ORIGIN OF EARTH AND EVOLUTION OF THE ENVIRONMENT



Similar documents
UNIT V. Earth and Space. Earth and the Solar System

Chapter 9: Earth s Past

STUDY GUIDE: Earth Sun Moon

Asteroids. Earth. Asteroids. Earth Distance from sun: 149,600,000 kilometers (92,960,000 miles) Diameter: 12,756 kilometers (7,926 miles) dotted line

Related Standards and Background Information

CHARACTERISTICS OF THE SOLAR SYSTEM

The Fossil Record and Geologic Time Scale

THE SOLAR SYSTEM - EXERCISES 1

Unit 5: Formation of the Earth

Astronomy Notes for Educators

Name: João Fernando Alves da Silva Class: 7-4 Number: 10

The Solar System. Source

California Standards Grades 9 12 Boardworks 2009 Science Contents Standards Mapping

KINDERGARTEN 1 WEEK LESSON PLANS AND ACTIVITIES

Section 1 The Earth System

4 HOW OUR SOLAR SYSTEM FORMED 750L

3 The Mesozoic and Cenozoic Eras

The Earth, Sun, and Moon

2007 Pearson Education Inc., publishing as Pearson Addison-Wesley. The Jovian Planets

A SOLAR SYSTEM COLORING BOOK

Earth Sciences -- Grades 9, 10, 11, and 12. California State Science Content Standards. Mobile Climate Science Labs

SGL 101 MATERIALS OF THE EARTH Lecture 1 C.M.NYAMAI LECTURE ORIGIN, STRUCTURE AND COMPOSITION OF THE EARTH

Name Class Date WHAT I KNOW. about how organisms have changed. grown in complexity over time.

Unit 2 Lesson 4 The Geologic Time Scale. Copyright Houghton Mifflin Harcourt Publishing Company

astronomy A planet was viewed from Earth for several hours. The diagrams below represent the appearance of the planet at four different times.

THE WATER CYCLE. Ecology

Grade Level Expectations for the Sunshine State Standards

Geologic Time Scale Notes

Solar System Fact Sheet

A Solar System Coloring Book

THE SOLAR SYSTEM. Worksheets UNIT 1. Raül Martínez Verdún

Introduction to the Solar System

Study Guide due Friday, 1/29

Introduction and Origin of the Earth

GLOBAL CIRCULATION OF WATER

Assignment 5. Multiple Choice Identify the letter of the choice that best completes the statement or answers the question.

1 A Solar System Is Born

Study Guide: Solar System

Science Standard 4 Earth in Space Grade Level Expectations

NOTES: GEORGIA HIGH SCHOOL SCIENCE TEST THE SOLAR SYSTEM

Composition of the Atmosphere. Outline Atmospheric Composition Nitrogen and Oxygen Lightning Homework

Class 2 Solar System Characteristics Formation Exosolar Planets

A: Planets. Q: Which of the following objects would NOT be described as a small body: asteroids, meteoroids, comets, planets?

Name: DUE: May 2, 2013 Ms. Galaydick. Geologic Time Scale Era Period End date (in millions of years) Cenozoic Quaternary present

1.1 A Modern View of the Universe" Our goals for learning: What is our place in the universe?"

Solar System Overview

The Sun and the Stars

Lecture 23: Terrestrial Worlds in Comparison. This lecture compares and contrasts the properties and evolution of the 5 main terrestrial bodies.

Lecture 10 Formation of the Solar System January 6c, 2014

The Main Point. Lecture #34: Solar System Origin II. Chemical Condensation ( Lewis ) Model. How did the solar system form? Reading: Chapter 8.

The Inner Solar System by Leslie Cargile

Lecture 12: The Solar System Briefly

Georgia Performance Standards Framework for Science Grade 6. Unit Organizer: UNIVERSE AND SOLAR SYSTEM (Approximate Time 3 Weeks)

History of the Earth/Geologic Time 5E Unit

The Earth System. The geosphere is the solid Earth that includes the continental and oceanic crust as well as the various layers of Earth s interior.

Science 9 Worksheet 13-1 The Solar System

Match the term or person with the appropriate phrase. You may use each answer once, more than once or not at all.

CHAPTER 6 THE TERRESTRIAL PLANETS

Geologic Time Scale Newcomer Academy Visualization Three

The sun and planets. On this picture, the sizes of the sun and 8 planets are to scale. Their positions relative to each other are not to scale.

