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  • 1
    Keywords: Hochschulschrift ; Nordpolarmeer ; Erwärmung ; Versauerung ; Rotalgen
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (64 Blatt = 3,7 MB)
    Language: English
    Location Call Number Limitation Availability
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  • 2
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    Unknown
    PANGAEA
    In:  Supplement to: Hellemann, Dana; Tallberg, Petra; Bartl, Ines; Voss, Maren; Hietanen, Susanna (2017): Denitrification in an oligotrophic estuary: a delayed sink for riverine nitrate. Marine Ecology Progress Series, 583, 63-80, https://doi.org/10.3354/meps12359
    Publication Date: 2024-01-24
    Description: Sediment samples for measuring N2 production and for the characterization of the sediment system were taken in spring and summer 2015 in the Öre Estuary at the Swedish coast of the Quark Strait, northern Baltic Sea. Sediment was sampled with a HAPS bottom corer (sand) and with a GEMINI twin corer (mud). The grain size of the sand sediment was analyzed via wet sieving from the sediment layers 0-1, 1-2, 2-3 cm (spring campaign) and 0-0.5, 0.5-1.0, 1.0-1.5 cm (summer campaign); due to vertical homogeneity, these surface sediments were subsequently pooled and the sediment type was classified after Wentworth (1922). Porosity and water content were analyzed both from sediment slices and from entire core subsamples, which means that sediment in a sampling core (heights 20 cm, iD 2.3 cm) was mixed and sub sampled, assuming vertical homogeneity; sediment was dried overnight at 105°C and calculations followed Burdige (2006). Sediment organic matter content was analyzed as loss on ignition (LOI), for which dried sediment was combusted at 550°C for 4h. Sediment permeability was measured from pooled surface sediments (~1-2 cm homogeneous surface layer) with a permeameter cell following the constant head method for laminar flow of water through granular soil; calculations were derived from Darcie's Law. The oxygen penetration depth (OPD) was determined by manual (spring) and automated (summer) profiling at bottom water temperature (electrode tip 100 µm). Denitrification rates were measured with the revised isotope pairing technique (r-IPT; Risgaard-Petersen et al. 2003, 2004) that accounts for the potential contribution of anammox (anaerobic ammonium oxidation) to total N2 production. Incubations were done in acrylic cores (heights 20 cm, iD 2.3 cm) in a concentration series of 30, 60, 90, 120 µM 15NO3- (n=3) for 4-5h at in situ bottom water temperature and darkness. Dw gives denitrification of nitrate from the water column; Dn gives denitrification of nitrate from sediment nitrification (coupled nitrification-denitrification). If no contribution of anammox to total N2 production was found, columns hold a zero (0).
    Keywords: after Risgaard-Petersen et al. 2003 (r-IPT); Amorphous, biogenic silicate per dry mass; Anammox rates; Calcium extractable silicate per dry mass; Calculation according to Burdige 2006; Comment; Cruise/expedition; Date/Time of event; Depth, bottom/max; Depth, description; Depth, top/min; DEPTH, water; Description; Event label; Latitude of event; Longitude of event; Loss on ignition; MULT; Multiple investigations; Nitrate denitrification, total; Nitrate denitrification from sediment nitrification; Nitrate denitrification from water column; Ore_estuary_20150421_N3; Ore_estuary_20150421_NB1; Ore_estuary_20150422_N6_1; Ore_estuary_20150422_N8; Ore_estuary_20150423_N10; Ore_estuary_20150423_N11; Ore_estuary_20150424_N5; Ore_estuary_20150424_N7; Ore_estuary_20150425_N14; Ore_estuary_20150425_NB8; Ore_estuary_20150804_N3; Ore_estuary_20150804_NB1; Ore_estuary_20150805_N34; Ore_estuary_20150805_N6_1; Ore_estuary_20150806_N10; Ore_estuary_20150806_N11; Ore_estuary_20150807_N5; Ore_estuary_20150807_NB8_1; Ore_estuary_20150808_N14; Ore_estuary_20150808_N7; Ore