Amanda Ackerman

 Key Points 

Types

1.1        Fossils can be divided into two categories, fossilized body parts and fossilized traces.  Fossilized body parts include bones, claws, teeth, skin, and eggs and even whole organisms or animals.  Fossilized traces are footprints, nests, teethmarks and droppings or anything that shows movement or behavior. Fossils can be remains of animals or plants.

¨       Standard(s): Science 2.1.3, 2.2.5 

1.2                There are different ways that fossils have been formed. Sometimes the organism leaves an impression in the mud that hardens and sometimes a fossil can be the whole animal or plant.

¨       Standard(s): Science 2.1.3, 2.2.5 

1.3        There are three types of rock that include sedimentary, igneous, and metamorphic.  The rock that we are most interested in is sedimentary because fossils are most commonly found buried and preserved in sedimentary rock.

¨       Standard(s): Science 2.1.1, 2.6.1, 2.6.2           

1.4        Fossils tell us things about the past.  Dinosaur fossils are extremely valuable because they are one of the only things left to study about dinosaurs.  It is really rare to find a whole dinosaur buried, usually just parts or traces are found. Putting all the pieces or parts together is like a puzzle and is very difficult because there are so many types of dinosaurs.

¨       Standard(s): Science 2.1.1, 2.5.6, 2.6.2 

1.5                Organisms can be classified as invertebrates or vertebrates. An invertebrate is an organism without a backbone like a worm. A vertebrate is an organism that has a backbone.

¨       Standard(s): Science 2.4.1        

Formation

2.1                Fossils can be formed several ways. Most fossils are actually casts or molds of animals or plants. One of the ways that a fossil can form is if the animal dies and either stays on the ground or sinks to the ocean floor.  The body begins to decay and is buried under layers of sediment such as mud or sand. These layers become rock.  The hard parts of the animal are replaced with minerals and these minerals form the fossil.  Usually fossils show hard parts of the animal or plants such as shell or bones. This is because the soft parts are destroyed quickly after an organism dies.

¨       Standard(s): Science 2.1.1, 2.6.2 

2.2               Mummification can occur in ice or amber.  Amber is a hardened form of tree sap.  Mummification means that a plant or animals (usually insects) are trapped in either ice or amber. This is a unique way to find a whole organism or plant preserved because it was trapped in either substance.

¨       Standard(s): Science 2.1.1, 2.1.6, 2.4.1 

2.3               Fossils are rock colored because they are rocks. A fossilized object is just a rocky model of an ancient object.  A fossil is composed of different materials then the original object was.  Fossils come in many colors and are made of many different kinds of minerals depending on what kind of rock is surrounding the fossil.

¨       Standard(s): Science 2.1.1, 2.3.3, 2.6.2

Location

3.1                A map has several parts that aid in using or reading a map. A compass rose is used to help with directions of north, south, east, and west. These are called cardinal directions. A map has a key or legend that has symbols to identify the type of kind of place is on the map. Sometimes these symbols are pictures.

¨       Standard(s): Social Studies 2.1.2, 2.3.1-2.3.5 

3.1a      Fossils are found in all parts of the world, from the United States to Greenland to Antarctica.  They can be found by drilling in the ocean floor or even on top of the highest mountains.  Fossils found in the ocean are known as marine fossils.

¨       Standard(s): Social Studies 2.1.2, 2.3.1-2.3.5 

3.1b      Fossils can be found in many places in Indiana.  For example, the Falls of the Ohio located in Clarksville on the Ohio River.  Also, Monroe County has lots of fossils.

¨       Standard(s): Social Studies 2.1.2, 2.3.1-2.3.5 

3.2       The best places to look for fossils are where fossils can come to the surface or top.  Such places include old rock quarries, ploughed fields where rocks are near the surface, road cuttings, and even the seaside. The seaside is an ideal place because fossils will be falling out of cliffs as a result of the waves hitting the cliffs. 

¨       Standard(s): Science 2.1.1, 2.1.6, 2.6.1 

3.3       There are fossils that can be found in Indiana.  Indiana has a lot of limestone, which is made of the remains of countless marine animals or shells of tiny animals.  It is also made of a mineral called calcium that is used to make bones and shells. Between 345-435 million years ago, much of Indiana was under water.  This helped form the limestone and is the reason why Indiana is the world’s leading producer of limestone. Bedford and Salem are known for having lots of limestone. Many buildings around Indiana and across the United States are made of limestone, including the Pentagon in Washington D.C.

¨       Standard(s): Science 2.1.1, 2.3.3 

3.4               Brachiopods are among the most common fossils in Indiana rocks.  They resemble clams, but are a different type of marine animal with two shells.  They are asymmetrical from a side view (one shell is larger that the other). Asymmetrical means that the shells are not identical or exactly the same. 

