How life and Earth have changed each other
Grade 9 Science Worksheet - Challenge Me

Circle the best answer.
Microbes made oxygen for a long time before it built up in the air. Noah looks for the best explanation of the delay. Which fits?
- Ozone destroyed the oxygen as fast as the microbes made it
- Oxygen escaped to space, so very little remained in the air
- Microbes made no oxygen until the delay ended, so nothing built up
- Early oxygen reacted with dissolved iron and volcanic gases before it could build up in the air
A, warmer climate, faster weathering, less CO₂, cooler climate; B, warmer climate, less snow, darker ground, more warming. Bo compares the loops. Which statement about their feedback fits?
- Both loops amplify the warming, since each starts with a warmer climate
- Loop A damps the warming, while loop B amplifies it
- Neither loop is a feedback, since each ends in a different system
- Loop A amplifies the warming, while loop B damps it
Read this first
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Reef-building corals live in sunlit water, mostly shallower than about 50 m. A drill core through an island's limestone cap shows shallow-water coral fossils from the top down to 1,400 m.
Luz reads the core. What does it show about the reef and the island?
- Currents carried the corals down to 1,400 m after the reef formed there
- The corals lived at 1,400 m depth, deep in the dark sea where they were found
- The sea once stood 1,400 m higher, so the corals grew at the surface
- The reef grew upward as the island sank, so life and Earth changed together
A student says oxygen has been 21% of the air since microbes first made it. Jun replies using what is known. Which reply is best?
- No: the air held no oxygen until land plants appeared
- No: oxygen stayed far below today's level for a very long time after it first rose
- Yes: the first microbes set the air at 21%, and it has not changed since
- Yes: oxygen jumped to 21% within a few thousand years of the first microbes
Mineral grains, 45; Water, 25; Air, 25; Roots, microbes and humus, 5. A student says soil is just crushed rock. Kira uses the table. Which reply is best?
- No: organic matter is the largest part, at 45% of the volume of the soil
- Yes: minerals are the largest part at 45%, so the water, air and roots do not matter
- No: minerals are only 45%; the 5% organic part comes from living things
- No: roots, microbes and humus are 50%, as much as water and air
Three planets' air (NASA)
Planet CO₂ (%) O₂ (%) Earth 0.04 21 Mars 95 0.17 Venus 96.5 0 A student says life only lives on Earth and never changes it. Pia uses the table. Which reply is best?
- No: Mars has the most oxygen, so life made its air
- Yes: the three airs are alike, so life cannot have changed any of them
- No: Earth's air is 21% oxygen and 0.04% CO₂, unlike its neighbors, because of life
- Yes: Earth's air differs from its neighbors just because it is closer to the Sun than Mars
Squeeze Earth's 4.54 billion years into one 24-hour day. Oxygen rose 2.4 billion years ago and land life spread 0.43 billion years ago. How many hours apart, by Ren's math?
- About 12.7 hours
- About 10.4 hours
- About 2.3 hours
- About 21.7 hours
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Burying 12 g of plant carbon leaves 32 g of oxygen in the air. (C + O₂ is CO₂ running backward.)
A coal swamp buries 1 million tonnes of plant carbon. How much oxygen does Tala say is left in the air?
- About 1 million tonnes
- About 3.7 million tonnes
- About 0.38 million tonnes
- About 2.7 million tonnes
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Volcanoes add 250 million tonnes of CO₂ a year and weathering removes 240 million (example data). The air holds about 3 trillion tonnes of CO₂ now.
Zee adds up the gap for 1 million years with no other change. About how much CO₂ builds up in the air?
- About 250 trillion tonnes, about eighty times today's total
- About 0 tonnes, since a feedback loop cancels any imbalance as soon as it appears
- About 10 trillion tonnes, three times today's total, so feedbacks must balance
- About 10 billion tonnes, a small fraction of today's total
Rates of change (example data)
Process Rate (mm per year) Coral reef growth 5 Soil formation 0.1 Milo turns the rates into change per 1,000 years. Which summary of the pace of life's changes to Earth fits?
- Reefs add about 10 cm and soils about 5 m per 1,000 years, so soils are faster
- Reefs and soils both add about 5 m per 1,000 years, so they run at one speed
- Reefs add about 50 m and soils about 1 m per 1,000 years, so both are fast
- Reefs add about 5 m and soils about 10 cm per 1,000 years, so the processes run at very different speeds