Estuary; Oxide bound silicate per dry mass; Oxygen penetration depth; Permeability (earth science); Porosity; Sediment type; Size fraction 〈 0.063 mm, mud, silt+clay; Size fraction 〉 1 mm, gravel; Size fraction 0.125-0.063 mm, 3.0-4.0 phi, very fine sand; Size fraction 0.250-0.125 mm, 2.0-3.0 phi, fine sand; Size fraction 0.500-0.250 mm, 1.0-2.0 phi, medium sand; Size fraction 1.000-0.500 mm, 0.0-1.0 phi, coarse sand; Station label; Water content, wet mass
    Type: Dataset
    Format: text/tab-separated-values, 1763 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-01-24
    Description: Sediment samples for measuring N2 production rates and for the characterization of the sediment system were taken every month (early spring to late autumn) over 2 years from a sand and a mud sediment in the Tvärminne Archipelago at the Finnish coast of the Gulf of Finland, Northern Baltic Sea. Sediment was sampled with a HAPS bottom corer (sand) and a GEMAX twin corer (mud). Bottom water dissolved oxygen (O2) and nutrients (nitrate [NO3-], nitrate + nitrite [NO3- + NO2-], ammonium [NH4+], phosphate [PO43-]) were analysed from a sample withdrawn ~ 5 cm above the sediment surface. O2 concentrations were measured with Winkler titration; nutrient samples were 0.2 µm filtered and kept dark and cool until measurement with an autosampler (Thermo Scientific Aquakem 250). Photosynthetic active radiation (PAR) was measured close to the bottom and at the water surface with a spherical light sensor (Li-COR). The grain size of the sand sediment was analyzed with a particle detector (CILAS 1180 Naß) and the sediment type was classified after Wentworth (1922). Porosity and water content were analyzed both from sediment slices and from entire core subsamples, which means that sediment in a sampling core (heights 20 cm, iD 2.3 cm) was mixed and sub sampled, assuming vertical homogeneity; sediment was dried overnight at 105°C and calculations followed Burdige (2006). Sediment organic matter content was analyzed as loss on ignition (LOI), for which dried sediment was combusted at 550°C for 4h. Sediment permeability was measured from pooled surface sediments (~1-2 cm homogeneous surface layer) with a permeameter cell following the constant head method for laminar flow of water through granular soil; calculations were derived from Darcy's Law. The oxygen penetration depth (OPD) was determined by automated O2 profiling (except for May, October 2015: manual profiling) at bottom water temperature, electrode tip 100 µm (except for May 2016, Storfjärden: 250 µm). Benthic denitrification rates were measured with the revised isotope pairing technique (r-IPT; Risgaard-Petersen et al. 2003, 2004) that accounts for the potential contribution of anammox (anaerobic ammonium oxidation) to total N2 production. Incubations were done in acrylic cores (heights 15-20 cm, iD 2.3 cm) in a concentration series of 30, 60, 90, 120 µM 15NO3- (n=3; 2015), and 40 (n=4), 80 (n=4), 120 (n=8) µM 15NO3- (2016) for 4h at in situ bottom water temperature and darkness. Incubations were done in diffusive cores in both mud and sand, as sand permeability was 〈2.5*10-12 m2 and thus significant effects of advective pore water flow on sediment biogeochemistry could be neglected (2.5*10-12 m2 was used as threshold for the onset of effects of advection in Baltic Sea coastal sediments according to Forster et al. 2003). Dw gives denitrification of nitrate from the water column; Dn gives denitrification of nitrate from sediment nitrification (coupled nitrification-denitrification). If no contribution of anammox to total N2 production was found, columns hold a zero (0).
