Search results for "Earth system"

showing 10 items of 109 documents

(Table 1) Stable oxygen and carbon isotopic ratios of tree rings, and tree ring width of white spruce (Picea glauca), Ennadai Lake

2012

Stable isotope ratios from tree rings and peatland mosses have become important proxies of past climate variations. We here compare recent stable carbon and oxygen isotope ratios in cellulose of tree rings from white spruce (Picea glauca), growing near the arctic tree line; and cellulose of Sphagnum fuscum stems, growing in a hummock of a subarctic peatland, in west-central Canada. Results show that carbon isotopes in S. fuscum correlate significantly with July temperatures over the past ~20 yr. The oxygen isotopes correlate with both summer temperature and precipitation. Analyses of the tree-ring isotopes revealed summer temperatures to be the main controlling factor for carbon isotope var…

Picea glauca standard deviationPicea glauca δ18O tree ringsPicea glauca tree ring widthInternational Polar Year (2007-2008) (IPY)tree ring widthtree ringsSample IDTree ring samplingPicea glauca δ13C tree ringsInternational Polar Year 2007 2008 IPYδ13CEarth System Researchstandard deviationPicea glaucaδ18O
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Calcifying zooplankton standing stocks and in the North Pacific from the R/V Kilo Moana cruise KM1712

2022

This dataset compiles the standing stocks (ind/m³), the integrated standing stocks (ind/m²) and the integrated CaCO3 standing stocks (mg/m²) for three groups of zooplanktonic calcifying organisms: pteropods, heteropods and foraminifers. The organisms were collected by oblique towing (Ø 0.5 m, 90 μm mesh size, SeaGear mechanical flowmeter) in the North Pacific between Hawaii and the Gulf of Alaska during the R/V Kilo Moana cruise KM1712 in August 2017. The sampling strategy was designed to capture an integrated sample of all foraminifers, pteropods and heteropods from juveniles to adults living throughout the upper water column. Pteropods and heteropods were quantified and shell diameter mea…

Pteropoda standard deviationDate Time of event 2RV Kilo MoanaForaminiferaLight microscopeLatitude of eventDate/Time of event 2Foraminifera calcium carbonate per areaPlankton netKM1712CalculatedpteropodsNorth PacificForaminifera standard deviationLeicaWater volumeStanding stocksEarth System Researchstandard deviationMechanical flowmeter SeaGearMechanical flowmeterSeaGearStation labelPteropoda calcium carbonate per areaZ16 AP0Carbonate productionLongitude of eventPterotracheoidea calcium carbonate per areawaterPterotracheoideaDate Time localfilteredDate/Time of eventCoccolithophoresPteropodaPteropoda calcium carbonate per area standard deviationPterotracheoidea standard deviationDEPTH waterLongitude of event 2Date/Time localEvent labelDate Time of eventWater volume filteredPterotracheoidea calcium carbonate per area standard deviationcalcium carbonate per areaLatitude of event 2Foraminifera calcium carbonate per area standard deviationDEPTHLight microscope Leica Z16 AP0Heteropods
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Dataset of a globally relevant stock of soil nitrogen in the Yedoma permafrost domain

2022

This dataset merges nitrogen data from the Yedoma domain. It includes numerous fieldwork campaigns, which take place since 1998. In total 467 samples from the active layer (seasonally thawed layer), 175 samples from perennially frozen Holocene cover deposits, 479 samples from thermokarst deposits in drained thermokarst, 175 in-situ thawed, diagenetically (anaerobic microbial decomposition possible during unfrozen phase) altered Yedoma deposits (called Taberite), and 917 samples from frozen Yedoma deposits are included. Moreover it includes a NH4+ and NO3- quantification basing on of 658 samples, including 378 data points for NH4+ (active layer, 93; Holocene cover, 108; thermokarst sediment,…

Reference sourceNitrogenpermafrost thawLocationStratigraphyorganicDensityDEPTH sediment/rockPermafrost Research AWI_PermaArcticDensity bulk permafrostPermafrost Research (AWI_Perma)Sample numbernitrogen cycletop minCarbon Nitrogen ratiobulkELEVATIONLONGITUDEtotalorganic matterbottom maxDepthDepth top/minWater (ice) segregatedCarbonCarbon/Nitrogen ratiosediment rocksegregatedSample IDWater iceNitrogen totalclimate feedbackLATITUDEEarth System ResearchDepth bottom/maxPersistent IdentifierCarbon organic totalReference/sourcepermafrost
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(Table 1) Sea surface temperature reconstruction for eastern equatorial Pacific surface sediment samples

2012

Significant uncertainties persist in the reconstruction of past sea surface temperatures in the eastern equatorial Pacific, especially regarding the amplitude of the glacial cooling and the details of the post-glacial warming. Here we present the first regional calibration of alkenone unsaturation in surface sediments versus mean annual sea surface temperatures (maSST). Based on 81 new and 48 previously published data points, it is shown that open ocean samples conform to established global regressions of Uk'37 versus maSST and that there is no systematic bias from seasonality in the production or export of alkenones, or from surface ocean nutrient concentrations or salinity. The flattening…

