Abstract
Changes in the concentrations of CO2 and the calcium budget of the world's oceans are examined with reference to glacial periods. Changes in the concentration of CO2 in the atmosphere may be seen to have a positive reciprocal connection (sustained feedback) with regard to continental glaciations. -translated by P.Cooke
| Original language | English |
|---|---|
| Pages (from-to) | 16-24 |
| Number of pages | 9 |
| Journal | Izvestiya - Akademiya Nauk SSSR, Seriya Geograficheskaya |
| Volume | 6 |
| State | Published - 1987 |
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