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- W600073905 abstract "The opening of a marine gateway between South America and the Antarctic Peninsula since the Late Eocene to Early Oligocene involved the disruption of the final barrier to the initiation of the Antarctic Circumpolar Current (ACC). The separation of the southern continents increased the thermal isolation of Antarctica and favored the accumulation of extensive ice sheets which reached progressively the shelf edge. The deep water from the Weddell Gyre flows northward into the Scotia Sea through corridors within the South Scotia Ridge and interacts with the ACC, resulting in large contourite waves and drifts. These deposits were largely developed from the Miocene and their distribution and extent highlight the importance of Antarctic deep water production, which in turn may had profound influences on the global circulation system and present climate." @default.
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- W600073905 date "2001-01-01" @default.
- W600073905 modified "2023-10-18" @default.
- W600073905 title "Bottom Deposits In The Central Scotia Sea: The Importance Of The Antarctic Circumpolar Current And The Weddell Gyre Flows" @default.
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- W600073905 doi "https://doi.org/10.3997/2214-4609-pdb.217.367" @default.
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