    Keywords: after Risgaard-Petersen et al. 2003 (r-IPT); Ammonium; Anammox rates; Autoanalyser (Thermo Scientific Aquakem 250); Calculation according to Burdige 2006; Comment; Date/Time of event; Depth, bottom/max; Depth, top/min; DEPTH, water; Description; Event label; Grain size, CILAS 1180 Laser Particle Analyser; Latitude of event; Longitude of event; Loss on ignition; MULT; Multiple investigations; Nitrate; Nitrate and Nitrite; Nitrate denitrification, total; Nitrate denitrification from sediment nitrification; Nitrate denitrification from water column; Oxygen; Oxygen penetration depth; Permeability (earth science); Phosphate; Porosity; Radiation, photosynthetically active; Salinity; Sediment type; Size fraction 〈 0.063 mm, mud, silt+clay; Size fraction 0.125-0.063 mm, 3.0-4.0 phi, very fine sand; Size fraction 0.250-0.125 mm, 2.0-3.0 phi, fine sand; Size fraction 0.500-0.250 mm, 1.0-2.0 phi, medium sand; Size fraction 1.000-0.500 mm, 0.0-1.0 phi, coarse sand; Station label; Temperature, water; Titration, Winkler; TVÄ-Archipelago_20150316-i30; TVÄ-Archipelago_20150507-i30; TVÄ-Archipelago_20150507-Storfjärden; TVÄ-Archipelago_20150609-i30; TVÄ-Archipelago_20150609-Storfjärden; TVÄ-Archipelago_20150708-i30; TVÄ-Archipelago_20150813-i30; TVÄ-Archipelago_20150813-Storfjärden; TVÄ-Archipelago_20150907-Storfjärden; TVÄ-Archipelago_20150917-Storfjärden; TVÄ-Archipelago_20151020-i30; TVÄ-Archipelago_20151020-Storfjärden; TVÄ-Archipelago_20160405-i30; TVÄ-Archipelago_20160406-Storfjärden; TVÄ-Archipelago_20160503-i30; TVÄ-Archipelago_20160504-Storfjärden; TVÄ-Archipelago_20160607-i30; TVÄ-Archipelago_20160608-Storfjärden; TVÄ-Archipelago_20160705-i30; TVÄ-Archipelago_20160706-Storfjärden; TVÄ-Archipelago_20160808-i30; TVÄ-Archipelago_20160809-Storfjärden; TVÄ-Archipelago_20160913-i30; TVÄ-Archipelago_20160914-Storfjärden; TVÄ-Archipelago_20161011-i30; TVÄ-Archipelago_20161012-Storfjärden; TVÄ-Archipelago_20161114-i30; TVÄ-Archipelago_20161115-Storfjärden; Tvärminne, Finnland; TvärminneArchipelago_20150316-i30; TvärminneArchipelago_20150507-i30; TvärminneArchipelago_20150507-Storfjärden; TvärminneArchipelago_20150609-i30; TvärminneArchipelago_20150609-Storfjärden; TvärminneArchipelago_20150708-i30; TvärminneArchipelago_20150813-i30; TvärminneArchipelago_20150813-Storfjärden; TvärminneArchipelago_20150907-Storfjärden; TvärminneArchipelago_20150917-Storfjärden; TvärminneArchipelago_20151020-i30; TvärminneArchipelago_20151020-Storfjärden; TvärminneArchipelago_20160405-i30; TvärminneArchipelago_20160406-Storfjärden; TvärminneArchipelago_20160503-i30; TvärminneArchipelago_20160504-Storfjärden; TvärminneArchipelago_20160607-i30; TvärminneArchipelago_20160608-Storfjärden; TvärminneArchipelago_20160705-i30; TvärminneArchipelago_20160706-Storfjärden; TvärminneArchipelago_20160808-i30; TvärminneArchipelago_20160809-Storfjärden; TvärminneArchipelago_20160913-i30; TvärminneArchipelago_20160914-Storfjärden; TvärminneArchipelago_20161011-i30; TvärminneArchipelago_20161012-Storfjärden; TvärminneArchipelago_20161114-i30; TvärminneArchipelago_20161115-Storfjärden; Water content, wet mass
    Type: Dataset
    Format: text/tab-separated-values, 2714 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-01-24
    Description: Sediment samples for measuring N2 production rates and for the characterization of the sediment system were taken in three seasons (winter, spring, summer) from sand and mud sediments of the Vistula Estuary and the open Bay of Gdansk at the Polish coast, Southern Baltic Sea. Sediment was sampled with a HAPS bottom corer (coarse sand), a Multicorer and a Boxcorer (fine sand, mud). Porosity was analyzed both from sediment slices and from entire core subsamples, which means that sediment in a sampling core (heights 15-20 cm, iD 2.3 cm) was mixed and sub sampled, assuming vertical homogeneity; sediment was dried overnight at 105°C and calculations followed Burdige (2006). Sediment organic matter content was analyzed as loss on ignition (LOI), for which dried sediment was combusted at 550°C for 4h. Sediment permeability was measured from pooled surface sediments (~1-2 cm homogeneous surface layer) with a permeameter cell following the constant head method for laminar flow of water through granular soil; calculations were derived from Darcy's Law. The oxygen penetration depth (OPD) was determined by manual (EMB 77, AL 449) and automated (EMB 123) profiling at bottom water temperature, electrode tip 100 µm: EMB 123, AL 449 (mud) and 250 µm: EMB 77, AL 449 (sand), EMB 123 (VE05, VE49). Denitrification rates were measured with the revised isotope pairing technique (r-IPT; Risgaard-Petersen et al. 2003, 2004) that accounts for the potential contribution of anammox (anaerobic ammonium oxidation) to total N2 production. Incubations were done in acrylic cores (heights 15-20 cm, iD 2.3 cm) in a concentration series of 30, 60, 90, 120 µM 15NO3- (n=3, EMB 77, AL 449) and 40 (n=4), 80 (n=4), 120 (n=12) µM 15NO3- for 3-5h at in situ bottom water temperature and darkness. In the presence of significant advective pore water flow, an advective incubation design was used. Dw gives denitrification of nitrate from the water column; Dn gives denitrification of nitrate from sediment nitrification (coupled nitrification-denitrification). If no contribution of anammox to total N2 production was found, columns hold a zero (0). The sediment silicate content (ASi =amorphous, biogenic Si (Na2CO3-extractable), Ca-Si = easily available Si (CaCl2-extractable), Ox-Si = oxide-bound Si (extractable by acid oxalate)) was analyzed from the top sediment layer.
