Making a Trace Fossil

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WSC National Fossil Day 2020@ HOME Making a Trace Fossil Gathering Supplies: Soft Modeling Clay or Homemade Salt Dough Rolling Pen Toothpick Leaves, Sticks, Bark and/or Shells Paint Brushes (Optional) Types of Fossils! There are two main types of fossils that paleontologists study: body fossils and trace fossils. So what is the difference between the two? Body fossils are probably what you think of most when you hear the word fossil. Like the large bones of a dinosaur. Body fossils are fossils that retain or keep the actual remains of an animal, even though it goes through the fossilization process. Think about fossils of a tooth, a claw, or skull of an ancient animal. These are all parts of the actual animal that have become a fossil. So if the original remains of a plant, insect or animal become fossilized, this would be a body fossil. Trace fossils show the activity of a plant or animal, without any of the actual remains being present. Examples of trace fossils are tracks of animals, or signs of their scratching and burrowing. Even fossilized poop is a type of trace fossil. The imprint of a leaf or bark from a tree or the texture of a shell are all examples of trace fossils. Remember a trace fossil will show the presence of an living organism without an actual part of their remains being fossilized. They can give clues to what animals did and how they acted along with what their environment was like. Try This! Making your own trace fossil. Go out on a nature walk with your family, in your neighborhood or in your backyard. See what plants and animals are living around you. Collect some leaves, along with a piece of bark or a twig. See if you have any shells at home. Use a soft piece of modeling clay (air dry or oven bake). Don’t have any? No problem just make some salt dough. There are many different recipes on-line. Take a ball of clay and roll it flat with a rolling pin. Then press your shell, bark or twig into the clay. You don’t have to press hard! Gently lift your object off of the clay and see what impression was left behind. For the leaves, place the leaves flat on the clay and roll the rolling pin over them. You can use a toothpick to help take the leaf off of the clay. Once you have an impression that you like, bake the clay or let it air dry. After the clay is hard you can paint your own trace fossil! .

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In Pliocene Deposits, Antarctic Continental Margin (ANDRILL 1B Drill Core) Molly F
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln ANDRILL Research and Publications Antarctic Drilling Program 2009 Significance of the Trace Fossil Zoophycos in Pliocene Deposits, Antarctic Continental Margin (ANDRILL 1B Drill Core) Molly F. Miller Vanderbilt University, [email protected] Ellen A. Cowan Appalachian State University, [email protected] Simon H. H. Nielsen Florida State University Follow this and additional works at: http://digitalcommons.unl.edu/andrillrespub Part of the Oceanography Commons, and the Paleobiology Commons Miller, Molly F.; Cowan, Ellen A.; and Nielsen, Simon H. H., "Significance of the Trace Fossil Zoophycos in Pliocene Deposits, Antarctic Continental Margin (ANDRILL 1B Drill Core)" (2009). ANDRILL Research and Publications. 61. http://digitalcommons.unl.edu/andrillrespub/61 This Article is brought to you for free and open access by the Antarctic Drilling Program at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in ANDRILL Research and Publications by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Published in Antarctic Science 21(6) (2009), & Antarctic Science Ltd (2009), pp. 609–618; doi: 10.1017/ s0954102009002041 Copyright © 2009 Cambridge University Press Submitted July 25, 2008, accepted February 9, 2009 Significance of the trace fossil Zoophycos in Pliocene deposits, Antarctic continental margin (ANDRILL 1B drill core) Molly F. Miller,1 Ellen A. Cowan,2 and Simon H.H. Nielsen3 1. Department of Earth and Environmental Sciences, Vanderbilt University, Nashville, TN 37235, USA 2. Department of Geology, Appalachian State University, Boone, NC 28608, USA 3. Antarctic Research Facility, Florida State University, Tallahassee FL 32306-4100, USA Corresponding author — Molly F.
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