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  • 1
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    PANGAEA
    In:  Supplement to: Bergauer, Kristin; Fernandez-Guerra, Antonio; Garcia, Juan A L; Sprenger, Antoinette; Stepanauskas, Ramunas; Pachiadaki, Maria G; Jensen, Ole N; Herndl, Gerhard J (2018): Organic matter processing by microbial communities throughout the Atlantic water column as revealed by metaproteomics. Proceedings of the National Academy of Sciences, 115(3), E400-E408, https://doi.org/10.1073/pnas.1708779115
    Publication Date: 2023-01-13
    Description: The phylogenetic composition of the heterotrophic microbial community is depth stratified in the oceanic water column down to abyssopelagic layers. In the layers below the euphotic zone, it has been suggested that heterotrophic microbes rely largely on solubilized particulate organic matter as a carbon and energy source rather than on dissolved organic matter. To decipher whether changes in the phylogenetic composition with depth are reflected in changes in the bacterial and archaeal transporter proteins, we generated an extensive metaproteomic and metagenomic dataset of microbial communities collected from 100- to 5,000-m depth in the Atlantic Ocean.
    Keywords: MALASPINA-2010; Malaspina circumnavigation expedition
    Type: Dataset
    Format: application/zip, 73.6 kBytes
    Location Call Number Limitation Availability
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  • 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
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  • 3
    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. The flag denotes if FDOM values were from direct measurement or are interpolated values (some interpolated values were added to match the 16S amplicon data). Integrated values were estimated by multiplying the discrete measurements by the distance, in meters, between samples.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; 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; Campaign; Chlorophyll a, integrated; 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; CTD, Sea-Bird, SBE 911plus; CTD/Rosette; CTD-RO; dark ocean; Date/Time of event; DEPTH, water; e-IMPACT; Event label; Fluorescence intensity, maximum, DOM; fluorescent dissolved organic matter; FLUXES; Hespérides; Latitude of event; Longitude of event; 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; mesopelagic; Migrants and Active Flux In the Atlantic Ocean; optimum multiparameter analysis; Oxygen; Oxygen, apparent utilization; Oxygen, Benson & Krause 1984; Parallel factor analysis (PARAFAC); Pressure, water; Salinity; Sample ID; Spectrophotometer, Ocean Optics USB2000; Station label; SUMMER; Sustainable Management of Mesopelagic Resources; Temperature, water, potential; Titration, Winkler; Validation flag/comment; water masses
    Type: Dataset
    Format: text/tab-separated-values, 3925 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-03-22
    Description: This dataset contains the results of the characterisation of the prokaryotic community by flow cytometry and tritiated leucine incorporation 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 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. Abundance and cell characteristics (high nucleic acid content fraction, cell volume, viability) were based on measurements performed with a FACSCalibur (Becton-Dickinson) flow cytometer. Leucine incorporation rates were estimated with tritiated leucine (Kirchman et al. 1985) using centrifugation and filtration methods (Smith and Azam 1992). The aim of this dataset was to estimate the influence of surface productivity on the standing stock, characteristics and activity (as leucine incorporation) of prokaryotes across the water column.
    Keywords: 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; Biomass; Bulk 3H-leucine incorporation rate; Calculated; Calculated after Calvo-Díaz and Morán (2006); Calculated after Norland (1993); Campaign; cell volume; Chlorophyll a; Chlorophyll fluorometer, Seapoint, Seapoint chlorophyll fluorometer; 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; CTD, Sea-Bird, SBE 911plus; CTD/Rosette; CTD-RO; cytometry; Date/Time of event; deep ocean; DEPTH, water; e-IMPACT; Event label; FACSCalibur flow-cytometer (Becton Dickinson); FLUXES; Hespérides; High nucleic acid prokaryotes; High nucleic acid prokaryotes/low nucleic acid prokaryotes ratio; Latitude of event; leucine incorporation; Longitude of event; Low nucleic acid prokaryotes; 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; mesopelagic; microbial community; Migrants and Active Flux In the Atlantic Ocean; NADS; Pressure, water; productivity; prokaryote; Prokaryotes; Prokaryotes, biomass as carbon; Prokaryotes, cell volume; prokaryotic abundance; Salinity; Sample ID; Sea surface chlorophyll a; Specific 3H-leucine incorporation rate; Station label; subtropical - tropical Atlantic; SUMMER; Sustainable Management of Mesopelagic Resources; Temperature, water, potential; Tritiated leucine incorporation (Kirchman et al. 1985) with centrifugation and filtration methods (Smith and Azam 1992); viability; Viable cell fraction
    Type: Dataset
    Format: text/tab-separated-values, 4251 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-03-22
    Description: This dataset contains the results of the characterisation of the prokaryotic community by flow cytometry and tritiated leucine incorporation 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 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. Abundance and cell characteristics (high nucleic acid content fraction, cell volume, viability) were based on measurements performed with a FACSCalibur (Becton-Dickinson) flow cytometer. Leucine incorporation rates were estimated with tritiated leucine (Kirchman et al. 1985) using centrifugation and filtration methods (Smith and Azam 1992). Integrated or average values of variables were estimated for the epipelagic (0-200 m), mesopelagic (200-1000 m) and bathypelagic (1000-3000 m) layers, based on an interpolated grid estimated with DIVA. The aim of this dataset was to estimate the influence of surface productivity on the standing stock, characteristics and activity (as leucine incorporation) of prokaryotes across the water column.