    Keywords: after Risgaard-Petersen et al. 2003 (r-IPT); Amorphous, biogenic silicate per dry mass; Anammox rates; Calcium extractable silicate per dry mass; Calculation according to Burdige 2006; Comment; Cruise/expedition; Date/Time of event; Depth, description; DEPTH, water; Description; Event label; Latitude of event; Longitude of event; Loss on ignition; MULT; Multiple investigations; Nitrate denitrification, total; Nitrate denitrification from sediment nitrification; Nitrate denitrification from water column; Oxide bound silicate per dry mass; Oxygen penetration depth; Permeability (earth science); Porosity; Sediment type; Station label; Vistula_estuary_20140705-VE15; Vistula_estuary_20140707-VE02; Vistula_estuary_20140707-VE46; Vistula_estuary_20140707-VE53; Vistula_estuary_20140708-VE03; Vistula_estuary_20140708-VE05; Vistula_estuary_20140709-VE09; Vistula_estuary_20140709-VE13; Vistula_estuary_20140710-VE18; Vistula_estuary_20140710-VE23; Vistula_estuary_20140710-VE23a; Vistula_estuary_20140710-VE24; Vistula_estuary_20140711-VE49a; Vistula_estuary_20140712-VE38; Vistula_estuary_20140713-TF0233; Vistula_estuary_20140713-VE43; Vistula_estuary_20140714-VE39; Vistula_estuary_20150201-VE04; Vistula_estuary_20150201-VE05; Vistula_estuary_20150201-VE06; Vistula_estuary_20150202-VE07; Vistula_estuary_20150203-VE10; Vistula_estuary_20150204-VE02; Vistula_estuary_20150205-TF0233; Vistula_estuary_20150205-VE38; Vistula_estuary_20150205-VE39; Vistula_estuary_20150206-VE09; Vistula_estuary_20150206-VE13; Vistula_estuary_20150207-VE49a; Vistula_estuary_20150209-VE02; Vistula_estuary_20160229-VE07; Vistula_estuary_20160301-VE06; Vistula_estuary_20160302-VE04; Vistula_estuary_20160303-VE18; Vistula_estuary_20160304-VE38; Vistula_estuary_20160305-VE13; Vistula_estuary_20160305-VE15; Vistula_estuary_20160306-VE09; Vistula_estuary_20160307-VE05; Vistula_estuary_20160308-VE02; Vistula_estuary_20160309-VE49a; Vistula River, Poland
    Type: Dataset
    Format: text/tab-separated-values, 2597 data points
    Location Call Number Limitation Availability
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  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Boxhammer, Tim; Taucher, Jan; Bach, Lennart Thomas; Achterberg, Eric Pieter; Algueró-Muñiz, Maria; Bellworthy, Jessica; Czerny, Jan; Esposito, Mario; Haunost, Mathias; Hellemann, Dana; Ludwig, Andrea; Yong, Jaw-Chuen; Zark, Maren; Riebesell, Ulf; Anderson, Leif G (2018): Enhanced transfer of organic matter to higher trophic levels caused by ocean acidification and its implications for export production: A mass balance approach. PLoS ONE, 13(5), e0197502, https://doi.org/10.1371/journal.pone.0197502
    Publication Date: 2024-03-06
    Description: The present biogeochemical parameters were measured or calculated in 2013 during a long-term mesocosm CO2 perturbation study in Gullmar Fjord (Sweden). The natural plankton community was enclosed in ten pelagic mesocosms following the natural winter-to-summer plankton succession. Five of the mesocosms were enriched with CO2 to simulate end-of the century ocean acidification (760 µatm) while the others served as controls. The data set was used for mass balance calculations to investigate the impact of realistic end-of-the-century CO2 concentrations on the development and partitioning of the carbon, nitrogen, phosphorus, and silica pools in a coastal pelagic ecosystem.
