Squamates Squamate research • Review of studies on the origin and early evolution of squamates from the preceding years is published by Simões, Tollis & Burbrink (2025). • A study on the
biogeography of squamates throughout their evolutionary history is published by Wilenzik & Pyron (2025), who identify Europe and northeastern Asia as the most likely areas of the origin of Squamata. • Lizard teeth showing adaptations to
durophagy are described from the strata of the
Deccan Intertrappean Beds from the Cretaceous-Paleogene transition from Kesavi (
Madhya Pradesh,
India) by Yadav & Verma (2025). • Villa & Rummel (2025) describe a specimen of
Rhodanogekko vireti from the Oligocene strata from Weißenburg (
Bavaria,
Germany), representing the first record of the species outside
France and extending its known stratigraphic record by about 10 million years. • Čerňanský, Tabuce & Vidalenc (2025) report the first fossil evidence of presence of
scincoids and
pleurodontan
iguanians in the Cos locality (Quercy Phosphorites Formation, France) during the
Ypresian. • Brownstein et al. (2025) argue that the common ancestor of extant
night lizards originated before the
Cretaceous–Paleogene extinction event and that members of the group survived the extinction in spite of living in the areas close to the site of the
Chicxulub impact crater. • Jiang et al. (2025) review the taxonomic composition, phylogenetic affinities, morphological diversity and geographical distribution of
polyglyphanodontians. • Santos et al. (2025) describe a new specimen of
Calanguban alamoi from the Lower Cretaceous
Crato Formation (
Brazil), designated by the authors as the
neotype of the species, and interpret is as a borioteiioid (polyglyphanodontian). • Evidence from the study population genomic data and probable Quaternary fossils, indicative of impact changes of temperature and precipitation during the Quaternary on changes of range of
Rankinia diemensis, is presented by Ramm et al. (2025). • Revision of the
Paleogene fossil material of
glyptosaurids from
Kazakhstan and
Mongolia is published by Syromyatnikova (2025). • Syromyatnikova & Tarasova (2025) describe fossils of the legless lizard
Pseudopus apodus from the
Lower Pleistocene Taurida Cave (Crimea), representing the first
anguid fossil found in the region and one of the geologically oldest occurrences of the species. • A maxilla representing the first cranial material of a
monitor lizard from the
Miocene of
India reported to date is described by Čerňanský & Patnaik (2025). • Fossil material of a monitor lizard which might represent the latest record of
Varanus marathonensis in Europe reported to date is described from the Pliocene strata from the Megalo Emvolon locality (
Greece) by Drakopoulou et al. (2025). • Song & Lindgren (2025) reconstruct soft-tissue outline of the tail fin of
mosasaurs on the basis of comparisons with extant sharks, infer the presence of a bilobed tail fin in all hydropedal mosasaurs, and interpret their findings as indicating that such tail fins evolved independently at least four times in mosasaurs. • López-Rueda et al. (2025) describe new mosasaur material from the Upper Cretaceous
Labor-Tierna and
Plaeners formations (
Colombia), including the first record of a member of the genus
Globidens from northern South America reported to date. • A study on patterns of the foraging area preference of members of different mosasaur groups throughout the Late Cretaceous, as indicated by carbon isotope composition of tooth enamel, is published by Polcyn et al. (2025). • A study on teeth of mosasaurs from the
Campanian Bearpaw Formation (
Alberta,
Canada), providing evidence of dietary niche differentiation of the studied taxa, is published by Holwerda et al. (2025). • A study on diversity of tooth shapes and likely dietary preferences of
Maastrichtian mosasaurs from the Phosphates of
Morocco is published by Bardet et al. (2025), who also transfer
Platecarpus (?)
