GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 14C incorporation; 14C-POC; artificial upwelling; Calculated; Canarias Sea; carbon sequestration; Day of experiment; Depth, water, experiment, bottom/maximum; Depth, water, experiment, top/minimum; Event label; Field experiment; Food web; KOSMOS_2018; KOSMOS_2018_Mesocosm-A; KOSMOS_2018_Mesocosm-M1; KOSMOS_2018_Mesocosm-M2; KOSMOS_2018_Mesocosm-M3; KOSMOS_2018_Mesocosm-M4; KOSMOS_2018_Mesocosm-M5; KOSMOS_2018_Mesocosm-M6; KOSMOS_2018_Mesocosm-M7; KOSMOS_2018_Mesocosm-M8; KOSMOS_2018_Mesocosm-M9; KOSMOS Gran Canaria; MESO; mesocosm experiment; Mesocosm experiment; Mesocosm label; Ocean Artificial Upwelling; Ocean-artUp; Phytoplankton; primary production; Primary production of carbon, organic, dissolved; Primary production of carbon, organic, dissolved, standard deviation; Primary production of carbon, organic, particulate; Primary production of carbon, organic, total; Sampling date/time, experiment; Treatment; Type of study  (1)
  • Absorption coefficient, colored dissolved organic matter at 254 nm; Antarctic Intermediate Water of 3.1°C, relative volume contribution; Antarctic Intermediate Water of 5°C, relative volume contribution; Atlantic; Atlantic Ocean; bathypelagic; Biogeochemical impact of mesoscale and sub-mesoscale processes along the life history of cyclonic and anticyclonic eddies: plankton variability and productivity; Calculated; Calculated after Broecker (1974); Campaign; Chlorophyll a, integrated; Circumpolar Deep Water, relative volume contribution; Constraining organic carbon fluxes in an eastern boundary upwelling ecosystem (NW Africa): the role of non-sinking carbon in the context of the biological pump; Continuous Segmented Flow Analyzer, SEAL Analytical, QuAAtro39; CTD, Sea-Bird, SBE 911plus; CTD/Rosette; CTD-RO; dark ocean; Date/Time of event; DEPTH, water; Eastern North Atlantic Central Water of 12°C, relative volume contribution; Eastern North Atlantic Central Water of 15°C, relative volume contribution; e-IMPACT; Equatorial Water, relative volume contribution; Event label; Fluorescence intensity, maximum, DOM; fluorescent dissolved organic matter; FLUXES; Hespérides; Latitude of event; Longitude of event; Madeira Mode Water, relative volume contribution; MAFIA; MAFIA_01_D-1; MAFIA_02_L-1; MAFIA_03_L-1; MAFIA_04_L-1; MAFIA_05_L-1; MAFIA_06_L-1; MAFIA_07_L-1; MAFIA_08_L-1; MAFIA_09_L-1; MAFIA_10_D-1; MAFIA_11_L-1; MAFIA_12_L-1; MAFIA_13-1; Mediterranean Water, relative volume contribution; mesopelagic; Migrants and Active Flux In the Atlantic Ocean; Nitrate + Oxygen tracer; North Atlantic Deep Water of 2°C, relative volume contribution; North Atlantic Deep Water of 4.6°C, relative volume contribution; optimum multiparameter analysis; Optimum multiparameter analysis; Oxygen; Oxygen, apparent utilization; Oxygen, Benson & Krause 1984; Parallel factor analysis (PARAFAC); Pressure, water; Salinity; Salinity Maximum Water, relative volume contribution; Sample ID; Silicate; Spectrophotometer, Ocean Optics USB2000; Station label; Subpolar Mode Water, relative volume contribution; subtropical - tropical Atlantic; SUMMER; Sustainable Management of Mesopelagic Resources; Temperature, water, potential; Titration, Winkler; water masses  (1)
Document type
Keywords
Publisher
Years
  • 1
    Publication Date: 2023-08-15
    Description: Size fractionated primary productivity rate measurements through 14C radioisotope incorporation rates from 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 the phytoplankton community. Data shown includes production rates of dissolved organic carbon, particulate organic carbon in 3 size fractions (0.2-2 µm, 2-20 µm, 〉20 µm) and total organic carbon.
