1.
The Meerkats
–
The Meerkats, also known as Meerkats, The Movie, is a feature-length 2008 British wildlife fiction film which anthropomorphises the daily struggles of a clan of meerkats in the Kalahari Desert. It was produced by BBC Films and The Weinstein Company, and it is the debut directorial feature of James Honeyborne, previously a producer of natural history programmes for television. The worldwide premiere was held at the Dinard Film Festival, France in October 2008, the film was released in 2009, on 7 August in the UK. A US date has not yet been announced and this was dedicated to actor Paul Newman, who died in 2008, shortly before this movie was released. The documentary follows the adventure of a meerkat who is forced to leave his home by a group of meerkats who wanted more territory. Lost in the African savannah, he tries to reunite with his family, but encounters large, fierce, the Meerkats was announced in November 2006 as BBC Films and The Weinstein Company agreed a co-financing deal for the film, with The Weinstein Company also handling international distribution. The year-long principal photography began on location in the Kalahari Desert, the script was written by Alexander McCall Smith, author of many books set in Botswana. Paul Newman provides the narration, which was recorded at a studio near his home shortly before his death, the Meerkats was the final film credit of Newmans long career. Meerkat Manor, The Story Begins, a second feature-length wildlife film on meerkats, was released in 2008. It was produced by Animal Planet, Discovery Films and Oxford Scientific Films, the makers of Meerkat Manor, BBC Films Joe Oppenheimer, a producer of The Meerkats, has stated that the two films are very different in character. James Honeyborne has described The Meerkats as a stand-alone, blue-chip wildlife film from the ground up, there will be a huge sense of place on a massive scale. You will really see real wild animals, writing in The Guardian reviewer Philip French noted that the. Nature movie made in the Kalahari desert has some good footage but is more Disney-anthropomorphic than Attenborough-authentic, official website The Meerkats at the Internet Movie Database The Meerkats at Rotten Tomatoes
2.
Pliocene
–
The Pliocene Epoch is the epoch in the geologic timescale that extends from 5.333 million to 2.58 million years BP. It is the second and youngest epoch of the Neogene Period in the Cenozoic Era, the Pliocene follows the Miocene Epoch and is followed by the Pleistocene Epoch.588 to 1.806 million years ago, and is now included in the Pleistocene. As with other geologic periods, the geological strata that define the start and end are well identified but the exact dates of the start. The boundaries defining the Pliocene are not set at an easily identified worldwide event, the upper boundary was set at the start of the Pleistocene glaciations. The Pliocene was named by Sir Charles Lyell, the name comes from the Greek words πλεῖον and καινός and means roughly continuation of the recent, referring to the essentially modern marine mollusc faunas. H. W. Fowler called the term a regrettable barbarism, in the official timescale of the ICS, the Pliocene is subdivided into two stages. From youngest to oldest they are, Piacenzian Zanclean The Piacenzian is sometimes referred to as the Late Pliocene, in the system of North American Land Mammal Ages include Hemphillian, and Blancan. The Blancan extends forward into the Pleistocene, South American Land Mammal Ages include Montehermosan, Chapadmalalan and Uquian. In the Paratethys area the Pliocene contains the Dacian and Romanian stages, as usual in stratigraphy, there are many other regional and local subdivisions in use. In Britain the Pliocene is divided into the stages, Gedgravian, Waltonian, Pre-Ludhamian, Ludhamian, Thurnian, Bramertonian or Antian, Pre-Pastonian or Baventian, Pastonian and Beestonian. The exact correlations between these stages and the ICS stages is still a matter of detail. The formation of an Arctic ice cap is signaled by a shift in oxygen isotope ratios and ice-rafted cobbles in the North Atlantic. Mid-latitude glaciation was probably underway before the end of the epoch, the global cooling that occurred during the Pliocene may have spurred on the disappearance of forests and the spread of grasslands and savannas. Continents continued to drift, moving from positions possibly as far as 250 km from their present locations to positions only 70 km from their current locations, africas collision with Europe formed the Mediterranean Sea, cutting off the remnants of the Tethys Ocean. The border between the Miocene and the Pliocene is also the time of the Messinian salinity crisis, Sea level changes exposed the land-bridge between Alaska and Asia. Pliocene marine rocks are exposed in the Mediterranean, India. Elsewhere, they are exposed largely near shores, the change to a cooler, dry, seasonal climate had considerable impacts on Pliocene vegetation, reducing tropical species worldwide. Deciduous forests proliferated, coniferous forests and tundra covered much of the north, tropical forests were limited to a tight band around the equator, and in addition to dry savannahs, deserts appeared in Asia and Africa
3.
Precambrian
–
The Precambrian is the earliest period of Earths history, set before the current Phanerozoic Eon. The Precambrian is a supereon that is subdivided into three eons of the time scale. It spans from the formation of Earth about 4.6 billion years ago to the beginning of the Cambrian Period, about 541 million years ago, the Precambrian accounts for 89% of geologic time. Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earths history, the Precambrian fossil record is poorer than that of the succeeding Phanerozoic, and fossils from that time are of limited biostratigraphic use. This is because many Precambrian rocks have been metamorphosed, obscuring their origins, while others have been destroyed by erosion. A stable crust was apparently in place by 4,412 Ma, the term Precambrian is recognized by the International Commission on Stratigraphy as a general term including the Archean and Proterozoic eons. It is still used by geologists and paleontologists for general discussions not requiring the more specific eon names and it was briefly called the Cryptozoic eon. A specific date for the origin of life has not been determined, carbon found in 3.8 billion year old rocks from islands off western Greenland may be of organic origin. Well-preserved microscopic fossils of bacteria older than 3.46 billion years have found in Western Australia. Probable fossils 100 million years older have been found in the same area, there is a fairly solid record of bacterial life throughout the remainder of the Precambrian. The oldest fossil evidence from that era of such complex life comes from the Lantian formation of the Ediacarian period, a very diverse collection of soft-bodied forms is found in a variety of locations worldwide and date to between 635 and 542 Ma. These are referred to as Ediacaran or Vendian biota, hard-shelled creatures appeared toward the end of that time span, marking the beginning of the Phanerozoic era. By the middle of the following Cambrian period, a diverse fauna is recorded in the Burgess Shale. The explosion in diversity of lifeforms during the early Cambrian is called the Cambrian explosion of life, while land seems to have been devoid of plants and animals, cyanobacteria and other microbes formed prokaryotic mats that covered terrestrial areas. Evidence of the details of plate motions and other activity in the Precambrian has been poorly preserved. It is generally believed that small proto-continents existed prior to 4280 Ma, the supercontinent, known as Rodinia, broke up around 750 Ma. A number of glacial periods have been identified going as far back as the Huronian epoch, one of the best studied is the Sturtian-Varangian glaciation, around 850–635 Ma, which may have brought glacial conditions all the way to the equator, resulting in a Snowball Earth. The atmosphere of the early Earth is not well understood, most geologists believe it was composed primarily of nitrogen, carbon dioxide, and other relatively inert gases, and was lacking in free oxygen
4.
Cambrian
–
The Cambrian Period was the first geological period of the Paleozoic Era, of the Phanerozoic Eon. The Cambrian lasted 55.6 million years from the end of the preceding Ediacaran Period 541 million years ago to the beginning of the Ordovician Period 485.4 mya and its subdivisions, and its base, are somewhat in flux. The period was established by Adam Sedgwick, who named it after Cambria, the Latinised form of Cymru, the Welsh name for Wales, as a result, our understanding of the Cambrian biology surpasses that of some later periods. The rapid diversification of lifeforms in the Cambrian, known as the Cambrian explosion, most of the continents were probably dry and rocky due to a lack of vegetation. Shallow seas flanked the margins of several continents created during the breakup of the supercontinent Pannotia, the seas were relatively warm, and polar ice was absent for much of the period. The United States Federal Geographic Data Committee uses a barred capital C ⟨Є⟩ character similar to the capital letter Ukrainian Ye ⟨Є⟩ to represent the Cambrian Period, the proper Unicode character is U+A792 Ꞓ LATIN CAPITAL LETTER C WITH BAR. Despite the long recognition of its distinction from younger Ordovician Period rocks and older Supereon Precambrian rocks, the base of the Cambrian lies atop a complex assemblage of trace fossils known as the Treptichnus pedum assemblage. Pedum in Namibia, Spain and Newfoundland, and possibly, in the western USA, the stratigraphic range of T. pedum overlaps the range of the Ediacaran fossils in Namibia, and probably in Spain. The Cambrian Period followed the Ediacaran Period and was followed by the Ordovician Period, the Cambrian is divided into four epochs and ten ages. Currently only two series and five stages are named and have a GSSP, because the international stratigraphic subdivision is not yet complete, many local subdivisions are still widely used. In some of these subdivisions the Cambrian is divided into three epochs with locally differing names – the Early Cambrian, Middle Cambrian and Furongian, rocks of these epochs are referred to as belonging to the Lower, Middle, or Upper Cambrian. Trilobite zones allow biostratigraphic correlation in the Cambrian, each of the local epochs is divided into several stages. The International Commission on Stratigraphy list the Cambrian period as beginning at 541 million years ago, the lower boundary of the Cambrian was originally held to represent the first appearance of complex life, represented by trilobites. The recognition of small shelly fossils before the first trilobites, and Ediacara biota substantially earlier and this formal designation allowed radiometric dates to be obtained from samples across the globe that corresponded to the base of the Cambrian. Early dates of 570 million years ago quickly gained favour, though the used to obtain this number are now considered to be unsuitable. A more precise date using modern radiometric dating yield a date of 541 ±0.3 million years ago, most continental land was clustered in the Southern Hemisphere at this time, but was drifting north. Large, high-velocity rotational movement of Gondwana appears to have occurred in the Early Cambrian, the sea levels fluctuated somewhat, suggesting there were ice ages, associated with pulses of expansion and contraction of a south polar ice cap. In Baltoscandia a Lower Cambrian transgression transformed large swathes of the Sub-Cambrian peneplain into a epicontinental sea, the Earth was generally cold during the early Cambrian, probably due to the ancient continent of Gondwana covering the South Pole and cutting off polar ocean currents
5.
Ordovician
–
The Ordovician is a geologic period and system, the second of six periods of the Paleozoic Era. The Ordovician spans 41.2 million years from the end of the Cambrian Period 485.4 million years ago to the start of the Silurian Period 443.8 Mya. Lapworth recognized that the fauna in the disputed strata were different from those of either the Cambrian or the Silurian periods. It received international sanction in 1960, when it was adopted as a period of the Paleozoic Era by the International Geological Congress. Life continued to flourish during the Ordovician as it did in the earlier Cambrian period, invertebrates, namely molluscs and arthropods, dominated the oceans. The Great Ordovician Biodiversification Event considerably increased the diversity of life, fish, the worlds first true vertebrates, continued to evolve, and those with jaws may have first appeared late in the period. Life had yet to diversify on land, about 100 times as many meteorites struck the Earth during the Ordovician compared with today. The Ordovician Period began with a major extinction called the Cambrian–Ordovician extinction event and it lasted for about 42 million years and ended with the Ordovician–Silurian extinction event, about 443.8 Mya which wiped out 60% of marine genera. The dates given are recent radiometric dates and vary slightly from those found in other sources and this second period of the Paleozoic era created abundant fossils that became major petroleum and gas reservoirs. The boundary chosen for the beginning of both the Ordovician Period and the Tremadocian stage is highly significant and it correlates well with the occurrence of widespread graptolite, conodont, and trilobite species. The base of the Tremadocian allows scientists to relate these species not only to each other and this makes it easier to place many more species in time relative to the beginning of the Ordovician Period. A number of terms have been used to subdivide the Ordovician Period. In 2008, the ICS erected an international system of subdivisions. There exist Baltoscandic, British, Siberian, North American, Australian, the Ordovician Period in Britain was traditionally broken into Early, Middle and Late epochs. The corresponding rocks of the Ordovician System are referred to as coming from the Lower, Middle, the Floian corresponds to the lower Arenig, the Arenig continues until the early Darriwilian, subsuming the Dapingian. The Llanvirn occupies the rest of the Darriwilian, and terminates with it at the base of the Late Ordovician. The Sandbian represents the first half of the Caradoc, the Caradoc ends in the mid-Katian, during the Ordovician, the southern continents were collected into Gondwana. Gondwana started the period in equatorial latitudes and, as the period progressed, drifted toward the South Pole, the small continent Avalonia separated from Gondwana and began to move north towards Baltica and Laurentia, opening the Rheic Ocean between Gondwana and Avalonia
6.