Multiple Choice Identify the choice that best completes the statement or answers the question.

The Solar System. Olivia Paquette

4 HOW OUR SOLAR SYSTEM FORMED 890L

Earth Is Not the Center of the Universe

The Solar System. Unit 4 covers the following framework standards: ES 10 and PS 11. Content was adapted the following:

Mission To Mars! A dialogue activity for upper KS2

2. What kind of energy is stored in food? A. chemical energy B. heat energy C. kinetic energy D. light energy

GETTING TO THE CORE: THE LINK BETWEEN TEMPERATURE AND CARBON DIOXIDE

GRADE 6 SCIENCE. Demonstrate a respect for all forms of life and a growing appreciation for the beauty and diversity of God s world.

Chapter 6 Formation of Planetary Systems Our Solar System and Beyond

2- The Top and bottom of the leaf is covered by thin layer of cells called epidermis that allow sunlight to easily pass into the middle of the leaf.

4 HOW OUR SOLAR SYSTEM FORMED 1020L

Journey to other celestial objects. learning outcomes

What are the subsystems of the Earth? The 4 spheres

Chapter 7 Our Planetary System. Agenda. Intro Astronomy. Intro Astronomy. What does the solar system look like? A. General Basics

The spectacular eruption of a volcano, the magnificent scenery of a

The Origin of Life. The Origin of Life. Reconstructing the history of life: What features define living systems?

Atmospheric Layers. Ionosphere. Exosphere. Thermosphere. Mesosphere. Stratosphere. Troposphere. mi (km) above sea level 250 (400) 50 (80) 30 (50)

Lesson Plan Title. Toilet Paper Tape Measure of Geologic Time

Cosmic Journey: A Solar System Adventure General Information

Which of the following can be determined based on this model? The atmosphere is the only reservoir on Earth that can store carbon in any form. A.

galaxy solar system supernova (noun) (noun) (noun)

Name Class Date. true

Chapter 1: Our Place in the Universe Pearson Education Inc., publishing as Addison-Wesley

Unit 1.8: Earth and Space Science Planets & Stars

Scope and Sequence Interactive Science grades 6-8

Introduction to Plants

Processes Within an Ecosystem

Question Bank Five Kingdom Classification

Science I Classroom Guide

Photosynthesis. Grade-Level Expectations The exercises in these instructional tasks address content related to the following grade-level expectations:

DESCRIPTION ACADEMIC STANDARDS INSTRUCTIONAL GOALS VOCABULARY BEFORE SHOWING. Subject Area: Science

ORANGE PUBLIC SCHOOLS OFFICE OF CURRICULUM AND INSTRUCTION OFFICE OF SCIENCE. GRADE 6 SCIENCE Post - Assessment

Earth Science: Sphere Interactions

Solar System Formation

Geologic History Review

Grade 6 Standard 3 Unit Test A Astronomy. 1. The four inner planets are rocky and small. Which description best fits the next four outer planets?

Review 1. Multiple Choice Identify the choice that best completes the statement or answers the question.

Chapter 7 Our Planetary System. What does the solar system look like? Thought Question How does the Earth-Sun distance compare with the Sun s radius

Transcription:

Origin of Earth and Evoluation of the Environment MODULE - 1 1 ORIGIN OF EARTH AND EVOLUTION OF THE ENVIRONMENT We live on a beautiful planet called earth, along with a wide variety of plants, animals and other organisms. Our earth, however, is part of a vast universe. The universe is about 15 to 20 billion years old. The age of the earth is approximately 4 to 5 billion years, while human beings evolved only around 2 million years ago. In this lesson, you shall learn how the earth originated, how it got its own environment and in what ways human beings have been using the environmental resources for their welfare and development. OBJECTIVES After completing this lesson, you will be able to: trace the origin of the earth; list the conditions, which make the earth a unique planet for supporting life; describe the sequence of steps in the origin and evolution of life prior to the appearance of humans; explain the term environment; enumerate the various biotic and abiotic constituents of the environment. 1.1 EARTH AS PART OF THE UNIVERSE AND THE SOLAR SYSTEM Our earth, with all its diversity alongwith other planets and their satellites, the sun, the moon, the many galaxies (huge groups of millions of stars) form the universe. There are also countless asteroids and comets in orbit around the sun. All these are also part of the universe. It extends much farther than can be seen by the most powerful telescope. No one knows where the universe ends. 1

