Manipulative studies have demonstrated that ocean acidification (OA) is a threat to coral reefs, yet no experiments have employed diurnal variations in pCO2 that are ecologically relevant to many shallow reefs. Two experiments were conducted to test the response of coral recruits (less than 6 days old) to diurnally oscillating pCO2; one exposing recruits for 3 days to ambient (440 uatm), high (663 uatm) and diurnally oscillating pCO2 on a natural phase (420–596 uatm), and another exposing recruits for 6 days to ambient (456 uatm), high (837 uatm) and diurnally oscillating pCO2 on either a natural or a reverse phase (448–845 uatm).
These data are published in Dufault et al. (2012), Proc. R. Soc. B. doi:10.1098/rspb.2011.2545
Related Datasets:
recruit_seawater_chemistry
recruit_growth_area
recruit_suvival
Edmunds, P. J. (2014) Coral recruit growth measured by weight change from calcification during CO2 experiments collected from the Natl Museum Mar. Bio. and Aquar., Taiwan in 2010 (MCR LTER project, Climate_Coral_Larvae project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 2014-03-07) Version Date 2014-04-09 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/506245 [access date]
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