Effects of ocean acidification on different life history stages of northern abalone (Haliotis kamtschatkana)
Anthropogenic atmospheric CO₂ levels are rapidly increasing; however, much of this CO₂ (ca. 30%) dissolves into the surface ocean (upper 200 m) where it reacts with seawater and disrupts both ocean pH and carbonate chemistry, a process termed ocean acidification. Average pH of the surface ocean has...
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| Language: | English |
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University of British Columbia
2010
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| Online Access: | http://hdl.handle.net/2429/29558 |
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