Search results for "ORC"

showing 10 items of 4623 documents

Causes and consequences of past and projected Scandinavian summer temperatures, 500-2100 AD

2011

Tree rings dominate millennium-long temperature reconstructions and many records originate from Scandinavia, an area for which the relative roles of external forcing and internal variation on climatic changes are, however, not yet fully understood. Here we compile 1,179 series of maximum latewood density measurements from 25 conifer sites in northern Scandinavia, establish a suite of 36 subset chronologies, and analyse their climate signal. A new reconstruction for the 1483–2006 period correlates at 0.80 with June–August temperatures back to 1860. Summer cooling during the early 17th century and peak warming in the 1930s translate into a decadal amplitude of 2.9°C, which agrees with existin…

010506 paleontologyAtmospheric Science010504 meteorology & atmospheric sciencesAtmospheric circulationClimate ChangeClimate changelcsh:MedicineForcing (mathematics)Scandinavian and Nordic Countries01 natural sciencesAtmospheric CirculationBiospherePaleoclimatologyEnvironmental GeographyAtmospheric DynamicsPaleoclimatologylcsh:Science0105 earth and related environmental sciencesClimatologySeries (stratigraphy)MultidisciplinaryGeographyAtmospherelcsh:RTemperature/dk/atira/pure/core/subjects/geography15. Life on landSea surface temperatureGeographyPhysical Geography13. Climate actionClimate RecordClimatologyPeriod (geology)Earth SciencesClimate modellcsh:QSeasonsEnvironmental SciencesResearch ArticleClimate ModelingPLOS One
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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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The Uniqueness of Planktonic Ecosystems in the Mediterranean Sea: The Response to Orbital- and Suborbital-Climatic Forcing over the Last 130,000 Years

2016

AbstractThe Mediterranean Sea is an ideal location to test the response of organisms to hydrological transformations driven by climate change. Here we review studies carried out on planktonic foraminifera and coccolithophores during the late Quaternary and attempt the comparison of data scattered in time and space. We highlight the prompt response of surface water ecosystems to both orbital- and suborbital-climatic variations.A markedly different spatial response was observed in calcareous plankton assemblages, possibly due to the influence of the North Atlantic climatic system in the western, central and northern areas and of the monsoon system in the easternmost and southern sites. Orbita…

010506 paleontologyQE1-996.5010504 meteorology & atmospheric sciencesGeologyForcing (mathematics)Environmental Science (miscellaneous)Plankton01 natural scienceslate quaternaryMediterranean seaOceanographyplanktonic foraminiferaClimatologyGeneral Earth and Planetary SciencesEcosystemUniquenessmediterranean seacoccolithophoresGeology0105 earth and related environmental sciencesOpen Geosciences
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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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Changing patterns of eastern Mediterranean shellfish exploitation in the Late Glacial and Early Holocene: Oxygen isotope evidence from gastropod in E…

2016

Abstract The seasonal pattern of shellfish foraging at the archaeological site of Haua Fteah in the Gebel Akhdar, Libya was investigated from the Epipaleolithic to the Neolithic via oxygen isotope (δ 18 O) analyses of the topshell Phorcus (Osilinus) turbinatus . To validate this species as faithful year-round palaeoenvironmental recorder, the intra-annual variability of δ 18 O in modern shells and sea water was analysed and compared with measured sea surface temperature (SST). The shells were found to be good candidates for seasonal shellfish forging studies as they preserve nearly the complete annual SST cycle in their shell δ 18 O with minimal slowing or stoppage of growth. During the ter…

010506 paleontologygeographyGBEpipaleolithicgeography.geographical_feature_category060102 archaeologybiologyPleistoceneArchaeological record06 humanities and the artsbiology.organism_classificationCC01 natural sciencesOceanographyRefugium (population biology)Cave13. Climate actionPhorcus0601 history and archaeology14. Life underwaterGlacial periodHoloceneGeology0105 earth and related environmental sciencesEarth-Surface Processes
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Reconstruction of late Holocene autumn/winter precipitation variability in SW Romania from a high-resolution speleothem trace element record

2018

We present the first high-resolution trace element (Mg/Ca, Sr/Ca, Ba/Ca) record from a stalagmite in southwestern Romania covering the last 3.6 ka, which provides the potential for quantitative climate reconstruction. Precise age control is based on three independent dating methods, in particular for the last 250 yr, where chemical lamina counting is combined with the identification of the 20th century radiocarbon bomb peak and Th-230/U dating. Long-term cave monitoring and model simulations of drip water and speleothem elemental variability indicate that precipitation-related processes are the main drivers of speleothem Mg/Ca ratios. Calibration against instrumental climate data shows a si…

010506 paleontologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesTrace elementSpeleothemStalagmiteForcing (mathematics)01 natural scienceslaw.inventionGeophysicsCaveSpace and Planetary ScienceGeochemistry and Petrologylawddc:550Earth and Planetary Sciences (miscellaneous)Institut für GeowissenschaftenRadiocarbon datingPhysical geographyPrecipitationHoloceneGeology0105 earth and related environmental sciencesEarth and Planetary Science Letters
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Modelling circulation in an ice-covered lake

