This is the self-learning module for Earth and Life Science, Quarter 1, Module 14: Geologic Timeline, for Senior High School learners. It was produced by DepEd Region IV-A CALABARZON under the Alternative Delivery Mode (First Edition, 2021). After working through it, learners can explain what fossils are, how fossils helped scientists build the geologic time scale, and how to use that time scale to trace Earth’s history.
On this page 6 sections
What learners will learn
The module has one lesson, Lesson 1: Geologic Timeline. By the end of it, learners are expected to:
- Describe how the Earth’s history can be interpreted from the geologic time scale.
- Define fossils and their types.
- Determine the guide fossils used to define and identify subdivisions of the geologic time scale.
- Track the Earth’s history using the geologic time scale.
- Identify the different divisions in the geologic time scale.
Fossils: the clues to Earth’s past
Fossils are the remains or evidence of prehistoric plants and animals that have turned to stone. The module introduces these key terms:
- Fossilization: the process that turns the remains of ancient living things into rock.
- Body fossils: actual parts of plants and animals turned to stone, such as bones, shells, and leaves.
- Trace fossils: signs that a plant or animal once lived in an area, such as footprints or coprolite.
- Coprolite: fossilized dinosaur dung.
- Paleontologist: a scientist who studies fossils and ancient life.
- Sedimentary rock: rock made of layers of tightly packed sand and clay. Sandstone is one type. Most fossils are found in sedimentary rock.
- Mineralization: converting into, or filling with, a mineral substance.
In the reading “The Story of Fossils” by Patti Hutchison, learners find out that scientists arrange fossils by age, which is called the fossil record. Fossils have taught scientists how and when rock layers formed, which life forms came and went, and even what Earth’s climate was like long ago.
The geologic time scale
The geologic time scale is the “calendar” of Earth’s history. It divides all time since the end of Earth’s formative period (nearly 4 billion years ago) into units. From longest to shortest, these are:
- Eons
- Eras
- Periods
- Epochs
Fossils were used as markers to build this scale. Most eon and era names end in “zoic” because those time periods were recognized by the animal life present at the time. Eras are defined by major changes in the fossils found in sedimentary rock layers. Rocks from the Proterozoic Eon hold fossils of simple organisms such as bacteria, algae, and wormlike animals. Rocks from the Phanerozoic Eon hold fossils of dinosaurs, mammals, and trees. The scale is usually drawn as a chart with the oldest time unit at the bottom and the youngest at the top.
The module’s chart lists these eras, periods, and events:
| Era | Period | Key events |
|---|---|---|
| Cenozoic | Quaternary | Evolution of humans |
| Cenozoic | Tertiary | Mammals diversify |
| Mesozoic | Cretaceous | Extinction of dinosaurs; first primates; first flowering plants |
| Mesozoic | Jurassic | First birds; dinosaurs diversify |
| Mesozoic | Triassic | First mammals; first dinosaurs |
| Paleozoic | Permian | Major extinctions; reptiles diversify |
| Paleozoic | Carboniferous (Pennsylvanian and Mississippian) | First reptiles; scale trees; seed ferns |
| Paleozoic | Devonian | First amphibians; jawed fishes diversify |
| Paleozoic | Silurian | First vascular land plants |
| Paleozoic | Ordovician | Sudden diversification of metazoan families |
| Paleozoic | Cambrian | First fishes; first chordates |
| Late Proterozoic | First skeletal elements; first soft-bodied metazoans; first animal traces |
Guide fossils in the module
The module describes five fossil examples:
- Branching tabulate coral (Devonian): a colonial marine animal; each individual animal is called a polyp.
- Trilobite (Devonian, phylum Arthropod): marine arthropods with exoskeletons made of chitin, related to crabs, spiders, and insects. They went extinct by 250 million years ago.
- Crinoid (Devonian, phylum Echinoderm): its name means “lily”; related to starfish, sea urchins, and sea cucumbers. Its stem pieces are its most common fossils.
- Gastropod (Cretaceous, phylum Mollusk): coiled-shell animals related to snails, slugs, and whelks.
- Fossil clam (Cretaceous, class Bivalve): has two symmetrical shells that are mirror images of each other; related to oysters, scallops, and mussels.
