Calcification Relative to Calcification at Current pH

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Ivory Bush Coral [Oculina arbuscula]

Statistics  
  Decline in pH from the Present
 
0.0 to 0.09
0.09 to 0.17
0.17 to 0.3
0.3 to 0.5
More than 0.5
Number of Results
2
 
2
 
2
Arithmetic Mean
0.98
 
0.94
 
0.32
Standard Error
0
 
0
 
0

Individual Experiement Results  
      Decline in pH from the Present    

Journal References

Experimental Conditions
0.0
to
0.09
0.09
to
0.17
0.17
to
0.3
0.3
to
0.5
More
than
0.5

Ries et al. (2009)

Calcification rates of coral grown for 60 days under normal and reduced pH conditions. pH was altered by the addition of CO2.
0.98

 

 

 

 

Ries et al. (2009)

Calcification rates of coral grown for 60 days under normal and reduced pH conditions. pH was altered by the addition of CO2.
 

 

0.94

 

 

Ries et al. (2009)

Calcification rates of coral grown for 60 days under normal and reduced pH conditions. pH was altered by the addition of CO2.
 

 

 

 

0.32

Ries et al. (2010)

Calcification rates of the temperate scleractinian coral Oculine arbuscula grown under normal and reduced pH conditions for 60 days. pH was altered by the addition of CO2. Temperature and salinity were held constant at 25°C and 31.7 psu, respectively. Aquaria were illuminated with 10 h/day of 426 W/m2
0.98

 

 

 

 

Ries et al. (2010)

Calcification rates of the temperate scleractinian coral Oculine arbuscula grown under normal and reduced pH conditions for 60 days. pH was altered by the addition of CO2. Temperature and salinity were held constant at 25°C and 31.7 psu, respectively. Aquaria were illuminated with 10 h/day of 426 W/m2
 

 

0.94

 

 

Ries et al. (2010)

Calcification rates of the temperate scleractinian coral Oculine arbuscula grown under normal and reduced pH conditions for 60 days. pH was altered by the addition of CO2. Temperature and salinity were held constant at 25°C and 31.7 psu, respectively. Aquaria were illuminated with 10 h/day of 426 W/m2
 

 

 

 

0.32


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