0000000000434867

AUTHOR

Nauzet Hernández-hernández

0000-0003-1503-4214

showing 7 related works from this author

Effect of Intensity and Mode of Artificial Upwelling on Particle Flux and Carbon Export

2021

Reduction of anthropogenic CO2 emissions alone will not sufficiently restrict global warming and enable the 1.5°C goal of the Paris agreement to be met. To effectively counteract climate change, measures to actively remove carbon dioxide from the atmosphere are required. Artificial upwelling has been proposed as one such carbon dioxide removal technique. By fueling primary productivity in the surface ocean with nutrient-rich deep water, it could potentially enhance downward fluxes of particulate organic carbon (POC) and carbon sequestration. In this study we investigated the effect of different intensities of artificial upwelling combined with two upwelling modes (recurring additions vs. on…

0106 biological sciences010504 meteorology & atmospheric sciencesPHYTOPLANKTON COMMUNITYScienceartificial upwellingchemistry.chemical_elementOcean EngineeringQH1-199.5Carbon sequestrationAquatic ScienceAtmospheric sciencesOceanography01 natural sciencesremineralization ratechemistry.chemical_compoundWater columnORGANIC-CARBONVDP::Matematikk og Naturvitenskap: 400::Geofag: 450particle propertiesOrganic matter1172 Environmental sciences0105 earth and related environmental sciencesWater Science and TechnologyCO2 CONCENTRATIONSTotal organic carbonchemistry.chemical_classificationGlobal and Planetary Change010604 marine biology & hydrobiologyQTECHNICAL NOTEUPPER OCEANGeneral. Including nature conservation geographical distributionsinking velocityPlanktoncarbon sequestrationMARINE SNOWBACTERIAL-GROWTHINVERSE RELATIONSHIPexport fluxchemistry13. Climate actionCarbon dioxideEnvironmental scienceUpwellingmesocosm studyremineralization depthCarbonTRANSPARENT EXOPOLYMER PARTICLESFrontiers in Marine Science
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Upwelled plankton community modulates surface bloom succession and nutrient availability in a natural plankton assemblage

2022

Upwelling of nutrient-rich waters into the sunlit surface layer of the ocean supports high primary productivity in eastern boundary upwelling systems (EBUSs). However, subsurface waters contain not only macronutrients (N, P, Si) but also micronutrients, organic matter and seed microbial communities that may modify the response to macronutrient inputs via upwelling. These additional factors are often neglected when investigating upwelling impacts on surface ocean productivity. Here, we investigated how different components of upwelled water (macronutrients, organic nutrients and seed communities) drive the response of surface plankton communities to upwelling in the Peruvian coastal zone. Re…

Pacific Oceanfungimarine ecologyplanktonseaskumpuaminenravinteetmerivesinutrients (plants)nutrientsVDP::Matematikk og Naturvitenskap: 400::Geofag: 450mikrobitmicrobesmeriekologiameretEcology Evolution Behavior and SystematicsEarth-Surface ProcessesseawaterTyyni valtameri
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Factors controlling plankton productivity, particulate matter stoichiometry, and export fluxin the coastal upwelling system off Peru

2020

Abstract. Eastern boundary upwelling systems (EBUS) are among the most productive marine ecosystems on Earth. The high productivity in surface waters is facilitated by upwelling of nutrient-rich deep waters, with high light availability enabling fast phytoplankton growth and nutrient utilization. However, there are numerous biotic and abiotic factors modifying productivity and biogeochemical processes. Determining these factors is important because EBUS are considered hotspots of climate change, and reliable predictions on their future functioning requires understanding of the mechanisms driving biogeochemical cycles therein. In this study, we used in situ mesocosms to obtain mechanistic un…

Biogeochemical cycleOceanographyWater columnbiologyPhytoplanktonAkashiwo sanguineaEnvironmental scienceUpwellingDominance (ecology)Planktonbiology.organism_classificationMesocosm
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KOSMOS 2018 Gran Canaria mesocosm study: water column biogeochemistry

2021

The data set compiles biogeochemical water column collected during a KOSMOS mesocosm experiment carried out in the frame work of the Ocean Artificial Upwelling project. The experiment was performed in the North-East Atlantic Ocean off the coast of Gran Canaria in autumn 2018 and lasted for 39 days. In this study we investigated the effect of different intensities of artificial upwelling combined with two upwelling modes (recurring additions versus one singular addition) on POC export and its potential transfer efficiency to depth. The data set includes the amounts of surface water that were exchanged with nutrient-rich deep water (from ~300 m depth), primary production and chlorophyll a, el…

DEPTH water experimentNitrogenorganicChlorophyll aOcean Artificial Upwelling Ocean artUpwaterartificial upwellingOcean Artificial Upwelling (Ocean-artUp)remineralization rateDATE TIMEparticle propertiesCarbon organic particulateCarbon Nitrogen ratioMesocosm labelparticulatetotalPrimary production cumulativeexperimentDeep water exchange totalPrimary productionMesocosm experimentcumulativeEvent labelsinking velocitycarbon sequestrationCarbonCarbon/Nitrogen ratioexport fluxTreatmentDeep water exchangeDATE/TIMEKOSMOS_2018Prokaryotic heterotrophic productionDEPTHNitrogen organic particulateEarth System ResearchExperiment daymesocosm studyremineralization depth
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KOSMOS 2018 Gran Canaria mesocosm study: particle flux data from sediment trap

