2022
DOI: 10.1016/j.foreco.2022.120106
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Differences in canopy and understorey diversities after the eruptions of Mount Usu, northern Japan — Impacts of early forest management

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Cited by 4 publications
(4 citation statements)
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“…As the canopy closes, they may be replaced by more shade-tolerant species due to light restriction; an indicator species change confirmed this phenomenon under RP (Table 7). Végh and Tsuyuzaki [97] held that stand spatial structure is more important than stand age, and passive restoration often leads to poor communities. Since the light environment under the stand changes with canopy closure, it is valid to consider that the emergence of various shade-tolerant climbing species, here referred to as woody vines (e.g., A. cochinchinensis and W. sinensis) and voluble herbs (e.g., Ipomoea nil (Linnaeus) Roth), as indicators in the later stage of RP restoration is a potential risk hindering healthy plantation development [98].…”
Section: Communities Stability and Stand Management Strategymentioning
confidence: 99%
“…As the canopy closes, they may be replaced by more shade-tolerant species due to light restriction; an indicator species change confirmed this phenomenon under RP (Table 7). Végh and Tsuyuzaki [97] held that stand spatial structure is more important than stand age, and passive restoration often leads to poor communities. Since the light environment under the stand changes with canopy closure, it is valid to consider that the emergence of various shade-tolerant climbing species, here referred to as woody vines (e.g., A. cochinchinensis and W. sinensis) and voluble herbs (e.g., Ipomoea nil (Linnaeus) Roth), as indicators in the later stage of RP restoration is a potential risk hindering healthy plantation development [98].…”
Section: Communities Stability and Stand Management Strategymentioning
confidence: 99%
“…Extreme volcanic eruptions, alongside the creation of new lava fields and massive landslide events, can result in the complete removal of all biotic material from a landscape and thus are an example of true primary succession [77][78][79][80]. During the eruption of Mount St. Helens (Lawetlat'la in the Cowlitz language; Washington State, USA) in 1980, all three of these disturbance types occurred simultaneously, and their interaction transformed vast areas by incinerating pre-existing forests and depositing up to 100 m of mostly inert material onto the landscape.…”
Section: Introductionmentioning
confidence: 99%
“…Globally, more than 1,300 volcanoes are known or thought to have erupted in the Holocene, and in the modern period around 80 eruptions a year are recorded 7 . While there have been many studies of the impacts of volcanism on vegetation dynamics, these have focused on the aftermath of a small number of eruptions, spanning relatively short timescales of decades, including Krakatau 1883 8 , Mount Usu 1910 9 , Surtsey 1963 10 and Mount St Helens 1980 11 . Studies concerning more ancient eruptions have tended to report paleobotanical inventories intended to characterize the contemporary ecologies and eruption season (e.g., Laacher See; ref.…”
Section: Introductionmentioning
confidence: 99%