    Keywords: 14C incorporation; 14C-POC; artificial upwelling; Calculated; Canarias Sea; carbon sequestration; Day of experiment; Depth, water, experiment, bottom/maximum; Depth, water, experiment, top/minimum; Event label; Field experiment; Food web; KOSMOS_2018; KOSMOS_2018_Mesocosm-A; KOSMOS_2018_Mesocosm-M1; KOSMOS_2018_Mesocosm-M2; KOSMOS_2018_Mesocosm-M3; KOSMOS_2018_Mesocosm-M4; KOSMOS_2018_Mesocosm-M5; KOSMOS_2018_Mesocosm-M6; KOSMOS_2018_Mesocosm-M7; KOSMOS_2018_Mesocosm-M8; KOSMOS_2018_Mesocosm-M9; KOSMOS Gran Canaria; MESO; mesocosm experiment; Mesocosm experiment; Mesocosm label; Ocean Artificial Upwelling; Ocean-artUp; Phytoplankton; primary production; Primary production of carbon, organic, dissolved; Primary production of carbon, organic, dissolved, standard deviation; Primary production of carbon, organic, particulate; Primary production of carbon, organic, total; Sampling date/time, experiment; Treatment; Type of study
    Type: Dataset
    Format: text/tab-separated-values, 3342 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2024-03-22
    Description: This dataset contains the results of the fluorescent dissolved organic matter characterisation (FDOM) and water mass optimum multiparameter analysis from the MAFIA cruise (Migrants and Active Flux In the Atlantic ocean). Samples were collected in the tropical and subtropical Atlantic during the MAFIA cruise (April 2015) on board the BIO Hespérides. Seawater samples for biogeochemical analyses were collected at 13 stations (from the Brazilian coast to the Canary Islands), from the surface down to 3500 m, using a General Oceanics oceanographic rosette equipped with 24 l PVC Niskin bottles. Oxygen solubility was computed using the equation of Benson and Krause (1984). AOU (µmol/kg) was calculated by subtracting measured oxygen concentration from the oxygen solubility values at saturation, with respect to the atmosphere. Fluorescence measurements were performed with a Perkin-Elmer LS55 spectrofluorometer and FDOM was characterised by means of a Parallel Factor analysis. Integrated values were estimated by multiplying the discrete measurements by the distance, in meters, between samples. The contribution of each water mass to each sample was objectively quantified applying an optimum multiparameter analysis (excluding mixed layer samples, here 〈 100 m). The aim of this dataset was to jointly characterise the FDOM and water mass distributions to infer the processes that shape the dissolved organic matter pool in the deep ocean (water mass mixing and history vs. local processes).
    Keywords: Absorption coefficient, colored dissolved organic matter at 254 nm; Antarctic Intermediate Water of 3.1°C, relative volume contribution; Antarctic Intermediate Water of 5°C, relative volume contribution; Atlantic; Atlantic Ocean; bathypelagic; Biogeochemical impact of mesoscale and sub-mesoscale processes along the life history of cyclonic and anticyclonic eddies: plankton variability and productivity; Calculated; Calculated after Broecker (1974); Campaign; Chlorophyll a, integrated; Circumpolar Deep Water, relative volume contribution; Constraining organic carbon fluxes in an eastern boundary upwelling ecosystem (NW Africa): the role of non-sinking carbon in the context of the biological pump; Continuous Segmented Flow Analyzer, SEAL Analytical, QuAAtro39; CTD, Sea-Bird, SBE 911plus; CTD/Rosette; CTD-RO; dark ocean; Date/Time of event; DEPTH, water; Eastern North Atlantic Central Water of 12°C, relative volume contribution; Eastern North Atlantic Central Water of 15°C, relative volume contribution; e-IMPACT; Equatorial Water, relative volume contribution; Event label; Fluorescence intensity, maximum, DOM; fluorescent dissolved organic matter; FLUXES; Hespérides; Latitude of event; Longitude of event; Madeira Mode Water, relative volume contribution; MAFIA; MAFIA_01_D-1; MAFIA_02_L-1; MAFIA_03_L-1; MAFIA_04_L-1; MAFIA_05_L-1; MAFIA_06_L-1; MAFIA_07_L-1; MAFIA_08_L-1; MAFIA_09_L-1; MAFIA_10_D-1; MAFIA_11_L-1; MAFIA_12_L-1; MAFIA_13-1; Mediterranean Water, relative volume contribution; mesopelagic; Migrants and Active Flux In the Atlantic Ocean; Nitrate + Oxygen tracer; North Atlantic Deep Water of 2°C, relative volume contribution; North Atlantic Deep Water of 4.6°C, relative volume contribution; optimum multiparameter analysis; Optimum multiparameter analysis; Oxygen; Oxygen, apparent utilization; Oxygen, Benson & Krause 1984; Parallel factor analysis (PARAFAC); Pressure, water; Salinity; Salinity Maximum Water, relative volume contribution; Sample ID; Silicate; Spectrophotometer, Ocean Optics USB2000; Station label; Subpolar Mode Water, relative volume contribution; subtropical - tropical Atlantic; SUMMER; Sustainable Management of Mesopelagic Resources; Temperature, water, potential; Titration, Winkler; water masses
    Type: Dataset
    Format: text/tab-separated-values, 6717 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...