How to use this module
The module follows the usual self-learning module parts:
- What I Know: a 15-item multiple-choice pretest.
- What’s In: vocabulary review with a fill-in-the-blank story (Activity 1), a word search (Activity 2), and questions on the geologic time scale chart (Activity 3).
- What’s New: the reading “The Story of Fossils” with guide questions (Activity 4).
- What Is It: true or false statements (Activity 5).
- What’s More: placing events in their era and period (Activity 6) and a crossword puzzle.
- What I Have Learned: fill-in-the-blank review of the lesson.
- What I Can Do: choose one of the fossil examples and draw its structure.
- Assessment: a 15-item multiple-choice post-test, followed by an additional activity on whether global temperature and carbon dioxide levels have stayed the same throughout Earth’s history.
Learners: Write all answers on a separate sheet of paper and keep the module free of marks. Check your work with the answer key at the end honestly, and ask your teacher if any task is unclear.
Parents: Help your child follow the parts in order and make sure the pretest and post-test are answered before looking at the answer key.
Teachers: The answer key covers the pretest, the post-test, and Activities 1, 5, 6, and the crossword. Activities 2, 3, and 4 are marked as open-ended, so plan to check those yourself.
Frequently asked questions
What grade level is this Earth and Life Science module for?
The module is labeled for Senior High School. It is Quarter 1, Module 14 of Earth and Life Science.
Does the module have an answer key?
Yes. It includes answers for the pretest, the post-test, Activities 1, 5, and 6, and the crossword puzzle. Activities 2, 3, and 4 are marked as answers that may vary.
What are the divisions of the geologic time scale?
From longest to shortest, the geologic time scale is divided into eons, eras, periods, and epochs. The chart is read with the oldest time at the bottom and the youngest at the top.
Why do most era names end in zoic?
According to the module, most eon and era names end in zoic because those time periods were recognized by the animal life present at the time.
What is the difference between body fossils and trace fossils?
Body fossils are actual parts of plants and animals turned to stone, such as bones, shells, and leaves. Trace fossils are signs that an organism lived in an area, such as footprints or coprolite.
Full text of the module
The text below is a transcription of the PDF above, as printed.
Earth and Life Science Quarter 1 – Module 14: Geologic Timeline
Senior High School
[illustration: students studying outdoors under a tree, a teacher helping students at a desk, a child working by a lamp, and a globe]
CO_Q1_ELS SHS Module 14
Earth and Life Science Alternative Delivery Mode Quarter 1 – Module 14: Geologic Timeline First Edition, 2021
Republic Act 8293, Section 176 states that: No copyright shall subsist in any work of the Government of the Philippines. However, prior approval of the government agency or office wherein the work is created shall be necessary for exploitation of such work for profit. Such agency or office may, among other things, impose as a condition the payment of royalties.
Borrowed materials (i.e., songs, stories, poems, pictures, photos, brand names, trademarks, etc.) included in this module are owned by their respective copyright holders. Every effort has been exerted to locate and seek permission to use these materials from their respective copyright owners. The publisher and authors do not represent nor claim ownership over them.
Published by the Department of Education
Secretary: Leonor Magtolis Briones
Undersecretary: Diosdado M. San Antonio
Development Team of the Module
Writer: Christian Jay D. Salazar
Editors: Melanie I. Samudio
Jocelyn M. Manset
Reviewers: Jason Ricaforte, Angelica Beriña, Princess Paolah L. De Guzman, Marissa C. Betchaida, Louie L. Alvarez, Gregorio M. De Chavez, Jr., Jocelyn M. Manset, Mario B. Maramot, Elaine T. Balaogan, Job S. Zape Jr., Jonathan V. Mayo
Illustrator: Ednelinda Robles, Lovely Joy La Rosa, Charles Erick A. Jusay, Sandro Carlo B. Tablizo
Layout Artist: Elizalde L. Piol, Anselma M. Ebero, Jocelyn M. Manset
Management Team: Francis Cesar B. Bringas
Job S. Zape, Jr.
