Frequently asked questions about ocean acidification
Cooley, Sarah R.
Mathis, Jeremy T.
Yates, Kimberly K.
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Over the past five years, no other issue has received more attention in the marine science community than ocean acidification. Ocean acidification is a multi-disciplinary research area that encompasses topics such as chemistry, paleontology, biology, ecology, biogeochemistry, modeling, social sciences and economics. With this complexity and the continued development of our understanding in mind, the U.S. Ocean Carbon and Biogeochemistry (OCB; www.us-ocb.org) program, with support from the UK Ocean Acidification Research Programme (UKOA; http://www.oceanacidification.org.uk/), has updated and expanded a list of frequently asked questions (FAQs) that were developed in 2010 by OCB, the European Project on Ocean Acidification (EPOCA), and UKOA. Equipped with the most up-to-date information, the global ocean acidification research community has drafted concise, understandable summaries of the current knowledge. The responses were carefully vetted during an open peer-review and revision process to ensure readability without any loss of scientific accuracy. This effort was international in scale, with 63 scientists from 47 institutions and 12 countries contributing to the process.
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Doney, Scott C.; Balch, William M.; Fabry, Victoria J.; Feely, Richard A. (Oceanography Society, 2009-12)Over a period of less than a decade, ocean acidification—the change in seawater chemistry due to rising atmospheric carbon dioxide (CO2) levels and subsequent impacts on marine life—has become one of the most critical ...
Cooley, Sarah R.; Mathis, Jeremy T. (2012-10-09)Many of the declarations and outcome documents from prior United Nations international meetings address ocean issues such as fishing, pollution, and climate change, but they do not address ocean acidification. This ...
Cooley, Sarah R.; Doney, Scott C. (2009-05)Ocean acidification, a consequence of rising anthropogenic CO2 emissions, is poised to change marine ecosystems profoundly by increasing dissolved CO2 and decreasing ocean pH, carbonate concentration, and calcium carbonate ...