    Keywords: 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; Biomass; Bulk 3H-leucine incorporation rate, integrated; Calculated; Campaign; cell volume; Chlorophyll fluorometer, Seapoint, Seapoint chlorophyll fluorometer; 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; CTD/Rosette; CTD-RO; cytometry; Date/Time of event; deep ocean; DEPTH, water; e-IMPACT; Event label; FLUXES; Hespérides; High nucleic acid prokaryotes/low nucleic acid prokaryotes ratio; Latitude of event; Layer description; leucine incorporation; Longitude of event; 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; mesopelagic; microbial community; Migrants and Active Flux In the Atlantic Ocean; NADS; productivity; prokaryote; Prokaryotes, abundance, integrated; Prokaryotes, cell volume; prokaryotic abundance; Sea surface chlorophyll a; Specific 3H-leucine incorporation rate; Station label; subtropical - tropical Atlantic; SUMMER; Sustainable Management of Mesopelagic Resources; viability; Viable cell fraction
    Type: Dataset
    Format: text/tab-separated-values, 375 data points
    Location Call Number Limitation Availability
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  • 6
    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. Fluorescence measurements were performed with a Perkin-Elmer LS55 spectrofluorometer and FDOM was characterised by means of a Parallel Factor analysis. 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: Atlantic; bathypelagic; Biogeochemical impact of mesoscale and sub-mesoscale processes along the life history of cyclonic and anticyclonic eddies: plankton variability and productivity; 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; dark ocean; e-IMPACT; fluorescent dissolved organic matter; FLUXES; MAFIA; mesopelagic; Migrants and Active Flux In the Atlantic Ocean; optimum multiparameter analysis; Oxygen; SUMMER; Sustainable Management of Mesopelagic Resources; water masses
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2024-03-22
    Description: This dataset contains the results of the characterisation of the prokaryotic community by flow cytometry and tritiated leucine incorporation 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 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. Abundance and cell characteristics (high nucleic acid content fraction, cell volume, viability) were based on measurements performed with a FACSCalibur (Becton-Dickinson) flow cytometer. Leucine incorporation rates were estimated with tritiated leucine (Kirchman et al. 1985) using centrifugation and filtration methods (Smith and Azam 1992). Integrated or average values of variables were estimated for the epipelagic (0-200 m), mesopelagic (200-1000 m) and bathypelagic (1000-3000 m) layers. The aim of this dataset was to estimate the influence of surface productivity on the standing stock, characteristics and activity (as leucine incorporation) of prokaryotes across the water column.
    Keywords: Atlantic; bathypelagic; Biogeochemical impact of mesoscale and sub-mesoscale processes along the life history of cyclonic and anticyclonic eddies: plankton variability and productivity; Biomass; cell volume; 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; cytometry; deep ocean; e-IMPACT; FLUXES; leucine incorporation; MAFIA; mesopelagic; microbial community; Migrants and Active Flux In the Atlantic Ocean; NADS; productivity; prokaryote; prokaryotic abundance; SUMMER; Sustainable Management of Mesopelagic Resources; viability
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-03-22
    Description: This dataset contains the dissolved organic matter (DOM) quantification and optical characterisation results from a KOSMOS mesocosm experiment carried out in the framework of the Ocean Artificial Upwelling project. The experiment was carried out in the autumn of 2018 in the oligotrophic waters of Gran Canaria. During the 39 days of experiment nutrient-rich deep water was added to the mesocosms in two modes (singular vs recurring additions), with four levels of intensity. Dissolved organic carbon, nitrogen and phosphorus were quantified with a Shimadzu TOC-5000 and a QuAAtro AutoAnalyzer. The absorption and fluorescence proprieties of DOM were determined making use of an Ocean Optics USB2000+UV-VIS-ES Spectrometer and a Jobin Yvon Horiba Fluoromax-4 spectrofluorometer, respectively. The aim of this dataset was to study the effect of artificial upwelling on the dissolved organic matter pool and its potential implications for carbon sequestration.
