nyuuzyou/wikis huggingface dataset:
Beyond Earth (The Future is Far)

this is part of the future is far, and it is about the development of the human race off the planet earth.
== history ==
after the collapse of civilization, and its recovery, mankind realized that if they wanted to survive as a species in the long term, would have to leave the earth.
for that big trip, we used the genesic, large ships designed to hold thousands of people. were built at least 14 of them.
each civilization was developed in different ways.
== posthuman ==
after the great migration into space, humanity to establecerce on selected planets began to evolve and develop their civilizations which were different from each other. something else that had come out of this division was the development of two new human species, smarter, stronger, and more prepared to inhabit the galaxy
the first races
in the first millennia after colonization, in two different worlds developed two different human species:
-the tanasian: human species characterized by being covered by a nanobots suit
-the kritaurians: this human species is highly intelligent, with a larger brain and higher. from 3000 to 6300 each race agreed to that neither would invade or colonize other way belica world that were owned by other races. but in the years 6300 tanasians an insurgent group, under the name dehomis they invade and they conquer tanasis. after that start a genocidal campaign against the humans, assuming they are more evolved and thus more apt to dominate all the planets. for more than 400 years war between dehomis and book other races, culminating in the extinction of the dehomis, and the destruction of tanasis, in the year 6700.
Bricket

The deciduous woodlands of the Palaearctic realm are found mostly north of the mountains at the western end of the continent, where the continent narrows and few places are far from the sea. It is a region of high rainfall and temperate climate. There are four marked seasons: dormant winter; spring in which leaves and flowers appear; summer with the most vigorous growth; and autumn, which is a time of fruiting just before the trees lose their leaves for winter. The predominant trees are oaks, ashes and beech, below which is usually an understorey of smaller trees and a thick undergrowth.A typical animal of this environment is the bricket, a small browsing hadrosaur, not dissimilar from its Cretaceous ancestors. In the Cretaceous period there were only the non-crested hadrosaurs living in this corner of the continent, but later the crested forms migrated here from further east - part of the great spread of the hadrosaurs over the northern continents. The bricket lives in small herds in the dense undergrowth and bramble thickets, usually resting during the day and feeding at dusk and at dawn. The expanded crest, found in both males and females, is both used as a display structure, particularly during the autumnal mating season, and as a deflecting device when it must move swiftly through the vegetation.
The long flat tail of the bricket is used both as a prop, when browsing from high branches, and as a warning flag at times of danger. Stuck straight up in the air its bright colours warn the rest of the herd of approaching predators.
The bricket’s streamlined shape is ideal for fast movement through the tangles and thickets of the temperate woodlands. The shape of the crest parts the vegetation as the animal runs, and the slim body allows it to pass between close-growing trees. The brownish colour camouflages the animal when motionless, but when it breaks cover and runs it can do so quickly, vanishing at speed into the depths of the forest.
Ticks, fleas, and other parasites are easily picked up by thicket-living animals. The bricket has a cleansing ritual that deals with this. A bricket suffering badly from parasites seeks out a piece of fur or a mat of hair that has been lost by another animal on the bramble thorns. Then, holding the fur in its beak, it walks backwards into a river, very slowly, until it is totally submerged, but for its snout. The parasites move up the body, the neck and the head, and are eventually all stranded in the piece of fur. The bricket then abandons the fur and its passengers to the current. There usually follows a period of playful high spirits in the water as several newly cleansed brickets frolic with one another. Mating usually takes place at this time. Further downstream the fur is seized by hungry zwims that feast on the parasites.
Carakiller

The carakiller is descended from the crested caracara and is quite similar to the terror birds (family Phorusrhacidae) of the early Cenozoic era. They have retained two large claws, one on each forelimb, much similar to the prehistoric terror bird Titanis. Around ten feet (three meters) tall, they are the largest predatory birds since the terror birds died out two million years ago, and are among the largest of all avian species.
Carakillers specialize in quick movements and hunt in packs. They commonly stroll along the outskirts of grasslands that have been set on fire, and kill any animal found struggling to escape the fire, similar to what storks do today by feeding on the fire edge. Carakillers can communicate by moving the feathers on the top of their heads. The carakillers main source of food is the babookari, although they will attempt to eat almost any animal and can easily kill any aside from the rattleback.
Category:The Future is Wild Species
Coconut Grab