    Keywords: AA; Ammonium; Autoanalyzer; BIOACID; Biogenic silica; Biological Impacts of Ocean Acidification; Calculated; Calculated, see reference(s); Carbon, inorganic, dissolved; Carbon, organic, dissolved; Carbon, total, particulate; Carbon/Nitrogen ratio; Carbon analyser; Chlorophyll a; CN-analyser; Coulometric titration; DATE/TIME; Day of experiment; Event label; Fluorometric; Gullmar Fjord, Skagerrak, Sweden; Hand-operated CTD (Sea&Sun Technology, CTD 60M); High Performance Liquid Chromatography (HPLC); KOSMOS_2013_Mesocosm-M1; KOSMOS_2013_Mesocosm-M10; KOSMOS_2013_Mesocosm-M2; KOSMOS_2013_Mesocosm-M3; KOSMOS_2013_Mesocosm-M4; KOSMOS_2013_Mesocosm-M5; KOSMOS_2013_Mesocosm-M6; KOSMOS_2013_Mesocosm-M7; KOSMOS_2013_Mesocosm-M8; KOSMOS_2013_Mesocosm-M9; KOSMOS 2013; MESO; Mesocosm experiment; Mesocosm label; Mesozooplankton, biomass as carbon; Mesozooplankton, biomass as nitrogen; Mesozooplankton, biomass as phosphorus; Nitrate and Nitrite; Nitrogen, organic, dissolved; Nitrogen, total, particulate; Nitrogen, total dissolved; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Phosphate; Phosphorus, organic, dissolved; Phosphorus, particulate; Phosphorus, total dissolved; Salinity; Silicate; Spectrophotometry; Temperature, water; Vertical flux, biogenic silica; Vertical flux, biogenic silica, cumulated; Vertical flux, carbon; Vertical flux, carbon, cumulated; Vertical flux, nitrogen; Vertical flux, nitrogen, cumulated; Vertical flux, phosphorus; Vertical flux, phosphorus, cumulated; Volume
    Type: Dataset
    Format: text/tab-separated-values, 21872 data points
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  • 6
    Publication Date: 2024-03-15
    Keywords: AA; Alkalinity, total; Ammonium; Aragonite saturation state; Autoanalyzer; Bicarbonate ion; Biogenic silica; Biomass/Abundance/Elemental composition; Calcite saturation state; Calculated; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, organic, dissolved; Carbon, total, particulate; Carbon/Nitrogen ratio; Carbon analyser; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chlorophyll a; CN-analyser; Coast and continental shelf; Coulometric titration; DATE/TIME; Day of experiment; Entire community; Event label; Field experiment; Fluorometric; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gullmar Fjord, Skagerrak, Sweden; Hand-operated CTD (Sea&Sun Technology, CTD 60M); High Performance Liquid Chromatography (HPLC); KOSMOS_2013_Mesocosm-M1; KOSMOS_2013_Mesocosm-M10; KOSMOS_2013_Mesocosm-M2; KOSMOS_2013_Mesocosm-M3; KOSMOS_2013_Mesocosm-M4; KOSMOS_2013_Mesocosm-M5; KOSMOS_2013_Mesocosm-M6; KOSMOS_2013_Mesocosm-M7; KOSMOS_2013_Mesocosm-M8; KOSMOS_2013_Mesocosm-M9; KOSMOS 2013; MESO; Mesocosm experiment; Mesocosm label; Mesocosm or benthocosm; Mesozooplankton, biomass as carbon; Mesozooplankton, biomass as nitrogen; Mesozooplankton, biomass as phosphorus; Nitrate and Nitrite; Nitrogen, organic, dissolved; Nitrogen, total, particulate; Nitrogen, total dissolved; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; Phosphate; Phosphorus, organic, dissolved; Phosphorus, particulate; Phosphorus, total dissolved; Salinity; Silicate; Spectrophotometric; Temperate; Temperature, water; Type; Vertical flux, biogenic silica; Vertical flux, biogenic silica, cumulated; Vertical flux, carbon; Vertical flux, carbon, cumulated; Vertical flux, nitrogen; Vertical flux, nitrogen, cumulated; Vertical flux, phosphorus; Vertical flux, phosphorus, cumulated; Volume
    Type: Dataset
    Format: text/tab-separated-values, 27282 data points
    Location Call Number Limitation Availability
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  • 7
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Paul, Allanah Joy; Bach, Lennart Thomas; Schulz, Kai Georg; Boxhammer, Tim; Czerny, Jan; Achterberg, Eric Pieter; Hellemann, Dana; Trense, Yves; Nausch, Monika; Sswat, Michael; Riebesell, Ulf (2015): Effect of elevated CO2 on organic matter pools and fluxes in a summer Baltic Sea plankton community. Biogeosciences, 12(20), 6181-6203, https://doi.org/10.5194/bg-12-6181-2015