    Keywords: Absorption coefficient, 254 nm; Absorption coefficient, 325 nm; artificial upwelling; Biogeochemical impact of mesoscale and sub-mesoscale processes along the life history of cyclonic and anticyclonic eddies: plankton variability and productivity; Calculated; Canarias Sea; Carbon, organic, dissolved; Carbon, organic, dissolved/Nitrogen, organic, dissolved ratio; Carbon, organic, dissolved/Phosphorus, organic, dissolved ratio; carbon sequestration; chromophoric dissolved organic matter; DATE/TIME; Day of experiment; Dissolved Organic Carbon; Dissolved Organic Matter; dissolved organic nitrogen; dissolved organic phosphorus; e-IMPACT; Event label; Fluorescence intensity, maximum, component 1; Fluorescence intensity, maximum, component 2; Fluorescence intensity, maximum, component 4; Fluorescence intensity, maximum, component 5; fluorescent dissolved organic matter; Jobin Yvon Horiba Fluoromax-4 spectrofluorometer; KOSMOS_2018; KOSMOS_2018_Mesocosm-A; KOSMOS_2018_Mesocosm-DW; 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 label; mesocosm study; Nitrogen, organic, dissolved; Nitrogen, organic, dissolved/Phosphorus, organic, dissolved ratio; Ocean Artificial Upwelling; Ocean-artUp; Ocean Optics USB2000+UV-VIS-ES Spectrometer; Phosphorus, organic, dissolved; PUMP; QuAAtro AutoAnalyzer; Shimadzu Total Organic Carbon Analyzer (TOC-5000A); Slope ratio; Spectral slope, 275-295 nm; Spectral slope, 350-400 nm; Treatment; Treatment: nutrients; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management; Water pump
    Type: Dataset
    Format: text/tab-separated-values, 3962 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2024-04-03
    Description: This dataset contains the results of the analysis of standing stocks and activity of prokaryotes during the KOSMOS mesocosm experiment carried out in the framework of the Ocean Artificial Upwelling project. The experiment was carried out in the autumn of 2018 in the oligotrophic waters off Gran Canaria. During the 39 days of experiment nutrient-rich deep water was added to the mesocosms in two modes (singular vs recurring additions), with four levels of intensity. Prokaryotic abundances and viability were quantified with a FACSCalibur flow cytometer (Becton-Dickinson). Prokaryotic activity (as protein synthesis) was assessed by means of BioOrthogonal Non-Canonical Amino acid Tagging (BONCAT), using a Zeiss Axio Imager.Z2m Epifluorescence Microscope (AxioCam MRm, Carl Zeiss MicroImaging). The aim of this dataset was to study the effect of different upwelling regimes on the prokaryotic communities and its potential implications for organic matter cycling.
    Keywords: Abundance; activity; artificial upwelling; Canarias Sea; DATE/TIME; Day of experiment; Depth, water, experiment, bottom/maximum; Depth, water, experiment, top/minimum; Epifluorescence Microscope, Carl Zeiss MicroImaging, AxioCam MRm, Zeiss Axio Imager.Z2m; Event label; FACSCalibur flow-cytometer (Becton Dickinson); Field experiment; High nucleic acid prokaryotes; High nucleic acid prokaryotes/prokaryotes ratio; KOSMOS_2018; KOSMOS_2018_Mesocosm-A; KOSMOS_2018_Mesocosm-DW; 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; Low nucleic acid prokaryotes; MESO; mesocosm experiment; Mesocosm experiment; Mesocosm label; Nanoeukaryotes; Ocean Artificial Upwelling; Ocean-artUp; Picoeukaryotes; Prochlorococcus; prokaryote; Prokaryotes; Prokaryotes, active; Prokaryotes, active, standard deviation; protein; Synechococcus; Treatment; Treatment: nitrogen; Type of study; viability; Viability
    Type: Dataset
    Format: text/tab-separated-values, 4394 data points
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2024-02-07
    Description: In the face of climate change there is a need to reduce atmospheric CO2 concentrations. Artificial upwelling of nutrient-rich deep waters has been proposed as a method to enhance the biological carbon pump in oligotrophic oceanic regions in order to increase carbon sequestration. Here we examine the effect of different artificial upwelling intensities and modes (single pulse versus recurring pulses) on the dynamics of the dissolved organic matter pool (DOM). We introduced nutrient-rich deep water to large scale mesocosms (~44 m3) in the oligotrophic subtropical North Atlantic and found that artificial upwelling strongly increased DOM concentrations and changed its characteristics. The magnitude of the observed changes was related to the upwelling intensity: more intense treatments led to higher accumulation of dissolved organic carbon (〉70 μM of excess DOC over ambient waters for the most intense) and to comparatively stronger changes in DOM characteristics (increased proportions of chromophoric DOM (CDOM) and humic-like fluorescent DOM), suggesting a transformation of the DOM pool at the molecular level. Moreover, the single upwelling pulse resulted in higher CDOM quantities with higher molecular weight than the recurring upwelling mode. Together, our results indicate that under artificial upwelling, large DOM pools may accumulate in the surface ocean without being remineralized in the short-term. Possible reasons for this persistence could be a combination of the molecular diversification of DOM due to microbial reworking, nutrient limitation and reduced metabolic capabilities of the prokaryotic communities within the mesocosms. Our study demonstrates the importance of the DOC pool when assessing the carbon sequestration potential of artificial upwelling.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
    Format: text
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