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    History of Life on Earth

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    Chapter 25: History of Life on Earth Synthesis of Organic Compounds on Early Earth * The Earth probably formed about 4.6 billion years ago‚ and was bombarded with rocks and other material until about 3.9 billion years ago. * The Earth then cooled‚ allowing for the formation of oceans. Scientists hypothesize the general atmosphere‚ or at least some regions‚ were naturally reducing environments‚ meaning that they added electrons to compounds. * Activation energy provided by lightening

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    Gobi Desert

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    to the expansion. Explorers have longed to delve into the intact Gobi Desert for centuries. Being scrutinized by professionals all over the world‚ many important fossil has been found in the desert‚ including the first scientifically recognized dinosaur egg fossils in 1923. Other than fossil findings‚ explorers had also spotted a large gold and copper deposit in the South of the Gobi Desert and named it as the Oyu Tolgoi Mine. The mining will inevitably credit to the countries’ income. Yet‚ the

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    Ttakji

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    the worst; vertebrate recovery took 30 million years.The most recent‚ the Cretaceous–Tertiary extinction event‚ occurred 65 million years ago‚ and has often attracted more attention than others because it resulted in the extinction of the nonavian dinosaurs. The period since the emergence of humans has displayed an ongoing biodiversity

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    Mass Extinctions What is the biological significance of mass extinctions? PART A You are living in the 23rd century. All knowledge of scientific things have been hidden from the human race by evil dictators during the last 2 generations of humans. One brilliant scientist‚ Albert Einstein the 16th‚ has rebelled against the dictators. He has devised a time machine and is asking for volunteers to go back in time and bring back important scientific discoveries. Your assignment is to go back to

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    Big Bend National Park Report 1. What is the depositional nature of the rocks in the study area and how does their lithologic compositions and sedimentary structures record changing water depths‚ environments of deposition‚ and paleogeography? Big bend national park has complex rocks that are subsided in two seas hundreds of millions of years ago. Fossil data from the mid to Upper Cretaceous period predicts the sequence of rock strata in Big Bend National Park to be from bottom to top: limestone

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    “Sound of Thunder” and “Being Prey” are like two peas in a pod‚ except they are two different types of peas. “Sound of Thunder‚” written by Ray Bradbury‚ and “Being Prey‚” written by Val Plumwood‚ are two similar stories but contains characteristics that make each of the stories unique. They are similar in terms of characters‚ setting‚ and suspense‚ but at the same time they all have certain things that the other story doesn’t have. To start off‚ the characters in “Sound of Thunder” and “Being Prey”

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    Overkill Hypothesis

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    1.) Were the North American megafauna wiped out by early human colonizers? The Overkill hypothesis is of the Clovis crossing into a “virgin continent” (The America’s) and wiped out the megafauna due to overhunting. First developed by Paul Martin in the 1960’s‚ Clovis started to occupy North and South America 13‚500-12‚500 years ago; soon after early sites were established 17 genera of North and South American megafauna went extinct between 13‚250-12‚900 (other species such as ground sloths become

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    Unit 9 Mass Extinctions

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    Task 9: Mass Extinctions Introduction: In this report I will talk to you about the 5 mass extinctions that have happened on earth over the past 434 million years. I will also talk to you about the effects of the current mass extinction. The last things i will show is a list of 10 recently extinct species and 10 endangered species. Number 1: The Ordovician Silurian Extinction This extinction happened about 439 million years ago‚ because of a drop in sea levels as glaciers formed. An ice age has been

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    The Triassic-Jurassic

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    The Triassic-Jurassic Boundary Extinction There have been five major extinction events in geologic history. The largest of which was the Permian-Triassic extinction that occurred approximately 251 million years ago. During this extinction‚ 96% of marine species and 70% of terrestrial vertebrate species went extinct. Other extinction events include the Cretaceous- Tertiary and the End Ordovician. The Triassic-Jurassic boundary extinction occurred 200 million years ago during the Phanerozoic

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    Mass Extinction

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    occurred about 251 million years ago and took about 96% of marine animals. It also took a huge toll on terrestrial animals. About 65 million years ago in the Cretaceous period‚ the earth had another mass extinction (Campell). During this day and age‚ dinosaurs reined the land and pterosaur ruled the sky. The causes of extinctions can be broken down into two different categories which are‚ terrestrial and extraterrestrial. Firstly‚ in terrestrial causes‚ moving continents can be a major factor in extinctions

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