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Canyonlands National ParkSeedling in Biological Soil Crust
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Canyonlands National Park
Lichens
 
photo: Closeup of lichens on sandstone
NPS Photo by Neal Herbert
Closeup of lichens on sandstone
 

(NPS Photo by Neal Herbert)

There is a great deal of exposed rock in Canyonlands, and much of it is covered by lichens. Lichens usually colonize north-facing surfaces since reduced solar radiation is an advantage for many organisms in the desert. Lichens also grow on healthy, mature cryptobiotic soil crust, and occasionally on live or dead plant material. Many species of lichen are found in Canyonlands.

A lichen is actually a simple community of at least two organisms, namely fungi with green algae or cyanobacteria, though sometimes with both. The lichen structure is more elaborate and durable than either fungi or algae alone. Green algae and cyanobacteria manufacture food via photosynthesis, while fungi provide a buffer against weather and are capable of extracting nutrients from soil and rock.

Lichens are well adapted to arid climates. They can carry on food production at any temperature above 32º Fahrenheit. Lichens can absorb more than their own weight of water, and can absorb temporary water like dew almost directly into their algal cells (the water does not need to go through roots and stems as it does in vascular plants).

Many plants benefit from the presence of lichens. The cyanobacterial component of lichens can transform atmospheric nitrogen (unusable to most organisms) into a form that is an essential nutrient for life. This is especially important in desert ecosystems, where lack of nitrogen is known to limit productivity.

Looking for more?
Looking for more?
Our bookstore contains a number of titles about the natural history of this area.
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Spanish Bottom on the Colorado River  

Did You Know?
At Spanish Bottom on the Colorado River, scientists discovered 260 feet of sediment below the water's surface. This could make Cataract Canyon one of the most actively filling canyons in the world.
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Last Updated: July 25, 2006 at 00:23 EST