Search results for "Earth System Research"

showing 10 items of 73 documents

Raster maps for 29 environmental variables in three geographical regions

2015

Aim: Greater understanding of the processes underlying biological invasions is required to determine and predict invasion risk. Two subspecies of olive (Olea europaea subsp. europaea and Olea europaea subsp. cuspidata) have been introduced into Australia from the Mediterranean Basin and southern Africa during the 19th century. Our aim was to determine to what extent the native environmental niches of these two olive subspecies explain the current spatial segregation of the subspecies in their non-native range. We also assessed whether niche shifts had occurred in the non-native range, and examined whether invasion was associated with increased or decreased occupancy of niche space in the no…

File nameFile sizeUniform resource locator link to fileUniform resource locator/link to fileEarth System Research
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Growth rates of F0 and F1 larval and juvenile European seabass Dicentrarchus labrax in resonse to ocean acidification and warming

2022

Ongoing climate change is leading to warmer and more acidic oceans. The future distribution of fish within the oceans depends on their capacity to adapt to these new environments. Only few studies have examined the effects of ocean acidification (OA) and warming (OW) on the metabolism of long-lived fish over successive generations. We therefore aimed to investigate the effect of OA on larval and juvenile growth and metabolism on two successive generations of European sea bass (Dicentrarchus labrax L.) as well as the effect of OAW on larval and juvenile growth and metabolism of the second generation. European sea bass is a large economically important fish species with a long generation time…

GenerationTank numberLife stagedry massType of studyocean warmingjuvenile growthAgeUniform resource locator/link to referenceWeightedDATE TIMEDicentrarchus labraxTreatment temperatureSpeciesbody lengthlarval growthteleostCaliperOcean acidificationTreatment partial pressure of carbon dioxideLaboratory experimentTreatment: temperatureDATE/TIMESample IDTreatment: partial pressure of carbon dioxideDicentrarchus labrax body lengthEarth System Researchmassmetabolic ratesUniform resource locator link to referenceDicentrarchus labrax dry massDicentrarchus labrax mass
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Global Coastal Permeability database (GCPdb)

2023

The Global Coastal Permeability Database contains both the input and output data of the Global Coastal Permeability Model developed by Tschaikowski et al. (2023) and available at DOI: 10.5281/zenodo.7845568. The model is implemented in R and calculates the coastal permeability for each shoreline segment of the global shoreline vector created by Sayre et al. (2019) with a 30-meter resolution and covering a spatial extent of 180.0°W to 180.0°E longitude and 60.8°S to 83.7°N latitude. The coastline is separated into three sections (A: coastal aquifer section, B: shoreline section, C: shallow section), and permeability values and ranges are provided for each section. Permeability values were de…

Global coastal groundwater dynamics in a changing climate COASTGUARDBinary Objectsubmarine groundwater dischargeCoastal hydrogeologyBinary Object Media TypeBinary Object (File Size)Binary Object (Media Type)Coastal permeabilityGlobal hydrogeologysaltwater intrusionEarth System ResearchcoastlineGlobal coastal groundwater dynamics in a changing climate (COASTGUARD)permeabilityBinary Object File Size
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Global distributions of diazotrophs abundance and biomass - Depth integrated values computed from a collection of source datasets - Contribution to t…

2013

The MAREDAT atlas covers 11 types of plankton, ranging in size from bacteria to jellyfish. Together, these plankton groups determine the health and productivity of the global ocean and play a vital role in the global carbon cycle. Working within a uniform and consistent spatial and depth grid (map) of the global ocean, the researchers compiled thousands and tens of thousands of data points to identify regions of plankton abundance and scarcity as well as areas of data abundance and scarcity. At many of the grid points, the MAREDAT team accomplished the difficult conversion from abundance (numbers of organisms) to biomass (carbon mass of organisms). The MAREDAT atlas provides an unprecedente…

Go-Flo bottlesSalinityCAIBEX-IRV Kilo MoanaDiazotrophs total biomass as carbonUniform resource locator link to source data fileNitrateRichelia carbon per cellCTD/RosetteLatitude of eventNiskinRoger A RevelleTemperature waterCalculatedtop minbiomass as carbonTrichodesmium biomass as carbontotalbottom maxCTD Seabirdareal concentrationMultiple investigationsTemperatureDepth top/minRichelia abundance cellsCTD RosetteSeabirdCalothrixRoger A. RevelleTrichodesmiumTrichodesmium carbon per trichomeEarth System ResearchRichelia abundanceCAIBEX-IICalothrix abundanceMARine Ecosystem Model Intercomparison Project MAREMIPDiazotrophsLongitude of eventRichelia associated speciesSample methodIronChlorophyll total areal concentrationBottle NiskinwaterTrichodesmium abundance free trichomesMARine Ecosystem Model Intercomparison Project (MAREMIP)PhosphateSarmiento de GamboaSample commentCAIBOXUniform resource locator/link to source data filetotal biomass as carbonCalothrix carbon per cellHeterocyst biomassGo Flo bottlescoloniesDate/Time of eventChlorophyll totalTrichodesmium abundance totalRicheliaDEPTH waterTrichodesmium abundance coloniesMP-6biomassBottleDepthEvent labelDate Time of eventCAIBEX IIcarbon per cellMeasured at sea surfacefree trichomesMP-9CTDCalothrix abundance cellscarbon per trichomeTrichodesmium abundanceCalothrix associated speciesMP 9MP 6CAIBEX IcellsDepth bottom/maxassociated speciesHeterocyst
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Global distributions of diazotrophs nitrogen fixation rates - Depth integrated values computed from a collection of source datasets - Contribution to…

