Diel and seasonal vertical migrations of zooplankton represent a widespread phenomenon occurring in marine and freshwater environments. Diel migrations are panoceanic, while seasonal migrations usually occur in temperate and polar areas. This paper describes differences in the diel and seasonal vertical migrations in the Drake passage north and south of the polar front (pf). We analyzed material of 85 stations collected in spring of 2008 and 2010 (October-November) and in summer of 2010 and 2011 (January) within the 0-300 m depth range during various time of a day. At each station we sampled the upper mixed (UL), the middle (ML), and the deeper layers (DL) bounded by hydrological gradients. Diel migrations were significantly different south and north of the PF in terms of total abundance, biomass, diversity and individual taxa density. in both seasons, mesoplankton dielly migrated between the ML/DL and the UL north of the PF and between layers below 300 m and the DL and ML south of the pf. Deeper range of diel migrations south of the pf was coupled with a general mesoplankton descent in summer period compared to spring. conversely, north of the pf, mesoplankton ascended to upper layers in summer, which was mirrored in lesser depths of diel migrations. The differences in the plankton distribution on both sides of the PF are likely associated with variations of vertical distribution of phytoplankton. Some abundant taxa such as Aetideus sp. and Oithona plumifera showed both common (nighttime ascend) and inverted (nighttime descend) vertical migrations depending on season and position related to the pf. Diel and seasonal vertical migrations of zooplankton represent a well-known phenomenon observed for many species 1,2. Adaptive significance of the migrations is mainly linked to feeding, predator-avoiding and/or reproductive behavior 2-9. The amplitude of diel vertical migrations ranges from a few to hundreds of meters 2,9,10. Most migrating zooplankton species ascent at night ("normal" migration pattern); however, a reversed movement (nighttime descent, inverted migrations) is known for some species 2,5,9,11. There are also more complicated migrations with a double ascent at sunset and after midnight with a short intermediate descent to deeper waters at midnight 7,8,12. In addition, different stages of the same species may have different migration patterns, as shown for Oithona and Oncaea copepods 13. Diel migrations of mesoplankton are believed to be caused by the predator evasion during daytime and by feeding during nighttime 3,14-16. Seasonal migrations of zooplankton to the surface waters for feeding and reproduction take place in temperate and polar areas, and are usually driven by phytoplankton bloom 16. In autumn and winter, when the phytoplankton production is low, most species descend to deeper layers. In the Southern Ocean, phytoplankton spring and summer blooms occur in a rather thin upper mixed water layer < 100 m 17 , which results in an extensive ascent of the zooplankton to the upper waters with maximu...