Denazinemys
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Denazinemys
''Denazinemys'' was a genus of baenid turtle that lived in the Late Cretaceous of New Mexico. The holotype specimen, which ''D. nodosa'' was based on, USNM 8345, consists of a partial carapace and plastron. It came from the De-na-zin Member of the Kirtland Formation, and therefore, ''Denazinemys'' lived in the Kirtlandian land-vertebrate age. Many specimens other than the holotype have been assigned to ''Denazinemys''. Distinguishing characteristics Previously, '' Scabremys ornata'' was assigned to ''Denazinemys'' as ''D. ornata''. Below are the features found in ''Denazinemys'' distinguishing the two genera: * a carapace that is sub-triangular with widest dimension posteriorly; * prepleurals present and touching the first vertebrae medially; * the first vertebrae an irregular hexagonal shape with the greatest width posteriorly, contacting anterior second vertebrae; * extracervicals lateral to the primary cervicals, the cervicals being sub-divided; * and carapace ...
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Baenid
Baenidae is an extinct family of paracryptodiran turtles known from the Early Cretaceous to Eocene of North America. While during the Early Cretaceous they are found across North America, during the Late Cretaceous they are only found in Laramidia, having disappeared from Appalachia. The majority of lineages survived the K-Pg Extinction, but the family was extinct by the latest Eocene. The name of the type genus, ''Baena,'' appears to be of Native American origin. They are primarily found in freshwater deposits, and are considered to be aquatic, with a largely generalist habit. Genera * †'' Arundelemys'' * †''Arvinachelys'' * †''Baena'' * †''Cedrobaena'' * †''Chisternon'' * †'' Edowa'' * †''Gamerabaena'' * †'' Hayemys'' * †'' Lakotemys'' Lakota Formation, Berriasian-Valanginian * †''Neurankylus'' * †''Palatobaena'' * †''Peckemys'' * †''Plesiobaena ''Plesiobaena'' is an extinct genus of turtle which existed in the Belly River Formation, Canada during t ...
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Baenodda
Baenidae is an extinct family of paracryptodiran turtles known from the Early Cretaceous to Eocene of North America. While during the Early Cretaceous they are found across North America, during the Late Cretaceous they are only found in Laramidia, having disappeared from Appalachia. The majority of lineages survived the K-Pg Extinction, but the family was extinct by the latest Eocene. The name of the type genus, ''Baena,'' appears to be of Native American origin. They are primarily found in freshwater deposits, and are considered to be aquatic, with a largely generalist habit. Genera * †'' Arundelemys'' * †''Arvinachelys'' * †''Baena'' * †''Cedrobaena'' * †''Chisternon'' * †'' Edowa'' * †''Gamerabaena'' * †'' Hayemys'' * †'' Lakotemys'' Lakota Formation, Berriasian-Valanginian * †''Neurankylus'' * †''Palatobaena'' * †''Peckemys'' * †''Plesiobaena ''Plesiobaena'' is an extinct genus of turtle which existed in the Belly River Formation, Canada during t ...
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Baenidae
Baenidae is an extinct family of paracryptodiran turtles known from the Early Cretaceous to Eocene of North America. While during the Early Cretaceous they are found across North America, during the Late Cretaceous they are only found in Laramidia, having disappeared from Appalachia. The majority of lineages survived the K-Pg Extinction, but the family was extinct by the latest Eocene. The name of the type genus, ''Baena,'' appears to be of Native American origin. They are primarily found in freshwater deposits, and are considered to be aquatic, with a largely generalist habit. Genera * †'' Arundelemys'' * †'' Arvinachelys'' * †'' Baena'' * †''Cedrobaena'' * †''Chisternon'' * †'' Edowa'' * †''Gamerabaena'' * †'' Hayemys'' * †'' Lakotemys'' Lakota Formation, Berriasian-Valanginian * †''Neurankylus'' * †'' Palatobaena'' * †'' Peckemys'' * †''Plesiobaena ''Plesiobaena'' is an extinct genus of turtle which existed in the Belly River Formation, Canada duri ...
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Kirtland Formation
The Kirtland Formation (originally the Kirtland Shale) is a sedimentary geological formation. Description The Kirtland Formation is the product of alluvial muds and overbank sand deposits from the many channels draining the coastal plain that existed on the inland seashore of North America, in the late Cretaceous period. It overlies the Fruitland Formation. It is found in the San Juan Basin in the states of New Mexico and Colorado, in the United States of America. The base of the Kirtland Formation and its lowest sub-unit, the Hunter Wash member, has been dated to 75.02 ± 0.13 Ma. Together with the upper part of the underlying Fruitland Formation, this contains fossils representing the Hunter Wash local fauna. The border between the Hunter Wash member and overlying Farmington member dates to approximately 74 million years ago. The top of the Farmington member and bottom of the overlying De-na-zin member has been radiometrically dated to 73.83 ± 0.18 Ma ago. The top of the ...
