Organic carbon accumulation in coastal zones since the last glacial maximum? A clue for varying atmospheric CO2 levels?
2004
Boski, T. | Veiga-Pires, C. | Moura, Delminda
It is a generally accepted concept that the carbon storage within the principal earth surface reservoirs varies in a multitude of time scales. The shallow water continental margins belong to the most fertile areas in terms of organic carbon (OC) production and are also very effective carbon traps.
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