The Weddell Gyre history from marine sedimentary records
The Weddell Gyre (WG) history is closely related to the formation of the Antarctic Circumpolar Current (ACC), which may have developed after the opening of the Tasman Gateway and Drake Passage between Antarctica and the adjoining continents in the upper Eocene (Huber et al., 2004; Francis et al., 20...
| Main Authors: | , |
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| Format: | Conference Object |
| Language: | unknown |
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Mario Hoppema & Walter Geibert
2012
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| Online Access: | https://epic.awi.de/id/eprint/32484/ https://hdl.handle.net/10013/epic.41095 |