Search results for "Earth"

showing 10 items of 12204 documents

Subaerial exposure and drowning processes in a carbonate platform during the Mesozoic Tethyan rifting: The case of the Jurassic succession of Western…

2016

Abstract The Liassic carbonate platform succession outcropping at Monte Maranfusa (central Western Sicily) consists of a shallowing-upward sequence of peritidal carbonates, with Jurassic to Paleogene pelagic limestone and siliciclastic Tertiary covers above. The cyclic sequences of subtidal wackestones/packstones, intertidal microcrystalline carbonates with bird's-eye pores, and supratidal bioclastic grainstones are interbedded with dark layers of the following composition: 1) dark-gray, compact, and well-cemented limestone with blackish clasts, interpreted as calcretes (a type of carbonate soil) and 2) reddish calcite laminae, deformed by elongated cavities, filled with vadose silt, interp…

010506 paleontologyDrowningOutcropCarbonate platformPaleospeleothemStratigraphyPeritidal cycleGeologyPelagic sediment010502 geochemistry & geophysics01 natural scienceschemistry.chemical_compoundPaleontologyCarbonate platformCalcretechemistryNeptunian sillSubaerialCarbonateCarbonate rockSiliciclasticPaleogeneGeology0105 earth and related environmental sciences
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A low seasonality scenario in the Mediterranean Sea during the Calabrian (Early Pleistocene) inferred from fossil Arctica islandica shells

2017

Understanding past seasonal temperature variability in the ocean is essential to evaluate the effects of future climate change on marine ecosystems. Here, we estimate seasonal water temperature amplitudes from stable oxygen isotope (δ18Oshell) values of fossil shells of Arctica islandica (assuming δ18Owater= + 0.9 ± 0.1‰ V-SMOW). Specimens were collected from three Pleistocene successions (Emilian and Sicilian substages of the Calabrian) in Central and Southern Italy (i.e., Rome, Lecce and Sicily). Biostratigraphic analyses from Rome Quarry deposits indicate an age between 1.6 and 1.2 Ma, whereas Sicily and Lecce successions are slightly more recent (between 1.1 and 0.62 Ma). Prior to …

010506 paleontologyEarly PleistoceneStable oxygen isotope010504 meteorology & atmospheric sciencesPleistoceneengineering.materialOceanography01 natural sciencesPaleontologyMediterranean seaSclerochronologySclerochronology14. Life underwaterGlacial periodArctica islandicaSicilyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyAragonitePaleontologybiology.organism_classificationEcology Evolution Behavior and Systematiclanguage.human_languagePaleotemperature reconstructionOceanography13. Climate actionEarth-Surface ProcesseengineeringlanguageSicilianGeology
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Marine Early Triassic Actinopterygii from Elko County (Nevada, USA): implications for the Smithian equatorial vertebrate eclipse

2017

AbstractThe Early Triassic vertebrate record from low paleolatitudes is spotty, which led to the notion of an ‘equatorial vertebrate eclipse’ during the Smithian. Here we present articulated ray-finned fishes (Actinopterygii), collected from the marine Lower Triassic Thaynes Group at three new localities in Elko County (Nevada, USA), which were deposited within the equatorial zone. From the Smithian of the Winecup Ranch, we describe two partial skulls of the predatory actinopterygianBirgeria(Birgeriidae), attributed toB.americananew species andBirgeriasp.Birgeria americanan. sp. is distinguished from other species by a less reduced operculogular series. With an estimated total length of 1.7…

010506 paleontologyEarly Triassic10125 Paleontological Institute and MuseumStructural basin010502 geochemistry & geophysics01 natural sciencesSaurichthysPaleontologyGroup (stratigraphy)biology.animal14. Life underwaterBirgeria[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorybiologyEcologyActinopterygiiPaleontologyVertebratebiology.organism_classification1911 Paleontology560 Fossils & prehistoric lifeRidge[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyJournal of Paleontology
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Transient metazoan reefs in the aftermath of the end-Permian mass extinction

