[Palaeontology, 2020, pp. 1–22] TRACING THE PATTERNS OF NON-MARINE TURTLE RICHNESS FROM THE TRIASSIC TO THE PALAEOGENE: FROM ORIGIN TO GLOBAL SPREAD by TERRI J. CLEARY1,2,5 , ROGER B. J. BENSON3 ,PATRICIAA.HOLROYD4 and PAUL M. BARRETT1,2 1Department of Earth Sciences, Natural History Museum, Cromwell Road, London, SW7 5BD, UK;
[email protected] 2Department of Cell & Developmental Biology, University College London, Gower Street, London, WC1E 6BT, UK 3Department of Earth Sciences, University of Oxford, South Parks Road, Oxford, OX1 3AN, UK 4University of California Museum of Paleontology, 1101 Valley Life Sciences Building, Berkeley, CA 94720, USA 5Current address: School of Geography, Earth & Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK Typescript received 12 September 2019; accepted in revised form 12 March 2020 Abstract: Turtles are key components of modern verte- Palaeogene (Danian). Informative data are lacking elsewhere brate faunas and their diversity and distributions are likely for this time period. However, the Selandian–Thanetian to be affected by anthropogenic climate change. However, interval, approximately 5 myr after the K–Pg mass extinc- there is limited baseline data on turtle taxonomic richness tion, shows low turtle richness in Asia, Europe and South through time or assessment of their past responses to glo- America, suggesting that the occurrence of exceptional tur- bal environmental change. We used the extensive Triassic– tle richness in the post-extinction Paleocene fauna of North Palaeogene (252–223 Ma) fossil record of terrestrial and America is not globally representative. Richness decreased freshwater turtles to investigate diversity patterns, finding over the Eocene–Oligocene boundary in North America but substantial variation in richness through time and between increased to its greatest known level for Europe, implying continents.