What is a fossil?
•   A fossil is the preserved remains of a once-
    living organism.

What do fossils tell us?
•   Fossils give clues about organisms that lived
    long ago. They help to show that evolution
    has occurred.
•   They also provide evidence about how
    Earth’s surface has changed over time.
•   Fossils help scientists understand what past
    environments may have been like.
HOW IS A FOSSIL FORMED?




1. Sediment                  2. Layers                  3. Movement              4. Erosion
An animal is buried by       More sediment layers       Movement of tectonic     Erosion from rain,
sediment, such as            accumulate above the       plates, or giant rock    rivers, and wind wears
volcanic ash or silt,        animal’s remains, and      slabs that make up       away the remaining
shortly after it dies. Its   minerals, such as silica   Earth’s surface, lifts   rock layers. Eventually,
bones are protected          (a compound of silicon     up the sediments and     erosion or people
from rotting by the          and oxygen), slowly        pushes the fossil        digging for fossils will
layer of sediment.           replace the calcium        closer to the surface.   expose the preserved
                             phosphate in                                        remains.
                             the bones.
FIVE MAIN TYPES OF FOSSILS


 Petrified             Molds and               Carbon
 Fossils                Casts                   Films




              Trace                Preserved
             Fossils               Remains
PETRIFIED FOSSILS
                              • The word “petrified” means
                                “turning into stone.”
                              • Petrified fossils form when
                                minerals replace all or part
                                of an organism.
                              • Water is full of dissolved
                                minerals. It seeps through
                                the layers of sediment to
                                reach the dead organism.
 PETRIFIED FOSSIL
The Field Museum in Chicago
                                When the water evaporates,
    displays a fossil of a      only the hardened minerals
     Tyrannosaurus rex.
                                are left behind.
MOLDS AND CASTS
                               • A mold forms when hard parts of an
                                 organism are buried in sediment,
                                 such as sand, silt, or clay.
   MOLD FOSSIL                 • The hard parts completely dissolve
This mold, or imprint, is of     over time, leaving behind a hollow
 an extinct mollusk called       area with the organism’s shape.
      an ammonite.
                               • A cast forms as the result of a mold.
                               • Water with dissolved minerals and
                                 sediment fills the mold’s empty
                                 spaces.
   CAST FOSSIL                 • Minerals and sediment that are left
 This ammonite cast was
                                 in the mold make a cast.
 discovered in the United
        Kingdom.               • A cast is the opposite of its mold.
CARBON FILMS
                               • All living things contain an
                                 element called carbon.
                               • When an organism dies
                                 and is buried in sediment,
                                 the materials that make up
                                 the organism break down.
                               • Eventually, only carbon
     FERN FOSSIL                 remains.
This carbon-film fossil of a   • The thin layer of carbon
     fern is more than           left behind can show an
  300 million years old.
                                 organism’s delicate parts,
                                 like leaves on a plant.
TRACE FOSSILS

                              • Trace fossils show the
                                activities of organisms.
                              • An animal makes a footprint
                                when it steps in sand or mud.
                              • Over time the footprint is
                                buried in layers of sediment.
                                Then, the sediment becomes
 FANCY FOOTWORK
This dinosaur footprint was
                                solid rock.
 found in Namibia, Africa.
PRESERVED REMAINS
 Some organisms get preserved in or close to their
original states. Here are some ways that can happen.




Amber                 Tar                    Ice
An organism,          An organism,           An organism,
such as an insect,    such as a              such as a woolly
is trapped in a       mammoth, is            mammoth, dies in
tree’s sticky resin   trapped in a tar pit   a very cold region.
and dies. More        and dies. The tar      Its body is frozen
resin covers it,      soaks into its         in ice, which
sealing the insect    bones and stops        preserves the
inside. It hardens    the bones from         organism—even
into amber.           decaying.              its hair!
For more on fossils visit:
                                                Video: Becoming a Fossil
                                   http://www.pbs.org/wgbh/evolution/library/04/3/l_043_01.html
                                                                                   PBS

                                                 Article: Major Fossil Find
                                     http://www2.scholastic.com/browse/article.jsp?id=3751945
                                                           Scholastic News Online

                                              Online Exhibit: Fossil Halls
                                         http://www.amnh.org/exhibitions/permanent/fossilhalls
                                          American Museum of Natural History

                                          Interactive Game: Fossil Hunt
               http://channel.nationalgeographic.com/episode/dino-death-trap-2998#tab-fossil-hunt
                                                               National Geographic

Scholastic Classroom Magazines. www.scholastic.com Photo Credits:                    PAGE 1: UTAH MUSEUM OF NATURAL HISTORY (DINOSAUR); PHOTOTAKE INC./ALAMY (ANT). PAGE
3: 5W INFORGRAPHIC (GRAPHIC). PAGE 4: Jason Lindsey/Alamy (DINOSAUR); Peter Bowater/Alamy (MOLD); David Lyons/Alamy (FERN); Hoberman Collection UK/Alamy (FOOTPRINT); John
Cancalosi/Alamy (MANTIS). PAGE 5: Gary Crabbe/Alamy (DINOSAUR). PAGE 6: Peter Bowater/Alamy (MOLD); Detail Heritage/Alamy (CAST). PAGE 7: David Lyons/Alamy (FERN). PAGE 8: Hoberman
Collection UK/Alamy (FOOTPRINT). PAGE 9: John Cancalosi/Alamy (MANTIS); R1/Alamy (TAR PITS); Gianni Dagli Orti/Corbis (MAMMOTH).

