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A synthesis可 modern methodological and analytical results begun under IGCP Project 133 (Geochronology of Mesozoic and Cenozoic Deposits of Europe) has been completed with the help of more than 130 geologists and using dates obtained from 40 geochronological laboratories. The result is a recalibration of the Phanerozoic time scale presented here, with many important di厂厂erences厂rom previous schemes. The new ages wil require the reconsideration of many relationships in the fields of sedimentology, palaeontology, and tectonics.

THE PHANEROZOIC TIME SCALE REVISITED