The age of the Drake Passage

• Published in: Alcheringa: An Australasian Journal of Palaeontology
• Main Author: Boltovskoy, Esteban
• Format: Article in Journal/Newspaper
• Language: English
• Published: Taylor & Francis 1980
• Subjects: Antarctic; Austral; Drake Passage; Pacific; Antarc*
• Online Access: https://oceanrep.geomar.de/id/eprint/33535/; https://oceanrep.geomar.de/id/eprint/33535/1/DrakePassage.pdf; https://doi.org/10.1080/03115518008558973

The distribution of benthic foraminifera in Miocene deposits of the continental margin of southeastern South America is compared with that in the Recent. The comparison indicates that Miocene zoogeographic boundaries were located in higher latitudes than at present, suggesting that the climate at that time was warmer than now. In the Pliocene, temperatures were lower than at present. This signifies that a considerable decrease in water temperature took place in the latest Miocene or at the Miocene/Pliocene boundary in the southwestern Atlantic. The main reason for this drop in temperature was the opening of the Drake Passage and the establishment of the Circumpolar Antarctic Current and a branch — the Malvin Current. The opening resulted from strong orogenic movements, in the latest Miocene, which created the main part of the Andes. Prior to the opening of the passage, the anticyclonic (counterclockwise) gyre of surface currents in the South Atlantic was much larger and warm Brazilian waters reached higher latitudes. The Austral Strait, connecting the Pacific and Atlantic Oceans, may have existed from the Cretaceous in the southern part of South America, but its location and character did not permit the establishment of the true Circumpolar Antarctic Current. The Austral Strait was closed simultaneously with the opening of the Drake Passage.