Effects of a Shallow-Water Hydrothermal Vent Gradient on Benthic Calcifiers, Tutum Bay, Ambitle Island, Papua New Guinea
Ocean acidification is occurring in response to rapidly increasing concentrations of atmospheric CO2. Shallow-water hydrothermal vent systems have been proposed as natural laboratories for studying the effects of elevated pCO2 on benthic communities. Hydrothermal vents occur at depths of approximate...
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Scholar Commons
2010
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Online Access: | http://scholarcommons.usf.edu/etd/3553 http://scholarcommons.usf.edu/cgi/viewcontent.cgi?article=4771&context=etd |