Silurian
–
The Silurian is a geologic period and system spanning 24.6 million years from the end of the Ordovician Period, at 443.8 million years ago, to the beginning of the Devonian Period,419.2 Mya. As with other periods, the rock beds that define the periods start and end are well identified. The base of the Silurian is set at a major Ordovician-Silurian extinction event when 60% of marine species were wiped out, a significant evolutionary milestone during the Silurian was the diversification of jawed and bony fish. However, terrestrial life would not greatly diversify and affect the landscape until the Devonian, the Silurian system was first identified by British geologist Sir Roderick Impey Murchison, who was examining fossil-bearing sedimentary rock strata in south Wales in the early 1830s. He named the sequences for a Celtic tribe of Wales, the Silures, inspired by his friend Adam Sedgwick and this naming does not indicate any correlation between the occurrence of the Silurian rocks and the land inhabited by the Silures. As it was first identified, the Silurian series when traced farther afield quickly came to overlap Sedgwicks Cambrian sequence, however, charles Lapworth resolved the conflict by defining a new Ordovician system including the contested beds. An early alternative name for the Silurian was Gotlandian after the strata of the Baltic island of Gotland, the French geologist Joachim Barrande, building on Murchisons work, used the term Silurian in a more comprehensive sense than was justified by subsequent knowledge. He divided the Silurian rocks of Bohemia into eight stages and his interpretation was questioned in 1854 by Edward Forbes, and the later stages of Barrande, F, G and H, have since been shown to be Devonian. Despite these modifications in the groupings of the strata, it is recognized that Barrande established Bohemia as a classic ground for the study of the earliest fossils. The epoch is named for the town of Llandovery in Carmarthenshire, the Wenlock, which lasted from 433.4 ±1.5 to 427.4 ±2.8 mya, is subdivided into the Sheinwoodian and Homerian ages. It is named after Wenlock Edge in Shropshire, England, during the Wenlock, the oldest known tracheophytes of the genus Cooksonia, appear. The first terrestrial animals also appear in the Wenlock, represented by air-breathing millipedes from Scotland. The Ludlow, lasting from 427.4 ±1.5 to 423 ±2.8 mya, comprises the Gorstian stage, lasting until 425.6 million years ago, and it is named for the town of Ludlow in Shropshire, England. The Pridoli, lasting from 423 ±1.5 to 419.2 ±2.8 mya, is the final and it is named after one locality at the Homolka a Přídolí nature reserve near the Prague suburb Slivenec in the Czech Republic. Přídolí is the old name of a field area. The high sea levels of the Silurian and the flat land resulted in a number of island chains. The southern continents remained united during this period, the melting of icecaps and glaciers contributed to a rise in sea level, recognizable from the fact that Silurian sediments overlie eroded Ordovician sediments, forming an unconformity. The continents of Avalonia, Baltica, and Laurentia drifted together near the equator and this event is the Caledonian orogeny, a spate of mountain building that stretched from New York State through conjoined Europe and Greenland to Norway
7.
Devonian
–
The Devonian is a geologic period and system of the Paleozoic, spanning 60 million years from the end of the Silurian,419.2 million years ago, to the beginning of the Carboniferous,358.9 Mya. It is named after Devon, England, where rocks from this period were first studied, the first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents, by the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. Various terrestrial arthropods also became well-established, Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fish. The first ray-finned and lobe-finned bony fish appeared, while the placodermi began dominating almost every aquatic environment. The ancestors of all four-limbed vertebrates began adapting to walking on land, as their strong pectoral, in the oceans, primitive sharks became more numerous than in the Silurian and Late Ordovician. The first ammonites, species of molluscs, appeared, trilobites, the mollusk-like brachiopods and the great coral reefs, were still common. The Late Devonian extinction which started about 375 million years ago severely affected marine life, killing off all placodermi, and all trilobites, save for a few species of the order Proetida. The palaeogeography was dominated by the supercontinent of Gondwana to the south, the continent of Siberia to the north, while the rock beds that define the start and end of the Devonian period are well identified, the exact dates are uncertain. According to the International Commission on Stratigraphy, the Devonian extends from the end of the Silurian 419.2 Mya, another common term is Age of the Fishes, referring to the evolution of several major groups of fish that took place during the period. Older literature on the Anglo-Welsh basin divides it into the Downtonian, Dittonian, Breconian and Farlovian stages, in the Late Devonian, by contrast, arid conditions were less prevalent across the world and temperate climates were more common. The Devonian Period is formally broken into Early, Middle and Late subdivisions, the rocks corresponding to those epochs are referred to as belonging to the Lower, Middle and Upper parts of the Devonian System. Early Devonian The Early Devonian lasted from 419.2 ±2.8 to 393.3 ±2.5 and began with the Lochkovian stage, which lasted until the Pragian. It spanned from 410.8 ±2.8 to 407.6 ±2.5, and was followed by the Emsian, which lasted until the Middle Devonian began,393. 3±2.7 million years ago. Middle Devonian The Middle Devonian comprised two subdivisions, first the Eifelian, which gave way to the Givetian 387. 7±2.7 million years ago. Late Devonian Finally, the Late Devonian started with the Frasnian,382.7 ±2.8 to 372.2 ±2.5, during which the first forests took shape on land. The first tetrapods appeared in the record in the ensuing Famennian subdivision. This lasted until the end of the Devonian,358. 9±2.5 million years ago, the Devonian was a relatively warm period, and probably lacked any glaciers
8.
Carboniferous
–
The Carboniferous is a geologic period and system that spans 60 million years from the end of the Devonian Period 358.9 million years ago, to the beginning of the Permian Period,298.9 Mya. The name Carboniferous means coal-bearing and derives from the Latin words carbō and ferō, and was coined by geologists William Conybeare and William Phillips in 1822. Based on a study of the British rock succession, it was the first of the system names to be employed. The Carboniferous is often treated in North America as two periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial life was established by the Carboniferous period. Amphibians were the dominant land vertebrates, of one branch would eventually evolve into amniotes. Arthropods were also common, and many were much larger than those of today. Vast swaths of forest covered the land, which would eventually be laid down, the atmospheric content of oxygen also reached their highest levels in geological history during the period, 35% compared with 21% today, allowing terrestrial invertebrates to evolve to great size. A major marine and terrestrial extinction event, the Carboniferous rainforest collapse, occurred in the middle of the period, the later half of the period experienced glaciations, low sea level, and mountain building as the continents collided to form Pangaea. In the United States the Carboniferous is usually broken into Mississippian and Pennsylvanian subperiods, the Silesian is roughly contemporaneous with the late Mississippian Serpukhovian plus the Pennsylvanian. In Britain the Dinantian is traditionally known as the Carboniferous Limestone, the Namurian as the Millstone Grit, and the Westphalian as the Coal Measures and Pennant Sandstone. There was also a drop in south polar temperatures, southern Gondwanaland was glaciated throughout the period and these conditions apparently had little effect in the deep tropics, where lush swamps, later to become coal, flourished to within 30 degrees of the northernmost glaciers. Mid-Carboniferous, a drop in sea level precipitated a major extinction, one that hit crinoids. This sea level drop and the unconformity in North America separate the Mississippian subperiod from the Pennsylvanian subperiod. This happened about 323 million years ago, at the onset of the Permo-Carboniferous Glaciation, the Carboniferous was a time of active mountain-building, as the supercontinent Pangaea came together. The southern continents remained tied together in the supercontinent Gondwana, which collided with North America–Europe along the present line of eastern North America, in the same time frame, much of present eastern Eurasian plate welded itself to Europe along the line of the Ural mountains. Most of the Mesozoic supercontinent of Pangea was now assembled, although North China, the Late Carboniferous Pangaea was shaped like an O. There were two major oceans in the Carboniferous—Panthalassa and Paleo-Tethys, which was inside the O in the Carboniferous Pangaea, other minor oceans were shrinking and eventually closed - Rheic Ocean, the small, shallow Ural Ocean and Proto-Tethys Ocean
9.
Permian
–
The Permian is a geologic period and system which spans 46.7 million years from the end of the Carboniferous Period 298.9 million years ago, to the beginning of the Triassic Period 252.2 Mya. It is the last period of the Paleozoic Era, the following Triassic Period belongs to the Mesozoic Era, the concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the city of Perm. The Permian witnessed the diversification of the early amniotes into the groups of the mammals, turtles, lepidosaurs. The world at the time was dominated by two known as Pangaea and Siberia, surrounded by a global ocean called Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior, amniotes, who could better cope with these drier conditions, rose to dominance in place of their amphibian ancestors. The Permian ended with the Permian–Triassic extinction event, the largest mass extinction in Earths history, in which nearly 90% of marine species and it would take well into the Triassic for life to recover from this catastrophe. Recovery from the Permian-Triassic extinction event was protracted, on land, the term Permian was introduced into geology in 1841 by Sir R. I. Murchison, president of the Geological Society of London, who identified typical strata in extensive Russian explorations undertaken with Edouard de Verneuil, the region now lies in the Perm Krai of Russia. This could have in part caused the extinctions of marine species at the end of the period by severely reducing shallow coastal areas preferred by many marine organisms. During the Permian, all the Earths major landmasses were collected into a supercontinent known as Pangaea. The Cimmeria continent rifted away from Gondwana and drifted north to Laurasia, a new ocean was growing on its southern end, the Tethys Ocean, an ocean that would dominate much of the Mesozoic Era. Large continental landmass interiors experience climates with extreme variations of heat and cold, deserts seem to have been widespread on Pangaea. Such dry conditions favored gymnosperms, plants with seeds enclosed in a cover, over plants such as ferns that disperse spores in a wetter environment. The first modern trees appeared in the Permian, the climate in the Permian was quite varied. At the start of the Permian, the Earth was still in an Ice Age, glaciers receded around the mid-Permian period as the climate gradually warmed, drying the continents interiors. In the late Permian period, the drying continued although the temperature cycled between warm and cool cycles, Permian marine deposits are rich in fossil mollusks, echinoderms, and brachiopods. By the close of the Permian, trilobites and a host of other groups became extinct. Terrestrial life in the Permian included diverse plants, fungi, arthropods, the period saw a massive desert covering the interior of Pangaea
10.
Triassic
–
The Triassic is a geologic period and system which spans 50.9 million years from the end of the Permian Period 252.17 million years ago, to the beginning of the Jurassic Period 201.3 Mya. The Triassic is the first period of the Mesozoic Era, both the start and end of the period are marked by major extinction events. Therapsids and archosaurs were the terrestrial vertebrates during this time. A specialized subgroup of archosaurs, called dinosaurs, first appeared in the Late Triassic, the vast supercontinent of Pangaea existed until the mid-Triassic, after which it began to gradually rift into two separate landmasses, Laurasia to the north and Gondwana to the south. The global climate during the Triassic was mostly hot and dry, however, the climate shifted and became more humid as Pangaea began to drift apart. The end of the period was marked by yet another mass extinction, the Triassic-Jurassic extinction event. The Triassic is usually separated into Early, Middle, and Late Triassic Epochs, from the east, along the equator, the Tethys sea penetrated Pangaea, causing the Paleo-Tethys Ocean to be closed. Later in the mid-Triassic a similar sea penetrated along the equator from the west, the remaining shores were surrounded by the world-ocean known as Panthalassa. All the deep-ocean sediments laid down during the Triassic have disappeared through subduction of oceanic plates, thus, the supercontinent Pangaea was rifting during the Triassic—especially late in that period—but had not yet separated. In North America, for example, marine deposits are limited to a few exposures in the west, thus Triassic stratigraphy is mostly based on organisms that lived in lagoons and hypersaline environments, such as Estheria crustaceans. At the beginning of the Mesozoic Era, Africa was joined with Earths other continents in Pangaea, Africa shared the supercontinents relatively uniform fauna which was dominated by theropods, prosauropods and primitive ornithischians by the close of the Triassic period. Late Triassic fossils are found throughout Africa, but are common in the south than north. The time boundary separating the Permian and Triassic marks the advent of an event with global impact. At Paleorrota geopark, located in Rio Grande do Sul, Brazil, in these formations, one of the earliest dinosaurs, Staurikosaurus, as well as the mammal ancestors Brasilitherium and Brasilodon have been discovered. The Triassic continental interior climate was hot and dry, so that typical deposits are red bed sandstones and evaporites. Pangaeas large size limited the effect of the global ocean, its continental climate was highly seasonal, with very hot summers. The strong contrast between the Pangea supercontinent and the global ocean triggered intense cross-equatorial monsoons, the best studied of such episodes of humid climate, and probably the most intense and widespread, was the Carnian Pluvial Event. On land, the vascular plants included the lycophytes, the dominant cycadophytes, ginkgophyta, ferns, horsetails
11.
