There is uncertainty regarding the timing and fossil species in which mammalian 5 endothermy arose, with few studies of stem-mammals on key aspects of endothermy such as basal or maximum metabolic rates, or placing them in the context of living vertebrate metabolic ranges. Synchrotron X-ray imaging of incremental tooth cementum shows two Early Jurassic stem-mammals, Morganucodon and Kuehneotherium, had lifespans (a basal metabolic rate proxy) considerably longer than comparably sized living mammals, but similar to reptiles, and 10 that Morganucodon had femoral blood flow rates (a maximum metabolic rate proxy) intermediate between living mammals and reptiles. This shows maximum metabolic rates increased evolutionarily before basal rates, and that contrary to previous suggestions of a Triassic origin, Early Jurassic stem-mammals lacked the endothermic metabolism of living mammals. 15 One Sentence Summary: Surprisingly long lifespans and low femoral blood flow suggest reptile-like physiology in key Early Jurassic stem-mammals. Main Text: Recent discoveries and analyses have revolutionized our knowledge of Mesozoic mammals, revealing novel aspects of their ecology (1, 2) development (3, 4) systematics (2, 4) 20and macroevolution (5,6). However, details of physiology are more difficult to determine from fossils, and our knowledge of physiological evolution remains comparatively poor. Living mammals are endotherms, possessing the ability to control and maintain metabolically produced 3 heat, and have a substantially higher capacity for sustained aerobic activity than ectothermic animals (7-9). The origin of endothermy is an important event in mammalian evolution, often noted as key to their success (7-9). Several competing hypotheses seek to explain the selective pressures and adaptive pathways of endothermic evolution: (a) selection for higher maximum metabolic rates (MMR) enhanced sustained aerobic activity (7, 10, 11); (b) selection for higher 5 basal metabolic rates (BMR) enhanced thermoregulatory control (12, 13); or (c) MMR and BMR evolved in lockstep with each other (8,9).Direct evidence from living mammals to support these hypotheses is equivocal (7).Recent analyses find no long-term evolutionary trend in BMR (14) contradicting earlier suggestions of increasing BMR throughout the Cenozoic (13), and so implying that the Middle 10 Jurassic (~170 Ma) most recent common ancestor (MRCA) of living mammals (14) possessed a BMR within the range of present-day mammals. Several indirect indicators of metabolic physiology in fossil synapsids have been suggested but provide contradictory evidence for the timing of origin of endothermy and its evolutionary tempo. These include: the presence of fibrolamellar long-bone, first seen in the Early Permian (~300 Ma) synapsid Ophiacodon (15); 15the presence of an infraorbital canal and lack of parietal foramen, used to infer facial whiskers, fur, lactation and endothermy in Early Triassic (~245 Ma) cynodonts (16); inferred maxillary nasal turbinates in the Late Permian (~255 Ma) th...