Saudia(foram)
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Saudia(foram)
''Saudia'' is a genus of large discoidal to reniform (kidney shaped) forams, with a relatively thick test and complex interior, composed of agglutinated matter, or microgranular calcite. A.R.Loeblich & H.Tappan 1964. Sarcodina, Chiefly "Thecamoebians" and Foraminiferida. Treatise on Invertebrate Paleontology, Part C, Protista 2. Saudia is known from the Paleocene to middle Eocene of Saudi Arabia, Iraq and the balkans. Related genera include '' Vania'', '' Sornayina'', and '' Haurania''. References Loftusiida Prehistoric Foraminifera genera {{foraminifera-stub ...
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Spirocyclinidae
Spirocyclinidae is a family of foraminifera included in the order Loftusiida. Tests are variably discoidal, aggulitinated with calcareous or microgranular cement. Interiors are complex with chambers partially subdivided. Walls and septa are pierced with ramifying and anastomosing channels. The family presently includes the following genera; ''Spirocyclina'', ''Anchispirocyclina'', ''Haurania'', ''Martiguesia'', ''Pseudospirocyclina'', ''Qataria'', ''Reissella'', ''Saudia'', ''Sornayina'', ''Spiraloconulus'', ''Streptocyclammina'', ''Timidonella'', and '' Vania''. Previous the subfamily Spyrocylininae according to Loeblich and Tappan, 1964 in the Treatise on Invertebrate Paleontology which then included ''Spriocyclina'', ''Anchispirocyclina'', ''Orbitammiina'', and ''Sornayina''. '' Orbitammina'' has been moved to the textulariid Orbitopsellidae where it rests along with '' Orbitopsella'', '' Cyclorbitopsella'', and '' Labyrinthina''. Foraminifera, to which the Spirocyclinidae b ...
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Paleocene
The Paleocene, ( ) or Palaeocene, is a geological epoch (geology), epoch that lasted from about 66 to 56 mya (unit), million years ago (mya). It is the first epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name is a combination of the Ancient Greek ''palaiós'' meaning "old" and the Eocene Epoch (which succeeds the Paleocene), translating to "the old part of the Eocene". The epoch is bracketed by two major events in Earth's history. The K–Pg extinction event, brought on by Chicxulub impact, an asteroid impact and possibly volcanism, marked the beginning of the Paleocene and killed off 75% of living species, most famously the non-avian dinosaurs. The end of the epoch was marked by the Paleocene–Eocene Thermal Maximum (PETM), which was a major climatic event wherein about 2,500–4,500 gigatons of carbon were released into the atmosphere and ocean systems, causing a spike in global temperatures and ocean acidification. In the Pal ...
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Eocene
The Eocene ( ) Epoch is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', "dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope Carbon-13, 13C in the atmosphere was exceptionally low in comparison with the more common isotope Carbon-12, 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Popigai impact structure, Siberia and in what is now ...
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Eukaryota
Eukaryotes () are organisms whose Cell (biology), cells have a cell nucleus, nucleus. All animals, plants, fungi, and many unicellular organisms, are Eukaryotes. They belong to the group of organisms Eukaryota or Eukarya, which is one of the Three-domain system, three domains of life. Bacteria and Archaea (both prokaryotes) make up the other two domains. The eukaryotes are usually now regarded as having emerged in the Archaea or as a sister of the Asgard (archaea), Asgard archaea. This implies that there are only Two-domain system, two domains of life, Bacteria and Archaea, with eukaryotes incorporated among archaea. Eukaryotes represent a small minority of the number of organisms, but, due to their generally much larger size, their collective global biomass (ecology), biomass is estimated to be about equal to that of prokaryotes. Eukaryotes emerged approximately 2.3–1.8 billion years ago, during the Proterozoic eon, likely as Flagellated cell, flagellated phagotrophs. The ...
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SAR Supergroup
The SAR supergroup, also just SAR or Harosa, is a clade that includes stramenopiles (heterokonts), alveolates, and Rhizaria. The name is an acronym derived from the first letters of each of these clades; it has been alternatively spelled "RAS". The term "Harosa" (at the subkingdom level) has also been used. The SAR supergroup is a node-based taxon. Note that as a formal taxon, "Sar" has only its first letter capitalized, while the earlier abbreviation, SAR, retains all uppercase letters. Both names refer to the same group of organisms, unless further taxonomic revisions deem otherwise. Members of the SAR supergroup were once included under the separate supergroups Chromalveolata (Chromista and Alveolata) and Rhizaria, until phylogenetic studies confirmed that stramenopiles and alveolates diverged with Rhizaria. This apparently excluded haptophytes and cryptomonads, leading Okamoto ''et al.'' (2009) to propose the clade Hacrobia to accommodate them. Phylogeny Based on a compi ...
