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  • 1
    Publication Date: 2023-04-13
    Keywords: 77DN20140705; 77DN20140705/1; 77DN20140705/100; 77DN20140705/101; 77DN20140705/102; 77DN20140705/103; 77DN20140705/104; 77DN20140705/105; 77DN20140705/106; 77DN20140705/107; 77DN20140705/131; 77DN20140705/132; 77DN20140705/135; 77DN20140705/138; 77DN20140705/142; 77DN20140705/144; 77DN20140705/145; 77DN20140705/146; 77DN20140705/147; 77DN20140705/148; 77DN20140705/149; 77DN20140705/150; 77DN20140705/151; 77DN20140705/152; 77DN20140705/154; 77DN20140705/59; 77DN20140705/60; 77DN20140705/62; 77DN20140705/63; 77DN20140705/64; 77DN20140705/65; 77DN20140705/66; 77DN20140705/67; 77DN20140705/93; 77DN20140705/94; 77DN20140705/95; 77DN20140705/96; 77DN20140705/97; 77DN20140705/98; 77DN20140705/99; Alkalinity, total; Arctic Ocean; CARBOCHANGE; Carbon, inorganic, dissolved; Changes in the carbon uptake and emissions by oceans in a changing climate; Coulometric titration (Johnson et al., 1985, 1987, 1993); CTD; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; East Siberian Sea; Event label; High-precision potentiometric titration (Haraldsson et al., 1997); Laptev Sea; LATITUDE; LONGITUDE; Oden; Oxygen; pH; Pressure, water; Salinity; Spectrophotometry (Clayton & Byrne, 1993); Station label; SWERUS_C3_Leg1/1; SWERUS_C3_Leg1/100; SWERUS_C3_Leg1/101; SWERUS_C3_Leg1/102; SWERUS_C3_Leg1/103; SWERUS_C3_Leg1/104; SWERUS_C3_Leg1/105; SWERUS_C3_Leg1/106; SWERUS_C3_Leg1/107; SWERUS_C3_Leg1/131; SWERUS_C3_Leg1/132; SWERUS_C3_Leg1/135; SWERUS_C3_Leg1/138; SWERUS_C3_Leg1/142; SWERUS_C3_Leg1/144; SWERUS_C3_Leg1/145; SWERUS_C3_Leg1/146; SWERUS_C3_Leg1/147; SWERUS_C3_Leg1/148; SWERUS_C3_Leg1/149; SWERUS_C3_Leg1/150; SWERUS_C3_Leg1/151; SWERUS_C3_Leg1/152; SWERUS_C3_Leg1/154; SWERUS_C3_Leg1/59; SWERUS_C3_Leg1/60; SWERUS_C3_Leg1/62; SWERUS_C3_Leg1/63; SWERUS_C3_Leg1/64; SWERUS_C3_Leg1/65; SWERUS_C3_Leg1/66; SWERUS_C3_Leg1/67; SWERUS_C3_Leg1/93; SWERUS_C3_Leg1/94; SWERUS_C3_Leg1/95; SWERUS_C3_Leg1/96; SWERUS_C3_Leg1/97; SWERUS_C3_Leg1/98; SWERUS_C3_Leg1/99; SWERUS-C3; Temperature, water, potential
    Type: Dataset
    Format: text/tab-separated-values, 4760 data points
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  • 2
    Publication Date: 2023-10-28
    Keywords: 77DN_2005-08; 77DN2005-08/01; 77DN2005-08/02; 77DN2005-08/03; 77DN2005-08/04; 77DN2005-08/05; 77DN2005-08/08; 77DN2005-08/09; 77DN2005-08/11; 77DN2005-08/12; 77DN2005-08/14; 77DN2005-08/15; 77DN2005-08/17; 77DN2005-08/19; 77DN2005-08/20; 77DN2005-08/21; 77DN2005-08/23; 77DN2005-08/25; 77DN2005-08/26; 77DN2005-08/29; 77DN2005-08/30; 77DN2005-08/31; 77DN2005-08/32; 77DN2005-08/33; 77DN2005-08/34; 77DN2005-08/35; 77DN2005-08/36; 77DN2005-08/37; 77DN2005-08/38; 77DN2005-08/39; 77DN2005-08/40; 77DN2005-08/41; 77DN2005-08/42; 77DN2005-08/43; 77DN2005-08/44; 77DN2005-08/46; 77DN2005-08/47; 77DN2005-08/49; 77DN2005-08/50; 77DN2005-08/51; 77DN2005-08/53; Alkalinity, total; Arctic Ocean; Beringia_III/01; Beringia_III/02; Beringia_III/03; Beringia_III/04; Beringia_III/05; Beringia_III/08; Beringia_III/09; Beringia_III/11; Beringia_III/12; Beringia_III/14; Beringia_III/15; Beringia_III/17; Beringia_III/19; Beringia_III/20; Beringia_III/21; Beringia_III/23; Beringia_III/25; Beringia_III/26; Beringia_III/29; Beringia_III/30; Beringia_III/31; Beringia_III/32; Beringia_III/33; Beringia_III/34; Beringia_III/35; Beringia_III/36; Beringia_III/37; Beringia_III/38; Beringia_III/39; Beringia_III/40; Beringia_III/41; Beringia_III/42; Beringia_III/43; Beringia_III/44; Beringia_III/46; Beringia_III/47; Beringia_III/49; Beringia_III/50; Beringia_III/51; Beringia_III/53; Beringia