Search results for "Surface Processes"

showing 10 items of 1294 documents

Detrital-zircon geochronology and provenance of the El Oro Metamorphic Complex, Ecuador: Geodynamic implications for the evolution of the western Gon…

2019

Abstract The El Oro Metamorphic Complex (EOMC) in SW Ecuador has been the subject of debate for several decades. While previous studies have focused on the metamorphic and deformation history of the complex to determine its geodynamic evolution, the pre-metamorphic history and its association to units in the north-central Andes remains poorly understood. Here we present a U-Pb detrital zircon provenance study to provide insights into the depositional history and the geodynamic setting of the EOMC. Our results imply that the southern portion of the EOMC (the Tahuin division) is composed of an older Palaeozoic (pre-Famatinian) sequence in the south (El Tigre unit; c. 525-510 Ma), and younger …

010506 paleontologyProvenancePaleozoicGeology15. Life on land010502 geochemistry & geophysics01 natural sciencesSedimentary depositional environmentPaleontologyGondwana13. Climate actionGeochronologyddc:550Sedimentary rockGeology0105 earth and related environmental sciencesEarth-Surface ProcessesTerraneZircon
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Initial quartz OSL and dust mass accumulation rate investigation of the Kisiljevo loess sequence in north-eastern Serbia

2020

The thick and apparently continuous loess-palaeosol sequences in the Vojvodina region of northern Serbia are recognized and well understood as some of the oldest and most complete terrestrial European palaeoclimatic archives. By contrast, there are few published records for loess profiles from other regions in Serbia. Here we address this knowledge gap by investigating an 8 m thick loess sequence exposed near the village of Kisiljevo in north eastern Serbia, describing the pedostratigraphy and environmental magnetic signatures in detail and placing these within a chronologic framework using quartz optically stimulated luminescence (OSL) on the 4-11 and 63-90 μm size fractions. Our result…

010506 paleontologySequence (geology)Optically stimulated luminescenceLoessGeochemistrySize fractions010502 geochemistry & geophysics01 natural sciencesQuartzHoloceneGeology0105 earth and related environmental sciencesEarth-Surface Processes
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Reconstructing early Holocene seasonal bottom-water temperatures in the northern North Sea using stable oxygen isotope records of Arctica islandica s…

2021

The knowledge of seasonal temperature variability in the ocean is essential for understanding climate and its response to forcing factors. Time intervals with highly dynamic climate and increased seasonal forcing such as the early Holocene are of particular interest. Yet, the temporal resolution of most existing climate records is not sufficient to reconstruct temperature seasonality. Here, we present the first seasonally resolved, early Holocene, bottom-water temperature record from the Viking Bank in the northern North Sea. The reconstruction is based on the stable oxygen isotope data (δ18Oshell) of two crossdated, radiocarbon-dated subfossil shells of Arctica islandica (Bivalvia). Oxygen…

010506 paleontologySubfossilbiologyPaleontologyForcing (mathematics)Seasonality010502 geochemistry & geophysicsOceanographymedicine.diseasebiology.organism_classification01 natural sciencesBottom waterOceanographymedicineArctica islandicaEcology Evolution Behavior and SystematicsGeologySea levelHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesTemperature recordPalaeogeography, Palaeoclimatology, Palaeoecology
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Characterization of recent marks produced on fossil bone surface during sullegic and trephic processes and their influence on taphonomic studies

2018

Different taphonomic processes throughout the history of a fossil assemblage may preserve, modify or destroy, particular palaeobiological traits, but these processes always increase taphonomic information of the past. Similarly, fossils are affected during later stages of taphonomic history, i.e. excavation, preparation, study and storage of fossils, known as sullegic and trephic phases. Tools used during excavation and preparation of fossils can damage them and produce marks on their surface. Some of these recent marks highly mimic taphonomic marks produced before excavation. Both modern and fossil marks lead to misinterpretations and erroneous conclusions when similarities are not clearly…

010506 paleontologyTaphonomy060102 archaeologyModern and ancient marks06 humanities and the artsFossil boneSullegic and trephic processes01 natural sciencesArchaeologyExperimentPaleontologyTaphonomyAssemblage (archaeology)0601 history and archaeologyExperimental workGeology0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary International
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Taphonomic processes inconsistent with indigenous Mesolithic acculturation during the transition to the Neolithic in the Western Mediterranean

2018

Abstract We applied taphonomic analysis combined with geostatistical approaches to investigate the hypothesis that Cocina cave (Eastern Iberia) represents an acculturation context for the appearance of Neolithic Cardial pottery. In the 1970s, Fortea suggested that this important site was a prime example of acculturation because of the presence of early Neolithic pottery in late Mesolithic contexts. Since that time Cocina cave has been heralded as an example of indigenous hunter-gatherers incorporating Neolithic cultural elements into their lifeways. We analyzed the area excavated by Fortea in the 1970s by digitizing archaeological records and testing the spatial distribution of artifacts us…