Reference sourceRC23RR9702ASea surface temperatureannual meaninterpolatedV21Roger A RevellePiston corer (BGR type)ME0005Aunsaturation index UK 37VemaKNR182 91988RC18Marion Dufresne (1995)Hakuho MaruKH-03-1MultiCorerTemperaturePiston corer BGR typeAMPHITRITEsediment rockRoger A. RevelleKH 03 1Earth System ResearchLeg138Robert ConradCoreWecomaCalculated from UK 37 Prahl et alPiston corerMoana WaveLongitude of eventHakuho-MaruAlkenone unsaturation index UK'37Thomas WashingtonW7706differenceKNR176-2KNR195-5Leg201DEPTH sediment/rockVNTR01SO147PLDS 3Sea surface temperature annual meanPLDS-3Giant piston corerMW8708MelvilleMD126Marion Dufresne 1995KnorrRC11RC13Event labelJoides ResolutionYALOC69Calculated from UK'37 (Prahl et al. 1988)V19ArgoSonneKNR176 2KNR195 5DEPTHYaquinaKNR182-9Gravity corerTemperature differenceBox corerAlkenoneComposite CoreSCANReference/source
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Eclogites and garnet pyroxenites: Similarities and differences

2010

Eclogites and garnet pyroxenites are genetically linked to basaltic precursors. Traditionally garnet pyroxenites are linked to fractionation of basaltic Magmas Over a range of mantle pressures and more recently they have been implicated in the genesis of ocean islands. in contrast eclogites are linked to the subduction of slab basalt and gabbro precursors which may be hydrothermally altered. Recently this subduction paradigm has been questioned. We present mineralogical, trace element and O isotopic data for eclogites and garnet pyroxenites that reveal some similarities but also important chemical and isotopic differences that support a distinct provenance (i.e., age and process). Continent…

SALT-LAKE-CRATERSM-NDGeochemistryResearch Groups and Centres\Earth Sciences\Ancient and Modern Earth SystemsXENOLITHIC ECLOGITESMantle (geology)ONTONG JAVA PLATEAUxenolithsResearch Groups and Centres\Earth Sciences\GeochemistryGeochemistry and PetrologyTRACE-ELEMENTSFaculty of Science\Earth SciencesXenolithHIGH-PRECISIONgarnet pyroxenitesLU-HFWEST-AFRICAPeridotiteBasaltgeographygeography.geographical_feature_categorySOLOMON-ISLANDSGabbrooxygen isotopesmantle eclogitesmineral chemistryCratonIgneous rockGeophysicsEclogiteGeologyKAAPVAAL CRATONJournal of Volcanology and Geothermal Research
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Oxygen isotope and salinity measurements of coastal surface waters in the Gulf of Maine

2020

These data include salinity and oxygen isotope measurements of water samples collected from coastal sites along the Gulf of Maine between 2003 and 2015. In particular, a suite of samples were collected along the coast of Maine, east of Penobscot Bay, on a monthly basis between April 2014 and March 2015. These data also include several freshwater samples collected from the Kennebec and Penobscot Rivers on a semi-monthly basis in 2014 and 2015. For the water samples with sample IDs starting with DSW, JSW, NSW, or OSW: The water samples were collected by hand from shore or boat using French square glass bottles with phenolic polycone lined caps. Salinity was measured using a Oakton SALT 6+ han…

SalinityGulf of MainewaterCommentWater sampleδ18O waterReference of dataDATE/TIMESample IDOxygen isotopesDATE TIMEEarth System ResearchLATITUDEYear of observationδ18OLONGITUDE
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Toward a Collective Agenda on AI for Earth Science Data Analysis

2021

In the last years we have witnessed the fields of geosciences and remote sensing and artificial intelligence to become closer. Thanks to both the massive availability of observational data, improved simulations, and algorithmic advances, these disciplines have found common objectives and challenges to advance the modeling and understanding of the Earth system. Despite such great opportunities, we also observed a worrying tendency to remain in disciplinary comfort zones applying recent advances from artificial intelligence on well resolved remote sensing problems. Here we take a position on research directions where we think the interface between these fields will have the most impact and be…