    Publication Date: 2024-03-22
    Description: Ocean acidification is expected to influence plankton community structure and biogeochemical element cycles. To date, the response of plankton communities to elevated CO2 has been studied primarily during nutrient-stimulated blooms. In this CO2 manipulation study, we used large-volume (~ 55 m3) pelagic in situ mesocosms to enclose a natural summer, post-spring-bloom plankton assemblage in the Baltic Sea to investigate the response of organic matter pools to ocean acidification.
    Keywords: Ammonium; Aphanizophyll; Aragonite saturation state; BIOACID; Biogenic silica; Biological Impacts of Ocean Acidification; Calculated; Canthaxanthin; Carbon, inorganic, dissolved; Carbon, organic, dissolved; Carbon, total, particulate; Carbon/Nitrogen ratio; Carbon/Phosphorus ratio; Carbon/Silicon ratio; Chlorophyll a; Chlorophyll b; Chlorophyll c2; Chlorophytes, biomass; Cryptophytes, biomass; Cyanobacteria, biomass; DATE/TIME; Day of experiment; Diatoms, biomass; Dry mass; Euglenophytes, biomass; Fluorescence determination; Fucoxanthin; Fugacity of carbon dioxide in seawater; Hand-operated CTD (Sea&Sun Technology, CTD 60M); High Performance Liquid Chromatography (HPLC); KOSMOS_2012_Tvaerminne; MESO; Mesocosm experiment; Mesocosm label; Myoxoxanthophyll; Neoxanthin; Nitrate and Nitrite; Nitrogen, organic, dissolved; Nitrogen, organic, particulate; Nitrogen/Phosphorus ratio; pH; Phase; Phosphate; Phosphate, total, particulate; Phosphorus, inorganic, dissolved; Phosphorus, organic, dissolved; Prasinophytes, biomass; Prasinoxanthin; Salinity; Silicate; SOPRAN; Surface Ocean Processes in the Anthropocene; Temperature, water; Violaxanthin
    Type: Dataset
    Format: text/tab-separated-values, 11813 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-03-22
    Keywords: Alkalinity, total; Ammonium; Aphanizophyll; Aragonite saturation state; Baltic Sea; Bicarbonate ion; BIOACID; Biogenic silica; Biological Impacts of Ocean Acidification; Biomass/Abundance/Elemental composition; Calcite saturation state; Calculated; Calculated using seacarb after Nisumaa et al. (2010); Canthaxanthin; Carbon, inorganic, dissolved; Carbon, organic, dissolved; Carbon, total, particulate; Carbon/Nitrogen ratio; Carbon/Phosphorus ratio; Carbon/Silicon ratio; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chlorophyll a; Chlorophyll b; Chlorophyll c2; Chlorophytes, biomass; Coast and continental shelf; Community composition and diversity; Cryptophytes, biomass; Cyanobacteria, biomass; DATE/TIME; Day of experiment; Diatoms, biomass; Dry mass; Entire community; Euglenophytes, biomass; Field experiment; Fluorescence determination; Fucoxanthin; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Hand-operated CTD (Sea&Sun Technology, CTD 60M); High Performance Liquid Chromatography (HPLC); KOSMOS_2012_Tvaerminne; MESO; Mesocosm experiment; Mesocosm label; Mesocosm or benthocosm; Myoxoxanthophyll; Neoxanthin; Nitrate and Nitrite; Nitrogen, organic, dissolved; Nitrogen, organic, particulate; Nitrogen/Phosphorus ratio; OA-ICC; Ocean Acidification International Coordination Centre; Other metabolic rates; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; Phase; Phosphate; Phosphate, total, particulate; Phosphorus, inorganic, dissolved; Phosphorus, organic, dissolved; Prasinophytes, biomass; Prasinoxanthin; Salinity; Silicate; SOPRAN; Spectrophotometric; Surface Ocean Processes in the Anthropocene; Temperate; Temperature, water; Type; Violaxanthin
    Type: Dataset
    Format: text/tab-separated-values, 14305 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2021-04-23
