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In contrast, there were short-term increases in richness of mosses and of species growing on disturbed mineral soil, but these species numbers returned to mature-forest levels in the young stands.
While the inoculum is likely to be randomly drawn from regional pools and accumulates over time, our data provide no support for increases in richness over time since deglaciation, as is commonly observed for plant communities.
The rapid initial increases in richness and density were highly correlated with leaf area which, on plots that were heavily stocked prior to cutting, returned to precut levels by year 6 or 7. Species richness on 6-year-old clearcuts was more than twice that of any mature stand sampled.
Decreases in progressive similarity may be related to declines in richness or abundance relative to the historic baseline, or they may be related to increases in richness or abundance relative to the historic baseline.
At local scales, species loss is less frequently observed, and the spread of weedy or exotic species often instead results in increases in richness [ 2].
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Species richness of frugivores and nectarivores decreased with increasing distance to forest, whereas granivorous birds increased in richness.
An initial sharp increase in richness and density from post-cut years 2 6 preceded a steep decline by year 25.
Forbs, both native and exotic, were the most responsive lifeform and increased in richness and cover after thinning, with the greatest response in the thin-burn.
The apparent increase in richness may be due to maintenance of original vegetation-specific species in untransformed fragments in highly transformed areas combined with species that exploit transformed habitats well in the transformed areas.
Whereas an increase in richness to 200 m depth was observed in both studies, no evidence was found to support a LSDG once sampling effort (number of stations, area sampled) and depth covariates were removed [63], [53].
In deeper waters of the continental shelf, several studies have shown an increase in richness to approximately 200 m depth followed by a decline to 300 500 m (Northern European polychaetes [119], Greenland shelf peracarid crustaceans [128], European-scale infauna [53]).
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