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Aipichthys
''Aipichthys'' is an extinct genus of bony fish that is possibly polyphyletic. Species Five species have traditionally placed within ''Aipichthys'', but a redescription of the type species in 2016 suggested the genus to be polyphyletic, with only the type species as a member of the genus. The other four species were not moved out of the genus by the authors and were referred as ''`Aipichthys`''. *''Aipichthys pretiosus'' Steindachner, 1860 (Komen Limestone, Volčji Grad, Komen, Slovenia) (type species) *''Aipichthys minor'' (Pictet, 1850) (Hakel and Hjoula, Lebanon) *''Aipichthys nuchalis'' (Dixon, 1850) (Upper Cenomanian English Chalk The Chalk Group (often just called the Chalk) is the lithostratigraphic unit (a certain number of rock strata) which contains the Upper Cretaceous limestone succession in southern and eastern England. The same or similar rock sequences occur ac ..., Washington, Sussex, UK) *''Aipichthys oblongus'' Gayet, 1980 (Hakel and Hjoula, Lebanon) *'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
François Jules Pictet De La Rive
François Jules Pictet-De la Rive (27 September 180915 March 1872) was a Swiss zoologist and palaeontologist. Biography He was born in Geneva. He graduated B. Sc. at Geneva in 1829, and pursued his studies for a short time at Paris, where under the influence of Georges Cuvier, de Blainville and others, he worked at natural history and comparative anatomy. On his return to Geneva in 1830 he assisted A. P. de Candolle by giving demonstrations in comparative anatomy. Five years later, when de Candolle retired, Pictet was appointed professor of zoology and comparative anatomy. Endnotes: *Obituary by W. S. Dallas, ''Quart. Journ. Geol. Soc.'' (1873), vol. xxix. In 1846 his duties were restricted to certain branches of zoology, including geology and palaeontology, and these he continued to teach until 1859, when he retired to devote his energies to the museum of natural history and to special palaeontological work. He was rector of the Academy from 1847 to 1850, and again from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hjoula
Hjoula ( ar, حجولا) is a municipality in the Byblos District of Keserwan-Jbeil Governorate, Lebanon. It is 70 kilometers north of Beirut. Hjoula has an elevation of between 920 and 1,100 meters above sea level. Hjoula has a total land area of 528 hectares. The village of Hjoula is known for its fertile soil and its woods, as well as Early Cretaceous fossils. Etymology The word is an Aramaic one, however the meaning is uncertain. Most historians and linguists suggest it means "Oval" due to its oval shape, while some others speculate it comes from the Syriac root "G-l-a" and subsequently to the word "Guola" which supposedly means "The place of the wandering salesman". History Many old relics and monuments were found in Hjoula. There was found a Phoenician inscription in "Jarabta". A Roman statue that represented a shepherd and his sheep was also found beside the lake, and was dated to the era of emperor Tiberius c. 20 CE; along small sets of coins that were written in Kufic wi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Polymixiiformes
The beardfishes consist of a single extant genus, ''Polymixia'', of deep-sea marine ray-finned fish named for their pair of long hyoid barbels. They are classified in their own order Polymixiiformes . But as Nelson says, "few groups have been shifted back and forth as frequently as this one, and they were recently added to Paracanthoptergii". For instance, they have previously been classified as belonging to the Beryciformes. They are of little economic importance. They are found in tropical and subtropical waters of the Atlantic, Indian and western Pacific Ocean. They are bottom-dwelling fish, found down to about depth. Most are relatively small fish, although one species, '' Polymixia berndti'', is over in length. Classification * Order Polymixiiformes Rosen & Patterson, 1969 ** Genus †'' Cumbaaichthys'' Murray 2016 *** †'' Cumbaaichthys oxyrhynchus'' Murray 2016 ** Family † Boreiohydriidae Murray & Cumbaa 2013 *** Genus †'' Boreiohydrias'' Murray & Cumbaa 2013 **** ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Animalia
Animals are multicellular, eukaryotic organisms in the biological kingdom Animalia. With few exceptions, animals consume organic material, breathe oxygen, are able to move, can reproduce sexually, and go through an ontogenetic stage in which their body consists of a hollow sphere of cells, the blastula, during embryonic development. Over 1.5 million living animal species have been described—of which around 1 million are insects—but it has been estimated there are over 7 million animal species in total. Animals range in length from to . They have complex interactions with each other and their environments, forming intricate food webs. The scientific study of animals is known as zoology. Most living animal species are in Bilateria, a clade whose members have a bilaterally symmetric body plan. The Bilateria include the protostomes, containing animals such as nematodes, arthropods, flatworms, annelids and molluscs, and the deuterostomes, containing the echinode ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chordata
