2005
DOI: 10.3732/ajb.92.12.1948
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Vegetation patterns 25 years after the eruption of Mount St. Helens, Washington, USA

Abstract: In 2004, we surveyed the vegetation on Mount St. Helens to document changes since 1992. We asked how communities differentiate and if they develop predictable relationships with local environments. We sought evidence from links between species and environment and changes in community structure in 271 250-m(2) plots. The habitats of the seven community types (CTs) overlapped broadly. Ordination methods demonstrated weak correlations among species distributions and location, elevation, and surface variables. Com… Show more

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Cited by 75 publications
(46 citation statements)
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“…Landscape effects such as elevation and geographic position were highly associated with vegetation change, as they were on Mount St. Helens (del Moral and Lacher 2005). Despite these similarities, the speed of vegetation recovery on Mount Pinatubo is noteworthy, with dense cover of species occurring in less than 15 yr.…”
Section: Other Volcanoesmentioning
confidence: 98%
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“…Landscape effects such as elevation and geographic position were highly associated with vegetation change, as they were on Mount St. Helens (del Moral and Lacher 2005). Despite these similarities, the speed of vegetation recovery on Mount Pinatubo is noteworthy, with dense cover of species occurring in less than 15 yr.…”
Section: Other Volcanoesmentioning
confidence: 98%
“…del Moral and Lacher 2005). If these river systems on Mount Pinatubo follow patterns observed on other volcanoes, species diversity eventually will increase dramatically (e.g., Whittaker and Fernández Palacios 2007).…”
Section: Plant-mediated Successionmentioning
confidence: 99%
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“…), del Moral and Lacher (2005) used canonical correspondence analysis (CCA) and found only weak explanatory variables. We reanalyzed their data with RDA and obtained much improved results (RDA = 28.7% of the species variation, CCA = 13.0%).…”
Section: Heterogeneitymentioning
confidence: 99%
“…As river deltaic plains [4], riparian floodplains [5], salt marshes [6] freshwater marshes [7], coastal or inland sand dunes [8,9], volcanic erupted areas [10] and deglaciation areas (edge of retreating glacier; glacier forelands) [11] are offer an excellent opportunity to study processes of primary succession. However deltaic plains of big rivers belong to the most variable and least predictable environments on earth.…”
Section: Introductionmentioning
confidence: 99%