Jurassic
–
The Jurassic is a geologic period and system that spans 56.3 million years from the end of the Triassic Period 201.3 million years ago to the beginning of the Cretaceous Period 145 Mya. The Jurassic constitutes the middle period of the Mesozoic Era, also known as the Age of Reptiles, the start of the period is marked by the major Triassic–Jurassic extinction event. The Jurassic is named after the Jura Mountains within the European Alps, by the beginning of the Jurassic, the supercontinent Pangaea had begun rifting into two landmasses, Laurasia to the north and Gondwana to the south. This created more coastlines and shifted the continental climate from dry to humid, on land, the fauna transitioned from the Triassic fauna, dominated by both dinosauromorph and crocodylomorph archosaurs, to one dominated by dinosaurs alone. The first birds also appeared during the Jurassic, having evolved from a branch of theropod dinosaurs, other major events include the appearance of the earliest lizards, and the evolution of therian mammals, including primitive placentals. Crocodilians made the transition from a terrestrial to a mode of life. The oceans were inhabited by marine reptiles such as ichthyosaurs and plesiosaurs, the chronostratigraphic term Jurassic is directly linked to the Jura Mountains. The name Jura is derived from the Celtic root jor, which was Latinised into juria, the Jurassic period is divided into the Early Jurassic, Middle, and Late Jurassic epochs. The Jurassic System, in stratigraphy, is divided into the Lower Jurassic, Middle, the separation of the term Jurassic into three sections goes back to Leopold von Buch. The Jurassic North Atlantic Ocean was relatively narrow, while the South Atlantic did not open until the following Cretaceous period, the Tethys Sea closed, and the Neotethys basin appeared. Climates were warm, with no evidence of glaciation, as in the Triassic, there was apparently no land over either pole, and no extensive ice caps existed. In contrast, the North American Jurassic record is the poorest of the Mesozoic, the Jurassic was a time of calcite sea geochemistry in which low-magnesium calcite was the primary inorganic marine precipitate of calcium carbonate. Carbonate hardgrounds were thus very common, along with calcitic ooids, calcitic cements, the first of several massive batholiths were emplaced in the northern American cordillera beginning in the mid-Jurassic, marking the Nevadan orogeny. Important Jurassic exposures are found in Russia, India, South America, Japan, Australasia. As the Jurassic proceeded, larger and more groups of dinosaurs like sauropods and ornithopods proliferated in Africa. Middle Jurassic strata are well represented nor well studied in Africa. Late Jurassic strata are also poorly represented apart from the spectacular Tendaguru fauna in Tanzania, the Late Jurassic life of Tendaguru is very similar to that found in western North Americas Morrison Formation. During the Jurassic period, the primary living in the sea were fish
12.
Cretaceous
–
The Cretaceous is a geologic period and system that spans 79 million years from the end of the Jurassic Period 145 million years ago to the beginning of the Paleogene Period 66 Mya. It is the last period of the Mesozoic Era, the Cretaceous Period is usually abbreviated K, for its German translation Kreide. The Cretaceous was a period with a warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites and rudists, during this time, new groups of mammals and birds, as well as flowering plants, appeared. The Cretaceous ended with a mass extinction, the Cretaceous–Paleogene extinction event, in which many groups, including non-avian dinosaurs, pterosaurs. The end of the Cretaceous is defined by the abrupt Cretaceous–Paleogene boundary, the name Cretaceous was derived from Latin creta, meaning chalk. The Cretaceous is divided into Early and Late Cretaceous epochs, or Lower and Upper Cretaceous series, in older literature the Cretaceous is sometimes divided into three series, Neocomian, Gallic and Senonian. A subdivision in eleven stages, all originating from European stratigraphy, is now used worldwide, in many parts of the world, alternative local subdivisions are still in use. As with other geologic periods, the rock beds of the Cretaceous are well identified. No great extinction or burst of diversity separates the Cretaceous from the Jurassic and this layer has been dated at 66.043 Ma. A140 Ma age for the Jurassic-Cretaceous boundary instead of the usually accepted 145 Ma was proposed in 2014 based on a study of Vaca Muerta Formation in Neuquén Basin. Víctor Ramos, one of the authors of the study proposing the 140 Ma boundary age sees the study as a first step toward formally changing the age in the International Union of Geological Sciences, due to the high sea level there was extensive space for such sedimentation. Because of the young age and great thickness of the system. Chalk is a type characteristic for the Cretaceous. It consists of coccoliths, microscopically small calcite skeletons of coccolithophores, the group is found in England, northern France, the low countries, northern Germany, Denmark and in the subsurface of the southern part of the North Sea. Chalk is not easily consolidated and the Chalk Group still consists of sediments in many places. The group also has other limestones and arenites, among the fossils it contains are sea urchins, belemnites, ammonites and sea reptiles such as Mosasaurus. In southern Europe, the Cretaceous is usually a marine system consisting of competent limestone beds or incompetent marls
13.
Paleogene
–
The Paleogene is a geologic period and system that spans 43 million years from the end of the Cretaceous Period 66 million years ago to the beginning of the Neogene Period 23.03 Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon and this period consists of the Paleocene, Eocene and Oligocene epochs. The terms Paleogene System and lower Tertiary System are applied to the rocks deposited during the Paleogene Period. By dividing the Tertiary Period into two periods instead of directly into five epochs, the periods are more comparable to the duration of periods of the preceding Mesozoic and Paleozoic Eras. The trend was caused by the formation of the Antarctic Circumpolar Current. During the Paleogene, the continued to drift closer to their current positions. India was in the process of colliding with Asia, subsequently forming the Himalayas, the Atlantic Ocean continued to widen by a few centimeters each year. Africa was moving north to meet with Europe and form the Mediterranean, inland seas retreated from North America early in the period. Australia had also separated from Antarctica and was drifting towards Southeast Asia, mammals began a rapid diversification during this period. Some of these mammals would evolve into forms that would dominate the land, while others would become capable of living in marine, specialized terrestrial. Those that took to the oceans became modern cetaceans, while those that took to the trees became primates, the group to which humans belong. Birds, which were well established by the end of the Cretaceous. In comparison to birds and mammals, most other branches of life remained unchanged during this period. As the Earth cooled, tropical plants became less numerous and were now restricted to equatorial regions, deciduous plants, which could survive through the seasonal climates the world was now experiencing, became more common. The Paleogene is notable in the context of offshore oil drilling, and especially in Gulf of Mexico oil exploration and these rock formations represent the current cutting edge of deep-water oil discovery. Lower Tertiary explorations to date include, Kaskida Oil Field Tiber Oil Field Jack 2 Paleogene Microfossils, 180+ images of Foraminifera
14.
Neogene
–
The Neogene is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period 23.03 million years ago to the beginning of the present Quaternary Period 2.58 Mya. The Neogene is sub-divided into two epochs, the earlier Miocene and the later Pliocene, some geologists assert that the Neogene cannot be clearly delineated from the modern geological period, the Quaternary. During this period, mammals and birds continued to evolve into modern forms. Early hominids, the ancestors of humans, appeared in Africa near the end of the period, some continental movement took place, the most significant event being the connection of North and South America at the Isthmus of Panama, late in the Pliocene. This cut off the ocean currents from the Pacific to the Atlantic ocean. The global climate cooled considerably over the course of the Neogene, the terms Neogene System and upper Tertiary System describe the rocks deposited during the Neogene Period. The continents in the Neogene were very close to their current positions, the Isthmus of Panama formed, connecting North and South America. The Indian subcontinent continued to collide with Asia, forming the Himalayas, sea levels fell, creating land bridges between Africa and Eurasia and between Eurasia and North America. The global climate became seasonal and continued an overall drying and cooling trend which began at the start of the Paleogene. The ice caps on both poles began to grow and thicken, and by the end of the period the first of a series of glaciations of the current Ice Age began, marine and continental flora and fauna have a modern appearance. The reptile group Choristodera became extinct in the part of the period. Mammals and birds continued to be the dominant terrestrial vertebrates, the first hominids, the ancestors of humans, appeared in Africa and spread into Eurasia. In response to the cooler, seasonal climate, tropical plant species gave way to deciduous ones, grasses therefore greatly diversified, and herbivorous mammals evolved alongside it, creating the many grazing animals of today such as horses, antelope, and bison. The Neogene traditionally ended at the end of the Pliocene Epoch, just before the definition of the beginning of the Quaternary Period. However, there was a movement amongst geologists to also include ongoing geological time in the Neogene, by dividing the Cenozoic Era into three periods instead of seven epochs, the periods are more closely comparable to the duration of periods in the Mesozoic and Paleozoic eras. The International Commission on Stratigraphy once proposed that the Quaternary be considered a sub-era of the Neogene, with a date of 2.58 Ma. In the 2004 proposal of the ICS, the Neogene would have consisted of the Miocene and Pliocene epochs, thus the Neogene Period ends bounding the succeeding Quaternary Period at 2.58 Mya. Digital Atlas of Neogene Life for the Southeastern United States — by San Jose State University via Web Archive
15.
Tswalu Kalahari Reserve
–
The Tswalu Kalahari Reserve is a privately owned game reserve in the Northern Cape, South Africa. It is South Africa’s largest private reserve, covering an area of over 100,000 hectares. The Tswalu game reserve in the Kalahari Desert was created by Stephen Boler and he bought dozens of farms covering more than a thousand square kilometres to create a hunting reserve. His will specified that Nicky Oppenheimer should have first refusal on Tswalu, hunting was stopped by the Oppenheimers and man-made structures, farm buildings and fences were removed. New land was added to extend and protect habitats and territories, the grasses were allowed to grow. Indigenous game such as the endangered desert black rhino and black-maned Kalahari lions were introduced. Tswalu Kalahari is a private lodge in the reserve, a member of Relais & Châteaux. 24 guests can be accommodated in the Motse and the private Tarkuni has five suites, the reserve has all the big five, with the exception of elephant. Tswalu Kalahari reserve is part of the Diamond Route, the conservation work of Nicky and Strilli Oppenheimer was recognized with the WWF-Lonmin Award from the World Wide Fund for Nature in 2007. Media related to Tswalu Kalahari Reserve at Wikimedia Commons
16.
South Africa
–
South Africa, officially the Republic of South Africa, is the southernmost country in Africa. South Africa is the 25th-largest country in the world by land area and it is the southernmost country on the mainland of the Old World or the Eastern Hemisphere. About 80 percent of South Africans are of Sub-Saharan African ancestry, divided among a variety of ethnic groups speaking different Bantu languages, the remaining population consists of Africas largest communities of European, Asian, and multiracial ancestry. South Africa is a multiethnic society encompassing a variety of cultures, languages. Its pluralistic makeup is reflected in the recognition of 11 official languages. The country is one of the few in Africa never to have had a coup détat, however, the vast majority of black South Africans were not enfranchised until 1994. During the 20th century, the black majority sought to recover its rights from the dominant white minority, with this struggle playing a role in the countrys recent history. The National Party imposed apartheid in 1948, institutionalising previous racial segregation, since 1994, all ethnic and linguistic groups have held political representation in the countrys democracy, which comprises a parliamentary republic and nine provinces. South Africa is often referred to as the Rainbow Nation to describe the multicultural diversity. The World Bank classifies South Africa as an economy. Its economy is the second-largest in Africa, and the 34th-largest in the world, in terms of purchasing power parity, South Africa has the seventh-highest per capita income in Africa. However, poverty and inequality remain widespread, with about a quarter of the population unemployed, nevertheless, South Africa has been identified as a middle power in international affairs, and maintains significant regional influence. The name South Africa is derived from the geographic location at the southern tip of Africa. Upon formation the country was named the Union of South Africa in English, since 1961 the long form name in English has been the Republic of South Africa. In Dutch the country was named Republiek van Zuid-Afrika, replaced in 1983 by the Afrikaans Republiek van Suid-Afrika, since 1994 the Republic has had an official name in each of its 11 official languages. Mzansi, derived from the Xhosa noun umzantsi meaning south, is a name for South Africa. South Africa contains some of the oldest archaeological and human fossil sites in the world, extensive fossil remains have been recovered from a series of caves in Gauteng Province. The area is a UNESCO World Heritage site and has termed the Cradle of Humankind
17.