2013

The MAREDAT atlas covers 11 types of plankton, ranging in size from bacteria to jellyfish. Together, these plankton groups determine the health and productivity of the global ocean and play a vital role in the global carbon cycle. Working within a uniform and consistent spatial and depth grid (map) of the global ocean, the researchers compiled thousands and tens of thousands of data points to identify regions of plankton abundance and scarcity as well as areas of data abundance and scarcity. At many of the grid points, the MAREDAT team accomplished the difficult conversion from abundance (numbers of organisms) to biomass (carbon mass of organisms). The MAREDAT atlas provides an unprecedente…

Go-Flo bottlesSalinityCAIBEX-ITrichodesmium nitrogen fixation rateRV Kilo MoanaUniform resource locator link to source data fileNitrateCTD/RosetteLatitude of eventNiskinAlisRoger A RevelleTemperature waterwhole seawatertop minCalculatedbottom maxareal concentrationNitrogen fixation rateTemperatureDepth top/minCTD RosetteUnicellular cyanobacteria nitrogen fixation rateTrichodesmiumRoger A. RevelleNitrogen fixation rate integrated per dayEarth System ResearchMooring (long time)CAIBEX-IIMARine Ecosystem Model Intercomparison Project MAREMIPDiapalis 3Longitude of eventDiapalis 4Diapalis 5Sample methodIronwaterChlorophyll total areal concentrationBottle NiskinWater pumpMARine Ecosystem Model Intercomparison Project (MAREMIP)PhosphateWater sampleSarmiento de GamboaSample commentCAIBOXDiapalis 6Diapalis 7Uniform resource locator/link to source data fileDiapalis 9Go Flo bottlesNitrogen fixation rate whole seawaterintegrated per dayUnicellular cyanobacteriaDate/Time of eventChlorophyll totalMooring long timeDiapalis-7Diapalis-9Diapalis-3Diapalis-4Diapalis-5Diapalis-6DEPTH waterMP-6BottleDepthEvent labelDate Time of eventCAIBEX IIMeasured at sea surfaceMP-9MP 9MP 6CAIBEX IDepth bottom/maxHeterocyst nitrogen fixation rateHeterocyst
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Growth rates of late Miocene corals from Crete (Greece)

2006

Modern scleractinian corals are classical components of marine shallow warm water ecosystems. Their occurrence and diversity patterns in the geological record have been widely used to infer past climates and environmental conditions. Coral skeletal composition data reflecting the nature of the coral environment are often affected by diagenetic alteration. Ghost structures of annual growth rhythms are, however, often well preserved in the transformed skeleton. We show that these relicts represent a valuable source of information on growth conditions of fossil corals. Annual growth bands were measured in massive hemispherical Porites of late Miocene age from the island of Crete (Greece) that …

Growth rateEarth System ResearchLATITUDESample code labelSample commentLONGITUDEGeographic name/localityGeographic name localitySample code/label
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Molecular hydrogen (H2) mixing ratio and stable isotopic composition (dD) at the Cabauw tall tower in the Netherlands (2008-2012)

2016

Measurements of the stable isotopic composition (dD(H2) or dD) of atmospheric molecular hydrogen (H2) are a useful addition to mixing ratio (X(H2)) measurements for understanding the atmospheric H2 cycle. dD datasets published so far consist mostly of observations at background locations. We complement these with observations from the Cabauw tall tower at the CESAR site, situated in a densely populated region of the Netherlands. Our measurements show a large anthropogenic influence on the local H2 cycle, with frequently occurring pollution events that are characterized by X(H2) values that reach up to 1 ppm and low dD values. An isotopic source signature analysis yields an apparent source s…

HEIGHT above groundDATE/TIMEIdentificationδ DeuteriumMonitoring stationDATE TIMEEarth System Researchδ Deuterium standard deviationSample commentHydrogen mixing ratio standard deviationstandard deviationHydrogen mixing ratioQuality code
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(Supplement Table S2) Results of 230Th/U-dating