¨       Standard(s): Science 2.1.1, 2.1.6

3.5               Crinoids, which are only found in Indiana, are similar to starfishes and sea urchins.  They lived in fast running or flowing shallow water and their skeletons fell apart after they died.  Crinoids have a head and a stem that is either round or star-shaped.  Horn corals are individual corals shaped like a small cow’s horn.

¨       Standard(s): Science 2.1.1, 2.1.6 

3.6               Bryozoans are small, about the size of a pinhole.  However, they formed colonies. Trace fossils tell about the activities of a variety of soft-bodied animals like worms.  These animals had no hard parts to be fossilized and showed up as indentations or markings in the rock.

¨       Standard(s): Science 2.1.1, 2.1.6

Paleontologists

4.1                Paleontology is the study of fossils.  Paleontologists study these fossils and attempt to use them to study the history of the earth and living things.  Fossils can provide historical information on past climates and which can be used to understand the future.

¨       Standard(s): Social Studies 2.4.2, 2.4.7, 2.5.1 

4.2               Paleontology is one of the few fields of science left in which amateurs can and frequently do make important contributions.  An amateur is a person that is working for enjoyment or a hobby. Being a paleontologist requires a strong sense of patience to keep visiting sites, keep good notes, and  familiarize yourself with what is known about the fossils and the time period that is being studied.

¨       Standard(s): Social Studies 2.4.2, 2.4.7, 2.5.1 

4.3               People chose many different careers or jobs.  Every job is important.  Some people go to college to learn more about their career and specialize in areas of interest like teachers, school nurses, police officers, firefighters, and many others.  Some people are producers like farmers and some careers are to serve others like dentists or trash removers.

¨       Standard(s): Social Studies 2.4.2, 2.4.7, 2.5.1, 2.5.5 

4.3a      Most paleontologists go to college. Some work in museums while others are digging trying to discover new fossils. Before a paleontologist begins new digs or fieldwork, he or she studies the rock history or geology of the region to determine if it is likely that fossils are present. 

¨       Standard(s): Social Studies 2.4.2, 2.4.7, 2.5.1 

4.4               To record data, paleontologists draw sketches and even take pictures.  They also take detailed notes about what they found, including where the fossil was found. Usually each fossil is given an identifier, like a number, so that the data recorded from the site can be related to individual fossils. Paleontologists also record information about the rock type and the rock layers around the fossil if the layers can be seen.

¨       Standard(s): Science 2.1.3, 2.2.5, 2.3.3, 2.6.2 

4.5               Paleontologists classify or sort fossils by comparing their shape, size, color, texture, and by checking to see if it is similar to any other organisms.  This is very difficult and detailed work and they are constantly looking for an easier and more effective way to classify fossils.

¨       Standard(s): Science 2.1.1, 2.1.3, 2.3.3 

4.6               A paleontologist may need lots of equipment depending on the job. The typical tools that a paleontologist uses include: hammer, chisels, eye protection, hard hat, a notebook and pen, hand lens, camera, collecting bags, maps, and a compass.

¨       Standard(s): Science 2.1.1, 2.1.2  

Change Over Time

5.1                The fossil record contains evidence of how life has changed and evolved throughout the earth’s history. The fossil record also reveals how individual species evolved over time. It is possible to study such changes by comparing older fossils found lower in a sedimentary formation with the younger fossils found higher in the formation. The study of these sediments and geological time is known as stratigraphy. 

¨       Standard(s): Science 2.4.1 and Social Studies 2.3.4, 2.6.3 

5.2               Timelines are a way to organize important dates or events. They are a helpful tool or resource to use, especially if a large time span is being studied.

¨       Standard(s): Social Studies 2.1.5

5.2a      There are three distinct time periods that paleontologists study.  The Paleozoic Era was from 565-225 million years ago.  This early period is known as the age of invertebrates. Fossils from this time are simple and usually microscopic or very small.  Jellyfish and worms appear in fossils from this time period as well. Most organisms from this time lived in the water.

¨       Standard(s): Science 2.4.1 and Social Studies 2.1.5 

5.2b     The Mesozoic Era occurred between 225-65 million years ago. This middle period is termed the age of the reptiles. Organisms began migrating or moving onto land and vertebrates, which are organisms with a backbone, became more common. This is when dinosaurs roamed the earth. After the dinosaurs became extinct, mammals and flowering plants started to live in the habitats or areas left by the dinosaurs.

¨       Standard(s): Science 2.4.1 and Social Studies 2.1.5 

5.2c      The Cenozoic Era is from 65 million years ago to the present.  It is known as the age of mammals and is the current time period.

¨       Standard(s): Science 2.4.1 and Social Studies 2.1.5 

5.3               Paleontologists can also gather information about the climates of prehistoric times by studying fossils and sediments.  This field is known as paleoclimatology.  In general, animal and plant life is more active in warm, humid climates and less active in dry climates. 

¨       Standard(s): Social Studies 2.3.1, 2.6.3