010506 paleontologyTaphonomyContext (archaeology)01 natural scienceslaw.inventionPrehistoryCavelaw0601 history and archaeologygeostatisticsRadiocarbon datingMesolithicneolithic transition0105 earth and related environmental sciencesEarth-Surface Processesgeography.geographical_feature_category060102 archaeologytaphonomycocina cave06 humanities and the artsArchaeologytaphonomy; geostatistics; radiocarbon; neolithic transition; cocina caveAcculturationGeographyradiocarbonPottery
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Refitting lithic laminar fragments to assess Palaeolithic sequences: The case of Cova de les Cendres (Teulada-Moraira, Alicante, Spain)

2020

Abstract The integrity of the different levels that form a sequence and the formation processes of the archaeological deposit must be assessed as a previous step to the construction of behavioural, cultural and evolutionary interpretations. This is especially relevant when dealing with long sequences and cultural evolution constructed on them, as is the case in the research on Upper Palaeolithic. Lithic taphonomy provides insight into these issues and refitting is one of its powerful tools. This approach has been applied to the Aurignacian, Gravettian and Solutrean levels of Cova de les Cendres (Teulada-Moraira, Alicante, Spain), where fracture refits of laminar fragments –including blades,…

010506 paleontologyTaphonomyHorizontal and verticalLaminar flow010502 geochemistry & geophysicsSolutrean01 natural sciencesArchaeologySequence (geology)BladeletsSequence stratigraphyAurignacianGeology0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary International
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The space-time relationship of taxonomic diversity and morphological disparity in the Middle Jurassic ammonite radiation.

2007

14 pages; International audience; The Middle Jurassic ammonite radiation (from the late Aalenian to the end of the mid-Bathonian) is traced using combined analyses of morphological disparity and taxonomic diversity. The global signals of disparity and diversity are compared. These signals are then broken down by paleogeographical provinces to detect any heterogeneity in the radiation. An examination of the global signals reveals three biodiversity crises (discordances between signals) where morphological disparity grows while taxonomic diversity declines. The subdivision of the signals indicates the radiation was heterogeneous between provinces: the global signal is an aggregate of signals …

010506 paleontologyTaxonomic diversitymedia_common.quotation_subjectBiodiversity[SDV.BID]Life Sciences [q-bio]/BiodiversityJurassic010502 geochemistry & geophysicsOceanography01 natural sciencesPaleontologyAmmonitesPalaeogeographyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesSubdivisionmedia_common[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyAmmonite[ SDV.BID ] Life Sciences [q-bio]/Biodiversitybusiness.industrySpace timePaleontologylanguage.human_languagePaleogeographylanguagebusiness[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyDiversity (politics)Morphological disparity
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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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Modern sedimentary analogues and integrated monitoring to understand varve formation in the Mediterranean Lake Montcortès (Central Pyrenees, Spain)

2018

Este artículo contiene 13 páginas, 6 figuras, 1 tabla.

010506 paleontologyVarve010504 meteorology & atmospheric sciencesModern analoguesPaleontologySedimentOceanography01 natural sciencesSediment trapsDeposition (geology)Calcite precipitationOceanographyWater columnBiogenic varvesSediment trapPhotic zoneSedimentary rockMediterranean regionSeasonal resolutionHypolimnionEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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A multiproxy study of Younger Dryas and Early Holocene climatic conditions from the Grabia River paleo-oxbow lake (central Poland)

2015

International audience; A multi-proxy reconstruction of water depth, temperature and precipitation inferred from Cladocera, Chironomidae and pollen assemblages has been obtained from Świerczyna paleo-oxbow (central Poland) during the Younger Dryas (YD) and Early Holocene. Results suggest that the YD was relatively cold and comprised two main phases. The first (ca. 12,500–12,000 cal. yrs BP) is characterized by a continental climatic regime and a decrease in winter temperatures and precipitation but an increase in spring/summer precipitation. The second phase (ca. 12,000–11,500 cal. yrs BP) was more mild with a variable continental climate, an increase in summer and winter temperature, a len…

010506 paleontologyYounger Dryas010504 meteorology & atmospheric sciencesPaleoclimateta1171Climate changeGrowing seasonOceanography01 natural sciencesChironomidaeEarly HoloceneMirePaleoclimatologyYounger DryasPrecipitationEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesPaleontology15. Life on landCladoceraWater level13. Climate actionClimatology[SDE]Environmental SciencesPollenPhysical geographyGeology
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