Ramonito Elumbaring
Reicon C. Condes
Elaine T. Balaogan
Fe M. Ong-ongowan
Merthel M. Evardome
Nadine C. Celindro
Nicolas M. Burgos
Mario B. Maramot
Fe M. Ong-ongowan
Rosalinda A. Mendoza
Printed in the Philippines by _______________________
Department of Education – Region IV-A CALABARZON
Office Address: Gate 2 Karangalan Village, Barangay San Isidro, Cainta, Rizal 1800
Telefax: 02-8682-5773/8684-4914/8647-7487
E-mail Address: region4a@deped.gov.ph
Earth and Life Science Quarter 1 – Module 14: Geologic Timeline
Senior High School
Introductory Message
This Self-Learning Module (SLM) is prepared so that you, our dear learners, can continue your studies and learn while at home. Activities, questions, directions, exercises, and discussions are carefully stated for you to understand each lesson.
Each SLM is composed of different parts. Each part shall guide you step-by-step as you discover and understand the lesson prepared for you.
Pre-tests are provided to measure your prior knowledge on lessons in each SLM. This will tell you if you need to proceed on completing this module or if you need to ask your facilitator or your teacher’s assistance for better understanding of the lesson. At the end of each module, you need to answer the post-test to self-check your learning. Answer keys are provided for each activity and test. We trust that you will be honest in using these.
In addition to the material in the main text, Notes to the Teacher are also provided to our facilitators and parents for strategies and reminders on how they can best help you on your home-based learning.
Please use this module with care. Do not put unnecessary marks on any part of this SLM. Use a separate sheet of paper in answering the exercises and tests. And read the instructions carefully before performing each task.
If you have any questions in using this SLM or any difficulty in answering the tasks in this module, do not hesitate to consult your teacher or facilitator.
Thank you.
What I Need to Know
This module was designed and written with you in mind. It is here to help you master the nature of Biology. The scope of this module permits it to be used in many different learning situations. The language used recognizes the diverse vocabulary level of students. The lessons are arranged to follow the standard sequence of the course. But the order in which you read them can be changed to correspond with the textbook you are now using.
The module covers:
- Lesson 1 – Geologic Timeline
After going through this module, you are expected to:
- Describe how the Earth’s history can be interpreted from the geologic time scale.
- Define fossils and its type.
- Determine the guide fossils that are used to define and identify subdivision of the geologic time scale.
- Track the Earth’s history using the geologic time scale.
- Identify the different divisions in the geologic time scale.
What I Know
Choose the letter of the best answer. Write the chosen letter on a separate sheet of paper.
Which of the following does NOT belong to Paleozoic Era?
- A. Cambrian
- B. Devonian
- C. Jurassic
- D. Ordovician
What do you call the remains or evidence used as markers when building up the geologic time scale?
- A. fossil
- B. minerals
- C. piles of rock
- D. sandstone
Why do most of the eons and eras end in “zoic”?
- A. because these time periods were recognized by the plants present at that time
- B. because these time periods were recognized by the animal life present at that time
- C. A and B
- D. none of the above
In what type of rocks are fossils made up of?
- A. igneous rock
- B. metamorphic rock
- C. sedimentary rock
- D. all of the above
What do you call the person who studies fossils and ancient life?
- A. anthropologist
- B. archeologist
- C. biologist
- D. paleontologist
What do you call the process by which the remains of ancient living things are turned into rock?
- A. fertilization
- B. fossilization
- C. fragmentation
- D. metamorphosis
How were the scientists able to arrange the fossils they gathered?
- A. They were able to arrange the fossils according to age.
- B. They were able to arrange the fossils according to structure.
- C. They were able to arrange the fossils according to chemical content.
- D. They were able to arrange the fossils according to place of discovery.
In what era did the rocks with fossils of animals and plants such as dinosaurs, mammals, and trees form?
- A. Cenozoic Era
- B. Mesozoic Era
- C. Paleozoic Era
- D. Phanerozoic Era
In what era did the first skeletal elements, soft-bodies metazoans, and animal traces exist?
- A. Cenozoic Era
- B. Late Proterozoic
- C. Mesozoic Era
- D. Paleozoic Era
What period the first mammals and dinosaurs existed?