MODULE - 1 Environmental Science Senior Secondary Course When you look up at the sky on a clear night, you see many points of light most of which are stars. Stars are huge balls of bright, hot glowing gases. The Sun is also a star. It is the star nearest to earth about 150 mk (million kilometers) away. A solar system consists of a star in the middle with a number of planets orbiting around it. The earth is a part of its solar system. It is one of the eight planets of the solar system that has the sun (a star) in the middle and the eight planets moving around it. Until recently solar system was believed to have nine planets. However, on the basis of the latest scientific assessment, Pluto, is no longer regarded as a planet of earth s solar system. (Fig. 1.1) Sun Fig. 1.1: Planets orbiting the sun 1.2 ORIGIN OF THE UNIVERSE AND ORIGIN OF THE EARTH The widely accepted theory of the origin of universe is the BIG BANG theory. According to this theory, universe started with a huge explosion and matter (dust and gases) filled the entire space. The temperature of the universe then, was about hundred billion degrees Celsius. Scientists believe that the big bang occurred about 15 to 20 billion years ago. The huge collection of dust and gases then began to spin. As it spun faster and faster, the centre became very hot. It became the Sun. From the edges of this ball of dust and gas, big blobs or chunks of dust broke off and formed eight ball shaped planets. This founded our solar system (Fig. 1.2). The earth broke off about 4.5 billion years ago with an explosion. It was a burning hot white mass of gas and dust. Over a long period of time, dust and gas gradually condensed to form solid rock. Such condensation and shrinking made the earth heat up so much that the rock melted into a gluey liquid. After millions of years, the outer surface of the earth or the earth s crust cooled and formed hard rock again, just as melted chocolate or wax solidifies upon cooling. The interior of the earth is still very hot. 2

Origin of Earth and Evoluation of the Environment MODULE - 1 Vast rotating mass of gas becomes spherical and bulges at its equator Ring of matter flung off from central mass Ring of matter cools, contracts becoming a solid planet in the oribit of the central mass which becomes sun (a) (b) (c) Fig. 1.2: Formation of planets The crust of the earth was formed from cooling and hardening of the molten matter and hot gases. With cooling of the earth the crust hardened and formed the land. Cooling of the earth also condensed water vapour into liquid water filling the depressions to form seas. 1.2.1 The earth The earth with its blue skies, vast oceans and lush green forests is the home to wide variety of organisms. It has its own unique atmosphere. The atmosphere also helps to regulate the ambient (surrounding) temperature which is suitable for supporting life. If you could dig a deep hole into earth the deeper you go, the hotter it becomes. At the depth of about eight km it is hot enough to roast a human body. About 32 km deep you would reach the part of earth which is called mantle. This is made of hard rock. The centre or core of the earth is approximately 6,400 km from the surface having a temperature close to 5000ºC. Much of the earth s core is hot liquid (Fig. 1.3a) 2900 Kms Crust (Upper lithosphere) (Depth 45 kms) Lithosphere 100 kms Axis Core (1420 kms) Mantle Fig. 1.3a: Interior of the earth Fig. 1.3b: Rotation of the earth 3

MODULE - 1 Environmental Science Senior Secondary Course As you already know, once every 24 hours, the earth rotates on its axis like a spinning top. So the day and night cycle is of 24 hours. A planet s axis is an imaginary line passing through the centre of the planet. (Fig. 1.3b). The earth not only rotates around its axis but also revolves around the sun. The earth completes one full circle around the sun or completes one orbit of the sun in 365¼ days. An orbit is the path along which a planet moves around the sun. While earth revolves around the sun, moon orbits the earth. The moon completes one orbit in 27.33 days. The moon, as we know today, is without water and air and life. From the space, the earth looks like a beautiful bright bluish planet because of its blue oceans. INTEXT QUESTIONS 1.1 1. Approximately how old is the earth? 2. Name the star around which the earth revolves along with other planets of the solar system. 3. What do you mean by solar system? 4. Why does the day and night cycle consist of only 24 hours? 5. If you were to view earth from space, which colour would earth reflect? 1.3 EARTH THE UNIQUE PLANET WHICH SUSTAINS LIFE In our solar system, earth is the only planet which is known to sustain life. Only earth has air and water to support life. Let us briefly review the conditions on the other seven planets of the solar system. Mercury (Buddha) is closest to the sun. It has a temperature range of 427ºC on its side facing the Sun and 270ºC, on its dark side. It has no atmosphere. Venus (Shukra) is the closest neighbour of the earth. It is about 40 mk away. It is an extremely hot planet with a temperature of 480ºC. Its atmosphere has 96% carbon dioxide and poisonous gases like sulphur dioxide and carbon monoxide. Mars (Mangal) is also close to earth. It is called the red planet. It has 95% carbon monoxide and reddish dust. It is relatively a very cold planet and as of now presence 4

