By Jaap Vermeulen, Tony Whitten
Read or Download Biodiversity and Cultural Property in the Management of Limestone Resources in East Asia: Lessons from East Asia (Directions in Development (Washington, D.C.).) PDF
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Additional resources for Biodiversity and Cultural Property in the Management of Limestone Resources in East Asia: Lessons from East Asia (Directions in Development (Washington, D.C.).)
In contrast, their ability to regulate water is enhanced: They have developed means of expelling water in 100 percent humidity and expelling excess water without losing body salts. If their ancestors had wings, cave animals have lost them. Diurnal rhythms are lost. Their life span increases, and their fertility decreases dramatically. These adaptations have confined cave species to their habitatthey cannot survive elsewhere. If the cave in which they live is destroyed, they perish. East Asian cave fauna include many exceptional organisms.
Tectonic movements lifted them above sea level, often after a long burial beneath layers of sediment. " East Asia has the world's largest single expanse of limestone (in China) and the largest tropical limestone caverns (in Sarawak, Malaysia). Limestone dissolves in water at a rate that results in distinct landforms. The rate at which other kinds of rock dissolve in water is usually either too rapid to form karst landscapes or too slow, in which case chemical and mechanical weathering processes under the combined effects of sun, rain, and frost prevail.
At this time the carbon dioxide concentration may become 100 times higher than in the atmosphere. Acids, released by either the soil or by minerals in the rock, further increase rainwater's dissolving capacity. This water is, in the long run, capable of eroding limestone rock surfaces beneath a soil cover and widening cracks into caves and gorges. It will also line cave walls with stalactites, stalagmites, and other features together called speleothems, because once it emerges from a tight fissure into the air, some carbon dioxide will escape from the water, so that it suddenly becomes "supersaturated" and precipitates calcite.