2008
DOI: 10.1016/j.landurbplan.2007.12.005
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Forest remnants in the Long Point region, Southern Ontario: Tree species diversity and size structure

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Cited by 9 publications
(12 citation statements)
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“…This could explain the increase in light-demanding species but not in shade-demanding species richness in the edge zone in our woodlots, as also found by Cayuela et al (2006). Given their longevity, woody plants can persist for a long time (Hill and Curran, 2005) in sub-optimal conditions, leading to time lags between habitat degradation (by exposure to edge effects) and species response (Simberloff and Gotelli, 1984;Richart and Hewitt, 2008), i.e. 'extinction debt' (Tilman et al, 1994).…”
Section: Discussionmentioning
confidence: 52%
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“…This could explain the increase in light-demanding species but not in shade-demanding species richness in the edge zone in our woodlots, as also found by Cayuela et al (2006). Given their longevity, woody plants can persist for a long time (Hill and Curran, 2005) in sub-optimal conditions, leading to time lags between habitat degradation (by exposure to edge effects) and species response (Simberloff and Gotelli, 1984;Richart and Hewitt, 2008), i.e. 'extinction debt' (Tilman et al, 1994).…”
Section: Discussionmentioning
confidence: 52%
“…Concerning the survival of forest specialists in small fragments, the question arises about the slow response of longlived plants to forest fragmentation (Richart and Hewitt, 2008), as work based on simulations for Fagus grandifolia, a late-successional species in Wisconsin fragmented forests, suggests problems of recruitment of shade-tolerant species present as adults in the edge zone (Ranney et al, 1981). Hill and Curran (2005) also showed that shade-tolerant species responded to increased irregularity of fragment boundaries at the seedling stage but not at the adult stage.…”
Section: Resultsmentioning
confidence: 99%
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“…North America, temperate forests are significant for future climate mitigation strategies, as they are impacted by warming and disturbance events (Bonan, 2008;Cubasch et al, 2013;Weed et al, 2013). These areas were a large source of carbon, due to land clearing for agricultural purposes, at the start of the 20th century (Bonan, 2008;Richart and Hewitt, 2008). With the rise of industrial development and movement of agriculture into western states, many of these agricultural areas were abandoned and reforested through natural regrowth and afforestation practices (Canadell and Raupach, 2008).…”
mentioning
confidence: 99%