The evolution of Patagonian climate and vegetation from the Mesozoic to the present

By A. Iglesias, A. Artabe, E. Morel. 2011

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A tale of worldwide success: Behind the scenes of Carex (Cyperaceae) biogeography and diversification (2019, background): “…of the last tundra remains there (Lewis et al., 2008), coupled with climate cooling and changes in biota composition in the surrounding lands (Mildenhall, 1980; Iglesias et al., 2011; Pole, 2014) that might have facilitated the establishment and diversi ﬁ cation of new cold ‐ temperate lineages.”
Biogeography and diversification of colletid bees (Hymenoptera: Colletidae): emerging patterns from the southern end of the world (2012, background): “Lower temperatures in the Southern Hemisphere, coupled with colder southern sea currents (in the case of both Australia and South America), were important for cooler continental climates and expansion of xeric environments (Dingle & Lavelle, 1998; Martin, 2006; Iglesias et al., 2011).”
Splendid and Seldom Isolated: The Paleobiogeography of Patagonia (2013, background): “…syntheses (e.g., Bonaparte 1996; Pascual 2006; de la Fuente et al. 2007; Gasparini et al. 2007a,b; Prámparo et al. 2007; Vucetich et al. 2007; Iglesias et al. 2011), there has been no previous attempt to integrate the records of more than one major group of Mesozoic and Cenozoic Patagonian…”