Supplementary Materials for Reptile-like physiology in Early Jurassic stem-mammals Authors: Elis Newham1*, Pamela G. Gill2,3*, Philippa Brewer3, Michael J. Benton2, Vincent Fernandez4,5, Neil J. Gostling6, David Haberthür7, Jukka Jernvall8, Tuomas Kankanpää9, Aki Kallonen10, Charles Navarro2, Alexandra Pacureanu5, Berit Zeller-Plumhoff11, Kelly Richards12, Kate Robson-Brown13, Philipp Schneider14, Heikki Suhonen10, Paul Tafforeau5, Katherine Williams14, & Ian J. Corfe8*. Correspondence to:
[email protected];
[email protected];
[email protected] This PDF file includes: Materials and Methods Supplementary Text Figs. S1 to S5 Tables S1 to S5 1 Materials and Methods Choice of fossil specimens. All Morganucodon and Kuehneotherium specimens are from the Early Jurassic St Brides Island fissure suite, from Glamorgan, South Wales, UK (1, 44). The two genera co-existed on a small landmass during the Early Jurassic marine transgression (Hettangian-early Sinemurian, ~200 Ma) (45). Thousands of their bones and teeth were washed into karst fissures that have subsequently been revealed by quarrying. The Morganucodon and Kuehneotherium specimens used for cementum analysis are from the Natural History Museum, London, UK (NHMUK) and Morganucodon femora specimens from the University Museum of Zoology, Cambridge, UK (UMZC). Morganucodon specimens are Morganucodon watsoni from Pontalun 3 fissure in Pontalun quarry (now Lithalun), excavated in 1962-1963 (44, 45). Kuehneotherium specimens are from three Glamorgan fissures in Pontalun and Pant quarries; Pontalun 3, Pant 2 and Pant 4. Although the Pant 2 Kuehneotherium collection is more extensive, teeth are poorly mineralized and so produced relatively fewer usable increment counts. Pontalun 3 and Pant 2 fissures have a relatively impoverished fauna, and Pant 4 has a more diverse biota (45).