- A. Cretaceous
- B. Jurassic
- C. Permian
- D. Triassic
- In Paleozoic Era, in what period did the first vascular land planet exist?
- A. Cambrian
- B. Devonian
- C. Ordovician
- D. Silurian
- These marine animals lived inside their shells, taking up the whole inside of the long shell.
- A. echinoderms
- B. gastropods
- C. mollusks
- D. sea arthropods
- In what phylum do crinoids belong?
- A. echinoderms
- B. arthropods
- C. gastropods
- D. mollusks
- What do you call the marine arthropods that were made of chitin, like some insects and other organisms like lobsters?
- A. crinoids
- B. fossil clam
- C. gastropods
- D. trilobites
- Which of the following marine animals are bivalves with two symmetrical shells – the shells are mirror images of each other?
- A. crinoids
- B. fossil clam
- C. gastropods
- D. trilobites
Lesson 1 Geologic Timeline
Fossils are the remains or evidence of prehistoric plants and animals that have fossilized. Fossils were used as markers when building up the geologic time scale. The names of most of the eons and eras end in “zoic”, because these time periods were recognized by the animal life present at the time. Rocks formed during the Proterozoic Eon have fossil evidence of simple organisms, such as bacteria, algae, and wormlike animals. In the Phanerozoic Eon, the rocks formed have fossils of animals and plants such as dinosaurs, mammals, and trees.
And with that, geologists have developed the geological time scale, which divides the Earth’s history into eons that are subdivided into eras, which are further divided into periods and then into epochs. The geologic time scale is the “calendar” for events in Earth’s history. It subdivides all time since the end of the Earth’s formative period as a planet (nearly 4 billion years ago) into named units of abstract time: in descending order of duration, which are eons, eras, periods, and epochs.
The geologic time scale provides a system of chronologic measurement relating stratigraphy to time that is used by geologists, paleontologists, and other Earth scientists to describe the timing and relationships between events that have occurred during the history of the Earth. The detailed studies made of rocks throughout the world have allowed geologists to correlate rock units globally, and break them into time units. The result is the Geologic Time Scale, usually presented in a chart like form with the oldest event and time unit at the bottom and the youngest at the top.
What’s In
Activity 1
Review the vocabulary words and complete the activity on the other side of this worksheet.
- Fossils – remains of ancient life that have been turned to stone
- Body Fossils – actual parts of plants and animals that have been turned to stone (i.e. bone, shells, leaves)
- Coprolite – fossilized dinosaur dung (scat)
- Fossilization – process by which the remains of ancient living things are turned to rock
- Paleontologist – a scientist who studies fossils and ancient life
- Sedimentary Rock – rock made of layers of tightly packed sand and clay
[transcriber’s note: the heading for the activity that these vocabulary items and fill-in-the-blank passage belong to is not on this page]
- Sandstone – a type of sedimentary rock that is made of sand
- Trace Fossil – a fossilized sign that a plant or animal once lived in an area (i.e. footprints, coprolite)
- Porous – full of tiny holes that water, air, and light can pass through
- Mineralization – to convert into a mineral substance; to fill with a mineral substance
Instructions: Fill in the blanks, using vocabulary words.
Jay, a famous p _____ _____ _____ _____ _____ _____ _____ _____ _____ _____ _____ t, was hiking in the Cordillera mountains searching for f _____ _____ _____ _____ _____, which are remains of ancient life that have turned to stone. All of a sudden, the ground shook beneath him. Jay ran over a hill and saw that there had been a huge landslide. He went over to look at the piles of rocks and saw layers of s _____ _____ s _____ _____ _____ _____, a type of sedimentary rock. Fossils are found in sandstone, so Jay was excited to search through the rocks! Just as he began to dig, he found fossilized bones. The bones had turned to stone through a process called _____ _____ s s _____ _____ _____ _____ _____ _____ _____ _____. Jay saw that the fossils belonged to an Apatosaurus. These bones are examples of b _____ _____ _____ _____ _____ _____ i l _____, which are fossilized parts of plants and animals. Jay hiked further up the mountain and found fossilized dinosaur dung, called c _____ _____ _____ _____ _____ _____ _____ _____. He also found a huge footprint, which is an example of a t _____ _____ _____ f _____ _____ _____ _____ _____. Jay carefully removed the fossils from the rocks and donated them to a museum.
