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Interesting times on Krakatau: stand dynamics in the 1990s

机译:Krakatau上的有趣时光:1990年代的展台动态

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摘要

The Krakatau Islands, Indonesia, have provided an opportunity for ecologists to track primary succession from the 'clean slate' of 1883, through forest closure in the 1920s, to the contemporary period, in which successional changes take the form of alterations in composition and stature of forest stands rather than gross changes in ecosystem type. This paper reports on permanent forest plots established on the islands in 1989, and fully surveyed again in both 1992 and 1997. Since 1989, the plots have been subject to natural disturbance phenomena in the form of varying combinations of, for example, deposition of volcanic ejecta, landslides, lightning strikes, storm damage and drought. These effects have been concentrated between 1992 and 1997, during which the volcano Anak Krakatau has deposited ash on the islands of Sertung and Panjang, but not on Rakata. Data on stand responses are presented for growth rates (dbh (diameter at breast height, 1.3 m) increment), stem recruitment and mortality, biomass changes (partitioned into mortality, ingrowth and growth of established trees), and compositional shifts. The discussion focuses on evaluation of questions and successional models framed earlier in the programme. One general finding is that the stand dominants as of 1989 have tended to decline in number within the plots, generally through low levels of recruitment failing to balance rates of mortality. The effects of disturbance to the plots appear to be evident in terms of mortality and recruitment, dbh increment, and changes in biomass. The patterns of change in the eight plots are quite varied, such that relatively few generalizations are possible. The difficulties of establishing meaningful baseline rates for tree growth and stand biomass are discussed.
机译:印度尼西亚的喀拉喀托群岛为生态学家提供了一个机会,可以追踪从1883年的“纯净石板”到1920年代的森林封闭到现代时期的主要演替,在此期间,演替变化以成分和身高的变化为形式林分的数量而不是生态系统类型的总体变化。本文报告了1989年在这些岛屿上建立的永久性森林地块,并在1992年和1997年再次进行了全面调查。自1989年以来,这些地块一直受到自然干扰现象的影响,例如火山沉积的不同组合形式喷射,滑坡,雷击,风暴破坏和干旱。这些影响集中在1992年至1997年之间,在此期间,阿纳克·克拉卡托火山(Anak Krakatau)将火山灰沉积在Sertung和Panjang岛上,但不沉积在Rakata上。给出了林分响应的数据,包括生长速率(dbh(胸高处的直径,1.3 m)增量),茎招募和死亡率,生物量变化(分为已死树的死亡率,向内生长和生长)以及组成变化。讨论的重点是评估计划较早时提出的问题和继任模型。一个普遍的发现是,自1989年起,林地的优势种群数量趋于下降,这通常是由于招募的人数很少,未能平衡死亡率。在死亡率和募集,dbh增量和生物量变化方面,扰动对样地的影响似乎很明显。八个图中的变化模式变化很大,因此可以进行相对较少的概括。讨论了为树木生长和林分生物量建立有意义的基准速率的困难。

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