How life and Earth have changed each other
Grade 9 Science Worksheet - Building Confidence
Circle the best answer.
Read this first
Four events (approximate)
Event Billions of years ago Earth forms 4.5 Microbes raise oxygen in the air 2.4 Animals with hard shells appear 0.54 Land plants appear 0.47 Ari reads the table. Which pair shows life changing the air first, and the changed air then allowing new life?
- Earth forms (4.5); microbes alone then raise oxygen (2.4)
- Land plants appear (0.47); microbes then raise oxygen afterward (2.4)
- Microbes raise oxygen (2.4); animals that use oxygen appear (0.54)
- Animals appear (0.54); microbes then raise oxygen (2.4)
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 made microbes release oxygen, which formed the rust bands
- Oxygen from living microbes reacted with iron in the sea and made rust
- Iron in the sea rusted by itself, with no help from living things
- The air lost its oxygen, so iron rusted less than before
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 2.4%, the number of billions
- About 5%, a small slice at the end
- About 190%, more than the whole of Earth's history
- About 53%, a little more than half
Card
Ultraviolet light splits O₂ into 2 oxygen atoms. Each atom joins an O₂ to make ozone (O₃). Overall: 3 O₂ make 2 O₃.
Jun follows the card. How many ozone molecules can 6 oxygen molecules (O₂) make?
- 2 ozone molecules
- 6 ozone molecules
- 9 ozone molecules
- 4 ozone molecules
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
Organic matter in soil (example data)
Site Organic matter (%) Bare rock debris 0.1 Forest floor 5 Pia compares the sites. What do the data show about where soil's organic matter comes from?
- Living things add it: the forest holds 50 times as much as bare rock debris
- Weathering adds it: the bare rock debris holds 50 times as much as the forest
- Living things add it: the forest holds 5 times as much as bare rock debris
- Rock itself makes it: both sites hold about the same amount
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 600 years
- About 6,000 years
- About 15 years
- About 60,000 years
A rock sample (example)
Test Result Weak acid fizzes Under a hand lens shell fragments Crystals of cooled lava none Tala tests a rock. Which source does the evidence point to?
- Shells and hard parts of sea life that settled and hardened
- Lava that cooled quickly and hardened
- Salt left behind as a lake dried out
- Sand grains that were cemented together
A reef is 50 m thick and grew at 5 mm a year (example data). How long did it take, by Zee's math?
- About 250 years
- About 100,000 years
- About 1,000 years
- About 10,000 years
Coal formed from plants buried in swamps long ago. How do coal beds connect life and rock, by Esme's reading?
- Cooled lava rich in carbon became coal
- Sea shells piled up and hardened into coal
- Plants took carbon from the air, and burial turned their remains into coal
- Volcanic ash settled in swamps and became coal