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Journal ArticleDOI

Composition of the microbial communities in the mineral soil under different types of natural forest

TLDR
In this article, the composition of soil microbial communities under 12 natural forest stands including oak and beech, spruce-fir-beech, floodplain and pine forests were quantified by substrate-induced respiration and chloroform fumigation-extraction.
Abstract
Phospholipid fatty acid (PLFA) patterns were used to describe the composition of the soil microbial communities under 12 natural forest stands including oak and beech, spruce–fir–beech, floodplain and pine forests. In addition to the quantification of total PLFAs, soil microbial biomass was measured by substrate-induced respiration and chloroform fumigation–extraction. The forest stands possess natural vegetation, representing an expression of the natural site factors, and we hypothesised that each forest type would support a specific soil microbial community. Principal component analysis (PCA) of PLFA patterns revealed that the microbial communities were compositionally distinct in the floodplain and pine forests, comprising azonal forest types, and were more similar in the oak, beech and spruce–fir–beech forests, which represent the zonal vegetation types of the region. In the nutrient-rich floodplain forests, the fatty acids 16:1u5, 17:0cy, a15:0 and a17:0 were the most prevalent and soil pH seemed to be responsible for the discrimination of the soil microbial communities against those of the zonal forest types. The pine forest soils were set apart from the other forest soils by a higher abundance of PLFA 18:2u6,9, which is typical of fungi and may also indicate ectomycorrhizal fungi associated with pine trees, and high amounts of PLFA 10Me18:0, which is common in actinomycetes. These findings suggest that the occurrence of azonal forest types at sites with specific soil conditions is accompanied by the development of specific soil microbial communities. The study provides information on the microbial communities in undisturbed forest soils which may facilitate interpretation of data derived from managed or even damaged or degraded forests. q 2004 Elsevier Ltd. All rights reserved.

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Soil moisture is the major factor influencing microbial community structure and enzyme activities across seven biogeoclimatic zones in western Canada

TL;DR: In this paper, the authors compared the structure and function of soil microbial communities in seven mature, undisturbed forest types across a range of regional climates in British Columbia and Alberta, and examined the variation in community composition within forest types.
Journal ArticleDOI

Quantitative assessment of the fungal contribution to microbial tissue in soil

TL;DR: This review of literature data indicated that fungi dominated microbial biomass, respiration or non-biomass microbial residues, with mean percentages obtained by the different methodological approaches varying between 35 and 76% in different soil groups, i.e. arable, grassland, and forest soils and litter layers.
Journal ArticleDOI

Who is who in litter decomposition? Metaproteomics reveals major microbial players and their biogeochemical functions

TL;DR: Fungi were found to be the main producers of extracellular hydrolytic enzymes, with no bacterial hydrolases being detected by the metaproteomics approach, providing evidence that the litter nutrient content and the stoichiometry of C:N:P affect the decomposer community structure and activity.
Journal ArticleDOI

Tree species influence on microbial communities in litter and soil: Current knowledge and research needs

TL;DR: The evidence that tree species influence the composition of the microbial communities in decomposing litter, forest floors, soil and the rhizo/mycorrhizosphere is examined to definitively deduce the influence of tree species.
Journal ArticleDOI

Experimental warming effects on the microbial community of a temperate mountain forest soil.

TL;DR: The 4 °C increase in soil temperature during the snow-free season had no influence on microbial community composition and biomass but strongly increased microbial metabolic activity and hence reduced carbon use efficiency.
References
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World Reference Base for Soil Resources

TL;DR: The World Reference Base for Soil Resources (WRB) as mentioned in this paper is a reference base for soil resources developed by the International Union of Soil Sciences (IUSS) for soil correlation.
Journal ArticleDOI

The use of phospholipid fatty acid analysis to estimate bacterial and fungal biomass in soil

TL;DR: The cell content of 12 bacterial phospholipid fatty acids (PLFA) was determined in bacteria extracted from soil by homogenization/centrifugation and the soil content of the PLFA 18:2ω6 was correlated with the ergosterol content, which supports the use of this PLFA as an indicator of fungal biomass.
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Determination of the sedimentary microbial biomass by extractible lipid phosphate.

TL;DR: The high content of plasmalogen phospholipids in these sediments suggests that the anaerobic prokaryotic Clostridia are found in the aerobic sedimentary horizon, which would require anaer aerobic microhabitats in the aerated zones.
Journal ArticleDOI

Shifts in the structure of soil microbial communities in limed forests as revealed by phospholipid fatty acid analysis

TL;DR: Analysis of phospholipid fatty acid composition of soils from two areas in the south of Sweden indicated that the increased pH caused a shift in the bacterial community to more Gram-negative and fewer Gram-positive bacteria, while the amount of fungi was unaffected.
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