Coral and mollusc resistance to ocean acidification adversely affected by warming

By R. Rodolfo-Metalpa, F. Houlbrèque, É. Tambutté, F. Boisson, C. Baggini, F. Patti, R. Jeffree, M. Fine, A. Foggo, Jean-Pierre Gattuso and 1 more. 2011

512 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/e93f033bdb62924f88efc440acd07dd6d1360940

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Ecology

1. H. Pörtner
2. C. Bock
3. L. Hofmann
4. K. Bischof
5. T. Hirse
6. R. Carpenter
7. Peter J. Edmunds
8. R. Kordas

In Global and Planetary Change

1. H. Pörtner
2. C. Bock
3. R. Crim
4. R. Kordas
5. T. Hirse
6. J. Hall‐Spencer
7. P. Range
8. X. Álvarez‐Salgado

In Oceanography

1. L. Hofmann
2. K. Bischof
3. H. Pörtner
4. S. Comeau
5. J. Hall‐Spencer
6. R. Carpenter
7. Peter J. Edmunds
8. R. Crim

Citations in the corpus

• Fast coral reef calcifiers are more sensitive to ocean acidification in short‐term laboratory incubations (2014, background): “Initial studies reporting bold and uniformly negative effects of OA on reef biota (Kleypas et al. 1999) are giving way to reports of responses that are more nuanced (Rodolfo-Metalpa et al. 2011; Edmunds et al. 2012), and highly variable among taxa (Pandolfi et al. 2011; Comeau et al. 2013b).”
• Tolerance of juvenile Mytilus galloprovincialis to experimental seawater acidification (2012, background): “Oceanic (e.g. upwelling) and continental (e.g. river discharge) processes may lead to a coastal zone with low oxygen waters that are supersaturated with CO2 and have reduced CO32− and pH (Salisbury et al. 2008, Koch & Gobler 2009).”
• Ocean acidification effects on calcifying macroalgae (2014, background): “…determining their sensitivity to low pH, but recent studies have suggested that increased dissolution rates, rather than decreased calcifica - tion rates, are the real threat to calcifying organisms under ocean acidification conditions (Ries 2011b, Rodolfo-Metalpa et al. 2011, Roleda et al. 2012).”
• Impacts of ocean acidification on marine organisms: quantifying sensitivities and interaction with warming (2013, background): “2009), the presence or absence of biogenic coverings that separate calcified material from seawater (e.g., the periostracum in mussels Ries et al., 2009; Rodolfo-Metalpa et al., 2011), or the amount of calcium carbonate in an organism’s shell or skeleton (Kroeker et al.”
• Linking the biological impacts of ocean acidification on oysters to changes in ecosystem services: A review (2017, background): “…  shown that, in oligotrophic conditions, reduced pH levels benefit non-calcified 314   algae, but impairs mollusc larval recruitment and dissolves carbonate habitat 315   (Cigliano et al., 2010; Comeau et al., 2015; Kroeker et al., 2012; Milazzo et al., 316   2014; Rodolfo-Metalpa et al., 2011).”
• Competition between calcifying and noncalcifying temperate marine macroalgae under elevated CO2 levels (2012, background): “Recent research on the consequences of these changes on marine organisms has shown varied responses across multiple taxonomic levels (Fabry 2008, Ries 2009, Kroeker et al. 2010, Fabricius et al. 2011, Rodolfo-Metalpa et al. 2011).”
• Responses of marine benthic microalgae to elevated CO2 (2011, unknown): “…experiments utilising areas that are naturally enriched with CO 2 such as cold-water CO 2 vents (Hall-Spencer et al. 2008; Fabricius et al. 2011; Rodolfo-Metalpa et al. 2011), hydrothermal vents (Couto et al. 2010; Vizzini et al. 2010; Bianchi et al. 2011) and upwelling areas (Thomsen et al.…”
• Impact of ocean acidification and warming on the Mediterranean mussel (Mytilus galloprovincialis) (2014, background): “…in net calcification rates and growth as observed after summer is a consequence of lower pH levels during that period (pH offsets of −0.4 vs. −0.3 during the rest of the experiment) or a consequence of a combined effect of acidification and warming as suggested by Rodolfo-Metalpa et al. (2011).”
• Acidification and warming affect both a calcifying predator and prey, but not their interaction (2012, background): “This shift will eventually lead to reduced population sizes of snails, provided that larger individuals produce higher numbers of offspring, as has been shown for several Littorina species, such as L. rudis (Roberts & Hughes 1980), L. saxatilis (Ross & Berry 1991) and L. neglecta (Johnson 1999).”