The coconut grab, Nuctoceras litureperus, is an ammonite that crawls onto land to grab coconuts, similar to our robber crab. The coconut grab can even climb trees.
Scattered across the vast ocean that covers almost half the globe, is a multitude of islands. These are not fragments of any continent, but have grown completely independently of Gondwana. They have appeared mainly through volcanic action, where an underwater volcano has reached the surface and cooled. The flanks of these islands are further extended by reefs built up by corals and other sea creatures. Belonging to no recognized zoogeographic realm, this array of islands is described here as part of the Australasian realm.
At the same time as the dinosaurs developed to be the most significant animals on earth, other creatures evolved to dominate the seas. A group of animals of some importance were the ammonites, cephalopods that were encased in coiled shells. The shells consisted of empty air chambers that could be used by the animal to regulate its buoyancy. The ammonites evolved into many shapes and sizes during the Mesozoic period and are commonly found as fossils in rocks that date from that time. The coconut grab is an unusual ammonite in that it can spend much of its time out of the water crawling about on land. On many of the tropical islands of the ocean it can crawl up the beach and eat coconuts, and even climb trees to find the nuts when there are none available lying in the sand or washed up on the shore.
The coiled shell of the coconut grab is flat on the bottom, providing a skid-like surface that allows it to be dragged over the sand. There are eight tentacles. The four at the rear are broad and very muscular. They are used for pulling the animal over the ground and up coconut palms, left. The front four tentacles are long and delicate, allowing the ammonite to reach for a coconut. The eyes can focus both submerged and out of the water. Coconut grabs usually come ashore at night when it is cooler, and dawn finds the beach criss-crossed by their distinctive trails, right.
Coneater

The coniferous forest of the Palaearctic realms is the largest area of unbroken forest on Earth. It stretches right across the continent along the sub-polar latitudes and, but for the narrow inlet of the sea, would be continuous with that of the northern Nearctic realm. It is bounded by the tundra to the north and the deciduous forests and cold grasslands to the south. The coniferous forests contain relatively few species, compared with other forests further south. The most common conifers are pines, firs, spruces and larches. These reproduce by means of seed-dispersing cones, and it is these cones that provide the food for most of the animal life of the region. Almost the only large animal found here is the coneater, a 3-metre-long (10 ft) hypsilophodont that resembles its Cretaceous ancestors.The hypsilophodonts were a very widespread and successful group in Cretaceous times. Lightly built running animals, very much like small iguanodonts, they spread over all the continents before the end of the period. They have continued to be successful all over the world until the present day, occupying a large number of different niches. In the dark depths of the coniferous forest they run in small herds, over the soft undergrowth-free forest floor, and browse in more open country along the river banks. Although the coneater generally eats the cones and the seeds they contain, in winter it eats tree bark, needles, mosses and lichens, and seeks out stores of nuts hoarded by smaller animals.
The coneater is an animal of small herds, each herd consisting of about a dozen individuals. Its body is insulated from the intense winter cold by deep folds and wrinkles of fat. Its beak can snip twigs and cones (a), and its tough food is ground up between batteries of grinding teeth at the back of the mouth.
Crackbeak

