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Paleodictyon
''Paleodictyon'' is a trace fossil, usually interpreted to be a burrow, which appears in the geologic marine record beginning in the Precambrian/Early Cambrian and in modern ocean environments.Swinbanks, D. D., 1982: ''Paleodictyon'': the traces of infaunal xenophyophores? Science, v. 218, 47-49. ''Paleodictyon'' were first described by Giuseppe Meneghini in 1850. The origin of the trace fossil is enigmatic and numerous candidates have been proposed. Description ''Paleodictyon'' consist of thin tunnels or ridges that usually form hexagonal or polygonal-shaped honeycomb-like network.KU Ichnology - Studying the Traces of Life IBGS Research Group Both irregular and regular nets are known throughout the stratigraphic range of ''Paleodictyon'', but it is the striking regular honeycomb patte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeodictyon
''Paleodictyon'' is a trace fossil, usually interpreted to be a burrow, which appears in the geologic marine record beginning in the Precambrian/Early Cambrian and in modern ocean environments.Swinbanks, D. D., 1982: ''Paleodictyon'': the traces of infaunal xenophyophores? Science, v. 218, 47-49. ''Paleodictyon'' were first described by Giuseppe Meneghini in 1850. The origin of the trace fossil is enigmatic and numerous candidates have been proposed. Description ''Paleodictyon'' consist of thin tunnels or ridges that usually form hexagonal or polygonal-shaped honeycomb-like network.KU Ichnology - Studying the Traces of Life IBGS Research Group Both irregular and regular nets are known throughout the stratigraphic range of ''Paleodictyon'', but it is the striking regular honeycomb patte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleodictyon P
''Paleodictyon'' is a trace fossil, usually interpreted to be a burrow, which appears in the geologic marine record beginning in the Precambrian/Early Cambrian and in modern ocean environments.Swinbanks, D. D., 1982: ''Paleodictyon'': the traces of infaunal xenophyophores? Science, v. 218, 47-49. ''Paleodictyon'' were first described by Giuseppe Meneghini in 1850. The origin of the trace fossil is enigmatic and numerous candidates have been proposed. Description ''Paleodictyon'' consist of thin tunnels or ridges that usually form hexagonal or polygonal-shaped honeycomb-like network.KU Ichnology - Studying the Traces of Life IBGS Research Group Both irregular and regular nets are known throughout the stratigraphic range of ''Paleodictyon'', but it is the striking regular honeycomb patte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleodictyon Nodosum
''Paleodictyon nodosum'' is a living creature thought to produce a certain form of burrow nearly identical to ''Paleodictyon'' fossils. The modern burrows were found around mid-ocean ridge systems in the Pacific and Atlantic Oceans. Although scientists have collected many of the burrows of ''Paleodictyon nodosum'', they have never seen a live one. What a live specimen would look like is widely debated, with the debate being split into two main sides. * Adolf Seilacher who discovered the original fossils of ''Paleodictyon nodosum'' hypothesizes that the creature is a worm-like species that burrows into the sediment around hydrothermal vents and deflects water flow through the burrows to catch food or farm its own food. * Peter A. Rona, discoverer of the modern burrows, suggests that ''Paleodictyon nodosum'' may actually be a large protist. There are other known examples of protists reaching the sizes that ''Paleodictyon'' reaches, and they are known to be infaunal. Scientists ra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Occultammina Sp
''Occultammina'' is a genus of xenophyophorean foraminifera known from the Atlantic and Pacific oceans. It is notable for being the first known infaunal xenophyophore as well as for being a possible identity for the enigmatic trace fossil ''Paleodictyon''. Distribution and habitat Like all other known xenophyophores, ''Occultammina'' is found in the deep ocean; the first known specimen was first discovered in 1980 at a depth of in the Ogasawara Trench, off the coast of Japan and described in 1982 by a joint research team from the University of Copenhagen and the University of Tokyo. Further specimens referred to ''Occultammina'' sp. have been found at a depth of in the Porcupine Abyssal Plain, in the North Atlantic. Further studies have expanded its geographical and bathymetric range from in the Ogasawara Trench and from in the North Atlantic, and also recorded its presence at in the Japan trench. ''Occultammina'' sp. has also been recovered at a depth of about near the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Occultammina
''Occultammina'' is a genus of xenophyophorean foraminifera known from the Atlantic and Pacific oceans. It is notable for being the first known infaunal xenophyophore as well as for being a possible identity for the enigmatic trace fossil ''Paleodictyon''. Distribution and habitat Like all other known xenophyophores, ''Occultammina'' is found in the deep ocean; the first known specimen was first discovered in 1980 at a depth of in the Izu–Ogasawara Trench, Ogasawara Trench, off the coast of Japan and described in 1982 by a joint research team from the University of Copenhagen and the University of Tokyo. Further specimens referred to ''Occultammina'' sp. have been found at a depth of in the Porcupine Abyssal Plain, in the North Atlantic. Further studies have expanded its geographical and bathymetric range from in the Ogasawara Trench and from in the North Atlantic, and also recorded its presence at in the Japan Trench, Japan trench. ''Occultammina'' sp. has also been rec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Xenophyophore
Xenophyophorea is a clade of foraminiferans. Members of this class are multinucleate unicellular organisms found on the ocean floor throughout the world's oceans, at depths of . They are a kind of foraminiferan that extract minerals from their surroundings and use them to form an exoskeleton known as a test. They were first described by Henry Bowman Brady in 1883. They are abundant on abyssal plains, and in some regions are the dominant species. Fifteen genera and 75 species have been described, varying widely in size. The largest, ''Syringammina fragilissima'', is among the largest known coenocytes, reaching up to in diameter. Naming and classification The name Xenophyophora means "bearer of foreign bodies", from the Greek. This refers to the sediments, called xenophyae, which are cemented together to construct their tests. In 1883, Henry Bowman Brady classified them as primitive Foraminifera. Later they were placed within the sponges. In the beginning of the 20th centur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Xenophyophorea
