Lentiarenium Cristolii Cranium In Dorsal View
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Lentiarenium Cristolii Cranium In Dorsal View
''Lentiarenium'' was an early sea cow from the Late Oligocene ( Chattian) Linz-Melk Formation of Austria. Known since the mid 19th century, ''Lentiarenium'' was long considered to be a species of ''Halitherium'' until a 2016 analysis showed it to be distinct. History and naming The earliest discoveries of ''Lentiarenium'' date to the early 19th century, with a mandible, ribs, vertebrae and molars being found in sandpits of the city of Linz. Following communication between several researchers across multiple Austrian institutions, the remains were correctly identified as belonging to an extinct species of seacow by paleontologist Leopold Fitzinger, who would go on to describe the material in 1842. Fitzinger believed the bones to belong to the sirenian ''Halitherium'', described by Johann Jakob Kaup just four years prior. At the time of its description, it was thought to be the only sirenian of the area surrounding Linz. However additional finds from Upper Austria were made follo ...
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Late Oligocene
The Chattian is, in the geologic timescale, the younger of two ages or upper of two stages of the Oligocene Epoch/Series. It spans the time between . The Chattian is preceded by the Rupelian and is followed by the Aquitanian (the lowest stage of the Miocene). Stratigraphic definition The Chattian was introduced by Austrian palaeontologist Theodor Fuchs in 1894. Fuchs named the stage after the Chatti, a Germanic tribe.Berry, Edward W"The Mayence Basin, a Chapter of Geologic History" ''The Scientific Monthly'', Vol. 16, No. 2, February 1923. pp. 114. Retrieved March 18, 2020. The original type locality was near the German city of Kassel. The base of the Chattian is at the extinction of the foram genus ''Chiloguembelina'' (which is also the base of foram biozone P21b). An official GSSP for the Chattian Stage was ratified in October of 2016. The top of the Chattian Stage (which is the base of the Aquitanian Stage, Miocene Series and Neogene System) is at the first appearance of ...
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Wastebasket Taxon
Wastebasket taxon (also called a wastebin taxon, dustbin taxon or catch-all taxon) is a term used by some taxonomists to refer to a taxon that has the sole purpose of classifying organisms that do not fit anywhere else. They are typically defined by either their designated members' often superficial similarity to each other, or their ''lack'' of one or more distinct character states or by their ''not'' belonging to one or more other taxa. Wastebasket taxa are by definition either paraphyletic or polyphyletic, and are therefore not considered valid taxa under strict cladistic rules of taxonomy. The name of a wastebasket taxon may in some cases be retained as the designation of an evolutionary grade, however. The term was coined in a 1985 essay by Steven Jay Gould. Examples There are many examples of paraphyletic groups, but true "wastebasket" taxa are those that are known not to, and perhaps not intended to, represent natural groups, but are nevertheless used as convenient groups ...
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Frontal Bone
The frontal bone is a bone in the human skull. The bone consists of two portions.''Gray's Anatomy'' (1918) These are the vertically oriented squamous part, and the horizontally oriented orbital part, making up the bony part of the forehead, part of the bony orbital cavity holding the eye, and part of the bony part of the nose respectively. The name comes from the Latin word ''frons'' (meaning " forehead"). Structure of the frontal bone The frontal bone is made up of two main parts. These are the squamous part, and the orbital part. The squamous part marks the vertical, flat, and also the biggest part, and the main region of the forehead. The orbital part is the horizontal and second biggest region of the frontal bone. It enters into the formation of the roofs of the orbital and nasal cavities. Sometimes a third part is included as the nasal part of the frontal bone, and sometimes this is included with the squamous part. The nasal part is between the brow ridges, and ends in ...
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Hands
A hand is a prehensile, multi-fingered appendage located at the end of the forearm or forelimb of primates such as humans, chimpanzees, monkeys, and lemurs. A few other vertebrates such as the koala (which has two opposable thumbs on each "hand" and fingerprints extremely similar to human fingerprints) are often described as having "hands" instead of paws on their front limbs. The raccoon is usually described as having "hands" though opposable thumbs are lacking. Some evolutionary anatomists use the term ''hand'' to refer to the appendage of digits on the forelimb more generally—for example, in the context of whether the three digits of the bird hand involved the same homologous loss of two digits as in the dinosaur hand. The human hand usually has five digits: four fingers plus one thumb; these are often referred to collectively as five fingers, however, whereby the thumb is included as one of the fingers. It has 27 bones, not including the sesamoid bone, the number ...
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Forearms
The forearm is the region of the upper limb between the elbow and the wrist. The term forearm is used in anatomy to distinguish it from the arm, a word which is most often used to describe the entire appendage of the upper limb, but which in anatomy, technically, means only the region of the upper arm, whereas the lower "arm" is called the forearm. It is homologous to the region of the leg that lies between the knee and the ankle joints, the crus. The forearm contains two long bones, the radius and the ulna, forming the two radioulnar joints. The interosseous membrane connects these bones. Ultimately, the forearm is covered by skin, the anterior surface usually being less hairy than the posterior surface. The forearm contains many muscles, including the flexors and extensors of the wrist, flexors and extensors of the digits, a flexor of the elbow (brachioradialis), and pronators and supinators that turn the hand to face down or upwards, respectively. In cross-section, the fo ...
