8 citations as recorded by crossref.

1. Absence of a strong, deep-reaching Antarctic Circumpolar Current zonal flow across the Tasmanian gateway during the Oligocene to early Miocene D. Evangelinos et al. 10.1016/j.gloplacha.2021.103718
2. Climatic and tectonic drivers of late Oligocene Antarctic ice volume B. Duncan et al. 10.1038/s41561-022-01025-x
3. Gateway-driven weakening of ocean gyres leads to Southern Ocean cooling I. Sauermilch et al. 10.1038/s41467-021-26658-1
4. Strength and variability of the Oligocene Southern Ocean surface temperature gradient F. Hoem et al. 10.1038/s43247-022-00666-5
5. Eocene to Oligocene vegetation and climate in the Tasmanian Gateway region were controlled by changes in ocean currents and <i>p</i>CO<sub>2</sub> M. Amoo et al. 10.5194/cp-18-525-2022
6. An expanded database of Southern Hemisphere surface sediment dinoflagellate cyst assemblages and their oceanographic affinities L. Thöle et al. 10.5194/jm-42-35-2023
7. Late Eocene–early Miocene evolution of the southern Australian subtropical front: a marine palynological approach F. Hoem et al. 10.5194/jm-40-175-2021
8. Temperate Oligocene surface ocean conditions offshore of Cape Adare, Ross Sea, Antarctica F. Hoem et al. 10.5194/cp-17-1423-2021