The effects of secular calcium and magnesium concentration changes on the thermodynamics of seawater acid/base chemistry: Implications for Eocene and Cretaceous ocean carbon chemistry and buffering

• Published in: Global biogeochemical cycles 2015-05, Vol.29 (5), p.517-533
• Main Authors: Hain, Mathis P., Sigman, Daniel M., Higgins, John A., Haug, Gerald H.
• Format: Article
• Language: English
• Subjects: acidification; Calcium; Carbon; carbon chemistry; Carbon cycle; Carbon dioxide; Cenozoic; Chemistry; Cretaceous; Dissolved inorganic carbon; Eocene; ion pairing; Magnesium; Marine; Photosynthesis; Seawater; seawater buffering; seawater calcium; Thermodynamics
• ISSN: 0886-6236; 1944-9224
• DOI: 10.1002/2014GB004986

Reconstructed changes in seawater calcium and magnesium concentration ([Ca2+], [Mg2+]) predictably affect the ocean's acid/base and carbon chemistry. Yet inaccurate formulations of chemical equilibrium “constants” are currently in use to account for these changes. Here we develop an efficient implementation of the MIAMI Ionic Interaction Model to predict all chemical equilibrium constants required for carbon chemistry calculations under variable [Ca2+] and [Mg2+]. We investigate the impact of [Ca2+] and [Mg2+] on the relationships among the ocean's pH, CO2, dissolved inorganic carbon (DIC), saturation state of CaCO3 (Ω), and buffer capacity. Increasing [Ca2+] and/or [Mg2+] enhances “ion pairing,” which increases seawater buffering by increasing the concentration ratio of total to “free” (uncomplexed) carbonate ion. An increase in [Ca2+], however, also causes a decline in carbonate ion to maintain a given Ω, thereby overwhelming the ion pairing effect and decreasing seawater buffering. Given the reconstructions of Eocene [Ca2+] and [Mg2+] ([Ca2+]~20 mM; [Mg2+]~30 mM), Eocene seawater would have required essentially the same DIC as today to simultaneously explain a similar‐to‐modern Ω and the estimated Eocene atmospheric CO2 of ~1000 ppm. During the Cretaceous, at ~4 times modern [Ca2+], ocean buffering would have been at a minimum. Overall, during times of high seawater [Ca2+], CaCO3 saturation, pH, and atmospheric CO2 were more susceptible to perturbations of the global carbon cycle. For example, given both Eocene and Cretaceous seawater [Ca2+] and [Mg2+], a doubling of atmospheric CO2 would require less carbon addition to the ocean/atmosphere system than under modern seawater composition. Moreover, increasing seawater buffering since the Cretaceous may have been a driver of evolution by raising energetic demands of biologically controlled calcification and CO2 concentration mechanisms that aid photosynthesis. Key Points At 1000 ppm CO2 and modern Ω, Eocene ocean had modern DIC and low pH of 7.65 For given Ω, [Mg] increase slightly raises and [Ca] strongly lowers buffering Cenozoic [Ca] decline drives evolution and stabilizes climate against CO2 release