Xenophyophorea is a clade of foraminiferans. Members of this class are multinucleate unicellular organisms found on the ocean floor throughout the world's oceans, at depths of . They are a kind of foraminiferan that extract minerals from their surroundings and use them to form an exoskeleton known as a test. They were first described by Henry Bowman Brady in 1883. They are abundant on abyssal plains, and in some regions are the dominant species. Fifteen genera and 75 species have been described, varying widely in size. The largest, ''Syringammina fragilissima'', is among the largest known coenocytes, reaching up to in diameter. Naming and classification The name Xenophyophora means "bearer of foreign bodies", from the Greek. This refers to the sediments, called xenophyae, which are cemented together to construct their tests. In 1883, Henry Bowman Brady classified them as primitive Foraminifera. Later they were placed within the sponges. In the beginning of the 20th ce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Foraminifera
Foraminifera (; Latin for "hole bearers"; informally called "forams") are single-celled organisms, members of a phylum or class of amoeboid protists characterized by streaming granular Ectoplasm (cell biology), ectoplasm for catching food and other uses; and commonly an external shell (called a "Test (biology), test") of diverse forms and materials. Tests of chitin (found in some simple genera, and Textularia in particular) are believed to be the most primitive type. Most foraminifera are marine, the majority of which live on or within the seafloor sediment (i.e., are benthos, benthic), while a smaller number float in the water column at various depths (i.e., are planktonic), which belong to the suborder Globigerinina. Fewer are known from freshwater or brackish conditions, and some very few (nonaquatic) soil species have been identified through molecular analysis of small subunit ribosomal DNA. Foraminifera typically produce a test (biology), test, or shell, which can have eithe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanoes Of The Deep Sea
''Volcanoes of the Deep Sea'' is a 2003 documentary film in the IMAX format about undersea volcanoes directed by Stephen Low. Production Richard Lutz served as Principal Investigator and Lutz and Peter A. Rona served as Science Directors of the film, which was funded by the National Science Foundation and co-produced by Rutgers University. Content The film included footage, research, and stories from the deep-sea ''Alvin'' expeditions of Lutz and his colleagues. Scientists use the deep-water submersible DSV Alvin to search for an organism, the Paleodictyon nodosum maker, that produces a honeycomb patterned fossil called a Paleodictyon, near volcanic vents that lie 3500 meters (12,000 feet) underwater in the Mid-Atlantic Ridge. Reception The film received the award for "best IMAX film of the Year" at the Paris Film Festival, and in 2005 Richard Lutz received the Scientific Literacy Achievement Award from the New Jersey Association for Biomedical Research for his contribution ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adolf Seilacher
Adolf "Dolf" Seilacher (February 24, 1925 – April 26, 2014) was a German palaeontologist who worked in evolutionary and ecological palaeobiology for over 60 years. He is best known for his contributions to the study of trace fossils; constructional morphology and structuralism; biostratinomy, '' Lagerstätten'' and the Ediacaran biota. Career Seilacher worked for his doctorate under Otto Heinrich Schindewolf, at the University of Tübingen. He was also influenced by local palaeontologist Otto Linck. He served in World War II and resumed his studies at Tübingen, corresponding with the French ichnologist, Jacques Lessertisseur. Gaining his doctorate in 1951 on trace fossils, Seilacher moved to the University of Frankfurt (1957) and then the University of Baghdad before taking up a chair in palaeontology in Göttingen. He returned to Tübingen in 1964 as the successor to Schindewolf. After 1987 he held an Adjunct Professorship at Yale University. Significant work Seilacher's ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
DSV Alvin
''Alvin'' (DSV-2) is a crewed deep-ocean research submersible owned by the United States Navy and operated by the Woods Hole Oceanographic Institution (WHOI) in Woods Hole, Massachusetts. The vehicle was built by General Mills' Electronics Group in Minneapolis, Minnesota. Named to honor the prime mover and creative inspiration for the vehicle, Allyn Vine, ''Alvin'' was commissioned on 5 June 1964. The submersible is launched from the deep submergence support vessel , which is also owned by the U.S. Navy and operated by WHOI. The submersible has made more than 5,000 dives, carrying two scientists and a pilot, to observe the lifeforms that must cope with super-pressures and move about in total darkness, as well as exploring the wreck of ''Titanic''. Research conducted by ''Alvin'' has been featured in nearly 2,000 scientific papers. Design ''Alvin'' was designed as a replacement for bathyscaphes and other less maneuverable oceanographic vehicles. Its more nimble design was made ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mid-Atlantic Ridge
The Mid-Atlantic Ridge is a mid-ocean ridge (a divergent or constructive plate boundary) located along the floor of the Atlantic Ocean, and part of the longest mountain range in the world. In the North Atlantic, the ridge separates the North American from the Eurasian Plate and the African Plate, north and south of the Azores Triple Junction respectively. In the South Atlantic, it separates the African and South American plates. The ridge extends from a junction with the Gakkel Ridge (Mid-Arctic Ridge) northeast of Greenland southward to the Bouvet Triple Junction in the South Atlantic. Although the Mid-Atlantic Ridge is mostly an underwater feature, portions of it have enough elevation to extend above sea level, for example in Iceland. The ridge has an average spreading rate of about per year. Discovery A ridge under the northern Atlantic Ocean was first inferred by Matthew Fontaine Maury in 1853, based on soundings by the USS ''Dolphin''. The existence of the ridge and its ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