ptychodon Arambourg (1952) to the genus
Gavialimimus, and interpret it as a probable
senior synonym of
Gavialimimus almaghribensis. • Evidence from the study of a tooth fragment of
cf. Prognathodon sp. from the Upper Cretaceous strata in
South Africa, indicating that the studied individual had a higher body temperature than closely associated
Squalicorax shark, and likely higher than seawater temperature, is presented by Woolley et al. (2025). • Grigoriev et al. (2025) describe fossil material of
Latoplatecarpus cf. L. willistoni from the Campanian
Rybushka Formation (
Saratov Oblast,
Russia), representing the first known record of the genus outside of North America. • Longrich et al. (2025) provide new information on the teeth of
Xenodens calminechari based on CT scans and a referred specimen, and support the interpretation of
Xenodens as a valid, distinct taxon with unusual dental anatomy. • During et al. (2025) describe a tooth of a mosasaurine mosasaur (likely a member of the tribe Prognathodontini) from the
Hell Creek Formation (
North Dakota, United States), and interpret the results of the analysis of isotopic composition of tooth enamel as indicating that the tooth most likely formed when the studied individual lived in a freshwater environment. • Redescription of the skeletal morphology and taxonomic revision of
Cadurceryx is published by Szyndlar & Georgalis (2025), who interpret the type species
C. filholi as the only known species present in France during the middle and late Eocene, and consider the second species
C. pearchi to be a
nomen dubium. • Scanferla, Babot & García Lopez (2025) describe a snake neurocranium from the Eocene
Geste Formation (Argentina), preserving a combination of features otherwise known only in
uropeltids, and report evidence of morphological convergences in the skeleton of burrowing and surface-dwelling miniaturized snakes, making it uncertain whether the uropeltid-like traits of the specimen from the Geste Formation are phylogenetically informative. • Georgalis (2025) revises
Plesiotortrix edwardsi from the
Quercy Phosphorites Formation (
France), and considers it to be
nomen dubium. • The oldest cranial remains of a member of Constrictores (the group including boas and pythons) described and figured from the Cenozoic of Europe to date are reported from the Eocene (Ypresian) strata from the Cos locality (Quercy Phosphorites Formation, France) by Čerňanský et al. (2025). • A vertebra of a member of Constrictores, representing the oldest vertebra of a terrestrial snake from the Paleogene of eastern North America reported to date, is described from the Eocene
Nanjemoy Formation (Virginia, United States) by Pritchard et al.(2025). • Nascimento et al. (2025) describe fossil material of a member of the genus
Boa from the Late Pleistocene Toca do Angico site (
Brazil), interpreted on the basis of stable carbon isotope analyses as feeding on animals living in an open environment dominated by
C4 vegetation. • Alfonso-Rojas et al. (2025) describe new fossil material of
Colombophis sp. and
Eunectes sp. from the Socorro and
Urumaco formations (
Venezuela), providing evidence of existence of anacondas exceeding 5 metres in length in the Miocene. • Fossil material of a member of the genus
Acrochordus, morphologically distinct from
Acrochordus dehmi and possibly representing a new species, is described from the Miocene strata from Kutch (
India) by Datta & Bajpai (2025). • Hunt & Lucas (2025) describe the first known fossil snake
regurgitalites from the Eocene
Messel Formation in Germany, and name new ichnotaxa
Ophiemeticus smithi and
Messelemeticus lehmanni. • Venczel et al. (2025) describe new fossil material of snakes from Eocene and Oligocene localities in the Transylvanian Basin (
Romania), including
cf. Messelophis variatus from the Oligocene (
Rupelian) strata of the Dâncu Formation which might represent the last occurrence of
ungaliophiids in Europe. • The first known assemblage of snake fossils from
Taiwan, probably originating from the Middle Pleistocene
Chiting Formation, is described by Lin et al. (2025). • Petermann & Lyson (2025) compare the diversity of squamate faunas from the Cretaceous-Paleogene transition from the
Denver Basin (
Colorado, United States), and report evidence indicating that local squamate assemblage was severely affected by the
Cretaceous–Paleogene extinction event. • Evidence from the study of lizard and snake fossils from Eocene localities in Wyoming and North Dakota (United States), interpreted as indicative of warmer and wetter climate in mid-latitude North America during the late Eocene than indicated by earlier studies, is presented by Smith & Bruch (2025). • Xerri et al.(2025) report the first discovery of fossil material of a wall lizard (
Podarcis cf. filfolensis) and an indeterminate
colubrid snake from the Pleistocene fossil record from
Malta. • Woolley, Bottjer & Smith (2025) report evidence indicating that, on global scale, the completeness of the fossil record of squamates is influenced by differences in body size and form and by lithological and depositional biases to a greater degree than by human-based sampling biases.
Other lepidosauromorphs Other lepidosauromorph research • Evidence of adaptations for climbing in the skeleton of
Marmoretta oxoniensis is presented by Ford et al. (2025). == Ichthyosauromorphs ==