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Supplement
Nature 451, 274-276 (17 January 2008) | doi:10.1038/nature06586; Published online 16 January 2008
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Assistant / Associate Professor
- Yale University
- New Haven, CT
Postdoctoral Associate in Enzyme Biochemistry
- Cornell University
- Ithaca, New York
From landscapes into geological history
Philip A. Allen1
Abstract
Erosional and depositional landscapes are linked by the sediment-routing system. Observations over a wide range of timescales might show how these landscapes are translated into the narrative of geological history.
Earth's landscape, shaped by the interplay between tectonics and climate, is a dynamic interface over which many biogeochemical cycles operate. The mass fluxes associated with the physical, biological and chemical processes acting across the landscape involve the transport of particulate sediment and solutes.
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