Search results for "climate"

showing 10 items of 4934 documents

High-resolution clay mineralogy as a proxy for orbital tuning: example of the Hauterivian-Barremian transition in the Betic Cordillera (SE Spain).

2012

11 pages; International audience; The response of clay mineral assemblages to potential orbital forcing is tested in Mesozoic hemipelagic marl- limestone rhythmites of the Río Argos section (Betic Cordillera, Southeastern Spain). Along the section, marls are pervasively enriched in kaolinite and illite, whereas limestones are enriched in smectite-rich illite/smectite mixed-layers, suggesting that marl-limestone alternations are produced by cyclic high-frequency fluctuations of continental runoff. Spectral analyses show that clay mineral assemblages evolve accordingly to precession, obliquity and eccentricity cycles. Durations of ammonite zones are assessed at 535 kyr for the Late Hauterivia…

010506 paleontologyOrbital forcingStratigraphyCyclostratigraphyengineering.material010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyPalaeoclimate01 natural sciencesPaleontologyGeologic time scaleHauterivianMarl0105 earth and related environmental sciencesRhythmiteGeologyCyclostratigraphyFaraoni Oceanic Anoxic EventCretaceousClay minerals13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyIlliteengineeringSedimentary rockBarremianGeology
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Smithian shoreline migrations and depositional settings in Timpoweap Canyon (Early Triassic, Utah, USA).

2014

AbstractIn Timpoweap Canyon near Hurricane (Utah, USA), spectacular outcrop conditions of Early Triassic rocks document the geometric relationships between a massive Smithian fenestral-microbial unit and underlying, lateral and overlying sedimentary units. This allows us to reconstruct the evolution of depositional environments and high-frequency relative sea-level fluctuations in the studied area. Depositional environments evolved from a coastal plain with continental deposits to peritidal settings with fenestral-microbial limestones, which are overlain by intertidal to shallow subtidal marine bioclastic limestones. This transgressive trend of a large-scale depositional sequence marks a lo…

010506 paleontologyOutcropEarly Triassicshoreline migrationsEarly Triassic010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesSedimentary depositional environmentrelative sea levelPaleontology14. Life underwaterSea level0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyCanyongeographySW Utahgeography.geographical_feature_categoryTerrigenous sedimentSmithianmicrobialitesGeology15. Life on land13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesSedimentary rock[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologydepositional environments
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Climatic fluctuations and seasonality during the Late Jurassic (Oxfordian–Early Kimmeridgian) inferred from delta18O of Paris Basin oyster shells.

2008

10 pages; International audience; Oxygen isotope data from biostratigraphically well-dated oyster shells from the Late Jurassic of the eastern Paris Basin are used to reconstruct the thermal evolution of western Tethyan surface waters during the Early Oxfordian–Early Kimmeridgian interval. Seventy eight oyster shells were carefully screened for potential diagenetic alteration using cathodoluminescence microscopy. Isotope analyses were performed on nonluminescent parts of shells (n=264). Intra-shell δ18O variability was estimated by microsampling along a transect perpendicular to the growth lines of the largest oyster shell. The sinusoidal distribution of the δ18O values along this transect …

010506 paleontologyOysterδ18O[SDE.MCG]Environmental Sciences/Global ChangesJurassic010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesIsotopes of oxygenPaleontologycarbonateGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistrybiology.animalParis BasinEarth and Planetary Sciences (miscellaneous)medicinepaleotemperatureBathymetry14. Life underwaterTransect0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologybiologyoxygen isotopesSeasonalitymedicine.disease[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryDiagenesisWaves and shallow water[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsOceanography13. Climate actionSpace and Planetary Science[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphyoysters[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Continental-scale temperature variability during the past two millennia

2013

Past global climate changes had strong regional expression. To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to two millennia. The most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multi-decadal to centennial scales, temperature variability shows distinctly different regional patterns, with more similarity within each hemisphere than between them. There were no globally synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period or Little Ice Age, but all reconstructi…

