This article records new taxa of fossil mammals of every kind that are scheduled to be described during the year 2026, as well as other significant discoveries and events related to paleontology of mammals that are scheduled to occur in the year 2026.
Afrotherians Proboscideans Name NoveltyStatusAuthorsAgeType localityCountryNotesImagesArchaeobelodon tassyiSp. novValidSanders et al.MioceneBakate FormationChesalophodonGen. et sp. novValidEshelman et al.Miocene (Clarendonian)Choptank Formation()A gomphothere. The type species is C. gulottai.EochoerodonGen. et comb. novValidLi & Wang MioceneA member of the family Choerolophodontidae. Genus includes "Choerolophodon" guangheensis Wang & Deng (2011) and "Mastodon (Trilophodon) angustidens" var. palaeindicus Lydekker (1884).ParachoerodonGen. et sp. et comb. novValidLi & Wang MioceneHalamagai Formation Keramaria Formation Zhangenbao FormationA member of the family Choerolophodontidae. Genus includes new species P. rhynchus, as well as "Choerolophodon" chioticus Tobien (1980) and "Trilophodon" connexus Hopwood (1935).Protanancus presbytatosSp. novValidSanders et al.MioceneBakate FormationZygolophodon microgigasSp. novValidSanders et al.MioceneBakate Formation
Proboscidean research A study on the morphology of the astragalus and calcaneus in extant and extinct proboscideans, providing evidence of morphological changes of ankles bones related to increase of the body mass and evolution of the columnar posture of members of the group, is published by Tetaert et al. (2026). A study on humeri of extant and extinct proboscideans, providing evidence of different impact of compressive loading on humeri representing slender and robust morphotypes, is published by Wagner, Chatar & Hennekam (2026). Semprebon, Sanders & Uttecht (2026) reconstruct diets and habitats of Moeritherium and Phiomia on the basis of their tooth wear, interpreting the former taxon as feeding on soft vegetation and likely frequenting aquatic habitats, and interpreting the latter taxon as likely living in a terrestrial forest or woodland environment. Alquézar-Blesa et al. (2026) study the feeding behaviors of Miocene Gomphotherium and Prodeinotherium from Artesilla and Tarazona (Spain), reporting evidence from the study of tooth wear indicative of a greater degree of dietary flexibility than indicated by tooth morphology, including evidence of grass consumption. Bader, Gasparik & Segesdi (2026) compare the microanatomy of femur of Deinotherium giganteum and mammoths, reporting evidence of differences that might be linked to distinct weight-bearing adaptations. Description of new fossil material of Mammut shansiense from the Yushe Basin (China) and a study on the phylogenetic affinities of the species is published by Zhang et al. (2026), who recover the studied species as closely related to the American mastodon. Sanders, Ji & Jablonski (2026) describe fossil material of Stegodon zhaotongensis from the Miocene strata of the Zhaotong Formation at the Shuitangba site (Yunnan, China), reaffirm the validity of the species, and interpret its anatomical features as consistent with origination of stegodonts from stegolophodonts in Asia. Liu et al. (2026) report the first discovery of fossil material of Stegodon from the late Pliocene or early Pleistocene strata from the Shandong Province (China), referred to the species Stegodon chiai. A study on the chemical composition of teeth of Gomphotherium angustidens from the Miocene (Langhian) strata from Quinta da Farinheira (Portugal), providing evidence of seasonal changes in the diet of the studied proboscidean and probable evidence of geophagia during fixed times of the year, is published by Coimbra et al. (2026). Han et al. (2026) report the discovery of a molar of a member of the genus Gomphotherium from the Miocene strata of the Jinsu Formation (North Korea), extending known geographical distribution of members of this genus in Asia. New fossil material of Notiomastodon platensis is described from the Lujanian strata of the La Chumbiada Member of the Lujan Formation (Buenos Aires Province, Argentina) by Prado et al. (2026). Evidence from the study of strontium, carbon and oxygen isotopic composition of remains of Notiomastodon platensis from Pleistocene sites in the states of Pernambuco, Paraíba and Sergipe (Brazil), indicative of a predominantly C4-based diet of the studied individuals and indicating that the studied sample included both sedentary and mobile individuals, is presented by Cruz et al. (2026). The first complete skull of a member of the genus Cuvieronius (C. cf. tropicus) from North America reported to date is described from the Pleistocene (Irvingtonian) strata of the Camp Rice Formation (New Mexico, United States) by Houde et al. (2026), who argue that North/Central American and South American members of the genus Cuvieronius likely represent two distinct cryptic species. González-Guarda et al. (2026) reconstruct the environment of late Pleistocene Notiomastodon platensis and Cuvieronius hyodon from Ecuador on the basis of their tooth wear and carbon isotopic composition of their tooth enamel, interpreted as indicative of predominantly open and dry habitats. Kumar (2026) reports the first discovery of fossil material of Anancus sivalensis from Indian Siwaliks, recovered from the Pliocene Tatrot Formation in Himachal Pradesh. Lambert (2026) reevaluates the affinites of "Platybelodon" barnumbrowni from the Late Miocene of Nebraska (United States), transferring the species to the genus Protanancus (the first record of the genus from North America), as well as describing "Serbelodon" burnhami and an unnamed taxon from the Bone Valley of Florida as sharing affinities with Protanancus. Armaroli et al. (2026) reconstruct the ecology and habitat use of straight-tusked elephants from the Neumark-Nord site (Germany) on the