Microbial community response to changes in substrate availability and habitat conditions in a reciprocal subsoil transfer experiment. (February 2017)

• Record Type: Journal Article
• Authors: Preusser, Sebastian; Marhan, Sven; Poll, Christian; Kandeler, Ellen
• Is Part Of: Soil biology and biochemistry. Volume 105(2017)
• Page Start: 138
• Page End: 152
• Publication Date: 2017-02
• Subjects: Carbon cycle -- Stable isotope probing -- Phospholipid fatty acids (PLFAs) -- Soil microorganisms -- Micro-environment -- Micro-climate; Soil biochemistry -- Periodicals; Soil biology -- Periodicals; Sols -- Biochimie -- Périodiques; Sols -- Biologie -- Périodiques; Sols -- Microbiologie -- Périodiques; Bodembiologie; Biochemie; 631.46
• DOI: 10.1016/j.soilbio.2016.11.021
• Languages: English
• ISSNs: 0038-0717

Abstract

Abstract: While habitat conditions influencing the abundance of microorganisms in topsoil are well known, these dynamics have been largely unexplored in deeper soil horizons. We investigated the effects of different substrate availabilities and environmental conditions on microbial community composition and carbon flow into specific groups of microorganisms in subsoils using a reciprocal soil transfer experiment within an acid and sandy Dystric Cambisol from a ∼100-year old European beech ( Fagus sylvatica L.) forest in Lower Saxony, Germany. Containers filled with subsoil from 10 to 20 cm (SUB20) and 110 to 120 cm (SUB120) soil depths and with additions of different amounts of 13 C labelled cellulose (1% and 5% of the respective organic carbon content of both soil layers) were exposed either in their home field environment or transferred reciprocally between SUB20 and SUB120 horizons for periods of one, four and twelve months. During the exposure of twelve months, 13 C accumulated up to 15 percent in total microbial biomass and up to 25 percent in fungal PLFAs. Similar microbial 13 C incorporation rates in SUB20 samples located at either 20 or 120 cm depth indicated comparable microclimatic conditions in both soil environments with no depth-dependent effects on the decomposer communities. While low nitrogen availability (when primary C-limitation was alleviated) and water content limited bacterial growth and activity at both depths, fungal abundance and activity were less affected due to their ability to efficiently exploit resources in surrounding soil by hyphal growth and higher drought resistance. Consequently, bacterial PLFAs (phospholipid fatty acids) incorporated less 13 C than fungi. The relatively high, from 1% to 5% cellulose addition linearly increased, 13 C incorporation rates in SUB120 samples at 120 cm depth clearly showed the potential of efficient carbon turnover in deeper soil layers. Spatial separation between subsoil microorganisms and their substrates may therefore be an important factor influencing carbon accumulation in subsoil. Highlights: Reciprocal soil transfer as an approach to study natural C dynamics in subsoils. High 13 C cellulose incorporation into fungal community in subsoils. Dominance of fungal activity under nutrient and water limitation. Spatial separation as important factor for C accumulation in subsoils.