2021

The data set compiles sinking flux data collected during a KOSMOS mesocosm experiment carried out in the frame work of the Ocean Artificial Upwelling project. The experiment was performed in the North-East Atlantic Ocean off the coast of Gran Canaria in autumn 2018 and lasted for 39 days. In this study we investigated the effect of different intensities of artificial upwelling combined with two upwelling modes (recurring additions versus one singular addition) on POC export and its potential transfer efficiency to depth. The data set includes the amounts of surface water that were exchanged with nutrient-rich deep water (from ~300 m depth). It also contains particle flux data, i.e. POC flux…

DEPTH water experimentRemineralisation rate of carbon per dayNitrogenorganicOcean Artificial Upwelling Ocean artUpwaterartificial upwellingOcean Artificial Upwelling (Ocean-artUp)Particle porosityremineralization rateRemineralisation length scaleBiogenic silicaDATE TIMEparticle propertiesCarbon Nitrogen ratioCarbon Silicon ratioMesocosm labelparticulatetotalNitrogen organic particulate flux per dayflux per dayexperimentDeep water exchange totalCarbon organic particulate flux cumulativeMesocosm experimentcumulativeEvent labelsinking velocityCarbon/Silicon ratiocarbon sequestrationCarbonCarbon/Nitrogen ratiofluxexport fluxTreatmentNitrogen organic particulate flux cumulativeDeep water exchangeDATE/TIMEKOSMOS_2018DEPTHEarth System ResearchExperiment dayBiogenic silica flux per daymesocosm studyremineralization depthCarbon organic particulate flux per day
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KOSMOS 2017 Peru Side Experiment: nutrients, phytoplankton abundances, enzyme rates, photophysiology

2022

This data was collected during an short-term incubation experiment in March 2017 that investigated the response of a surface plankton community to upwelling. This experiment was carried in the framework of the SFB754-funded KOSMOS mesocosm study that took place in La Punta, Callao, Peru between February-April 2017. A total of six different treatments were used to disentangle chemical and biological characteristics of deep water that influence surface plankton blooms: 2 different deep water sources with different nutrient concentrations; 3 treatments to distinguish the effects of inorganic nutrients, organic nutrients and deep water microbial populations. Measured variables include inorganic…

ratioDay of experimentSFB754colored dissolved organic matter at 325 nmNitriteChlorophyll aAbsorption coefficient colored dissolved organic matter at 254 nmClimate - Biogeochemistry Interactions in the Tropical Ocean (SFB754)colorimetric determinationFluorometerFluorometricNitrateNanoplanktonPhytoplankton cells phycocyanin-containing (FL-4)PicoeukaryotesFluorometer fast repetition rateCalculatedFlow cytometryNutrient consumption ratioforward scatterSynechococcusupwelling systemsMesocosm experimentSpectrophotometricClimate Biogeochemistry Interactions in the Tropical Ocean SFB754SilicateBiogeochemistryBiospheric SciencesMaximum photochemical quantum yield of photosystem IIenzyme activitycell sizeDissolved inorganic nitrogen/dissolved inorganic phosphorus ratioKOSMOS_2017chainsAbsorption coefficient colored dissolved organic matter 250 nm/365 nm ratioeastern tropical South Pacific OceanKOSMOSExcess phosphateAbsorption coefficient colored dissolved organic matter at 325 nmNatural SciencesGeosciencescolored dissolved organic matter at 254 nmphycocyanin containing FL 4Absorption coefficientPhosphateTank numberPhytoplankton cells chainsNetwork of Leading European AQUAtic MesoCOSM Facilities Connecting Mountains to Oceans from the ArctReplicatenutrientsfast repetition rateDATE TIMECryptophytesMicrophytoplanktonPhytoplankton cellsLeucine aminopeptidase activityDissolved inorganic nitrogen dissolved inorganic phosphorus ratiofungiEnzymatic assayContinuous flow analyserTreatmentDATE/TIMEcolored dissolved organic matter 250 nm 365 nmPhytoplanktonPhytoplankton cell size forward scatterNetwork of Leading European AQUAtic MesoCOSM Facilities Connecting Mountains to Oceans from the Arctic to the Mediterranean (AQUACOSM)CDOMContinuous flow analyser colorimetric determinationNitrate and Nitrite
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KOSMOS 2017 Peru mesocosm study: overview data

2020

Eastern boundary upwelling systems (EBUS) are among the most productive marine ecosystems on Earth. The production of organic material is fueled by upwelling of nutrient-rich deep waters and high incident light at the sea surface. However, biotic and abiotic factors can mod- ify surface production and related biogeochemical processes. Determining these factors is important because EBUS are considered hotspots of climate change, and reliable predic- tions of their future functioning requires understanding of the mechanisms driving the biogeochemical cycles therein. In this field experiment, we used in situ mesocosms as tools to improve our mechanistic understanding of processes con- trolling…

KOSMOS_2017Binary ObjectMesocosm experimentClimate - Biogeochemistry Interactions in the Tropical Ocean (SFB754)Climate Biogeochemistry Interactions in the Tropical Ocean SFB754BiogeochemistryBinary Object Media TypeNatural SciencesBinary Object (File Size)Binary Object File SizeBiospheric SciencesGeosciencesBinary Object (Media Type)
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