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Eelgrass beds have been postulated to support different faunal communities from unvegetated sandflats, in part because of the stabilisation of sediments in eelgrass beds and their destabilisation in sandflats due to bioturbation. More specifically, eelgrass beds have been hypothesised to support disproportionately greater numbers of small, flexible and non-burrowing species, and bioturbated sandflats to support more large, hard-bodied burrowers. These concepts were tested in Langebaan Lagoon on the west coast of South Africa, where beds of the eelgrass Zostera capensis and sandflats dominated by Callianassa kraussi bioturbation are mutually exclusive. In eelgrass beds, sediment penetrability was significantly reduced compared to that in sandflats. Distinctly different faunal communities occurred in the two habitats, and the suite of species characteristic of each was consistent between years and between sites. Overall, density was higher in eelgrass beds than in sandflats. In contrast to previous studies, however, richness and diversity in sandflats were greater than, or equal to, values for eelgrass beds. There is convincing support for the hypothesis that burrowers are more prevalent in sandflats and less prevalent in eelgrass beds. Conversely, body flexibility does not differ between habitats and sizes are greater in the eelgrass beds than in the sandflats.  相似文献   
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Callianassid sandprawns and eelgrasses have been postulated to have mutually negative effects on each other. The relationship between Callianassa kraussi and Zostera capensis was investigated in Langebaan Lagoon on the west coast of South Africa by correlative field surveys. Seven facts point to mutually antagonistic interactions between the species: (1) cover of Z. capensis was negatively correlated with density of C. kraussi; (2) Z. capensis was largely confined to the high shore, whereas C. kraussi occurred in unvegetated sandbanks below the eelgrass beds; (3) at sites where Z. capensis was absent, C. kraussi extended farther up the shore than in its presence; (4) C. kraussi reached a larger maximum size in sandbanks than in beds of Z. capensis; (5) immediately below eelgrass beds there was a 'frontier zone' where above-ground Z. capensis was absent but below-ground root-rhizomes appeared to exclude C. kraussi; (6) sediment penetrability was greater in sandbanks than in eelgrass beds; (7) rate of burrowing by C. kraussi was faster in unvegetated sandbanks than in eelgrass beds. Conversely, the density and sizes of the mudprawn Upogebia africana were greater in beds of Z. capensis than in sandflats dominated by C. kraussi. Although this evidence is correlative, it suggests that Z. capensis excludes C. kraussi because it stabilises the sediment and inhibits burrowing, and that C. kraussi prevents establishment of eelgrass beds by destabilising the sediment and suspending material that smothers the eelgrass. In the process, two distinct habitats are created. U. africana may benefit directly from eelgrass because it requires stable sediment for its semi-permanent U-tubes; but also indirectly because Z. capensis excludes C. kraussi, which may disrupt these feeding burrows. At the head of the lagoon where sediments are very fine and compact, U. africana occurs both in and below the eelgrass bed, and coexists with at least low densities of C. kraussi, although Z. capensis and C. kraussi are still negatively correlated.  相似文献   
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