Search results for "Processes"

showing 10 items of 3831 documents

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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The Valanginian isotope event: a complex suite of palaeoenvironmental perturbations.

2011

17 pages; International audience; The Valanginian records a severe crisis of carbonate systems, both on platforms and in the pelagic realm. This crisis is roughly concomitant with the Weissert Event, characterized by a positive δ13C excursion of about 2‰in marine carbonates. However, it is unclear if the response of these two carbonate systems to the global perturbations is contemporaneous, or if they react differently. For this purpose, accumulation rates of pelagic carbonates produced by nannofossils and of platform-derived carbonates have been quantified in a hemipelagic environment (the Vocontian Basin, SE France) that has the potential to record the reaction of both shallow-water and p…

010506 paleontology[SDE.MCG]Environmental Sciences/Global ChangesGeochemistryClimate changeWeathering[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysicsOceanography01 natural sciencesCarbon cyclePaleontologychemistry.chemical_compound[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryClimate changeCarbonate production crisis14. Life underwaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesδ13CExcursionPaleontologyPelagic zoneAccumulation ratesCyclostratigraphy[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[ SDE.MCG ] Environmental Sciences/Global Changeschemistry13. Climate actionValanginian[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateGeologyδ13C Weissert Event
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Continental late Pliocene paleoclimatic history recorded in the Bresse Basin (France)

1992

International audience; We present results to show that the Beaune P & C borehole, cored in the Bresse Basin (France), records late Pliocene climatic variations. Pollen analysis allows precise correlations with northern and southern European stratigraphies. Using Kukla et al.'s (1981) climate index, we show that cold climate phases occur during the Brunssumian, at around 3.2, 3.6 and 5.2 Myr B.P., respectively, in agreement with Atlantic core results. The onset of a general cooling trend is felt early in the Reuverian, at about 3 Myr B.P. which corresponds to the end of a warm event characterized by high percentages of oak. This is followed by minor climatic pulses of increasing magnitude s…

010506 paleontology[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and Prehistory[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryBoreholePaleontologyMagnitude (mathematics)myrStructural basin010502 geochemistry & geophysicsOceanographymedicine.disease_causeNeogene01 natural sciences[SHS]Humanities and Social SciencesPaleontology13. Climate actionPollenPaleoclimatologymedicine[SHS] Humanities and Social SciencesQuaternaryEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface Processes
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Conodonts from Late Devonian island arc settings (Baruunhuurai Terrane, western Mongolia)

2020

Abstract Upper Devonian marine deposits of the Baruunhuurai Terrane in western Mongolia represent island arc settings, which yielded a diverse conodont assemblage of 30 taxa, including species of Ancyrognathus (as well as one new species), Icriodus, Mehlina, Polygnathus and Palmatolepis. Biodiversity analysis of Ancyrognathus, Pelekysgnathus, Mehlina and Icriodus shows that the Mongolian conodont assemblage consists of two endemic and few cosmopolitan taxa. Representatives of the otherwise globally distributed genus Pelekysgnathus are absent. An important factor influencing the regional distribution of conodont taxa seems to be the siliciclastic-dominated sedimentation of the Baruunhuurai T…

010506 paleontologybiologyBiodiversityPaleontology010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesDevonianPaleontologyGenusAssemblage (archaeology)Island arcLate Devonian extinctionConodontEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesTerranePalaeogeography, Palaeoclimatology, Palaeoecology
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