A case is made that in the absence of an effective feedback control on
the rate of delivery of CaO to the oceans, the CO2 content of the Ear
th's atmosphere would have wandered over a large range threatening lif
e either by overheating or by carbon dioxide starvation. In this paper
, we defend the suggestion by Walker er al. [1981] that control is exe
rted by the interaction between the CO2 content of the atmosphere and
the continental weathering rates. We contend that in spite of the argu
ments raised against it [Raymo and Ruddiman, 1992; Edmond and Huh, 199
7] the CO2-chemical weathering feedback is the dominant mechanism that
stabilizes the atmospheric carbon dioxide content.