The effect of carbonate chemistry on calcification and photosynthesis in the hermatypic coral Acropora eurystoma

By K. Schneider, J. Erez. 2006

359 citations recorded by the source corpus.

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Citations in the corpus

Effects of acidified seawater on early life stages of scleractinian corals (Genus Acropora) (2009, background): “Previous studies have demonstrated that acidified seawater has negative effects on adult growth of Acropora species [9, 28], but the detailed effects of increased CO2 on early life stages of this genus remain unknown (but see [12, 16]).”
Bioassays, batch culture and chemostat experimentation, Approaches and tools to manipulate the carbonate chemistry (2010, background): “The situation is clearer in reef-building corals as Schneider & Erez (2006) measured the rate of calcifi cation under constant DIC, constant pH and constant p(CO2) and showed that calcifi cation is controlled by the concentration of € CO3 2− , the future value of which is relatively well mimicked…”
The effects of exposure to near-future levels of ocean acidification on shell characteristics of Pinctada fucata (Bivalvia: Pteriidae) (2010, background): “Dissolution of calcareous structures and reduced calcification rates have been documented in many marine invertebrates, including scleractinian corals (Gattuso et al. 1998; Marubini et al. 2001; Schneider and Erez 2006; Anthony et al. 2008; Ries et al. 2009), coccolithophores (Sciandra et al.”
Interactive effects of ocean acidification and temperature on two scleractinian corals from Moorea, French Polynesia (2012, background): “…unresolved relationships among light, the Symbiodinium symbionts, photosynthesis, and the capacity to calcify rapidly (Allemand et al., 2004, 2011), as well as which DIC spe- cies (i.e., HCO3 vs. CO3 2 ) is favored for calcification (Schneider & Erez, 2006; Jury et al., 2009; Herfort et al., 2008).”
Living in the now: physiological mechanisms to tolerate a rapidly changing environment. (2010, background): “Mechanistically, the decline in calcification is linked to the acidification-driven decrease in carbonate concentrations and not to the effects of seawater acidification on symbiont photosynthesis (84, 85).”
Nutritional status and metabolism of the coral Stylophora subseriata along a eutrophication gradient in Spermonde Archipelago (Indonesia) (2011, methodology): “The calcification rate was determined in the light (GL) and in the dark (GD) using the alkalinity anomaly method as described by Schneider and Erez (2006).”
Response of the temperate coral Cladocora caespitosa to mid- and long-term exposure to p CO 2 and temperature levels projected for the year 2100 AD (2010, background): “Photosynthesis does not seem to be greatly affected by ocean acidification in symbiotic corals (e.g. Langdon et al., 2003; Reynaud et al., 2003; Schneider and Erez, 2006), probably because corals do not rely on dissolved CO2 for photosynthesis (Gattuso et al.”
A corrosive concoction: The combined effects of ocean warming and acidification on the early growth of a stony coral are multiplicative (2011, background): “Although several advances have been made in understanding the individual effects of increased seawater temperature or ocean acidification on coral physiology (e.g. Dove and Hoegh-Guldberg, 2006; Schneider and Erez, 2006), the potential cumulative effects of both remain unexplored, especially on the ”
Possible effects of ocean acidification on coral reef biogeochemistry: topics for research (2008, background): “Even though calcification observed under light is greater than that under dark conditions (reviewed by Gattuso et al. 1999), the relationship between calcification and Ω appears to have a similar slope in both the light and the dark (Ohde & Hossain 2004, Schneider & Erez 2006).”
Combined effects of ocean acidification and solar UV radiation on photosynthesis, growth, pigmentation and calcification of the coralline alga Corallina sessilis (Rhodophyta) (2009, background): “Nevertheless, calcifying organisms in coastal waters have to tolerate and cope with the chemical changes in the carbonate system as ocean acidification advances (Schneider & Erez, 2006).”
Ocean acidification causes bleaching and productivity loss in coral reef builders (2008, background): “Also, the study by Schneider and Erez (2006) (23) found no effect of CO2 dosing on rates of photosynthesis and respiration, but similar to Reynaud et al. (2003) (22) used an experimental irradiance of only 350 mol photons m 2 s 1.”
Effect of pH on Gene Expression and Thermal Tolerance of Early Life History Stages of Red Abalone (Haliotis rufescens) (2010, background): “…(Shirayama &Thornton 2005, Kurihara 2008, Clark et al. 2009, Todgham& Hofmann 2009), corals (Marubini & Thake 1999, Langdon & Atkinson 2005, Schneider & Erez 2006, Hoegh-Guldberg et al. 2007, Herfort et al. 2008, Marubini et al. 2008), coralline algae (Kuffner et al. 2008) and molluscs…”
The impact of seawater saturation state and bicarbonate ion concentration on calcification by new recruits of two Atlantic corals (2011, background): “In several other studies, coral calcification rates were observed to be positively correlated with increased [HCO3 ] (Marubini and Thake 1999; Schneider and Erez 2006; Marubini et al. 2008).”
Long-term effects of nutrient and CO2 enrichment on the temperate coral Astrangia poculata (Ellis and Solander, 1786) (2010, neutral): “…2001, r= Langdon et al., 2003, s =Marubini et al., 2003, t =Ohde and Hossain, 2004 dark, u=Ohde and Hossain, 2004 light, v= Langdon and Atkinson, 2005, w= Schneider and Erez, 2006, x= Schneider and Erez, 2006 dark, y=Herfort et al., 2008 Acropora sp. dark, z =Herfort et al., 2008 Acropora sp.…”
Assessing the potential long-term increase of oceanic fossil fuel CO 2 uptake due to CO 2 -calcification feedback (2007, positive): “The ﬁlled grey circle represents the year 2100 prediction of the ocean GCM of Heinze (2004), which assumed the calciﬁcation sensitivity of Emiliania huxleyi (Zondervan et al., 2001) (indicated by the vertical dotted white line) and no feedbacks with climate (and calculated at a comparable…”
Changes in morphology and diet of the coral Stylophora pistillata along a depth gradient (2009, background): “Additionally, the presence of zooxanthellae enhances the propagation of corals through the light-enhanced calcification phenomenon (Goreau & Goreau 1959, Muscatine et al. 2005, Schneider & Erez 2006).”
Coral calcification responds to seawater acidification: a working hypothesis towards a physiological mechanism (2008, methodology): “The lack of pH effect on photosynthesis was also observed by Goiran et al. (1996) and more recently by Schneider and Erez (2006).”