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- W105156686 abstract "ABSTRACT On the probable assumption that the Louann Salt mass extends beneath the Gulf of Mexico basin, its volume is calculated at about 4 million km3. When such an amount of salt is added to the volume of present ocean water, along with that of other post-Louann Salt masses of Africa and the Middle East, the oceanic waters of the close of the Paleozoic are found to be at least 20% saltier than those of the present. The evidence of extinction of many forms of marine life at the close of the Paleozoic probably reflects their inability to survive in such salty waters, but it also suggests that such saltiness was not typical of Paleozoic seas and was a consequence of Permian climatic and weathering conditions. The extraction and accumulation of the Louann Salt mass required prolonged continuance of evaporating conditions. The extensive occurence of aeolian sandstones in North America, South America, Africa, Antarctica, Australia, and Europe in the Triassic systems of these continents indicates that desert and semi-arid regions were probably far more extensive then than now, and that highly evaporative winds related thereto were the agencies effecting the return to normal oceanic salinity as the Louann Salt was deposited. In turn, surviving stocks were able to proliferate and fill the Jurassic seas. It is probable that these conditions also exercised significant control in accumulation of such non-metallic deposits as phosphates, uranium, potash, sulfur, and bauxite. End_of_Record - Last_Page 49--------" @default.
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- W105156686 date "1968-01-01" @default.
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- W105156686 title "Abstract: Paleoclimatologic and Paleobiologic Implications of Louann Salt Deposition" @default.
- W105156686 hasPublicationYear "1968" @default.
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