![]() GENERAL How to be a Good Guest Where is Bat Cave? The AREA Area rock Layers Topography Geomorphology Geological History The Paleozoic The Mesozoic The Cenozoic Water The Hydrologic Cycle Solution Solution chemistry Karst Landscapes Erosional Features Depositional Features Environmental Issues BAT CAVE How was Bat Cave formed? Surface Plan of the site Map of the Cave Life in and around Bat Cave A Virtual Trip Through Bat Cave TEST YOUR KNOWLEDGE |
![]() Before it was cleared for farming and ranching, the area surrounding Bat Cave was originally a mixed southern hardwood forest, dominated by oak and hickory. Today, open fields stretch on either side of the road to the cave. In the immediate vicinity of the property, and on the surrounding acreage, the land was used for sylviculture, the intensive growing of slash pine, Pinus palustris. Growth of competing species was suppressed and the only diversity is in the understory species where native shrubs (especially saw palmetto, Serenoa repens) and ferns can re-establish themselves between periodic discings and burns. On the site proper, the immediate cave vicinity has not been planted for obvious reasons and several species of hardwoods, notably live oak (Quercus virginiana) and wild cherry (Prunus serotina) have been able to establish themselves. The cooler and damper microclimate near the mouth of the cave supports the growth of several fern species not found on the woodland floor. The lack of sunlight prevents photosynthesis (and therefore primary production) within the cave itself, and vegetative growth is limited to fungi and molds. Organisms that are found in caves fall into several categories. Some are occasional, some are transients such as bats, others are permanent residents that make a living by feeding on decaying vegetative and animal matter. Some do not make caves their habitat and have fallen or slid into the cave and are trapped, unable to get out. The transients
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