Evidence for a major extinction of insect herbivores is provided by presence-absence data for 51 plant-insect associations on 13,441 fossil plant specimens, spanning the Cretaceous͞Paleogene boundary in southwestern North Dakota. The most specialized associations, which were diverse and abundant during the latest Cretaceous, almost disappeared at the boundary and failed to recover in younger strata even while generalized associations regained their Cretaceous abundances. These results are consistent with a sudden ecological perturbation that precipitated a diversity bottleneck for insects and plants.O ne of the most scrutinized events in the history of life is the Cretaceous-Paleogene (K͞T) mass extinction at 65.51 Ϯ 0.3 million years before present (1, 2). This event has been linked to the impact of an extraterrestrial object (3) on the Yucatán Peninsula of Mexico (4) that resulted in the losses of numerous lineages within such disparate animal groups as pelagic vertebrates, dinosaurs, mammals, foraminifera, and marine and freshwater mollusks (5-11). Paleobotanical evidence indicates a drastic decline of seed plants in the Western Interior of North America, seen in both the megafloral and palynofloral records (11)(12)(13)(14)(15)(16)(17).Several quantitative studies at the family level indicate that the diversity of insects suffered no decrease beyond normal levels of background extinction at the K͞T boundary (18)(19)(20). The extinction resistance of insect families is probably attributable to the high diversity of their constituent species and the spatiotemporal plasticity of their geographic ranges, resulting in exceptional longevity in the fossil record (19,21). Although few studies exist below the family level, the demise of Late Cretaceous aphidioid, beetle, and ant genera (20,22,23) provides some evidence for extinctions. Establishing a comprehensive test for the presence or absence of an insect extinction has been hindered by the worldwide lack of appropriate, local deposits that span the K͞T boundary and contain well-preserved, diverse, and sufficiently abundant insect faunas (24). The deposits that come closest to meeting these criteria are: Canadian amber of the upper Campanian Foremost Formation, occurring approximately 10 million years before the K͞T boundary (20); and the Fur Formation, a Danish unit that brackets the Paleocene to Eocene boundary and contains an assemblage of insect compression fossils from approximately 11 million years after the event (25). Even if more suitable deposits are found, taxonomic occurrence data are inherently limited for addressing the ecological aspects of extinction (26).Here, we use an explicitly ecological approach that takes advantage of insect-damaged fossil plants (ref. 27; Fig. 1), which document the trophic associations between plants and their insect herbivores, the latter estimated as approximately half of all extant insect species (28). This approach also allows us to investigate a possible insect extinction at the K͞T boundary by using a high sample siz...