basis of the study of the strontium isotopic composition of their remains and on the basis of proteomic analysis, reporting evidence indicating that the studied elephant assemblage included both male and female individuals from geographically separated populations that migrated to the lake basins of Neumark-Nord, and evidence of seasonal mobility of the studied individuals, including probable evidence of two male individuals dwelling in mountainous areas within 300 km of Neumark-Nord. Farrell et al. (2026) identify fossil material of a straight-tusked elephant from the mid-Pleistocene North Bridge Acheulian site north of Gesher Benot Ya'aqov (Israel), and interpret its tooth wear and isotopic composition of its tooth enamel, coupled with the studies of local palynological assemblages and climatic reconstructions, as indicative of a mixed-feeding strategy of the studied individual, as well as indicating that it lived in a mosaic woodland-wetland habitat with a Mediterranean climate. Kusaka et al. (2026) provide the radiocarbon ages of fossils of Palaeoloxodon naumanni from Honshu and Shikoku (Japan), determine the last appearance date of the species to be 36,400–35,700 calibrated years before present, and interpret the fossil record as indicative of short coexistence of the species with Upper Paleolithic humans and its likely extinction at 35,000-33,000 calibrated years before present. Evidence from the study of the long bones of adult Palaeoloxodon tiliensis and juvenile Palaeoloxodon falconeri, indicating that bones of the former species were not scaled-down version of bones of its mainland ancestors but rather included a combination of ancestral traits, adaptations associated with a graviportal lifestyle and juvenile-like characteristics, is presented by Bader, Göhlich & Houssaye (2026). Evidence from the study of the straight-tusked elephant specimen from Middle Pleistocene site of Contrada Monticelli (Apulia, Italy) and other specimens of straight-tusked elephants and Mammuthus meridionalis from the Lower and Middle Pleistocene of Italy, indicating that the majority of purported morphological characters differentiating Mammuthus and Palaeoloxodon are not reliable when intraspecific variability is taken into consideration, is presented by Stefanelli et al. (2026). A study on the anatomy and life history of the woolly mammoth specimen from Niederweningen (Switzerland) that was the first scientifically described perinatal mammoth individual is published by Scarborough et al. (2026). Moreland et al. (2026) recover ancient DNA from mammoth ivory from the Hohle Fels cave (Germany), and report evidence of presence of mammoth specimens from multiple distinct lineages in the studied sample. Zanina et al. (2026) reconstruct the environment and diet of the woolly mammoth calf specimen "Yana" from the Batagay section (Sakha, Russia) on the basis of the study of contents of its gastrointestinal tract and the material found between its forelimbs. A new, nearly complete skeleton of a woolly mammoth, identified as a male aged approximately 30–40 years, is described from the latest Pleistocene strata from the Taymyr Peninsula (Russia) by Petrova et al. (2026). Moots et al. (2026) determine sex of 521 woolly mammoth specimens on the basis of the study of ancient DNA, reporting evidence indicating that mammoths from bone accumulation sites were predominantly female, while mammoths from other depositional settings were predominantly male, and interpret these findings as suggestive of anthropogenic origin of mammoth bone accumulations and of preferential targeting of mammoth females by humans. Hannold et al. (2026) reconstruct the diets of pygmy mammoths from Northern Channel Islands and Columbian mammoths from Rancho La Brea and coastal Santa Barbara in southern California on the basis of stable isotopes in tooth enamel. Evidence from the study of tooth enamel of Columbian mammoths from 14 sites in the Central Basin of Mexico, interpreted as indicative of a generalist diet with varying proportions of C3 and C4 plants, is presented by Rodríguez-Franco et al. (2026). Rodríguez-Franco et al. (2026) report evidence of dental anomalies in Columbian mammoth specimens from 15 localities in the Basin of Mexico. Evidence from the study of carbon, oxygen and strontium isotope composition of Columbian mammoth remains from the Colby Site (Wyoming, United States), indicative of the studied mammoths feeding mainly on C3 plants and having a range of less than 250 km, is presented by Doering, Mackie & Herron (2026), who interpret the assemblage of mammoth remains from the studied site as more likely resulting from multiple hunting episoded than from a single massive one. Evidence indicating that morphology of the astragalus of Quaternary elephantids was influenced by their body size to a greater degree than by their phylogenetic affinities is presented by Fidalgo et al. (2026).
Sirenians Name NoveltyStatusAuthorsAgeType localityCountryNotesImagesKharisirenGen. et sp. novSaha et al.MioceneKhari Nadi FormationA member of the family Dugongidae. Genus includes new species K. cristata.
Sirenia research Saha, Bhardwaj & Bajpai (2026) study the restructuring of the sirenian skull throughout the evolutionary history of the group on the basis of data from extant and fossil taxa. Wagner et al. (2026) provide a methodology for quantification of the degree of pachyostosis in ribs and vertebrae of sirenians on the basis of the study of extant and extinct taxa. Pérez-Ramos et al. (2026) present a virtual reconstruction of the vertebral column of Pezosiren portelli. New fossil material of sirenians with dugongid affinities, associated with an invertebrate assemblage that might be indicative of presence of seagrass habitats, is described from the Oligocene strata of the Maniyara Fort Formation (India) by Joshi et al. (2026).