Other Activities: Life on Land
Materials:
- Ruler or tape measure
- Paper, markers, or printed insect outlines
- Optional: string for measuring wingspan
Instructions:
- Show images of Carboniferous insects, like the giant dragonfly (Meganeura) with a wingspan of ~2 feet (60 cm).
- Measure the wingspan and compare to modern insects like dragonflies or beetles.
- Discussion: Why could insects grow so large during the Carboniferous?
- Sample answer (Level 1): There was more oxygen in the air, so bugs could get bigger.
- Sample answer (Level 2): Higher oxygen concentration allowed larger bodies because insects rely on diffusion through tracheae; less oxygen limits maximum size today.
- Have students calculate the ratio of ancient insect size to modern relatives.
- Layers of soil, leaves, or paper
- Plastic containers or clear jars
- Heavy books or weights
- Layer leaves/paper and soil in a container to represent swampy forest layers.
- Press down with a heavy book to simulate compression over time.
- Talk with your child about how these layers eventually become coal over millions of years.
- Level 1: “Plants get squished over a long, long time to make coal.”
- Level 2: “Peat forms first, and over millions of years, pressure and heat turn it into coal through chemical changes.”
- Balloons or candles
- Optional: jars for different air conditions
- Inflate balloons to see how much “air” they can hold.
- Or, light a candle in a jar and see how long it burns. Discuss how oxygen helps living things “breathe” and grow.
- Relate it to giant insects of the Carboniferous—more oxygen allowed them to grow bigger than today’s insects.
- Level 1: “When there’s more oxygen, bugs can grow bigger.”
- Level 2: “Carboniferous oxygen levels were higher, allowing insects to reach huge sizes because their tracheal system could support larger bodies.”
Materials:
- Pieces of coal
- Fossil imprints or sedimentary rocks
- Magnifying glass (optional)
- Examine coal and fossils. Look for plant imprints or patterns.
- Discuss how these rocks formed from Carboniferous forests and swampy environments.
- Level 1: “Coal comes from really old plants that got squished a long time ago.”
- Level 2: “Sedimentary rocks and coal preserve evidence of ancient forests, showing us how Earth and ecosystems changed over millions of years.”