010506 paleontologyPALAEOCLIMATE AND PALAEOCENOGRAPHYPaleoclimate010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Climate change[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]910 Geography & travel01 natural sciencesCiencias de la Tierra y relacionadas con el Medio AmbienteInvestigación ClimatológicaCentennial550 Earth sciences & geology540 ChemistryPaleoclimatologyIce ageEarth temperaturePaleoclimatologySouthern Hemisphere0105 earth and related environmental sciencesCLIMATE SCIENCEAtmospherePaleoclimate; Temperature; Little Ice Age; Medieval Warm PeriodsTemperatureNorthern HemisphereClimatic changesScale (music)ClimatologyMedieval Warm PeriodsLittle Ice AgePeriod (geology)570 Life sciences; biologyGeneral Earth and Planetary SciencesCIENCIAS NATURALES Y EXACTASGeologyNature Geoscience
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Unravelling extrinsic and intrinsic factors of the early Palaeozoic diversification of blastozoan echinoderms

2010

19 pages; International audience; The Subphylum Blastozoa represents more than one third of the early Palaeozoic echinoderm fauna. A comprehensive database including all records of blastozoans was built to provide quantitative analyses of palaeogeography and diversity patterns and processes, for the 10 classes currently included in this subphylum during the early Palaeozoic. The global pattern of taxonomic diversity shows two peaks during the Cambrian Series 3 and the Late Ordovician intervals. In Cambrian times, the high taxonomic diversity seems to be related with a high turnover rate and a high endemicity of blastozoan genera, whereas in Ordovician times, the rise in diversity is associa…

010506 paleontologyPaleozoicEvolutionBlastozoaEvolutionary fauna010502 geochemistry & geophysicsOceanography01 natural sciencesBlastozoaPaleontologyEcology Evolution Behavior and Systematics[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesEarth-Surface ProcessesExtinction eventDiversitybiologyCambrian Series 3EcologyEarly PalaeozoicPaleontology15. Life on landbiology.organism_classification13. Climate actionOrdovicianSiliciclastic[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyPalaeogeographyOriginationGeologyEchinodermataPalaeogeography, Palaeoclimatology, Palaeoecology
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Rich fen development in CE Europe, resilience to climate change and human impact over the last ca. 3500 years

2017

Here, for the first time in SE Poland, we document the long-term development of a rich fen and assess its sensitivity to climate change and human impacts over the last ca. 3500 years. Our results are based on a high-resolution, continuous plant macrofossil remains, mollusc and pollen record, complemented by geochemical, mineral magnetic and physical characterisation, and radiocarbon dating from Bagno Serebryskie rich fen located in SE Poland. Based on the palaeoecological data we distinguished five stages of wet habitat conditions: 5000–3300, 2800–2150, 1600–1100, 750–230, 150–10 cal yr BP and five dry periods at ca. 3300–2800, 2150–1600, 1100–750, 230–150, 10 to − 64 cal yr BP. The pollen …

010506 paleontologyPeat010504 meteorology & atmospheric sciencesClimate changeOmbrotrophicOceanographymedicine.disease_cause01 natural scienceslaw.inventionlawPollenmedicineRadiocarbon datingBogEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categoryCladium mariscusbiologyEcologyPaleontologyMacrofossilbiology.organism_classificationGeologyPalaeogeography, Palaeoclimatology, Palaeoecology
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Vegetation dynamics of Kisima Ngeda freshwater spring reflect hydrological changes in northern Tanzania over the past 1200 years: implications for pa…

2021

13 pages; International audience; Kisima Ngeda (KN), a spring on the northern margin of saline Lake Eyasi, Tanzania, sustains an Acacia-Hyphaene palm woodland and Typha swamps, while the surrounding vegetation is semi-desert. To study the vegetation changes associated with this spring, which represents a plausible modern analog for the fossil springs documented in the nearby paleoanthropological and archaeological sites of Olduvai Gorge, we analyzed the pollen content of a 43 cm-long sediment core that documents vegetation changes since the last ~1200 years (from cal yrs. C.E. 841 to 2011). Our results show that (1) Hyphaene palms, which require meso-halophytic soil conditions were most abu…

