The influence of diel carbonate chemistry fluctuations on the calcification rate of Acropora cervicornis under present day and future acidification conditions

I. C. Enochs, D. P. Manzello, P. J. Jones, C. Aguilar, K. Cohen, L. Valentino, S. Schopmeyer, G. Kolodziej, M. Jankulak, Diego Lirman

Research output: Contribution to journalArticle

3 Citations (Scopus)

Abstract

Ocean acidification (OA) will result in lower calcification rates for numerous marine taxa, including many species of corals which create important reef habitat. Seawater carbonate chemistry fluctuates over cycles ranging from days to seasons, often driven by biological processes such as respiration and photosynthesis. The magnitude of diel fluctuations varies spatially and may become more pronounced in the future due to OA. Due to technical constraints, OA experiments that incorporate diel variability into treatments are few in number. As a result, the degree to which coral reef organisms are influenced by ambient daily carbonate chemistry variability is poorly understood. Here we describe an experiment conducted in a novel seawater system which can independently manipulate carbonate chemistry in 16 separate aquaria, in real time, allowing precise control of the mean and magnitude of pH oscillations while minimizing pseudoreplication. Five genotypes of the threatened Caribbean coral Acropora cervicornis were subjected to a total of five pH treatments, 7.80 ± 0.20, 7.80 ± 0.10, and 7.80 ± 0.00, as well as 8.05 ± 0.10 and 8.05 ± 0.00. Those corals exposed to variable contemporary conditions (8.05 ± 0.10) calcified faster than those in current and future static treatment levels, which did not significantly differ from each other. Variable contemporary pH also resulted in faster growth rates than highly variable future conditions (7.80 ± 0.20), but were not significantly different than future conditions with the same ±0.10 diel pH oscillation. These findings support the importance of incorporating diel variability into OA experiments and suggest that more variable natural ecosystems may yield higher calcification rates for corals.

Original languageEnglish (US)
Pages (from-to)135-143
Number of pages9
JournalJournal of Experimental Marine Biology and Ecology
Volume506
DOIs
StatePublished - Sep 1 2018

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calcification
acidification
carbonates
corals
coral
chemistry
carbonate
oscillation
seawater
experiment
aquarium
aquariums
biological processes
coral reefs
coral reef
breathing
reefs
photosynthesis
respiration
genotype

Keywords

  • Calcification
  • Coral
  • Diurnal fluctuation
  • Experimental aquaria
  • Ocean acidification
  • pH variability

ASJC Scopus subject areas

  • Ecology, Evolution, Behavior and Systematics
  • Aquatic Science

Cite this

The influence of diel carbonate chemistry fluctuations on the calcification rate of Acropora cervicornis under present day and future acidification conditions. / Enochs, I. C.; Manzello, D. P.; Jones, P. J.; Aguilar, C.; Cohen, K.; Valentino, L.; Schopmeyer, S.; Kolodziej, G.; Jankulak, M.; Lirman, Diego.

In: Journal of Experimental Marine Biology and Ecology, Vol. 506, 01.09.2018, p. 135-143.

Research output: Contribution to journalArticle

Enochs, I. C. ; Manzello, D. P. ; Jones, P. J. ; Aguilar, C. ; Cohen, K. ; Valentino, L. ; Schopmeyer, S. ; Kolodziej, G. ; Jankulak, M. ; Lirman, Diego. / The influence of diel carbonate chemistry fluctuations on the calcification rate of Acropora cervicornis under present day and future acidification conditions. In: Journal of Experimental Marine Biology and Ecology. 2018 ; Vol. 506. pp. 135-143.
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AU - Cohen, K.

AU - Valentino, L.

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AB - Ocean acidification (OA) will result in lower calcification rates for numerous marine taxa, including many species of corals which create important reef habitat. Seawater carbonate chemistry fluctuates over cycles ranging from days to seasons, often driven by biological processes such as respiration and photosynthesis. The magnitude of diel fluctuations varies spatially and may become more pronounced in the future due to OA. Due to technical constraints, OA experiments that incorporate diel variability into treatments are few in number. As a result, the degree to which coral reef organisms are influenced by ambient daily carbonate chemistry variability is poorly understood. Here we describe an experiment conducted in a novel seawater system which can independently manipulate carbonate chemistry in 16 separate aquaria, in real time, allowing precise control of the mean and magnitude of pH oscillations while minimizing pseudoreplication. Five genotypes of the threatened Caribbean coral Acropora cervicornis were subjected to a total of five pH treatments, 7.80 ± 0.20, 7.80 ± 0.10, and 7.80 ± 0.00, as well as 8.05 ± 0.10 and 8.05 ± 0.00. Those corals exposed to variable contemporary conditions (8.05 ± 0.10) calcified faster than those in current and future static treatment levels, which did not significantly differ from each other. Variable contemporary pH also resulted in faster growth rates than highly variable future conditions (7.80 ± 0.20), but were not significantly different than future conditions with the same ±0.10 diel pH oscillation. These findings support the importance of incorporating diel variability into OA experiments and suggest that more variable natural ecosystems may yield higher calcification rates for corals.

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