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Physical Factors: Rock, Soil, Landform, Water, and Wind

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Forgotten Grasslands of the South
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Abstract

With this chapter we begin a more detailed exploration of the origin and maintenance of grasslands in the South. As reviewed in chapter 2, prolonged periods of drier climate or increased seasonality can convert forest to grassland. This process has occurred periodically in the past. Positive feedback loops involving megaherbivores and fire further contribute to grassland formation and can maintain grassland after climatic conditions favorable for its development have ended. The long sequence of grassland-adapted vertebrates in the fossil record, patterns of disjunction in plant and animal taxa between the semiarid West and the Southeast, and positive responses to fire in the flora and fauna provide evidence of this history.

The most satisfactory system of geographical classification of the vegetation of temperate Eastern North America is one based on geology.

Roland Harper (1906a)

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References

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Correspondence to Reed F. Noss .

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Noss, R.F. (2013). Physical Factors: Rock, Soil, Landform, Water, and Wind. In: Forgotten Grasslands of the South. Island Press, Washington, DC. https://doi.org/10.5822/978-1-61091-225-9_4

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