How life and Earth have changed each other

Grade 9 Science Worksheet - Building Confidence

NameDate

Circle the best answer.

  1. Read this first

    Four events (approximate)

    EventBillions of years ago
    Earth forms4.5
    Microbes raise oxygen in the air2.4
    Animals with hard shells appear0.54
    Land plants appear0.47
  2. Ari reads the table. Which pair shows life changing the air first, and the changed air then allowing new life?

    • Microbes raise oxygen (2.4); animals that use oxygen appear (0.54)
    • Earth forms (4.5); microbes alone then raise oxygen (2.4)
    • Animals appear (0.54); microbes then raise oxygen (2.4)
    • Land plants appear (0.47); microbes then raise oxygen afterward (2.4)
  3. Lower, 2.8, dissolved iron, no rust; Middle, 2.4, red-brown iron rust bands; Upper, 2.0, rust and red soils on land. Bo reads the layers. Which explanation fits the rust that appears at 2.4 billion years?

    • Iron in the sea rusted by itself, with no help from living things
    • The air lost its oxygen, so iron rusted less than before
    • Iron in the sea made microbes release oxygen, which formed the rust bands
    • Oxygen from living microbes reacted with iron in the sea and made rust
  4. Earth is 4.54 billion years old, and oxygen began to rise in the air 2.4 billion years ago. What share of Earth's history has had oxygen in the air, by Kira's math?

    • About 190%, more than the whole of Earth's history
    • About 5%, a small slice at the end
    • About 2.4%, the number of billions
    • About 53%, a little more than half
  5. Card

    Ultraviolet light splits O₂ into 2 oxygen atoms. Each atom joins an O₂ to make ozone (O₃). Overall: 3 O₂ make 2 O₃.

  6. Jun follows the card. How many ozone molecules can 6 oxygen molecules (O₂) make?

    • 9 ozone molecules
    • 4 ozone molecules
    • 6 ozone molecules
    • 2 ozone molecules
  7. Luz asks why land life had to wait for the ozone layer. Which reason fits?

    • Ozone absorbs ultraviolet light, which would damage cells on land
    • Ozone warms the surface, so land was too cold before it formed
    • Ozone formed first and made the oxygen that later filled the air
    • Ozone supplies the oxygen that land animals breathe
  8. Milo puts three events in order: oxygen in the air, the ozone layer, and life on land. Which order is right?

    • Oxygen, then life on land, then ozone
    • Life on land, then ozone, then oxygen
    • Ozone, then oxygen, then life on land
    • Oxygen, then ozone, then life on land
  9. Granite plots after 10 years (example data)

    PlotRock surface lost (mm)
    Bare rock0.1
    Rock under lichens0.5
  10. Noah compares the plots. What does the experiment show about living things and rock?

    • Lichens make no difference, since both plots lose a little rock
    • Lichens protect rock, so it wears 5 times slower under them
    • Lichens speed up the breakdown, but just 0.4 times as fast here
    • Lichens speed up the breakdown of rock, 5 times as fast here
  11. Organic matter in soil (example data)

    SiteOrganic matter (%)
    Bare rock debris0.1
    Forest floor5
  12. Pia compares the sites. What do the data show about where soil's organic matter comes from?

    • Weathering adds it: the bare rock debris holds 50 times as much as the forest
    • Living things add it: the forest holds 50 times as much as bare rock debris
    • Rock itself makes it: both sites hold about the same amount
    • Living things add it: the forest holds 5 times as much as bare rock debris
  13. New soil forms at about 0.05 mm a year (example data). How long does Ren say a 30 cm layer of soil takes to form?

    • About 6,000 years
    • About 15 years
    • About 60,000 years
    • About 600 years
  14. A rock sample (example)

    TestResult
    Weak acidfizzes
    Under a hand lensshell fragments
    Crystals of cooled lavanone
  15. Tala tests a rock. Which source does the evidence point to?

    • Lava that cooled quickly and hardened
    • Salt left behind as a lake dried out
    • Sand grains that were cemented together
    • Shells and hard parts of sea life that settled and hardened
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How life and Earth have changed each other

Answer Key - Grade 9 Science Worksheet - Building Confidence

Circle the best answer.

