TY - JOUR
T1 - Similar controls on calcification under ocean acidification across unrelated coral reef taxa
AU - Comeau, Steeve
AU - Cornwall, Christopher E.
AU - DeCarlo, Thomas M.
AU - Krieger, Erik
AU - McCulloch, Malcolm T.
N1 - Funding Information:
B Moore, A‐M Comeau‐Nisumaa, and V Schoepf provided vital laboratory support. MTM was supported by an ARC Laureate Fellowship (LF120100049), S. C. was supported by an ARC DECRA (DE160100668). The authors acknowledge the facilities, and the scientific and technical assistance of the Australian Microscopy & Microanalysis Research Facility at the Centre for Microscopy, Characterisation & Analysis, The University of Western Australia, a facility funded by the University, State and Commonwealth Governments.
Publisher Copyright:
© 2018 John Wiley & Sons Ltd
PY - 2018/10
Y1 - 2018/10
N2 - Ocean acidification (OA) is a major threat to marine ecosystems, particularly coral reefs which are heavily reliant on calcareous species. OA decreases seawater pH and calcium carbonate saturation state (Ω), and increases the concentration of dissolved inorganic carbon (DIC). Intense scientific effort has attempted to determine the mechanisms via which ocean acidification (OA) influences calcification, led by early hypotheses that calcium carbonate saturation state (Ω) is the main driver. We grew corals and coralline algae for 8–21 weeks, under treatments where the seawater parameters Ω, pH, and DIC were manipulated to examine their differential effects on calcification rates and calcifying fluid chemistry (Ωcf, pHcf, and DICcf). Here, using long duration experiments, we provide geochemical evidence that differing physiological controls on carbonate chemistry at the site of calcification, rather than seawater Ω, are the main determinants of calcification. We found that changes in seawater pH and DIC rather than Ω had the greatest effects on calcification and calcifying fluid chemistry, though the effects of seawater carbonate chemistry were limited. Our results demonstrate the capacity of organisms from taxa with vastly different calcification mechanisms to regulate their internal chemistry under extreme chemical conditions. These findings provide an explanation for the resistance of some species to OA, while also demonstrating how changes in seawater DIC and pH under OA influence calcification of key coral reef taxa.
AB - Ocean acidification (OA) is a major threat to marine ecosystems, particularly coral reefs which are heavily reliant on calcareous species. OA decreases seawater pH and calcium carbonate saturation state (Ω), and increases the concentration of dissolved inorganic carbon (DIC). Intense scientific effort has attempted to determine the mechanisms via which ocean acidification (OA) influences calcification, led by early hypotheses that calcium carbonate saturation state (Ω) is the main driver. We grew corals and coralline algae for 8–21 weeks, under treatments where the seawater parameters Ω, pH, and DIC were manipulated to examine their differential effects on calcification rates and calcifying fluid chemistry (Ωcf, pHcf, and DICcf). Here, using long duration experiments, we provide geochemical evidence that differing physiological controls on carbonate chemistry at the site of calcification, rather than seawater Ω, are the main determinants of calcification. We found that changes in seawater pH and DIC rather than Ω had the greatest effects on calcification and calcifying fluid chemistry, though the effects of seawater carbonate chemistry were limited. Our results demonstrate the capacity of organisms from taxa with vastly different calcification mechanisms to regulate their internal chemistry under extreme chemical conditions. These findings provide an explanation for the resistance of some species to OA, while also demonstrating how changes in seawater DIC and pH under OA influence calcification of key coral reef taxa.
KW - calcifying fluid
KW - calcium
KW - coral
KW - coralline alga
KW - dissolved inorganic carbon
KW - pH
KW - physiology
UR - http://www.scopus.com/inward/record.url?scp=85052449926&partnerID=8YFLogxK
U2 - 10.1111/gcb.14379
DO - 10.1111/gcb.14379
M3 - Article
C2 - 29957854
AN - SCOPUS:85052449926
SN - 1354-1013
VL - 24
SP - 4857
EP - 4868
JO - Global change biology
JF - Global change biology
IS - 10
ER -