For the majority of the year these crusty organisms are all dried out and dormant, appearing almost completely lifeless. Even in this crunchy dry state cryptobiotic soil crust function in extremely crucial ways by covering the soil, thus preventing it from blowing away and also helping to retain water in the soil. Given even a little rain however these crunchy crusts soften and become biological powerhouses. As rain drops fall, the crusts protect the soil again by holding it in place, preventing erosion and therefore preserving the soil and landscape. Infiltration of these raindrops is also facilitated so more water goes into the soil. Lastly, cyanobacteria remove nitrogen into the air and fixes it into the soil, increasing soil nutrients. So basically, these crusts protect the soil, increase and preserve soil water content, and enrich the soil with nutrients.
Cryptobiotic soil crust with pink lichens forming on the surface in the Sonoran Desert. |
Found at: http://www.soilcrust.org |
Being these crusts have such a strong bottom-up effect, their destruction can have huge effects on entire landscapes. Foot traffic, trampling by grazing animals, and off-road vehicles all can quickly destroy crusts that took anywhere from years to century's to form. Grazing and off-road vehicles are especially destructive being these activities cover so much area so quickly. Once a cryptobiotic soil crust is destroyed the soil becomes prone to erosion and there are less nutrients and water in the soil, harming the entire food chain. So the best way to preserve these crusts is to limit grazing and keep all foot and vehicle traffic on the trail or road.
After disturbance, it can take anywhere from years to centuries for a crust to form again. Deserts with summer rains, such as the Sonoran, form crusts more quickly in a matter of years to decades. Cooler deserts with winter precipitation, such as the Great Basin, can take centuries to form crusts. If a crust is undisturbed for very long periods of time mosses, liverworts, lichens and even ferns will colonize on top of the cyanobateria, algae, and fungi. Protecting soil crusts is essential to maintaining healthy desert ecosystem function.
For a lot more great information check out: http://www.soilcrust.org
This website even has a great free downloadable field guide for soil crusts.
After disturbance, it can take anywhere from years to centuries for a crust to form again. Deserts with summer rains, such as the Sonoran, form crusts more quickly in a matter of years to decades. Cooler deserts with winter precipitation, such as the Great Basin, can take centuries to form crusts. If a crust is undisturbed for very long periods of time mosses, liverworts, lichens and even ferns will colonize on top of the cyanobateria, algae, and fungi. Protecting soil crusts is essential to maintaining healthy desert ecosystem function.
For a lot more great information check out: http://www.soilcrust.org
This website even has a great free downloadable field guide for soil crusts.
Hi,
ReplyDeleteI am new to biotic soils and have a grass or grass-like species I am unable to identify.
The area is southern Oregon around 20 miles north of Medford in the Klamath geologic province. The location is in the forest at 2,000 to 3,000 feet with around 25" annual precipitation on a BLM road.
The species appears as a blackish-brown hair-like tangle with the naked eye then like a grass under a microscope.
The "grass" is around 5 cm long, 0.2 to 0.3 mm wide. The interesting structure is a basal "tube" 3mm long and 1mm in diameter that the grass sets in which is buried into the soil.
Can you tell what it may be from this description?
Thanks,
Mac McClure
popco@toast.net
Based on your description it may be the hair like tangle you see under the microscope are filamentous cyanobacteria (possibly the hairs you are talking about) which commonly form a sheath (possibly the tube you are talking about). I wonder if it resembles anything like this picture found here: http://www.soilcrust.org/figure6.htm
ReplyDeleteStill, I would have some questions about actually sizes and forms of the crust before I could make any real identification.