Origin of Earth and Evoluation of the Environment of life on it has not been conclusively established. Jupiter (Brahaspati) is the largest planet of the solar system. It is mainly a rapidly spinning ball of gas specially clouds of ammonia, and has no solid surface. Saturn (Shani) consists mainly of hydrogen and helium. Its atmosphere has 90% nitrogen and a temperature of (-184ºC). It is also made up of hydrogen cyanide which is a highly poisonous gas. It is characterized by a ring that surrounds it. Uranus (Arun) is also a very cold planet. Uranus is a distant planet of solar system and 7 th in order from the sun. Uranus and Neptune are the outermost planets of the solar system. Uranus has a highly tilted rotational axis. Neptune (Varun) is much smaller than earth, cold and dark with its surface coated with frozen methane. Earth is the only planet known to sustain life. Scientists do not know of any other planet in the universe Fig. 1.4: Our solar system besides the earth, where there is life. There are hundreds of stars in the universe and they have planets orbiting round them. But whether the necessary conditions to support life exist there is not known. As compared to other planets mentioned above, earth has the following unique conditions which have enabled it to sustain life. 1.3.1 Conditions necessary for sustaining life a. Presence of water As already mentioned, during the evolution of the earth, water vapour in the primitive atmosphere condensed into liquid water. This gave rise to the formation of oceans, rivers and other fresh water bodies. Three-fourth of earth s surface is covered with water. Water is a universal solvent and life originated in water. Two thirds of a living organism consists of water and 90 percent of cell content is also water. Biochemical reactions in living organisms require an aqueous medium. Therefore, water is important for the survival of living organisms. b. Atmosphere Neptune Uranus Saturn Jupiter Mars Earth Venus Mercury Sun The earth is enveloped by a gaseous atmosphere that supports life. The earth s atmosphere consists of nitrogen (78%) and oxygen (21%), small amounts of carbon dioxide, water vapour, ozone and rare gases like argon, neon etc. Oxygen from the atmosphere is used by the living organisms during respiration. Oxygen is necessary to oxidize food for liberating energy required for various activities in the living organisms. Green plants utilize carbon dioxide from the atmosphere during photosynthesis. MODULE - 1 5

MODULE - 1 c. Temperature Environmental Science Senior Secondary Course The average temperature of the earth is 16ºC. This is the most comfortable temperature for the living organisms to survive. d. Buffering capacity of earth The most unique feature of the earth is its buffering action due to which a neutral ph (ph- 7) is maintained in the soil and water bodies. The neutral ph is congenial for the survival and sustenance of living organisms. Earth gets light from the sun, the star nearest to earth, approximately 150 km away. It is the ultimate source of energy. Sun Ozone layer 25 22 Land Sea Meters Kilometers O Limit of 125 photosynthesis Deep ocean 200 400 600 800 1000 1200 1400 1600 Fig. 1.5: Solar radiations and life on the earth INTEXT QUESTIONS 1.2 1. List the conditions that make earth a unique planet. 6