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Lacrimal Bones
The lacrimal bone is a small and fragile bone of the facial skeleton; it is roughly the size of the little fingernail. It is situated at the front part of the medial wall of the orbit. It has two surfaces and four borders. Several bony landmarks of the lacrimal bone function in the process of lacrimation or crying. Specifically, the lacrimal bone helps form the nasolacrimal canal necessary for tear translocation. A depression on the anterior inferior portion of the bone, the lacrimal fossa, houses the membranous lacrimal sac. Tears or lacrimal fluid, from the lacrimal glands, collect in this sac during excessive lacrimation. The fluid then flows through the nasolacrimal duct and into the nasopharynx. This drainage results in what is commonly referred to a runny nose during excessive crying or tear production. Injury or fracture of the lacrimal bone can result in posttraumatic obstruction of the lacrimal pathways. Structure Lateral or orbital surface The lateral or orbital surface i ...
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Premaxilla
The premaxilla (or praemaxilla) is one of a pair of small cranial bones at the very tip of the upper jaw of many animals, usually, but not always, bearing teeth. In humans, they are fused with the maxilla. The "premaxilla" of therian mammal has been usually termed as the incisive bone. Other terms used for this structure include premaxillary bone or ''os premaxillare'', intermaxillary bone or ''os intermaxillare'', and Goethe's bone. Human anatomy In human anatomy, the premaxilla is referred to as the incisive bone (') and is the part of the maxilla which bears the incisor teeth, and encompasses the anterior nasal spine and alar region. In the nasal cavity, the premaxillary element projects higher than the maxillary element behind. The palatal portion of the premaxilla is a bony plate with a generally transverse orientation. The incisive foramen is bound anteriorly and laterally by the premaxilla and posteriorly by the palatine process of the maxilla. It is formed from the ...
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Lentiarenium Cristolii Mandible In Occlusal View
''Lentiarenium'' was an early sea cow from the Late Oligocene ( Chattian) Linz-Melk Formation of Austria. Known since the mid 19th century, ''Lentiarenium'' was long considered to be a species of ''Halitherium'' until a 2016 analysis showed it to be distinct. History and naming The earliest discoveries of ''Lentiarenium'' date to the early 19th century, with a mandible, ribs, vertebrae and molars being found in sandpits of the city of Linz. Following communication between several researchers across multiple Austrian institutions, the remains were correctly identified as belonging to an extinct species of seacow by paleontologist Leopold Fitzinger, who would go on to describe the material in 1842. Fitzinger believed the bones to belong to the sirenian ''Halitherium'', described by Johann Jakob Kaup just four years prior. At the time of its description, it was thought to be the only sirenian of the area surrounding Linz. However additional finds from Upper Austria were made follo ...
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Jules De Christol
Jules de Christol (25 August 1802 – 25 June 1861) was a French paleontologist and geologist who identified the fossil horse ancestor ''Hipparion''. He was among the first French zoologists to suggest the existence of human remains that were "antediluvian", older than the supposed Biblical flood, contrary to the dominant view of earth history at the time. De Christol was born in Montepellier and became a student of Marcel de Serres, a professor at Montpellier. In 1828 he discovered human remains and pottery in Souvignargues alongside remains of rhino, bear, and hyena bones. He then suggested the existence of humans alongside animals that were traditionally supposed to have gone extinct after the Biblical flood, a view supported by the dominant French zoologists of the time like Georges Cuvier. His idea was however supported by William Buckland who visited him during the digs in Lunel-Viel. He saw similar remains in 1829 in a cave in Pondres digging along with Dumas Emilien. In ...
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Lectotype
In biology, a type is a particular specimen (or in some cases a group of specimens) of an organism to which the scientific name of that organism is formally attached. In other words, a type is an example that serves to anchor or centralizes the defining features of that particular taxon. In older usage (pre-1900 in botany), a type was a taxon rather than a specimen. A taxon is a scientifically named grouping of organisms with other like organisms, a set that includes some organisms and excludes others, based on a detailed published description (for example a species description) and on the provision of type material, which is usually available to scientists for examination in a major museum research collection, or similar institution. Type specimen According to a precise set of rules laid down in the International Code of Zoological Nomenclature (ICZN) and the International Code of Nomenclature for algae, fungi, and plants (ICN), the scientific name of every taxon is almost a ...
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Syntypes
In biological nomenclature, a syntype is any one of two or more biological types that is listed in a description of a taxon where no holotype was designated. Precise definitions of this and related terms for types have been established as part of the International Code of Zoological Nomenclature and the International Code of Nomenclature for algae, fungi, and plants. In zoology In zoological nomenclature, a syntype is defined as "Each specimen of a type series (q.v.) from which neither a holotype nor a lectotype has been designated rts. 72.1.2, 73.2, 74 The syntypes collectively constitute the name-bearing type." (Glossary of the zoological Code ). Historically, syntypes were often explicitly designated as such, and under the present ICZN this is a requirement (Art. 72.3), but modern attempts to publish species or subspecies descriptions based on syntypes are generally frowned upon by practicing taxonomists, and most are gradually being replaced by lectotypes. Those that still ex ...
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Italosiren
''Italosiren'' is an extinct genus of early dugong from the Early Miocene ( Aquitanian) Libano Formation in northern Italy. Classification It was originally classified as a species of ''Halitherium'', ''H. bellunense'', but was eventually recognized as closer to the dugong than to ''Halitherium schinzii'', necessitating erection of the new generic name ''Italosiren''. See also * Evolution of sirenians Sirenia is the order of placental mammals which comprises modern "sea cows" (manatees and the Dugong) and their extinct relatives. They are the only extant herbivorous marine mammals and the only group of herbivorous mammals to have become com ... References Miocene sirenians Prehistoric placental genera Aquitanian (stage) Miocene mammals of Europe Neogene Italy Fossils of Italy Fossil taxa described in 2017 {{Paleo-sirenian-stub ...
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