Long-period astronomical forcing of mammal turnover

• Published in: Nature
• Main Authors: van Dam, Jan A., Abdul Aziz, Hayfaa, A'Lvarez Sierra, M. A'Ngeles, J. Hilgen, Frederik, W. van den Hoek Ostende, Lars, J. Lourens, Lucas, Mein, Pierre, J. van Der Meulen, Albert, Pelaez-Campomanes, Pablo
• Other Authors: Department of Earth Sciences Utrecht, Universiteit Utrecht / Utrecht University Utrecht, PaleoEnvironnements et PaleobioSphere (PEPS), Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2006
• Subjects: [SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology; Ice Sheet
• Online Access: https://hal.science/hal-00141414; https://doi.org/10.1038/nature05163

Mammals are among the fastest-radiating groups, being characterized by a mean species lifespan of the order of 2.5 million years (Myr). The basis for this characteristic timescale of origination, extinction and turnover is not well understood. Various studies have invoked climate change to explain mammalian species turnover , but other studies have either challenged or only partly confirmed the climate–turnover hypothesis. Here we use an exceptionally long (24.5–2.5Myr ago), dense, and welldated terrestrial record of rodent lineages from central Spain, and show the existence of turnover cycles with periods of 2.4–2.5 and 1.0Myr. We link these cycles to low-frequency modulations of Milankovitch oscillations, and show that pulses of turnover occur at minima of the 2.37-Myr eccentricity cycle and nodes of the 1.2-Myr obliquity cycle. Because obliquity nodes and eccentricity minima are associated with ice sheet expansion and cooling and affect regional precipitation, we infer that long-period astronomical climate forcing is a major determinant of species turnover in small mammals and probably other groups as well.