Seawater carbonate chemistry and calcification during tropical reef studies at Moorea (French Polynesia), 1997


Autoria(s): Gattuso, Jean-Pierre; Payri, Claude E; Pichon, Michel; Delesalle, Bruno; Frankignoulle, Michel
Cobertura

DATE/TIME START: 1992-07-16T00:13:00 * DATE/TIME END: 1992-07-16T22:54:00 * MINIMUM DEPTH, water: 0 m * MAXIMUM DEPTH, water: 1 m

Data(s)

05/06/1997

Resumo

Community metabolism and air-sea carbon dioxide (CO2) fluxes were investigated in July 1992 on a fringing reef at Moorea (French Polynesia). The benthic community was dominated by macroalgae (85% substratum cover) and comprised of Phaeophyceae Padina tenuis (Bory), Turbinaria ornata (Turner) J. Agardh, and Hydroclathrus clathratus Bory (Howe); Chlorophyta Halimeda incrassata f. ovata J. Agardh (Howe); and Ventricaria ventricosa J. Agardh (Olsen et West), as well as several Rhodophyta (Actinotrichia fragilis Forskál (Børgesen) and several species of encrusting coralline algae). Algal biomass was 171 g dry weight/m**2. Community gross production (Pg), respiration (R), and net calcification (G) were measured in an open-top enclosure. Pg and R were respectively 248 and 240 mmol Co2/m**2/d, and there was a slight net dissolution of CaCO3 (0.8 mmol/m**2/d). This site was a sink for atmospheric CO2 (10 ± 4 mmol CO2/m**2/d), and the analysis of data from the literature suggests that this is a general feature of algal-dominated reefs. Measurement of air-sea CO2 fluxes in open water close to the enclosure demonstrated that changes in small-scale hydrodynamics can lead to misleading conclusions. Net CO2 evasion to the atmosphere was measured on the fringing reef due to changes in the current pattern that drove water from the barrier reef (a C02 source) to the study site.

Formato

text/tab-separated-values, 320 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.717469

doi:10.1594/PANGAEA.717469

Idioma(s)

en

Publicador

PANGAEA

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Fonte

Supplement to: Gattuso, Jean-Pierre; Payri, Claude E; Pichon, Michel; Delesalle, Bruno; Frankignoulle, Michel (1997): Primary production, calcification, and air-sea CO2 fluxes of a macroalgal-dominated coral reef community (Moorea, French Polynesia). Journal of Phycology, 33(5), 729-738, doi:10.1111/j.0022-3646.1997.00729.x

Palavras-Chave #Alkalinity, total; Alkalinity anomaly technique (Smith and Key, 1975); Aragonite saturation state; Bicarbonate ion; Calcification rate of calcium carbonate; Calcite saturation state; Calculated; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbon dioxide; DATE/TIME; DEPTH, water; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gattuso_etal_97; LICOR quantameter (LI-COR LI-192SA); Moorea (French Polynesia); OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Radiation, photosynthetically active; Salinity; Temperature, water; Titration potentiometric
Tipo

Dataset