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In general, there two types of communities: Hard and Soft communities.
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Abiotic variables did not discriminate sufficiently between different soft bottom communities to be a reliable basis for mapping.
While taxonomic distinctness may differ naturally among habitats, the effect does not seem to be strong, at least among soft bottom communities (e.g., mud versus sand).
Hence, the total living carbon prediction in this study (Figure 7) should be considered as a conservative estimate for the soft bottom communities solely reling on sinking phytodetritus, with the anomalies causing the observed biomass to deviate from this baseline (Figure 5b).
The DN principle and the DN gel have already attracted much attention in the soft matter community.
In soft-sediment communities near reefs, a variety of patterns have been described with distance from the reef edge.
Although many general ecological patterns have been established, often a significant amount of the spatial and temporal variation in soft-sediment communities within and among systems remains unexplained.
Differential transport rates caused by aggregations of mussels and other foundation species must be considered in explanations of spatial pattern in soft-bottom communities.
Organic loading from fish farming constitutes a significant disturbance to marine sediment, normally reducing species abundance and richness and creating disturbed patches in soft-bottom communities.
Compared to soft-sediment communities, an evidently increasing succession of species richness, abundance, and diversity descriptors (Shannon-Wiener H′ and Pielou's evenness J′) was observed with the community inhabiting empty Pinna shells.
Individual flats in this study were dug as much as 155% and as little as 0% annually, but rarely were they dug more than once a year as studies assessing the impact of digging on soft-sediment communities have assumed.
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