010506 paleontologyPeat010504 meteorology & atmospheric sciencesOlduvaClimate[SDE.MCG]Environmental Sciences/Global ChangesOlduvai GorgeOlduvaiWetlandWoodlandOceanography01 natural sciencesPaleovegetationEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesgeographyHyphaenegeography.geographical_feature_categorybiologyHydrosystemPaleontologyHomininVegetationGroundwater recharge15. Life on landbiology.organism_classificationArid13. Climate action[SDU]Sciences of the Universe [physics][SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPhysical geographyGeologyNgorongoro
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COMMENT TO LEHRMANN ET AL. NEW SECTIONS AND OBSERVATIONS FROM THE NANPANJIANG BASIN, SOUTH CHINA

2016

In the study of Earth-surface environmental processes during the events associated with the Permian–Triassic boundary, a key issue is the nature of the latest Permian pre-extinction surface in shallow marine limestones in numerous sites, principally within the Tethyan realm. Sediments below this surface pre-date the extinction event, so that the limestones comprising these latest Permian facies contain diverse fossil remains of organisms that lived just before the extinction. At all reported sites, this surface is disconformably overlain by post-extinction sediments, which contain microbialites in many places, particularly in Tethys. The nature of the youngest pre-extinction surface remains…

010506 paleontologyPermianOutcropStructural basin[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesPaleontology14. Life underwaterGeopetal sediemntComputingMilieux_MISCELLANEOUSEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesExtinction eventExtinctionPendent CementsMicrobialitePaleontologyOcean acidification13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesSubaerial[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyErosional historyPALAIOS
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Amphibians and reptiles as palaeonvironmental proxies during the Late Pleistocene (MIS3): The case of Stratigraphic Unit V of El Salt, Alcoi, Spain

2021

The locality of El Salt (Alcoi, Spain) is a key site for understanding the extirpation of Neanderthals in the eastern part of Iberia. In this paper, we analyse an assemblage of amphibians and reptiles from Stratigraphic Unit V (45.2 ± 3.4 ka to 44.7 ± 3.4 ka), which corresponds to one of the last regional records of Neanderthals, to improve knowledge of the palaeoecology and palaeoclimate of this event. The assemblage comprises three anurans (Pelodytes sp., Alytes obstetricans, and Epidalea calamita), two lizards (Lacertidae indet. and Chalcides bedriagai), and five snakes (Colubridae indet., Coronella sp., Coronella sp./Zamenis sp., Natrix maura, and Vipera latastei). Palaeoclimatic recons…

010506 paleontologyPleistocene[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory010502 geochemistry & geophysicsOceanography01 natural sciences//purl.org/becyt/ford/1 [https]HWMLATE PLEISTOCENE//purl.org/becyt/ford/1.5 [https]PALAEOCLIMATEZamenisLacertidaeCoronellaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyChalcides bedriagaiEcologyEpidalea calamitaIBERIAN PENINSULAPaleontology15. Life on landHERPETOFAUNAbiology.organism_classificationAridificationMERPaleoecologyGeology
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Using growth and geochemical composition of Clathromorphum compactum to track multiscale North Atlantic hydro-climate variability

2020

International audience; Records of ocean/atmosphere dynamics over the past centuries are essential to understand processes driving climate variability. This is particularly true for the Northwest Atlantic which is a key region with an essential role in global climate regulation. Over the past two decades, coralline red algae have been increasingly used as environmental and climatic archives for the marine realm and hold the potential to extend long-term instrumental measurements. Here, we investigate the possibility to extract climate and environmental information from annual growth patterns and geochemical composition of the coralline red algae, Clathromorphum compactum, from Saint-Pierre …

010506 paleontologyPopulationClimate change010502 geochemistry & geophysicsOceanography01 natural sciencesCoralline algaeAtmosphereSclerochronologyEnvironmental reconstructionSclerochronologyClathromorphum compactumClimate change14. Life underwatereducationArctica islandicaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processeseducation.field_of_studygeographygeography.geographical_feature_categorybiologyACLEnvironmental proxyPaleontologyCoralline algaebiology.organism_classification13. Climate actionArchipelagoPhysical geography[SDE.BE]Environmental Sciences/Biodiversity and EcologyGeology
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