2016

We compared the suitability of two skeletal materials of the Atlantic brain coral Diploria strigosa for 230Th/U-dating: the commonly used bulk material comprising all skeletal elements and the denser theca wall material. Eight fossil corals of presumably Last Interglacial age from Bonaire, southern Caribbean Sea, were investigated, and several sub-samples were dated from each coral. For four corals, both the ages and the activity ratios of the bulk material and theca wall agree within uncertainty. Three corals show significantly older ages for their bulk material than for their theca wall material as well as substantially elevated 232Th content and (230Th/238U) ratios. The bulk material sam…

Hand drillUranium 238Thorium 230 Uranium 238 activity ratioThorium-230/Uranium-238 activity ratioUranium-238Thorium-230/Uranium-238 activity ratio standard deviationAGECenter for Marine Environmental Sciences MARUMMulti collector inductively coupled plasma mass spectrometer MC ICP MSCenter for Marine Environmental Sciences (MARUM)Thorium 232Thorium 232 Uranium 238 activity ratioThorium-232/Uranium-238 activity ratio standard deviationEvent labelCommentUranium 234 Uranium 238 activity ratioUranium-234/Uranium-238 activity ratioDrilling/drill rigAge 230Th/U Thorium-UraniumAge standard deviationDrilling drill rigThorium-232/Uranium-238 activity ratioUranium-234/Uranium-238 activity ratio standard deviationThorium-232230Th U Thorium UraniumEarth System ResearchGroupMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)standard deviation
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Oxygen consumption of F0 and F1 larval and juvenile European seabass Dicentrarchus labrax in resonse to ocean acidification and warming

2022

Ongoing climate change is leading to warmer and more acidic oceans. The future distribution of fish within the oceans depends on their capacity to adapt to these new environments. Only few studies have examined the effects of ocean acidification (OA) and warming (OW) on the metabolism of long-lived fish over successive generations. We therefore aimed to investigate the effect of OA on larval and juvenile growth and metabolism on two successive generations of European sea bass (Dicentrarchus labrax L.) as well as the effect of OAW on larval and juvenile growth and metabolism of the second generation. European sea bass is a large economically important fish species with a long generation time…

IdentificationDicentrarchus labrax routine metabolic rate per dry massLife stagedry massType of studyDicentrarchus labrax fork lengthGermanyWeightedCalculatedTreatment temperaturebody lengthlarval growthteleostOcean acidificationdissolvedTreatment partial pressure of carbon dioxideOptical oxygen meter with sensor OXR50 FireStingLaboratory experimentstandard metabolic rate per fresh massTreatment: temperatureDicentrarchus labrax standard metabolic rate per fresh massEarth System Researchmetabolic ratesUniform resource locator link to referenceDicentrarchus labrax dry massStereomicroscopy Leicafork lengthStereomicroscopy (Leica)GenerationOxygen dissolvedTank numberocean warmingjuvenile growthPyroScience GmbHAgeUniform resource locator/link to referenceDATE TIMEDicentrarchus labraxroutine metabolic rate per dry masswet weightedFulton's condition factorSpeciesFish wet weightedCaliperOptical oxygen meter with sensor OXROB10 (FireSting PyroScience GmbH Germany)Optical oxygen meter with sensor OXROB10 FireStingOptical oxygen meter with sensor OXR50 (FireSting PyroScience GmbH Germany)Fulton s condition factorOxygenDATE/TIMEFishSample IDTreatment: partial pressure of carbon dioxideDicentrarchus labrax body lengthmassDicentrarchus labrax mass
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(Table 1) Geochemistry of ODP Site 160-963 sediments

2010

The Mediterranean Sea acts as a miniature ocean with the development of its own conveyor belt. It constitutes an ideal location to study and forecast how the marine environment responds to rapid climatic change. Here we present a palaeoenvironmental study carried out on the sediments of ODP Site 963, recovered in the Sicily Channel, the sill which divides the western from the eastern Mediterranean basin. We focused on the transition between the penultimate glacial (MIS 6) and the last interglacial (MIS 5), between approximately 130 and 115 kyr BP. A novel approach is proposed, taking into account centennial-scale geochemical data on major elements, selected trace elements, and yttrium and R…

Leg160Inductively coupled plasma - mass spectrometry (ICP-MS)GadoliniumLutetiumOcean Drilling Program (ODP)HolmiumAGEEuropiumLanthanumManganese oxideIron oxide Fe2O3Iron oxideSilicon dioxideDysprosiumCalculatedYttriumInductively coupled plasma mass spectrometry ICP MSAluminium oxideYtterbiumTerbiumInductively coupled plasma optical emission spectrometryRatioMagnesium oxideNeodymiumYttrium Holmium ratioSamariumJoides ResolutionCalcium oxideCeriumICP OESCerium anomalyBariumYttrium/Holmium ratioThuliumEarth System ResearchOcean Drilling Program ODPTitanium dioxideFe2O3PraseodymiumICP-OES Inductively coupled plasma - optical emission spectrometryComposite CoreErbium
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