III; Calculated from depth, temperature, and salinity; Calculated from pH and alkalinity; Carbon, inorganic, dissolved; CARBOOCEAN; CTD/Rosette; CTD-RO; Date/Time of event; Density, mass density; DEPTH, water; Event label; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Latitude of event; Longitude of event; Marine carbon sources and sinks assessment; Oden; pH; Pressure, water; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Salinity; Sample code/label; see reference(s); Spectrophotometry; SPP1158; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 3235 data points
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  • 3
    Publication Date: 2024-01-06
    Description: The Tara Oceans Expedition (2009-2013) sampled the world oceans on board a 36 m long schooner, collecting environmental data and organisms from viruses to planktonic metazoans for later analyses using modern sequencing and state-of-the-art imaging technologies. Tara Oceans Data are particularly suited to study the genetic, morphological and functional diversity of plankton. During the entire expedition (2009-2013), underway measurements were obtained from a meteorological station (BATOS), a thermosalinograph (TSG, SBE 45), a Fast Repetition Rate Flurometer (FRRF, LIFT-FRR01), and a spectrophotometer (WETLabs AC-S). In 2013 underway measurements were enhanced by adding a Photosynthetically Available Radiation (PAR) sensor (QCP2350, Biospherical Instruments, Inc.), a laser spectrofluorometer (WETLabs ALFA, Chekalyuk et al., 2012) that replaced the FRRF, a spectral backscattering sensor (WETLabs Eco-bb3), a pCO2 sensor (ProOceanus CO2-Pro), a pH sensor (Satlantic, SeaFET) and a particle imaging system triggered by chlorophyll-a fluorescence (a prototype of McLane Research Laboratories' Imaging FlowCytobot, Sosik Lab, WHOI). Discrete measurements of CDOM absorption measurements were made using an Ultrapath (WPI Inc.) to calibrate the in-line AC-S. Hence the AC-S was also used to provide CDOM absorption in addition to particulate matter properties. The present collection includes three data sets that are harmonised with a common time stamp. The source data sets given in the reference section.
    Keywords: Fondation Tara Expeditions; FondTara; Tara_Oceans_2009-2013; Tara Oceans Expedition
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 4
    Publication Date: 2024-02-17
    Description: The Tara Oceans Expedition (2009-2013) sampled the world oceans on board a 36 m long schooner, collecting environmental data and organisms from viruses to planktonic metazoans for later analyses using modern sequencing and state-of-the-art imaging technologies. Tara Oceans Data are particularly suited to study the genetic, morphological and functional diversity of plankton. The present data set provides raw validated data of continuous pH measurements made during 2013 expedition with a Satlantic SeaFET instrument that was connected to the flowthrough system. Data calibration was performed according to Bresnahan et al. (2014) (using spectrophotometric pH measurements on discrete samples (Clayton and Byrne 1993). pH_internal values were taken to calibrate the data (rather than pH_external) because of the better calibration coefficient (there was no trend associated with it). The equations of Clayton and Byrne (1993) was used to compute pH from the measured absorbance values at the temperature of measurement. The data was converted to in situ temperature using the “CO2-sys” program (van Heusen et al. 2011).
