堪察加托尔巴钦斯基火山高原林带植被的原始植物演替

A P Korablev, V Yu Neshataeva
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引用次数: 0

摘要

研究了堪察加中部托尔巴辛斯基高原火山沉积的原生植物演替。揭示了影响演替率的主要因素。熔岩流和灰渣沉积的植物演替特征差异显著。揭示了世界上所有火山地区的一些共同机制。植物演替对熔岩流的主导影响因素是熔岩表面类型、熔岩结构和细层堆积速率。影响灰渣沉积物植物演替的主要因素是风蚀、水蚀和离种子源的距离。次生永久落叶松(cajanderi Mayr.)森林的形成时间在熔岩流上大约需要1500-2000年,在灰渣平原上需要1000年(但不少于300-500年)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Primary Plant Successions of Forest Belt Vegetation on the Tolbachinskii Dol Volcanic Plateau (Kamchatka).

Primary plant successions on volcanic deposits of the Tolbachinskii DoI 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.

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