    Description: Ongoing acidification of the ocean through uptake of anthropogenic CO2 is known to affect marine biota and ecosystems with largely unknown consequences for marine food webs. Changes in food web structure have the potential to alter trophic transfer, partitioning, and biogeochemical cycling of elements in the ocean. Here we investigated the impact of realistic end-of-the-century CO2 concentrations on the development and partitioning of the carbon, nitrogen, phosphorus, and silica pools in a coastal pelagic ecosystem (Gullmar Fjord, Sweden). We covered the entire winter-to-summer plankton succession (100 days) in two sets of five pelagic mesocosms, with one set being CO2 enriched (~760 μatm pCO2) and the other one left at ambient CO2 concentrations. Elemental mass balances were calculated and we highlight important challenges and uncertainties we have faced in the closed mesocosm system. Our key observations under high CO2 were: (1) A significantly amplified transfer of carbon, nitrogen, and phosphorus from primary producers to higher trophic levels, during times of regenerated primary production. (2) A prolonged retention of all three elements in the pelagic food web that significantly reduced nitrogen and phosphorus sedimentation by about 11 and 9%, respectively. (3) A positive trend in carbon fixation (relative to nitrogen) that appeared in the particulate matter pool as well as the downward particle flux. This excess carbon counteracted a potential reduction in carbon sedimentation that could have been expected from patterns of nitrogen and phosphorus fluxes. Our findings highlight the potential for ocean acidification to alter partitioning and cycling of carbon and nutrients in the surface ocean but also show that impacts are temporarily variable and likely depending upon the structure of the plankton food web.
    Type: Article , PeerReviewed
    Format: text
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  • 10
    Publication Date: 2021-04-23
    Description: Every year, the oceans absorb about 30% of anthropogenic carbon dioxide (CO2) leading to a re-equilibration of the marine carbonate system and decreasing seawater pH. Today, there is increasing awareness that these changes–summarized by the term ocean acidification (OA)–could differentially affect the competitive ability of marine organisms, thereby provoking a restructuring of marine ecosystems and biogeochemical element cycles. In winter 2013, we deployed ten pelagic mesocosms in the Gullmar Fjord at the Swedish west coast in order to study the effect of OA on plankton ecology and biogeochemistry under close to natural conditions. Five of the ten mesocosms were left unperturbed and served as controls (~380 μatm pCO2), whereas the others were enriched with CO2-saturated water to simulate realistic end-of-the-century carbonate chemistry conditions (~760 μatm pCO2). We ran the experiment for 113 days which allowed us to study the influence of high CO2 on an entire winter-to-summer plankton succession and to investigate the potential of some plankton organisms for evolutionary adaptation to OA in their natural environment. This paper is the first in a PLOS collection and provides a detailed overview on the experimental design, important events, and the key complexities of such a “long-term mesocosm” approach. Furthermore, we analyzed whether simulated end-of-the-century carbonate chemistry conditions could lead to a significant restructuring of the plankton community in the course of the succession. At the level of detail analyzed in this overview paper we found that CO2-induced differences in plankton community composition were non-detectable during most of the succession except for a period where a phytoplankton bloom was fueled by remineralized nutrients. These results indicate: (1) Long-term studies with pelagic ecosystems are necessary to uncover OA-sensitive stages of succession. (2) Plankton communities fueled by regenerated nutrients may be more responsive to changing carbonate chemistry than those having access to high inorganic nutrient concentrations and may deserve particular attention in future studies.
    Type: Article , PeerReviewed
    Format: text
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