"The new method will help us to understand the rate at which some of the Earth's most important mountains have uplifted," she added. "It will also show how the process of mountain building influenced climatic patterns as well as plant and animal evolution."
The new method of paleoelevation involves counting the stomata on leaves of plants going back as far as 65 million years ago. Stomata are minute openings on the surface of leaves through which plants absorb gases, including carbon dioxide, which plants need for photosynthesis.
Anyone who has climbed a mountain knows that the air gets "thinner" as you climb higher. As with oxygen, carbon dioxide is less concentrated at higher elevations. Therefore, the higher the elevation, the more stomata per square inch of leaf surface a plant would need to survive. By simply counting the number of fossil stomata, Dr. McElwain can estimate how much carbon dioxide was in the air when the fossil leaf developed. From that, she can estimate the elevation at which the fossil plant once lived.
Dr. McElwain used historical and modern collections of California Black Oak (Quercus kelloggii) leaves for her study because the California Black Oak grows at an unusually wide range of elevations from 200 to 8,000 feet (60 to 2,440 meters). The historical leav
Contact: Greg Borzo