The regulation of coralline algal physiology, an in situ study of Corallina officinalis (Corallinales, Rhodophyta)

• Published in: Biogeosciences
• Main Authors: C. J. Williamson, R. Perkins, M. Voller, M. L. Yallop, J. Brodie
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2017
• Subjects: Ecology; QH540-549.5; Life; QH501-531; Geology; QE1-996.5; Ocean acidification
• Online Access: https://doi.org/10.5194/bg-14-4485-2017; https://doaj.org/article/484775e33200449cb309e4db7b5de280

Calcified macroalgae are critical components of marine ecosystems worldwide, but face considerable threat both from climate change (increasing water temperatures) and ocean acidification (decreasing ocean pH and carbonate saturation). It is thus fundamental to constrain the relationships between key abiotic stressors and the physiological processes that govern coralline algal growth and survival. Here we characterize the complex relationships between the abiotic environment of rock pool habitats and the physiology of the geniculate red coralline alga, Corallina officinalis (Corallinales, Rhodophyta). Paired assessment of irradiance, water temperature and carbonate chemistry, with C. officinalis net production ( NP ), respiration ( R ) and net calcification ( NG ) was performed in a south-western UK field site, at multiple temporal scales (seasonal, diurnal and tidal). Strong seasonality was observed in NP and night-time R , with a P max of 22.35 µmol DIC (g DW) −1 h −1 , E k of 300 µmol photons m −2 s −1 and R of 3.29 µmol DIC (g DW) −1 h −1 determined across the complete annual cycle. NP showed a significant exponential relationship with irradiance ( R 2 = 0.67), although was temperature dependent given ambient irradiance > E k for the majority of the annual cycle. Over tidal emersion periods, dynamics in NP highlighted the ability of C. officinalis to acquire inorganic carbon despite significant fluctuations in carbonate chemistry. Across all data, NG was highly predictable ( R 2 = 0.80) by irradiance, water temperature and carbonate chemistry, providing a NG max of 3.94 µmol CaCO 3 (g DW) −1 h −1 and E k of 113 µmol photons m −2 s −1 . Light NG showed strong seasonality and significant coupling to NP ( R 2 = 0.65) as opposed to rock pool water carbonate saturation. In contrast, the direction of dark NG (dissolution vs. precipitation) was strongly related to carbonate saturation, mimicking abiotic precipitation dynamics. Data demonstrated that C. officinalis is adapted to both long-term (seasonal) and ...