Origin of Earth and Evoluation of the Environment 2. From where earth gets energy? 3. Why oxygen is essential for life? MODULE - 1 1.4 ORIGIN AND EVOLUTION OF LIFE PRIOR TO THE APPEARANCE OF HUMAN BEINGS To begin with, conditions on earth were inhospitable for life. Gases of the primitive atmosphere were primarily methane, ammonia, carbon dioxide and hydrogen. Water vapour filled the atmosphere but there was no free oxygen. It was thus a reducing atmosphere on primitive earth and no life existed. Biological evolution- from the simple organisms to complex organisms As earth cooled, water vapour condensed to form liquid water. Rains poured to form water bodies on earth. The molecules of life were formed in the water. From the molecules of the life evolved bacteria, the earliest and simplest organisms. The oldest fossils of bacteria which were the first living organisms on earth have been found in rocks that are 3-5 billion years old. For almost two billion years, different kinds of bacteria lived on earth. One of these evolved a green pigment called chlorophyll. These chlorophyll-containing bacteria used carbon dioxide and water and released oxygen through photosynthesis and started accumulating in the atmosphere. Millions of years before present 600 1000 mya 0 Similar to those living today evolve 2500 mya 3,500 mya 5000 mya No life (Reducing atmosphere) Fig. 1.6: Diagrammatic representation of major events of life on earth (mya = millions of years ago) 7

MODULE - 1 Environmental Science Senior Secondary Course Continued photosynthesis by such bacteria progressively accumulated oxygen in the atmosphere. Thus the atmosphere gradually transformed from reducing to oxidizing. At one point of time oxygen content in the atmosphere become 21%. Such changes served as a big trigger for biological evolution to begin and progress and this led to the invasion of land by living organism. As time passed, protists evolved from bacteria. Both bacteria and protists are unicellular. Then came multicellular organisms, the fungi followed by plants and animals. Today the diversity of living organisms is comprised of five kingdoms of life. Monera, Prototictista, Fungi, Plantae and Animalia. THE GEOLOGICAL TIME SCALE Era Period Epoh Age Some important (million events in the year) history of life Recent 0.01 Historic time Quaternary Pleistocene 1.8 Ice ages; humans appear Pliocene 5 Ape like ancestors of humans appear Miocene Continued radiation of mammals and Cenozoic 23 angiosperms Oligocene Origins of most modern mammalian orders, Tertiary 34 including apes Cretaceous Mesozoic Jurassic Triassie Permain Eocene Paleocene Angiosperm dominance increases; 57 further increase in mammalian diversity Major radiation of mammals, birds, 65 and pollinating insects Flowering plants (angiosperms) appear; dinosaurs 144 and many groups of organisms become extinct Gymnosperms continue as dominant plants; 208 dinosaurs dominant first birds Gymnosperms dominate landscape; 245 first dinosaurs and mammals Radiation of reptiles, origin of mammal-like reptiles and most modern orders of insects; extinction of many marine invertebrates 285 Extensive forests of vascular plants; Carboniferous first seed plants; origin of reptiles; Paleozoic 360 amphibians dominant Devonian Siturian Ordovician Cambrian Diversification of bony fishes; 408 first amphibians dominant Diversity of jawless vertebrates; colonization of land 438 by plants and arthropods; origin of vascular plants First vertebrates (jawless fishes); 505 marine algae abundant Origin of most invertebrate phyla; 544 diverse algae 700 Origin of first animals 1500 Oldest eukaryotic fossils Precambrian 2500 Oxygen begins accumulating in atmosphere 3500 Oldest definite fossils knows (prokaryotes) 4600 Approximate origin of Earth RELATIVE TIME SPAN OF ERAS Cenozoic Mesozoic Paleozoic Precambrian Fig. 1.7: Geological time scale 8

Origin of Earth and Evoluation of the Environment MODULE - 1 INTEXT QUESTIONS 1.3 1. Name the gases that were found in the primitive atmosphere. 2. Which were the earliest organisms that evolved on earth? 3. How did oxygen come into atmosphere? 4. Name the five kingdoms of life 1.5 WHAT IS ENVIRONMENT Every living organism is constantly interacting with its environment comprised of air, light, water, land or substratum and the various kinds of living organisms. The environment may be defined as the surroundings or conditions in which an organism lives or operates. The environment broadly includes living and non living components which are listed in the table given below. Table 1.1: Components of the environment Abiotic Light, climate (humidity and temperature) atmospheric gases, water, substrata (soil, river/sea bed). Biotic Living organisms including plants, animals, microorganisms (bacteria, fungi, protozoa), and human beings. A. Abiotic components i. Light Sunlight provides energy. Green plants utilize sun light for photosynthesis for synthesizing food for themselves as well as all other living organisms. ii. Rainfall Water is essential for all living beings. Majority of biochemical reactions take place in an aqueous medium. Water helps to regulate body temperature. Further, water bodies form the habitat for many aquatic plants and animals. iii. Temperature Temperature is a critical factor of the environment which greatly influences survival of organisms. Organisms can tolerate only a certain range of temperature and humidity. 9