  1. Read this first

    Four events (approximate)

    EventBillions of years ago
    Earth forms4.5
    Microbes raise oxygen in the air2.4
    Animals with hard shells appear0.54
    Land plants appear0.47
  2. Ari reads the table. Which pair shows life changing the air first, and the changed air then allowing new life?

    • Microbes raise oxygen (2.4); animals that use oxygen appear (0.54)
    • Earth forms (4.5); microbes alone then raise oxygen (2.4)
    • Animals appear (0.54); microbes then raise oxygen (2.4)
    • Land plants appear (0.47); microbes then raise oxygen afterward (2.4)
  3. Lower, 2.8, dissolved iron, no rust; Middle, 2.4, red-brown iron rust bands; Upper, 2.0, rust and red soils on land. Bo reads the layers. Which explanation fits the rust that appears at 2.4 billion years?

    • Iron in the sea rusted by itself, with no help from living things
    • The air lost its oxygen, so iron rusted less than before
    • Iron in the sea made microbes release oxygen, which formed the rust bands
    • Oxygen from living microbes reacted with iron in the sea and made rust
  4. Earth is 4.54 billion years old, and oxygen began to rise in the air 2.4 billion years ago. What share of Earth's history has had oxygen in the air, by Kira's math?

    • About 190%, more than the whole of Earth's history
    • About 5%, a small slice at the end
    • About 2.4%, the number of billions
    • About 53%, a little more than half
  5. Card

    Ultraviolet light splits O₂ into 2 oxygen atoms. Each atom joins an O₂ to make ozone (O₃). Overall: 3 O₂ make 2 O₃.

  6. Jun follows the card. How many ozone molecules can 6 oxygen molecules (O₂) make?

    • 9 ozone molecules
    • 4 ozone molecules
    • 6 ozone molecules
    • 2 ozone molecules
  7. Luz asks why land life had to wait for the ozone layer. Which reason fits?

    • Ozone absorbs ultraviolet light, which would damage cells on land
    • Ozone warms the surface, so land was too cold before it formed
    • Ozone formed first and made the oxygen that later filled the air
    • Ozone supplies the oxygen that land animals breathe
  8. Milo puts three events in order: oxygen in the air, the ozone layer, and life on land. Which order is right?

    • Oxygen, then life on land, then ozone
    • Life on land, then ozone, then oxygen
    • Ozone, then oxygen, then life on land
    • Oxygen, then ozone, then life on land
  9. Granite plots after 10 years (example data)

    PlotRock surface lost (mm)
    Bare rock0.1
    Rock under lichens0.5
  10. Noah compares the plots. What does the experiment show about living things and rock?

    • Lichens make no difference, since both plots lose a little rock
    • Lichens protect rock, so it wears 5 times slower under them
    • Lichens speed up the breakdown, but just 0.4 times as fast here
    • Lichens speed up the breakdown of rock, 5 times as fast here
  11. Organic matter in soil (example data)

    SiteOrganic matter (%)
    Bare rock debris0.1
    Forest floor5
  12. Pia compares the sites. What do the data show about where soil's organic matter comes from?

    • Weathering adds it: the bare rock debris holds 50 times as much as the forest
    • Living things add it: the forest holds 50 times as much as bare rock debris
    • Rock itself makes it: both sites hold about the same amount
    • Living things add it: the forest holds 5 times as much as bare rock debris
  13. New soil forms at about 0.05 mm a year (example data). How long does Ren say a 30 cm layer of soil takes to form?

    • About 6,000 years
    • About 15 years
    • About 60,000 years
    • About 600 years
  14. A rock sample (example)

    TestResult
    Weak acidfizzes
    Under a hand lensshell fragments
    Crystals of cooled lavanone
  15. Tala tests a rock. Which source does the evidence point to?

    • Lava that cooled quickly and hardened
    • Salt left behind as a lake dried out
    • Sand grains that were cemented together
    • Shells and hard parts of sea life that settled and hardened