Abstract Aetosauria is a clade of obligately quadrupedal, heavily armoured pseudosuchians known from Upper Triassic (late Carnian–Rhaetian) strata on every modern continent except Australia and Antarctica. As many as 22 genera and 26 species ranging from 1 to 6 m in length, and with a body mass ranging from less than 10 to more than 500 kg, are known. Aetosauroides scagliai was recently recovered as the most basal aetosaur, placed outside of Stagonolepididae (the last common ancestor of Desmatosuchus and Aetosaurus ). Interrelationships among the basal aetosaurs are not well understood but two clades with relatively apomorphic armour – the spinose Desmatosuchinae and the generally wide-bodied Typothoracisinae – are consistently recognized. Paramedian and lateral osteoderms are often distinctive at the generic level but variation within the carapace is not well understood in many taxa, warranting caution in assigning isolated osteoderms to specific taxa. The aetosaur skull and dentition varies across taxa, and there is increasing evidence that at least some aetosaurs relied on invertebrates and/or small vertebrates as a food source. Histological evidence indicates that, after an initial period of rapid growth, lines of arrested growth (LAGs) are common and later growth was relatively slow. The common and widespread Late Triassic ichnogenus Brachychirotherium probably represents the track of an aetosaur.

Abstract Apateon , a small temnospondyl from the Permian freshwater-lake deposits of the Saar-Nahe Basin (SW Germany), is known by exceptionally well-preserved material. Here we report the first palaeohistological analysis of Apateon that focuses on its life-history traits and palaeoenvironments. Different samples (different localities and horizons) of Apateon caducus and Apateon pedestris have been analysed. Their stylopod histology shows different growth rhythms that might be correlated to changes in palaeoecosystems: food availability and/or presence of predators. Palaeoenvironmental influences are also recognized during the limb-bone osteogenesis by the expression of simple and/or double patterns of Lines of Arrested Growth (LAG). A double-LAG pattern expresses hibernating and aestivating arrests of growth in extant newts. The fossil samples from the two stratigraphically oldest horizons preserved a similar double-LAG pattern, suggesting that they may have hibernated and aestivated every year because of harsh climatic conditions. The Saar-Nahe lake system probably passed from a higher altitude zone into a lower one, possibly because of subsidence and/or erosion. It could also be correlated to the size of the lakes that differs from one locality to another, inducing different responses of the organisms to the climatic variations.