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Rhizaria
The Rhizaria are an ill-defined but species-rich supergroup of mostly unicellular eukaryotes. Except for the Chlorarachniophytes and three species in the genus Paulinella in the phylum Cercozoa, they are all non-photosynthethic, but many foraminifera and radiolaria have a symbiotic relationship with unicellular algae. A multicellular form, ''Guttulinopsis vulgaris'', a cellular slime mold, has also been described. This group was used by Cavalier-Smith in 2002, although the term "Rhizaria" had been long used for clades within the currently recognized taxon. Being described mainly from rDNA sequences, they vary considerably in form, having no clear morphological distinctive characters (synapomorphies), but for the most part they are amoeboids with filose, reticulose, or microtubule-supported pseudopods. In the absence of an apomorphy, the group is ill-defined, and its composition has been very fluid. Some Rhizaria possess mineral exoskeleton (thecae or loricas), which is in differ ...
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Retaria
Retaria is a clade within the supergroup Rhizaria containing the Foraminifera and the Radiolaria. In 2019, the Retaria were recognized as a basal Rhizaria group, as sister of the Cercozoa Cercozoa is a phylum of diverse single-celled eukaryotes. They lack shared morphological characteristics at the microscopic level, and are instead defined by molecular phylogenies of rRNA and actin or polyubiquitin. They were the first major eu .... References External links Taxa named by Thomas Cavalier-Smith SAR supergroup phyla {{Retaria-stub ...
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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 ...
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Textulariia
Globothalamea comprises a class of multichambered foraminifera based in part on SSU rDNA evidence; the other is Tubothalamea. Six orders are included, which vary notably in composition, wall structure, and chamber arrangement. The Lituolida, Loftusiida, and Textulariida (as emended) have tests (shells) of agglutinated matter, glued together by various cements, but differ in chamber arrangement, wall structure, and complexity. In contrast the Carterinida, Robertinida and Rotaliida, with buliminids lumped into the Rotaliida, have calcareous tests. Those of rotaliid genera, which vary considerably, are of perforate hyaline (glassy) calcite. in contrast the Carterinida have tests composed of bundled calcite spicules. The Robertida differ in being composed, instead, of aragonite. Foraminifera genera and their descri ...
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Loftusiida
Loftusiida is an order of foraminifers in the class Globothalamea. Subtaxa Suborder Ataxophragmiina * Superfamily Ataxophragmioidea ** Family Ataxophragmiidae ** Family † Cuneolinidae ** Family Dictyopsellidae ** Family Dicyclinidae ** Family Globotextulariidae ** Family Montsaleviidae ** Family Textulariellidae Suborder Biokovinina * Superfamily Biokovinoidea (Biokovinacea) ** Family Biokovinidae ** Family Charentiidae ** Family Lituoliporidae * Superfamily Coscinophragmatoidea ** Family Coscinophragmatidae ** Family Haddoniidae Suborder Cyclolinina * Superfamily Cyclolinoidea ** Family Cyclolinidae Suborder Loftusiina * Superfamily Haplophragmioidea ** Family Cribratinidae ** Family Haplophragmiidae ** Family Labyrinthidomatidae * Superfamily Loftusioidea (Loftusiacea) ** Family Cyclamminidae ** Family Ecougellidae ** Family Everticyclamminidae ** Family Hottingeritidae ** Family Loftusiidae ** Family Mesoendothyridae ** Family Spirocyclini ...
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Vania (foram)
''Vania'' is a genus of benthic forams from the upper Paleocene of Turkey with a large discoidal test up to 6.5mm in diameter. The microspheric test begins with a short planispiral stage, later chambers spreading successively from flabelliform (fan-shaped) to reniform (kidney-shaped) and finally annular. The interior is subdivided by radial primary beams intercalated with secondary beams. The wall finely agglutinated, imperforate; aperture, two alternating rows of pores on the periphery. References ''Vania'' in GSI Paleontology Loftusiida Prehistoric Foraminifera genera Paleocene life {{foraminifera-stub ...
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