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Vertebrae
The spinal column, a defining synapomorphy shared by nearly all vertebrates,Hagfish are believed to have secondarily lost their spinal column is a moderately flexible series of vertebrae (singular vertebra), each constituting a characteristic irregular bone whose complex structure is composed primarily of bone, and secondarily of hyaline cartilage. They show variation in the proportion contributed by these two tissue types; such variations correlate on one hand with the cerebral/caudal rank (i.e., location within the vertebral column, backbone), and on the other with phylogenetic differences among the vertebrate taxon, taxa. The basic configuration of a vertebra varies, but the bone is its ''body'', with the central part of the body constituting the ''centrum''. The upper (closer to) and lower (further from), respectively, the cranium and its central nervous system surfaces of the vertebra body support attachment to the intervertebral discs. The posterior part of a vertebra fo ...
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Neurankylus
''Neurankylus'' is an extinct genus of turtles in the family Baenidae that lived between 112 and 61 million years ago in Canada and the United States. It was originally placed within the monotypic family Neurankylidae, but it has since been placed in the Neurankylinae, alongside '' Trinitichelys''. The type species, ''Neurankylus eximius'', was described by Lawrence Lambe in 1902. The species ''N. lithographicus'' was discovered in the Milk River Formation ( Canada), alongside the holotype of the pachycephalosaurid dinosaur ''Acrotholus audeti ''Acrotholus'' (Greek for "highest dome"- akros meaning highest and tholos meaning dome) is an extinct genus of pachycephalosaur dinosaur that lived during the Santonian of the late Cretaceous, in the Milk River Formation of Canada. The type spec ...''. References {{Taxonbar, from1=Q73170070 Baenidae Cretaceous turtles Paleocene turtles Cretaceous reptiles of North America Paleocene reptiles of North America Hell Creek ...
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Chisternon
''Chisternon'' is a genus of baenid turtles from the Eocene of North America North America is a continent in the Northern Hemisphere and almost entirely within the Western Hemisphere. It is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the southeast by South America and the Car .... References *''The Osteology of the Reptiles'' by Alfred Sherwood Romer External links''Chisternon''in the Paleobiology Database Baenidae Prehistoric turtle genera Eocene turtles Eocene reptiles of North America Fossil taxa described in 1872 Taxa named by Joseph Leidy {{paleo-turtle-stub ...
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Baena (turtle)
''Baena'' is an extinct genus of baenid turtles. Fossils of ''Baena'' have been found in locations including Kirtland Formation, Campanian New Mexico (''B.'' sp.) (Cretaceous) and Ravenscrag Formation, Maastrichtian Canada Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by tot ... (''B.'' sp.) (Cretaceous). References Baenidae Prehistoric turtle genera {{Paleo-turtle-stub ...
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Plesiobaena
''Plesiobaena'' is an extinct genus of turtle which existed in the Belly River Formation, Canada during the late Cretaceous period (Campanian age). It was first named by Lawrence Lambe Lawrence Morris Lambe (August 27, 1863 – March 12, 1919) was a Canadian geologist, palaeontologist, and ecologist from the Geological Survey of Canada (GSC). His published work, describing the diverse and plentiful dinosaur discoveries from th ... in 1902 and the type species is ''Plesiobaena antiqua''. References Baenidae Prehistoric turtle genera Late Cretaceous turtles of North America Hell Creek fauna Laramie Formation Fossil taxa described in 1902 Taxa named by Lawrence Lambe {{paleo-turtle-stub ...
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Osteoderm
Osteoderms are bony deposits forming scales, plates, or other structures based in the dermis. Osteoderms are found in many groups of extant and extinct reptiles and amphibians, including lizards, crocodilians, frogs, temnospondyls (extinct amphibians), various groups of dinosaurs (most notably ankylosaurs and stegosaurians), phytosaurs, aetosaurs, placodonts, and hupehsuchians (marine reptiles with possible ichthyosaur affinities). Osteoderms are uncommon in mammals, although they have occurred in many xenarthrans (armadillos and the extinct glyptodonts and mylodontid and scelidotheriid ground sloths). The heavy, bony osteoderms have evolved independently in many different lineages. The armadillo osteoderm is believed to develop in subcutaneous dermal tissues. These varied structures should be thought of as anatomical analogues, not homologues, and do not necessarily indicate monophyly. The structures are however derived from scutes, common to all classes of amniotes and ...
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