Warmer more acidic conditions cause decreased productivity and calcification in subtropical coral reef sediment‐dwelling calcifiers

135 citations recorded by the source corpus.

How researchers see this paper

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

The responses of eight coral reef calcifiers to increasing partial pressure of CO2 do not exhibit a tipping point (2013, background): “Halimeda appears to respond to OA by linearly decreasing calcification as a function of decreasing pH (Sinutok et al. 2011) or as a curvilinear response to Varag (Ries et al. 2009), although some studies have indicated a species-specific response (Price et al. 2011).”
Ocean acidification effects on calcifying macroalgae (2014, background): “In general, the size of aragonite crystals in the skeleton decreases, while crystal density in - creases under pH conditions lower than 7.7 (Robbins et al. 2009, Sinutok et al. 2011).”
Climate change and ocean acidification effects on seagrasses and marine macroalgae (2013, background): “…significantly lowered maximum photosynthetic quantum yield (Fv/Fm-dark adapted) in H. macroloba and H. cylindracea at pH 7.4 at ambient temperature (28 °C) and pH 7.7 and 7.9 at 32 °C, showing a clear pH effect and a negative synergism between pH and high temperature (Sinutok et al., 2011).”