Associations between forest vegetation and the fertility of soil organic horizons in northwestern Russia

Abstract Background Being the product of the same environment, soil and vegetation are mutually associated with each other, but the relationships between edaphic properties and vegetation characteristics are still far from clear. Accordingly, the specific aim of this study is to identify relationshi...

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Bibliographic Details
Published in:Forest Ecosystems
Main Authors: Natalia V. Lukina, Elena V. Tikhonova, Maria A. Danilova, Olga N. Bakhmet, Aleksandr M. Kryshen, Daria N. Tebenkova, Anastasia I. Kuznetsova, Vadim E. Smirnov, Tatiana Yu Braslavskaya, Aleksey V. Gornov, Maksim P. Shashkov, Svetlana V. Knyazeva, Anton D. Kataev, Ludmila G. Isaeva, Natalia V. Zukert
Format: Article in Journal/Newspaper
Language:English
Published: SpringerOpen 2019
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Online Access:https://doi.org/10.1186/s40663-019-0190-2
https://doaj.org/article/18c5c264b66042918cae48eacbcbdae7
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Summary:Abstract Background Being the product of the same environment, soil and vegetation are mutually associated with each other, but the relationships between edaphic properties and vegetation characteristics are still far from clear. Accordingly, the specific aim of this study is to identify relationships between forest site types/forest types and the fertility of soil organic horizons in northwestern Russia. The relationships were assessed at the level of three large forest regions, the northern and middle taiga of the Republic of Karelia, and the Karelian Isthmus (Leningrad region), based on 37 spruce, 66 pine, and 16 birch plots which were integrated with the International Cooperative Programme on Assessment and Monitoring of Air Pollution Effects on Forests (ICP Forests). Results Soil forming rock and land-use history partly explain the differences in the fertility of soil organic horizons between the forest ecosystems in northwestern Russia. Climatic factors are closely correlated with plant species richness, density and the fertility of soil organic horizons. Nutrient content in the organic horizons increased from poor to rich site types identified according to composition of understory vegetation and the occurrence of certain indicator species, i.e. Cajander’s forest site types. The most informative parameters in explaining differences between Cajander’s types were nitrogen, carbon to nitrogen ratio, exchangeable calcium, magnesium, potassium, and base saturation. Extractable phosphorus, carbon to nitrogen ratio, exchangeable calcium, magnesium, aluminum and base saturation were the most informative parameters in explaining differences between forest types identified within the Cajander types in accordance with the tree species composition, i.e. Sukachev’s forest types. The organic horizons of spruce and birch-dominated forests contained significantly more nutrients, compared to those dominated by pine. These differences were explained by differences in litter quality, and the crown shape and density of tree ...