Conservation status
–
The conservation status of a group of organisms indicates whether the group still exists and how likely the group is to become extinct in the near future. Various systems of conservation status exist and are in use at international, multi-country, the IUCN Red List of Threatened Species is the best known worldwide conservation status listing and ranking system. Also included are species that have gone extinct since 500 AD, when discussing the IUCN Red List, the official term threatened is a grouping of three categories, critically endangered, endangered, and vulnerable. Widespread and abundant taxa are included in this category, Data deficient – Not enough data to make an assessment of its risk of extinction Not evaluated – Has not yet been evaluated against the criteria. The Convention on International Trade in Endangered Species of Wild Fauna and Flora aims to ensure that trade in specimens of wild animals. Many countries require CITES permits when importing plants and animals listed on CITES, in the European Union, the Birds and Habitats Directives are the legal instruments that evaluate the conservation status within the EU of species and habitats. NatureServe conservation status focuses on Latin America, United States, Canada, and it has been developed by scientists from NatureServe, The Nature Conservancy, and the network of natural heritage programs and data centers. It is increasingly integrated with the IUCN Red List system and its categories for species include, presumed extinct, possibly extinct, critically imperiled, imperiled, vulnerable, apparently secure, and secure. The system also allows ambiguous or uncertain ranks including inexact numeric ranks, NatureServe adds a qualifier for captive or cultivated only, which has a similar meaning to the IUCN Red List extinct in the wild status. The Red Data Book of the Russian Federation is used within the Russian Federation, in Australia, the Environment Protection and Biodiversity Conservation Act 1999 describes lists of threatened species, ecological communities and threatening processes. The categories resemble those of the 1994 IUCN Red List Categories & Criteria, prior to the EPBC Act, a simpler classification system was used by the Endangered Species Protection Act 1992. Some state and territory governments also have their own systems for conservation status, in Belgium, the Flemish Research Institute for Nature and Forest publishes an online set of more than 150 nature indicators in Dutch. In Canada, the Committee on the Status of Endangered Wildlife in Canada is a group of experts that assesses and designates which wild species are in danger of disappearing from Canada. Under the Species at Risk Act, it is up to the federal government, in China, the State, provinces and some counties have determined their key protected wildlife species. There is the China red data book, in Finland, a large number of species are protected under the Nature Conservation Act, and through the EU Habitats Directive and EU Birds Directive. In Germany, the Federal Agency for Nature Conservation publishes red lists of endangered species, india has the Wild Life Protection Act,1972, Amended 2003 and the Biological Diversity Act,2002. In Japan, the Ministry of Environment publishes a Threatened Wildlife of Japan Red Data Book, in the Netherlands, the Dutch Ministry of Agriculture, Nature and Food Quality publishes a list of threatened species, and conservation is enforced by the Nature Conservation Act 1998. Species are also protected through the Wild Birds and Habitats Directives, in New Zealand, the Department of Conservation publishes the New Zealand Threat Classification System lists
18.
Least Concern
–
A least concern species is one which has been categorized by the International Union for Conservation of Nature as evaluated but not qualified for any other category. As such they do not qualify as threatened, near threatened, species cannot be assigned the Least Concern category unless they have had their population status evaluated. That is, adequate information is needed to make a direct, or indirect, since 2001 the category has had the abbreviation LC, following the IUCN2001 Categories & Criteria. However, around 20% of least concern taxa in the IUCN database use the code LR/lc, prior to 2001 least concern was a subcategory of the Lower Risk category and assigned the code LR/lc or. While least concern is not considered a red listed category by the IUCN, the number of animal species listed in this category totals 14033. There are also 101 animal subspecies listed and 1500 plant taxa, there are also two animal subpopulations listed, the Australasian and Southern African subpopulations of spiny dogfish. No fungi or protista have the classification, though only four species in those kingdoms have been evaluated by the IUCN, humans qualify for this category, and in 2008 were formally assessed as such by the IUCN
19.
IUCN Red List
–
The IUCN Red List of Threatened Species, founded in 1964, is the worlds most comprehensive inventory of the global conservation status of biological species. The International Union for Conservation of Nature is the main authority on the conservation status of species. A series of Regional Red Lists are produced by countries or organizations, the IUCN Red List is set upon precise criteria to evaluate the extinction risk of thousands of species and subspecies. These criteria are relevant to all species and all regions of the world, the aim is to convey the urgency of conservation issues to the public and policy makers, as well as help the international community to try to reduce species extinction. Major species assessors include BirdLife International, the Institute of Zoology, the World Conservation Monitoring Centre, collectively, assessments by these organizations and groups account for nearly half the species on the Red List. The IUCN aims to have the category of every species re-evaluated every five years if possible, the 1964 IUCN Red List of Threatened Plants used the older pre-criteria Red List assessment system. Plants listed may not, therefore, appear in the current Red List, IUCN advise that is best to check both the online Red List and the 1997 plants Red List publication. The 2006 Red List, released on 4 May 2006 evaluated 40,168 species as a whole, plus an additional 2,160 subspecies, varieties, aquatic stocks, on 12 September 2007, the World Conservation Union released the 2007 IUCN Red List of Threatened Species. Russ Mittermeier, chief of Swiss-based IUCNs Primate Specialist Group, stated that 16,306 species are endangered with extinction,188 more than in 2006, the Red List includes the Sumatran orangutan in the Critically Endangered category and the Bornean orangutan in the Endangered category. The study shows at least 1,141 of the 5,487 mammals on Earth are known to be threatened with extinction, and 836 are listed as Data Deficient. The Red List of 2012 was released 19 July 2012 at Rio+20 Earth Summit, nearly 2,000 species were added, the IUCN assessed a total of 63,837 species which revealed 19,817 are threatened with extinction. With 3,947 described as endangered and 5,766 as endangered. At threat are 41% of amphibian species, 33% of reef-building corals, 30% of conifers, 25% of mammals, the IUCN Red List has listed 132 species of plants and animals from India as Critically Endangered. Extinct – No known individuals remaining, extinct in the wild – Known only to survive in captivity, or as a naturalized population outside its historic range. Critically endangered – Extremely high risk of extinction in the wild, Endangered – High risk of extinction in the wild. Vulnerable – High risk of endangerment in the wild, near threatened – Likely to become endangered in the near future. Does not qualify for a more at-risk category, widespread and abundant taxa are included in this category. Data deficient – Not enough data to make an assessment of its risk of extinction, Not evaluated – Has not yet been evaluated against the criteria
20.
Taxonomy (biology)
–
Taxonomy is the science of defining groups of biological organisms on the basis of shared characteristics and giving names to those groups. The exact definition of taxonomy varies from source to source, but the core of the remains, the conception, naming. There is some disagreement as to whether biological nomenclature is considered a part of taxonomy, the broadest meaning of taxonomy is used here. The word taxonomy was introduced in 1813 by Candolle, in his Théorie élémentaire de la botanique, the term alpha taxonomy is primarily used today to refer to the discipline of finding, describing, and naming taxa, particularly species. In earlier literature, the term had a different meaning, referring to morphological taxonomy, ideals can, it may be said, never be completely realized. They have, however, a value of acting as permanent stimulants. Some of us please ourselves by thinking we are now groping in a beta taxonomy, turrill thus explicitly excludes from alpha taxonomy various areas of study that he includes within taxonomy as a whole, such as ecology, physiology, genetics, and cytology. He further excludes phylogenetic reconstruction from alpha taxonomy, thus, Ernst Mayr in 1968 defined beta taxonomy as the classification of ranks higher than species. This activity is what the term denotes, it is also referred to as beta taxonomy. How species should be defined in a group of organisms gives rise to practical and theoretical problems that are referred to as the species problem. The scientific work of deciding how to define species has been called microtaxonomy, by extension, macrotaxonomy is the study of groups at higher taxonomic ranks, from subgenus and above only, than species. While some descriptions of taxonomic history attempt to date taxonomy to ancient civilizations, earlier works were primarily descriptive, and focused on plants that were useful in agriculture or medicine. There are a number of stages in scientific thinking. Early taxonomy was based on criteria, the so-called artificial systems. Later came systems based on a complete consideration of the characteristics of taxa, referred to as natural systems, such as those of de Jussieu, de Candolle and Bentham. The publication of Charles Darwins Origin of Species led to new ways of thinking about classification based on evolutionary relationships and this was the concept of phyletic systems, from 1883 onwards. This approach was typified by those of Eichler and Engler, the advent of molecular genetics and statistical methodology allowed the creation of the modern era of phylogenetic systems based on cladistics, rather than morphology alone. Taxonomy has been called the worlds oldest profession, and naming and classifying our surroundings has likely been taking place as long as mankind has been able to communicate
21.
Animal
–
Animals are multicellular, eukaryotic organisms of the kingdom Animalia. The animal kingdom emerged as a clade within Apoikozoa as the group to the choanoflagellates. Animals are motile, meaning they can move spontaneously and independently at some point in their lives and their body plan eventually becomes fixed as they develop, although some undergo a process of metamorphosis later in their lives. All animals are heterotrophs, they must ingest other organisms or their products for sustenance, most known animal phyla appeared in the fossil record as marine species during the Cambrian explosion, about 542 million years ago. Animals can be divided broadly into vertebrates and invertebrates, vertebrates have a backbone or spine, and amount to less than five percent of all described animal species. They include fish, amphibians, reptiles, birds and mammals, the remaining animals are the invertebrates, which lack a backbone. These include molluscs, arthropods, annelids, nematodes, flatworms, cnidarians, ctenophores, the study of animals is called zoology. The word animal comes from the Latin animalis, meaning having breath, the biological definition of the word refers to all members of the kingdom Animalia, encompassing creatures as diverse as sponges, jellyfish, insects, and humans. Aristotle divided the world between animals and plants, and this was followed by Carl Linnaeus, in the first hierarchical classification. In Linnaeuss original scheme, the animals were one of three kingdoms, divided into the classes of Vermes, Insecta, Pisces, Amphibia, Aves, and Mammalia. Since then the last four have all been subsumed into a single phylum, in 1874, Ernst Haeckel divided the animal kingdom into two subkingdoms, Metazoa and Protozoa. The protozoa were later moved to the kingdom Protista, leaving only the metazoa, thus Metazoa is now considered a synonym of Animalia. Animals have several characteristics that set apart from other living things. Animals are eukaryotic and multicellular, which separates them from bacteria and they are heterotrophic, generally digesting food in an internal chamber, which separates them from plants and algae. They are also distinguished from plants, algae, and fungi by lacking cell walls. All animals are motile, if only at life stages. In most animals, embryos pass through a stage, which is a characteristic exclusive to animals. With a few exceptions, most notably the sponges and Placozoa and these include muscles, which are able to contract and control locomotion, and nerve tissues, which send and process signals
22.
Chordate
–
Chordates are deuterostomes, as during the embryo development stage the anus forms before the mouth. They are also bilaterally symmetric coelomates, in the case of vertebrate chordates, the notochord is usually replaced by a vertebral column during development, and they may have body plans organized via segmentation. There are also additional extinct taxa, the Vertebrata are sometimes considered as a subgroup of the clade Craniata, consisting of chordates with a skull, the Craniata and Tunicata compose the clade Olfactores. Of the more than 65,000 living species of chordates, the worlds largest and fastest animals, the blue whale and peregrine falcon respectively, are chordates, as are humans. Fossil chordates are known from at least as early as the Cambrian explosion, Hemichordata, which includes the acorn worms, has been presented as a fourth chordate subphylum, but it now is usually treated as a separate phylum. The Hemichordata, along with the Echinodermata, form the Ambulacraria, the Chordata and Ambulacraria form the superphylum Deuterostomia, composed of the deuterostomes. Attempts to work out the relationships of the chordates have produced several hypotheses. All of the earliest chordate fossils have found in the Early Cambrian Chengjiang fauna. Because the fossil record of early chordates is poor, only molecular phylogenetics offers a prospect of dating their emergence. However, the use of molecular phylogenetics for dating evolutionary transitions is controversial and it has also proved difficult to produce a detailed classification within the living chordates. Attempts to produce family trees shows that many of the traditional classes are paraphyletic. While this has been known since the 19th century, an insistence on only monophyletic taxa has resulted in vertebrate classification being in a state of flux. Although the name Chordata is attributed to William Bateson, it was already in prevalent use by 1880, ernst Haeckel described a taxon comprising tunicates, cephalochordates, and vertebrates in 1866. Though he used the German vernacular form, it is allowed under the ICZN code because of its subsequent latinization, among the vertebrate sub-group of chordates the notochord develops into the spine, and in wholly aquatic species this helps the animal to swim by flexing its tail. In fish and other vertebrates, this develops into the spinal cord, the pharynx is the part of the throat immediately behind the mouth. In fish, the slits are modified to form gills, a muscular tail that extends backwards behind the anus. This is a groove in the wall of the pharynx. In filter-feeding species it produces mucus to gather food particles, which helps in transporting food to the esophagus and it also stores iodine, and may be a precursor of the vertebrate thyroid gland
23.
