Floral response to rapid warming in the earliest Eocene and implications for concurrent faunal change

By S. Wing, G. Harrington. Paleobiology, 2001

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Mammalian responses to climate change at the Paleocene-Eocene boundary: Polecat Bench record in the northern Bighorn Basin, Wyoming (2003, background): “Parallel studies of sedimentology, paleobotany, and mollusks have been carried out by Kraus (1980, 1987, 1996, 2001), Hickey (1980), Wing (1998), Hartman and Roth (1998), Wing et al. (2000), and Wing and Harrington (2001).”
Long-Term Stasis in Ecological Assemblages: Evidence from the Fossil Record* (2004, methodology): “In the geographically extensive Williston Basin of North Dakota, 143 floras from 106 time slices encompass a 2.2-Myr interval that straddles 183 m of the Cretaceous-Paleogene boundary (Table 1).”
Fossil insect folivory tracks paleotemperature for six million years (2010, background): “…diversity and composition in the Paleocene and Eocene of the Bighorn Basin (Wing et al. 1995, 2000, 2005, Davies-Vollum and Wing 1998, Wing 1998, Wing and Harrington 2001), showing that the sites we investigated are representative of these much larger paleobotanical studies, and, importantly,…”