A physicochemical framework for interpreting the biological calcification response to CO 2 -induced ocean acidification

By J. Ries. 2011

265 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/572b07c2e0851eed5013ab17fb9e398524155172

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. Peter J. Edmunds
2. S. Comeau
3. R. Carpenter
4. N. B. Spindel
5. S. Davies
6. A. Marchetti
7. K. Castillo
8. J. Raven

In Global and Planetary Change

1. Peter J. Edmunds
2. S. Comeau
3. R. Carpenter
4. N. B. Spindel
5. C. Langdon
6. J. Raven
7. K. Crawfurd
8. G. Waldbusser

In Oceanography

1. Peter J. Edmunds
2. R. Carpenter
3. S. Comeau
4. N. B. Spindel
5. C. Langdon
6. A. Marchetti
7. S. Davies
8. J. Ries

Citations in the corpus

• Elevated pCO2 causes developmental delay in early larval Pacific oysters, Crassostrea gigas (2013, background): “If oyster larvae remove a fixed number of H? from their calcifying fluid versus maintaining a fixed ratio of extracellular/intracellular H?, then their energy budget would be more taxed during environmental hypercapnia (Ries 2011).”
• Thermal and pCO2 Stress Elicit Divergent Transcriptomic Responses in a Resilient Coral (2016, background): “…with respect to aragonite) has previously been proposed as a mechanism for coral calcification (Cohen and McConnaughey, 2003), with microelectrode (Ries, 2011), boron isotope (McCulloch et al., 2012), antibody immunolabeling (Barott et al., 2015), and pHsensitive dye studies (Venn et al., 2013)…”
• A developmental and energetic basis linking larval oyster shell formation to acidification sensitivity (2013, background): “Mollusks employ two strategies to overcome the kinetic constraint: (1) use of organic molecules that increase rates of mineral formation [Elhadj et al., 2006] and (2) increase of proton pumping [Ries 2011] to elevate saturation state at the mineral formation sites.”
• Climate change and ocean acidification effects on seagrasses and marine macroalgae (2013, background): “This diversity of Reviewed in: (1) Borowitzka et al. (1974); (2) Borowitzka (1982); (3) Borowitzka (1987); (4) Ries (2011a). aAragonite/Calcite can vary with season in some species. bMgCO3 concentrations can vary with season and Mg : Ca ratios in seawater. cHigh-Mg calcite thalli ~7–30% MgCO3.…”
• Environmental controls on coccolithophore calcification (2012, background): “Ries (2011) also considered energetic constraints on calcification in a high-CO2 environment.”
• The Pacific oyster, Crassostrea gigas, shows negative correlation to naturally elevated carbon dioxide levels: Implications for near‐term ocean acidification effects (2012, background): “However, only a handful of studies have addressed the underlying physiological and ecological mechanisms of these responses to develop a clear and well-founded argument for how other related organisms will respond (Wood et al. 2008; Thomsen et al. 2010; Ries 2011).”
• Fast coral reef calcifiers are more sensitive to ocean acidification in short‐term laboratory incubations (2014, background): “This effect elevates the chemical challenges of transporting H+ away from the calcifying surface, potentially increasing the metabolic costs of calcification (Ries 2011).”