Abstract
Ongoing ocean acidification (OA) is rapidly altering carbonate chemistry in the oceans. The projected changes will likely have deleterious consequences for coral reefs by negatively affecting their growth. Nonetheless, diverse responses of reef-building corals calcification to OA hinder our ability to decipher reef susceptibility to elevated pCO2. Some of the inconsistencies between studies originate in measuring net calcification (NC), which does not always consider the proportions of the "real" (gross) calcification (GC) and gross dissolution in the observed response. Here we show that microcolonies of Stylophora pistillata (entirely covered by tissue), incubated under normal (8.2) and reduced (7.6) pH conditions for 16 months, survived and added new skeletal CaCO3, despite low (1.25) Ωarg conditions. Moreover, corals maintained their NC and GC rates under reduced (7.6) pH conditions and displayed positive NC rates at the low-end (7.3) pH treatment while bare coral skeleton underwen
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Cohen, S., & Fine, M. (2012). Measuring gross and net calcification of a reef coral under ocean acidification conditions: methodological considerations. Biogeosciences Discussions, 9(7), 8241–8272. Retrieved from http://www.biogeosciences-discuss.net/9/8241/2012/%5Cnhttp://libproxy.mit.edu/login?url=http://search.ebscohost.com/login.aspx?direct=true&db=edb&AN=79551738&site=eds-live
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