Activity 2: Find Me
Directions. Encircle the 8 words listed below. Words may appear straight across, back-word straight across, up, and down.
COPROLITE PALEONTOLOGIST FOSSILS MINERALIZATION SEDIMENTARY SANDSTONE FOSSILIZATION POROUS
| L | N | O | I | T | A | Z | I | L | A | R | E | N | I | M |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| S | T | S | I | G | O | L | O | T | N | O | E | L | A | P |
| E | K | B | K | S | D | Z | U | I | L | I | H | K | M | F |
| D | C | L | T | J | Q | L | W | O | G | B | M | I | N | O |
| I | Y | E | I | N | M | P | Q | R | K | J | P | A | T | S |
| M | F | P | D | L | S | A | N | D | S | T | O | N | E | S |
| E | R | O | I | M | I | X | Y | U | E | R | J | P | J | I |
| N | D | K | S | Z | R | F | Z | T | J | A | X | T | Q | L |
| T | E | B | P | S | M | E | I | L | W | B | P | I | Y | I |
| A | Q | V | Y | E | I | L | X | V | Y | O | F | Q | V | Z |
| R | Z | I | K | F | O | L | P | M | R | A | M | R | G | A |
| Y | C | V | W | R | H | R | Y | O | K | V | F | I | L | T |
| M | L | S | P | Q | U | N | U | P | I | P | W | E | H | I |
| T | V | O | F | M | B | S | A | R | T | F | N | F | B | O |
| N | C | G | Z | U | R | N | L | O | N | I | H | O | A | N |
Activity 3: Let’s Trace
Look and analyze at the illustration below and answer the question listed below.
[chart: geologic time scale; GEOLOGIC TIME SCALE, 650 MILLION YEARS AGO TO THE PRESENT]
Axis label: Million of years ago. Printed axis ticks: 0, 1.8, 50, 100, 150, 200, 250, 300, 350, 400, 450, 500, 550, 600, 650. Values are not labeled on the chart for individual rows.
| Era | Period | Events |
|---|---|---|
| Cenozoic | Quaternary | evolution of humans |
| Cenozoic | Tertiary | mammals diversify |
| Mesozoic | Cretaceous | extinction of dinosaurs; first primates; first flowering plants |
| Mesozoic | Jurassic | first birds; dinosaurs diversify |
| Mesozoic | Triassic | first mammals; first dinosaurs |
| Palezoic | Permian | major extinctions; reptiles diversify |
| Palezoic | Carboniferous: Pennsylvanian | first reptiles; scake trees; seed ferns [transcriber’s note: this events cell spans the Pennsylvanian and Mississippian rows] |
| Palezoic | Carboniferous: Mississippian | |
| Palezoic | Devonian | first amphibians; jawed fishes diversify |
| Palezoic | Silurian | first vascular land plants |
| Palezoic | Ordovician | sudden diversification of metazoan families |
| Palezoic | Cambrian | first fishes; first chordates |
| Late Proterozoic | first skeletal elements; first soft-bodied metazoans; first animal traces |
- For how long has there been life on Earth?
- For what percentage of time has life existed on Earth (round to the nearest whole number)?
- For about how many years of geological time have humans existed on Earth?
- For about how many years of geological time have the dinosaurs existed on Earth?
- Did dinosaurs exist at the same time as humans?
- How do scientists determine when an era begins and when it ends?
- What is the purpose of making a geological timeline?
Notes to the Teacher
This module will help you understand the concepts about animal reproduction. All parts are comprised of activities. Be guided with the instructions on how you will answer each. Expectedly, you will meet the target at the end of the module.
What’s New
The Story of Fossils by Patti Hutchison
Imagine you are hiking in the woods. As you walk up a steep hill, you find a fossil. It is a mold of many tiny seashells. What would seashells be doing in the middle of the woods?
