Description of Benthic Communities in Karst, Spring-Fed Streams of North Central Florida
Description of Benthic Communities in Karst, Spring-Fed Streams of North Central Florida
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佛罗里达州中北部喀斯特、泉水溪流中底栖群落的描述
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通讯作者:
R. W. Hull
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作者:
Robert A. Mattson;J. H. Epler;Michael K. Hein3;J. C. G. L. F. Rosenau;C. W. Hendry;R. W. Hull
: North-central Florida is dominated by a karst geology which gives rise to numerous springs and spring-influenced streams. These systems are fed by a regional aquifer system; the Floridan Aquifer. The periphyton communities of spring-influenced stream systems, such as the lower Suwannee and lower Santa Fe rivers, are characterized by an algal community typically dominated by diatoms (comprising 73% of the taxa list). Beds of submergent aquatic vegetation (SAV) are common in spring-influenced stream systems, dominated by macroalgae (primarily Chara spp.) and vascular plants (Sagittaria kurziana, Vallisneria americana, and others). Benthic invertebrate communities are dominated by chironomids, Ephemeroptera and Trichoptera on woody substrata (as suggested by data from Hester-Dendy samplers), with gastropod molluscs and crustaceans (primarily the amphipod Hyalella azteca) occasionally being relatively abundant. Sandy substrata are dominated by chironomids, gastropod and bivalve molluscs and oligochaetes. Our data indicate that a more species rich community is associated with hard substrata (such as wood and limestone shoals) than with soft-bottom communities. Epiphytic invertebrate communities on SAV are dominated by chironomids and ephemeropterans. Spring influ ence is a major structuring force in stream systems in north-central Florida. Increases in benthic invertebrate species richness and