“…The large magnitude of change (>35°C), however, is more likely to be indicative of a secondary, burial-related signal, given that the entire stratigraphic section thickens to the west (Peterson & Pipiringos, 1979;Peterson, 1988;Blakey, 2008). If these carbonate rocks are assumed to have all been precipitated in temperate lacustrine environments around 20°C (Kenny, 2015; estimated from chert), and the geothermal gradient within the Navajo basin was consistently ca 30°C km À1 (e.g. Parry et al, 2009), the approximate burial depth of these sites can be estimated based on apparent-equilibrium modelling of the measured clumped isotope temperatures here (e.g.…”