2012/05/02 by Richard E. Zeebe · 428 citations
Chemistry · Earth and Planetary Sciences · Environmental Science · #Carbon dioxide #Carbon dioxide in Earth's atmosphere #Carbonate #Carbonate minerals #Chemical oceanography #Chemistry #Climate change #Context (archaeology) #Earth history #Earth science #Environmental science #Geochemistry #Geologic record #Geology #Marine Biology and Ecology Research #Marine Bivalve and Aquaculture Studies #Ocean Acidification Effects and Responses #Ocean acidification #Ocean chemistry #Oceanography #Paleontology #Seawater
paper · doi:10.1146/annurev-earth-042711-105521
published in Annual Review of Earth and Planetary Sciences 40(1), 141-165 (Annual Reviews)
openalex publication_date 2012/05/02 · openalex created_date 2025/10/10 · openalex updated_date 2026/08/04
Humans are continuing to add vast amounts of carbon dioxide (CO 2 ) to the atmosphere through fossil fuel burning and other activities. A large fraction of the CO 2 is taken up by the oceans in a process that lowers ocean pH and carbonate mineral saturation state. This effect has potentially serious consequences for marine life, which are, however, difficult to predict. One approach to address the issue is to study the geologic record, which may provide clues about what the future holds for ocean chemistry and marine organisms. This article reviews basic controls on ocean carbonate chemistry on different timescales and examines past ocean chemistry changes and ocean acidification events during various geologic eras. The results allow evaluation of the current anthropogenic perturbation in the context of Earth's history. It appears that the ocean acidification event that humans are expected to cause is unprecedented in the geologic past, for which sufficiently well-preserved records are available.