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• W2093142430 endingPage "84" @default.
• W2093142430 startingPage "57" @default.
• W2093142430 abstract "Measurements of the δ13C of total dissolved inorganic carbon (ΣCO2) in the world oceans are presented. Most of the samples are from the GEOSECS expeditions which covered the Atlantic, Pacific, and Indian oceans between 1971 and 1978. The results from 2252 samples from 107 hydrographic stations are presented as north-south vertical (depth) sections with δ13C contoured at intervals of 0.1%. The data show that the distribution of δ13C is controlled mainly by the input of organically produced material and its subsequent oxidation as it falls through the water column. This covariance can be summarized by the regression equation: δ13C=1.5−0.0075·AOU, where AOU represents the oxygen utilization within a water sample after leaving the surface. Other factors influencing the distribution of δ13C are the dissolution of inorganic carbonate and the addition of anthropogenic CO2 to the oceans. A complex mathematical model was employed to estimate the levels of ΣCO2 and δ13C in pre-industrial oceanic surface waters. The results suggest that the ΣCO2 of surface waters has increased by 40 μmole kg−1 from a pre-industrial level of approximately 2135 μmole kg−1. The δ13C of the ΣCO2 has decreased by 0.5% from a pre-industrial value of approximately 2.5%." @default.
• W2093142430 created "2016-06-24" @default.
• W2093142430 creator A5041317559 @default.
• W2093142430 date "1985-01-01" @default.
• W2093142430 modified "2023-10-10" @default.
• W2093142430 title "The distribution of 13C of ΣCO2 in the world oceans" @default.
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• W2093142430 doi "https://doi.org/10.1016/0198-0149(85)90017-2" @default.
• W2093142430 hasPublicationYear "1985" @default.
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