Lithology and Mineral Resources

, Volume 49, Issue 2, pp 117–137 | Cite as

Cenozoic glaciation of Antarctica and sedimentation in the Southern Ocean

  • M. A. Levitan
  • G. L. Leichenkov


Literature pertaining to history of the Cenozoic glaciation in Antarctica and its influence on sedimentation in marginal areas of the continent and deep-water domains of the Southern Ocean are reviewed. Original data obtained by G.L. Leichenkov on seismostratigraphy of the East Antarctica margin are also used. Particular attention is paid to the history of silica accumulation, ice-rafted material deposition, and formation of contourites. The results make it possible to define the following main stages of Antarctic glaciation in the Cenozoic: (1) middle-late Eocene; (2) Oligocene; (3) early Miocene; (4) middle Miocene; (5) late Miocene-early Pliocene; and (6) late Pliocene-Holocene.


Miocene Eocene Oligocene Southern Ocean Middle Miocene 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


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© Pleiades Publishing, Inc. 2014

Authors and Affiliations

  1. 1.Vernadsky Institute of Geochemistry and Analytical ChemistryRussian Academy of SciencesMoscowRussia
  2. 2.All-Russia Research Institute of Geology and Mineral Resources of the World OceanSt. PetersburgRussia

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