Science World Fossils

  • 2.
    What is afossil? • A fossil is the preserved remains of a once- living organism. What do fossils tell us? • Fossils give clues about organisms that lived long ago. They help to show that evolution has occurred. • They also provide evidence about how Earth’s surface has changed over time. • Fossils help scientists understand what past environments may have been like.
  • 3.
    HOW IS AFOSSIL FORMED? 1. Sediment 2. Layers 3. Movement 4. Erosion An animal is buried by More sediment layers Movement of tectonic Erosion from rain, sediment, such as accumulate above the plates, or giant rock rivers, and wind wears volcanic ash or silt, animal’s remains, and slabs that make up away the remaining shortly after it dies. Its minerals, such as silica Earth’s surface, lifts rock layers. Eventually, bones are protected (a compound of silicon up the sediments and erosion or people from rotting by the and oxygen), slowly pushes the fossil digging for fossils will layer of sediment. replace the calcium closer to the surface. expose the preserved phosphate in remains. the bones.
  • 4.
    FIVE MAIN TYPESOF FOSSILS Petrified Molds and Carbon Fossils Casts Films Trace Preserved Fossils Remains
  • 5.
    PETRIFIED FOSSILS • The word “petrified” means “turning into stone.” • Petrified fossils form when minerals replace all or part of an organism. • Water is full of dissolved minerals. It seeps through the layers of sediment to reach the dead organism. PETRIFIED FOSSIL The Field Museum in Chicago When the water evaporates, displays a fossil of a only the hardened minerals Tyrannosaurus rex. are left behind.
  • 6.
    MOLDS AND CASTS • A mold forms when hard parts of an organism are buried in sediment, such as sand, silt, or clay. MOLD FOSSIL • The hard parts completely dissolve This mold, or imprint, is of over time, leaving behind a hollow an extinct mollusk called area with the organism’s shape. an ammonite. • A cast forms as the result of a mold. • Water with dissolved minerals and sediment fills the mold’s empty spaces. CAST FOSSIL • Minerals and sediment that are left This ammonite cast was in the mold make a cast. discovered in the United Kingdom. • A cast is the opposite of its mold.
  • 7.
    CARBON FILMS • All living things contain an element called carbon. • When an organism dies and is buried in sediment, the materials that make up the organism break down. • Eventually, only carbon FERN FOSSIL remains. This carbon-film fossil of a • The thin layer of carbon fern is more than left behind can show an 300 million years old. organism’s delicate parts, like leaves on a plant.
  • 8.
    TRACE FOSSILS • Trace fossils show the activities of organisms. • An animal makes a footprint when it steps in sand or mud. • Over time the footprint is buried in layers of sediment. Then, the sediment becomes FANCY FOOTWORK This dinosaur footprint was solid rock. found in Namibia, Africa.
  • 9.
    PRESERVED REMAINS Someorganisms get preserved in or close to their original states. Here are some ways that can happen. Amber Tar Ice An organism, An organism, An organism, such as an insect, such as a such as a woolly is trapped in a mammoth, is mammoth, dies in tree’s sticky resin trapped in a tar pit a very cold region. and dies. More and dies. The tar Its body is frozen resin covers it, soaks into its in ice, which sealing the insect bones and stops preserves the inside. It hardens the bones from organism—even into amber. decaying. its hair!
  • 10.
    For more onfossils visit: Video: Becoming a Fossil http://www.pbs.org/wgbh/evolution/library/04/3/l_043_01.html PBS Article: Major Fossil Find http://www2.scholastic.com/browse/article.jsp?id=3751945 Scholastic News Online Online Exhibit: Fossil Halls http://www.amnh.org/exhibitions/permanent/fossilhalls American Museum of Natural History Interactive Game: Fossil Hunt http://channel.nationalgeographic.com/episode/dino-death-trap-2998#tab-fossil-hunt National Geographic Scholastic Classroom Magazines. www.scholastic.com Photo Credits: PAGE 1: UTAH MUSEUM OF NATURAL HISTORY (DINOSAUR); PHOTOTAKE INC./ALAMY (ANT). PAGE 3: 5W INFORGRAPHIC (GRAPHIC). PAGE 4: Jason Lindsey/Alamy (DINOSAUR); Peter Bowater/Alamy (MOLD); David Lyons/Alamy (FERN); Hoberman Collection UK/Alamy (FOOTPRINT); John Cancalosi/Alamy (MANTIS). PAGE 5: Gary Crabbe/Alamy (DINOSAUR). PAGE 6: Peter Bowater/Alamy (MOLD); Detail Heritage/Alamy (CAST). PAGE 7: David Lyons/Alamy (FERN). PAGE 8: Hoberman Collection UK/Alamy (FOOTPRINT). PAGE 9: John Cancalosi/Alamy (MANTIS); R1/Alamy (TAR PITS); Gianni Dagli Orti/Corbis (MAMMOTH).