The ocean acidification seascape and its relationship to the performance of calcifying marine invertebrates: Laboratory experiments on the development of urchin larvae framed by…

By P. C. Yu, P. Matson, T. Martz, Gretchen E. Hofmann. 2011

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Interactive effects of elevated temperature and pCO2 on early-life-history stages of the giant kelp Macrocystis pyrifera (2014, background): “These populations are naturally exposed to values of temperature and pH that exceed, in some cases, those predicted to occur in surface oceans at the end of the century (Yu et al., 2011; Gruber et al., 2012; IPCC, 2013).”
Elevated pCO2 causes developmental delay in early larval Pacific oysters, Crassostrea gigas (2013, background): “…respect to aragonite (Kurihara et al. 2007; Miller et al. 2009; Crim et al. 2011; Gazeau et al. 2011; Byrne et al. 2010a, b), although some species are still able to form apparently normal calcified structures in undersaturated conditions (Dupont et al. 2010; Catarino et al. 2011; Yu et al. 2011).”
Appropriate pCO2 treatments in ocean acidification experiments (2013, methodology): “…researchers have incorporated explicit consideration of in situ carbon conditions into species exposure experiments, in some cases, using detailed knowledge of local carbon environments and the microhabitat used by the study species (e.g., Melzner et al. 2011; Thomsen et al. 2010; Yu et al. 2011).”
Adaptation and the physiology of ocean acidification (2013, unknown): “We can therefore make predictions about the likelihood of standing variation for OA resistance in different habitats based on what we know about regional and historical variation in pH, the ‘OA seascape’ (Yu et al. 2011).”