Mammal
–
Mammals are any vertebrates within the class Mammalia, a clade of endothermic amniotes distinguished from reptiles by the possession of a neocortex, hair, three middle ear bones and mammary glands. All female mammals nurse their young with milk, secreted from the mammary glands, Mammals include the largest animals on the planet, the great whales. The basic body type is a quadruped, but some mammals are adapted for life at sea, in the air, in trees. The largest group of mammals, the placentals, have a placenta, Mammals range in size from the 30–40 mm bumblebee bat to the 30-meter blue whale. With the exception of the five species of monotreme, all modern mammals give birth to live young, most mammals, including the six most species-rich orders, belong to the placental group. The largest orders are the rodents, bats and Soricomorpha, the next three biggest orders, depending on the biological classification scheme used, are the Primates, the Cetartiodactyla, and the Carnivora. Living mammals are divided into the Yinotheria and Theriiformes There are around 5450 species of mammal, in some classifications, extant mammals are divided into two subclasses, the Prototheria, that is, the order Monotremata, and the Theria, or the infraclasses Metatheria and Eutheria. The marsupials constitute the group of the Metatheria, and include all living metatherians as well as many extinct ones. Much of the changes reflect the advances of cladistic analysis and molecular genetics, findings from molecular genetics, for example, have prompted adopting new groups, such as the Afrotheria, and abandoning traditional groups, such as the Insectivora. The mammals represent the only living Synapsida, which together with the Sauropsida form the Amniota clade, the early synapsid mammalian ancestors were sphenacodont pelycosaurs, a group that produced the non-mammalian Dimetrodon. At the end of the Carboniferous period, this group diverged from the line that led to todays reptiles. Some mammals are intelligent, with some possessing large brains, self-awareness, Mammals can communicate and vocalize in several different ways, including the production of ultrasound, scent-marking, alarm signals, singing, and echolocation. Mammals can organize themselves into fission-fusion societies, harems, and hierarchies, most mammals are polygynous, but some can be monogamous or polyandrous. They provided, and continue to provide, power for transport and agriculture, as well as commodities such as meat, dairy products, wool. Mammals are hunted or raced for sport, and are used as model organisms in science, Mammals have been depicted in art since Palaeolithic times, and appear in literature, film, mythology, and religion. Defaunation of mammals is primarily driven by anthropogenic factors, such as poaching and habitat destruction, Mammal classification has been through several iterations since Carl Linnaeus initially defined the class. No classification system is accepted, McKenna & Bell and Wilson & Reader provide useful recent compendiums. Though field work gradually made Simpsons classification outdated, it remains the closest thing to a classification of mammals
24.
Carnivora
–
Carnivora is a diverse scrotiferan order that includes over 280 species of placental mammals. Its members are referred to as carnivorans, whereas the word carnivore can refer to any meat-eating organism.9 m in length. Some carnivorans, such as cats and pinnipeds, depend entirely on meat for their nutrition, carnivorans have teeth and claws adapted for catching and eating other animals. Many hunt in packs and are social animals, giving them an advantage over larger prey, carnivorans are split into two suborders, feliforms and caniforms. Carnivorans all share the same arrangement of teeth in which the last upper premolar, carnivorans have had this arrangement for over 60 million years with many adaptions, and these dental adaptions help identify carnivoran species and groupings of species. Carnivorans evolved in North America out of members of the family Miacidae about 42 million years ago and they soon split into cat-like and dog-like forms. Their molecular phylogeny shows the extant Carnivora are a monophyletic group, the last premolar of the upper jaw and first molar of the lower are termed the carnassials or sectorial teeth. These blade-like teeth occlude with an action for shearing and shredding meat. Carnassials are most highly developed in the Felidae and the least developed in the Ursidae, carnivorans have six incisors and two conical canines in each jaw. The only two exceptions to this are the sea otter, which has four incisors in the jaw, and the sloth bear. The number of molars and premolars is variable between species, but all teeth are deeply rooted and are diphyodont. Incisors are retained by carnivorans and the incisor is commonly large. Carnivorans have either four or five digits on each foot, with the first digit on the forepaws, also known as the dew claw, being vestigial in most species and absent in some. Most species are plain in coloration, lacking the flashy spotted or rosetted coats like many species of felids and viverrids have. This is because Canoidea tend to range in the temperate and subarctic biomes, most are terrestrial, although a few species, like procyonids, are arboreal. All families except the Canidae and a few species of Mustelidae are plantigrade, diet is varied and most tend to be omnivorous to some degree, and thus the carnassial teeth are less specialized. Canoidea have more premolars and molars in an elongated skull and this is because these species tend to range in tropical habitats, although a few species do inhabit temperate and subarctic habitats. Many are arboreal or semiarboreal, and the majority are digitigrade, diet tends to be more strictly carnivorous, especially in the family Felidae
25.
Herpestidae
–
Mongoose is the popular English name for 29 of the 34 species in the 14 genera of the family Herpestidae, which are small feliform carnivorans native to southern Eurasia and mainland Africa. The other five species in the family are the four kusimanses in the genus Crossarchus, Herpestidae is placed within the suborder Feliformia, together with the cat, hyena, and civet families. The word mongoose is likely derived from the Marathi name mungūs or probably ultimately from Telugu name mangisu, the form of the English name was altered to its -goose ending by folk-etymology. It has no connection with the word goose. Historically, it has also been spelled mungoose, the plural form is mongooses, or, rarely, mongeese. Mongooses live in southern Asia, Africa, and southern Europe, as well in Fiji, Puerto Rico, and some Caribbean and Hawaiian islands, the 34 species range from 24 to 58 cm in length, excluding the tail. Mongooses range in weight from the dwarf mongoose, at 320 g, to the cat-sized white-tailed mongoose. Some species lead predominantly solitary lives, seeking out food only for themselves, while others travel in groups, sharing food among group members and offspring. Mongooses bear a resemblance to mustelids, having long faces and bodies, small, rounded ears, short legs. Most are brindled or grizzly, a few have strongly marked coats and their nonretractile claws are used primarily for digging. Mongooses, much like goats, have narrow, ovular pupils, most species have a large anal scent gland, used for territorial marking and signaling reproductive status. The dental formula of mongooses is similar to that of viverrids,3.1. 3-4. 1-23.1. 3-4. 1-2. Mongooses also have receptors for acetylcholine that, like the receptors in snakes, are shaped so that it is impossible for snake venom to attach to them. Mongooses are one of four known species with mutations in the nicotinic acetylcholine receptor that protect against snake venom. Pigs, honey badgers, hedgehogs, and mongooses all have modifications to the pocket that prevents the snake venom α-neurotoxin from binding. These represent four separate, independent mutations, in the mongoose, this change is effected uniquely, by glycosylation. Researchers are investigating whether similar mechanisms protect the mongoose from hemotoxic snake venoms, in contrast to the arboreal, nocturnal viverrids, mongooses are more commonly terrestrial and many are active during the day. The Egyptian mongoose is sometimes held as an example of a solitary mongoose, Mongooses mostly feed on insects, crabs, earthworms, lizards, birds, and rodents
26.
Binomial nomenclature
–
Such a name is called a binomial name, a binomen, binominal name or a scientific name, more informally it is also called a Latin name. The first part of the name identifies the genus to which the species belongs, for example, humans belong to the genus Homo and within this genus to the species Homo sapiens. The formal introduction of system of naming species is credited to Carl Linnaeus. But Gaspard Bauhin, in as early as 1623, had introduced in his book Pinax theatri botanici many names of genera that were adopted by Linnaeus. Although the general principles underlying binomial nomenclature are common to these two codes, there are differences, both in the terminology they use and in their precise rules. Similarly, both parts are italicized when a binomial name occurs in normal text, thus the binomial name of the annual phlox is now written as Phlox drummondii. In scientific works, the authority for a name is usually given, at least when it is first mentioned. In zoology Patella vulgata Linnaeus,1758, the original name given by Linnaeus was Fringilla domestica, the parentheses indicate that the species is now considered to belong in a different genus. The ICZN does not require that the name of the person who changed the genus be given, nor the date on which the change was made, in botany Amaranthus retroflexus L. – L. is the standard abbreviation used in botany for Linnaeus. – Linnaeus first named this bluebell species Scilla italica, Rothmaler transferred it to the genus Hyacinthoides, the ICN does not require that the dates of either publication be specified. Prior to the adoption of the binomial system of naming species. Together they formed a system of polynomial nomenclature and these names had two separate functions. First, to designate or label the species, and second, to be a diagnosis or description, such polynomial names may sometimes look like binomials, but are significantly different. For example, Gerards herbal describes various kinds of spiderwort, The first is called Phalangium ramosum, Branched Spiderwort, is aptly termed Phalangium Ephemerum Virginianum, Soon-Fading Spiderwort of Virginia. The Latin phrases are short descriptions, rather than identifying labels, the Bauhins, in particular Caspar Bauhin, took some important steps towards the binomial system, by pruning the Latin descriptions, in many cases to two words. The adoption by biologists of a system of binomial nomenclature is due to Swedish botanist and physician Carl von Linné. It was in his 1753 Species Plantarum that he first began using a one-word trivial name together with a generic name in a system of binomial nomenclature. This trivial name is what is now known as an epithet or specific name
27.
Johann Christian Daniel von Schreber
–
Johann Christian Daniel von Schreber, often styled J. C. D. von Schreber, was a German naturalist. He was appointed professor of materia medica at the University of Erlangen in 1769, in 1774 he began writing a multi-volume set of books entitled Die Säugethiere in Abbildungen nach der Natur mit Beschreibungen, which focused on the mammals of the world. Many of the animals included were given a name for the first time. From 1791 until his death in 1810, he was the President of the German Academy of Sciences Leopoldina and he was elected a member of the Royal Swedish Academy of Sciences in 1787. In April 1795 he was elected a Fellow of the Royal Society Numerous honors were bestowed on him including the office of a count palatine. Schreber also wrote on entomology notably Schreberi Novae Species Insectorvm and his herbarium collection has been preserved in the Botanische Staatssammlung München since 1813
28.
Mongoose
–
Mongoose is the popular English name for 29 of the 34 species in the 14 genera of the family Herpestidae, which are small feliform carnivorans native to southern Eurasia and mainland Africa. The other five species in the family are the four kusimanses in the genus Crossarchus, Herpestidae is placed within the suborder Feliformia, together with the cat, hyena, and civet families. The word mongoose is likely derived from the Marathi name mungūs or probably ultimately from Telugu name mangisu, the form of the English name was altered to its -goose ending by folk-etymology. It has no connection with the word goose. Historically, it has also been spelled mungoose, the plural form is mongooses, or, rarely, mongeese. Mongooses live in southern Asia, Africa, and southern Europe, as well in Fiji, Puerto Rico, and some Caribbean and Hawaiian islands, the 34 species range from 24 to 58 cm in length, excluding the tail. Mongooses range in weight from the dwarf mongoose, at 320 g, to the cat-sized white-tailed mongoose. Some species lead predominantly solitary lives, seeking out food only for themselves, while others travel in groups, sharing food among group members and offspring. Mongooses bear a resemblance to mustelids, having long faces and bodies, small, rounded ears, short legs. Most are brindled or grizzly, a few have strongly marked coats and their nonretractile claws are used primarily for digging. Mongooses, much like goats, have narrow, ovular pupils, most species have a large anal scent gland, used for territorial marking and signaling reproductive status. The dental formula of mongooses is similar to that of viverrids,3.1. 3-4. 1-23.1. 3-4. 1-2. Mongooses also have receptors for acetylcholine that, like the receptors in snakes, are shaped so that it is impossible for snake venom to attach to them. Mongooses are one of four known species with mutations in the nicotinic acetylcholine receptor that protect against snake venom. Pigs, honey badgers, hedgehogs, and mongooses all have modifications to the pocket that prevents the snake venom α-neurotoxin from binding. These represent four separate, independent mutations, in the mongoose, this change is effected uniquely, by glycosylation. Researchers are investigating whether similar mechanisms protect the mongoose from hemotoxic snake venoms, in contrast to the arboreal, nocturnal viverrids, mongooses are more commonly terrestrial and many are active during the day. The Egyptian mongoose is sometimes held as an example of a solitary mongoose, Mongooses mostly feed on insects, crabs, earthworms, lizards, birds, and rodents
29.