Most fossils are found in sedimentary rocks. These rocks form on the surface of the earth. They record the processes that have happened on the surface, including life. Scientists are able to arrange fossils according to age. This is called the fossil record. By studying the fossil record, scientists have found that the earth and its life forms have gone through many changes in the past.
Fossils have taught us how and when rock layers have formed. They have also helped scientists learn about life forms that have come and gone. Fossils have even taught us about the climate of the earth long ago.
The Geologic Time Scale is divided into huge blocks of time called eras. Eras are defined by major changes in the fossils found in the sedimentary rock layers that were formed during those time spans.
Activity 4
Directions: Read the story entitled “The Story of Fossil” by Patti Hutchison. Answer the guide questions stated below.
- In what type of rocks are FOSSILS made of?
- How do scientists arrange discovered fossils?
- How did fossils help and teach scientist about the history of the earth?
- Aside from geological aspect, what other aspects can be predicted by guide fossils? How? (climatic, organismic etc.)
What is It
Activity 5
Read and analyze the statements below. Write T if the statement is TRUE and F if the statement is FALSE.
_______ 1. Scientists determine when an era begins and when it ends through geological timeline.
_______ 2. Dinosaurs exist at the same time as humans.
_______ 3. The purpose of making a geological timeline is to identify age of organism through its fossils.
________ 4. Quaternary period of geological time has humans evolved on Earth.
_______ 5. Triassic Period of geological time have the dinosaurs existed on Earth.
What’s More
Activity 6
Directions: Write the division and period of the listed organism below. Refer to geological time scale.
| Organism | Era | Period |
|---|---|---|
| 1. first vascular land plants | ____________ | ____________ |
| 2. jawed fish diversity | ____________ | ____________ |
| 3. evolution of humans | ____________ | ____________ |
| 4. first chordates | ____________ | ____________ |
| 5. mammals diversify | ____________ | ____________ |
| 6. first primates | ____________ | ____________ |
| 7. dinosaurs’ diversity | ____________ | ____________ |
| 8. major extinctions of reptiles’ diversity | ____________ | ____________ |
| 9. sudden diversification of metazoan families | ____________ | ____________ |
| 10. first flowering plants | ____________ | ____________ |
Activity 7: Crossword Puzzle
Directions. Complete the crossword by filling in the word that describes each clue.
[illustration: blank crossword grid with clue numbers 1 to 8 printed in some of the cells]
Across:
- a term used with two symmetrical shells – mirror images of each other.
- the term “crinoid” means
- type of proteins that make up the skin, hair and nails.
- multicellular organisms in the sea that often live in colonies and served as habitat of marine organisms
Down:
- exoskeletons are made up of this material
- common slow-moving gastropod lived inside their shells
- phylum where starfish and sea urchins belong
- individuality of coral is called _____.
What I Have Learned
Fill in the blanks. Read and analyze the statements below. Write the word that will complete the sentence/paragraph.
- _____________________ are the remains or evidence of prehistoric plants and animals that have fossilized.
- Fossils were used as markers when building up the geologic time scale. The names of most of the eons and eras end in “zoic” because these time periods were recognized by the _____________________ present at the time.
- The geologic time scale is the “calendar” for events in Earth’s history. It subdivides all time since the end of the Earth’s formative period as a planet (nearly 4 billion years ago) into named units of abstract time: in descending order of duration, which are _________, __________, _________ and ___________.
- The _____________________ provides a system of chronologic measurement relating stratigraphy to time that is used by geologists, paleontologists and other Earth scientists to describe the timing and relationships between events that have occurred during the history of the Earth.
- The Geologic Time Scale is divided into huge blocks of time called eras. Eras are defined by major changes in the fossils found in the _____________________ rock layers that were formed during those time spans.
What I Can Do
Activity 7
There are tables of fossils presented below. In the first box, choose an example and draw its physical structure. Second box and third box are references that serve as your guide to choose what organism you prefer to draw. Check the example. Good luck!
