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  • OceanRep  (4)
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  • 1
    Publication Date: 2024-02-02
    Keywords: Ammonium; Bacteria; Bacteria, biomass as carbon; Calculated; Carbon, organic, particulate; Carbon/nitrogen analyser (GF/F filtered); Carbon biomass estimation (unspec.); Chlorophyll a; Chlorophyll a, fluorometric determination (Grasshoff et al., 1983, Chemie GmbH); Coccolithophoridae, biomass as carbon; Colorometric analysis, manual; Continuous Flow Automated Analysis (Gordon et al., 1993, WOCE Tech Rpt 93-1); CTD; CTD/Rosette; CTD-RO; Cyanobacteria; Cyanobacteria, biomass as carbon; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Diatoms, biomass as carbon; Dinoflagellates, biomass as carbon; Elevation of event; Epifluorescence microscopy; Event label; Flagellates, heterotrophic and autotrophic, biomass as carbon; JGOFS; Joint Global Ocean Flux Study; Latitude of event; Longitude of event; M10/2; M10/2-CTD-427_224; M10/2-CTD-430_225; M10/2-CTD-432_226; M10/2-CTD-435_227; M10/2-CTD-435_228; M10/2-CTD-435_229; M10/2-CTD-435_230; M10/2-CTD-435_231; M10/2-CTD-435_232; M10/2-CTD-436_233; M10/2-CTD-437_234; M10/2-CTD-437_235; M10/2-CTD-437_236; M10/2-CTD-438_237; M10/2-CTD-440_239; M10/2-CTD-443_240; M10/2-CTD-445_242; M10/2-CTD-448_243; M10/2-CTD-450_244; M10/2-CTD-453_245; M10/2-CTD-455_246; M10/2-CTD-455_247; M10/2-CTD-455_248; M10/2-CTD-458_249; M10/2-CTD-460_250; M10/2-CTD-460_251; M10/2-CTD-463_252; M10/2-CTD-465_253; M10/2-CTD-465_254; M10/2-CTD-465_255; M10/2-CTD-468_256; M10/2-CTD-470_257; M10/2-CTD-470_258; M10/2-CTD-473_259; M10/2-CTD-473_513; M10/2-CTD-475_261; M10/2-CTD-475_262; M10/2-CTD-478_263; M10/2-CTD-480_264; M10/2-CTD-480_265; M10/2-CTD-480_266; M10/2-CTD-483_267; M10/2-CTD-484_268; M10/2-CTD-485_269; M10/2-CTD-485_270; M10/2-CTD-488_271; M10/2-CTD-490_272; M10/2-CTD-490_273; M10/2-CTD-490_274; M10/2-CTD-493_275; M10/2-CTD-495_276; M10/2-CTD-495_277; M10/2-CTD-499_278; M10/2-CTD-499_279; M10/2-CTD-500_280; M10/2-CTD-501_281; M10/2-CTD-502_282; M10/2-CTD-503_283; M10/2-CTD-504_284; M10/2-CTD-505_285; M10/2-CTD-506_286; M10/2-CTD-507_287; M10/2-CTD-518_288; M10/2-CTD-519_289; M10/2-CTD-550_290; M10/2-CTD-551_291; M10/2-CTD-552_292; M10/2-CTD-553_293; M10/2-CTD-554_294; M10/2-CTD-555_295; M10/2-CTD-556_296; M10/2-CTD-557_297; M10/2-CTD-558_298; M10/2-CTD-559_299; M10/2-CTD-560_300; M10/2-CTD-561_301; M10/2-CTD-562_302; M10/2-CTD-563_303; M10/2-CTD-564_304; M10/2-CTD-564_305; M10/2-CTD-567_306; M10/2-CTD-569_307; M10/2-CTD-569_308; M10/2-CTD-569_309; M10/2-CTD-572_310; M10/2-CTD-574_311; M10/2-CTD-575_312; M10/2-CTD-576_313; M10/2-CTD-579_314; M10/2-CTD-581_319; M10/2-CTD-581_320; M10/2-CTD-584_321; M10/2-CTD-586_324; M10/2-CTD-586_325; M10/2-CTD-589_326; M10/2-CTD-591_327; M10/2-CTD-591_331; M10/2-CTD-591_333; M10/2-CTD-594_334; M10/2-CTD-596_335; M10/2-CTD-596_338; M10/2-CTD-596_341; M10/2-CTD-599_342; M10/2-CTD-601_343; M10/2-CTD-601_344; M10/2-CTD-601_345; M10/2-CTD-604_346; M10/2-CTD-606_347; M10/2-CTD-606_348; M10/2-CTD-609_349; M10/2-CTD-611_350; M10/2-CTD-611_351; M10/2-CTD-611_352; M10/2-CTD-614_353; M10/2-CTD-616_354; M10/2-CTD-616_355; M10/2-CTD-624_361; Meteor (1986); NABE; Nitrate and Nitrite; Nitrite; Nitrogen, organic, particulate; North Atlantic Bloom Experiment, 1989-1991; Oxidation (alkaline) with borate buffered potassium persulphate; Oxygen; Oxygen, Winkler (Culberson, 1991, WOCE Report 68/91); Phosphate; Pressure, water; Salinity; Silicate; Silicoflagellates, biomass as carbon; Silicon, particulate; Temperature, water; Thymidine incorporation; Thymidine uptake rate
    Type: Dataset
    Format: text/tab-separated-values, 11166 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-02-02
