavated. Largescale excavation and cross-section analysis provide evidence of changing fluvial conditions during the period under study. At about AD 20 or earlier, this lateral part of the floodplain, affected by very fine sedimentation, was occupied by moribund marshy palaeochannels. When…

geographygeography.geographical_feature_category[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryFloodplainFluvialExcavationContext (language use)[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyArchaeologyGraben[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and Prehistory[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyRiver terracesPalaeochannelAlluviumGeologyEarth-Surface Processes
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Distribution and spatial structure of pelagic fish schools in relation to the nature of the seabed in the Sicily Channel (Central Mediterranean).

2009

Hydroacoustic data collected during two echosurveys carried out in the Sicily Channel in 1998 and 2002 were analysed to investigate the distribution and spatial structure of small pelagic fish species in relation to the sedimentological nature of the sea bottom. The study was carried out on two contiguous areas (labelled ZONE 1 and ZONE 2) of the continental shelf off the southern coast of Sicily, characterised by different dominant texture, ‘sand’ for ZONE 1 and ‘clayey-silt’ for ZONE 2. Simultaneous information on small pelagic fish schools and the seabed was obtained using a quantitative echo-sounder (SIMRAD EK500) that measures echoes due to the scattering from both fish schools and the…

geographygeography.geographical_feature_categoryacoustic surveySicily ChannelEcologyContinental shelffish schoolFishingPelagic zoneseabedAquatic ScienceSubstrate (marine biology)Demersal zoneEcho soundingOceanographyacoustic surveys; bottom and fish backscattering; echo-sounder; fish school; seabed; Sicily Channel.bottom and fish backscatteringGranulometryecho-sounderEcology Evolution Behavior and SystematicsSeabedGeology
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A high resolution record of the last deglaciation in the southern Tyrrhenian Sea: environmental and climatic evolution.

2002

A multidisciplinary study was carried out on core C106 collected in the Salerno Gulf (southern Tyrrhenian Sea). Two tephra layers recovered in the core, N 18 O record of Globigerinoides ruber and Globigerina bulloides and seven 14 C calibrated ages provided the stratigraphic framework. The core sediments cover the last 28 kyr BP. Seismostratigraphic analysis of a high resolution acoustic profile, integrated by the dated core samples, allowed us to reconstruct the architecture and age of sedimentary bodies on the continental shelf. An integrated study based on different taxonomic groups (nannofossils, pteropods, foraminifera, and palynomorphs) provided palaeoclimatic trends, in agreement wit…

geographygeography.geographical_feature_categorybiologyContinental shelfGeologyGlobigerina bulloidesSapropelOceanographybiology.organism_classificationPaleontologyMediterranean seaOceanographyGeochemistry and PetrologyDeglaciationGlacial periodGlobigerinoidesHoloceneGeology
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Persentase Tutupan Terumbu Karang di Perairan Pasir Putih Kabupaten Manokwari

2017

Penelitian ini dilakukan pada bulan Oktober sampai November 2014 di perairan Pasir Putih Kabupaten Manokwari, berlokasi di Pantai Air Salobar. Tujuan penelitian adalah untuk mengetahui persentase tutupan terumbu karang, kualitas fisik-kimia air dan korelasi kualitas fisik-kimia air terhadap persentase tutupan terumbu karang di bagian barat daya perairan Pasir Putih, Manokwari. Metode yang digunakan untuk memperoleh data persentase tutupan karang adalah Point Intercept Transect (PIT) pada kedalaman 3 m (Transek I), 7 m (Transek II) dan 10 m (Transek III). Hasil pengamatan diperoleh persentase tutupan karang pada Transek I adalah 91%, Transek II adalah 78% dan Transek III adalah 54%. Kondisi …

geographygeography.geographical_feature_categorybiologyCoralCoral reefbiology.organism_classificationMontipora digitataMontiporaWater depthSalinityOceanographyWater qualityTransectGeologyJURNAL SUMBERDAYA AKUATIK INDOPASIFIK
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Coral growth bands: A new and easy to use paleothermometer in paleoenvironment analysis and paleoceanography (late Miocene, Greece)

2006

[1] Modern scleractinian corals are classical components of marine shallow warm water ecosystems. Their occurrence and diversity patterns in the geological record have been widely used to infer past climates and environmental conditions. Coral skeletal composition data reflecting the nature of the coral environment are often affected by diagenetic alteration. Ghost structures of annual growth rhythms are, however, often well preserved in the transformed skeleton. We show that these relicts represent a valuable source of information on growth conditions of fossil corals. Annual growth bands were measured in massive hemispherical Porites of late Miocene age from the island of Crete (Greece) t…

geographygeography.geographical_feature_categorybiologyCoralPoritesPaleontologyLate MioceneOceanographyGeologic recordNeogenebiology.organism_classificationPaleontologyPaleothermometerOceanographyPaleoceanographyReefGeologyPaleoceanography
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