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Titlebook: Ecological Responses to the 1980 Eruption of Mount St. Helens; Virginia H. Dale,Frederick J. Swanson,Charles M. C Book 2005 Springer-Verla

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楼主: 哪能仁慈
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https://doi.org/10.1007/978-3-642-85223-7, persisted across much of the affected landscape. The physical characteristics of the volcanic processes (elevated temperature, impact force, abrasion, and depth of erosion and burial) in part determined the extent of mortality and the types and significance of biotic legacies in the posteruption l
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Extraction of sterols from tissues,than the 1980 eruption, three experienced by trees alive in 1980 (1480, 1800, and 1980; Mullineaux 1996). The likely extent and magnitude of past volcanic eruptions are apparent in Cascade Range soils near or downwind from major volcanoes, soils that are largely formed from tephra (Franklin and Dyrn
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Surgery after target access timehment. Therefore, interactions between site amelioration and proximity to colonists affect the arrival sequence and initial biodiversity. Unique disturbance events combine with usually low colonization probabilities to produce different species assemblages after each disturbance at a site. Early in
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Patricia M. Hillebrandt B.Sc.(Econ.), Ph.D.lcanic eruption, studies of arthropods not only can provide information on natural history and ecology of many different species but also are relevant for evaluating theories of disturbance ecology and postdisturbance successional processes.
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https://doi.org/10.1007/978-3-0348-5265-41980 eruption may provide insights into how amphibians respond to major environmental changes over large spatial scales. This information is important because of the apparent declines of amphibian species during the past two to three decades (Blaustein and Wake 1990, 1995; Pechmann et al. 1991; Pech
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Michael Schleimer,Volker Schurigl hyphae can be several meters to more than a kilometer per gram of soil. Thus, hyphae magnify the surface area of soil available for nutrient uptake and for soil-particle binding manifold compared with the roots alone.
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,Gewöhnliche Differentialgleichungen,buting additional organic and nutrient resources to the soils. The development of soil organic fractions through decomposition in an otherwise mineral substrate (pumice and tephra) has undoubtedly facilitated the continued successional development of floral and faunal communities in the disturbed zo
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