Kalahari Desert
–
The Kalahari Desert is a large semi-arid sandy savannah in Southern Africa extending 900,000 square kilometres, covering much of Botswana, parts of Namibia, and regions of South Africa. Derived from the Tswana word Kgala, meaning the great thirst, or Kgalagadi, meaning a waterless place, drainage is by dry valleys, seasonally inundated pans, and the large salt pans of the Makgadikgadi Pan in Botswana and Etosha Pan in Namibia. The only permanent river, the Okavango, flows into a delta in the northwest, ancient dry riverbeds—called omuramba—traverse the central northern reaches of the Kalahari and provide standing pools of water during the rainy season. A semi-desert, with tracts of excellent grazing after good rains. There are small amounts of rainfall and the temperature is very high. The driest areas usually receive 110–200 millimetres of rain per year, the surrounding Kalahari Basin covers over 2,500,000 square kilometres extending further into Botswana, Namibia and South Africa, and encroaching into parts of Angola, Zambia and Zimbabwe. The Kalahari is home to migratory birds and animals. The area is now heavily grazed and cattle fences restrict the movement of wildlife, among deserts of the Southern Hemisphere, the Kalahari most closely resembles some Australian deserts in its latitude and its mode of formation. The Kalahari Desert came into existence approximately sixty years ago along with the formation of the African continent. North and east, approximately where the dry forests, savannahs and salt lakes prevail, South and west, where the vegetation is predominantly xeric savanna or even a semi-desert, the climate is Kalaharian semi-arid. The Kalaharian climate is subtropical, and is semi-arid with the dry season during the cold season and it is the southern tropical equivalent of the Sahelian climate. For example, winter frost is common from June to August, as in the Sahel, the wet season in the Kalahari is during the six coldest months of the year. The dry season lasts eight months or more, and the wet season typically from less than one month to four months, the southwestern Kalahari is the driest area, in particular a small region located towards the west-southwest of Tsaraxaibis. The average annual rainfall ranging from around 110 mm to more than 500 mm in areas of the north. In the driest and sunniest parts of the Kalahari, over 4,000 hours of sunshine are recorded annually on average. There are huge subterranean water reserves beneath parts of the Kalahari, such reserves may be in part the residues of ancient lakes, the Kalahari Desert was once a much wetter place. The ancient Lake Makgadikgadi dominated the area, covering the Makgadikgadi Pan and surrounding areas and it may have once covered as much as 120,000 square kilometres. The Kalahari has had a complex climatic history over the past million or so years, changes in the last 250,000 years have been reconstructed form various data sources, and provide evidence of both former extensive lakes and periods drier than now
30.
Botswana
–
Botswana, officially the Republic of Botswana, is a landlocked country located in Southern Africa. The citizens refer to themselves as Batswana, formerly the British protectorate of Bechuanaland, Botswana adopted its new name after becoming independent within the Commonwealth on 30 September 1966. Since then, it has maintained a tradition of stable representative democracy. Botswana is topographically flat, with up to 70 percent of its territory being the Kalahari Desert and it is bordered by South Africa to the south and southeast, Namibia to the west and north, and Zimbabwe to the northeast. Its border with Zambia to the north near Kazungula is poorly defined, a mid-sized country of just over 2 million people, Botswana is one of the most sparsely populated nations in the world. Around 10 percent of the lives in the capital and largest city. The economy is dominated by mining, cattle, and tourism, Botswana boasts a GDP per capita of about $18,825 per year as of 2015, which is one of the highest in Africa. Its high gross national income gives the country a modest standard of living, Botswana is a member of the African Union, the Southern African Development Community, the Commonwealth of Nations, and the United Nations. The country has been among the hardest hit by the HIV/AIDS epidemic, the death rate due to AIDS or AIDS-related causes has fallen sharply from 2005 to 2013, and the number of new infections in children has also fallen. As of 2014, Botswana has the third-highest prevalence rate for HIV/AIDS, the history of Botswana starts more than 100,000 years ago, when the first humans inhabited the region. The original inhabitants of southern Africa were the Bushmen and Khoi peoples, both speak Khoisan languages and lived as hunter-gatherers. About a thousand years ago, large chiefdoms emerged that were later eclipsed by the Great Zimbabwe empire, around 1300 CE, peoples in present-day Transvaal began to coalesce into three main linguistic and political groups, including the Batswana. The Batswana, a term used also to all citizens of Botswana. Prior to European contact, the Batswana lived as herders and farmers under tribal rule, as groups broke off and moved to new land, new tribes were created. Some human development occurred before the colonial period, during the 1700s, the slave and ivory trades were expanding. To resist these pressures, Shaka, the king of the Zulu Empire, conquered tribes began to move northwest into Botswana, destroying everything in their path. In their efforts to re-establish themselves at the end of period, tribes began to exchange ivory and skins for guns with European traders. Christian missionaries sent from Europe also spread to the interior, often at the invitation of tribal chiefs who wanted guns, by 1880 every major village had a resident missionary, and their influence became permanent
31.
Namib
–
The Namib is a coastal desert in southern Africa. The name Namib is of Nama origin and means vast place, the Namibs northernmost portion, which extends 450 kilometres from the Angola-Namibia border, is known as Moçâmedes Desert, while its southern portion approaches the neighboring Kalahari Desert. From the Atlantic coast eastward, the Namib gradually ascends in elevation, annual precipitation ranges from 2 millimetres in the most arid regions to 200 millimetres at the escarpment, making the Namib the only true desert in southern Africa. Having endured arid or semi-arid conditions for roughly 55–80 million years, the desert geology consists of sand seas near the coast, while gravel plains and scattered mountain outcrops occur further inland. The sand dunes, some of which are 300 metres high, fogs that originate offshore from the collision of the cold Benguela Current and warm air from the Hadley Cell create a fog belt that frequently envelops parts of the desert. Coastal regions can experience more than 180 days of fog a year. While this has proved a hazard to ships—more than a thousand wrecks litter the Skeleton Coast—it is a vital source of moisture for desert life. Owing to its antiquity, the Namib may be home to endemic species than any other desert in the world. Most of the wildlife is arthropods and other small animals that live on little water. Near the coast, the ocean water is rich in fishery resources and supports populations of brown fur seals and shorebirds. Further inland, the Namib-Naukluft National Park, the largest game park in Africa, supports populations of African Bush Elephants, Mountain Zebras, and other large mammals. Although the outer Namib is largely barren of vegetation, lichens and succulents are found in areas, while grasses, shrubs. A few types of trees are able to survive the extremely arid climate. The Namib Desert is one of the 500 distinct physiographic provinces of the South African Platform physiographic division and it occupies an area of around 80,950 km², stretching from the[Usiab River to the town of Lüderitz and from the Atlantic Ocean to the Namib Escarpment. It is about 1,000 miles long north to south. To the south, the Namib borders on the South African Karoo semi-desert, southern Namib comprises a vast dune sea with some of the tallest and most spectacular dunes of the world, ranging in color from pink to vivid orange. In the Sossusvlei area, several dunes exceed 300 meters in height, the complexity and regularity of dune patterns in its dune sea have attracted the attention of geologists for decades, but it remains poorly understood. Moving north from Sossusvlei, the sand gradually gives way to a desert that extends all the way from Sossusvlei to the Swakop river
32.
Namibia
–
Namibia, officially the Republic of Namibia, is a country in southern Africa whose western border is the Atlantic Ocean. It shares land borders with Zambia and Angola to the north, Botswana to the east and South Africa to the south, although it does not border Zimbabwe, a part of less than 200 metres of the Zambezi River separates the two countries. Namibia gained independence from South Africa on 21 March 1990, following the Namibian War of Independence. Its capital and largest city is Windhoek, and it is a state of the United Nations, the Southern African Development Community, the African Union. The dry lands of Namibia were inhabited since early times by the San, Damara, since about the 14th century, immigrating Bantu peoples arrived as part of the Bantu expansion. Since then the Bantu groups in total, known as the Ovambo people, have dominated the population of the country, in the late 19th century during European colonization, the German Empire established rule over most of the territory as a protectorate in 1884. It began to develop infrastructure and farming, and maintained this German colony until 1915, after the end of World War I, in 1920 the League of Nations mandated the country to the United Kingdom, under administration by South Africa. It imposed its laws, including racial classifications and rules, from 1948, with the National Party elected to power, South Africa applied apartheid also to what was known as South West Africa. In 1878 the Cape of Good Hope had annexed the port of Walvis Bay and the offshore Penguin Islands, following continued guerrilla warfare, South Africa installed an interim administration in Namibia in 1985. Namibia obtained full independence from South Africa in 1990, but Walvis Bay and the Penguin Islands remained under South African control until 1994. Namibia has a population of 2.1 million people and a stable multi-party parliamentary democracy, Agriculture, herding, tourism and the mining industry – including mining for gem diamonds, uranium, gold, silver, and base metals – form the basis of its economy. The large, arid Namib Desert has resulted in Namibia being overall one of the least densely populated countries in the world, Namibia enjoys high political, economic and social stability. The name of the country is derived from the Namib Desert, before its independence in 1990, the area was known first as German South-West Africa, then as South-West Africa, reflecting the colonial occupation by the Germans and the South Africans. The dry lands of Namibia were inhabited since early times by San, Damara, from about the 14th century, immigrating Bantu peoples arrived during the Bantu expansion from central Africa. From the late 18th century onwards, Oorlam people from Cape Colony crossed the Orange River and their encounters with the nomadic Nama tribes were largely peaceful. The missionaries accompanying the Oorlam were well received by them, the right to use waterholes, on their way further northwards, however, the Oorlam encountered clans of the Herero at Windhoek, Gobabis, and Okahandja, who resisted their encroachment. The Nama-Herero War broke out in 1880, with hostilities ebbing only after the German Empire deployed troops to the places and cemented the status quo among the Nama, Oorlam. The first Europeans to disembark and explore the region were the Portuguese navigators Diogo Cão in 1485 and Bartolomeu Dias in 1486, like most of interior Sub-Saharan Africa, Namibia was not extensively explored by Europeans until the 19th century
33.
Angola
–
Angola /æŋˈɡoʊlə/, officially the Republic of Angola, is a country in Southern Africa. It is the seventh-largest country in Africa and is bordered by Namibia to the south, the Democratic Republic of the Congo to the north, Zambia to the east, and the Atlantic Ocean to west. The exclave province of Cabinda has borders with the Republic of the Congo, the capital and largest city of Angola is Luanda. In the 19th century, European settlers slowly and hesitantly began to themselves in the interior. As a Portuguese colony, Angola did not encompass its present borders until the early 20th century, following resistance by groups such as the Cuamato, the Kwanyama and the Mbunda. Independence was achieved in 1975 under a communist one-party state backed by the Soviet Union, however, the country soon descended into an even lengthier civil war that lasted until 2002. It has since become a relatively stable presidential republic. Angola has vast mineral and petroleum reserves, and its economy is among the fastest growing in the world, Angolas economic growth is highly uneven, with the majority of the nations wealth concentrated in a disproportionately small sector of the population. Angola is a state of the United Nations, OPEC, African Union, the Community of Portuguese Language Countries, the Latin Union. A highly multiethnic country, Angolas 25.8 million people span various tribal groups, customs, Angolan culture reflects centuries of Portuguese rule, namely in the predominance of the Portuguese language and the Catholic Church, combined with diverse indigenous influences. The name Angola comes from the Portuguese colonial name Reino de Angola, the toponym was derived by the Portuguese from the title ngola held by the kings of Ndongo. Ndongo was a kingdom in the highlands, between the Kwanza and Lukala Rivers, nominally tributary to the king of Kongo but which was seeking greater independence during the 16th century, modern Angola was populated predominantly by nomadic Khoi and San prior to the first Bantu migrations. The Khoi and San peoples were neither pastoralists nor cultivators, following a hunter-gatherer lifestyle and they were displaced by Bantu peoples arriving from the north, some of whom likely originated in northwestern Nigeria. Bantu speakers introduced the cultivation of bananas and taro, as well as large herds, to Angolas central highlands. During this time, the Bantu established a number of entities in most of what today comprises Angola. To its south lay the Kingdom of Ndongo, from which the area of the later Portuguese colony was known as Dongo. The region now known as Angola was reached by the Portuguese explorer Diogo Cão in 1484, the year before, the Portuguese had established relations with the Kongo, which stretched at the time from modern Gabon in the north to the Kwanza River in the south. The Portuguese established their primary trading post at Soyo, which is now the northernmost city in Angola apart from the Cabinda exclave
34.
