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Primary plant successions of forest belt vegetation on the Tolbachinskii Dol volcanic plateau (Kamchatka)

机译:托尔巴钦斯基多尔火山高原(堪察加半岛)森林带植被的主要植物演替

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摘要

Primary plant successions on volcanic deposits of the Tolbachinskii Dol Plateau (Central Kamchatka) were studied. The main factors determining the succession rate were revealed. The peculiarities of plant successions on lava flows and ash-scoria deposits differed significantly. Some common mechanisms for all volcanic regions of the world were revealed. The leading factors of plant succession on lava flows were the type of lava surface, the texture of lava, and the fine tephra accumulation rate. The main factors determining plant succession on ash-scoria deposits were wind and water erosion and the distance to the seed sources. The time of formation of a secondary permanent larch (Larix cajanderi Mayr.) forest should take about 1500-2000 years on lava flows and up to 1000 years (but not less than 300-500 years) on ash-scoria plains.
机译:研究了Tolbachinskii Dol高原(堪察加中部)的火山岩沉积物中的原生植物演替。揭示了决定继承率的主要因素。熔岩流和灰渣沉积物中植物演替的特殊性差异很大。揭示了世界所有火山地区的一些共同机制。植物在熔岩流中演替的主要因素是熔岩表面的类型,熔岩的质地和细的红喉草积累速率。影响灰渣沉积物植物演替的主要因素是风蚀和水蚀以及与种子源的距离。在熔岩流上,次生永久落叶松(Larix cajanderi Mayr。)森林的形成时间大约需要1500-2000年,而在灰火山灰平原上最多需要1000年(但不少于300-500年)。

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  • 来源
    《Biology Bulletin》 |2016年第4期|307-317|共11页
  • 作者单位

    Russian Acad Sci, Komarov Bot Inst, Ul Prof Popova 2, St Petersburg 197376, Russia;

    Russian Acad Sci, Komarov Bot Inst, Ul Prof Popova 2, St Petersburg 197376, Russia;

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