A chordate () is an animal of the phylum Chordata (). All chordates possess, at some point during their larval or adult stages, five synapomorphies, or primary physical characteristics, that distinguish them from all the other taxa. These five synapomorphies include a notochord, dorsal hollow nerve cord, endostyle or thyroid, pharyngeal slits, and a post-anal tail. The name “chordate” comes from the first of these synapomorphies, the notochord, which plays a significant role in chordate structure and movement. Chordates are also Bilateral symmetry, bilaterally symmetric, have a coelom, possess a circulatory system, and exhibit Metameric, metameric segmentation. In addition to the morphological characteristics used to define chordates, analysis of genome sequences has identified two conserved signature indels (CSIs) in their proteins: cyclophilin-like protein and mitochondrial inner membrane protease ATP23, which are exclusively shared by all vertebrates, tunicates and cep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Actinopterygii
Actinopterygii (; ), members of which are known as ray-finned fishes, is a class of bony fish. They comprise over 50% of living vertebrate species. The ray-finned fishes are so called because their fins are webs of skin supported by bony or horny spines (rays), as opposed to the fleshy, lobed fins that characterize the class Sarcopterygii (lobe-finned fish). These actinopterygian fin rays attach directly to the proximal or basal skeletal elements, the radials, which represent the link or connection between these fins and the internal skeleton (e.g., pelvic and pectoral girdles). By species count, actinopterygians dominate the vertebrates, and they constitute nearly 99% of the over 30,000 species of fish. They are ubiquitous throughout freshwater and marine environments from the deep sea to the highest mountain streams. Extant species can range in size from ''Paedocypris'', at , to the massive ocean sunfish, at , and the long-bodied oarfish, at . The vast majority of Actinopt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bony Fish
Osteichthyes (), popularly referred to as the bony fish, is a diverse superclass of fish that have skeletons primarily composed of bone tissue. They can be contrasted with the Chondrichthyes, which have skeletons primarily composed of cartilage. The vast majority of fish are members of Osteichthyes, which is an extremely diverse and abundant group consisting of 45 orders, and over 435 families and 28,000 species. It is the largest class of vertebrates in existence today. The group Osteichthyes is divided into the ray-finned fish ( Actinopterygii) and lobe-finned fish (Sarcopterygii). The oldest known fossils of bony fish are about 425 million years old, which are also transitional fossils, showing a tooth pattern that is in between the tooth rows of sharks and bony fishes. Osteichthyes can be compared to Euteleostomi. In paleontology the terms are synonymous. In ichthyology the difference is that Euteleostomi presents a cladistic view which includes the terrestrial tet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Komen Limestone
Komen (, it, Comen or ''Comeno'') is a settlement in Slovenia. It is the seat of the Municipality of Komen. It is located on the Karst Plateau in the Slovenian Littoral. Name Komen was attested in written sources in 1247 as ''Cominum'' (and as ''Cumin'' in 1255, ''de Cumino'' in 1269, and ''Comein'' in 1526). The name is probably derived from the Slavic common noun ''*komъ'' 'hill, mountain, elevation'. Derivation from the noun ''komin'' 'stove, chimney' is unlikely for accentual reasons. The Italian name, which is derived from the Slovene name, is given as ''Comen'' in older sources and ''Comeno'' in newer sources. History In the Middle Ages, it was first part of the Duchy of Friuli and in the 13th century it was included in the County of Gorizia. Komen was first mentioned in a document from 1247. In 1500, the whole region fell under Habsburg dominion and it was included in the County of Gorizia and Gradisca until 1918. During World War I, the western parts of the municipal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
English Chalk
The Chalk Group (often just called the Chalk) is the lithostratigraphic unit (a certain number of rock strata) which contains the Upper Cretaceous limestone succession in southern and eastern England. The same or similar rock sequences occur across the wider northwest European chalk ' province'. It is characterised by thick deposits of chalk, a soft porous white limestone, deposited in a marine environment. Chalk is a limestone that consists of coccolith biomicrite. A biomicrite is a limestone composed of fossil debris ("bio") and calcium carbonate mud (" micrite"). Most of the fossil debris in chalk consists of the microscopic plates, which are called coccoliths, of microscopic green algae known as coccolithophores. In addition to the coccoliths, the fossil debris includes a variable, but minor, percentage of the fragments of foraminifera, ostracods and mollusks. The coccolithophores lived in the upper part of the water column. When they died, the microscopic calcium ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