Afrikaans
–
Afrikaans is a West Germanic language spoken in South Africa, Namibia and, to a lesser extent, Botswana and Zimbabwe. Hence, it is a language of Dutch, and was previously referred to as Cape Dutch or kitchen Dutch. Although, it is described as a creole, a partially creolised language the least. The term is derived from Dutch Afrikaans-Hollands meaning African Dutch. It is the first language of most of the Afrikaner and Coloured people of Southern Africa, therefore, differences with Dutch often lie in the more analytic morphology and grammar of Afrikaans, and a spelling that expresses Afrikaans pronunciation rather than standard Dutch. There is a degree of mutual intelligibility between the two languages—especially in written form. With about 7 million native speakers in South Africa, or 13. 5% of the population and it has the widest geographical and racial distribution of all the eleven official languages of South Africa, and is widely spoken and understood as a second or third language. About 1. 5% of black South Africans speak it as their first language, large numbers of speakers of Bantu languages and English-speaking South Africans also speak it as their second language. It is taught in schools, with about 10.3 million second-language students and it, along with German, was among the official languages of Namibia until the country became independent in 1990, 25% of the population of Windhoek spoke Afrikaans at home. Both Afrikaans and German survive as recognised regional languages in the country, estimates of the total number of Afrikaans speakers range between 15 and 23 million. The Afrikaans language arose in the Dutch Cape Colony, through a gradual divergence from European Dutch dialects, there is a degree of mutual intelligibility between the two languages, particularly in written form. Nevertheless, Dutch speakers are confronted with fewer non-cognates when listening to Afrikaans than the way round. Mutual intelligibility thus tends to be asymmetrical, as it is easier for Dutch speakers to understand Afrikaans than for Afrikaans speakers to understand Dutch, in general, mutual intelligibility between Dutch and Afrikaans is better than between Dutch and Frisian or between Danish and Swedish. The workers and slaves who contributed to the development of Afrikaans were Asians and Malagasys, as well as the Khoi, San, and Bantu peoples who also lived in the area. African creole people in the early 18th century — documented on the cases of Hendrik Bibault, Only much later in the second half of the 19th century did the Boers adopt this attribution, too. The Khoi and mixed-race groups became collectively referred to as Coloureds, beginning in about 1815, Afrikaans started to replace Malay as the language of instruction in Muslim schools in South Africa, written with the Arabic alphabet, see Arabic Afrikaans. Later, Afrikaans, now written with the Latin alphabet, started to appear in newspapers and political, in 1925, Afrikaans was recognised by the South African government as a real language, rather than simply a slang version of Dutch proper. Before the Boer Wars, and indeed for some time afterwards, rather, Afrikaans was described derogatorily as ‘a kitchen language’ or as ‘a bastard jargon, suitable for communication mainly between the Boers and their servants
35.
Dutch language
–
It is the third most widely spoken Germanic language, after English and German. Dutch is one of the closest relatives of both German and English and is said to be roughly in between them, Dutch vocabulary is mostly Germanic and incorporates more Romance loans than German but far fewer than English. In both Belgium and the Netherlands, the official name for Dutch is Nederlands, and its dialects have their own names, e. g. Hollands, West-Vlaams. The use of the word Vlaams to describe Standard Dutch for the variations prevalent in Flanders and used there, however, is common in the Netherlands, the Dutch language has been known under a variety of names. It derived from the Old Germanic word theudisk, one of the first names used for the non-Romance languages of Western Europe. It literarily means the language of the people, that is. The term was used as opposed to Latin, the language of writing. In the first text in which it is found, dating from 784, later, theudisca appeared also in the Oaths of Strasbourg to refer to the Germanic portion of the oath. This led inevitably to confusion since similar terms referred to different languages, owing to Dutch commercial and colonial rivalry in the 16th and 17th centuries, the English term came to refer exclusively to the Dutch. A notable exception is Pennsylvania Dutch, which is a West Central German variety called Deitsch by its speakers, Jersey Dutch, on the other hand, as spoken until the 1950s in New Jersey, is a Dutch-based creole. In Dutch itself, Diets went out of common use - although Platdiets is still used for the transitional Limburgish-Ripuarian Low Dietsch dialects in northeast Belgium, Nederlands, the official Dutch word for Dutch, did not become firmly established until the 19th century. This designation had been in use as far back as the end of the 15th century, one of them was it reflected a distinction with Hoogduits, High Dutch, meaning the language spoken in Germany. The Hoog was later dropped, and thus, Duits narrowed down in meaning to refer to the German language. g, in English, too, Netherlandic is regarded as a more accurate term for the Dutch language, but is hardly ever used. Old Dutch branched off more or less around the same time Old English, Old High German, Old Frisian and Old Saxon did. During that period, it forced Old Frisian back from the western coast to the north of the Low Countries, on the other hand, Dutch has been replaced in adjacent lands in nowadays France and Germany. The division in Old, Middle and Modern Dutch is mostly conventional, one of the few moments linguists can detect somewhat of a revolution is when the Dutch standard language emerged and quickly established itself. This is assumed to have taken place in approximately the mid-first millennium BCE in the pre-Roman Northern European Iron Age, the Germanic languages are traditionally divided into three groups, East, West, and North Germanic. They remained mutually intelligible throughout the Migration Period, Dutch is part of the West Germanic group, which also includes English, Scots, Frisian, Low German and High German
36.
Guenon
–
The guenons are the genus Cercopithecus of Old World monkeys. Nonetheless, the use of the term guenon for monkeys of this genus is widely accepted, all members of the genus are endemic to sub-Saharan Africa, and most are forest monkeys. Many of the species are quite local in their ranges, many are threatened or endangered because of habitat loss. The species currently placed in the genus Chlorocebus, such as vervet monkeys, in the English language, the word guenon is apparently of French origin. In French, guenon was the name for all species and individuals. In all other monkey and apes species, the French word guenon only designates the females, media related to Cercopithecus at Wikimedia Commons Primate Info Net Cercopithecus Factsheets
37.
Feliformia
–
Feliformia is the name of a suborder within the order Carnivora consisting of cat-like carnivorans, including cats, hyenas, mongooses, civets, and related taxa. Feliformia stands in contrast to the suborder of Carnivora, Caniformia. The separation of the Carnivora into the groups of feliforms and caniforms is widely accepted. The classification of feliforms as part of the Feliformia suborder or under separate groupings continues to evolve, systematic classifications dealing with only extant taxa include all feliforms into the Feliformia suborder, though variations exist in the definition and grouping of families and genera. Indeed, molecular phylogenies suggest that all extant Feliformia are monophyletic, the extant families as reflected in the taxa chart at right and the discussions in this article reflect the most contemporary and well-supported views. Systematic classifications dealing with both extant and extinct taxa vary more widely, some separate the feliforms as, Aeluroidea and Feliformia. Others include all feliforms into the Feliformia suborder, recent studies suggest this inclusion of possible ancestors into Feliformia may be spurious. The extinct families as reflected in the chart are the least problematic in terms of their relationship with extant feliforms. All extant feliforms share a common attribute, their auditory bullae and this is a key diagnostic in classifying species as feliform versus caniform. In feliforms, the auditory bullae are double-chambered, composed of two joined by a septum. Caniforms have single-chambered or partially divided auditory bullae, composed of a single bone and this feature, however, is problematic for the classification of the extinct Nimravidae as feliforms. Nimravid fossils show ossified bullae with no septum, or no trace at all of the entire bulla and it is assumed that they had a cartilaginous housing of the ear mechanism. The specific characteristics of extant feliform bullae suggest a common ancestor, there are other characteristics that differentiate feliforms from caniforms and probably existed in their stem taxa. But, due to speciation, these do not apply unambiguously to all extant species, Feliforms tend to have shorter rostrums than caniforms, fewer teeth, and more specialized carnassials. Feliforms tend to be carnivorous and are generally ambush hunters. Caniforms tend more toward omnivorous and opportunity-based feeders, many feliforms have retractile or semi-retractile claws and many are arboreal or semi-arboreal. Feliforms also tend to be more digitigrade, in contrast, most caniforms are terrestrial, have non-retractile claws and tend to be plantigrade. There are seven extant families, twelve subfamilies,56 genera and 114 species in the Feliformia suborder and they range natively across all continents except Australia and Antarctica
38.
Felidae
–
Felidae is the family of cats. A member of family is also called a felid. They are sometimes referred to as hypercarnivores because of the large proportion of protein they require in their diet. Of the 13 terrestrial families in the order Carnivora, they are the strictest carnivores, the first cats emerged during the Oligocene, about 25 million years ago. In prehistoric times, there was a subfamily, the Machairodontinae. Other superficially cat-like mammals, such as the metatherians Thylacosmilus and Thylacoleo, the 42 known cat species in the world today are all descended from a common ancestor. Cats originated in Asia and spread across continents by crossing land bridges, about 60% of the modern cat species are estimated to have developed within the last million years. Felidaes closest relatives are thought to be the Asiatic linsangs, together with the Viverridae, hyenas, mongooses, and Madagascar carnivores, they form the suborder Feliformia. Most cat species share a genetic anomaly that prevents them from tasting sweetness, most cat species have a haploid number of 18 or 19. New World cats have a number of 18, possibly due to the combination of two smaller chromosomes into a larger one. Domestic cats may either have a long or short tail, at one point, biologists had to consider whether the short tail also found in the lynx was the ancestral or derived trait. Without looking at the record, researchers were able to look at the character states found in their outgroups. Because all animals belonging to Felidae’s sister taxa, Viverridae, have long tails, some domestic cats display a rosette pattern on their coats. This character state, however, is not related to the rosettes found on big cats, domestic cats and big cats underwent convergent evolution for this trait. The most common ancestor to all cats had a flecked coat, the jaguarundi lost this character state secondarily. The most common recent ancestor of snow leopards, tigers, jaguars, lions, tigers and lions, however, do not display rosettes as adults. They both have lost this character state over time. Adult tigers actually display elongated rosettes that now appear as stripes, adult lions seem to lack any distinctive markings altogether
39.
Sanskrit
–
Sanskrit is the primary liturgical language of Hinduism, a philosophical language of Hinduism, Buddhism, and Jainism, and a literary language and lingua franca of ancient and medieval South Asia. As a result of transmission of Hindu and Buddhist culture to Southeast Asia and parts of Central Asia, as one of the oldest Indo-European languages for which substantial written documentation exists, Sanskrit holds a prominent position in Indo-European studies. The body of Sanskrit literature encompasses a rich tradition of poetry and drama as well as scientific, technical, philosophical, the compositions of Sanskrit were orally transmitted for much of its early history by methods of memorization of exceptional complexity, rigor, and fidelity. Thereafter, variants and derivatives of the Brahmi script came to be used, Sanskrit is today one of the 22 languages listed in the Eighth Schedule of the Constitution of India, which mandates the Indian government to develop the language. It continues to be used as a ceremonial language in Hindu religious rituals and Buddhist practice in the form of hymns. The Sanskrit verbal adjective sáṃskṛta- may be translated as refined, elaborated, as a term for refined or elaborated speech, the adjective appears only in Epic and Classical Sanskrit in the Manusmṛti and the Mahabharata. The pre-Classical form of Sanskrit is known as Vedic Sanskrit, with the language of the Rigveda being the oldest and most archaic stage preserved, Classical Sanskrit is the standard register as laid out in the grammar of Pāṇini, around the fourth century BCE. Sanskrit, as defined by Pāṇini, evolved out of the earlier Vedic form, the present form of Vedic Sanskrit can be traced back to as early as the second millennium BCE. Scholars often distinguish Vedic Sanskrit and Classical or Pāṇinian Sanskrit as separate dialects, although they are quite similar, they differ in a number of essential points of phonology, vocabulary, grammar and syntax. Vedic Sanskrit is the language of the Vedas, a collection of hymns, incantations and theological and religio-philosophical discussions in the Brahmanas. Modern linguists consider the metrical hymns of the Rigveda Samhita to be the earliest, for nearly 2000 years, Sanskrit was the language of a cultural order that exerted influence across South Asia, Inner Asia, Southeast Asia, and to a certain extent East Asia. A significant form of post-Vedic Sanskrit is found in the Sanskrit of Indian epic poetry—the Ramayana, the deviations from Pāṇini in the epics are generally considered to be on account of interference from Prakrits, or innovations, and not because they are pre-Paninian. Traditional Sanskrit scholars call such deviations ārṣa, meaning of the ṛṣis, in some contexts, there are also more prakritisms than in Classical Sanskrit proper. There were four principal dialects of classical Sanskrit, paścimottarī, madhyadeśī, pūrvi, the predecessors of the first three dialects are attested in Vedic Brāhmaṇas, of which the first one was regarded as the purest. In the 2001 Census of India,14,035 Indians reported Sanskrit to be their first language, in India, Sanskrit is among the 14 original languages of the Eighth Schedule to the Constitution. The state of Uttarakhand in India has ruled Sanskrit as its official language. In October 2012 social activist Hemant Goswami filed a petition in the Punjab. More than 3,000 Sanskrit works have been composed since Indias independence in 1947, much of this work has been judged of high quality, in comparison to both classical Sanskrit literature and modern literature in other Indian languages
40.