Signal Processing (eess.SP)FOS: Computer and information sciences010504 meteorology & atmospheric sciencesGeneral Computer Science530 PhysicsInterface (Java)Computer Vision and Pattern Recognition (cs.CV)Earth sciencedata analysisComputer Science - Computer Vision and Pattern Recognition0211 other engineering and technologiesearth observation02 engineering and technology01 natural sciencesEnvironmental scienceData modelingFOS: Electrical engineering electronic engineering information engineeringClimate science1700 General Computer ScienceElectrical Engineering and Systems Science - Signal ProcessingElectrical and Electronic EngineeringInstrumentation021101 geological & geomatics engineering0105 earth and related environmental sciences11476 Digital Society Initiative3105 Instrumentation2208 Electrical and Electronic Engineering1900 General Earth and Planetary SciencesDeep learninginterpretable AIRemote sensingartificial intelligencehybrid modelsEarth system scienceAIRemote sensing (archaeology)10231 Institute for Computational ScienceGeneral Earth and Planetary SciencesPotential gameDisciplineIEEE Geoscience and Remote Sensing Magazine
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Mapping the global distribution of the freshwater hydrozoan Craspedacusta sowerbii

2021

The invasive freshwater jellyfish Craspedacusta sowerbii (Limnomedusae, Olindiidae) is native to East Asia and since the end of the 19th century, was observed in Europe, then in North America, and across the globe. In recent decades, reports of C. sowerbii have drastically increased in Europe, North and South America, Australia, Asia, and parts of Africa. However, the worldwide distribution of C. sowerbii remains poorly documented due to the lack of information in various aquatic environments. This dataset globalises the occurrences of this species from an extensive literature review and database review. Information extracted from the literature/database were organised and synthesised accor…

SpeciesIdentificationReference sourceLocationSiteCountryHabitatContinentUniform resource locator/link to referenceLATITUDEEarth System ResearchYear of observationELEVATIONLONGITUDEUniform resource locator link to referenceReference/sourceglobal compilation
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Effects of ocean acidification on embryonic respiration and development of a temperate wrasse living along a natural CO2 gradient

2016

Volcanic CO2 seeps provide opportunities to investigate the effects of ocean acidification on organisms in the wild. To understand the influence of increasing CO2 concentrations on the metabolic rate (oxygen consumption) and the development of ocellated wrasse early life stages, we ran two field experiments, collecting embryos from nesting sites with different partial pressures of CO2 [pCO2; ambient (400 µatm) and high (800-1000 µatm)] and reciprocally transplanting embryos from ambient- to high-CO2 sites for 30 h. Ocellated wrasse offspring brooded in different CO2 conditions had similar responses, but after transplanting portions of nests to the high-CO2 site, embryos from parents that sp…

StageOcean Acidification International Coordination Centre (OA-ICC)TemperateRegistration number of speciesSalinityinorganicYolk area standard errorAlkalinityExperimentTemperature waterCarbon inorganic dissolvedCalculated using seacarb after Nisumaa et al 2010Aragonite saturation stateRespiration rate oxygenChordataAlkalinity totaltotalCO2 ventpHPelagosReproductionRespirationSymphodus ocellatusTemperatureYolk areadissolvedCarbonate ionPartial pressure of carbon dioxide (water) at sea surface temperature (wet air)Field experimentTemperature water standard deviationTime pointstandard errorRespiration rateEarth System Researchstandard deviationFOS: Medical biotechnologyUniform resource locator link to referenceTime point descriptiveHatchling lengthCalcite saturation statewaterPartial pressure of carbon dioxidedescriptiveGrowth MorphologyFigureUniform resource locator/link to referenceSalinity standard deviationOcean Acidification International Coordination Centre OA ICCMediterranean SeaAnimaliaEggs areaTypeBicarbonate ionNektonEggs area standard errorCalculated using seacarb after Nisumaa et al. (2010)SpeciesPartial pressure of carbon dioxide standard deviationCarbonate system computation flagpH standard deviationHatchling length standard errorFugacity of carbon dioxide (water) at sea surface temperature (wet air)CarbonTreatmentOxygenPartial pressure of carbon dioxide water at sea surface temperature wet airCarbon dioxideGrowth/MorphologySingle speciesOxygen standard deviationFugacity of carbon dioxide water at sea surface temperature wet airCoast and continental shelf
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The Role of Fire in Achieving the Sustainable Development Goals of the United Nations

2019

The Sustainable Development Goals (SDGs) of the United Nations do not mention Fire as a key factor in achieving an environmentally-friendly human society. This paper reviews the key aspects of the impact of fire that make it necessary to update the SDGs. Upon reviewing the scientific literature, it was found that fire has been part of the Earth System for the last 400 million years, and that it is part of biogeochemical cycles. From a geological perspective, fire shaped the current Earth System. Humans have used fire in the last million years as hunter-gatherers, and the last Pleistocene period evolved with the presence of fire. Since the Neolithic revolution, humankind spread the use of fi…

Sustainable developmentBiogeochemical cyclegeographygeography.geographical_feature_categorybusiness.industryEphemeral keynaturelcsh:AsustainabilityShrublandEarth system sciencesocietyDisturbance (ecology)AgricultureEnvironmental protectionSustainabilityforest firesEnvironmental sciencelcsh:General WorkshumansbusinessTERRAenVISION 2019
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