Carbon isotopic fractionation by plankton in the Southern Indian Ocean: relationship between δ of particulate organic carbon and dissolved carbon dioxide

1998 ◽  
Vol 17 (1-4) ◽  
pp. 39-58 ◽  
Author(s):  
I. Bentaleb ◽  
M. Fontugne ◽  
C. Descolas-Gros ◽  
C. Girardin ◽  
A. Mariotti ◽  
...  
1976 ◽  
Vol 54 (16) ◽  
pp. 2577-2580 ◽  
Author(s):  
Robert H. Betts ◽  
Wayne D. Buchannon

The formation of carbon dioxide by photolysis of aqueous solutions of ferric oxalate is accompanied by carbon isotopic fractionation. 12C appears preferentially in the evolved CO2, but the isotope effect depends markedly on the wavelength of the light used. Fractionation is essentially zero (k12/k13 = 1.001) at 366 nm, and increases with wavelength, reaching 1.050 at 520 nm. It is proposed that this variation of isotopic discrimination arises from the differing properties of the excited levels formed by photochemical activation.


1975 ◽  
Vol 10 (1) ◽  
pp. 33-41 ◽  
Author(s):  
J. Butcher ◽  
M. Boyer ◽  
CD. Fowle

Abstract Eleven small ponds, lined with polyethylene, were used to assess the consequences of applications of *DursbanR at 0.004, 0.030, 0.100 and 1.000 ppm and AbateR at 0.025 and 0.100 ppm active ingredient. The treated ponds showed a more pronounced long-term increase in pH and dissolved oxygen and decreasing total and dissolved carbon dioxide in comparison with untreated ponds. Algal blooms were of longer duration in treated ponds than in controls. Total photosynthetic productivity was higher in treated ponds but bacterial numbers did not change significantly. Photosynthetic productivity was estimated by following the changes in total carbon dioxide.


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