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PANGAEA.
Data Publisher for Earth & Environmental Science
Abstract:
Seawater was sampled from five depths in the euphotic zone corresponding to 100 % (ca. 3 m depth), 50 %, 20 %, 7 % and 1 % of incident Photosynthetically Active Radiation (PAR). For each depth, four 72 mL polystyrene bottles (three clear bottles and one dark bottle) were filled with unfiltered seawater, inoculated with 10 - 20 µCi NaH¹⁴CO₃ and incubated on-deck from dawn to dusk. Temperature and irradiance in the incubators simulated the water temperature and the incident irradiance at the corresponding depth of each sample by using a combination of neutral density and blue filters (Mist Blue, ref. 061, Lee Filters ®). After incubation, samples from three of the five depths (100 %, 20 % and 1 % PAR) were sequentially filtered through 20, 2 and 0.2 µm polycarbonate filters while the other depths (50 % and 7 % PAR) were directly filtered by 0.2 µm. Immediately after filtering, filters were then exposed to concentrated HCl fumes at least 12 h to remove the non-fixed inorganic ¹⁴C. Filters were placed in scintillation vials to which 5 mL of liquid scintillation cocktail was added. The radioactivity on each filter (disintegrations per minute, DPM) was determined using a Wallac scintillation counter. To compute the rate of photosynthetic carbon fixation, the dark-bottle DPM was subtracted from the light-bottle DPM values. A constant value of 24,720 µg L-1 (or 2,060 µmol L-1) was assumed for the concentration of dissolved inorganic carbon for surface waters in tropical ocean (Key et al., 2004). A correction factor of 1.05 was applied to this constant value for discrimination isotopic. Total primary production was calculated as the sum of the primary production on each size class.
Keyword(s):
CSIC; primary production; subtropical gyres
Project(s):
Funding:
Ministerio de Ciencia e Innovación (MICINN), grant/award no. CSD2008-00077: Circumnavigation expedition Malaspina 2010: Global Change and Exploration of Biodiversity of the Global Ocean
Coverage:
Median Latitude: -6.124516 * Median Longitude: -34.203952 * South-bound Latitude: -40.550000 * West-bound Longitude: -178.210000 * North-bound Latitude: 32.910000 * East-bound Longitude: 142.500000
Date/Time Start: 2010-12-22T00:00:00 * Date/Time End: 2011-07-11T00:00:00
Minimum DEPTH, water: m * Maximum DEPTH, water: 160 m
Event(s):
MALASPINA_LEG1_006-3 (MH008_006) * Latitude: 23.270000 * Longitude: -22.220000 * Date/Time: 2010-12-22T00:00:00 * Campaign: MALASPINA_LEG1 (29HE20101215) * Basis: Hespérides * Method/Device: CTD/Rosette (CTD-RO)
MALASPINA_LEG1_007-3 (MH009_007) * Latitude: 21.450000 * Longitude: -23.450000 * Date/Time: 2010-12-23T00:00:00 * Campaign: MALASPINA_LEG1 (29HE20101215) * Basis: Hespérides * Method/Device: CTD/Rosette (CTD-RO)
MALASPINA_LEG1_008-3 (MH010_008) * Latitude: 20.260000 * Longitude: -24.250000 * Date/Time: 2010-12-24T00:00:00 * Campaign: MALASPINA_LEG1 (29HE20101215) * Basis: Hespérides * Method/Device: CTD/Rosette (CTD-RO)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventRegaudie-de-Gioux, Aurore
2Latitude of eventLatitudeRegaudie-de-Gioux, Aurore
3Longitude of eventLongitudeRegaudie-de-Gioux, Aurore
4Date/Time of eventDate/TimeRegaudie-de-Gioux, Aurore
5DEPTH, waterDepth watermRegaudie-de-Gioux, AuroreGeocode
6Primary production of carbon per hourPP Cmg/m3/hRegaudie-de-Gioux, Auroresee abstract
7Primary production of carbon, standard deviationPP C std dev±Regaudie-de-Gioux, Auroresee abstractmg/m³/h
Size:
1241 data points

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