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Catastrophic chemical events in the history of the ocean William T. Holser
Max-Planck-Institut für Chemie, D−6500 Mainz, Germany (BRD) Department of Geology, University of Oregon, Eugene, Oregon 97403
Catastrophic chemical events are characterised by sharp rises in 34S in the surface of the whole world ocean, and by greater overshoots locally. Three events are recognised and named for the formation in which they are most sharply displayed. The sharpness of the rise in 34S suggests that the sulphide deposition necessary to explain it must have been accumulating residual high- 34S seawater for some tens of millions of years out of contact with the surface ocean. A modified geological model is presented: brine generated by evaporite deposition is stored in deeps of a mediterranean basin; underneath the brine, pyrite precipitation builds a store of brine heavy in 34Sso4, whose corresponding buildup of 38Oso4 may balance the decrease of 38Oso4 from evaporite deposition. Catastrophic mixing of the brine and the surface ocean, initiated by destruction of the storing basin, is the source of the sharp rise in the sulphur isotope age curve detected world-wide in evaporites. These events have important implications not only for modelling of the chemical history of the ocean, atmosphere, and sediments, but also for the explanation of faunal crises, and the many aspects of geology that depend on the composition and circulation of the oceans and their peripheral basins.
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