Dutch East India Company
–
It is often considered to be the worlds first truly transnational corporation and the first company in history to actually issue bonds and shares of stock to the general public. In other words, the VOC was officially the first publicly traded company of the world, the company was also considered by many to be the very first major and the greatest corporation in history. Statistically, the VOC eclipsed all of its rivals in international trade for almost 200 years of existence. Between 1602 and 1796 the VOC sent almost a million Europeans to work in the Asia trade on 4,785 ships, the VOC enjoyed huge profits from its spice monopoly through most of the 17th century. Having been set up in 1602, to profit from the Malukan spice trade, in 1619 the VOC established a capital in the city of Jayakarta. Over the next two centuries the Company acquired additional ports as trading bases and safeguarded their interests by taking over surrounding territory and it remained an important trading concern and paid an 18% annual dividend for almost 200 years. Around the world and especially in English-speaking countries, the VOC is widely known as the Dutch East India Company, the name ‘Dutch East India Company’ is used to make a distinction with the East India Company and other East Indian companies. The abbreviation VOC stands for Vereenigde Oost-Indische Compagnie or Verenigde Oostindische Compagnie in Dutch, the VOC monogram was possibly the first globally-recognized corporate logo. The logo of the VOC consisted of a large capital V with an O on the left and it appeared on various corporate items, such as cannon and coins. The first letter of the hometown of the conducting the operation was placed on top. An Australian vintner has used the VOC logo since the late 20th century, the flag of the company was orange, white, and blue, with the company logo embroidered on it. Before the Dutch Revolt, Antwerp had played an important role as a centre in northern Europe. At the same time, the Portuguese trade system was unable to supply to satisfy growing demand. Demand for spices was relatively inelastic, and therefore each lag in the supply of pepper caused a rise in pepper prices. These three factors motivated Dutch merchants to enter the spice trade themselves. Further, a number of Dutchmen like Jan Huyghen van Linschoten and Cornelis de Houtman obtained first hand knowledge of the secret Portuguese trade routes and practices, thereby providing opportunity. The stage was set for Houtmans 1595 four-ship exploratory expedition to Banten, the main pepper port of West Java. Houtmans expedition then sailed east along the north coast of Java, losing twelve crew to a Javanese attack at Sidayu, half the crew were lost before the expedition made it back to the Netherlands the following year, but with enough spices to make a considerable profit
41.
Paul Gervais
–
Paul Gervais full name François Louis Paul Gervaise was a French palaeontologist and entomologist. Gervais beaked whale is named after him, in 1841 he obtained the chair of zoology and comparative anatomy at the Faculty of Sciences in Montpellier, of which he was in 1856 appointed dean. He died in Paris on 10 February 1879, according to Florentino Ameghino Paul Gervais studied a fossil collection obtained from Juan Manuel de Rosas the governor of Buenos Aires. Earlier on this collection would have donated or donated-by-force to the Buenos Aires Province by Francisco Javier Muñiz
42.
Diurnality
–
Diurnality is a form of plant or animal behavior characterized by activity during the day, with a period of sleeping, or other inactivity, at night. The common adjective used for daytime activity is diurnal, the timing of activity by an animal depends on a variety of environmental factors such as the temperature, the ability to gather food by sight, the risk of predation, and the time of year. Diurnality is a cycle of activity within a period, cyclic activities called circadian rhythms are endogenous cycles not dependent on external cues or environmental factors. Animals active at dawn or dusk are crepuscular, those active at night are nocturnal, plants that open their flowers during the day are referred to as diurnal, while those that bloom at night are nocturnal. The timing of opening is often related to the time at which preferred pollinators are foraging. For example, sunflowers open during the day in order to attract bees, many animal species are diurnal, including many mammals, insects, reptiles and birds. In some animals, especially insects, external patterns of the environment control the activity, diurnality is descriptive, it refers to an observed 24-hour pattern, as opposed to ~24-hour circadian rhythms which are self-sustaining within the organism. In many species, the switches from nocturnal to diurnal foraging depending on the environmental temperature. This allows the individual to maximize its feeding efficiency during the summer and lower its risk of predation during the winter. Diurnal insects include some bees, such as Anthidium maculosum and these carder bees are diurnal and active only when the temperatures are above freezing. They are also most active when there are plenty of such as flowers, from which they can extract pollen. Some primarily nocturnal or crepuscular animals, like dogs and cats, have been domesticated and have become diurnal to coincide with the cycle of human life, however, these animals may exhibit their species original behavior when they are born feral. Other animals have been forced from their normal cycle to a one as a means of avoiding predators. Many plants are diurnal or nocturnal, depending on the period when the most effective pollinators, i. e. insects. Most angiosperm plants are visited by insects, so the flower adapts its phenology to the most effective pollinators. For example, the baobab is pollinated by bats and starts blooming in late afternoon. Services that alternate between high and low utilization in a daily cycle are described as being diurnal, many web sites have the most users during the day and little utilization at night, or vice versa. Operations planners can use this cycle to plan, for example, maintenance that needs to be done when there are fewer users on the web site
43.
Binocular vision
–
Binocular vision is vision in which creatures having two eyes use them together. The word binocular comes from two Latin roots, bini for double, and oculus for eye, according to Fahle, having two eyes confers six advantages over having one. It gives a creature a spare eye in one is damaged. It gives a wider field of view and it can give stereopsis in which binocular disparity provided by the two eyes different positions on the head gives precise depth perception. This also allows a creature to break the camouflage of another creature and it allows the angles of the eyes lines of sight, relative to each other, and those lines relative to a particular object to be determined from the images in the two eyes. These properties are necessary for the third advantage and it allows a creature to see more of, or all of, an object behind an obstacle. It gives binocular summation in which the ability to detect faint objects is enhanced, other phenomena of binocular vision include utrocular discrimination, eye dominance, allelotropia, binocular fusion or singleness of vision, and binocular rivalry. Binocular vision helps with performance skills such as catching, grasping and it also allows humans to walk over and around obstacles at greater speed and with more assurance. Optometrists and/or Orthoptists are eyecare professionals who fix binocular vision problems, some animals, usually, but not always, prey animals, have their two eyes positioned on opposite sides of their heads to give the widest possible field of view. Examples include rabbits, buffaloes, and antelopes, in such animals, the eyes often move independently to increase the field of view. Even without moving their eyes, some birds have a 360-degree field of view, other animals that are not necessarily predators, such as fruit bats and a number of primates also have forward-facing eyes. These are usually animals that need fine depth discrimination/perception, for instance, binocular vision improves the ability to pick a chosen fruit or to find, the direction of a point relative to the head is called visual direction, or version. The angle between the line of sight of the two eyes when fixating a point is called the disparity, binocular parallax, or vergence demand. The relation between the position of the two eyes, version and vergence is described by Herings law of visual direction, in animals with forward-facing eyes, the eyes usually move together. Eye movements are either conjunctive, version eye movements, usually described by their type, or they are disjunctive, vergence eye movements. The relation between version and vergence eye movements in humans is described by Herings law of equal innervation, some animals use both of the above strategies. A starling, for example, has laterally placed eyes to cover a wide field of view, a remarkable example is the chameleon, whose eyes appear as if mounted on turrets, each moving independently of the other, up or down, left or right. Nevertheless, the chameleon can bring both of its eyes to bear on an object when it is hunting, showing vergence
44.
Knie's Kinderzoo
–
Knies Kinderzoo is a zoo aimed for children. It is located in the Swiss municipality of Rapperswil, aimed for children, the zoo is located at Oberseestrasse nearby Seedamm respectively Rapperswil railway station on upper Lake Zürich. Ending winter season, Kinderzoo opens daily from 9 am to 6 pm between the first Saturday in March and October 31, including Sundays and public holidays. On 15 February 1963 the first birth of an Asian elephant in Switzerland was announced, Sahib-Fridolin was the son of the elephants Ceylon and Siam. The baby elephant is reared by elephant expert and animal trainer Josef Hack with the bottle because Ceylon had no milk and died three months after giving birth. The dolphins Sindbad and Skipper became an attraction on 19 June 1965. On 4 August birth of the second Asian elephant Madura, a female, was celebrated, on 25 July 1970 the first permanent dolphinarium featuring an 800, 000-litre pool opened at Knie’s Kinderzoo – it was closed for animal protection reasons in 199x. 1976 became the year in the zoos history, totalling 399,331 visitors -7,8 millions by 1987. In 1991 the fur seals swimming pool with an observation window opened. On 24 March 1993 Diva, a Giraffa camelopardalis rothschildi, gave birth of her son Baluku who became the first Giraffa born in the zoo. In 2000 the renewed elephant facility with bath, waterfall, clay wallows, scratching posts, and that same year, the zoo launched its website. Besides, the new ship for children was opened,2001 saw the launch of the zoo slogan, literally animals up close. On 9 April, the newborn giraffe bull of mother Luana,2003 saw the inauguration of an adventure playground with a hatchery for ducks and chickens, and a plant for guinea pigs and rabbits. Diva, the ancestress of the zoos Rothschild giraffe breed, and Miniak, one of the oldest elephant in captivity, died at the age of 22, respectively 52. The facility for Suricata suricatta and Cynictis penicillata was opened in 2005, and at the so-called Steinwal, the landmark of the zoo, the cooperation with Ocean Care to protect the Mediterranean monk seals was also renewed. On 6 March 2008 one of the largest plants in Europe for Camelus ferus in Mongolian style was opened on 3,500 square metres. The two elephants houses were built and offer over 800 square metres, and ten individual boxes 34 square metres, scratching walls/ posts, solarium. In 2009 and 2010, the establishments have been upgraded with a new infrastructure
45.
Rapperswil
–
The towns main sights are concentrated in the Altstadt of Rapperswil and can be seen while strolling through the medieval alleys. Rapperswil is often referred to as the town of roses because of its displays of roses in three designated parks. No less than 15,000 plants of 600 different kinds may be viewed between June and October, there is also a rose garden in the town center, accessible to blind and disabled people. The old town is dominated by the Schloss Rapperswil located at the peninsula called Endingen, Lindenhof, the castle dates back to the early 13th century. In 1350, it was destroyed by Rudolf Brun, the mayor of Zürich, deer inhabit lands surrounding the castle. Since 1870, the castle has been home to the Polish National Museum created by Polish émigrés, including the castles lessee and restorer, a small Capuchins monastery was established in 1606 at the lakeside Endingerhorn as a Catholic counterpart to the Reformations centre in the city of Zürich. The monastery buildings belong to the citizens of Rapperswil rather than to the monks who inhabit it, the main churches in town include the Roman Catholic St. Johns Church, the cemetery chapel and a small Protestant church. The locational advantage of the place attracted the national Circus Knie who built its headquarters in Rapperswil in 1919, the circus is now also responsible for the Circus Museum and the Knies Kinderzoo located in Rapperswil which is particularly aimed at children. Rapperswil also hosts the Hochschule für Technik Rapperswil HSR and an Economics school for parts of the cantons Zürich, settlements in the region of Rapperswil date back to at least 5000 years ago. The three neighbouring Prehistoric settlements, as well as the early crossings, are part of the UNESCO World Heritage Site Prehistoric Pile dwellings around the Alps. The neolithic bridge between Hurden and Rapperswil was renewed by the Romans at least around 165 AD, St. Martin Busskirch is one of the oldest churches around uper Lake Zürich. Even the citizens of Rapperswil had to attend services in Busskirch until Count Rudolf II built the Stadtpfarrkirche on Herrenberg next to Rapperswil Castle on Lindenhof hill. Known members of the family are Countess Elisabeth von Rapperswil, her sons Wernher von Homberg, Reichsvogt and minnesang poet, in 1415, the town bought freedom for itself. In 1442, during Old Zurich War, Rapperswil was in alliance with Zürich, because of its strategic location along important infrastructure lines, and because of flourishing trade, the town grew rich. This allowed a degree of freedom within the Swiss Confederation which ended with the formation of the Swiss cantons by Napoleon in 1799. In 1656 and 1712, Rapperswil was involved in wars between the Catholic and Reformed cantons of the Old Swiss Confederation, Rapperswil was at first part of the Helvetic and the canton of Linths capital city. After the 1803 Act of Mediation, it joined the canton of St. Gallen, on January 1,2007, the former municipalities of Rapperswil and Jona merged to form a new political entity, Rapperswil-Jona has a population of 25,777. This makes it the second-largest town in the canton after the capital of St. Gallen itself, ironman 70.3 Switzerland and the Triathon Challenge took place in Rapperswil-Jona on 6 June 2010, and was repeated several times
_Tswalu.jpg)
_2012-10-03_16-27-22.JPG)
_digging.jpg)
![[icon]](/wiki/File:Wiki_letter_w_cropped.svg){kind=small}
. PMID 23234867.
