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- W256424178 abstract "An interval of high variable, enriched benthic /sup 18/O values was found to bracket the Miocene/Pliocene boundary, between 5.6 and 5.1 Ma, in five sites from the Southwest Pacific and Atlantic Oceans. The duration of this enrichment event was less than 500,000 years, and is shown by paleomagnetic correlation to be equivalent in time with the deposition of Messinian evaporites. The /sup 18/O enrichment occurred in two main stages separated by a brief interval of relatively depleted /sup 18/O values. Between 5.5 and 5.3 Ma, glacioeustatic lowering of sea level due to increased Antarctic ice volume isolated the Mediterranean basin, and resulted in the deposition of the lower evaporite unit (Main Salt unit). A temporary decrease in ice volume occurred between 5.3 and 5.2 Ma, and corresponded to the intra-Messinian transgression where evaporite deposition ceased temporarily. Between 5.2 and 5.1 Ma, a second Antarctic glacial advance lowered sea level again and resulted in the deposition of the upper evaporite unit. A rapid decreased in delta/sup 18/O values occurred in all sites during the early Pliocene at 5.0 Ma. This depletion marks a glacial retreat and marine transgression, which refilled the Mediterranean Basin and permanently terminated evaporite deposition." @default.
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- W256424178 date "1985-01-01" @default.
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- W256424178 title "Relationship among latest Miocene oxygen isotopic enrichment, antarctic ice volume, and the Messinian salinity crisis" @default.
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