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Betsy Purdum

Dry Prairie

Dry prairie is a fast disappearing community occuring only in central Florida. “Dry” prairie does not describe a permanent condition: portions of “dry” prairies are often “wet.” During the summer rainy season, standing water may drain as overland sheet flow, and even in the winter during El Nino years, dry prairies may be wet for a month or more. Dry prairies are dry only in relation to marshes, the other major treeless community in central Florida.

Dry prairies often share soil types, topography, and hydrologic regimes with neighboring mesic flatwoods. Their distinguishing characteristic is absence of trees, most likely the result of more intense and more frequent fires historically caused by lightning. Central Florida has more thunderstorm days and lightning strikes than any place in the United States. The largest, most intense burns historically occurred in late spring and early summer when conditions were relatively dry and fuel abundant. Fires later in the summer were probably smaller and less intense because of wetter conditions. In frequently burned dry prairies, the understory is diverse although wiregrass, sparse stunted palmetto, and low-growing runner oak commonly dominate.

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