Scientific name : Uniculo unicorn Common name : Unicorn Because of sexual selection, female choose the strongest and the most beautiful horn male to become their mate. This is the reason why unicorns are very beautiful and a lot of human want to hunt them for the horn.
The Cretaceous Period was the last and longest segment of the Mesozoic Era. It lasted approximately 79 million years, from the minor extinction event that closed the Jurassic Period about 145.5 million years ago to the Cretaceous-Paleogene (K-Pg) extinction event dated at 65.5 million years ago.
Scientific name : Uniculo amecorn Common name : Acorn Acorn is the ancestor of all organism in the Uniculo genus. It is unicellular eukaryote organism. Acorn has special organelle called “horn” for communicate to other acorn.
Scientific name : Uniculo yeticorn Common name : Yecorn Because extremely cold weather of Ice age, yecorns adapt themselves by has a lot of adipose tissue and thick fur cover their body.
The Jurassic period is the second of the three divisions of the Mesozoic era, "The Age of Reptiles." The Jurassic lasted for 64 million years, from about 208 to 144 million years ago. The period is named for rock strata found in the Jura Mountains on the border between Switzerland and France.
Scientific name : Uniculo pegacorn Common name : Pegasus Unicorn evolve their wings and become Pegasus to be able to escape from human. They still have like snow fur color for hide from the predators and human.
The Neogene Period traditionally comprised the Miocene and Pliocene Epochs. Recent changes by the ICS appeared to eliminate the Quaternary, so that the Neogene included the Pleistocene and Holocene. Even more recently, the ICS has indicated it will reanimate the Quaternary as a sort of stratigraphic Frankenstein assembled from ill-fitting spare parts, "gigantic in stature, yet uncouth and distorted in its proportions." However, in doing so, the ICS proposes to preserve the extension of the Neogene to the Present.
The Proterozoic is known for large‐scale rifting of continental crust across the world and the filling of these rifts with huge amounts of sedimentary and volcanic rocks.
The Mesozoic era occurred from about 245 million to 66 million years ago. The fossil record from this era (the “Age of the Dinosaurs”) is dominated by a multitude of dinosaur species. Common sedimentary deposits are red sandstones and mudstones.
The Triassic Period was the first period of the Mesozoic Era and occurred between 251 million and 199 million years ago. It followed the great mass extinction at the end of the Permian Period and was a time when life outside of the oceans began to diversify.
Scientific name : Uniculo spikorn Common name : Sicorn Spicorn develop their skin become harder and has spike to use for protect from other predators.
The Permian period lasted from 299 to 251 million years ago* and was the last period of the Paleozoic Era. The distinction between the Paleozoic and the Mesozoic is made at the end of the Permian in recognition of the largest mass extinction recorded in the history of life on Earth. It affected many groups of organisms in many different environments, but it affected marine communities the most by far, causing the extinction of most of the marine invertebrates of the time. Some groups survived the Permian mass extinction in greatly diminished numbers, but they never again reached the ecological dominance they once had, clearing the way for another group of sea life. On land, a relatively smaller extinction of diapsids and synapsids cleared the way for other forms to dominate, and led to what has been called the "Age of Dinosaurs." Also, the great forests of fern-like plants shifted to gymnosperms, plants with their offspring enclosed within seeds. Modern conifers, the most familiar gymnosperms of today, first appear in the fossil record of the Permian. The Permian was a time of great changes and life on Earth was never the same again.
Scientific name : Uniculo wihorcorn Common name : Horcorn The earth become warmer, so horcorn have thinner fur and become smaller to adapt to the environment.
The Pennsylvanian (also known as Upper Carboniferous or Late Carboniferous) is, in the ICS geologic timescale, the younger of two subperiods (or upper of two subsystems) of the Carboniferous Period. It lasted from roughly 323.2 million years ago to 298.9 million years ago Ma (million years ago). As with most other geochronologic units, the rock beds that define the Pennsylvanian are well identified, but the exact date of the start and end are uncertain by a few hundred thousand years. The Pennsylvanian is named after the U.S. state of Pennsylvania, where the coal-productive beds of this age are widespread.
Scientific name : Uniculo lizarkorn Common name : Licorn Licorn start to live permanently in the land. They use lung for exchange gas instate of gill.