Example:
| [illustration: branching tabulate coral fossil] | Branching Tabulate Coral Age: Devonian (approximately 416 to 359 million years ago) Class: Anthozoa Modern Relatives: Corals still exists today. | Branching Tabulate Coral is a marine animal. Corals are multicellular organisms that often live in colonies. The individual animal is called a polyp. There are many different species of coral, with different forms, shapes, and sizes. |
| 1. | TRILOBITE Age: Devonian (approximately 416 to 359 million year ago) Phylum: Arthropod Modern Relatives: Crabs, Spiders and insects | Trilobites were marine arthropods. The first trilobites show up in the fossil record dating back to about 525 million years ago. There were many different types of trilobites, ranging in size from 1mm to 72mm (28 inches long!) Trilobite species went extinct by 250 million years ago. Trilobite fossils are formed from the exoskeletons. These were made of chitin, like some insects and others organisms like lobsters. They split apart and shed their shell as they grow, just like lobsters do. |
| 2. | Crinoid Age: Devonian (approximately 416 to 359 million years ago) Phylum: Echinoderm Modern Relatives: Starfish, sea urchins and sea cucumbers | Crinoids were marine animals. Its name means “Lily”. It is in the same phylum (Echinoderm) as starfish and sea urchins. Crinoids ate by filtering food out of the water with it arms. Its mouth and anus were next to each other in the calyx. It “rooted” in place with a holdfast. When crinoids die, their stems quickly break apart. The most common fossils of crinoids are the stem which is sometimes broken into little “cheerio” like pieces. |
| 3. | Gastropod Age: Cretaceous (Approximately 146 to 65 million years ago) Phylum: Mollusk Modern Relatives: Snails, Slugs and Whelks | Gastropods were marine animals. There were many different species of gastropods. All had coiled shells, but some were tightly coiled while some were loosely coiled. They had many different shapes and surface texture. The animals lived inside their shells, taking up the whole inside of the long shell. They could retract into their shells, covering the opening with their foot. |
| 4. | Fossil Clam Age: Cretaceous (approximately 146 to 65 million years ago) Class: Bivalve Modern Relatives: Oysters, Scallops and Mussels | Fossil clams are marine animals. Clams are bivalves, with two symmetrical shells – the shells are mirror images of each other. Fossil clams range in size from a few millimeters to up to 2 meters (about 6 feet) in diameter. Clams lived inside their shells and had a muscular foot they used to borrow and move around. They lived in colonies on the ocean floor. Some clams had smooth shells while some were rough. |
Assessment
Multiple Choice. Choose the letter of the best answer. Write the chosen letter on a separate sheet of paper.
- Why do most of the eons and eras end in “zoic”?
- A. because these time periods were recognized by the animal life present at that time
- B. because these time periods were recognized by the plants present at that time
- C. A and B
- D. none of the above
- Which of the following marine animals are bivalves with two symmetrical shells – the shells are mirror images of each other?
- A. crinoids
- B. fossil clam
- C. gastropods
- D. trilobites
- How were the scientists able to arrange the fossils they gathered?
- A. They were able to arrange the fossils according to age.
- B. They were able to arrange the fossils according to structure.
- C. They were able to arrange the fossils according to chemical content.
- D. They were able to arrange the fossils according to place of discovery.
- What do you call the marine arthropods that were made of chitin, like some insects and other organisms like lobsters?
- A. crinoids
- B. fossil clam
- C. gastropods
- D. trilobites
- What do you call the process by which the remains of ancient living things are turned into rock?
- A. fertilization
- B. fossilization
- C. fragmentation
- D. metamorphosis
- In what phylum do crinoids belong?
- A. arthropods
- B. echinoderms
- C. gastropods
- D. mollusks
- What do you call the person who studies fossils and ancient life?
- A. anthropologist
- B. archeologist
- C. biologist
- D. paleontologist
- Which of the following marine animals lived inside their shells, taking up the whole inside of the long shell?
- A. echinoderms
- B. gastropods
- C. mollusks
- D. sea arthropods
- In what type of rocks are fossils made of?
- A. igneous rock
- B. metamorphic rock
- C. sedimentary rock
- D. all of the above
10.In Paleozoic Era, in what period did the first vascular land planet exist?
- A. Cambrian
- B. Devonian
- C. Ordovician
- D. Silurian
11.In what period the first mammals and dinosaurs existed?