2011

5 pages; International audience; Recovery from the devastating Permian-Triassic mass extinction about 252 million years ago is usually assumed to have spanned the entire 5 million years of the Early Triassic epoch1,2. The post-crisis interval was characterized by large-scale fluctuations of the global carbon cycle and harsh marine conditions, including a combination of ocean acidification, euxinia, and fluctuating productivity3. During this interval, metazoan-dominated reefs are thought to have been replaced by microbial deposits that are considered the hallmark of the Early Triassic4-7. Here we use field and microscopic investigations to document Early Triassic bioaccumulations and reefs f…

010506 paleontologyEarly Triassic10125 Paleontological Institute and Museum[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesCarbon cyclePaleontology14. Life underwaterReefPermian–Triassic extinction event[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesExtinction eventgeographygeography.geographical_feature_categoryExtinction1900 General Earth and Planetary SciencesfungiOcean acidificationsocial scienceshumanitiesOceanography560 Fossils & prehistoric life13. Climate actionBenthic zone[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeneral Earth and Planetary Sciences[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontologygeographic locationsGeologyNature Geoscience
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Diagenesis of clay minerals and K-bentonites in Late Permian/Early Triassic sediments of the Sichuan Basin (Chaotian section, Central China).

2014

10 pages; International audience; Detailed clay mineralogical analyses were carried out on Late Permian/Early Triassic carbonate sediments exposed on the Chaotian section (Sichuan Basin, Central China). The clay assemblages are dominantly composed of illite in platform carbonates and clay seams, and illite-smectite mixed-layers (I/S) in tuff layers (K-bentonites) intercalated in the carbonate succession. Detrital and authigenic volcanogenic clay minerals have been partially replaced through illitisation processes during burial, raising questions about diagenetic effects. The precise determination of I/S occurring in K-bentonites shows that the sediments reached a temperature of about 180 °C…

010506 paleontologyEarly TriassicGeochemistry[SDV.BID]Life Sciences [q-bio]/Biodiversityengineering.material010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPalaeothermicitychemistry.chemical_compoundPaleontologySouth ChinaPermian-Triassic boundaryComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesK-bentonitesGeologyAuthigenicDiagenesischemistry13. Climate action[SDU]Sciences of the Universe [physics]Clastic rock[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyIlliteengineeringCarbonateSedimentary rockSichuan BasinClay minerals[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Direct terrestrial–marine correlation demonstrates surprisingly late onset of the last interglacial in central Europe

2011

AbstractAn interdisciplinary study of a small sedimentary basin at Neumark Nord 2 (NN2), Germany, has yielded a high-resolution record of the palaeomagnetic Blake Event, which we are able to place at the early part of the last interglacial pollen sequence documented from the same section. We use this data to calculate the duration of this stratigraphically important event at 3400 ± 350 yr. More importantly, the Neumark Nord 2 data enables precise terrestrial–marine correlation for the Eemian stage in central Europe. This shows a remarkably large time lag of ca. 5000 yr between the MIS 5e ‘peak’ in the marine record and the start of the last interglacial in this region.

010506 paleontologyEemiangeographyPaleomagnetismgeography.geographical_feature_category010504 meteorology & atmospheric sciencesAardwetenschappenBlake EventMIS 5ePalaeomagnetismLast interglacialTime lagLate onsetEemianSedimentary basin01 natural sciencesSequence (geology)PaleontologyArts and Humanities (miscellaneous)InterglacialShort PaperGeneral Earth and Planetary SciencesGeology0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary Research
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Unknown Deformations on the Facades of the Pyramid of Khafre at Giza Pyramid Complex in Egypt

