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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Insectivora
Using three-dimensional geometric morphometric and dental topographic analyses to infer the systematics and paleoecology of fossil treeshrews (Mammalia, Scandentia) Available to Purchase
Biostratigraphy of the Lystrosaurus declivis Assemblage Zone (Beaufort Group, Karoo Supergroup), South Africa Available to Purchase
Northern Asian Pliocene–Pleistocene beremendiin shrews (Mammalia, Lipotyphla, Soricidae): a description of material from Russia (Siberia), Kazakhstan, and Mongolia and the paleobiology of Beremendia Available to Purchase
Vertebrate fossils from the Claron Formation, Sweetwater Creek area, Garfield County, Utah, U.S.A. Available to Purchase
Eudaemonema webbi sp. nov. (Mammalia, Mixodectidae) from the late Paleocene of western Canada: the youngest known mixodectid Available to Purchase
WHAT IF ELEPHANT SHREWS REALLY WERE RELATED TO ELEPHANTS? Available to Purchase
THE MICROMAMMAL FAUNA FROM NEGRATÍN-1 (GUADIX BASIN, SOUTHERN SPAIN): NEW EVIDENCE OF AFRICAN-IBERIAN MAMMAL EXCHANGES DURING THE LATE MIOCENE Available to Purchase
A new erinaceid (Mammalia, Insectivora) from the Late Paleocene of western Canada Available to Purchase
Early African hyaenodontid mammals and their bearing on the origin of the Creodonta Available to Purchase
ANOUROSORICINI (MAMMALIA: SORICIDAE) FROM THE MEDITERRANEAN REGION: A PRE-QUATERNARY EXAMPLE OF RECURRENT CLIMATE-CONTROLLED NORTH-SOUTH RANGE SHIFTING Available to Purchase
A NEW PALAEORYCTID (INSECTIVORA: MAMMALIA) FROM THE LATE PALEOCENE OF ALBERTA, CANADA Available to Purchase
A peculiar new fossil shrew (Lipotyphla, Soricidae) from the High Arctic of Canada Available to Purchase
Using large mammal communities to examine ecological and taxonomic structure and predict vegetation in extant and extinct assemblages Free
Koniaryctes, a new genus of apternodontid insectivore from lower Eocene rocks of the Powder River basin, Wyoming Available to Purchase
Micromammal-Based Palaeoenvironment of Upper Siwaliks Exposed Near Village Saketi, H. P. Available to Purchase
Upper Pleistocene Soricidae and Muridae from Bhimtal-Bilaspur Deposits, Kumaun Himalaya, India Available to Purchase
A latest Chadronian (Late Eocene) mammalian fauna from the Cypress Hills, Saskatchewan Free
Paromomyidae (?Dermoptera) from the Powder River basin, Wyoming, and a discussion of microevolution in closely-related species Available to Purchase
Pliocene Soricidae (Insectivora, Mammalia) from Kashmir Intermontane Basin, Northwestern Himalaya Available to Purchase
Mammals of the Bridgerian (middle Eocene) Elderberry Canyon Local Fauna of eastern Nevada Available to Purchase
The first Eocene vertebrate assemblage known from the Great Basin, the Elderberry Canyon Local Fauna, occurs in rocks referred to the Sheep Pass Formation near Ely, Nevada. Approximately 40 taxa are now known, including small anuran amphibians, small reptiles, birds, and mammals. The mammalian component consists of: the insectivorans Apatemys bellus, Pantolestes longicaudus, a tiny apternodont, at least one nyctitheriid, and at least four other taxa representing dormaalid and/or erinaceid erinaceomorphs; an epoicotheriid palaeanodont, cf. Tetrapassalus mckennai; the primates Notharctus tenebrosus, Trogolemur myodes, and two species of uintasoricines; the rodents Reithroparamys delicatissimus, R. cf. R. huerfanensis, Sciuravus sp., Microparamys sp., Pauromys sp., Mattimys sp., and two new genera; the hyaenodont Sinopa minor; two viverravid carnivores including Viverravus; the condylarth Hyopsodus paulus; the perissodactyls Hyrachyus modestus, Hyrachyus affinis, Helaletes nanus, Isectolophus latidens, and a new genus and species; and the artiodactyl Antiacodon pygmaeus. Greatest faunal similarity is with the Black’s Fork Member (or lower), Bridger Formation, and other early Bridgerian localities such as Powder Wash in the Douglas Creek Member of the Green River Formation in northeastern Utah. The age of the Elderberry Canyon Local Fauna can confidently be called early Bridgerian. The Elderberry Canyon Fauna is preserved in carbonate rocks believed to have been deposited in a shallow, warm, heavily vegetated, permanent, hardwater lake. The mammals lived on marshy wetland terrain adjacent to the lake, although some faunal elements may have been transported in from more distant habitats.