The Crackbeak, Fortirostrum fructiphagum, is an arboreal hypsilophodont that evolved specialized perching feet. They use their beaks for cracking seeds and fruit (Africa, Asia, and Australia).
High in the luxuriant branches of the tropical forest trees in the north-east of the Australasian continent, a black and white creature throws itself from one branch to another and disappears among the foliage. At first glance it looks like an arbrosaur, one of the tree-living coelurosaurs that are found all over the world. Then it appears again, and its bright face, surmounted by a high crest, is its most obvious feature. This is a crackbeak , a tree-living descendant of the successful hypsilophodonts.Crackbeak ancestors were lightly built running animals, evolved to run swiftly across open country. Now the legs have developed into jumping legs, and the lightweight feet have evolved for perching. The small first toe has turned round to face the rear, so the foot can now be used for grasping branches. The tail is still a long, stiff balancing organ but can now be used as a third leg; pressed against a tree-trunk it gives the animal a firm anchor while feeding. As in the arbrosaurs, the crackbeak has developed a strong system of bones and muscles in the shoulder region to help it climb trees. The front feet have become dextrous hands. Crack-beaks are found in many other parts of the world, particularly in the tropical rainforests of the Ethiopian and Oriental realms, but it is only on the Australasian continent that they are so abundant and varied.
The crackbeak's bill is delicate enough to pick individual berries out of a bunch, yet powerful enough to crack open even the hardest nuts. The beak is used only for picking and cracking; the actual chewing is done by the back teeth. The horny crest on the head, along with the bright colour of the face and dewlap, are used for signalling both to mates and to enemies.
The superficial resemblance in size and shape between the Australasian crackbeak and the arbrosaurs of the northern continents have come about by convergent evolution. They both evolved from lightly built running ancestors and have become lightly built tree-dwelling animals, but whereas the arbrosaurs subsist on a diet of insects and small vertebrates, the crackbeak is strictly vegetarian.
The crackbeak hand, like those of all hypsilophodonts and most of their descendants, has a full complement of five fingers. All the fingers are long and mobile. Both the first and the fifth fingers are opposable, or able to cross over the palm of the hand in order to grasp things. These are very useful to the crackbeak while climbing in the branches and selecting food from between the twigs.
Cribrum

The cribrum, Cribrusaurus rubicundus, is a flamingo-like predatory dinosaur with slender teeth for straining soda lakes for microorganisms.
The rivers that drain from the eastern mountains into the arid hinterland of the Australasian continent often seep away into the desert, or else form lakes. Lakes that form in the rainy season support an explosive burst of algae and crustaceans, and the cribrum feeds on these. Coelurosaurs have been present on the Australasian continent at least since Kakuru (rainbow lizard) hunted there in early Cretaceous times. It would be from a creature such as this that the cribrum evolved. In build it is rather like a conventional 2-metre-long (6 ft) coelurosaur, but the long curved jaws are armed with thousands of tiny, needle-like teeth. These strain living creatures from the fine mud and water of the deltas and lakes. An unusual feature of the cribrum is that it changes colour depending on where it is feeding. When it is feeding in the fresh water of the streams, the colour is a light grey. When it feeds on crustaceans and algae in the salty waters of the lakes, however, its skin and hair turn pink. The red coloration in the algae is concentrated in the bodies of the crustaceans that feed on it, and thus appears in the pigmentation of the cribrum that feed on them.
The cribrum stands in the shallow water, often on one leg, and feeds by sieving the water through its finely toothed jaws. It swings its head around in a wide arc to cover as much water as possible.
There are few predators on the shores of the salty lakes, but when one does appear, slinking down to the water's edge to try and trap an unwary cribrum, the herds panic and scatter in all directions. The milling surge of pink distracts and confuses the hunter, while the voluminous curtains of spray thrown up by the dash through the shallow water conceals the direction of the fleeing herd.
Category:The New Dinosaurs
Cutlasstooth

The Cutlasstooth, Caedosaurus gladiadens, is a saber-toothed predatory dinosaur (South America).
Many animals flooded into the Neotropical continent about four million years ago, when the string of volcanic islands linking with the Nearctic continent to the north, fused to form a land bridge. The animals quickly evolved and developed to fill the ecological niches they found. In most instances the animals that came south were more successful and began to replace the indigenous animals that had dominated the continent for the previous 50 million years. The reason for this may be that the indigenous animals had evolved few variations in that period of time. The continent itself had not shifted substantially and there had been little change in the environment and the climate except for the spread of the grasslands. There was no necessity then, for the animals to evolve, and they had settled into a long period of decadence.animals from the north, on the other hand, had suffered millions of years of change, with changes in climate and interchange of animals with the Palaearctic realm, and had been evolving vigorously. When they reached the Neotropical continent they were more able to adapt to the conditions found there and, as a result, the native animals suffered. The most noticeable instance is found among the meat-eaters. The first of the northern animals to reach the continent were the mountain-leapers. Being skilled at traversing high mountain ranges, they were well able to cross the mountainous neck of land that connected the two continents and spread into many of the ecological niches. Large meat-eaters quickly developed from this stock and preyed on the swift-footed sauropods of the plains. Even larger types developed, some with their heavy heads and small arms, looking as if they had evolved from the great carnosaurs of the Cretaceous period rather than the small agile coelurosaurs.One such is the cutlasstooth which has evolved huge cutting teeth that enable it to prey on the large sauropods like the lumber. Hunting in packs, cutlasstooths can set upon a lumber and slash it until it bleeds to death.
The cutlasstooth's dental arrangement is unique among dinosaurs. The first tooth of each upper row is a long, curved slashing weapon (a). Those behind it are continually growing. Once the front tooth is broken and discarded there is another to take its place (b).
The jaws of the cutlasstooth can open remarkably wide, so that the lower jaw is well away from the cutting teeth when the heavy head is thrust downwards in the slashing stroke (c). The undersides of the large teeth are serrated and work against the lower teeth as carnassial (meat-shearing) blades for ripping and chewing flesh when the animal is eating. When hunting, a pack of four or five can inflict deep bleeding wounds on the flanks of their prey (d), and then wait until it bleeds to death.
Dougal Dixon

