Primary production using ¹⁴C method in subtropical gyres regions

DOI

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.

Supplement to: Regaudie-de-Gioux, Aurore; Huete-Ortega, Maria; Sobrino, Cristina; López-Sandoval, Daffne C; González, N; Fernández-Carrera, Ana; Vidal, Montserrat; Marañón, Emilio; Cermeño, Pedro; Latasa, Mikel; Agustí, Susana; Duarte, Carlos Manuel (2019): Multi-model remote sensing assessment of primary production in the subtropical gyres. Journal of Marine Systems, 196, 97-106

Identifier
DOI https://doi.org/10.1594/PANGAEA.899853
Related Identifier https://doi.org/10.1016/j.jmarsys.2019.03.007
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.899853
Provenance
Creator Regaudie-de-Gioux, Aurore ORCID logo; Huete-Ortega, Maria ORCID logo; Sobrino, Cristina ORCID logo; López-Sandoval, Daffne C ORCID logo; González, Natalia ORCID logo; Fernández-Carrera, Ana ORCID logo; Vidal, Montserrat ORCID logo; Marañón, Emilio ORCID logo; Cermeño, Pedro ORCID logo; Latasa, Mikel ORCID logo; Agustí, Susana ORCID logo; Duarte, Carlos ORCID logo
Publisher PANGAEA
Publication Year 2019
Funding Reference Ministerio de Ciencia e Innovación https://doi.org/10.13039/501100004837 Crossref Funder ID CSD2008-00077 Circumnavigation expedition Malaspina 2010: Global Change and Exploration of Biodiversity of the Global Ocean
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 1241 data points
Discipline Earth System Research
Spatial Coverage (-178.210W, -40.550S, 142.500E, 32.910N)
Temporal Coverage Begin 2010-12-22T00:00:00Z
Temporal Coverage End 2011-07-11T00:00:00Z