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TITLE PAGE - acumen - The University of Alabama

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Discussion<br />

<strong>The</strong> energy-limitation hypothesis<br />

<strong>The</strong> results <strong>of</strong> this study provided general support for the energy-limitation hypothesis in<br />

cave ecosystems. First, the patterns in the biomass and secondary production <strong>of</strong> O. australis<br />

mirrored the gradients in standing crop organic matter and macroinvertebrate biomass among<br />

caves (Fig. 1A, B). Second, the comparisons <strong>of</strong> resource supply rates and crayfish demand<br />

indicate that nearly all macroinvertebrate production would need to be consumed to support the<br />

populations, which suggests these populations <strong>of</strong> O. australis are limited by prey availability.<br />

Resource availability<br />

<strong>The</strong> range in standing crop organic matter (22-133 g AFDM m -2 ) within the cave streams<br />

in this study falls within the lower range <strong>of</strong> reports from other cave (0-850 g AFDM m -2 ; Simon<br />

& Benfield 2001 & 2002; Venarsky et al., 2012a; Huntsman et al., 2011 a, b; see Chapter 3) and<br />

surface streams (20-35,000 g m -2 ; Jones, 1997). <strong>The</strong> large range in organic matter biomass<br />

among the cave streams in this study illustrates that, similar to surface streams, resource inputs<br />

can vary greatly. One factor likely contributing to the large variability in organic matter biomass<br />

among these cave streams is cave structure, such as the depth <strong>of</strong> cave and size <strong>of</strong> voids and<br />

fractures in the surrounding bedrock. For example, the higher quantities <strong>of</strong> organic matter in<br />

Tony Sinks Cave were probably the result <strong>of</strong> strong surface connections. This cave contained<br />

several entrances, both vertical and horizontal, that intersected intermittent stream channels.<br />

Additionally, large ceiling fissures were present in portions <strong>of</strong> the cave, below which large<br />

deposits <strong>of</strong> organic matter were observed.<br />

112

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