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Both algae and fungi are not independent...

Both algae and fungi are not independently capable of initiating seral changes on bare rocks but lichens can do so becase they

A

Adapt suitably to xeric conditions

B

Are a combination of alge and fungi

C

Can secrete acids for weathering

D

Do not require much sunlight

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**Step-by-Step Solution:** 1. **Understanding the Question**: The question asks why lichens can initiate seral changes on bare rocks, while algae and fungi cannot do so independently. 2. **Defining Seral Changes**: Seral changes refer to the ecological succession process that transforms bare or uninhabitable environments into more complex ecosystems. This process often starts with pioneer species that can survive in harsh conditions. 3. **Role of Algae and Fungi**: Algae and fungi, when present independently, do not have the capability to initiate these changes. Algae primarily require sunlight for photosynthesis, while fungi do not contribute to the weathering process on their own. 4. **Understanding Lichens**: Lichens are a symbiotic association between algae and fungi. This means that they work together, combining the strengths of both organisms. 5. **Acid Secretion**: One of the key reasons lichens can initiate seral changes is that they can secrete acids. These acids help in the weathering of rocks, breaking them down into smaller particles that can eventually form soil. 6. **Weathering Process**: Weathering is essential for soil formation, as it involves the breakdown of rocks into smaller particles. This process is crucial for creating a substrate where other plants can grow. 7. **Conclusion**: Therefore, lichens can initiate seral changes on bare rocks because they are a combination of algae and fungi that work together to secrete acids, facilitating the weathering of rocks and the formation of soil. **Final Answer**: Lichens can initiate seral changes on bare rocks because they are a symbiotic association of algae and fungi that secrete acids, which contribute to the weathering of rocks and the formation of soil. ---
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