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Titlebook: Ecological Responses at Mount St. Helens: Revisited 35 years after the 1980 Eruption; Charles M. Crisafulli,Virginia H. Dale Book 2018 Spr

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Introductory Remarks on Samplingns. Data were from repeat sampling of permanent plots, grids and depressions that formed during the eruption (potholes). We assessed succession rates using turnover, community similarity and trajectory complexity. We estimated turnover from community type change, while information theory described t
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A. Sdika,R. Cabridenc,C. Hennequinew plant fragments, and primary succession mostly being initiated by the seeds dispersed onto the newly emplaced material. Vegetation changes on the debris-avalanche deposit during the first 30 years post eruption are analyzed, considering the role of non-native species and potential future vegetati
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https://doi.org/10.1007/978-1-4614-1743-9ed land that could be susceptible to exotic plant invasion. We studied spatial patterns of exotic plant richness and abundance along a road and pedestrian trail that traverse a volcanic disturbance gradient with varying management prescriptions. In blast areas, exotic plant richness and abundance in
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https://doi.org/10.1007/978-3-030-48206-0e event that covered a topographically complex land area with disturbances of varying intensity that altered survival of soil organisms. Animals from rodents to elk fed upon and transported mycorrhizal fungi through the different disturbance zones, facilitating succession and altering the newly form
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M. Ataharul Islam,Rafiqul I. Chowdhurycommunities in young (23- to 25-year-old) fishless ponds following a large natural disturbance. Over a 3-year period, Large-bodied macroinvertebrates were sampled from 97 ponds with a range of hydroperiods and biophysical characteristics. Macroinvertebrate communities from these ponds were spatially
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Inorganic fillers and trace metal analysis, through 2015, we documented the arrival of 34 of the 45 mammals in the regional species pool and the successful establishment of 25 species. The majority of small mammals that established were likely derived from source populations that survived in isolated refugia in adjacent areas that were less
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https://doi.org/10.1007/978-3-642-60282-5t eruption events leave biological legacies of the pre-disturbance ecosystems, and the course of post-disturbance succession involves the protracted interplay of these legacies with immigrating species, biotic interactions, site amelioration, and secondary biological and geophysical disturbance proc
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