The Carboniferous Period lasted from about 359.2 to 299 million years ago during the late Paleozoic Era. The term "Carboniferous" comes from England, in reference to the rich deposits of coal that occur there. These deposits of coal occur throughout northern Europe, Asia, and midwestern and eastern North America. The term "Carboniferous" is used throughout the world to describe this period, although in the United States it has been separated into the Mississippian (early Carboniferous) and the Pennsylvanian (late Carboniferous) Subsystems. This division was established to distinguish the coal-bearing layers of the Pennsylvanian from the mostly limestone Mississippian, and is a result of differing stratigraphy on the different continents. The Mississippian and Pennsylvanian, in turn, are subdivided into a number of internationally recognized stages based on evolutionary successions of fossil groups . These stages are (from early to late) Tournaisian, Visean, and Serpukhovian for the Mississippian — and Bashkirian, Moscovian, Kasimovian, and Gzhelian for the Pennsylvanian.
The Archean was dominated by crustal building and the development of extensive volcanic belts, arcs, and sedimentary basins that were probably related to plate tectonic activity.
The Rhynie Chert in Scotland is a Devonian age deposit containing fossils of both zosterophylls and trimerophytes, some of the earliest vascular plants. This indicates that prior to the start of the Devonian, the first major radiations of plants had already happened. The oldest known vascular plants in the Northern Hemisphere are from the Devonian Period. The vegetation of the early Devonian consisted primarily of small plants, the tallest being only a meter tall. By the end of the Devonian, ferns, horsetails and seed plants had also appeared, producing the first trees and the first forests.
Scientific name : Uniculo salamancorn Common name : Salacorn Salacorn migrate to live in the shallow sea and can also live in the land. They develop their legs for moving and can still swimming. Salacorn is the amphibian.
was a time when the Earth underwent considerable changes that had important repercussions for the environment and life within it. One result of these changes was the melting of large glacial formations. This contributed to a substantial rise in the levels of the major seas. The Silurian witnessed a relative stabilization of the Earth's general climate, ending the previous pattern of erratic climatic fluctuations.
Scientific name : Uniculo megsharkorn Common name : Magcorn Magcorn evolve one more pair of fin for better swimming. They develop their horn to be the radar and can use for protect themselves.
Little is known about the Hadean because there are so few rocks of that age, and those that do exist are intensely deformed and metamorphosed.
Scientific name : Uniculo sharkorn Common name : Shacorn Shacorn evolve their inside organ system and skin. They evolve fin for better moving in the water. They migrate to live near the water surface, so the develop their eyes.
The Ordovician Period lasted almost 45 million years, beginning 488.3 million years ago and ending 443.7 million years ago. During this period, the area north of the tropics was almost entirely ocean, and most of the world's land was collected into the southern supercontinent Gondwana. Throughout the Ordovician, Gondwana shifted towards the South Pole and much of it was submerged underwater.
Scientific name : Uniculo jellycorn Common name : Jacorn Jacorn is evolved from acorn. They evolve the tentacle to use for moving, hunting and protecting themselves. Jacon live in very deep ocean, so they do not need eyes for looking.
The Paleozoic era was long believed by geologists to mark the beginning of life, because of the sudden abundance of complex organisms with hard parts in the fossil record.
The Cambrian marked a profound change in life on Earth; prior to the Cambrian, the majority of living organisms on the whole were small, unicellular and simple; the Precambrian Charnia being exceptional. Complex, multicellular organisms gradually became more common in the millions of years immediately preceding the Cambrian, but it was not until this period that mineralized—hence readily fossilized—organisms became common.
The Cenozoic era, also called the “Age of Recent Life” or “Age of Mammals,” encompasses the last 66 million years of the earth's history. Life forms continued to become more complex. The Cenozoic has the most complete geologic record of any era because it is so recent.
is a geologic period and system that spans 43 million years from the end of the Cretaceous Period 66 million years ago (Mya) to the beginning of the Neogene Period 23.03 Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The Paleogene is most notable for being the time during which mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of the Cretaceous–Paleogene extinction event that ended the preceding Cretaceous Period.
Scientific name : Uniculo polarkor Common name : Porcorn After the mass extinction, some of Spicorn can survive and migrate to the top of the mountain that have snow cover and evolve to the porcorn , so their make white fur to camouflaged with the environment.
We'd love to hear from you. Please send questions or feedback to the below email addresses.
Before contacting us, you may wish to visit our FAQs page which has lots of useful info on Tiki-Toki.
We can be contacted by email at: hello@tiki-toki.com.
You can also follow us on twitter at twitter.com/tiki_toki.
If you are having any problems with Tiki-Toki, please contact us as at: help@tiki-toki.com
Close