Life: The Science of Biology
Life: The Science of Biology
11th Edition
ISBN: 9781319010164
Author: David E. Sadava, David M. Hillis, H. Craig Heller, Sally D. Hacker
Publisher: W. H. Freeman
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Chapter 24, Problem 3Q
Summary Introduction

To review:

The factors that resulted in the extinction of Ediacaran biota and the rise of the Cambrian type biota.

Introduction:

Ediacaran fossils are the strata formed by organisms found in the Ediacaran period. This period lasted from about 635 million years to 542 million years ago. Ediacaran strata are unique collection of soft-bodied organisms, mostly sessile organisms that are conserved worldwide as fossil impressions in this Ediacaran period.

The Cambrian period is the period of ancient life that lasted about 53 million years ago and it is known for dramatic evolutionary changes in life on the earth. Cambrian period faced Cambrian explosion that saw the diversity of life typically major animal groups alive today. The animal group majorly contains chordates, vertebrates such as humans.

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The Cambrian Explosion occurred due to the widespread adoption of bilateral symmetry and the extinction of the Ediacaran fauna. What is this burst of diversity referred to? Explain what kind of triggers these two factors are and why they led to greater diversity.
Explain what significant events happened during the Five major extinction events between the late Cambrian until the late cretaceous period.
The eon comprising the Cambrian period up to the present is called the (1). It is divided into three eras: Paleozoic, Mesozoic, and Cenozoic. The Paleozoic era, first (2) appeared. Finally, the Cenozoic era is where (3), flourished, lasting up to this day.
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