
The San Juan Basin, New Mexico. Photo credit: Daniel J. Peppe
Asteroids, as Neil deGrasse Tyson explains, are ancient remnants from our early solar system, wandering through space, potential bearers of life’s ingredients or agents of apocalyptic death.
In 1980, in a landmark lecture, U.S. physicist Luis Alvarez declared, “Lucifer’s Hammer killed the dinosaurs,” presenting the geochemical evidence he and his son had uncovered for a colossal asteroid strike at the end of the Cretaceous period. The following year, the Mexican oil company Pemex identified the Chicxulub crater on the Yucatán Peninsula as the site of this massive asteroid impact. The impact released an estimated energy equivalent of 100 teratonnes of TNT. Three-quarters of the plant and animal species on Earth disappeared, including non-avian dinosaurs, pterosaurs, marine reptiles, ammonites, and planktonic foraminifera.

Paleogeography of North America during the late Campanian Stage of the Late Cretaceous (∼75 Ma). From Sampson et al., 2010
In recent decades, there has been a heated debate over whether the dinosaurs were in decline or whether they continued to thrive until they were abruptly wiped out by the asteroid impact, the main pulse of the K/Pg extinction. This controversy is worsened by a geographical bias, as most data comes from the Northern Hemisphere. The Naashoibito Member (San Juan Basin, New Mexico) provides a crucial piece of this puzzle, capturing a snapshot of the continent’s final dinosaur communities and their diversity at the Cretaceous boundary.
The emplacement of the Western Interior Seaway (about 99.5 Mya) split the North American continent into two separate landmasses: Laramidia (a long, narrow landmass from present-day Alaska to Mexico) and Appalachia (the eastern part of the continent). During the Campanian (83.6–72.1 million years ago), Laramidia had a high regional diversity, with distinct northern and southern faunas. In the Maastrichtian (72.1–66.0 Ma), those ecosystems became more uniform. The “homogenization” of those ecosystems could have pushed non-avian dinosaurs into a prolonged decline, setting the stage for their eventual extinction. A new study provides a new look at the last-surviving dinosaur-dominated ecosystems by presenting a revised geochronology of the Naashoibito Member (contemporaneous with the Hell Creek faunas) to test whether there were changes in faunal provinciality during the Cretaceous-Paleogene boundary.

Latest Cretaceous–early Paleogene terrestrial basins in western North America and their faunas. From Flynn et al., 2025
Ecological analysis shows that the Naashoibito dinosaurs were highly diverse, spanning many species, body sizes, and diets. This diversity matches that of earlier periods and suggests that dinosaurs continued to thrive in New Mexico until the Cretaceous-Paleogene boundary. The new study further indicates that temperature was a key factor of dinosaur distribution, with sauropods dominating warmer environments (southwestern North America), and hadrosaurines dominating the cooler temperate regions (modern Great Plains). These results emphasise the importance of abiotic factors in promoting heterogeneity in dinosaur-dominated ecosystems prior to the Cretaceous–Paleogene extinction event.
References:
Flynn, A. G., Brusatte, S. L., Chiarenza, A. A., García-Girón, J., Davis, A. J., Fenley, C. W., Leslie, C. E., Secord, R., Shelley, S., Weil, A., Heizler, M. T., Williamson, T. E., & Peppe, D. J. (2025). Late-surviving New Mexican dinosaurs illuminate high end-Cretaceous diversity and provinciality. Science, 390(6771), 400–404. https://doi.org/10.1126/science.adw3282
Dean, C. D., Chiarenza, A. A., Doser, J. W., Farnsworth, A., Jones, L. A., Lyster, S. J., Outhwaite, C. L., Valdes, P. J., Butler, R. J., & Mannion, P. D. (2025). The structure of the end-Cretaceous dinosaur fossil record in North America. Current Biology: CB. https://doi.org/10.1016/j.cub.2025.03.025
Sampson SD, Loewen MA, Farke AA, Roberts EM, Forster CA, Smith JA, et al. (2010) New Horned Dinosaurs from Utah Provide Evidence for Intracontinental Dinosaur Endemism. PLoS ONE 5(9): e12292. https://doi.org/10.1371/journal.pone.0012292