2010

In deep ice-covered lakes with temperatures below 4 °C the heat flux from the bottom sediment results in a horizontal density gradient and a consequent flow along the bottom slope. Measurements in Lake Paajarvi, Finland, show a stable temperature field where a heat gain through the bottom and a heat loss through the ice nearly balance each other. The circulation is thermal with low velocities (less than 1.5 cm s -1 ). We used the 3D hydrodynamic Princeton Ocean Model as a tool to simulate the water circulation and the temperature distribution under the ice. The model forcing was based on field temperature measurements. The model simulations suggest that in midwinter the velocity field of th…

0106 biological sciences010504 meteorology & atmospheric sciences010604 marine biology & hydrobiologyFlow (psychology)lcsh:QE1-996.5SedimentForcing (mathematics)Atmospheric sciences01 natural sciencesPrinceton Ocean ModelCurrent (stream)lcsh:GeologyCirculation (fluid dynamics)Heat fluxhydrodynamic modelling13. Climate actionAnticycloneClimatologyGeneral Earth and Planetary Sciences14. Life underwaterLake Pääjärvi.Geologycurrents0105 earth and related environmental sciencesWater Science and TechnologyEstonian Journal of Earth Sciences
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Benthic hydroids (Cnidaria, Hydrozoa) from bathyal and abyssal depths of the Northeast Atlantic held in the moderniDiscovery/iiCollections/i.

2017

The deep-sea benthic hydroid fauna remains poorly known, in part because of less frequent sampling than the shelf fauna, in part owing to the immense study area, and partly also because available samples have been little studied by experts. In order to correct this, deep-sea benthic hydroid material from the modern Discovery Collections has been studied. Samples come from localities in the North-East Atlantic including the Porcupine Seabight, Porcupine Abyssal Plain, Rockall Trough, Rockall Bank, and the Mid-Atlantic Ridge. Sixteen species belonging to 12 families and 16 genera were found. Leptothecata are clearly dominant, being represented by 14 species; the remaining species belong to An…

0106 biological sciences010504 meteorology & atmospheric sciencesEcology010604 marine biology & hydrobiologyFaunaSpecies diversityBiologybiology.organism_classification01 natural sciencesBathyal zoneAbyssal zoneHydrozoaBenthic zoneHydroid (zoology)AnimalsAnimal Science and ZoologyPorcupine Abyssal PlainEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesHydrozoaZootaxa
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Ocean Circulation Model Applications for the Estuary-Coastal-Open Sea Continuum

2021

Coastal zones are among the most variable environments. As such, they require adaptive water management to ensure the balance of economic and social interests with environmental concerns. High quality marine data of hydrographic conditions e.g., sea level, temperature, salinity, and currents are needed to provide a sound foundation for the decision making process. Operational models with sufficiently high forecasting quality and resolution can be used for a further extension of the marine service toward the coastal-estuary areas. The Limfjord is a large and shallow water body in Northern Jutland, connecting the North Sea in the West and the Kattegat in the East. It is currently not covered …

0106 biological sciences010504 meteorology & atmospheric sciencesScienceStorm surgedown-stream servicesOcean EngineeringFjordForcing (mathematics)Aquatic ScienceQH1-199.5Oceanography01 natural sciencescoastal managementHBMBathymetry14. Life underwaterCMEMSSea level0105 earth and related environmental sciencesWater Science and TechnologyGlobal and Planetary Changegeographygeography.geographical_feature_category010604 marine biology & hydrobiologyQGeneral. Including nature conservation geographical distributionEstuaryseamless ocean modeling estuary-coastal-open sea interaction coastal management CMEMS HBM down-stream services Limfjordestuary-coastal-open sea interactionOceanographyseamless ocean modeling13. Climate actionEnvironmental scienceHydrographyThermoclineFrontiers in Marine Science
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Constraint and adaptation in the evolution of carnivoran skull shape

2011

The evolutionary history of the Order Carnivora is marked by episodes of iterative evolution. Although this pattern is widely reported in different carnivoran families, the mechanisms driving the evolution of carnivoran skull morphology remain largely unexplored. In this study we use coordinate-point extended eigenshape analysis (CP-EES) to summarize aspects of skull shape in large fissiped carnivores. Results of these comparisons enable the evaluation of the role of different factors constraining the evolution of carnivoran skull design. Empirical morphospaces derived from mandible anatomy show that all hypercarnivores (i.e., those species with a diet that consists almost entirely of verte…

0106 biological sciences010506 paleontologyEcologyPhylogenetic treeEcologyNicheMandiblePaleontologyVertebrateBiology010603 evolutionary biology01 natural sciencesBite force quotientSkullmedicine.anatomical_structureEvolutionary biologybiology.animalHypercarnivoremedicineAdaptationGeneral Agricultural and Biological SciencesEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesPaleobiology
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