2016

Abstract The pyramids of Giza in Egypt are the architectural heritage of ancient civilizations and for many thousand years served as great examples of ancient design, planning and construction solutions. Their scale is grandiose and the attempts of ancient architects to find perfect forms to ensure the structure stands for eternity are admirable. The initial geometry of the structures, their form, proportions and symmetry, was adapted to construction material and technologies available at that time. However, during more than 4500 years these monuments were damaged and partly destroyed; some pyramids were razed to the ground due to construction faults and seismic activity. The second largest…

010506 paleontologyEngineering060102 archaeologybusiness.industryPhotographic documentation06 humanities and the artsGeneral MedicineStructural engineeringfractures01 natural sciencesstone materialArchitectural heritagePyramidForensic engineeringFracture (geology)0601 history and archaeologyFacadecracksbusinessEngineering(all)photographic documentation ;0105 earth and related environmental sciencesProcedia Engineering
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Bioavailable 87Sr/86Sr in different environmental samples — Effects of anthropogenic contamination and implications for isoscapes in past migration s…

2012

(87)Sr/(86)Sr reference maps (isoscapes) are a key tool for investigating past human and animal migrations. However, there is little understanding of which biosphere samples are best proxies for local bioavailable Sr when dealing with movements of past populations. In this study, biological and geological samples (ground vegetation, tree leaves, rock leachates, water, soil extracts, as well as modern and archeological animal teeth and snail shells) were collected in the vicinity of two early medieval cemeteries ("Thuringians", 5-6th century AD) in central Germany, in order to characterize (87)Sr/(86)Sr of the local biosphere. Animal tooth enamel is not appropriate in this specific context t…

010506 paleontologyEnvironmental EngineeringFreshwater bivalveIsoscapesHuman MigrationSoil acidificationPopulationBiological AvailabilityContext (language use)Environmental pollution01 natural sciencesStrontium IsotopesAnimalsHumansEnvironmental Chemistry0601 history and archaeologyeducationWaste Management and Disposal0105 earth and related environmental scienceseducation.field_of_study060102 archaeologyEcologyBiosphereGeology06 humanities and the artsVegetation15. Life on landPollutionAnimal MigrationEnvironmental PollutionGeologyScience of The Total Environment
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New research on the development of high-resolution palaeoenvironmental proxies from geochemical properties of biogenic carbonates

2017

Abstract Geochemical signatures from biogenic carbonates are being increasingly employed as palaeoenvironmental proxies. In turn, many of these proxy archives including mollusc shells, corals, and otoliths have periodic growth structures, which allow the reconstruction of chronologically constrained records of palaeoenvironmental variability at unparalleled high temporal resolution. Studying the growth and chemistry of these periodic growth structures is known as sclerochronology. Biogenic hard parts accumulate in geological or archaeological deposits, and can be directly dated using radiometric and racemisation methods. They therefore offer the opportunity for high-resolution palaeoenviron…

010506 paleontologyEnvironmental changebiologyPaleontologyClimate change010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesProxy (climate)OceanographyMediterranean seaSclerochronologyClimate modelRadiometric datingArctica islandicaEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Cultural evolution and environmental change in Central Europe between 40 and 15 ka

2020

The role of environmental change in the evolution of cultural traits is a topic of long-standing scientific debate with strongly contrasting views. Major obstacles for assessing environmental impacts on the evolution of material culture are the fragmentary nature of archaeological and – to a somewhat lesser extent – geoscientific archives and the insufficient chronological resolution of these archives and related proxy data. Together these aspects are causing difficulties in data synchronization. By no means does this paper attempt to solve these issues, but rather aims at shifting the focus from demonstrating strict chains of causes and events to describing roughly contemporaneous developm…

010506 paleontologyEnvironmental changemedia_common.quotation_subjectArchaeological recordBig Five personality traits and culture010502 geochemistry & geophysics01 natural sciencesCausality[SDE.ES]Environmental Sciences/Environmental and SocietyGeographyScientific debateEconomic geographySociocultural evolutionPeriod (music)ComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesDiversity (politics)media_common
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