In the hyper-arid, frigid desert of Antarctica's McMurdo Dry Valleys, visible life on rock surfaces is virtually non-existent. Instead, microbial life, dominated by endolithic lichens, colonizes the pore spaces just millimeters beneath the surface of translucent sandstones. Rather than merely surviving in a dormant state, these organisms actively drive physical and chemical weathering processes. By executing cyclic expansion during brief hydration periods and producing oxalic acid, they gradually dissolve cement minerals, causing the sandstone to flake off. While researchers initially theorized that these micro-ecosystems were static relics of past milder climates, recent metabolic monitoring confirms that they function as active, albeit slow, geomorphological agents that continuously reshape the local landscape.
Which choice best states the main idea of the text?
- AMicrobial communities in extreme environments utilize specialized chemical and physical strategies to withstand harsh climatic conditions.
- Endolithic lichens in the McMurdo Dry Valleys actively contribute to the alteration and erosion of sandstone rather than remaining passive or dormant.Answer
- CEndolithic lichens are static remnants of a historical era when Antarctica experienced a much milder and wetter climate.
- DThe physical weathering caused by endolithic lichens will eventually allow larger, visible organisms to colonize the surface of Antarctic sandstones.