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The geological record of ocean acidification
Bärbel Hönisch1, Andy Ridgwell, Daniela N Schmidt
1Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA. hoenisch@ldeo.columbia.edu
Summary
The geological record reveals past ocean acidification events and their impact on marine life. However, current CO2 release rates are unprecedented, making future impacts uncertain.
Area of Science:
- Paleontology
- Marine Biology
- Climate Science
Background:
- Ocean acidification poses severe risks to marine ecosystems.
- Laboratory and field studies have limitations in assessing long-term impacts.
- The geological record offers insights into past environmental changes and biotic responses.
Purpose of the Study:
- To review past geological events of ocean acidification and associated environmental changes.
- To compare past events with current projections of ocean acidification.
- To understand the long-term consequences of elevated atmospheric CO2 on marine calcifiers.
Main Methods:
- Review of geological records spanning the past 300 million years.
- Analysis of evidence for elevated atmospheric CO2, global warming, and ocean acidification.
- Examination of contemporaneous extinction and evolutionary turnover events.
Main Results:
- Several past geological events show evidence of increased atmospheric CO2, warming, and ocean acidification.
- Some of these events coincided with marine calcifier extinctions and evolutionary changes.
- No past event perfectly matches the projected speed and scale of current CO2-driven ocean chemistry disruption.
Conclusions:
- Past geological events provide valuable context for understanding ocean acidification.
- The current rate of CO2 release is unparalleled in Earth's history.
- Future impacts on marine carbonate chemistry and ecosystems may be more severe than previously understood.
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