## Abstract The Fosa de Cariaco off the coast of Venezuela is an anoxic basin which is subject to small seasonal fluctuations in the depth of the anoxic water. Samples taken in the interface region (between oxic and anoxic waters) contained from 13 to 37 species represented by 117 to 380 individual
The effect of habitat stability on benthic invertebrate communities: the utility of species abundance distributions
โ Scribed by R.G. Death
- Publisher
- Springer
- Year
- 1996
- Tongue
- English
- Weight
- 747 KB
- Volume
- 317
- Category
- Article
- ISSN
- 1573-5141
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โฆ Synopsis
Spatial and temporal patterns in the species abundance distribution of benthic invertebrate communities of 11 fresh ater habitats (10 streams and a ind-s ept lake shore) ere examined ith respect to habitat stability . Abundance patterns varied markedly bet een seasons at most sites . Ho ever, mean abundance distributions at 4 of the 5 unstable sites and the 2 most stable sites ere dominated by one or t o taxa ith a large number of rare species, hereas sites of intermediate stability had more equitable distributions . Both the log series and log normal distributions ere statistically indistinguishable, at the 5% level, from all the observed mean abundance patterns . In contrast, graphical comparisons of the observed and fitted distributions suggested the log series may be the better fit at most of the unstable sites and the t o most stable sites, hereas the more equitable distribution at sites of intermediate stability suggested the log normal distribution as the better fit . If conditions at a site favoured one or t o species, either through severe physical conditions, or through competitive superiority in the absence of disturbance then the log series distribution may result . Ho ever, if no species in the community as strongly advantaged over others, a log normal distribution should result . Given the discriminating po er of the appropriate statistical test it may not, ho ever, be possible to pick up these differences ithout graphical comparisons as ell .
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