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• W2039697920 abstract "Abstract The 13 C: 12 C ratio of benthic foraminiferal calcite preserves the indications of the 13 C: 12 C ratio of the total dissolved CO 2 and can be used as a tracer of the residence time of the oceanic deep water. The tracer is applied to the reconstruction of the deep-water exchanges between the Atlantic and Pacific oceans, from middle Miocene times (15 × 10 6 y ago) to the Pliocene. Results from two Atlantic DSDP sites are compared with results from another Atlantic and three Pacific sites. The present pattern of thermohaline circulation was initiated 13.2 × 10 6 y ago, when the Scotland-Faeroe-Iceland-Greenland Ridge was sufficiently subsided to allow Arctic Bottom Water (ABW) to overflow the ridge. During the Messinian the salt deficiency due to the closure of the Mediterranean Sea caused all deep-water formation in the northern hemisphere to stop; the present deep circulation started again in the North Atlantic when the Mediterranean reopened at the beginning of the Pliocene, but deep-water formation did not resume in the North Pacific because the transfer of deep, saline water from the Atlantic was hindered by the shoaling of the Balboa Sill." @default.
• W2039697920 created "2016-06-24" @default.
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• W2039697920 date "1982-12-01" @default.
• W2039697920 modified "2023-10-05" @default.
• W2039697920 title "The deep-water circulation during the Neogene and the impact of the Messinian salinity crisis" @default.
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• W2039697920 doi "https://doi.org/10.1016/0198-0149(82)90033-4" @default.
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