Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/134398
Title: Variations of polyphenols and carbohydrates of Emiliania huxleyi grown under simulated ocean acidification conditions
Authors: Rico Santos, Milagros 
Santiago Díaz, Paula 
Samperio Ramos,Guillermo 
González-Dávila, Melchor 
Santana Casiano, Juana Magdalena 
UNESCO Clasification: 251001 Oceanografía biológica
251002 Oceanografía química
241707 Algología (ficología)
Keywords: Phaeodactylum-Tricornutum
Biochemical-Composition
Southern-Ocean
Climate-Change
Trace-Metals, et al
Issue Date: 2024
Project: Respuesta Del Fe en Un Océano Acidificado 
Journal: Biogeosciences 
Abstract: Cultures of the coccolithophore Emiliania huxleyi were grown under four different CO2-controlled pH conditions (7.75, 7.90, 8.10, and 8.25) to explore variations in extra- and intracellular polyphenols and carbohydrates in response to different ocean acidification scenarios. Acidification did not significantly affect final cell densities and carbohydrate contents. Intra- and extracellular phenolic compounds were identified and quantified by reverse-phase high-performance liquid chromatography (RP-HPLC), with the highest concentrations of total exuded phenolics at a pH of 8.25 (43 ± 3 nM) and 7.75 (18.0 ± 0.9 nM). Accumulation of intracellular phenolic compounds was observed in cells with decreasing pH, reaching the maximum level (9.24 ± 0.19 attomole per cell) at the lowest pH (7.75). The phenolic profiles presented significant changes in exuded epicatechin and protocatechuic acid (p < 0.05 and 0.01, respectively) and intracellular vanillic acid (p < 0.001), which play an essential role in the availability of trace metals. A significant increase in chlorophyll a content was observed in cells grown at the most acidic pH (p < 0.01), which also showed significantly higher radical inhibition activity (p < 0.01). The nature and concentration of these organic compounds present in the culture medium may influence trace metal bioavailability, affecting the biogeochemical cycling of carbon and microbial functional diversity.
URI: http://hdl.handle.net/10553/134398
ISSN: 1726-4189
DOI: 10.5194/bg-21-4381-2024
Source: Biogeosciences [ISSN 1726-4189], v. 21, n. 19, p. 4381–4394
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