Jacques-Joseph ةbelmen, the founder of earth system science

The fundamental principles of the factors affecting the global carbon cycle, the global sulfur cycle and the levels of atmospheric CO2 and O2 over long-term (multimillion year) time scales were first elucidated by Jacques-Joseph ةbelmen in 1845. He covered all major processes in such a correct manner that no appreciable changes in them have been elucidated since then. Unfortunately, his ideas were forgotten and were independently deduced by others only 100 to 150 years later. In this article, his reasoning is shown in detail, via a number of original quotations, and the results of a mathematical model by the author for CO2 and O2 over the Phanerozoic Eon (past 542 million years) are presented. In agreement with ةbelmenʹs predictions, there apparently have been large changes in the levels of atmospheric CO2 and O2 over geologic time.