Search results for "oceanography"

showing 10 items of 1567 documents

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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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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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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Water mass exchange and variations in seawater temperature in the NW Tethys during the Early Jurassic: evidence from neodymium and oxygen isotopes of…

2009

10 pages; International audience; Oxygen and neodymium isotope analyses performed on biostratigraphically well-dated fish remains recovered from the Hettangian to Toarcian of the Paris Basin were used to reconstruct variations of Early Jurassic seawater temperature and to track oceanographic changes in the NW Tethys. Our results indicate a strong correlation between δ18O trends recorded by fish remains and belemnites, confirming the paleoenvironmental origin of oxygen isotope variations. Interestingly, temperatures recorded by pelagic fishes and nektobenthic belemnites and bottom dwelling fishes are comparable during the Late Pliensbachian sea-level lowstand but gradually differ during the …

010506 paleontologyWater mass[SDE.MCG]Environmental Sciences/Global ChangesToarcian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesIsotopes of oxygenPaleontologyWater columnGeochemistry and PetrologyPaleoceanography[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrypaleoclimateEarth and Planetary Sciences (miscellaneous)14. Life underwater0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyRadiogenic nuclidebiologyoxygen isotopesPelagic zonebiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsOceanography13. Climate actionSpace and Planetary Science[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphypaleoceanographyfish toothSeawaterneodymium isotopes[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyBelemnitesGeology
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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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Occurrence of organic-matter-rich beds in Early Cretaceous coastal evaporitic setting (Dorset, UK): a link to long-term palaeoclimate changes?

2009

11 pages; International audience; In Dorset (southern U.K.), the Durlston Bay and Lulworth Cove sections expose lowermost Cretaceous coastal marine and non-marine partly evaporitic sediments (the so-called Purbeckian facies). An interval with organic matter (OM)-rich layers is recognized in both sections. This OM-rich interval is 20 m thick in the middle of the Durlston Bay section. Within these beds, a large OM accumulation is recorded, with total organic carbon (TOC) of up to 8.5 wt%. High hydrogen index (HI) values (up to 956 mgHC/gTOC) point to a Type I OM, generally considered as derived from algal-bacterial biomass. This contrasts with the OM present in the underlying and overlying in…

010506 paleontology[SDE.MCG]Environmental Sciences/Global ChangesClimate changeJurassic[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesPalynofaciesDeposition (geology)CretaceousPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwaterCoveSea level0105 earth and related environmental sciencesTotal organic carbonCretaceous.geographygeography.geographical_feature_categoryPaleontology15. Life on land[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryCretaceousPalynofaciesBotryococcus-type algae[ SDE.MCG ] Environmental Sciences/Global ChangesOceanography13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPurbeckian faciesOrganic matterBayGeology
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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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Facies variations in response to Holocene sea-level and climate change on Bora Bora, French Polynesia: Unravelling the role of synsedimentary siderit…

2017

International audience; Five mixed carbonate-siliciclastic sedimentary facies were identified in the barrier-reef lagoon of Bora Bora using microfacies and statistical analyses of 70 sediment samples taken at high resolution from two vibrocores. Fades and fades successions were interpreted with respect to Holocene sea-level and climate changes. The windward lagoon core is characterized by sideritic marly wackestones and foraminifera-sideritic wackestones, deposited around 7700 years BP (years before present) during the early-mid Holocene transgression. At that time, extensive weathering and erosion of iron-bearing minerals from the volcanic island, due to a wetter climate, were expressed in…

010506 paleontology[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysicsOceanography01 natural sciencesForaminiferaSideritechemistry.chemical_compoundGeochemistry and Petrology14. Life underwaterLithificationReefComputingMilieux_MISCELLANEOUSHolocene0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorybiologyGeologybiology.organism_classification6. Clean waterOceanographychemistry13. Climate action[SDE]Environmental SciencesSiliciclasticProgradationGeologyMarine transgression
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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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