Biology: The Dynamic Science (MindTap Course List)
Biology: The Dynamic Science (MindTap Course List)
4th Edition
ISBN: 9781305389892
Author: Peter J. Russell, Paul E. Hertz, Beverly McMillan
Publisher: Cengage Learning
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Chapter 25, Problem 2ITD
Summary Introduction

To review:

The modern levels of carbon dioxide and oxygen, as compared to the levels when they first came to exist.

Introduction:

The formation of Earth took place around 4.6 billion years ago. The asteroid impacts were at a peak after the earth’s formation but then started decreasing subsequently. The asteroid impacts ceased to be of consequence around 3.7 billion ago. As the asteroid impact decreased, the level of oxygen (O2) started increasing. The decrease in the impact of asteroid played a crucial role in the origin of life. The plausibility of life increased when the impact of asteroid diminished.

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After you feel comfortable with your counting method and identifying cells in the various stages of mitosis, use the four images below of whitefish blastula to count the cells in each stage until you reach 100 total cells, recording your data below in Data Table 1. (You may not need to use all four images. Stop counting when you reach 100 total cells.) After totaling the cells in each stage, calculate the percent of cells in each stage. (Divide total of stage by overall total of 100 and then multiply by 100 to obtain percentage.)   Data Table 1Stage    Totals    PercentInterphase        Mitosis:        Prophase        Metaphase        Anaphase        Telophase        Cytokinesis        Totals    100    100% To find the length of time whitefish blastula cells spend in each stage, multiply the percent (recorded as a decimal, in other words take the percent number and divide by 100) by 24 hours. (Example: If percent is 20%, then Time in Hours = .2 * 24 = 4.8) Record your data in Data…
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