Dougal Dixon is a geologist and author, born in Dumfries, Scotland, in 1947. He has had an important role in the development of the field known as speculative biology and is an authority on dinosaurs and prehistoric life. He is the author of over 20 books on dinosaurs as well as other topics of interest. Dixon graduated Bachelor of Science in geology in 1970 and Master of Science in 1972. He worked for two publishing companies as a consultant and editor before going freelance. He married Jean Dixon in 1971, and they currently have two children, Gavin and Lindsay.
==Author==
Dougal Dixon is a full-time writer and editor who has many books related to earth science and paleontology, more specifically dinosaurs. A majority of his publications have been related to mainstream earth science but he is more famous for his books involving speculative biology, beginning with After Man: A Zoology of the Future (1981). After Man postulates what life might be like 50 million years hence and demonstrate several scientific principles. His other speculative biology books include The New Dinosaurs (1988) and Man After Man (1990).
===Television===
He has also made appearances on television, and has acted as a consultant for a program about dinosaurs.
==Awards==
He has won a number of awards including Distinguished Achievement Award for Excellence in Educational Journalism by The Educational Press Association of America in 1993, the Helen Roney Sattler Award in 1993, The Children's Book Council 1994 Outstanding Trade Science Book Award, and the Times Educational Supplement Primary Schoolbook Award 1996. He was also appointed as a trustee of the Dinosaur Society, UK.
Category:People
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Kraken

The Kraken, Giganticeras fluitarus, is a massive floating ammonite with a shell 13 feet in diameter. Its tentacles are covered with poisonous barbs like those of a jellyfish. These deadly tentacles spread out in an area of 67 feet in diameter. The kraken only fears the pelorus, who is immune to its poisonous stings.
The ammonites of the Mesozoic seas were mostly swimming animals that moved freely about in the ocean waters chasing small swimming creatures that they caught with their tentacles. In Cretaceous times they developed into a number of different forms. There were those with heavy shells produced in irregular coils, that spent their time crawling along the sea bed. Others were freely drifting animals, filtering microscopic food particles from the water using very fine tentacles. This second trend has reached a pinnacle with the modern kraken.The shell of the kraken is truly enormous, some specimens reaching 4 metres (13 ft) in diameter. The shell acts as a protective armour, as well as a float to keep the animal in the fertile surface waters. It has twelve tentacles that it spreads out around itself, and each of these has thousands of trailing fibres that are armed with stings and hooks. The whole arrangement forms a deadly net that covers an area of about 20 metres (67 ft) in diameter. The kraken will eat almost anything that becomes entangled in its traps, from microscopic floating plants, to fairly large fish. Many krakens often drift in the same area of productive waters, their floating shells acting as perches for migrant birds and pterosaurs.
The internal structure of the kraken is a (scaled-up) version of the internal structure of any shelled cephalopod. The shell has a number of chambers, and the animal occupies the last one. As the kraken grows it produces more shell, moves forward and lays down a wall to create a new chamber behind. A blood vessel connecting all the chambers controls the air pressure and hence buoyancy.
The twelve tentacles with their trailing curtain of stings and hooks, radiate from the mouth at the shells entrance.
The air-filled chambers of the kraken's shell mean that it floats with the living animal and the tentacles just submerged (a). It moves by expelling waste water through its syphon, propelling the shell backwards and allowing the tentacles to trail behind (b).