    Keywords: Bottle, Niskin 30-L; Carbon, organic, particulate; Carbon/nitrogen analyser (GF/F filtered); Chlorophyll a; Counting 250-2000 µm fraction; Date/Time of event; DEPTH, water; Elevation of event; Event label; JGOFS; Joint Global Ocean Flux Study; Latitude of event; Longitude of event; M10/2; M10/2-RO6-427_076; M10/2-RO6-432_079; M10/2-RO6-437_081; M10/2-RO6-440_083; M10/2-RO6-445_086; M10/2-RO6-450_089; M10/2-RO6-455_091; M10/2-RO6-460_096; M10/2-RO6-465_098; M10/2-RO6-470_100; M10/2-RO6-475_103; M10/2-RO6-480_105; M10/2-RO6-485_106; M10/2-RO6-490_107; M10/2-RO6-495_109; M10/2-RO6-564_111; M10/2-RO6-569_113; M10/2-RO6-574_115; M10/2-RO6-581_117; M10/2-RO6-586_119; M10/2-RO6-591_121; M10/2-RO6-596_123; M10/2-RO6-601_125; M10/2-RO6-606_127; M10/2-RO6-611_129; M10/2-RO6-616_131; Meteor (1986); NABE; NIS_30L; Nitrogen, organic, particulate; North Atlantic Bloom Experiment, 1989-1991; Oxidation; then autoanalysis (GF/F filtered); Oxidation (alkaline) with borate buffered potassium persulphate; Phosphorus, particulate; Silicon, particulate
    Type: Dataset
    Format: text/tab-separated-values, 878 data points
    Location Call Number Limitation Availability
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  • 3
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    Elsevier
    In:  Deep Sea Research Part II: Topical Studies in Oceanography, 40 (1-2). pp. 91-114.
    Publication Date: 2018-03-05
    Description: An overview is given of the multinational investigations carried out at 47°N 20°W for the period 24 April–31 May, with the main emphasis on the succession of plankton communities and the flux of organic carbon through various plankton components. The depth of the upper mixed layer decreased rapidly after 25 April, triggering the start of the spring bloom that developed within a 2-week period. Chlorophyll a stocks integrated to 80 m water depth reached peak concentrations during the first 10 days in May. The observed decline was partly due to the seasonal development, but also may have been influenced by changes in water masses associated with a cyclonic eddy. Primary production ranged from 50 to 150 mmol C m−2 day−1 with highest values in the first half of May. After the first bloom phase, dominated by diatoms, nanophytoplankton gained more importance as primary producers when silicate was depleted. Stocks of bacteria, microzooplankton and mesozooplankton increased in the second half of May. Bacterial production averaged 30% of primary production and probably metabolized a large amount of dissolved organic carbon (DOC) per day, but due to uncertain carbon conversion efficiencies total bacterial carbon consumption is difficult to estimate. Largely daily changes in the DOC standing stock could not be reconciled with the measured primmary production and are probably an expression of spatial rather than temporal variations. Microzooplankton was found to consume around 64% of primary production in the second half of May. Grazing estimates for mesozooplankton varied but seem to be small (〈5% of primary production) for most of the investigation period. The small mesozooplankton size classes (〈1 mm) dominated biomass and grazing. Vertical particulate organnic carbon (POC) flux measured by sediment traps in 150 m depth was around 9.8 mmol C m−2 day−1 representing approximately 11% of primary production. The spring bloom pulse of particle flux reached the deep ocean and benthos 4–6 weeks after the surface water peak.
    Type: Article , PeerReviewed
    Format: text
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  • 4
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    In:  (PhD/ Doctoral thesis), Christian-Albrechts-Universität Kiel, Kiel, Germany, 126 pp
    Publication Date: 2018-04-27
    Type: Thesis , NonPeerReviewed
    Format: text
    Location Call Number Limitation Availability
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  • 5
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    In:  (Diploma thesis), Christian-Albrechts-Universität, Kiel, Kiel, Germany, 97 pp
    Publication Date: 2020-03-20
    Type: Thesis , NonPeerReviewed
    Format: text
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  • 6
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    Institut für Meereskunde Kiel
    In:  (PhD/ Doctoral thesis), Christian-Albrechts-Universität Kiel, Kiel, Germany, 125 pp . Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel, 152 . DOI 10.3289/IFM_BER_152 〈http://dx.doi.org/10.3289/IFM_BER_152〉.
    Publication Date: 2013-07-25
    Type: Thesis , NonPeerReviewed
    Format: text
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