By contrast, in August, nitrogen tissue content for A1FI-grown algae was significantly lower than under all other treatments (two-way factorial buy Talazoparib ANOVA, F(3,16) = 5.8, P = 0.007). For tissue phosphorus content, a significant Scenario × Time interaction was found (three-way factorial

ANOVA, F(3,32) = 3.5, P = 0.03). Algae grown in August, with the exception of the A1FI scenario, had significantly higher phosphorus content than algae grown in November. In November, PD and A1FI scenario-grown algae had lower phosphorus content, than found under PI or B1 scenarios. A significant interaction for Time × Nutrients was also detected for phosphorus tissue content. The interaction was driven by the fact that nutrient enrichment in August led to higher tissue concentrations of phosphorus than those

observed under ambient nutrient doses in August or either nutrient levels in November (three-way factorial ANOVA, F(3,32) = 19, P < 0.0001). Tissue phosphorus occurred at its lowest value in November under ambient nutrient doses. In the present study, the response of the brown alga C. implexa to predicted changes in ocean temperature and acidification was explored. The future growth rate of C. implexa was found to be either unchanged, or significantly reduced from present, depending on whether the experiment was performed in the spring month of November or in the winter month of August. Significantly, the results further suggested that optimal growth conditions for this mat-forming alga occurred in the PI past, countering suggestions that algae will “bloom” in the future (e.g., Hoegh-Guldberg et al. 2007, Hughes et al. 2010). Therefore, it seems that not all macroalgal Selleckchem Epigenetics Compound Library species have similar responses to ocean acidification and warming. Other studies have investigated the effects of acidification CYTH4 on brown algal growth and have come to opposing conclusions. For example, Diaz-Pulido et al. (2011) found that A1FI-like acidification levels led to decreased growth in Lobophora papenfussii, while

Israel and Hophy (2002) found no effect on Sargassum vulgare. It is not clear whether the different responses are species specific or associated with different, but undefined background temperatures, nutrient, and light conditions. Our data, however, suggest that limited or no differential responses between A1FI and present-day are derived because growth has already been significantly impacted since PI times. In the present study, C. implexa, experienced slight reductions in growth in winter under the dual impact of future A1FI warming and acidification. The data suggest, that prior to industrialization, C. implexa potentially exhibited much greater seasonal dynamics than it does today, potentially flourishing in November and hence at a time when its impact on coral recruitment may be at its greatest (Babcock et al. 1986). Clearly, further experiments need to be conducted at more time points and nested within seasons to gather a more accurate picture.