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      Reconstructing Ocean pH with Boron Isotopes in Foraminifera

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      Annual Review of Earth and Planetary Sciences
      Annual Reviews

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          The geological record of ocean acidification.

          Ocean acidification may have severe consequences for marine ecosystems; however, assessing its future impact is difficult because laboratory experiments and field observations are limited by their reduced ecologic complexity and sample period, respectively. In contrast, the geological record contains long-term evidence for a variety of global environmental perturbations, including ocean acidification plus their associated biotic responses. We review events exhibiting evidence for elevated atmospheric CO(2), global warming, and ocean acidification over the past ~300 million years of Earth's history, some with contemporaneous extinction or evolutionary turnover among marine calcifiers. Although similarities exist, no past event perfectly parallels future projections in terms of disrupting the balance of ocean carbonate chemistry-a consequence of the unprecedented rapidity of CO(2) release currently taking place.
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            Thermodynamics of the dissociation of boric acid in synthetic seawater from 273.15 to 318.15 K

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              Coral resilience to ocean acidification and global warming through pH up-regulation

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                Author and article information

                Journal
                Annual Review of Earth and Planetary Sciences
                Annu. Rev. Earth Planet. Sci.
                Annual Reviews
                0084-6597
                1545-4495
                June 29 2016
                June 29 2016
                : 44
                : 1
                : 207-237
                Article
                10.1146/annurev-earth-060115-012226
                18ae41cc-3376-4653-85e9-cc63dea2c8cc
                © 2016
                History

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