    Keywords: Fondation Tara Expeditions; FondTara; Tara_Oceans_2009-2013; Tara Oceans Expedition
    Type: Dataset
    Format: application/zip, 843.4 kBytes
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  • 5
    Publication Date: 2024-02-17
    Description: The Tara Oceans Expedition (2009-2013) sampled the world oceans on board a 36 m long schooner, collecting environmental data and organisms from viruses to planktonic metazoans for later analyses using modern sequencing and state-of-the-art imaging technologies. Tara Oceans Data are particularly suited to study the genetic, morphological and functional diversity of plankton. During the entire expedition (2009-2013), underway measurements were obtained from a meteorological station (BATOS), a thermosalinograph (TSG, SBE 45), a Fast Repetition Rate Flurometer (FRRF, LIFT-FRR01), and a spectrophotometer (WETLabs AC-S). In 2013 underway measurements were enhanced by adding a Photosynthetically Available Radiation (PAR) sensor (QCP2350, Biospherical Instruments, Inc.), a laser spectrofluorometer (WETLabs ALFA, Chekalyuk et al., 2012) that replaced the FRRF, a spectral backscattering sensor (WETLabs Eco-bb3), a pCO2 sensor (ProOceanus CO2-Pro), a pH sensor (Satlantic, SeaFET) and a particle imaging system triggered by chlorophyll-a fluorescence (a prototype of McLane Research Laboratories' Imaging FlowCytobot, Sosik Lab, WHOI). Discrete measurements of CDOM absorption measurements were made using an Ultrapath (WPI Inc.) to calibrate the in-line AC-S. Hence the AC-S was also used to provide CDOM absorption in addition to particulate matter properties. The present dataset contains surface water data measured during the 2013 campaigns of the Tara Oceans Expedition. Latitude and Longitude were obtained from TSG data. The time stamp of this data set is harmonised with that of other underway data in this collection.
    Keywords: [CSSS]; [day/night] [surface water layer (ENVO:00002042)]; Aquatic Laser Fluorescence Analyzer (ALFA); Backscattering coefficient of particles, 470 nm; Backscattering coefficient of particles, 526 nm; Backscattering coefficient of particles, 660 nm; Basis of event; Campaign of event; Chlorophyll a; Comment of event; Continuous Surface Sampling System; DATE/TIME; DEPTH, water; Dudinka to Pevek, Stations: TARA_182-192; Event label; Fluorescence, chlorophyll; Fluorescence, colored dissolved organic matter; Fondation Tara Expeditions; FondTara; Fugacity of carbon dioxide (water) at equilibrator temperature (wet air); Ilulissat to Québec, Stations: TARA_208-210; LATITUDE; LONGITUDE; Lorient to Tromsø, Stations: TARA_155-166; Maximum photochemical quantum yield of photosystem II; Method/Device of event; Murmansk to Dudinka, Stations: TARA_167-181; NASA Ocean Biology & Biogeochemistry Programme; OBB; Optional event label; Particle size distribution slope; Particulate organic carbon; Pevek to Tuktoyaktuk, Stations: TARA_193-199; pH; pH sensor, Satlantic SeaFET; Québec to Lorient, Stations: none; registered at PANGAEA, Data Publisher for Earth and Environmental Science; registered at the European Nucleotides Archive (ENA); Salinity; Spectral backscattering sensor (WET Labs, Eco-bb3); Spectrophotometer, WET Labs, Inc., AC-S; Station label; SV Tara; TARA_20130519Z; TARA_20130519Z_UDW_EVENT_CSSS; TARA_20130629Z; TARA_20130629Z_UDW_EVENT_CSSS; TARA_20130801Z; TARA_20130801Z_UDW_EVENT_CSSS; TARA_20130907Z; TARA_20130907Z_UDW_EVENT_CSSS; TARA_20130921Z; TARA_20130921Z_UDW_EVENT_CSSS; TARA_20131020Z; TARA_20131020Z_UDW_EVENT_CSSS; TARA_20131116Z; TARA_20131116Z_UDW_EVENT_CSSS; Tara_Oceans_2009-2013; Tara Oceans Expedition; Temperature, water; Thermosalinograph; TSG; Tuktoyaktuk to Ilulissat, Stations: TARA_200-207; underway pCO2 measuring instrument (ProOceanus CO2-Pro)
    Type: Dataset
    Format: text/tab-separated-values, 345386 data points
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  • 6
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    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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  • 7
    Publication Date: 2024-03-15
    Description: F/S Polarstern cruise ARK-XXVI/3, also known as TransArc (Trans-Arctic survey of the Arctic Ocean in transition). From 5. August (Tromsö) to 7. October (Bremerhaven) a total of 1254 samples were analyzed from 56 stations. Seawater samples were sampled throughout the water column according to Dickson et al. (2007) and analyzed on board within hours. Data quality is discussed. Resulting data is correctable through the use of certified reference material (CRM), after which data is deemed to be of reasonably high quality. All samples and data were sampled, analyzed and processed by Adam Ulfsbo and Ylva Ericson (University of Gothenburg, Sweden).
