Eocene bipolar glaciation associated with global carbon cycle changes

By A. Tripati, J. Backman, H. Elderfield, P. Ferretti. Nature, 2005

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The origin of the savanna biome (2006, background): “4a, pathway e–g), and the cooler drier climate that results from a weakened atmospheric greenhouse effect (Pagani et al., 2005; Tripati et al., 2005, Fig.”
Slowing down as an early warning signal for abrupt climate change (2008, background): “For instance, 34 million years ago the earth changed suddenly from the tropical state in which it had been for hundreds of millions of years to a state with ice caps, a shift known as the greenhouse–icehouse transition (2, 3) (Fig.”
Evolutionary pathways among shallow and deep-sea echinoids of the genus Sterechinus in the Southern Ocean (2011, background): “After the effective separation of South America from the Antarctic Peninsula, three types of barriers were installed around the Antarctic Continent: geographic, oceanographic and bathymetric (Lawver et al., 1992; Crame, 1999; Clarke and Barnes, 2005; Pfuhl and McCave, 2005; Tripati et al., 2005).”