“Today we’re going to use fossils and the geologic time scale as geologic tools to help us determine the ages of rock units.”
Geologic time scale. “The Earth is about 4.5 billion years old. So, when we consider Earth time, we are thinking in huge time measurement units millions and billions of years long. Naturalists before 1800 used relationships of rock layers (oldest to youngest, bottom to top) to create a relative time scale for the Earth.” Facilitate a short class discussion to differentiate between relative (older, younger, same age) and absolute (number of years) time, summarizing the information in graphic organizer form (Venn diagram, flow chart) on the board. In the 1900s, time measurement techniques based on the radioactive decay of atoms were developed. It was not until then that Earth scientists began to assign absolute ages to prehistoric geologic events. “Around 1800, naturalists began to use fossils in the rock layers to determine Earth’s time scale instead. How do you think these scientists used fossils to help figure out the age of rock units?” Facilitate a class discussion of student ideas, posting summaries on the board.
Fossil Succession and the Geologic Time Scale. Distribute the Time Scale, Succession, and Fossil worksheet (S-7-2-3_Time Scale, Succession, and Fossil Worksheet and KEY.doc). “Scientists use three basic rules when constructing the geologic time scale from fossil evidence.
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Rule 1: Fossils are the preserved remains or traces of organisms that were once alive.
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Rule 2: Most fossils are the preserved remains or traces of extinct organisms.
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Rule 3: Life on Earth has changed, so there are different fossils in rocks of different ages. So, if we find the same kinds of fossils in different rocks, the rocks are of the same age no matter where we find them in the world.”
Allow students time to record their answers to question 1.
Group students and pass out a copy of the geologic time scale with absolute age dates (S-7-2-3_Geologic Time Scale.doc) or use http://pubs.usgs.gov/gip/fossils/numeric.html. Allow group members a brief time to discuss the time scale among themselves. “What kind of information is represented in the time scale?”
Facilitate a short discussion of questions 2 and 3 on the worksheet. For example, for question 2: “The geologic time scale is divided into long intervals of time called eons, which are in turn divided into shorter intervals of time called eras, which are in turn divided into even shorter intervals of time called periods. The time units are arranged from youngest at the top to oldest at the bottom of the scale.” For question 3, “The ages, in millions of years from the present, refer to the age of the boundaries between the periods. Note that these ages were determined using radioactive decay of atoms.” It is not necessary to analyze the time scale in great detail. Students just need to understand that it is a time measurement scale for Earth history.
Now pass out the Fossil Succession chart (S-7-2-3_Fossil Succession Chart.doc) or use http://pubs.usgs.gov/gip/fossils/succession.html. “What does the chart show us?” Facilitate a short class discussion about the general interpretation of the chart for question 4 on the worksheet: “The chart shows us change in life over time (fossil succession) correlated with the geologic periods noted on the left. As we go back in geologic time, through the fossil record, there was a time in Earth’s history when there were no humans, no birds, no mammals, and so on.”
Using Fossils to Relatively Age-Date Rock Layers. Distribute the Index Fossil chart (S-7-2-3_Index Fossil Chart.doc) or use http://pubs.usgs.gov/gip/geotime/fossils.html. “Now let’s see how fossils can help us determine how old a rock unit is. For example, we’re studying a rock unit that contains fossils of the trilobite Bathyurus extans. During what geologic time period did this trilobite live?” The Ordovician Period. “So, how old would the rock unit that contains this fossil be?”Ordovician in age as well because it contains the fossils. Provide further practice using the chart until students understand how to use the chart.
Using Fossils to Sequence Rock Layers by Relative Geologic Age. “How might we use fossils to help us sequence fossiliferous rock layers around the world according to relative geologic age?” The fossils can tell us if a rock unit is older, younger, or the same age as another rock unit. “Suppose we are studying widely separated fossiliferous rock layers and we want to put them in order of relative geologic age from oldest to youngest. Rock Unit A contains fossils of Nerinea trinodosa, Unit B contains Mucrospirifer mucronatus, Unit C contains Paradoxides pinus, and Unit D contains Prolecanites gurleyi. How would we arrange the units in order of relative geologic age from oldest to youngest?” Unit C, Unit B, Unit D, and Unit A. Model how to use the Index Fossil chart to order the units. Provide further practice if needed.
“Now complete question 5 on the worksheet. Be prepared to report to the class.” Facilitate a brief class discussion of the group findings.
Students remain grouped. “Now create your own group hypothetical Index Fossil chart, each group member contributing two ‘fossils’ to the chart and a set of four hypothetical rock units that contain some of the fossils in the chart. Sequence and record the rock units by relative age, oldest to youngest, and explain how you determined this sequence.”
Extension:
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Students performing above and beyond the standards can investigate Phacops rana, the state fossil of Pennsylvania, and explain why it is a good index fossil. Students will provide a written report with the following information:
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approximate age of the organism
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description of Earth during that time
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diet
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habitat
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importance of the fossil and how science has benefited from its discovery