PYROGENIC CHANGES OF BOG VEGETATION AND PEAT IN WESTERN SIBERIA

A. Sinyutkina, L. Gashkova, Y. Kharanzhevskaya
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Abstract

Wildfires are an important environmental factor which determines the carbon cycle intensity in mires. The article presents the assessment of the consequences of pyrogenic transformation and the current state of burntout mires in the taiga and forest-tundra zones of Western Siberia 6-8 years after the wildfire, with regard to their microhabitat heterogeneity. Field studies were conducted in 2022 on three mires (a total of 13 post-pyrogenic and pristine plots) and included a total-station survey of the surface, an assessment of the occurrence of species in the grass-dwarf shrub and moss-lichen tiers, sampling for laboratory analysis of the physical properties and botanical composition of peat. Sphagnum mosses, Polytrichum strictum, lichens and dwarf shrubs were considered as recovery indicator species. As a result of the study, it was found that the intensity of pyrogenic transformation is determined by the initial state of bog ecosystem and increases in a row: the hydro forestation site on the Bakchar raised bog - palsa - the Ust-Bakchar raised bog drained for peat extraction. At most of the studied plots, microdepressions were more susceptible to burnout, while hummocks were preserved or only partially burned out. The transformation of peat deposit properties extends beyond the layer directly exposed to burnout, and manifests itself in a decrease in water content, and an increase in ash content, bulk density and degree of humification. At the first stages of post-pyrogenic successions, similar patterns were revealed for the mires of taiga and forest-tundra zones, i.e. an intensive overgrowth with P. strictum. According to the results of the study, it was concluded that the hydroforestation site in the Bakchar bog could possibly restore the species composition of vegetation cover and resume peat accumulation. Irreversible changes in vegetation cover have occurred in the Ust-Bakchar bog, where the restoration of sphagnum mosses does not occur even 20 years after the fire.
西伯利亚西部沼泽植被和泥炭的热源变化
野火是决定沼泽碳循环强度的重要环境因素。文章对西西伯利亚泰加和森林-苔原地带野火发生 6-8 年后的火原转化后果和烧毁沼泽的现状及其微生境异质性进行了评估。2022 年在三块沼泽地(共 13 块风化后和原始地块)上进行了实地研究,包括地表全站调查、评估禾本科-矮灌木和苔藓-栗子层的物种出现情况、取样进行泥炭物理特性和植物成分的实验室分析。泥炭藓、狭叶蓼、地衣和矮灌木被视为恢复指标物种。研究结果表明,热原转化的强度由沼泽生态系统的初始状态决定,并依次增加:巴卡尔高地沼泽上的水利造林地--帕尔萨--为提取泥炭而排水的乌斯特-巴卡尔高地沼泽。在大多数研究地块中,微凹陷更容易被烧毁,而沼泽则得以保留或仅部分被烧毁。泥炭沉积物性质的变化超出了直接暴露于烧毁的泥炭层,表现为含水量下降,灰分含量、体积密度和腐殖化程度增加。在风化后演替的最初阶段,泰加带和森林-苔原带的沼泽也呈现出类似的模式,即严格意义上的沼泽过度生长。研究结果表明,巴卡尔沼泽的水力造林地点有可能恢复植被的物种组成并恢复泥炭的积累。乌斯特-巴克恰尔沼泽的植被发生了不可逆转的变化,即使在火灾发生 20 年后,泥炭藓也没有恢复。
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