Abstract
The reconnection, with the world ocean, of temporarily isolated ocean basins results in injection either of hyper-saline waters favouring abyssal stratification and stagnation, or of brackish Waters from high latitudes leading to a low salinity surface layer. Mass extinctions and sudden climatic change are closely associated with Arctic injection.
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Thierstein, H., Berger, W. Injection events in ocean history. Nature 276, 461–466 (1978). https://doi.org/10.1038/276461a0
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DOI: https://doi.org/10.1038/276461a0
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