- A. Cretaceous
- B. Jurassic
- C. Permian
- D. Triassic
12.What do you call the remains or evidence used as markers when building up the geologic time scale?
- A. fossil
- B. minerals
- C. piles of rock
- D. sandstone
13.In what era did the first skeletal elements, soft-bodies metazoans, and animal traces exist?
A. Cenozoic Era
B. Late Proterozoic
C. Mesozoic Era
D. Paleozoic Era
14.Which of the following does NOT belong to Paleozoic Era?
- A. Cambrian
- B. Devonian
- C. Jurassic
- D. Silurian
15.In what era did the rocks with fossils of animals and plants such as dinosaurs, mammals and trees form?
- A. Cenozoic Era
- B. Mesozoic Era
- C. Paleozoic Era
- D. Phanerozoic Era
Additional Activities
Do you think that the average annual global temperature and carbon dioxide levels have been consistent throughout the history of earth? Justify your answer.
Answer Key
[transcriber’s note: this page is printed rotated 180 degrees; the sections are transcribed in their upright reading order]
Assessment
- A 1.
- B 2.
- A 3.
- D 4.
- B 5.
- B 6.
- D 7.
- B 8.
- C 9.
- D 10.
- D 11.
- A 12.
- B 13.
- C 14.
- D 15.
What I Know
- C 1.
- A 2.
- B 3.
- C 4.
- D 5.
- B 6.
- A 7.
- D 8.
- B 9.
- D 10.
- D 11.
- B 12.
- A 13.
- D 14.
- B 15.
What’s in
Activity 1
- Paleontologist
- Fossils
- Sandstone
- Fossilization
- Body fossils
- Coprolite
- Trace fossil
Activity 2
- Answer may vary according to student’s perception
What’s New
[transcriber’s note: in the printed key, the “What’s New” label and the Activity 4 entry sit in the same box as the Activity 3 entry, and the order of these three entries is taken from the upright layout]
Activity 3
Answer may vary according to student’s perception
Activity 4
Answer may vary according to student’s perception
What’s It
Activity 5
- T 1.
- F 2.
- T 3.
- T 4.
- F 5.
What’s More
Activity 6
- Silurian – Paleozoic 1.
- Devonian – Paleozoic 2.
- Quaternary – Cenozoic 3.
- Cambrian – Paleozoic 4.
- Tertiary – Cenozoic 5.
- Cretaceous – Mesozoic 6.
- Jurassic – Mesozoic 7.
- Permian – Paleozoic 8.
- Ordovician – Paleozoic 9.
- Cretaceous – Mesozoic 10.
Activity 7
Across 2. Bivalves 3. Lily 5. Keratin 7. Coral
Down
- Chitin
- Snails
- Echinoderm
- Polyp
References
Chambers, John E. (July 2004). “Planetary accretion in the inner Solar System” (PDF). Earth and Planetary Science Letters. 223 (3–4): 241–252. Bibcode:2004E&PSL.223..241C. doi:10.1016/j.epsl.2004.04.031.
Deconto, Robert M.; Pollard, David (2003). “Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2”. Nature. 421 (6920): 245–249. Bibcode:2003Natur.421..245D. doi:10.1038/nature01290. PMID 12529638.
Ogg, J.G.; Ogg, G.; Gradstein, F.M. (2016). A Concise Geologic Time Scale: 2016. Elsevier. p. 20. ISBN 978-0-444-63771-0. Ogg (eds.). The geologic time scale 2012 (1st ed.). Amsterdam: Elsevier. pp. 359–365. doi:10.1016/B978-0-444-59425-9.00016-0. ISBN 978-0-44-459425-9.
Claire; Macchiarelli, Roberto; et al. (2014). “The 2.1 Ga Old Francevillian Biota: Biogenicity, Taphonomy and Biodiversity”. PLoS ONE. 9 (6): e99438. Bibcode:2014PLoSO…999438E. doi:10.1371/journal.pone.0099438. PMC 4070892. PMID 24963687
Van Kranendonk, Martin J. (2012). “16: A Chronostratigraphic Division of the Precambrian: Possibilities and Challenges“. In Felix M. Gradstein; James G. Ogg; Mark D. Schmitz; abi M.
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