MODULE - 1 Environmental Science Senior Secondary Course iv. Atmosphere - The earth s atmosphere is made of 21% oxygen, 78% nitrogen and 0.038% carbon dioxide. Rest are inert gases (0.93% Argon, Neon etc). v. Substratum- Organisms may be terrestrial or aquatic. Land is covered by soil and a wide variety of microbes, protozoa, fungi and small animals (invertebrates) thrive in it. Roots of plants pierce through the soil to tap water and nutrients. Terrestrial animals live on land. Aquatic plants, animals and microbes live in fresh water as well as in the sea. Some microbes live even in hot water vents under the sea. B. Biotic components i. Green Plants Prepare food through photosynthesis for all living organisms. ii. Animals Individuals of the same species occur in a particular type of habitat. They also live with other species. One species forms food for another. Micro-organisms and fungi decompose dead plants and animals releasing nutrients locked in bodies of dead organisms for reuse by the growing plants. Living organisms, therefore, need both abiotic and biotic components of the environment for survival. A delicately balanced relationship between living organisms and their environment is critically important for their survival. INTEXT QUESTIONS 1.4 1. Define environment. 2. Name its biotic components. 3. List its abiotic components. 4. In a sentence, mention why environmental degradation should be prevented. WHAT YOU HAVE LEARNT The universe consists of galaxies of stars. Stars are huge balls of hot glowing gases. Sun is also a star. Our solar system is composed of the sun and eight planets moving around it. Earth is one of the planets of our solar system. 10

Origin of Earth and Evoluation of the Environment The universe originated when there was a huge explosion that filled all the space with dust and gases. The ball of dust and gases spun fast which gave out great heat and the very hot centre broke off as the sun. It is believed that planets broke off from the periphery of this hot ball of dust and gases. The earth has three parts namely the core, the mantle and the outermost crust. The earth rotates in its orbit around the sun; and also rotates upon on its own axis. This rotation causes day and night cycle. The earth is the only planet in the solar system which can sustain life as it has water, atmosphere, suitable temperature and gets sufficient light from the sun. The age of the earth is 4 to 5 billion years and life first originated on earth 3.5 billion years ago as evidenced by the oldest fossils found till now. The atmosphere of primitive earth was very different hot and full of gases carbon-dioxide, water vapour, methane, ammonia and hydrogen but no oxygen. When earth cooled, water vapour condensed into liquid water and fell as rains. How the first cell came into existence is still unknown, but perhaps the single celled bacteria were among the earliest organisms. Through biological evolution millions of different kinds of organisms have evolved subsequently. All organisms depend on their environment for survival. All organisms live in close association with their environment. Environment is defined as the surroundings of an organism. The environment comprises of non living (abiotic) components like temperature, light, water, humidity etc. and living or biotic components such as other organisms sharing those surroundings. MODULE - 1 TERMINAL EXERCISE 1. Trace the origin of the earth. 2. Describe briefly the solar system to which the earth belongs. 3. State the big bang theory of origin of universe. 4. Why is earth able to sustain life while no other planet is known to have life? 5 Name the five kingdoms of living organisms. 6. Define environment. List the various components of the environment. 11

MODULE - 1 Environmental Science Senior Secondary Course ANSWER TO INTEXT QUESTIONS 1.1 1. 4.5 billion years 2. Star 3. Planets orbiting central star 4. Because earth completes one full rotation s on its axis in 24 hours 5. Blue 1.2 1. (i) Presence of water (ii) Presence of Air (iii) Comfortable range of temperature (iv) Buffering capacity 2. Sun 3. Oxygen is used in respiration to oxidize food for liberating energy. 1.3 1. Methane, ammonia, carbon dioxide and hydrogen 2. Bacteria 3. Because of photosynthesis 4. Monera, Protista, Fungi, Plantae and Animalia 1.4 1. Surroundings or condition in which an organism lives and operates. 2. Biotic- living organism of all kinds including microbes. 3. Abiotic light, humidity temperature, atmosphere and substratum 4. Because it threatens the survival of living organisms including humans. 12