    Keywords: Alkalinity, total; Aragonite saturation state; Arctic Ocean; ARK-XXVI/3; Bicarbonate ion; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coulometric titration; CTD, SEA-BIRD SBE 911plus, SN T5027-C3290; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; EPOCA; European Project on Ocean Acidification; Event label; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Laptev Sea; Latitude of event; Longitude of event; MULT; Multiple investigations; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Polarstern; Potentiometric open-cell titration; Pressure, water; PS78/201-1; PS78/201-4; PS78/202-1; PS78/203-4; PS78/205-1; PS78/205-4; PS78/207-2; PS78/208-2; PS78/209-2; PS78/209-4; PS78/210-1; PS78/211-2; PS78/212-2; PS78/212-5; PS78/214-1; PS78/216-1; PS78/216-3; PS78/218-2; PS78/218-7; PS78/219-1; PS78/220-1; PS78/220-4; PS78/221-1; PS78/222-2; PS78/222-5; PS78/223-1; PS78/224-1; PS78/225-1; PS78/226-1; PS78/226-3; PS78/227-2; PS78/227-5; PS78/228-1; PS78/229-1; PS78/230-2; PS78/230-5; PS78/232-1; PS78/233-1; PS78/234-1; PS78/235-2; PS78/235-6; PS78/239-2; PS78/239-5; PS78/240-1; PS78/241-1; PS78/242-1; PS78/243-1; PS78/244-1; PS78/245-2; PS78/245-5; PS78/246-1; PS78/247-1; PS78/248-1; PS78/249-1; PS78/250-2; PS78/250-5; PS78/251-1; PS78/252-1; PS78/253-1; PS78/254-1; PS78/257-1; PS78/257-5; PS78/258-1; PS78/259-1; PS78/271-1; PS78/272-2; PS78/272-3; PS78/273-1; PS78/274-1; PS78/276-1; PS78/276-4; PS78/277-1; PS78/278-1; PS78/280-1; PS78/280-4; PS78 TransArc; Salinity; Spectrophotometry; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 18379 data points
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  • 8
    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
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 20 (2001), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: Because of its ice cover the central Arctic Ocean has not been considered as a sink of atmospheric carbon dioxide. With recent observations of decreasing ice cover there is the potential for an increased air–sea carbon dioxide flux. Though the sensitivity of the carbon fluxes to a climate change can at present only be speculated, we know the responses to some of the forcing, including: melting of the sea ice cover make the air–sea flux operate towards equilibrium; increased temperature of the surface water will decrease the solubility and thus the air-sea flux; and an open ocean might increase primary production through better utilization of the nutrients.The potential change in air-sea CO2 fluxes caused by different forcing as a result of climate change is quantified based on measured data. If the sea ice melts, the top 100 m water column of the Eurasian Basin has, with the present conditions, a potential to take up close to 50 g C m−2. The freshening of the surface water caused by a sea ice melt will increase the CO2 solubility corresponding to an uptake of ∼ g C m−2, while a temperature increase of 1°C in the same waters will out-gas 8 g C m−2, and a utilization of all phosphate will increase primary production by 75 g C m−2.
    Type of Medium: Electronic Resource
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  • 10
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